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M US Army Corps of EngineersUICL Ui Los Angeles District SANTA ANA RIVER BASIN, CALIFORNIA AD-A204 545 1 Design Memorandum No. 1 PHASE II GDM ON THE SANTA ANA RIVER MAINSTEM including Santiago Creek 2 FEB 19U VOLUME 4 MILL CREEK LEE b I,, W 9 2 o004 August 1988

including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

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Page 1: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

M

US Army Corpsof EngineersUICL UiLos Angeles District SANTA ANA RIVER BASIN, CALIFORNIAAD-A204 545 1

Design Memorandum No. 1

PHASE II GDM ON THESANTA ANA RIVER MAINSTEM

including Santiago Creek

2 FEB 19U

VOLUME 4MILL CREEK LEE b I,, W

9 2 o004August 1988

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REPORT DOCUMENTATION PAGE READ INSTRUCTIONSBEFORE COMPLETING FORM

I. REPORT NUMBER 2. GOVT ACCESSION NO. 3. RECIPIENT'S CATALOG NUMBER

Design Memorandum No. 1

4. TITLE (and Subtitle) S. TYPE OF REPORT & PERIOD COVERED

Phase II GDM on the Santa Ana River MainstemIncluding Santiago Creek Final

Volume 4, Mill Creek Levee 6. PERFORMING ORG. REPORT NUMBER

8. CONTRACT OR GRANT NUMBER(-)

U S Army Corps of EngineersLos Angeles District

9. PERFORMING ORGANIZATION NAME AND ADDRESS 10. PROGRAM ELEMENT, PROJECT, TASKAREA & WORK UNIT NUMBERS

Engineering Division300 N Los Angeles StreetLos Angeles, CA 90012

11. CONTROLLING OFFICE NAME AND ADDRESS 12. REPORT DATE

Project Management Branch August 1988300 N Los Angeles Street 13 NUMBER OF PAGESLos An eles, CA 90012 108

14. MONITORING AGENCY NAME & ADDRESS(t different from Controlling Office) 15. SECURITY CLASS. (of this report)

Same as Controlling Office UnclassifiedIS.. DECLASSIFICATION/DOWNGRADING

SCHEDULE

16. DISTRIBUTION STATEMENT (of thlis Report)

Approved for Public Release; Distribution Unlimited

17. DISTRIBUTION STATEMENT (of the ebftrec entered In 3lock 20, If different from Report)

Approved for Public Release; Distribution Unlimited

IS. SUPPLEMENTARY NOTES

19. KEY WORDS (Continue on revere de Ift nec.esary ar.d identfly by block numb.r)

- Project Plan - Streambed Analysis - Sedimentation- Hydrology - Stability Analysis - Standard Project Flood- Hydraulic Design - Floodwall

20. ABSTRACT (-Co ot.e s --. r.. td* if u -d identir by block number)

This volume accompanies the Main Report and Supplemental EnvironmentalImpact Statement for the Phase iI General Design Memorandum for the SantaAna River Mainstem including Santiago Creek and contains the general design

/ information for the Hill Creek Levee.

DD ,. 1473 EoITON OF I NOV 65 IS OBSOLETE Unclassified

SECURITY CLASSIFICATION OF THIS PAGE (W?,en, D.e1 Entered)

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Design Memorandum No. 1

Volume 4

Santa Ana River Mainstem

including Santiago Creek, California

Phase II General Design Memorandum

MILL CREEK LEVEE

Accession For

hfTIS GRA&IDTIC TAB

ri tr;nn Uce t['z

Av"~1A £2ity odc3

Di t "

/

1\ .p

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SYLLABUS

This volume accompanies the Main Report and Supplemental EnvironmentalImpact Statement for the Phase II General Design Memorandum for theSanta Ana River Mainstem including Santiago Creek and contains thegeneral design for the Mill Creek Levee. '-The project economic data ispresented in Volume 9,"Economics and Public Comment and Response.". Therecommended flood control plan for the Mill Creek levee consists ofraising a portion of the existing levee from stations 70+00 to 88+70,extending the toe protection from stations 70+00 to 129+33.33 and fromstations 130+72 to 196+25.37, and constructing a floodwall along the topof the levee from stations 70+00 to 130+20 and from stations 130+72 to196+25.37. Esthetic treatment will consist of groupings of native treesand large shrubs planted along the landward side of the embankment.Total first cost for this element of the Santa Ana River Mainstemproject is estimated at $5,109,000.

lii

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PHASE II GDh LISTING W VOLWES

Main Report and Supplemental Environmental Impact Statement

Volume 1 Seven Oaks Dam

Volume 2 Prado Dam

Volume 3 Lower Santa Ana River (Prado Dam to Pacific Ocean)

Volume 4 Mill Creek Levee

Volume 5 Oak Street Drain

Volume 6 Santiago Creek

Volume 7 Hydrology

Volume 8 Environmental

Volume 9 Economics and Public Comment and Response

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PERTINENT DATA

Hill Creek Levee

Item Unit

Drainage Area 52 mi2

Peak discharge, SPF 33,000 ft3/s

Levee:Length 13,600 feetHeight (above streambed) 10 feet (Maximum)

Slopes:Streamward side (existing) IV on 2.25HNew (Sta 70+00.00 to Sta 88+70.00) IV on 2HLandward side IV on 2H

Top width 18 feet

Recommended floodwall:Length 12,573 feetHeight 7' 6" (Maximum)Toe extension on streamward side 12' 6" (Maximum)Toe slope IV on 2H

vii

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CONTENTS

Page

Syllabus .................................................. iiiPhase II GDM Listing of Volumes ........................... vPertinent Data ............................................ viiContents .................................................. ix

I. INTRODUCTION ................ .............................. I-iAuthorization ............................................. I-IScope and Purpose of Report ............................... I-ILocal Cooperation ......................................... I-i

II. PROJECT PLAN .............................................. II-1Description of the Project Area ........................... II-1Existing Flood Control Facilities ......................... 11-2The Flood Problem ......................................... 11-3The Authorized Plan ....................................... !1-3The Plan Recommended in this Report ....................... 11-3

Raised Levee ............................................ II-4Toe Protection .......................................... II-4Floodwall ............................................... I -4Esthetic Treatment ........ ............................. 11-5

Consideration of Other Alternatives ....................... 11-5

III. HYDROLOGY ................................................. Ill-1Introduction .............................................. III-1General ................................................... III-1Design Flood Peak Discharge ............................... 111-2

IV. HYDRAULIC DESIGN .......................................... IV-1Introduction .............................................. IV-1Existing Project Conditions ............................... IV-1Historic Flooding and Remedial Measures ................... IV-2Historical Damage ....................................... IV-2Rehabilitation .......................................... IV-4

ix

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Contents (Continued)

Page

Recommended Project ..................................... IV-5Streambed Analysis ........................................ IV-6General ................................................. IV-6Historic Trends ......................................... IV-6Impact on Design ........................................ IV-7

Sediment Ramping .......................................... IV-7Phenomenon Description .................................. IV-7

Hydraulic Analysis of Sediment Ramping .................. IV-9

Impact on Design ........................................ IV-1O

V. GEOLOGY, SOILS, AND MATERIALS ............................. V-I

Regional Geologic Setting ................................. V-7

Site Topography and Geology ............................... V-I

Faulting and Seismicity ................................... V-2

Groundwater ............................................... V-2

Investigations ............................................ V-2

Previous Investigations ................................. V-2

Recent Investigations ................................... V-3Investigation During Advertising Period ................. V-3

Field and Laboratory Testing Results ...................... V-3

Design Values ............................................. V-4

Foundation .............................................. V-4

Embankment and Toe Backfill ............................. V-4

Stability Analysis ........................................ V-4

Construction Considerations ............................... V-4

Excavation .............................................. V-4

Placement and Compaction ................................ V-5

Slope Protection ........................................ V-5

Construction Materials .................................... V-5Borrow Material Sources ................................. V-5Stone Materials ......................................... V-5

Concrete Materials ........................................ V-6Structural Elements ..................................... V-6Climatic Conditions ..................................... V-7Cements ................................................. V-7Cement Sources ........................................ V-7Pozzolans ............................................. V-9

Aggregates .............................................. V-9

Geologic Aspects of Aggregate Sources ..................... V-9General ................................................. V-9Lytle Creek ............................................. V-10

Santa Ana River ......................................... V-10San Gorgonio River ...................................... V-10

Aggregate Sources .......................................... V-10

Owl Rock Products ....................................... V-1O

4th Street Crusher ....................................... V-11

Beaumont Concrete Company ............................... V-14

C. L. Pharris ............................................ V-16

x

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Contents (Continued)

Page

Aggregate Costs ........................................... V-18Water ..................................................... V-18Admixtures ................................................ V-19Mix Design Requirements ................................... V-19Cost of Concrete .......................................... V-19Specification Requirements ................................ V-20

Cements ................................................. V-20Pozzolans ............................................... V-20Admixtures .............................................. V-20Aggregates .............................................. V-21

References ................................................ V-21

VI. STRUCTURAL DESIGN ......................................... VI-IFloodwall ................................................. VI-1References ................................................ VI-1Material Properties ....................................... VI-2

VII. RELOCATION OF STREETS, RAILROADS AND UTILITIES ............ VII-1

VIII. ACCESS ROADS .............................................. VIII-IGeometric Design .......................................... VIII-1Pavement Design Values .................................... VIII-1

IX. ENVIRONMENTAL ANALYSIS .................................... IX-!General ................................................... IX-1Environmental Impacts ..................................... IX-1

Sedimentation ........................................... IX-IWater Resources .......................................... IX-1

Hydrology and Water Use ................................ IX-IWater Quality .......................................... IX-I

Air Quality ............................................. IX-2Land Use and Social Concerns ............................ IX-2

Prime and Unique Farmlands ............................ IX-2Recreation ............................................. IX-2Growth Inducement ...................................... IX-2

Transportation and Utilities ............................ IX-2Facilities ............................................ IX-2Access ................................................. IX-2Transport of Borrow Materials ......................... IX-2

Noise................................................... IX-2Biological Resources ..................................... IX-3Cultural Resources ....................................... IX-3

Site Restoration ........................................... IX-3

X. DIVERSION AND CONTROL OF WATER DURING CONSTRUCTION ........ X-1

XI. REAL ESTATE REQUIREMENTS .................................. XI-1

xi

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Contents (Continued)

Page

XII. COST ESTIMATES ........................................... XII-First Costs ............................................ . XII-iOperation and Maintenance ............................... .. XII-lComparison of Estimates ................................... XII-i

XIII. DESIGN AND CONSTRUCTION SCHEDULE .......................... XIII-1

XIV. OPERATION AND MAINTENANCE ................................. XIV-1

Tables

No. Title

II-1 Mill Creek Levee Plant List ............................ 11-5IV-1 Post Project Flood Events, Rehabilitation .............. IV-3IV-2 Summary of Aggradation and Degradation Trends .......... IV-8

V-i Stone Sources .......................................... V-5V-2 Estimated Concrete Material Quantities ................. V-6V-3 Cement Prices .......................................... V-8V-4 Cement Shipping Prices ................................. V-8V-5 Physical Tests on Concrete Aggregates for: OWL ROCK

PRODUCTS COMPANY ....................................... V-12V-6 Physical Tests on Concrete Aggregates for: 4TH STREET

CRUSHER ................................................ V-13V-7 Physical Tests on Concrete Aggregates for: BEAUMONT

CONCRETE COMPANY ....................................... V-15V-8 Physical Tests on Concrete Aggregates for:

C. L. PHARRIS .......................................... V-17V-9 Estimated Unit Costs for Concrete Aggregates ........... V-18

V-10 Estimated Costs of Redimix Concrete .................... V-20XII-1 Summary of First Cost .................................. XII-2XII-2 Detailed Estimate of First Cost ........................ XII-3XII-3 Comparison of First Cost ............................... XII-5

XIII-1 Design and Construction Schedule ....................... XIII-2XIV-1 Annual Operation and Maintenance Cost .................. XIV-I

Figures

No. Title

1. Standard Project Flood2. Results of Chemical Test for Reactivity of Aggregate with Sodium

Hydroxide, Owl Rock Company

3. Results of Chemical Test for Reactivity of Aggregate with SodiumHydroxide, 4th Street Crushers

4. Results of Test for Length Change Due to Chemical Reaction in

Concrete Materials, 4th Street Crushers

xii

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Contents (Continued)

Figures (Continued)

No. Title

5. Results of Chemical Test for Reactivity of Aggregate with SodiumHydroxide, Beaumont Concrete Co.

6. Results of Test for Length Change Due to Chemical Reaction inConcrete Materials, Beaumont Concrete Quarry

7. Results of Chemical Test for Reactivity of Aggregate with SodiumHydroxide, C. L. Pharris

8. Results of Test for Length Change Due to Chemical Reaction inConcrete Materials, C. L. Pharris

9. Floodwall Loading Conditions

Plates

No. Title

1. Project Location2. Vicinity Map and Plan3. Plan and Profile station 196+25.37 to station 182+29.264. Plan and Profile station 182+29.26 to station 167+25.175. Plan and Profile station 167+25.17 to station 152+23.646. Plan and Profile station 152+23.64 to station 137+22.107. Plan and Profile station 137+22.10 to station 121+81.578. Plan and Profile station 121+81.57 to station 108+76.809. Plan and Profile station 108+76.80 to station 92+36.1810. Plan and Profile station 92+36.18 to station 76+40.5011. Plan and Profile station 76+40.50 to station 70+00.0012. Levee Cross Sections13. Levee Terminus and Transition Details14. Structure, Ladder and Gate Details15. Esthetic Treatment Plan station 196+25.37 to station 182+29.26

station 182+29.26 to station 167+25.1716. Esthetic Treatment Plan station 167+25.17 to station 152+23.64

station 152+23.64 to station 137+22.1017. Esthetic Treatment Plan station 137+22.10 to station 121+81.57

station 121+81.57 to station 108+76.8020. Drainage Basin21. Historical Streambed Profiles at Levee Stations 197+50 to 175+0022. Historical Streambed Profiles at Levee Stations 175+00 to 152+5023. Historical Streambed Profiles at Levee Stations 152+50 to 130+0024. Historical Streambed Profiles at Levee Stations 130+00 to 107+5025. Historical Streambed Profiles at Levee Stations 107+50 to 85+0026. Historical Streambed Profiles at Levee Stations 90+00 to 67+5027. Cross-Section Near Levee Station 96+0028. Regional Geology29. Regional Tectonic Map30. Fault and Earthquake Epicenter Map31. Sources of Aggregates, Cements, and Pozzolans

xiii

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I. INTRODUCTION

Authorization

1-01 Authorization for construction of the Mill Creek Levee iscontained in the Water Resources Development Act of 1986, 99th Congress2nd Session, Public Law 99-662. The project for flood control iscontained in the Report of the Chief of Engineers for the Santa AnaRiver Mainstem, including Santiago Creek, California, dated January 15,1982, except that, in lieu of the Mentone Dam feature of the project,the Secretary is authorized to plan, design, and construct a floodcontrol storage dam on the upper Santa Ana River. The fullauthorization language is presented in the Main Report.

Scope and Purpose of Report

1-02 This volume of the Phase II General Design Memorandum (GDM)describes the existing physical conditions in the project area andprovides definite design for the Mill Creek Levee. This Phase II GDMprovides the basis for project features, establishing the projectrights-of-way and easements, updating the project costs, assessing theenvironmental effects, and preparing contract plans and specifications.

Local Cooperation

1-03 This division of federal and non-federal responsibilities forlocal cooperation are outlined in the Main Report.

I-I

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II. PROJECT PLAN

2-01 Mill Creek (pl. 1) is a tributary to the Santa Ana River and islocated in San Bernardino County, California. The confluence of MillCreek and the Santa Ana River is approximately 5 miles northeast of theCity of Redlands. The City of Mentone lies 2 miles south of theconfluence. Mill Creek generally flows in an east to west direction andoriginates in the high mountain peaks about 18 miles east of the SantaAna River confluence. Maximum streambed gradients along the projectexceed 200 feet per mile.

Description of the Project Area

2-02 The area tributary to the Mill Creek Levee comprises about52 square miles (mi ), bounded on the north by the San BernardinoMountains, on the east by the San Gorgonio Mountains, on the south bythe Crafton Hills and Yucaipa Ridge, and on the west by the Santa AnaRiver. Elevations in the drainage area range from about 11,500 feetNational Geodetic Vertical Datum of 1929 (NGVD) at San Gorgonio Peak toabout 1,700 feet NGVD at the confluence of Mill Creek and the Santa AnaRiver. The average slope of the streambed in the project reach isapproximately 4 percent. Upstream from the project reach, the averagegradient of the main channel of Mill Creek is about 565 feet per mile.The physiographic features of the Mill Creek watershed make it one ofthe most severe sediment producers in the area. Mill Creek is confinedby an existing Federal flood control levee on the south side; however,the floodway is relatively wide.

2-03 Urban developments occur primarily in the south overbank areas ofthe Mill Creek alluvial plain. The Cities of Redlands and Mentone lieon the historic alluvial fan of Mill Creek. There are some agriculturallands in the north overbank area of Mill Creek and a river runhydropower plant, the Mill Creek Powerplant Number 1, owned by theSouthern California Edison Company.

II-I

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Existing Flood Control Facilities

2-04 Levees and floodwalls have been constructed at various times byFederal and local interests along the south bank of Mill Creek. Theoriginal Federal flood control project was a unit of the Santa Ana RiverBasin project, which was authorized by the 1950 Flood Control Act.Construction of the existing Mill Creek Levee was completed in 1960.The improvements integrated two stone masonry floodwalls constructedimmediately after heavy flooding in 1938 by local interests with WorksProgress Administration (WPA) funds. The Mill Creek Levee was d~signedfor a maximum flood capacity of 33,000 cubic feet per second (ft Is),providing Standard Project Flood (SPF) protection to the Cities ofMentone and Redlands, and to the surrounding urban areas.

2-05 The existing Mill Creek Levee consists of three levee segments.The upstream levee joins a 1,297-foot-long stone masonry floodwall. Thefloodwall extends from station 216+86.93 to station 203+89.59 and isabout 24 feet high with a base width of 10 feet and a top width of4 feet. At the base of the floodwall there were 6-foot-high, 5-foot-

wide and 20-foot-long groins, at 100-foot spacings. These groins have

been destroyed by flooding and sediment movement.

2-06 The upstream levee is 520 feet long and extends from station208+50.38 to station 203+30.20 where it joins a second masonry wall.The levee height varies from 5 to 9 feet above the streambed with acrest width of 18 feet. The side slopes are 1 vertical on 2.25horizontal on the river side and 1 vertical on 2 horizontal on thelandward side. The river side of the levee is protected with a groutedcobblestone layer varying in thickness from 18 inches at the toe to 12inches at the top. The revetment extends 12 feet below the lowest pointin the streambed along this reach.

2-07 The second masonary floodwall is 705 feet long and extends fromstation 203+30.20 to station 196+25.37. The wall was constructed at thesame time and to the same dimensions as the upstream masonry floodwall.At the downstream end, the masonry floodwall joins a middle levee.

2-08 The middle levee is 6,553 feet long and extends from station196+25.37 to station 130+72.00, ending at the crossing of Garnet Street(pl. 2). The levee height varies from 5 to 9 feet above the streambed.The top width, side slopes, and revetment are the same as the upstreamlevee. The height from the top of levee to toe of revetment varies from14 to 22 feet.

2-09 The downstream levee begins at Garnet Street as a tie back andthen extends downstream 6,575 feet from station 135+75 to station 70+00(pl. 2). The top width and side slopes are the same as the upstreamlevees. Between stations 135+75 and 88+70, the revetment is alsoidentical to that on the other two levees and the height from top oflevee to toe of revetment varies from 11 to 20 feet. The levee heightin this reach varies from 4 to 11 feet above the streambed. Fromstation 88+70 to station 70+00 the revetment consists of a 24-inch layer

11-2

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of dumped stone extending from the top of the levee to the streambed.The toe of the revetment extends 2 feet below grade. The height of thelevee in this reach varies from 2 to 4 feet above the streambed.

2-10 Since construction of the existing Mill Creek Levee, floodssmaller than the design capacity of the project have overtopped thelevee and caused damage. Additional features, such as gabion deflectionbaffles, mid-stream "pushed-up" dikes, and low flow pilot channels, havebeen constructed under Federal emergency programs to rehabilitate andimprove the project. These features are further discussed in theHydraulic Design section of this report.

2-11 The Mill Creek Levee was constructed in 1960 for $653,720. Acumulative total of $1,087,000 has been spent under Federal emergencyprograms to rehabilitate the project after flood damage.

The Flood Problem

2-12 The flood problem results from overtopping of the levee duringflows of less than design capacity, which transport large amounts ofsediment while following a meandering flow pattern. This sediment hasdeposited on the levee slopes and created a ramp, allowing flows toescape. Scour in other reaches has undermined the revetment in thepast. For a complete description of the flooding phenomena andhydraulic design see section IV.

The Authorized Plan

2-13 The 1980 Santa Ana River Phase I GDM plan consisted of raising theexisting levee and constructing an additional 1.2 miles of levee toconvey flows to the proposed Mentone Reservoir. The authorized planalso included a groin field along the levee extension to protect thelevee and divert flows away from the Mentone Dam spillway. Theestimated cost of construction for the improvements was $15,095,000(October 1979 price levels).

The Plan Reoommended in this Report

2-14 The recommended flood control plan for Mill Creek Levee is similarin concept to the authorized plan, except that the channel will not beextended an additional 1.2 miles downstream; the existing levee toeprotection will be deepened, and a concrete floodwall will beconstructed on top of the levee berm in lieu of raising the entire levee(pls. 3 through 13). Replacement of Mentone Dam with Seven Oaks Damremoved the need to extend the Mill Creek Levee to protect the MentoneDam spillway from sediment deposition. Details of the recommendedimprovement to the Mill Creek Levee are described in the followingparagraphs.

11-3

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RAISED LEVEE

2-15 The levee will be raised 4 feet at station 70+00 tapering down to0 feet at station 88+70. The side slope will have an average height of18 feet and will be protected with 18 inches of grouted stone. The

existing ungrouted revetment will remain in place beneath the ntw side

slope.

TOE PRONECTION

2-16 The recommended toe protection for the Mill Creek Levee will be

constructed of grouted stone revetment with a slope of 1 vertical on

2 horizontal. It consists of the following:

(1) From station 70+00 to station 88+70, grouted stone slope

protection will be constructed as part of the levee

raising. The new toe depth will vary from 6.5 to 9 feet

deeper than the existing ungrouted toe.

(2) From station 88+70 to station 129+33.33, the toe of the

existing grouted revetment will be deepened. The new toe

depth will vary from 2 to 8 feet below the existing toe and

will consist of 18-inch-thick grouted stone.

(3) From station 130+72 to station 196+25.37, the toe of theexisting grouted revetment will be extended. The new toe

depth will vary from 8 to 12.5 feet below the existing toe

and will consist of 18-inch-thick grouted stone.

FLOODWALL

2-17 The recommended floodwall for the Mill Creek Levee will be

constructed along the existing top of the levee from station 88+70 to

station 130+20 and from station 130+72 to station 196+25.37 and along

the top of the raised levee between station 70+00 and station 88+70.

The height of the wall will vary from 5 feet 11 inches to 7 feet

6 inches. The wall will be designed as an inverted T-wall. The footing

will be 6-foot in length and will rest on top of the levee. The

thickness of the stem and the footing will be 8 inches and 10 itches

respectively. A cutoff wall, 3 feet deep and 10 inches thick, will be

provided at the end of the footing (river side). See plate 14 for a

typical floodwall section. The wall will be provided with two 3-foot

wide by 6-foot high access gates. The gates will be designed as

floodgates and will provide access to the existing catwalks for

diversion fdoillties at station 118+10 and station 157+00. Also, ladder

rungs will be provided at 300-foot intervals to assist viewing the river

side over the floodwall from the access road (pl. 14).

11-4

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Ea'mWnC TREUlTM

2-18 Groupings of native trees and large shrubs (table 1I-1) will beplanted on the landward side of the embankment, along the levee reachupstream of Garnet Street and the one-third distance of levee downstreamfrom Garnet Street, to reduce the unnatural horizontal line created bythe long floodwall. The plantings will be established by a singlemainline drip irrigation system. The esthetic treatment plan is shownon plates 15 through 17.

2-19 No coloring of the floodwall will be necessary since the existingpredominant grayish-white coloration of the riverbed is similar toconcrete. No esthetic treatment will be necessary on the river side ofthe levee since this side is generally visible only from greatdistances. The following plant species will be considered for plantingwithin the rights-of-way:

Table II-1. Mill Creek Levee Plant List.

Trees:

Black Willow Salix gooddingiiRed Willow Salix laevigataArroyo Willow Salix lasiolepisGolden Willow Salix lasiandraFremont Cottonwood Populus fremontiiCalifornia Sycamore Platanus racemosa

Shrubs:

Common Buckwheat Eriogonum fasciculatumBrittle Bush Encelia farinosaChamise Adenostoma fasciculatumWhite Sage Salvia apianaCalifornia Sagebrush Artemesia californicaMexican Elderberry Sambucus mexicanaMule Fat Baccharis glutinosaSugar Bush Rhu3 ovataHairy Yerba Buena Eriodictyon trichocalyx

Consideration of Other Alternatives

2-19 The following alternatives were also considered during this PhaseII GDM study:

a. Raising the levee with additional compacted fill andoonstructing groin fields and gabion deflection baffles at3trategic locations.

11-5

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b. Raising the levee with additional compacted fill and relocatingthe Garnet Street Bridge to improve the flow direction andcapacity through the bridge.

a. Constructing a parallel levee along the river side slope of theexisting levee and using the existing levee as a back-up in theevent of overtopping.

Each of the above alternatives also involved increasing the depti of he

levee toe protection approximately 10 to 15 feet.

2-20 As the flow capacity of the existing levee was adequate, raisingthe existing levee with additional compacted fill was considered forcontrolling the sediment ramping effect (described in the hydraulicdesign section of this report) during events below the SPF. Increasingthe height of the sloped levee face was not efficient because sedimentramps build higher on the slope surface. The cost of groin fields andgabion deflection baffles was extremely high and functionallyquestionable. The parallel levee concept could be implemented withinthe existing rights-of-way, but the costs exceeded the recommended plan.

2-21 Relocation of Garnet Bridge was considered as a possible solutionto improve flow conditions and prevent flows from impinging directly onthe levee face downstream from the bridge. The cost of constructing anew bridge over 400 feet long was estimated at about $2,000,000 and theeffectiveness to eliminate the flow impingement was questionable.

2-22 The historic performance of the levee and the WPA masonry walls

indicates that the vertical-faced masonry wall has effectively deflecteddebris and is less susceptible to build-up of sediment ramps than thesloped-face levee. Therefore, floodwalls were evaluated andsubsequently selected as the recommended plan. The floodwalls werefound to be the least costly alternative evaluated.

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III. HYDROLOGY

Introduction

3-01 Development of the hydrology for the original Mill Creek Levee waspresented in the report titled "Hydrology, Santa Ana River andTributaries, California," which was submitted as enclosure 2 to theDistrict Engineer's report dated 1 November 1946 and titled "Report ofSurvey of Santa Ana River and Tributaries, California, for FloodControl." The results of the hydrologic engineering studies werepresented in "Design Memorandum No. 1, Hydrology for Mill Creek Levees,"dated June 1958.

3-02 Hydrologic engineering evaluations conducted during the Phase IIstudies for the Mill Creek Levee and the entire Santa Ana River MainstemProject are presented in Volume 7, Hydrology, of this Phase II GDM.This section presents a brief description of Mill Creek and presents thedesign discharge for the existing levee.

General

3-03 The Mill Creek watershed (pl. 20) in the San BernardinoMountains, has a drainage area of 52 mi . Elevations range from11,502 feet at San Gorgonio Peak to 1,700 feet at the confluence withthe Santa Ana River. The principal channel of Mill Creek flows westerlyand has an average gradient of 565 ft/mile for the area upstream fromthe levee. The maximum gradients of the smaller tributaries exceed1,900 ft/mile. The watershed is presently in a natural undevelopedstate and is expected to remain in that state during the life of theproject. The existing Mill Creek levee and some channel stabilizationimprovements are the only existing flood control structures on MillCreek.

3-04 Mean seasonal precipitation for the project drainage area rangesfrom about 45 inches in the headwaters to about 20 inches at the site ofthe levee and averages about 32 inches. Nearly all precipitation occurs

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during the months of December through March. Rainless periods of

several months during the summer season are common. Most precipitation

in the drainage area results from general winter storms that are

associated with extratropical cyclones of north Pacific origin. Major

storms consisting of one or more cyclonic disturbances, occasionally

last 4 days or more, and result in intense precipitation over largeareas. Thunderstorms that may result in intense precipitation during

short periods over small areas occur occasionally either in associationwith general storms or independently. Summer thunderstorms and tropical

cyclones are infrequent. Snow is common in winter at the higher

elevations, but records indicate that peak flows resulting from rainfallare usually not affected appreciably by snowmelt.

3-05 Runoff concentrates quickly from the steep slopes in the mountains

and hydrographic records show that the streamflow increases rapidly inresponse to effective rainfall. High-intensity rainfall, in combination

with the effects of steep gradients and possible denudation by fire, can

result in highly intense, debris-laden floods. Except for a few days in

some years, Mill Creek streamflow is perennial upstream from the canyon

mouth, but intermittent in the levee reach and usually dry in the summer

season.

Design Flood Peak Discharge

3-06 The design flood peak discharge of 33,000 ft3 /s, used for theentire levee reach, is the standard project flood (SPF) peak

discharge. The SPF peak discharge was derived from the SPF hydrograph

(fig. 1), which was developed by critically centering a general winter

standard project storm over the Mill Creek watershed upstream of itsconfluence with the Santa Ana River.

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IV. HYDRAULIC DESIGN

Introduction

4-01 Hydraulic analysis and design for the recommended flood controlimprovements are in accordance with procedures in EM 1110-2-1601,"Hydraulic Design of Flood Control Channels." Background information onthe project was obtained from Mill Creek historical records documentedin "Report on Engineering Aspects--Floods of January and February 1969,"(compiled in 1974 by the Los Angeles District) and from field data foundat local archives. The recommended project plan is designed to containall flood discharges up to the Standard Project Flood of 33,000 ft3/s.

Existing Project Conditions

4-02 About 2 miles upstream of the project, Mill Creek flows out of anarrow canyon onto an alluvial fan and divides into a number of smallerchannels. A rock outcrop on the left bank just upstream of the projectcauses the channel to turn to the right. High ground on the right bankconfines the debris cone to a narrow channel. Stone masonry floodwallsbuilt in 1938 tie into the left bank rock outcrop and directs thefloodflows to the high ground on the right bank (pl. 2). The projectreach begins at the existing Corps levee which ties into the masonryfloodwall.

4-03 The original Corps project, completed in 1960, consists of asingle levee in three segments (total length 2.6 miles) on the southbank of Mill Creek and grading of the channel in the vicinity of thelevee. The levee side slope was revetted with grouted stone except forthe downstream 1,870 feet (stas. 70+00 to 88+70) where dumped stone wasplaced on the levee slope. The top of the levee is between 4 and11 feet above the design grade, and the grouted stone extended to a toedepth at least 7 feet below the design grade. Structures in the projectreach included Garnet Street Bridge (sta. 130+00) and two Bear ValleyMutual Water Company aqueducts (levee stas. 68+00 and 196+00).

4-04 Mill Creek Levee confines floodwaters to the extreme right of thealluvial fan, which in recent geologic time has been its natural course.In the flood of 1938, however, before the stone floodwalls were built, aflow split occurred at this location and floodflows were diverted down a

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manmade irrigation channel called "The Zanja" on the left side of thefan (pl. 2). Redlands, the major population center on the Mill Creekalluvial fan, sustained damage in 1938 from the flooding Zanja.

4-05 Through the project reach, Mill Creek maintains a slope of about4 percent. The channel thalweg contacts the levee at the upstream end,but moves to the right side of the channel through the Garnet StreetBridge, and continues on the right side downstream to the Sinta AnaRiver. The existing levee was designed to convey 33,000 ft /s with5 feet of freeboard for bank to bank flow. However, smaller magnitudefloods have produced meandering flows which have attacked and damagedthe levee.

4-06 Since 1960, the existing levee has prevented floods from damagingthe nearby population centers of Mentone and Redlands. But Los AngelesDistrict engineers inspecting the levee during and after major floods

have concluded that the levee has failed to perform as intended. Thereason for this failure is the instability of the channel bed. Small

flows that break away from the main channel transport massive quantitiesof sediment, including large boulders. Upon contact with the levee,these meandering "cross-channels" deposit ramps of material on the leveeslopes, sometimes to the extent that flows overtop the levee.Alternately, these attacking flows scour below the levee toe and causerevetment collapse. Continuing development has increased the need forsafe conveyance of Mill Creek floodwaters down the right side of the fan.

Historic Flooding and Remedial Measures

4-07 Five damaging floods occurred on Mill Creek after completion ofthe original levee project in 1960. Rehabilitation measures were under-taken after each flood and, in 1970, after extensive watershed burns.Historic profiles and cross-sections are shown on plates 21 through 27.Post-project flood events and associated rehabilitation costs aresummarized in table IV-1.

HISTOR:CAL DMAGE

4-08 Much of the 1965 flood damage was due to the natural phenomena ofmeandering and braiding. While the main channel safely conveyed most ofthe flood through the project reach, minor flows broke away at severalplaces and directly contacted the levee. The impingement of theseattacking channels caused local scour in some reaches and heavy deposi-tion in others. Near levee station 195+90, the channel scoured 10 feetbelow the channel elevation at the levee, destroyed a 24-inch diameterpipeline, and then deposited back 7 feet of sediment. At this samelocation an 8-foot section of levee toe revetment was carried away bythe flood. Deposition against the masonry floodwall (upstream from theexisting levee) occurred to within 2 feet of its top, Heavy depositionagainst the levee occurred at several places upstream of Garnet Streetbetween stations 160+00 and 196+00. Minor levee overtopping occurred atlocations in this reach where the stream deposited material nearly tothe levee top.

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Table IV-1. Post Project Flood Events, Rehabilitation.

Original Construction:

Date COE Design Peak (cfs) Federal Cost ($)

1960 33,000 $653,720

Damaging Flood Events:

COE Peak-"i USGS Peak2 '

Date Estimate Estimate Damage Type

22 Nov 1965 6,600 10,000 Levee, pipeline

6 Dec 1966 10,000 10,000 Levee, fence

25 Jan 1969 18,100 35,400 Levee, Garnet St.,gabions

25 Feb 1969 18,000 7,500 Levee, gabions

2 Feb 1978 5,400 5,400 Gabions

Rehabilitation:

Date Type Federal Cost ($)

1965 Levee repair, channel excavation $136,000and grading

1967 Levee repair, channel excavation 355,000

and grading, gabion baffle con-struction

1969 Levee repair, channel excavation 139,000and grading, gabion repair, addi-tional gabion baffle construction

1970 Channel excavation, berm construction 345,000

1978 Gabion repair, channel excavation 112,000

and grading

TOTAL $1,087,000

/ At Corps of Engineers levee, about 3 milei downstream of U.S.G.S.

gauge.2 At bridge on State Highway 38.

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4-09 Damage in 1966 was very similar to that of 1965 except that it wasless severe upstream from Garnet Street and more severe downstream. AtGarnet Street, sediment plugged the bridge and was deposited 3 feetthick on the deck. Downstream from Garnet, scour to and below the leveetoe caused some revetment damage (pl. 24). Near station 95+00 Sedimentdeposition formed a ramp (see paras. 4-26 to 4-34) allowing about 1,000ftl/s to overtop the levee. In addition, part of the ungrouted levee(stas. 75+00 to 77+00) was completely destroyed by the scour action ofmeandering and braiding flow which had separated from the main channel.

4-10 The flood of January 1969 caused severe deposition in places bothupstream and downstream from Garnet Street. Minor overtopping of flowsoccurred at the upstream location, but flows were diverted back into thechannel by high ground. Overtopping flow estimated at 1,000 ft3/s alsooccurred in the downstream reach ne r station 90+00. Garnet Streetbridge was flanked by about 1000 fti/s which broke away on the upstreamleft bank and destroyed a section of the roadway approach. Flow throughthe bridge severely undermined but did not topple the downstream gabiondeflection baffles (see para. 4-14).

4-11 A second 1969 flood, in February, continued some of the damage ofthe January flood. The flow overtopped the levee again downstream ofGarnet Street, and gabions were undermined in additional places. Theungrouted downstream end of the existing levee (stas. 70+00 to 73+00)was completely destroyed by the scour action of meandering and braidingflow which had separated from the main channel.

4-12 Flooding in February of 1978 caused minor damage. The gabiondeflection baffles placed upstream of Garnet Street after the 1969flooding were undermined but did not topple.

REHABILITATION

4-13 After each flood the levee was restored to its original condition(table IV-1). Extensive channel work was performed to hinder meanderingand braiding patterns. A pilot channel was excavated after each flood,and the material used tj regrade the channel to remove "cross-channels"and restore a 2.5 percent slope streamward from the levee. In 1970,excavated material was also used to construct a berm on the north sideof the floodplain in an effort to disrupt the "cross-channel" patterns.

4-14 After the 1966 flooding, further structural measures wereundertaken to try to prevent "cross-channels" from setting up anddirectly attacking the levee. Downstream of Garnet Street two gabiondeflection baffles were constructed. The length totaled about 1,500feet. In 1969 these gabion structures were repaired ard lengthenedanother 750 feet and an additional 1100 feet of gabion deflectionbaffles were placed upstream of Garnet Street (pl. 2). The upstreambaffles were repaired after the 1978 flood severely undermined them.

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4-15 Damages from historic post-project floods on Mill Creek have beenalmost exclusively incurred to flood control structures such as thelevee or gabion deflection baffles. Only the damage to Garnet Street in1969 and to a private fence in 1966 were unrelated to flood control

structures.

RECOHENED PROJECT

4-16 The recommended project (pls. 3 through 14) is an improvement ofthe original project required to assure conveyance of the standardproject flood. The re I ommended project will contain the designdischarge of 33,000 ft Is; provide for long term aggradation,degradation trends; and control local scour and deposition.

4-17 The components of the recommended project are:

a. Raising the top of the existing levee between station 70+00, thedownstream end of the project, and station 88+70. The leveewill be raised 4 feet at station 70+00 and taper to a 0 heightincrease at station 88+70.

b. Grouting the riprap levee face between stations 70+00 and 88+70.

c. Extending the existing levee toe an average of 7.5 feet betweenstations 70+00 and 129+33.33, an average of 8.5 feet betweenstations 130+72 and 155+00 and an average of 10 feet betweenstations 155.00 and 196+25.37 the upstream end of the project.

d. Constructing a vertical floodwall, average height of 6 feet, ontop of the levee from stations 70+00 to 130+20 and from stations130+72 to 196+25.37.

e. Restoring a 100-foot strip of streambed adjacent to the levee towithin 7 to 10 feet of the top of the levee. This strip will bemaintained after each flood event.

4-18 The vertical floodwall will provide a minimum of 9.5 feet offreeboard above the main channel SPF water surface, a minimum of8.2 feet above the main channel energy grade line, a minimum of 4.5 feetabove the water surface for the impinging flow channel attacking thelevee, and a minimum of 2.5 feet above the energy grade line of that

water surface (see para. 4-31).

4-19 The recommended project eliminates the need for further gabionbaffles construction and repair. The "line of protection" provided bythe levee with the proposed project in place is designed to withstanddirect attack from cross-channels.

4-20 The need for excavation of pilot channels and extensive streambed

grading after each flood is also eliminated by the recommended project.While some grading will be required, it will be limited to the 100-footstrip of streambed next to the levee. This grading will function moreto reduce the starting elevation of ramping deposition on levee slopes(see paras. 4-26 through 4-34), than to hinder cross channels.

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4-21 Analysis of historic scour at the levee was the basis for

determination of required levee toe depth (pls. 3 through 11). Therecommended toe elevation was established by identifying the maximumhistoric depth of scour and providing an additional depth of 5 feet toaccount for uncertainties. The streambed elevation at the levee will bemaintained between 7 and 10 feet vertically below the top of thelevee. The 7-foot upper limit was set to insure that the floodWall willnot be overtopped by flows due to ramping. Whereas, the 10-foot lowerlimit was set to insure that the revetment will not fail due to localscour. The downstream reach (stas. 70+00 to 88+70) is aggrading, thestreambed will be maintained at the minimum 7 feet vertical depth fromthe top of levee. In the upstream reach (stas. 160+00 to 196+25) thestreambed is degrading, so the streambed will be maintained at a maximumdepth of 10 feet below the top of the levee.

Streambed Analysis

G KRAL

4-22 On Mill Creek, the primary cause of flooding problems isundesirable sediment movement. Floodwaters are comprised not only ofrapidly flowing water, but also of a range of flowing sediment from finesand to large boulders. During a flood the stream will alternatelyscour and deposit material depending on rapidly fluctuating sediment

transport capacity. The creek's ability to move large quantities ofboulders, in particular, has been a cause for concern. An analysis of

sedimentation trends on Mill Creek was conducted as an essential factorin the hydraulic design. Aggradation and degradation are long-termsedimentation processes.

4-23 If the streambed was stable, the water surface of the StandardProject Flood would be 3.7 feet below the top of the existing levee

(pls. 21 through 26). This water surface was calculated using the Corpsprogram HEC-2, with cross-sections spaced an average of 400 feet apart,and Manning's n-values in the range of .07 to .09. The high n-values

reflect not only the predominance of large diameter material, but alsobraided channel bedforms. In addition, a sensitivity analysis onroughness showed that the water surface, often approaching criticaldepth, is not highly sensitive to the choice of n-value. Aggradation,however, increases the water surface. Degradation increases the abilityof the stream to undercut the existing levee toe. A final threat to

successful functioning of Mill Creek Levee has been a phenomenon called

"sediment ramping", which is discussed in paragraphs 4-26 to 4-34.

HISTORIC TREIDS

4-24 Trends of aggradation and degradation were analyzed by comparingthe topography of three different years: 1958 Corps mapping from theoriginal project, San Bernardino County mapping (dated 1964 downstreamfrom Garnet Street and 1967 upstream from Garnet Street), ane 1987 Corpsmapping. The streambed was divided into 80 cross-sections, showing

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change in streambed elevation over a 30-year period. Plate 27, for

example, shows that at a cross-section near levee station 96+00(downstream from Garnet Street) channel aggradation is a steady trend.

Table IV-2 summarizes the results for the entire project reach. Thepredicted 100-year trend is computed by taking the average trend over

the 30 years of record, adjusting for estimated human impact, andmultiplying by 1.5 (a factor to account for uncertainty). During its30-year lifetime the existing project has experienced a 50-year flood,two 27-year floods, and three other floods greater than 12-year infrequency. The predicted 100-year aggradation and degradation trendswere derived by considering this full range of normal streambedactivity. Human impacts include Garnet Street roadway and bridge,channel excavation and grading, and gabion deflection baffles.

IMPACT ON DESIGN

4-25 The Mill Creek hydraulic design accounts for aggradation anddegradation trends in the following ways: the levee will be raised fourfeet above its existing height at station 70+00, transitioning to theexisting top of levee at station 88+70. This will offset the highaggradation trend at the lower end of the project. Wall heights willnot in general reflect aggradation trends. The overriding factor inlevee overtopping, and thereby the wall height, is not aggradation, butrather the sediment-ramping effect discussed in the next section (paras.4-26 through 4-34). In addition, the freeboard will account for thegeneral instability of the streambed. Degradation, however, isaccounted for in the design of the levee toe depth.

Sediment Ramping

PHENOMENON DESCRIPTION

4-26 The flow in Mill Creek is typical of high-gradient naturalstreams. It is highly unstable, nearly always subcritical butapproaching critical depth. Chutes of supercritical flow develop, butare short and intermittent. The stream, instead of flowingsupercritically straight down the alluvial fan slope, breaks from thesteeper path, curving to less steep cross-fan slopes. The flowcontinuously scours and deposits sediment as it meanders and dividesinto braided channels.

4-27 The phenomenon of "sediment ramping" occurs when a meanderingchannel ontacts the levee. During floods larger than about5,000 fts/s, the meandering and braiding actior. of the stream causessmaller flows to break away from the main channel. These smaller flowsgenerally scour and meander their own channels and often come in contactwith the levee. Upon initial contact, a sudden change in flow directioncauses local scour. This material, in addition to the incoming sedimentload, gives the stream its full sediment capacity.

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Table IV-2. Summary of Aggradation and Degradation Trends.*

100-year 100-year 100-year 100-yeartrend trend trend trend

Station (channel) (levee) Station (channel) (levee)

70+00 130+00to +3.5 +3.8 to -3.0 +4.5

75+00 135+00to +5.5 +3.8 to -3.0 +3.5

80+00 140+00to +5.5 0.0 to -4.5 +3.0

85+00 145+00to +4.5 +1.8 to -4.5 +4.8

90+00 150+00to +5.3 +1.5 to -4.5 +4.5

95+00 155+00to +5.3 -0.8 to -4.5 +3.8

100+00 160+00to +4.8 -4.5 to -3.8 -2.3

105+00 165+00to +2.0 0.0 to -3.8 -1.5

110+00 170+00to +0.8 +4.5 to -4.5 -3.0

115+00 175+00to -3.0 0.0 to -4.5 -2.3

120+00 180+00

to -1.5 +2.3 to -4.5 -3.0125+00 185+00

to -3.8 0.0190+00

to -4.5 -1.5195+00

*The 100-year trend is the average predicted change in elevation of thechannel bed in feet. The column for channel values indicates the trendfor the main channel only and does not include the full bank to bankfloodplain. The column for levee values indicates the trend for the100-foot strip of streambed next to the levee. Human impacts have beenaccounted for and include the following: bridge and roadway, channelexcavation and grading, and gabion deflection baffles.

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4-28 Such attaiking channels have been observed to carry flows up to aK few thousand ft Is with bottom widths up to 50 feet. They curve away

from the main channel at angles near 25 degrees on slopes in the rangeof .035 to .05. Attacking channel flow is highly unstable, undulatingand breaking into whitewater. As it flows parallel to the levee,sediment begins to drop out and a natural levee forms on the channelwardside. The attacking channel thus confines itself to the levee until itregains the scour capacity to break from its own levee formation.Another factor in deflecting the attacking channel back toward the mainchannel is that the longer this channel remains confined to the levee

the steeper the channelward slopes become.

4-29 The steepening channelward slope is due to the fact thatdeposition by the attacking channel not only builds a natural levee butalso a rising invert or ramp (see para. 4-30). The quantity and extentof the deposition in the form of a ramp is a function of the duration offlow. The resulting profile slope of the attacking channel flattensgradually during the flood. Field observations of actual ramps at MillCreek have shown that the ramp tends to approach a .02 slope. Since thetop of levee slope is about .04, the flatter ramp slope will intersectthe top of levee at some downstream location. As a result the flow on

the ramp overtops the levee.

HYDRAULIC ANALYSIS OF SEDIMENT RAMPING

4-30 The purpose of the sediment ramping analysis is to determinerequired wall height, which is a function of ramp length. A ramp with a

2 percent slope will "rise" to meet the top of levee (4 percent slope)at a rate of 2 feet vertically per 100 horizontally. Note that the rampslope is not adverse. Given the elevation that ramping begins (thestreambed elevation at the levee), and the length that a ramp will reachduring a flood, the required wall height may be calculated.

4-31 Ramp length is a function of the full flood hydrograph (dischargeand duration), the attack channel hydrograph, sediment discharge, andsediment volume required for ramp and natural levee building. TheStandard Project Flood predicted ramp length was determined in thefollowing manner:

a. A typical attacking channel size, shape, and slope was estimated

from field observation, historical data, and attacking channeldischarge. Ten percent of the total design flow was used tocalculate the sediment volume for the levee ramp.

b. Sediment discharge was computed using he best availableequation (Meyer-Peter), calibrated with Mill Creek flood data.Since two 50-year floods have occurred on Mill Creek since theexisting levee was constructed, the sediment discharge equationvias adjusted to match observed ramps. It was then used tocompute the SPF sediment discharge.

c. Sediment accumulation resulted because incoming sedimentdischarge was calculated to be more than outgoing (due toflattening slope). The difference between incoming and outgoing

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was the sediment discharge available for ramp and natural levee

building. This sediment volume was calculated from the sedimentaccumulation hydrograph by dividing by the flood duration.

d. Historical field data indicated that the ramp tends to Approacha 0.02 slope, so ramp volume was computed as a function of ramp

length and size of typical attacking channel. By trial and

error a ramp length of 170 feet was determined.

e. The maximum height of the ramping channel water surface wasdetermined by calculating critical depth at the flood peak. Thewater surface for SPF resulted in a depth above the existinglevee top of 1.4 feet. The corresponding height of the energygrade line above the top of the levee was 3.5 feet.

IMPACT CM DESIGN

4-32 A floodwall was chosen as the best engineering solution to prevent

levee overtopping. A vertical wall face will be more effective indeflecting the attacking flow into the channel. Field observations haveconcluded that sediment does not climb as well against a wall as on asloping levee face.

4-33 The ramp length was calculated assuming an initial streambed

elevation of 7 feet below the top of levee, which is true for much ofthe project reach, since the design requires maintenance of this minimum7-foot clearance for a 100-foot strip of streambed next to the levee.

4-34 Freeboard was incorporated into the wall height calculation. A6-foot wall provides freeboard of 4.5 feet above the water surface and2.5 feet above the energy grade line. This accounts for uncertainties

in the calculations as well as for the general instability of the

streambed.

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V. GBOLOGY, SOILS AND MATERIALS

Regional Geologic Setting

5-01 The Mill Creek Valley is located at the southern base of the SanBernardino Mountains, which are in the eastern part of the TransverseRanges physiographic province. The Transverse Ranges province is anelongated geomorphic and structural unit that trends essentiallyeast-west, and is made up of chains of parallel mountain ranges andvalleys extending from Point Arguello eastward to the southern MojaveDesert. The principal geomorphic and structural features of theTransverse Ranges lie across the grain of adjacent physiographicprovinces, which are strongly influenced by the northwest-southeast-trending San Andreas fault system (pl. 28). Within and bounding theTransverse Ranges province are other major fault zones that have beenactive during the same span of geologic time that the San Andreas systemhas been active. Rock units within the province are represented byPrecambrian plutonic and metamorphic types, and complex sections ofCretaceous and younger plutonic and sedimentary rocks.

Site Topography and Geology

5-02 The project is located in an east-west trending valley whichextends from the mouth of Mill Creek Canyon on the east to the MillCreek/Santa Ana River confluence on the west. The valley is bounded bythe San Bernardino Mountains on the north and the Crafton Hills on thesouth, and is 1 to 2 miles wide. Elevations in the project area varyfrom 1,800 to 2,300 feet above NGVD, with a westward gradient of about220 feet per mile. The existing structures are founded primarily onrecent alluvium deposited by Mill Creek in a strip less than 1,000 feetwide along the center of the valley. Quaternary alluvium is exposed inthe remaining portion of the valley floor, underlying the Recentalluvium and resting on bedrock. The total thickness of alluvium isgenerally 100 to 200 feet along the center of the valley. In thevicinity of the levees at Garnet Street, however, there are occasionalexposures of bedrock, consisting of Precambrian pelona schist andTertiary quartz monzonite.

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Faulting and Seisicity

5-03 The region surrounding the project is highly faulted andtectonically active (pls. 29 and 30). The Crafton fault, a northeast-trending normal fault, extends under the project structure near GarnetStreet. This fault is part of the Crafton Hills horst and grabencomplex, which has been active in both Pleistocene and Recent time. Thesouth branch of the San Andreas fault is located about a mile north ofthe project, and is the dominant seismic feature in the area. Thisstretch of the San Andreas fault has exhibited a slip rate of as much as25 mm/yr., and is considered capable of a maximum credible earthquake ofmagnitude 8+. Assuming an epicenter 1 mile from the project, a peakground acceleration exceeding 0.7 g could occur at the site during suchan event (U.S. Army Corps of Engineers, SPD, 1979).

Groundwater

5-04 Groundwater levels along the project alignment are directlyaffected by flows in Mill Creek and the underlying alluvium. Seasonalrunoff appears to be the controlling factor in the geohydrology of theproject site; groundwater levels drop during the winter period of snowaccumulation and little runoff, and then tend to recover during latespring and summer snowmelt. In general, high groundwater levels haveoccurred from March through October, when depths to water may be aslittle as 10 to 15 feet below the streambed. The lowest levels occurfrom November through February, and may drop to as much as 150 feetbelow the surface. Groundwater pumping for irrigation, discharge frompowerhouses, and diversions for irrigation, domestic use, and spreadingall occur throughout the year at various locations in the valley, andmay modify the normal patterns. Groundwater elevations may varyconsiderably in the vicinity of Garnet Street, due to the presence ofthe Crafton fault groundwater barrier. Groundwater levels tend to beuniform across the fault at depths of 10 to 15 feet, however, when thedepth to groundwater is 20 feet or more upstream of the fault, thegroundwater level downstream may drop as low as 80 feet below thestreambed.

Investigations

PUEIOUS IIVSTIG&TIOKS

5-05 Prior to design and construction of the levees in 1960, thefoundation conditions at the project site were determined by visualobservation of the streambed surface and the existing cut banks in theproject reach. The foundation materials were observed to be recentalluvium consisting of streambed sand, gravel, cobbles, and boulders upto approximately 3 feet in diameter. The larger materials were moreabundant in the upstream portion of the project.

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RECENT INVESTIGATIONS

5-06 An investigation of the pervious borrow area for Seven Oaks Damwas conducted in October 1986. This investigation is considered to berepresentative of Mill Creek foundation conditions due to their closeproximity and the similarity between material types of both sites. Thearea investigated is located approximately 1 mile downstream of the MillCreek Levee project site at the confluence of Mill Creek and the SantaAna River.

5-07 Five test pits were excavated to depths ranging from 18 to 24 feetusing a Cat 235 tracked backhoe with a 4-foot wide bucket. Since thedeposits were observed to be uniform with depth, samples were obtainedby scraping the vertical walls of the pit and then cleaning out thematerials which fell to the bottom of the pit. Approximately40,000 pounds of material was removed from each pit for soils testing.

INVESTIGATION DURING ADVERTISING PERIOD

5-08 In order to better ascertain the material types to be excavated atMill Creek, test trenches will be excavated during the contractadvertising period. The trenches will be located as close to the leveetoe as reasonably possible and will be spaced far enough apart torepresent the entire levee reach. Testing of the materials obtainedfrom the trenches will not be required; the trenches are intended toprovide the contractor with a visual evaluation only. A visualobservation of the material types will allow contractors to determinethe extent of processing that will be required to provide floodwallbackfill and stone for the grouted stone revetment.

Field and Laboratory Testing Results

5-09 Mass gradations were determined for the materials sampled from theSeven Oaks Dam pervious borrow area. The gradation of plus 3-inchmaterial was determined in the field. Results indicate that thematerials larger than 3 inches range from 49 to 59 percent of the totalsample. The maximum size of the rock in the samples ranges from 20 to36 inches in diameter; however, rocks up to 60 inches in diameter wereexcavated from the test pits. Gradations of the minus 3-inch materialswere determined at the South Pacific Division laboratory and at the LosAngeles District laboratory. The minus 3-inch materials classified asgravelly sands (SP).

5-10 Maximum dry densities for the minus 3-inch portions of the sampleswere determined using vibratory compaction methods (ASTM D 4253). Theresults indicate that the average maximum dry density for the minus3-inch claterial is about 132 pcf.

5-11 Consolidated drained and consolidated undrained triaxialcompression tests were conducted on 12-inch diameter samples of gravellysand, compacted to 95 percent of maximum density at 3 percent overoptimum moisture content. The tests were run at confining pressures of1, 2.5, 5, and 10 tsf, and the pore pressures were monitr,,ed during the

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undrained tests. The maximum size particle in these tests was 2 inches.The results indicate a 0' angle of 40.5 degrees for the consolidateddrained tests, and a 0' angle of 36.5 degrees for the consolidatedundrained tests with pore pressure measurements.

Design Values

FOUNDATION

5-12 Design values for the Mill Creek Levee foundation are based upontests conducted on the Seven Oaks Dam pervious borrow materials. A 0angle of 36 degrees was conservatively assumed for the foundationmaterials. The in situ density of the foundation is assumed to be 135.0pcf at a moisture content of 8 percent. The density of the foundationfor saturated conditions is assumed to be 145.0 pcf.

ENBANXENT AND TOE BACKFILL

5-13 The existing Mill Creek Levee was constructed with materialsobtained from the required riverbed excavation as will the proposedlevee enlargement. The design values for the existing levee embankment,the proposed levee enlargement and the toe backfill are assumed to bethe same as those presented above for the levee foundation due to thesimilarity of material types. The maximum allowable bearing capacity ofthe levee for the proposed floodwall is 6,000 pounds per square foot andthe coefficient of friction between the concrete floodwall and the leveematerials is 0.6.

Stability Analysis

5-14 A typical levee section with the recommended modifications,landward side slopes of 1V on 2H and river side slopes of 1V on 2.25H,was analyzed for slope stability (assuming a levee height of 16 feet).Saturated conditions were not considered in the analysis because ofrelatively low groundwater and grouted side slopes which will preventmajor seepage into the levee from floodflows. The end of constructioncase was analyzed for the river side slope using a computer aidedcircular search which employs Spencer's procedure. The factor of safetyfor stability was calculated to be 1.9. kdditionally, the river sideslope was analyzed for surficial slides using the infinite slope methodand the factor of safety was calculated to be 1.6.

Construction Considerations

EXCAV&TION

5-15 Temporary slopes for the required streambed excavation at thelevee toe and for the levee excavation (i.e., for the floodwall) will beno steeper than 1V on 1H. Bedrock may occur within the excavationlimits in the vicinity of Garnet Street, and will consist of hard, dense

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schist and granitic rocks. Since excavation will be for placement ofrevetment for protection of the levee toes, excavation will be

terminated at bedrock.

PLACEMENT AND COMPACTION

5-16 Compacted fill, if required, will be obtained from the riverbed.The fill will be specified to have a maximum particle size of 9 inchesand will be placed in 12-inch layers. Each layer will be compacted to

95 percent of maximum density (ASTM D 4253). Any materials removed fromthe existing levee embankment during the floodwall construction will bereplaced and compacted as stated above.

SLOPE PROTECTION

5-17 The stone to be used for the grouted stone slope protection will

be well graded and range in size from 4 inches to 12 inches.

Construction Materials

BORROW MATERIAL SOURCES

5-18 Materials required for borrow can be obtained from the riverbed inthe area of the required toe excavation. Processing of these materialswill be required in order to remove stone which exceeds the maximum

stone size requirement. Oversized stone can be disposed of in the leveetoe backfill, provided it is not placed directly against the groutedstone revetment.

STORE MATERIALS

5-19 There are six quarries (table V-I) within 30 miles of the projectwhich have recently produced stone suitable for use on Corps ofEngineers' projects.

Table V-i. Stone Sources.

Distance to Specific TestQuarry Rock Type Project (mi.) Gravity (BSSD) Date

Atkinson granite 21 2.77 10/87Declesville granite 24 2.79 11/83Harlow andesite 28 2.66 6/85Juniper Flats diorite 21 2.74 7/83

Slover Mountain marble 13 2.72 11/83metasediment 2.90 11/83

Stringfellow granite 23 2.66 10/85

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Stone for revetment may be obtained from these sources, as well as othernearby quarries with suitable test results or service records. Thealluvium along the Mill Creek channel contains as much as 50 percentover 6-inch material, and may be processed to produce rock for groutedstone revetment.

Concrete Materials

STRUCTURAL EUIXTS

5-20 Structural elements to be constructed of concrete for the MillCreek Levee will be a concrete floodwall and grouted stone slopeprotection.

5-21 The recommended floodwall for the levee will be constructed alongthe existing top of levee from: station 88+70 to station 130+20 andfrom station 130+72 to station 196+25.37, and on top of the new raisedlevee from station 70+00 to station 88+70.

5-22 The height of the wall varies from 5 feet 11 inches to 7 feet6 inches. The wall is designed as an inverted T-wall. The footing willbe 6 feet in length and will rest on top of the levee. The thickness of

the stem and footing will be 8 inches and 10 inches respectively. Acutoff wall, 3 feet deep and 10 inches thick, will be provided at theend of the footing (river side). See plate 14 for a typical floodwallsection.

5-23 Grouted stone revetment will be constructed from station 70+00 tostation 88+70. The toe will be about 18 feet below the new top of thelevee and will have a thickness of 18 inches. Additionally, the existinggrouted stone toe revetment from station 88+70 to station 129+33.33 andstation 130+72 to station 196+25.37 will be extended. From station

88+70 to station 129+33.33 the new toe depth will vary from 2 to 8 feetbelow the existing toe with a thickness of 18 inches. Fromstation 130+72 to station 196+25.37 the new toe depth will vary from8 to 12.5 feet below the existing toe with a thickness of 18 inches.

5-24 The following table summarizes the approximate quantities ofconcrete, grout and cements to be used in project construction:

Table V-2. Estimated Concrete Material Quantities.

Concrete Grot Cement*(yd ) (yd ) (CWT)

Walls 1,920 - -

Footing and Stems 2,330 - -

Cutoff Walls 850 - -Grouted Revetment - 6,680 47,070

0 Calculated for Grouted Revetment Only.

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CLIMATIC CONDITIONS

5-25 The climate of the Mill Creek Levee drainage area is subtropicalsemi-arid with warm summers and relatively mild winters. From late

spring through mid-fall, with the greatest intensities during the

summer, the channel area is subject to air pollution accumulation

between the late morning and early evening. Variations in the climate

are almost entirely due to seasonal changes.

5-26 The area is generally mild, free from extremely low winter

temperatures and relatively immune to extremely high summer

temperatures. Summers are pleasantly warm, with daily maximumtemperatures averaging around 950F (extreme highs around 115 0F) and

nocturnal minimums ranging from 360F to near 580F. Winters are cool,with mild days. Normal daily winter temperatures range from highs of

680F to lows of 370F (all-time extremes from 170F to 930F).

5-27 The relative humidity in the Mill Creek Levee area can vary fromzero to 100 percent. Typical ranges during most of the year are from 80

to 90 percent during the early morning hours and 30 to 50 percent during

the early afternoon.

5-28 Mean seasonal precipitation in the drainage area is approximately32 inches. The primary rainy season is winter (November-April), withthe heaviest precipitation occurring normally from December throughmid-March. Summer (June-September) is the driest time of the year.

CEMTS

Cement Sources

5-29 There are a relatively large number of cement producers in and

near the Los Angeles Basin which are capable of supplying cementcertified by the Corps of Engineers ongoing cement certification

program. Among these plants are the Califorinia Portland Cement Companyplant at Colton, the Kaiser Cement Company plant at Lucerne Valley, the

Southwestern Cement Company plant at Victorville, and the RiversideCement Company plant at Riverside. All of these plants are in the Stateof California. The following paragraphs summarize the types of cementswhich these plants produce. Table V-3 supplies prices of various

cements from the sources specified, and table V-4 contains cost data onthe shipping of cement.

5-30 The California Portland Cement Company plant at Colton, located

approximately 15 miles west of the project site produces Type II and IIIcements conforming to the requirements of ASTM C 150.

5-31 The Kaiser Cement Company plant in the Lucerne Valley, locatedapproximately 55 miles north of the project site produces Type II cement

conforming to the requirements of ASTM C 150. This plant also produces

a blended cement conforming to the requirements of ASTM C 595, Type IP.

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5-32 The Riverside Cement Company plant at Oro Grande, California,located approximately 53 miles north of the project site producesType II cement conforming to the requirements of ASTM C 150.

5-33 The Southwestern Cement Company plant at Victorville, California,located approximately 50 miles north of the project site produces

Type II and V cements conforming to the requirements of ASTM C 150.

Table V-3. Cement Prices.

(Dollars Per Ton, FOB Plant, December 1987)

CEMENT TYPECement Plant and Location IP II III V

California Portland, Colton - $73.00 $78.00

Kaiser, Lucerne Valley $74.30 60.00 - -

Southwestern, Victorville - 64.00 - $80.30

Riverside Cement, Riverside - 63.00 -

Table V-4. Cement Shipping Prices.

(Dollars Per Ton, December 1987)

Distance Distance Distance(Miles) Cost (Miles) Cost (Miles) Cost

3-5 $3.142 30-35 $4.480 70-30 $7.8285-10 3.296 35-40 5.200 80-90 8.446

10-15 3.450 40-45 5.922 90-100 9.01215-20 3.760 45-50 6.386 100-110 9.682

20-25 3.966 50-60 6.902 110-120 10.300

25-30 4.224 60-70 7.314 120-130 11.072

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Pozzolans

5-34 ETL 1110-1-127, dated 17 August 1984, allows the use of flyash inconcrete construction except in those cases where its use can be provento be undesirable. The local practice of the ready-mix concreteindustry is to use flyashes as pozzolanic admixtures in concrete. Thereason for this is the reduction of heat of hydration, reduction in costdue to the price of flyashes in comparison to the price of cement,increase in workability at lower water contents, and the reduction inthe alkali-aggregate reaction. The practice of local agencies is tospecify Type F flyash generally conforming to the requirements ofASTM C 618. The Corps of Engineers has recently started a program toevaluate the quality and uniformity of flyashes and has set up acertification plan similar to the one used for cements. Materialsconforming to these requirements are produced at the plants shown onplate 31. The closest local producer, the Western Ash Company, suppliesflyash, conforming to the requirements of ASTM C 628, Type F, from aplant at Page, Arizona. A local distribution point is at SanBernardino, California approximately 12 miles west of the projectsite. F type ash would be available from this source at a cost of$40 per ton.

AGGREGATES

5-35 The Waterways Experiment Station Technical Memorandum No. 6-370,September 1953, titled "Test Data, Concrete Aggregates in ContinentalUnited States," Volume 1, Area 3, Western United States, indicates thatthe vicinity of the Mill Creek Levee project has a large number ofsources capable of producing aggregates suitable for use in concreteconstruction. In accordance with EM 1110-2-2000 some of these sourceswere sampled and tested at the South Pacific Division Laboratory by theLos Angeles District in the Spring of 1985. The names and locations ofthe sources are shown on plate 31.

5-36 Testing consisted of petrographic analysis, elementary physicaltests, tests for potential reactivity of aggregates and a concrete checkmix. The tests indicate that aggregates suitable for use in all aspectsof concrete construction are available from local sources. The resultsof the laboratory work are reported hereafter.

Geologic Aspects of Aggregate Sources

GHERAL

5-37 All aggregates from suppliers listed herein are mined from majorstreambeds on the alluvial plains several miles downstream from thesouthern margin of the San Bernardino Mountains. The aggregates areprocessed from alluvium which is derived from rocks exposed in themountain regions surrounding the streams and their tributaries. Theigneous and metamorphic basement complex of the San Bernardino Mountainsis the most abundant terrane in the source area, consequently most ofthe aggregate is composed of those rock types.

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LITLE CREEK

5-38 Both Owl Rock Company and Fourth Street Crusher are located in theLytle Creek streambed, 4 and 6 miles downstream from the mouth of theLytle Creek Canyon, respectively. Most of the rocks in the Lytle Creekbasin are Tertiary diorite, Cretaceous granite and diorite,pre-Cretaceous pelona schist, and various Precambrian metamorphicrocks. The granite, granodiorite, and diorite predominate in samplesfrom these suppliers, along with significant amounts of schist, gneiss,quartizite, and various metasedimentary and metavolcanic rocks. Minoramounts of gabbro are also present, from Mesozoic exposures west of thecanyon. Fina aggregate (No. 4 and smaller) produced from these twosources contain fragments of all of the above rocks, along withindividual grains of hornblende, quartz, biotite and feldspars.

SANTA ANA RIVER

5-39 The C. L. Pharris Company is located in the Santa Ana Riverstreambed approximately 5 miles downstream from the mouth of the SantaAna River Canyon. This source was previously operated by theLivingston-Graham Company. Rock exposed in the Santa Ana River drainageconsists mainly of Mesozoic intrusives and Precambrian igneous andmetamorphic rocks. Rock produced at the C. L. Pharris plant ispredominantly Mesozoic diorite, granodiorite, and gabbro, along withPrecambrian schist. A small proportion of sandstone and siltstonefragments is also present, derived from scattered outcrops of Te-tiarysediments. Fine aggregate consists of individual grains of feldspar,quartz, and biotite, with some fragments of granite, quartzite, schist,and metasedimentary rocks.

SAM GORGONIO RIVER

5-40 The Beaumont Concrete Company is located in the San Gorgonio Riverfloodplain about 6 miles downstream from the mouth of San Gorgonio RiverCanyon. Aggregate produced by this supplier is composed primarily ofMesozoic granite, granodiorite, gabbro, and diorite. Pelona schist isalso present, as well as gneiss and miscellaneous metamorphiclithologies probably derived from Precambrian outcrops. Fine aggregatefrom the Beaumont Concrete Company contains all of the above rock typesas well as individual grains of the constituent mineral.

Aggregate Sources

OWL ROCK PRODUCTS

5-41 This source is on Lytle Creek approximately 7 miles west of theproject site. The location of this source is shown on plate 31. Thissource excavates alluvial sands and gravels from the Lytle Creekstreambed deposits. Samples of aggregates were obtained from thissource in 1985 and were tested at the SPD Laboratory. Aggregate testresults are shown in table V-5 and in figure 2.

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5-42 At the time of the sampling the plant was producing three rock

sizes and a washed concrete sand, which were sampled for testing. The

course sized materials included 2-, 1-1/2-, and 3/8-inch topsizematerials. The 2-inch material meets the Standard Specifications forPublic Works Construction (SSPWC), a local specifying group made up of

public agencies and suppliers, specifications size No. 2, and ASTM C 33,size No. 4. The 1-1/2-inch material meets the SSPWC specifications sizeNo. 3 and ASTM C 33 size No. 56. The 3/8-inch material meets the SSPWCsize No. 4 but does not meet any ASTM size standard. The washedconcrete sand conforms to both the SSPWC and ASTM C 33 size for washedconcrete sand. Gradations determined from the samples taken are shownin table V-5.

5-43 The rock sizes tested had specific gravities (Sp. Gr.) of 2.65 to2.67 with Sp. Gr. of 2.67 and above for aggregates greater than 3/4-inchin size. The sand had a Sp. Gr. of 2.63. The aggregates hadabsorptions of 1.0 to 1.9 percent for the coarse and 1.6 percent for thefines. The coarse aggregate has an abrasion loss of 24 percent whentested in accordance with ASTM C 131, using gradation A. The chemicalmethod of reactivity of aggregates was performed and the results areshown in figure 2. The test results indicate that there should be nounfavorable reactions between cements and the aggregates. Theaggregates are generally of slightly higher quality than those found inthe Los Angeles Basin, but are about average for the localSan Bernardino area.

4TH STREET CRUSHER

5-44 This source is on Lytle Creek approximately 15 miles west of theproject site. This source excavates alluvial sands and gravels fromLytle Creek streambed deposits near its confluence with the Santa AnaRiver. The location of this source is shown on plate 31. Samples ofaggregates were obtained from this source in 1985 and were tested at theSPD Laboratory. Aggregate test results are shown in table V-6 andfigures 3 and 4.

5-45 At the time of sampling, the plant was producing three rock sizesand a washed concrete sand, which were sampled for testing. The coarsesized materials included 2-, 1-1/2-, and 3/8-inch topsize materials.The 2-inch material meets SSPWC specifications size No. 2, andASTM C 33, size No. 4. The 1-1/2-inch material met the ASTM C 33 sizeNo. 56 and barely failed the SSPWC size No. 3 on the 3/8 inch screen.The 3/8-inch material does not meet any size standard. The washedconcrete sand conforms to both the SSPWC and ASTM C 33 size for washedconcrete sand. Gradations determined from the samples taken are shownin table V-6.

5-46 The rock sizes tested had Sp. Gr. of 2.65 to 2.69 with Sp. Gr. of2.68 and above for aggregates greater than 3/4-inch in size. The sandhad a Sp. Gr. of 2.63. The aggregates had absorptions of 1.0 to1.6 percent for the coarse and 1.2 percent for the fines. The coarseaggregate has an abrasion loss of 25 percent when tested in accordancewith ASTM C 131, using gradation A. The chemical method of reactivityof aggregates was performed and the results are shown in figure 3.

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Table V-5. Physical Tests on Concrete Aggregates for:

OWL ROCK PRODUCTS COMPANYRiverside Avenue at Linda Street

Rialto, California(Date tested: January 1985)

Part A: GRADATIONS IN PERCENT FINER BY WEIGHT

Sieve Size 1.5" - 3.0" 3/4" - 1.5" #4 - 3/4" Fine Agg.

2 in. 1001-112 in. 96 1001 in. 23 983/4 in. 2 741/2 in. 313/8 in. 14 100 100No. 4 4 4 99No. 8 82No. 16 63No. 30 41No. 50 19No. 100 7No. 200 3

Part B: PHYSICAL TEST RESULTS

Test Requirement 1.5" - 3.0" 3/4" - 1.5" #4 - 3/4" Fine Agg.

Specific Gravity 2.67 2.67 2.65 2.63Absorption 1.0 1.6 1.9 1.6Soft Particles . 0.20 0.40

Part C: PHYSICAL TESTS ON COMBINED SAMPLES

Organic Impurities (ASTM C 40) OKMortar Strength ratio @ 7 days (ASTM C 87)Soundness: Magnesium Sulfate (ASTM C 88)

Coarse Aggregate 3/4"-1-1/2" 1.35Fine Aggregate 3/8"-3/4" 3.18

Decantation (ASTM C 117) 14.50Abrasion Loss, 500 rev. (ASTM C 131)

Grading Designation APercent Loss 24

Reactivity, Chemical Method (ASTM C 289)Coarse Aggregate Rc= 36 Sc= 29 InnocuousFine Aggregate Rc= 51 Sc: 43 Innocuous

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Table V-6. Physical Tests on Concrete Aggregates for:

4TH STREET CRUSHER1945 W. 4TH Street on Lytle Creek

Rialto, California

(Date tested: January 1985)

Part A: GRADATIONS IN PERCENT FINER BY WEIGHT

Sieve Size 1.5" - 3.0" 3/4" - 1.5" #4 - 3/14" Fine Agg.

2 in. 100

1-1/2 in. 97 1001 in. 27 99

3/4 in. 2 66

1/2 in. 22

3/8 in. 4 100 100

No. 4 8 97No. 8 86

No. 16 68

No. 30 41

No. 50 18

No. 100 6

No. 200 2

Part B: PHYSICAL TEST RESULTS

Test Requirement 1.5" - 3.0" 3/4" - 1.5" #4 - 3/4" Fine Agg.

Specific Gravity 2.69 2.68 2.65 2.63Absorption 1.0 1.1 1.6 1.2

Soft Particles . 1.3 0.1

Part C: PHYSICAL TESTS ON COMBINED SAMPLES

Organic Impurities (ASTM C 40)

Mortar Strength ratio @ 7 days (ASTM C 87)Soundness: Magnesium Sulfate (ASTM C 88)

Coarse Aggregate 3/4"-1-1/2" 1.5#4-3/4" 2.3

Fine Aggregate 12.6Decantation (ASTM C 117)Abrasion Loss, 500 rev. (ASTM C 131)

Grading Designation APercent Loss 25

Reactivity, Chemical Method (ASTM C 289)Coarse Aggregate Rc: 49 Sc 20 Innocuous

Fine Aggregate Rc= 28 Sc: 27 Innocuous

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The test results indicate that there should be no unfavorable Veactionsbetween cements and the aggregates. Mortar bar test results showexpansion of +0.025 percent at 180 days and +0.012 percent at 335 daysfor high alkali cement. Expansions of +0.009 percent at 180 days and360 days are noted for low alkali cements. Detailed results are shownin figure 4. The aggregates are generally of slightly higher qualitythan those found in the Los Angeles Basin, but are about average for thelocal San Bernardino area.

5-47 Subsequent review of this source in December 1987 indicated thatthe pit was no longer able to produce coarse aggregates. The onlymaterial being produced from the pit at this time was a concrete sand.Large size materials are periodically washed into the pit as a result ofstreamflows. The extended drought has introduced no coarse sizematerials into the pit, and as a consequence this source at this timedoes not supply coarse aggregates. If materials are depositedsubsequent to this report it is anticipated that they will haveproperties similar to those described herein. In accordance with SPDcriteria, this source and or any other source used in construction willbe subject to verification testing.

BEAU MOT CONCRETE COMPANY

5-48 This source is near Cabazon approximately 10 miles southeast ofthe project site. This source excavates alluvial sands and gravels.The location of this source is shown on plate 31. Samples of aggregateswere obtained from this source in 1985 and were tested at the SPDLaboratory, Aggregate test results are shown in table V-7 andfigures 5 and 6.

5-49 At the time of sampling, the plant was producing three rock sizesand a washed concrete sand, which were sampled for testing. The coarsesized materials included 2-, 1-1/2-, and 3/8-inch topsize materials.The 2-inch material meets the SSPWC specifications size No. 2, andASTM C 33, size No. 4. The 1-1/2-inch material meets the SSPWCspecifications size No. 3 and ASTM C 33 size No. 56. The 3/8-inchmaterial does not meet any size standard. The washed concrete sandconforms to both the SSPWC and ASTM C 33 size for washed concrete sand.Gradations determined from the samples taken are shown in table V-7.

5-50 The rock sizes tested had Sp. Gr. of 2.63 to 2.67 with Sp. Gr. of2.68 and above for aggregates greater than 3/4-inch in size. The sandhad a Sp. Gr. of 2.66. The aggregates had aborptions of 1.0 to 2.7percent for the coarse and 1.2 percent for the fines. The coarseaggregate has an abrasion loss of 39.1 percent when tested in accordancewith ASTM C 131, using gradation A. This result is 3lightly higher thandesired but conforms to ASTM and SSPWC requirements. The chemicalmethod of reactivity of aggregates was performed and the results areshown in figure 5. Mortar bar test results show expansion of +0.044percent at 180 days and +0.040 percent at 335 days for high alkalicements. A peak expansion of +0.046 percent at 225 days was noted.

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Table V-7. Physical Tests on Concrete Aggregates for:

BEAUMONT CONCRETE COMPANYCabazon Pit

San Gorgonio River at Apache TrailCabazon, California

(Date tested: January 1985)

Part A: GRADATIONS IN PERCENT FINER BY WEIGHT

Sieve Size 1.5" - 3.0" 3/4" - 1.5" #4 - 3/4" Fine Agg.

2 in. 100

1-1/2 in. 94 100

1 in. 21 993/4 in. 2 74 1001/2 in. 33 993/8 in. 11 56 100No. 4 2 99No. 8 86No. 16 66No. 30 43No. 50 19No. 100 6No. 200 2

Part B: PHYSICAL TEST RESULTS

Test Requirement 1.5" - 3.0" 3/4" - 1.5" #4 - 3/4" Fine Agg.

Specific Gravity 2.66 2.67 2.63 2.66Absorption 1.0 1.3 2.7 1.2

Soft Particles 0.0 0.0 0.0

Part C: PHYSICAL TESTS ON COMBINED SAMPLES

Organic Impurities (ASTM C 40)Mortar Strength ratio @ 7 days (ASTM C 87)Soundness: Magnesium Sulfate (ASTM C 88)

Coarse Aggregate 3/4"-1-1/2" 1.9#4-3/14" 2.5

Fine Aggregate 16.1Decantation (ASTM C 117)Abrasion Loss, 500 rev. (ASTM C 131)

Grading Designation APercent Loss 39.1

Reactivity, Chemical Method (ASTM C 289)Coarse Aggregate Rc: 36 Sc= 29 InnocuousFine Aggregate Rc 51 Sc= 43 Innocuous

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Expansions of +0.012 percent at 180 days and +0.014 percent at 335 dayswith a peak of +0.016 percent at 55 days were noted for low alkalicements. Detailed results are shown in figure 6. Although the valuesare below the limits for expansion, +0.05 percent at 180 days and +0.10percent at 360 days in accordance with EM 1110-2-2000, these reactionresults are much higher than most results in the Los Angeles District.Use of these aggregates may require special requirements.

C. L. PHARRIS

5-51 This source is on the Santa Ana River approximately 6 miles westof the project site. This source was previously identified asLivingston Graham. This source excavates alluvial sands and gravelsfrom Santa Ana River streambed deposits. The location of this source isshown on plate 31. Samples of aggregates were obtained from this sourcein 1985 and were tested at the SPD Laboratory. Aggregate test resultsare shown in table V-8 and figures 7 and 8.

5-52 At the time of sampling, the plant was producing three rock sizesand a washed concrete sand, which were sampled for testing. The coarsesized materials included 2-, 1-1/2-, and 3/8-inch topsize materials.The 2-inch material meets the SSPWC specifications size No. 2, andASTM C 33, size No. 4. The 1-1/2-inch material failed the SSPWCspecifications for size No. 3 on the 3/8-inch screen, but meetsASTM C 33 size No. 56. The 3/8-inch material does not meet any sizestandard. The washed concrete sand failed both the SSPWC and ASTM C 33size for washed concrete sand due to the presence of excess fines.Gradations determined from the samples taken are shown in table V-8.

5-53 The rock sizes tested had Sp. Gr. of 2.62 to 2.66 with Sp. Gr. of2.65 and above for aggregates greater than 3/4-inch in size. The sandhad a Sp. Gr. of 2.63. The aggregates had absorptions of 0.8 to1.7 percent for the coarse and 1.1 percent for the fines. The coarseaggregate has an abrasion loss of 32.7 percent when tested in accordancewith ASTM C 131, using gradation A. The chemical method of reactivityof aggregates was performed and the results are shown in figure 7. Thetest results indicate that there should be no unfavorable reactionsbetween cements and the aggregates. Mortar bar test results showexpansions of +0.025 percent at 180 days and +0.015 percent at 335 dayswith a peak of +0.030 percent at 235 days for high alkali cement.Expansions of +0.021 percent at 180 days and +0.013 percent at 335 daysare noted for low alkali cements. Detailed results are shown infigure 8. The aggregates are generally of slightly higher quality thanthose found in the Los Angeles Basin, but are about average for thelocal San Bernardino area.

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Table V-8. Physical Tests on Concrete Aggregates for:

C. L. PHARRIS

E. of Norton AFBSan Bernardino, California(Date tested: January 1985)

Part A: GRADATIONS IN PERCENT FINER BY WEIGHT

Sieve Size 1.5" - 3.0" 3/4" - 1.5" #4 - 3/4" Fine Agg.

2 in. 1001-1/2 in. 95 1001 in. 18 993/4 in. 1 70 1001/2 in. 1 23 993/8 in. 3 10 100No. 4 1 98No. 8 88No. 16 70No. 30 41No. 50 17No. 100 6No. 200 6

Part B: PHYSICAL TEST RESULTS

Test Requirement 1.5" - 3.0" 3/4" - 1.5" #4 - 3/4" Fine Agg.

Specific Gravity 2.66 2.65 2.62 2.63Absorption 0.8 0.9 1.7 1.1Soft Particles 0.0 1.5 0.3

Part C: PHYSICAL TESTS ON COMBINED SAMPLESOrganic Impurities (ASTM C 40) OKMortar Strength ratio @ 7 days (ASTM C 87)Soundness: Magnesium Sulfate (ASTM C 88)

Coarse Aggregate 3/4"-1-1/2 0.5#4-3/4 1.9

Fine Aggregate 10.4

Decantation (ASTM C 117)Abrasion Loss, 500 rev. (ASTM C 131)

Grading Designation APercent Loss 32.7

Reactivity, Chemical Method (ASTM C 289)Coarse Aggregate Re= 41 Sc= 26 InnocuousFine Aggregate Rc= 51 Sc= 24 Innocuous

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Aggregate Costs

5-54 Estimated unit costs of aggregate for use in construction of theMill Creek Levee are given in the following table. The quantitiesreflect materials to be used in the structural concrete work but do notreflect materials to be used in grout for grouted stone. Thedifferences in tonnages of materials reflect differences in producerspecific mix designs and material properties. The producers selectedmix designs according to the following criteria. The mixes were to bepumpable with 1-1/2-inch maximum size aggregate.

Table V-9. Estimated Unit Costs For Concrete Aggregates.(January 1988 prices)

Haul Unit

Distance CostTons Miles $/Ton

C. L. Pharris Coarse 7,250 6 5.50Sand 5,165 - 5.00

Owl Rock Coarse 7,670 17 4.95Sand 4,700 - 4.55

Beaumont Concrete Coarse 6,550 10 4.40Sand 5,740 - 4.40

4th Street Crusher Coarse 6,830 15 N/ASand 4,820 - 8.00

Additionally, approximately 6,570 tons of sand will be needed for groutfor the grouted stone requirements of the project.

Water

5-55 Sufficient water suitable for preparation of concrete is availablefrom commercial sources at the concrete production facilities citedabove. During geotechnical explorations for the Seven Oaks Dam,groundwater observed in one of the trenches upon drying, left a whiteresidue. It is believed that the residue may be calcium or carbonatebased. Further studies for Seven Oaks Dam will incluide studies todetermine the exact composition of this residue. For construction ofthe Mill Creek Levee, water will be required to conform to therequirements of CRD C-400, and a low alkali cement is recommended.

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kduixtures

5-56 A wide variety of chemical admixtures are used in southernCalifornia. Based on the structural elements to be constructed, onlythe simplest admixtures will be specified. These will include airentraining agents, and water reducing and retarding admixtures. Nospecific need for high range water reducing admixtures or"Superplasticizers" has been identified.

Mix Design Requirements

5-57 Specifications for concrete and concrete mix designs forconstruction of the Mill Creek Levee will be developed to meet therequirements of ER 1110-2-1150. Specific design requirements will bedeveloped based on the information supplied in EM 1110-2-2000 and willconsider the types of structures and the anticipated exposure conditionsto which they will be subjected.

5-58 The types of structures to be constructed for the projectdescribed above are relatively simple and the Los Angeles District hasextensive experience in construction of these types of structuralelements.

5-59 Based on EM 1110-2-2000 the maximum water-cement ratio of allconcrete exposed to flowing water shall be limited to 0.45.Additionally, the nominal maximum size coarse aggregate shall bespecified as 1-1/2 inches.

5-60 An additional requirement will be a limitation on the maximumplacing temperature of the concrete. Based on the ambient weatherconditions reported above and the requirements specified inEM 1110-2-2000 the maximum placing temperature of concrete will belimited to 850 F. As a protection from damage by sunlight to freshlyplaced concrete, specifications will require that the contractor eithershade freshly placed concrete for 3 days or apply an opaque curingcompound conforming to the requirements of CRD C-300.

Cost of Concrete

5-61 The following table presents current costs for concrete forconstruction of the proposed structural elements. Suppliers developedthe costs based on a 1-1/2 inch maximum aggregate size concrete mixturewhich would be pumpable and would supply compressive strengths of 3,000psi at 28 days. The prices include the cost of delivery to the jobsite.

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Table V-10. Estimated Costs of Redimix Concrete.(January 1988 Prices)

Supplier $/cu.yd.

Owl Rock Products 53.004th Street Crusher 48.00

Beaumont Concrete 46.00C. L. Pharris 44.80

Specifications Requirements

5-62 The following information details specification requirements for

construction.

CQDTS

5-63 Cements will be specified to conform to the requirements of

ASTM C 150, Type II, low alkali. The low alkali requirement shouldassist in offsetting any potential alkali-aggregate reactivity.

Additionally, Type V cement conforming to the requirements of ASTM C 150will be specified as an option, although the need for high sulfate

resistance has not been specifically identified. Blended cements shallconform to the requirements of ASTM C 595, Type IP. Flyash used to

manufacture Type IP cement shall conform to the requirements forpozzolan.

POZZOQAMS

5-64 Pozzolans for use in concrete construction will be specified tocomply with requirements of ASTM C 618, Type F. The loss on ignitionwill be limited to 6 percent maximum. Additionally, the optionalrequirements in table 1A shall be invoked.

A. IXTURES

5-65 Admixtures for use in concrete construction will be limited towater reducers, retarders, accelerators, and air entraining agents

conforming to the following requirements:

a. Water reducing admixtures will conform to the requirements ofASTM C 494, Types A or D.

b. Retarding admixtures will conform to the requirements ofASTM C 494, Types B or D.

c. Accelerating admixtures will conform to the requirements of

ASTM C 494, Types C or E. No calcium chloride will be allowed.

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d. Air entraining agents will conform to the requirements of

ASTM C 260.

ALGGREGATES

5-66 Aggregates will be specified to conform to the physical

requirements of ASTM C-33. Sizes of coarse aggregates to be used duringconstruction will be selected at the time of preparation of plans and

specifications based on materials available in the area at the time of

the proposed construction. Sizes will be selected to conform to the

requirements of ASTM C 33 or to SSPWC paragraph 200-1.4 and shall be anominal maximum size of 1-1/2 inches for structural elements over 7-1/2

inches wide, and in which the clear distance between reinforcement barsis at least 2-1/4 inches. All other elements will use a nominal maximum

size of 3/4 inches.

5-67 The following sources shall be described as supplying suitable

aggregates: (1) existing commercial sources on the Santa Ana River fromits confluence with Mill Creek to upstream from the Southern Pacific RR

bridge in San Bernardino, (2) existing commercial sources on Lytle Creekand the Cajon Wash to their confluence with the Santa Ana River, and(3) existing commercial sources on the San Gorgonio River downstreamfrom the mouth of the San Gorgonio River Canyon.

References

Bolt, Bruce A., 1987, Seismological Report for Seven Oaks Dam, Report toLos Angeles District Corps of Engineers, Contract No. DACWO9-87-M-1734.

California Department of Mines and Geology, 1976, Geologic Hazards

in Southwestern San Bernardino County, California, CDMG SpecialReport 113.

Carson, S.E. and Matti, J.C., 1985, Contour Map Showing Minimum Depth to

Groundwater, Upper Santa Ana River Valley, California, 1973-1979,United States Geologic Survey Miscellaneous Field Studies Map

MF-1802.

Dibblee, T.W., 1982, Geology of the San Bernardino Mountains, SouthernCalifornia, in Geology and Mineral Wealth of the CaliforniaTransverse Ranges, South Coast Geologic ;ociety Annual Symposium andGuidebook No. 10

Fife, D.L., Rodgers, D.A., Chase, G.W., Chapman, P.H., Sprotte, E.C.,Morton, D.M., 1976, Geologic Hazards in Southwestern San BernardinoCounty, California, California Division of Mines and Geology Special

Report 113.

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Krinitzky, E.L., and Chang, F.K., 1977, Specifying Peak Motions for

Design Earthquakes, U.S. Army Engineer Waterways Experiment StationMiscellaneous Paper S-73-1, Report 7.

Krinitzky, E.L., and Marcuson, W. F. III, 1983, Principles for SelectingEarthquake Motions in Engineering Design, in Bulletin of the

Association of Engineering Geologists Vol. XX, No. 3., August 1983.

Matti, J.C., Morton, D.M., and Cox, B.F., 1985, Distribution and

Geologic Relations of Fault Systems in the Vicinity of the CentralTransverse Ranges, Southern California, U.S. Geological Survey OpenFile Report 85-365.

U.S. Army Corps of Engineers, 1983, Earthquake Design and Analysis for

Corps of Engineers Projects, Engineering Regulation ER 1110-2-1806.

U.S. Army Corps of Engineers, South Pacific Division, 1979, ReportingEarthquake Effects, SPD Supplement to Engineering Regulation ER1110-2-1802.

United States Geologic Survey, 1959, Geology and Groundwater Hydrologyof the Mill Creek Area, USGS Open File Report.

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VI. STRUCTURAL DESIGN

Floodwall

6-01 A floodwall will be provided along the existing levee betweenstation 70+00 and station 129+33.33 and between station 130+72 andstation 196+25.37. The height of the wall above the existing top oflevee will vary from approximately 5 feet 11 inches to 7 feet 6 inchesaccording to hydraulic requirements.

6-02 The floodwall will be designed as an inverted T-wall. The footingwill be 6 feet in length and will rest on top of the levee. Thethickness of the stem and the footing will be 8 inches and 10 inchesrespectively. A cutoff wall, 3 feet deep and 10 inches thick, will beprovided at the end of the footing (river side).

6-03 The applied forces will be the hydrostatic force, the weight ofconcrete and other surcharges above the base of the wall. Upliftpressure in the base will not be considered because sloping groutedstone protection will be constructed from the existing grouted stone tothe wall footing, prohibiting the entrance of water under the wall base.The floodwall loading conditions are shown in figure 9.

6-04 Various water surface elevations will be considered in the design.

References

6-05 The design will be based on accepted engineering practice and willconform to the following Engineering Manuals (EM's), EngineeringTechnical Letters (ETL's), and Engineering Regulations (ER's):

Reference Title

EM 1110-1-2101 Working Stresses for Structural Design

EM 1110-2-2000 Standard Practice for Concrete

EM 1110-2-2103 Details of Reinforcement-Hydraulic Structures

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EM 1110-2-2502 Retaining Walls, Floodwalls (Draft Edition)

ER 1110-2-1806 Earthquake Design and Analysis for Corps ofEngineers Projects

ETL 1110-2-256 Sliding Stability

ETL 1110-2-312 Strength Design Criteria for ReinforcedHydraulic Structures

Other applicable ETL's, EM's (EM 1110-series), draft EM's, and codeslisted therin.

Material Properties

6-06 Material properties which will be used in the design of the

proposed structures are:

CONCRETE

Ultimate Compressive Strength:

Cast-in-place structures f'c 3,000 psi

Modulus of Elasticity Ec 57,000 (f'c) 1/2

REINFORCING STEEL

Yield Strength for Grade 40 Steel fy =40,000 psi

Yield Strength for Grade 60 Steel f = 48,000 psi

Modulus of Elasticity Es 29,000,000 psi

WEIGHT

Concrete = 150 pcf

Water = 62.5 pcf

For the weights and properties of soils, refer to Section V entitled"Geology, Soils and Materials," paragraph 5-12.

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VII. RELOCATION OF STREETS, RAILROADS AND UTILITIES

Under the recommended plan of improvements for the Mill Creek Levee,there will be no relocation of streets, railroads or utilities. TheGarnet Street bridge, which existed when the original Mill Creek Leveewas constructed, will remain in place and will continue to be subject toclosure during large floods. The bridge does not endanger thefunctioning of the flood control project. There are no railroads in theproject area. Bear Valley Mutual Water Company aqueducts (stas. 69+00and 196+00) will not be affected by the project. Other existingutilities were relocated or abandoned when the original Mill Creek Leveewas constructed and will not be affected by the proposed improvements.

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VIII. ACCESS ROADS

8-01 There are paved access roads on the existing levee system whichwill be partly removed to construct the floodwall. The roads will bereplaced or overlain along the levee top and widened from the existing9-foot width to 12 feet wide. They will continue to have gated accessentrances at the Garnet Street crossing. The paved road width willconsist of 4 feet-4 inches of concrete which also serves as thefloodwall footing and 7 feet-8 inches of flexible pavement which will beconstructed adjoining the footing. The access road will be overlainfrom station 196+25.37 to station 130+72 and from station 130+20 tostation 88+70. The road will be replaced from station 88+70 to station70+00. A 2 percent cross slope on the access road will provide drainageaway from the floodwall. There is an existing drainage system on thelandward side of the existing levee.

Geometric Design

8-02 Vehicular access roads, including ramps, will match existinggrades and alignment.

Pavement Design Values

8-03 The flexible pavement forming the paved access roads will bedesigned in accordance with Department of the Army TM 5-822-5. Based oninformation available in TM 5-825-2 a California Bearing Ratio (CBR)value of 30 can be assigned to the subgrade when the materials arecompacted to 95 percent of maximum density as determined in accordancewith ASTM D 4253. The road will be used only for operations,maintenance, and inspections and therefore the average number of dailyvehicle passes is estimated to be less than 25 on each lane. Thetraffic to which the road will be exposed will include some small trucksand a few heavy trucks. Based on the above information the flexiblepavement will be designed in accordance with the following values:

Category of Traffic = IIIClass of Road = EDesign Index = 2

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8-04 New pavement sections for the access road will consist of a 2-inchasphaltic concrete layer of 4 inches of an aggregate base course over6 inches of native materials compacted to 95 percent of maximum density.Overlays of the existing pavement would consist of a maximum of a 2-inchand a minimum of a 3/4-inch layer of bituminous surface course. Theoverlay thickness would be based on the condition of the existingpavement after construction of the floodwall.

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IX. ENVIRONMTAL ANALYSIS

General

9-01 An environmental impact statement on the proposed flood controlimprovements along the mainstem of the Santa Ana River including MillCreek was presented in the Phase I General Design Memorandum (GDM) datedSeptember 1980. For this Phase II GDM, the environmental evaluation hasbeen updated and broadened to include the presently proposed floodwallconstruction on the Mill Creek Levee. Details of the findings andconcerns are presented in the Supplemental Environmental ImpactStatement included in the Main Report of this Phase II GDM. Thissection presents a brief description of the environmental impacts whichmay be brought about as a result of the project. Compensation forimpacts are also discussed.

Environmental Impacts

SEDIMENTATION

9-02 The raising of the Mill Creek Levee, along with the additional toeprotection will not impact sedimentation. The improvements to the leveewill not preclude sedimentation processes from occurring in this area.

WATER RESOURCES

Hydrology and Water Use

9-03 Impacts will not occur to hydrology and water use in this projectarea.

Water Quality

9-04 Water quality in the area, other than high sediment loads, is verygood. No impact to the water quality of the area is expected with thisproject.

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AIR QU I Y

9-05 Impacts to air quality will be local and short term, due toconstruction activities, and will primarily be associated with vehicleemissions and dust generation. Increased vehicle emissions would resultfrom heavy equipment use on the construction site, from trucks haulingborrow materials to the construction site, and from personal vehiclesdriven by construction workers.

LAND USE AND SOCIAL CONCERNS

Prime and Unique Farmlands

9-06 No farmlands are located within or adjacent to the project area.

Recreation

9-07 There is no recreation associated with this project feature. Themaintenance road at the top of the levee will be gated and locked;public access will not be allowed.

Growth Inducement

9-08 Growth inducement as a result of the improvement to the existingMill Creek Levee is a possibility. Although land adjacent to the leveeis mostly owned by water districts and agencies, improved protection onland side of the levee may increase growth in the newly protected area.

TRAhNSPORTATION AND UTILITIES

Facilities

9-09 No streets, railroads or utilities will be relocated. The GarnetStreet bridge will not be impacted.

Access

9-10 Paved access roads to the existing levee will be removed duringconstruction, but will be replaced along the levee top as gated roadsfor operation and maintenance purposes.

Transport of Borrow Materials

9-11 Borrow materials will be obtained from within 100 feet of theexisting levee on the riverside. No public roads will be used fortransport of borrow materials. There will not be any excess excavationmaterials to be disposed of.

NOISE

9-12 The Mill Creek area is a relatively undisturbed area, with somehuman-induced noise present due to the presence of Highway 38 which runsalong a part of the levee. The project will have local short-term impactsto the environment, as construction-related noise will be present.

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Ti BILOGICAL RRSOURCES

9-13 Alluvial scrub vegetation, located in the streambed, will beimpacted by construction activities, along with minor amounts of juniperwoodland and mulefat. The construction area on both sides of GarnetAvenue also includes scattered cottonwoods and sycamores. Wildlifecurrently utilizing habitat within the construction zone will betemporarily displaced.

9-14 The recommended improvements of Mill Creek Levee will result inimpacts to a small group (50 to 70 plants) of the Santa Ana RiverWoolly-Star (Eriastrum densifolium sanctorum), an endangered species.There are no other known populations of any endangered or threatenedspecies which will be impacted. Additional surveys within the vicinityof Mill Creek were conducted during spring 1988 for the slender-hornedspineflower (Centrostegia). No additional populations of either specieswere found during these surveys.

9-15 Compensation for impacts to Eriastrum are covered under thediscussion for Seven Oaks Dam, Volume 1, and are included in thatproject feature.

CULTURAL RESOURCES

9-16 The construction of improvements to the levee will result in thedestruction of two non-significant historic sites. Two potentiallysignificant resources (active aqueduct pipelines) are in the area.Construction plans are to avoid these two active aqueduct pipelines.Both pipelines are located outside the project construction limits. TheBear Valley Highline is located just upstream from station 196+25.37 andthe Redlands Adequduct is just downstream from station 70+00 (pl. 2).

9-17 There is currently no proposed cultural resources mitigation forthe Mill Creek element of the project.

Site Restoration

9-18 Replanting for the temporary loss of habitat, esthetic values, andfor site restoration within Mill Creek, resulting from the recommendedproject will consist of reseeding disturbed areas with appropriatespecies following completion of all work. Seeding will be accomplishedby broadcast seeding followed by harrowing. Hydroseeding will not beacceptable as it does not encourage good seed to soil contact. Inaddition, cottonwoods, sycamores, willows, and junipers which occurwithin the 200-foot zone of construction but outside of the excavationzone will be avoided and protected from construction impacts. Any ofthese trees which are impacted by construction will be replaced with5-gallon container plants. In addition to a small amount of Eriastrum,the following species will be in the seed mix at the indicated rates:(1) Lotus scoparius, 6 lbs/acre; (2) Eriogonum fasciculatum, 10 lbs/acre;(3) Encelia farinosa, 3 lbs/acre; (4) Adenostoma fasciculatum,

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4 lbs/aare; (5) Salvia apiana, 2 lbs/acre; (6) Artemesia californica,2 lbs/acre; (7) a-caharis glutinosa, 2 lbs/acre;-and -(8) Er iodictyontrichocalyx, 3 lbs/acre.

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I. DIVERSION AND CONTROL OF WATER DURING CONSTRUCTION

Available climatological information indicates that most of the annualrainfall in the Mill Creek drainage area occurs between November andApril. To avoid flood damages, construction on the toe extension willbe scheduled to take place during the 6 month period between April andOctober. The low flows in Mill Creek generally occur in the incisedchannel north of the existing levee and the construction area.Extension of the levee toe can be accomplished during the summer monthswhen the flood threat is minimal; all other construction will take placeon the top of the levee, except for any borrow stockpiles produced fromthe required toe excavation. Measures for diversion and control ofwater would, therefore, be minimal.

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XI. REAL ESTATE REQUIREMENTS

11-01 The Mill Creek Levee begins just above the point where it entersthe Santa Ana River and terminates at a point approximately 13,600 feetupstream. It was designed to protect the cities of Mentone and Redlandsand surrounding urban areas. The material for raising the will comefrom the required excavations. The County of San Bernardino alreadyowns the required land area, which were acquired for the construction ofthe existing Federal flood control project.

11-02 Construction operations for the recommended Mill Creek Leveeimprovements will occur within existing project rights-of-way.

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III. COST ESTIMATES

12-01 The cost estimates are based on unit price data from recent bidsfor various items of work on other projects and on unit prices derivedusing established estimating procedures. In accordance with EM 1110-2-1301,a 15 percent contingency is added to the estimated construction cost.The cost for engineering and design, and supervision and administrationwas estimated to be 10 percent and 6 percent, respectively, of theconstruction costs (including contingencies). These percentages arebased on the actual prevailing rates experienced by the Los AngelesDistrict Office.

First Cost

12-02 The first cost of the proposed Mill Creek Levee is presentlyestimated at $5,109,000 (table XII-1). The detailed estimate of the

first cost is shown on table XII-2.

Operation and Maintenance

12-03 Upon completion of the proposed flood control improvements, theannual operation and maintenance cost is estimated at $15,000, which isbased on the costs incurred by the San Bernardino County Flood ControlDistrict for operation and maintenance of the original Mill Creek Levee.This estimated cost is comparable to the actual costs on similar typesof improvements experienced by the Los Angeles District.

Comparison of Estimates

12-04 The first cost for the Mill Creek Levee estimated in the Phase IGDM dated September 1980 (October 1979 Price Level) and this same cost

escalated to October 1987 price levels is shown in table XII-3.Compared to the escalated Phase I GDM estimate, the present estimate is$19,832,798 lower. The differences between the escalated Phase I GDMestimate and the current estimate are explained as follows:

XII-1

Page 65: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

a. Levee. A decrease of $5,086,082 is due to the elimination of1.2 miles of levee extension.

b. Floodwall. An increase of $1,578,800 is due to the addition of2.6 miles of concrete floodwall.

c. Groins. A decrease of $14,738,519 is due to the elimination ofgroins.

d. Engineering and Design. A decrease of $1,009,957 is due to adecrease in construction costs.

e. Supervision and Administration. A decrease of $706,040 is dueto a decrease in construction costs.

f. Operation and Maintenance Manual. An increase of $20,000 is dueto the addition of an Operation and Maintenance Manual.

g. Lands and Damages. A decrease of $91,000 is due to thereduction in real estate requirements.

h. Preconstruction Engineering and Design. An increase of $200,000is due to the addition of preconstruction costs previouslyincluded in the Engineering and Design Costs.

Table XII-I. Summary of First Cost.(October 1987 Price Level)

Acct.No. Description Amount

Construction

11.0 Levee $2,635,60011.0 Floodwall 1,578,80030.0 Engineering and Design 421,50031.0 Supervision and Administration 253,10051.22 Operation and Maintenance Manual 20,000

Total, Construction $4,909,000

Preconstruction Engineering and Design $ 200,000

Total, Flood Control First Cost $5,109,000

XII-2

Page 66: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

Table XII-2. Detailed Estimate of First Cost.(October 1987 Price Level)

CostAcct. Unit

No. Item Quantity Unit Cost Subtotal

11.0 LeveeClearing and 2 Acre $5,324.00 $10,648

GrubbingExcavation, Toe 101,000 CY 3.00 303,000

Compacted Fill, 3,000 CY 6.00 18,000

LeveeBackfill, Toe 101,110 CY 5.00 505,550

Stone 26,720 Ton 19.00 507,680

Grout 6,680 CY 80.00 534,400

Cement 47,070 CWT 5.00 235,350

AC Pavement 1,210 Ton 60.00 72,600

Prime Coat 96,400 SF 0.10 9,640

AC Removal 5,950 SY 1.50 8,925

Site Restoration 1 Job L.S. 86,000

Subtotal, Levee $2,291,793

Contingencies 343,807

Total, Levee $2,635,600

11.0 FloodwallExc. Wall Foot- 3,110 CY 3.00 9,330

ing and CutoffWall Concrete 1,920 CY 350.00 672,000

Footing and Stem 2,330 CY 130.00 302,900

ConcreteCutoff Wall 850 CY 90.00 76,500

ConcreteReinforcing Steel 454,840 Lb 0.50 227,420

.125"x6" Fibrous 3,320 LF 4.20 13,944

Mastic

Steel Door 2 Ea 350.00 700

3' -6"x5' -9"x.5"Ladder Rungs 57 Ea 19.00 1,083

.5"x12" Premolded 12,500 LF 2.00 25,000

Exp. Jt.

Esthetic Treatment 1 Job LS 44,000

Subtotal, Floodwall $1,372,877Contingencies 205,923

Total, Floodwall $1,578,800

30.0 Engineering and 421,500

Design (10%)

XII-3

Page 67: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

Table XII-2. (Continued)

CostAcct. UnitNo. Item Quantity Unit Cost Subtotal

31.0 Supervision and Admin- 253,100istration (6%)

51.22 Operation and Mainten- $ 20,000ance Manual

Total, Construction $4,909,000

Preconstruction Engineer- $ 200,000ing and Design

Total, Flood Control $5,109,000First Cost

XII-4

Page 68: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

Table XII-3. Comparison of First Cost.

Phase I GDM Phase I GDM PresentCost Estimate Estimate EstimateAcct. (October 1979 (October 1987 (October 1987No. Price Levels) Price Levels) Price Levels)

11.0 Levees

Diversion & Control $ 12,500 $ 18,598 $ 0of WaterClearing & Grubbing 17,500 26,036 12,226Excavation 31,250 46,494 348,435Fill 188,750 280,822 602,071Grouted Stone 4,940,000 7,349,732 1,469,047AC Pavement and 0 0 104,821Prime Coat

Site Restoration 0 0 99,000Total, Levees 5,190,000 7,721,682 2,635,600

11.0 Floodwall 0 0 1,578,800

16.0 Groins 9,906,250 14,738,519 0Subtotal 15,096,250 22,460,201 4,214,400

30.0 Engineering and Design 1,056,737 1,431,457 421,500

31.0 Supervision & Admin- 754,813 959,140 253,100istration

51.22 Operation & Mainten- 0 0 20,000ance Manual

Total, Construction 16,907,800 24,850,798 4,909,000

Total, Lands and Damages 61,000 91,000 0

Preconstruction Engineer- * 200,000

ing and Design

Total, Flood Control $16,968,800 $24,941,798 $5,109,000First Cost

*Included in the Engineering and Design Costs.

XII-5

Page 69: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

XIII. DESIGN AND CONSTRUCTION SCHEDULE

13-01 Preparation of Plans and Specifications. Preparation of contractplans and specifications for the construction of the proposed floodcontrol project will be initiated after the Phase II GDM for the SantaAna River is approved. Contract plans and specifications will takeabout 18 months to complete.

13-02 Construction Schedule. Construction of the project will bescheduled to start in the spring of year 2. Construction of the leveeimprovements including the concrete floodwall will take approximately12 months. Table XIII-1 shows a generalized construction schedule. Theschedule shown may be modified as required based on total projectrequirements. The overall project construction schedule is provided inthe main report.

13-03 Total Funds Required by Fiscal Years. Total funds includingFederal and non-Federal share which will be required for the preparationof contract plans and specifications and for construction are shown inthe Main Report. Table XIII-1 shows the total construction estimate andan undated schedule.

XIII-1

Page 70: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

UNIFORM PROJECT TOTAL AS OF

LINE COST FEATURE ITEMS COSTNO CLASSIFICATION ESTIMATE

I I I LEVEE 2,635.6

2 II FLOODWALL 1,578.8

3 30 ENGINEERING AND DESIGN 421.5

4 31 SUPERVISION AND ADMINISTRATION 253.1

5 51.22 OPERATION AND MAINTENANCE MANUAL 20

6

"7 TOTAL, CONSTRUCTION 4,909

8

9 PRE - CONSTRUCTION ENGINEERING & DESIGN 200

I0

II TOTAL, FLOOD CONTROL FIRST COST 5, 109

12

13

14

15

16

17

18

19

20

21

22

23

24

25

26

27

rFUNDS IN THOUSANDS OF DOLLARS

(=J NO

DESIGN ACTIVITY CONSTRUCTION

.

Page 71: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

19 ALAS OF FY 19 FY 19 FY 19 FY 19 FY 19 FY 19 FY 19 BALANCE

()Z4 -TO

34D0 120040 120040 1 1201-L01 40 IQ2f01Q 40 COMPLETE

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DATED APRILI I I1988 ISEET I OF Ix

Page 72: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

XIV. OPERATION AND MAINTENANCE

14-01 The existing operation and maintenance (O&M) manual would beupdated after construction of the flood control improvements inaccordanQe with ER 1130-2-304'"Project Operations" and applicableprovisions of ER 1150-2-301 "Local Cooperation." The estimated cost ofan updated O&M manual is $20,000. Upon completion of the proposed floodcontrol improvements, the annual operation and maintenance cost isestimated at $15,000, which is based on the costs incurred by the SanBernardino County Flood Control District for operation and maintenanceof the existing Mill Creek Levee. This estimated cost is comparable tothe actual costs on similar types of improvements experienced by the LosAngeles District. The local sponsors would be responsible for theoperation and maintenance of the flood control improvements. The majoritems of operation and maintenance and their estimated annual costs areshown in table XIV-1.

Table XIV-1. Annual Operation and Maintenance Cost.

(October 1987 Price Levels)

Description Amount

OperationCondition surveys $1,000Supervision and administration 2,000

MaintenanceDebris removal and maintenance 3,000Maintenance of 100-foot strip of streambed 3,000

Major replacement

Acces road overlay (20 years) 4,000

Subtotal 13,000

Contingency (15%) 2,000

Total $15,000

XIV-1

Page 73: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

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Page 74: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

TOTAL DRAIN AGE AREA----------------52 SO MIAVERAGE PRECIPITATION DEPTH OVER AREA

R OA SOM (48-HOURS) _ 28.10INCHES

..... EFFECTIVE TOTAL -------- 14.04 INCHES 3... .. RUNOFF (INCLUDING BASE INFLOW)

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2 STANDARD PROJECT FLOODwoiS

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7 2ND DAY 3RD DAY -lop=LOS ANGELES DISTRICT

Page 75: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

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Page 76: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

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Page 77: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

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Page 78: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

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Page 79: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

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Page 80: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

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Page 81: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

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Page 82: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

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FLOODWALL LOADING CONDITIONS

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FIGURE 9

Page 83: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

~S ARPAY ENGINEER GISTRICT

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Page 84: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

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Page 85: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

VALUE ENGINEE

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Page 86: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

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Page 87: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

VALUE El

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Page 88: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

4EERI ALUE PN~EI PAYS5

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Page 89: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

VALUE ENGINEER"I

2240 0620

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Page 90: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

VALUE ENGINEERING PAYS

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Page 91: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

VALUE ENGINEERIN

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1217,183

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Page 92: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

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Page 93: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

VALUE ENGINEERING

2120-

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2100

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Page 94: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

AYLUE ENGINEERING PAYS

£~2Op55oC12054 66

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Page 95: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

VALUE ENGINEERING I

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Page 96: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

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Page 97: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

VALUE ENGINEERING P

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Page 98: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

IVALUE ENGINEERING PAYS

0___ _ _ _

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Page 99: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

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Page 101: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

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Page 102: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

-T~ 0 -1.

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VALUE ENGINEERING PAY!

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Page 104: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

VALUE EGNEIGPY

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Page 105: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

VAL-"E ENGINEERING PAYS

LEVEE CONTOL LINiE

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Page 106: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

VALUE ENGINEERING PAYS

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Page 107: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

VALUE IENGIN-EERING -PAYS

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Page 108: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

LUE EGNEIGPY

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§A 'ETY PAYS PLATE 3

Page 109: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

VALUE ENGINEERING I

f N

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Page 110: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

SALUE ENGINEERING PAYS

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Page 111: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

VALUE ENGIN4EERIN,

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Page 113: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

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Page 114: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

VALUE ENGINEERING PAYS

7-

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SAFETY PAYS

Page 115: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

VALUE EiNERING P,

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Page 116: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

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Page 117: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

1170 05'

DRAINAGE BOUNDARY)

SUBAREA BOUNDARY

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RCALE IN MILES

1837

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Page 118: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

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Page 119: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

116 0 55k li16 50'

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US ARMY CORPS OF ENGINEERSLOS ANGELES DISTRICT

PLATE 20

Page 120: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

U. S. ARMY ENGINEER DISTRICT

197+50 195+00 192+502280

2275__________ £

NOV 1965. DEPO',S.O

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LEGEND- -- - - -LEVEE TOP (1960)

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---------------- (1967) STREAMBED AT LEVEE

21801- - - (11987) -LEVEE TOE (1960)

21751 LOWEST STREAMBED ELEV WITHIN 100' OF LEVEE

185+00 182+50 180+00 SATO

Page 121: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

12+50 190+00 187+50 185+00

NOV 1965, DEPOSITION TO WITHIN 2' OF LEVEE TOPSCOUR TO 15' BELOW LEVEE TOP

2260

- 2255

2250

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2240

2230S _____2225

2215

7) STATIONS 197+50 TO 175+00

historic StreambedProfiles at Levee

SANTA ANA RIVER. CALIFORNIAE U. S. ARMY ENGINEER DISTRICT10+00 SAIN 177+50 175+00 LOS ANGELES, CORPS OF ENGINEERS

Page 122: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

U. S. ARMY ENGINEER DISTRICT

17 +00 172+50 17_________167+

DEC 1966, DEPOSITION T,: ABOUT 2' BELOW LEVEE TOP

218

2145

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______________________ ______________________N

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210250 6+01 5 5

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Page 123: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

CORPS OF ENGINEERS

70+00 167+50 165+0 +50

TO ABOUT 2' BELOW LEVEE TOP

JAN 1969, HEAVY DEPO ITION ANDMINOR LEVEE OVERTOPPING(DIVERTED BACK TO CHANNEL BY HIGH GROUND) 27

2165

2160

2155

2150

N 2145

.2 2140

0 2135

MILL CREEK LEVEE7) STATIONS 175+00 TO 152+50

Historic StreambedProfiles at Levee

SANTA ANA RIVER, CALIFORNIAE _______________________ U. S. ARMY ENGINEER DISTRICT

57+50 155+00 152+50 LOS ANGELES, CORP~ OF ENGINEERSSTATION PLTE I

L~~~~~~~LT 22_______________

Page 124: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

U. S. ARMY ENGINEER DISTRICT

15+0150+00 147+50

2105

2095

2090

2060

Z 2055

>0 05

LU2045

2035

2030

2025

2020

LEGEND -

2015 - - - -- LEVEE TOP (1980)SPF MAIN CHANNEL WATER SURF(1967)(1 980)

------------- (1967) STRE AMBED AT LEVEE2010 -.- - - -(1987) -

LEVEE TOE (1960)

20051 0 LOWEST STREAMBED ELEV WITHIN 100' OF LEVEE140+00 13750 135+00 STATION

Page 125: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

T ~CORPS OF ENGINE ERS

1 1+50 145+00 14 +50 140+00

2085

-S %~S*5% ____ ___ ___ ____ ___ ___2080

2075

2070

2065

-2060

67) STATIONS 152+60 TO 130+00

Historic StreambedProfiles at Levee

SANTA ANA RIVER, CALIFORNIAEEA 7 U. S. ARMY ENGINEER DISTRICT

1135+00 SAIN132+50 130.00 LOS ANGELESCORPS OFENGINEERS

i

PLATE 23

Page 126: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

U. S. ARMY ENGINEER DISTRICT

130+00 127+50 125.002020

2015

2010

2005

2000

ZST 12+0

1975

0 1970F

> 196

1960

1955

1950__ _ _ _ _ _ _ _

1945

1940

1935 _ _ _ _ _ _ _ _ _ _ _ _ _

LEGEND-1-3-0 LEVEE TOP (1960) __________

193 -SPF MAIN CHANNEL WATER SURF.(1967)r -(19830)

-------------- (1967) STREAMBED AT LEVEE1925 - - - - -(1987)

LEVEE TOE (1980)

1920 LOWEST STREAMBED ELEV WITHIN 100' OF LEVEE

120 1___+00__112_50

STATION

Page 127: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

CORPS OF ENGINEERS

+00 122+50 120+00 117+50

2000

1995

1990

1985

1980

1970

1965

DEC 1966. TOE UNDERMINING 16

AND PARTIAL COLLAPSE

1955

MILCEE EE

2+50 ~ ~ ~- MI N10+01750LSALS CREK LFEVGIEESTATIONSPLAT 13+02O1045

Page 128: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

U. S. ARMY ENGINEER DISTRICT

107+50 105+00 102+50 loc1940

1935

1930

1915

DEC 1968, OVERTOPPING

FLOW (1000 cf.)o 1890 AND LEV EE DAM A G_ _ _ _ _ _ _ _ _-

> 1885w

1860

1870

1855LEGEND

- - - - LEVEE TOP (1980)_______1850 - - SPF MAIN CHANNEL WATER SURF.(1967)(1980)

------------------ 197)~ STrEAMBED AT LEVEE1845 - - . (1987)

LEVEE TOE (1960) ZSTA 88170

1840 LOWEST STREAMBED ELEV WITHIN 100' OF LEVEE

95+00 92+50 9+0 STATION 8

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CORPS OF ENGINEERS

02+50 100+00 97+50 95+00

............. 1 9 1 5

DC 1966, SCOUR TO BUT NOT BELOW TOE

-......... D 1910

1905

. ............. 1900

189

1895

5- JAN 1969, OVERTOPPING

______ -~MILL CREEK LEVEE)67) STATIONS 107450 TO 86+00

Historic StreambedProfiles at Levee

TA8+70 SANTA ANA RIVER, CALIFORNIAVEE Z-SA8U. S. ARMY ENGINEER DISTRICT

190+00 SAIN87+50 86400 LOS ANGELES, CORPS OF ENGINEERS

PLATE 25

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U. S. ARMY ENGINEER DISTRICT

__0+00__87+50__ 85____ 82

1870

1860

1855

1820__ _ _ _ _ _ _ _

w0

FEB 1 9,LEEEDETRYE

180

LEVE TO69 (1960) DETOE1790~~~~COSCUTN FLOWAN HNE WTRSRF(97

LEVEE TOE (1960)

0 LOWEST 6 STREAMBED LVWIAN10'O LEVEE1780 197

075 LO5E00 72+50BE 7LVWTI 0'O EE77+5075+00STATION

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CORPS OF ENGINEERS

85 00 82+50 80+00 77+505ING

DEC 196(, ROAD ON TOPOF LEVEE UNDERCUT

1845

1840

1835

1830

1825

1820

1815rB 1?69, LEVEE DESTROYED

BY CROSS-CUTTING FLOWY

____ ____ ____ ____ - -1810

DEC 1966. LEVEEL_,, BURIED BY DEPOSITION

MILL CREEK LEVEE967) STATIONS 90+00 TO 87+50

Historic StreambedProfiles at Levee

SANTA ANA RIVER. CALIFORNIAVEE U. S. ARMY ENGINEER DISTRICT72+50SATO 70+00 6 7450s LOS ANGELES, CORPS OF ENGINEERS

PLATE 26

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U. S. ARMY ENGINEER DISTRICT

I t__o_ t . ~

U _ _ _ i>____ ____ ___ ______________________

____ _ 4 __ .. .. . .

4. I

4 . . . . . . . . . .

w .~I~ ... . F7

so 10 o 204044 50 S 7

4 ~~~~~~ ~TTO (FEET)_ .~ 7. __ ____

Page 133: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

CORPS OF ENGINEERS

- -~. . . . . . .....

I

-t 1

I~ ~ I cr-'

__ *------ t .7 9

4 6 . . . .- ... -.-.

.. T7 .. ....__ ... ~+I _ _ __

.'*~- ... MILL CREEK LEVEEI..CROSS-SECTION

NEAR LEVEE STATION 96+00

SANT ANARIVER. CLFRI

0 ~O 50 ~ ~ 0 800 s. 90 0 10 U. S. ARYENGINEER DISTRICTSTATION (FEET) LOS ANGELES, CORPS OF ENGINEERS

PLATE 27

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VALUE ENGINEERING PAY

I- W' ;.'AcI

;J1 3 JN ~ / - "-

44 ~

T , 'P /

~WffU"7:.1

SPILWAY \

_ _ - K q d

-~5-3

N'--.

Q O G4Ar

SAET PAYS

Page 135: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

-4 4? .W

~- T k~-- 7-!il 31 0 Younger oluvium

As Potato SndstonT -~Kqm C~W t0"e mo tz ummozme

" Contact; ~qmo~eww ocle

446 It" ~ ~ Faunt whomie a.opprmoieA

X170 Strie &Wd dip of bedding

-~ e..aN4,' 'X Sim of Vertical beddina

'1,T5 Strike and dip of foliaition

1111, Strike of erticol foliation

~- - N - - ~NOTEKqd~K~

Cifnia otheser Snperrino Ceonty,Cal Soutlweer SoIJIG Seialrn Cunty,

n ,. -

~ -C. L

/ . w:/

- / *'~'Ii'C-.

o a N

0 N0

*MY ENGNEWE DiSUCT0 Ncl LO ANGELIS

50 I" .... A. -j.,o.

Ps MIL CREEK2~ LEE

~o~o,.REGIONAL GEOLOGY

-' -All

A. mOlIO WEC' OA0

SAFETY PAYS PLATE 28B

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________________VALUEENGINEERING__PAY

Sacrn r d adn o Mo>

3 41* 5'

SanCb riel

CF QC

wc$~

-3 40

2

B

2 6 8 10 1

5 C C le i mile

LE4;EOO C

fal, ab o h utrwQsdUn erait i fut ra e lo ato

siMilCore e Fa l mIon A deaea ltsR h e atrF

SAFETYPY

Page 137: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

~VALUE ENGINEERING PAYS

Mojave:Pr)23 Q Moun tain's Desert

354*15'

Son-S~.! iGorgonio .

% H.'Peakk -k Cr O/k

B[) F CoacheflloiValle

Banning 00 Gorgoni 10

San JacintoMountains

D R,

REVISION$-

U. S. AIAY ENCINIR IXSThRC

-OPS OF ENG114aS~SIAO y SANTA ANA RI ER AN M. CIFORNIA

SBSAF South Branch, Son Andreas Fault PAEr EEA EINMEOADU

'de Fut SF Son Jiacinto Fault MILL CREEK LEVEEWCF Wilson Creek Fault G" EINLTCOI A

WWR Whitewoter River o~., EINLTCOI A

SNBMITTDV0.UfOR 'CNO ACWD N. -

~, OF

SAFTY AYSPLATE 29

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VALUE ENGINEERING I

1180 ~ ~11 94 N ~ 7

- -894

N 9180

9 181 191

PACFI OCEA

.0"EY AY

Page 139: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

SVAU ENIERN PAYS

117- 1165 50

-'NTH A 'N

ER MI T DE1. 3

FAL - dohdweeNP--~~yl~ l di~

whr'reaeTHUS FAUL

IATQAE EICNE ANIUE 203

A 4 2 Bs fal ma omple dfo th MG elgi

Map. ofAL Ca o hd te. 5tortnylte.dt

5 0 0 5 2

SC GNE RA NOTESsIML

l- -SN- SI Al OltlQ~keSwil mgiltuds , 0, orM NGoter DIrn,

1.0 ^ "N

4 HstoeC Ottgu~e5

wit maniude 60 gret,

A 33LE MILELSREK L~ E

Isaer FAL'NNATOAK PCNE A

k'4esD II W N, W lis,.. ,- -0r.0 ROVSIO7

0 0 . . S A Y E H Q S U O ~ f O F

COO AGES I

SAFETYh OAY PLATIE 30

Page 140: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

VALUE ENGINEERING

~mS,\f ,, li, 4

j,.* w ~ /7

0. . f"72

~' 4

U, ' 1 "' 4

/40.= E'~

St o

- t-7

'000 . 60,1 90 -w.

SCALEHH F I I62I500 j' IE

SCALE 90101ff 1 - -3 0 LOMF'EOS

SAFETY PAY

Page 141: including Santiago Creek - DTIC · 4. Plan and Profile station 182+29.26 to station 167+25.17 5. Plan and Profile station 167+25.17 to station 152+23.64 6. Plan and Profile station

UEREAT ENGINERIN PAYSEDc M9

- A..

A~~ ~ ~ OI'RCOCMPN

Q, N-'A L AN A NA RI E

(SEE9 LO A INMP

(SEE ICINIY MAP

7 z BEAUMOTNET CNRUSERECMPN

SSANTAN SOVERCE

CALIFORNIACAL P0TLN CEMNTCESp(SEE ON CA ION MAP)AT

CL AV A ETY CMPN

SAN CNOSA COL O N A~ (SEE VICINIYLMAP

MOAEALMN CrO.IACAr OP

CEMELNT SOURCES

CJLTONCALl FOANI A

- E STEN AlSH CC A VAJO LA N

r CALISCRALA

(T WSTERN ASH CC. MPAAHE PLANT

C CHISE,ARIZONA

ATPROJECT LOCATION

RE ISIOSC NS N

SAEU PAYSNINERDST