NI 43-101 Technical Report - Nevada Energy Metals · NI 43-101 Technical Report Dixie Valley Project , Churchill County , Nevada, USA . Prepared for: Nevada Energy Metals Inc. 1220

NI 43-101 Technical Report Dixie Valley Project, Churchill County, Nevada, USA

Prepared for: Nevada Energy Metals Inc. 1220 -789 West Pender Street Vancouver, BC, Canada V6C 1H2 Location: Sections 13, 24, 25, 36 Township 23 North, Range 35 East Sections 7, 8, 9, 16, 17, 18, 19, 20, 21, 28, 29, 30, 31, 32, 33 Township 23 North, Range 36 East Sections 1, 10, 11, 12, 13, 14, 15, 22, 23, 24 Township 22 North, Range 35 East Sections 4, 5, 6, 8, 9, 18 Township 22 North, Range 36 East Mount Diablo Meridian Churchill County, Nevada 39.817° N, 117.963° W

This Report Prepared by the following Qualified Person: Alan J. Morris MSc, CPG Spring Creek, Nevada, USA Effective Date: August 8, 2016

NI 43-101 Technical Report Dixie Valley Project, Churchill County, Nevada Alan J. Morris CPG QP

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Important Notice

This report was prepared as a National Instrument 43-101 Technical Report in accordance with Form 43-101F1 for Nevada Energy Metals Inc., by Alan J. Morris, CPG, QP. The quality of information, conclusions, and estimates contained herein is consistent with: 1.) information available at the time of preparation, 2.) data supplied by outside sources, and 3.) the assumptions, conditions, and qualifications set forth in this report. This report is intended for use by the property owners and is approved for filing as a Technical Report with Canadian Securities Regulators.


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Certificate of Qualified Person

To accompany the report entitled “NI-43-101 Technical Report, Dixie Valley Project, Churchill County, Nevada”, prepared for Nevada Energy Metals dated August 8, 2016 with effective date 8 August 2016.

I, Alan Jesse Morris, residing in Spring Creek, Nevada, USA do hereby certify that:

1.) I am the Principal geologist with Ruby Mountain GIS with an office at 237 Ashford Drive, Spring Creek, Nevada, USA.

2.) I graduated with a Bachelor of Science degree in Geology from Fort Lewis College, Durango, Colorado in 1976 and a Master of Science Degree in Geographical Information Science from Manchester Metropolitan University in 2003. I have 37 years of geologic mineral exploration experience in the western United States, Alaska, and Yukon, Canada. My primary experience is with early stage generative projects and mid-stage drill projects for precious metals, base metals, uranium and lithium. My experience with lithium brine deposits in Western Nevada dates from 2010,

3.) I am a Certified Professional Geologist with the American Institute of Professional Geologists, registry number 10550. I am a Licensed Geologist in the State of Utah, USA (5411614-2250) and a Registered Professional Geologist in the State of Alaska, USA (555). Nevada does not have a registration or licensing program for Exploration Geologists.

4.) I spent one day on the property Dixie Valley Property on May 23, 2016.

5.) I have read the definition of a “qualified person” set out in National Instrument 43-101 and certify by virtue of my education, affiliation to a professional association and past relevant work experience, I fulfill the requirements to be a ”qualified person” for the purposes of National Instrument 43-101 Standards of Disclosure of Mineral Projects (NI 43-101) and form 43-101F1.

6.) I, as a qualified person, am independent of the Property, the vendor, and the issuer as defined in Section 1.5 of National Instrument 43-101.

7.) I am responsible for this report in its entirety.

8.) I reviewed the initial staking proposal for the property and visited the property prior to the preparation of this report.

9.) I have read National Instrument 43-101, and this report has been prepared in compliance with the instrument.

10.) I hereby consent to the public filing of the technical report entitled “NI-43-101 Technical Report, Humboldt Salt Marsh Project, Churchill County, Nevada” (the “Technical Report”) and any extracts from or summary of the Technical Report Dated 6 August 2016.

NI 43-101 Technical Report Dixie Valley Project, Churchill County, Nevada Alan J. Monis CPG QP

As of the date of this certificate, to the best of my knowledge and information, this report contains all scientific and technical information that is required to be disclosed to make this Technical Report not misleading .

Signed and Sealed

Alan J . Morris, CPG, QP

Dated: 8 August

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Contents 1.0 Summary ......................................................................................................................... 8

1.1 Introduction .................................................................................................................. 8

1.2 Property Location and History ...................................................................................... 8

1.3 Geology and Mineralization .......................................................................................... 8

1.4 Exploration ................................................................................................................... 9

1.5 Drilling .......................................................................................................................... 9

1.6 Sample Preparation, Analysis and Security.................................................................10

1.7 Data Verification .........................................................................................................10

1.8 Mineral Processing and Metallurgical Testing .............................................................10

1.9 Mineral Resource Estimate .........................................................................................10

2.0 Introduction ....................................................................................................................14

2.1 Purpose and Terms of Reference ...............................................................................14

2.2 Sources of Information ................................................................................................14

2.3 Qualified Persons .......................................................................................................15

2.4 Effective Date .............................................................................................................15

2.5 Field Involvement of Qualified Persons .......................................................................15

2.6 Contributors ................................................................................................................15

2.7 Units of Measure .........................................................................................................15

2.7.1 Common Units .....................................................................................................15

2.7.2 Metric Conversion Factors ...................................................................................16

2.7.3 Abbreviations .......................................................................................................16

3.0 Reliance on Other Experts..............................................................................................17

4.0 Property Description and Location ..................................................................................17

4.1 Location ......................................................................................................................17

4.2 Property Position ........................................................................................................17

4.2.1 Located Claims ....................................................................................................18

4.3 Property Agreements and Royalties ............................................................................18

4.4 Environmental Liability ................................................................................................18

4.5 Operational Permits and Jurisdictions .........................................................................18

4.6 Requirements to Maintain the Claims in Good Standing .............................................19


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5.0 Accessibility, Climate, Local Resources, Infrastructure and Physiography ......................24

5.1 Accessibility ................................................................................................................24

5.2 Climate and Physiography ..........................................................................................24

5.3 Local Resources and Infrastructure ............................................................................25

6.0 History ............................................................................................................................26

6.1 Regional Mining History ..............................................................................................26

6.2 Property History ..........................................................................................................26

7.0 Geological Setting and Mineralization .............................................................................27

7.1 Regional Geology .......................................................................................................27

7.2 Property Geology ........................................................................................................27

7.3 Mineralization ..............................................................................................................28

7.4 Alteration ....................................................................................................................28

8.0 Deposit Type ..................................................................................................................30

8.1 Exploration Model .......................................................................................................31

9.0 Exploration .....................................................................................................................32

9.1 Surface Exploration .....................................................................................................32

9.2 Geophysical Surveys ..................................................................................................32

9.2 Geochemical Exploration .............................................................................................38

10.0 Drilling ............................................................................................................................40

11.0 Sample Preparation, Analysis and Security ....................................................................40

12.0 Data Verification .............................................................................................................40

13.0 Mineral Processing and Metallurgy .................................................................................40

14.0 Mineral Resource Estimates ...........................................................................................40

23.0 Adjacent Properties ........................................................................................................40

24.0 Other Relevant Data and Information .............................................................................41

25.0 Interpretation and Conclusions .......................................................................................41

26.0 Recommendations .........................................................................................................41

Appendix 1. Claim Names and Serial Numbers ........................................................................45

Illustrations

FIGURE 1 DIXIE VALLEY PROJECT LOCATION ............................................................................................................... 12 FIGURE 2 DIXIE VALLEY PROJECT REGIONAL LOCATION MAP .................................................................................... 13 FIGURE 3 DIXIE VALLEY PROJECT ACCESS MAP........................................................................................................... 21


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FIGURE 4 DIXIE VALLEY PROJECT PROPERTY MAP ...................................................................................................... 22 FIGURE 5 DIXIE VALLEY PROJECT CLAIMS ................................................................................................................... 23 FIGURE 6 DIXIE VALLEY PROJECT GENERALIZED GEOLOGIC MAP .............................................................................. 29 FIGURE 7 DIXIE VALLEY PROJECT GENERALIZED GEOLOGIC UNITS ............................................................................ 30 FIGURE 8 DIXIE VALLEY PROJECT RESIDUAL GRAVITY ................................................................................................ 34 FIGURE 9 DIXIE VALLEY PROJECT LEVELED MAGNETICS ............................................................................................. 35 FIGURE 10 DIXIE VALLEY SEISMIC LINE LOCATIONS .................................................................................................... 36 FIGURE 11 DIXIE VALLEY SEISMIC SECTIONS ............................................................................................................... 37 FIGURE 12 USGS SOIL SAMPLE RESULTS ..................................................................................................................... 39


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1.0 Summary

1.1 Introduction

Alan J. Morris, C.P.G. was retained to prepare a technical report on the early stage Dixie Valley project. The purpose of the report is to summarize the location, general geology, and previous exploration on this property, and its viability as a Property of Merit for continued exploration. This report is intended to comply with the requirements of National Instrument 43-101 (NI 43-101).

1.2 Property Location and History

The project is located in Dixie Valley, Nevada, about 160 air-line km east-northeast of Reno, Nevada in Sections 13, 24, 25, and 36, Township 23 North, Range 35 East; Sections 7, 8, 9, 16, 17, 18, 19, 20, 21, 28, 29, 30, 31, 32, and 33, Township 23 North, Range 36 East; Sections 1, 10, 11, 12, 13, 14, 15, 22, 23, and 24, Township 22 North, Range 35 East; Sections 4, 5, 6, 8, 9, and 18, Township 22 North, Range 36 East, Mount Diablo Meridian, Churchill County, Nevada.

The center of the property is about 39.829° North Latitude, 117.989° West Longitude, (39° 49’ 30” N, 117° 56’ 57”): UTM X 417,500 UTMY 4,408,000 NAD 27; Zone 11 N.

1.3 Geology and Mineralization

Dixie Valley is located on the eastern margin of the Walker Lane, a structurally complex tectonic zone formed by interaction of the NNW trending strike-slip movement of the Pacific Plate and ENE – WSW extension of the Great Basin. This zone is still geologically very active with numerous earthquakes and recent volcanic activity. The interplay of the two structural regimes results in a trans-tensional environment characterized by deep rhombochasm basins and steep ranges. Since the extensional movement is on-going, the basins continue to sink, preserving the basin fill and fluids. Dixie Valley is more influenced by mostly east-west extension of the Great Basin and somewhat less by the strike – slip motion of the Walker Lane and its parent San Andreas Fault system.

The entire basin is about 98 km long and up to 16 km wide. Humboldt Salt Marsh, the central playa, is about 10 km northeast - southwest and 6 km east – west in extent. The basin is bounded on the west by the Stillwater Range and on the east by the Clan Alpine Range. Low divides in the valley floors mark the north and south boundaries of Dixie Valley.

The Stillwater and Clan Alpine Ranges are composed of thrust sheets of Triassic and Jurassic age marine sedimentary rocks and Jurassic intrusive complexes that were accreted to the North American continent during the Cretaceous. These rocks have in turn been intruded by Cretaceous and Tertiary igneous bodies and covered by their volcanic equivalents. In the southern Stillwater Range an entire Tertiary caldera complex, including the sub-volcanic intrusive body, is exposed in the range front.


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At the end of the last ice age, water filled the central part of Dixie Valley to a depth of about 70 meters. Radiocarbon dating of tufa in Dixie Valley and adjacent valleys indicate high water stands at about 12,000 to 14,000 and 45,000 to 50,000 years ago. Hydrogen and oxygen isotope data indicate the vast majority of the water in Dixie Valley is ice age in origin indicating very little modern input into the basin. Other stable isotope studies show the basin water contains between 10 and 20 percent geothermal water presumably sourced from deep faults on the western side of the basin.

These ranges are fault bounded, with the greatest movement along the Stillwater Range (west) side of the valley. Vertical displacement along this fault complex is at least 3,000 meters, as evidenced by volcanic rocks exposed near the top of the range being found beneath 1,500 to 2,000 meters of post-volcanic valley fill. These faults are still very active with earthquakes greater than magnitude 6 occurring in 1915 and 1954.

In the area of the Humboldt Salt Marsh playa, the valley appears to be about 2,000 meters deep, primarily filled with poorly sorted coarse conglomerate, gravel, sand and silt with volcanic rocks, and tuff beds, and finer sediments in the lower third of the section (Blackwell et al, 2014). Multiple governmental, academic and industrial geophysical studies have been conducted in the valley to help guide geothermal exploration in other basins. However, many of the conclusions of these studies were shown to be incorrect by production drilling so studies continue to search for surface exploration methods that hold up better to drill testing.

Dixie Valley is home to a large and long-lived geothermal system that is still active. The Caithness Dixie Valley geothermal plant, about 18 km northeast of the center of the playa, is currently producing about 66 megawatts of power. The active geothermal system extends about 30 km roughly north – south along the range front fault. The heat source appears to be simple very deep circulation into the crust; it is not related to igneous activity. Miocene to recent volcanic rocks are found in the ranges and valleys.

Geologically recent air fall tuff from the Long Valley Caldera event (740,000 years before present) and minor eruptions from the Mono – Indio crater chain (latest event was about 650 years ago) form ash beds barely exposed on the surface but likely preserved in the basin.

These ashes are enriched in lithium and readily release at least part of it during devitrification and hydration reactions with meteoric water. Deep circulating geothermal waters may also leach lithium from deeper sources in addition to surface sources. The lithium released to the water is then concentrated by evaporation within the playa, forming a brine deposit that may be economic to extract and process (Munk et al, 2015, Price et al, 2000).

1.4 Exploration

As of this report, Nevada Energy Metals has not conducted any field work on the property other than some geologic reconnaissance and claim staking.

1.5 Drilling

Nevada Energy Metals has not conducted any drilling on the property to date. Geothermal production wells and re-injection wells provide some subsurface data but the majority of these


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have targeted the range bounding structures on the western side of the valley that host the hottest water, not the more static and cooler central valley which hosts the lithium target.

1.6 Sample Preparation, Analysis and Security

As of the time of this report, no samples have been collected from this property by the current owners. Adjacent property owners and academic investigators have used a variety of sample preparation methods and analytical methods. At the time of the academic studies, sample security and chain of custody were not recorded.

1.7 Data Verification

No proprietary data have been identified or reviewed on this project area. All data used in preparation of this report are derived from public domain sources. These reports are authored by reputable individuals or organizations and are assumed to be factually accurate.

Information gleaned from 43-101 reports from adjacent properties is presumed to have been verified by the authors of those papers so will be used with attributions.

1.8 Mineral Processing and Metallurgical Testing

Not applicable; no metallurgical work has been done on the property.

1.9 Mineral Resource Estimate

Not applicable; no significant work has been done on this property.

1.10 Conclusions and Recommendations

The geologic setting and presence of lithium in active geothermal fluids and surface salts in Dixie Valley match characteristics of lithium brine deposits at Clayton Valley, Nevada and in South America. While the geothermal fluids in Dixie Valley contain lithium in the 3 to 5 ppm range and surface silt samples contain up to 530 ppm lithium, at this point the lithium target in this basin is highly conceptual.

Although several workers have studied the geology of Dixie Valley in some detail for geothermal energy production, the lithium potential has not been specifically addressed. Essentially no exploration work for lithium has been done in this valley.

It is recommended that Nevada Energy Metals undertake a phased exploration program of surface sampling, auger or push drill water sampling, and geophysical work to choose drill sites for an initial drill test of the property. Execution of each phase and steps within the phases would be contingent on favorable results from the previous efforts.

The initial part of phase one would include data compilation, creation of GIS data sets and base maps, auger or shovel sampling of sediments and/or water, supervision and reporting. This phase is underway and will cost about $35,000.

Phase one should also include gravity, seismic, or other geophysical surveys of the claim block to determine the depths to bedrock and sub-surface structure. This work would be


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supplemented by additional auger or deeper GeoProbe mud and water samples. This effort, including bonding, geologic supervision, and reporting, is budgeted at $200,000.

Phase two would be to drill test the property for lithium bearing brines and/or solids. Drilling, assays, and geologic supervision will run about $2,265,000. Depending on weather, rig availability, and permits, the drilling should also be broken into two stages to allow for results from the first round to guide locations for the second round.

The total budget for this program is in the $2,500,000 range and would be spread over about 6 months to a year depending on permitting, rig availability, and weather.


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Figure 1 Dixie Valley Project Location


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Figure 2 Dixie Valley Project Regional Location Map


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2.0 Introduction

This report was prepared by Alan J. Morris C.P.G., Q.P. at the request of Nevada Energy Metals for the purpose of compiling an overview of the previous exploration efforts in this district and specifically on the Dixie Valley property position. This report is intended to comply with the standards dictated by National Instrument 43-101 in regard to the DV, DVA, DVB, DVC, and DVD claim groups located in Churchill County, Nevada.

This report is not intended to define an economic conclusion upon which to make a development decision.

Alan J. Morris understands Nevada Energy Metals will use this document for reporting purposes.

Alan J. Morris is a consulting exploration geologist with approximately 37 years of experience at all levels of mineral exploration and development for several commodities. He is a Certified Professional Geologist through AIPG, a Fellow with the Society of Economic Geologists, and a member of the Geological Society of Nevada. He provides his services through Ruby Mountain GIS in Spring Creek, Nevada.

2.1 Purpose and Terms of Reference

This report is prepared using the industry accepted Canadian Institute of Mining, Metallurgy, and Petroleum (CIM) “Best Practices and Reporting Guidelines” for disclosing mineral exploration information, the Canadian Securities Administrators revised regulations in NI 43-101, Form 43-101F, (Standards of Disclosure for Mineral Projects) and Companion Policy 43-101CP and CIM definitions “Standards for Mineral Resources and Mineral Reserves” (December 11, 2005).

Alan J. Morris is not an associate or affiliate of Nevada Energy Metals and his fee for this Technical Report is not dependent in whole or in part on any prior or future engagement or understanding resulting from the conclusions of this report. The fee is in accordance with standard industry fees for work of this nature. Alan J. Morris does not have any financial interest in Nevada Energy Metals or any affiliated company.

2.2 Sources of Information

The information in this report has been compiled by the author from published historical works and personal experience in the district and region. These historical reports appear to be based on factual data and the interpretations of their authors. None appear to have been modified to mislead the prudent reader. The author does not know of any existing information in the public domain or developed by Nevada Energy Metals that has been intentionally omitted to mislead the reader about the viability of this project.


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2.3 Qualified Persons

The Qualified Person responsible for this report is Alan J. Morris, a consulting geologist contracted by Nevada Energy Metals.

2.4 Effective Date

The effective date of this report is August 8, 2016

2.5 Field Involvement of Qualified Persons

The author spent a day examining the land tenure and conducting a quick reconnaissance of the geology.

2.6 Contributors

There are no other contributors to the report.

2.7 Units of Measure

Units of measure in this report are metric unless otherwise noted. English equivalents are given in parentheses following the metric value where possible.

Budget numbers are given in US dollars.

Locations are given in Longitude – Latitude degrees or UTM X, Y (meters) in NAD 27 Zone 11 projection.

2.7.1 Common Units Above mean sea level AMSL

Cubic Foot feet3

Cubic inch in3

Cubic yard yd3

Day d

Degree °

Degrees Centigrade °C

Degrees Fahrenheit °F

Dollars (US) $

Gallon gal

Gallons per minute gpm

Grams per tonne g/t

Equal to or greater than ≥

Hectare ha

Hour h

Inch ”

Kilo (thousand) k

Equal to or less than ≤

Micrometer (micron) um

Million Years Ago Ma.

Milligram mg

Troy ounces per short ton oz/t

Parts per billion ppb

Parts per million ppm

Percent %

Pounds lb.

Short ton (2,000lb) st

Short ton (US) t

Specific gravity SG

Square foot feet2

Square inch in2

Yard yd.

Year yr

2.7.2 Metric Conversion Factors

Metric Conversion Factors (divided by)

Short tons to tonnes (1.10231)

Pounds to tonnes (2204.62)

Ounces (Troy) to tonnes (32150)

Ounces (Troy) to kilograms 32.150

Ounces (Troy) to grams (0.03215)

Ounces (Troy)/short ton to grams/tonne (0.02917)

Acres to hectares (2.47105)

Miles to kilometers (0.62137)

Feet to meters (3.28084)

2.7.3 Abbreviations

American Society for Testing and Materials ASTM

Atomic Absorption Spectrometry AAS

Bureau of Land Management BLM

Diamond Drill DD

Global Positioning System GPS

Internal Rate of Return IRR

Metallic Screen Fire Assay MSFA

Nevada Energy Metals NVEM

National Instrument 43-101 NI 43-101

Nearest Neighbor NN

Net Smelter Royalty NSR

Reverse Circulation RC/RCV

Rock Quality Designation RQD

Selective Mining Unit SMU

Universal Transverse Mercator UTM

United States Geological Survey USGS


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3.0 Reliance on Other Experts The author of this report did not consult with other experts concerning legal, political, environmental, or tax matters.

4.0 Property Description and Location

4.1 Location

The project is located in Dixie Valley, Nevada, about 160 air-line km (100 miles) east-northeast of Reno, Nevada and about 65 km (40 miles) northeast of Fallon, NV. The claims are in Sections 13, 24, 25, and 36, Township 23 North, Range 35 East; Sections 7, 8, 9, 16, 17, 18, 19, 20, 21, 28, 29, 30, 31, 32, and 33, Township 23 North, Range 36 East; Sections 1, 10, 11, 12, 13, 14, 15, 22, 23, and 24, Township 22 North, Range 35 East; Sections 4, 5, 6, 8, 9, and 18, Township 22 North, Range 36 East, Mount Diablo Meridian, Churchill County, Nevada.

The center of the property is about 39.829° North Latitude, 117.989° West Longitude, (39° 49’ 30” N, 117° 56’ 57”): UTM X 417,500 UTMY 4,408,000 NAD 27; Zone 11 N.

4.2 Property Position

The property consists of 907 placer claims in total, covering about 7340 hectares (28 square miles) of playa and alluvial fan. The claims were staked for Nevada Energy Metals by their agent, Sandy Sullivan of Carlin Trend Mining Services, in April, May and June of 2016. NVEM holds the claims outright with no underlying ownerships or royalty agreement. Holding costs for 907 claims in the block are about $151,035.50 per year in rental fees paid to the Bureau of Land Management and State of Nevada and local fees paid to Churchill County.

Claim rental fees were paid until September 1, 2016 upon filing with the BLM. BLM rental fees for the September 1, 2016 – August 31, 2017 claim year are due by September 1, 2016. A “Notice of Intent to Hold” and County fees for the 2016 – 2017 claim year are due by November 1, 2016.

The claim names and numbers are included in Appendix One.


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4.2.1 Located Claims

Nevada Energy Metals holds a contiguous block of 907 placer claims, each covering about 8 ha (20 acres). Claim location maps are shown in Figure 4 and Figure 5 below.

Block Claims Holding Cost DV 149 $24,812.50 DVA 348 $57,946.00 DVB 160 $26,644.00 DBC 99 $16,487.50 DVD 151 $25,145.50 Total 907 $151,035.50

4.2.2 Leased Properties

LiCo Energy Metals Inc. (formerly Wildcat Exploration Ltd.) entered into an option agreement with Nevada Energy Metals to acquire the DVA block of claims from Nevada Energy Metals. Terms of the agreement include:

1. Payment of $20,000 non-refundable deposit on signing

2. Payment of $180,000 and issuance of 2,000,000 common shares on Exchange approval

3. Issuance of 2,000,000 shares on the first anniversary of the agreement

4. Issuance of 2,000,000 shares on the second anniversary of the agreement

5. 1,250,000 in eligible exploration expenses on or before the third anniversary date of the Option Agreement.

All figures are in US dollars.

4.3 Property Agreements and Royalties

There is a three percent (3%) net smelter returns royalty on commercial production from the claims above in favor of Nevada Energy Metals.

4.4 Environmental Liability

No pre-existing environmental liability is known to exist on the property position.

4.5 Operational Permits and Jurisdictions

The project is located on open federal land managed by the Bureau of Land Management (BLM). Permits are required for all significant surface disturbances. Geologic mapping, soil and rock sampling, and other low-impact activities can be conducted without specific permits on a casual use basis. Any road or trail construction used for mechanized equipment, drilling, or trenching will require a permit from the BLM. Up to five acres of disturbance are allowed on a


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Notice of Intent (NOI) level permit. The NOI can come with restrictions to protect biological, historical, or archeological resources. A performance bond is required to insure the required reclamation work is done.

Disturbance in excess of five acres requires a Plan of Operation which in turn requires an Environmental Assessment. This process is standard practice in Nevada and both the regulators and applicants follow a standard set of rules. Going to a Plan of Operation can require significant environmental and archeological assessment work before the permit can be issued. Lead times for a Plan of Operation can take up to a year or two depending on the environment and the extent of proposed operations. If the regulators consider the property large enough or in a sensitive area, an Environmental Impact Statement may be required before operating permits are granted.

At this point, exploration can be conducted under the casual use provision. As exploration progresses and surface disturbance occurs, Notice of Intent or Plan of Operations level permits will be applied for as required. Permits have not been applied for to conduct exploration beyond casual use on this property.

4.6 Requirements to Maintain the Claims in Good Standing

Claims are subject to a $155 rental fee per 20 acre placer claim due by September 1 each year. A “Notice of Intent to Hold” must also be filed with Churchill County by November 1 each year; the recording fee is $10.50 per claim and a $4.00 document fee for each filing. Based on these numbers, total holding costs for the current Dixie Valley claim block is $151,035.50. .

4.7 Mineral Tenure

The Humboldt Salt Marsh property is held via unpatented mining claims under provisions of the Federal Mining Act of 1872 as amended and regulations issued by the U.S. Department of the Interior, Bureau of Land Management. As long as the rental fees are paid and document filings are made correctly, the claims do not expire. A mining claim grants discovery rights and the exclusive right to explore and develop the claims but it does not give the holder an unfettered right to extract and sell minerals as there are multiple local, state, and federal regulatory approvals and permits required before this can take place.

4.8 Significant Risk Factors

The author is not aware of any significant factors or risks that may affect access, title, or the right or ability to perform work on the property. The area is not within the parts of Nevada being proposed for withdrawal to mineral entry as part of the Greater Sage Grouse management plans. However, similar efforts to protect other species cannot be completely ruled out in the future.

As Nevada is on average the driest state in the nation, it has rather unique water rights laws. All water in the state is deemed the property of the state and water rights are granted by the state as a separate estate from the mineral or surface rights. The mineral rights obtained through the claim process for the lithium brine applies only to the dissolved minerals. The water remains the


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property of the state and water rights must be obtained to pump the water, however unsuitable for drinking or agriculture, from the basin. The availability of suitable water rights in Dixie Valley was not researched as part of this report.


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Figure 3 Dixie Valley Project Access Map


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Figure 4 Dixie Valley Project Property Map


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Figure 5 Dixie Valley Project Claims


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5.0 Accessibility, Climate, Local Resources, Infrastructure and Physiography

Property access, climate, and physical setting are all favorable. The site is remote from large population centers but not so much that it has wilderness value. Normal weather and climate of the area would not hinder year-round access or interfere with exploration and mining activities. Winter rains and occasional thunderstorms can make the playa surface too soft for vehicle travel. The soft surface may require the construction of gravel pads and roads for production well drilling.

5.1 Accessibility

The project is located on the Humboldt Salt Marsh, a dry playa lake in the central part of Dixie Valley in eastern Churchill County, about 160 km east-northeast of Reno (100 miles) and about 65 km (40 miles) northeast of Fallon, NV. The entire basin is about 98 km long and up to 16 km wide. The extent of the Humboldt Salt Marsh central playa is about 10 km northeast – southwest and 6 km east – west. The basin is bounded on the west by the Stillwater Range and on the east by the Clan Alpine Range.

The nearest supply center is Fallon, Nevada, about 128 road km (80 miles) to the southwest. Fallon offers food, lodging, fuel and some exploration services. All mineral exploration services including supplies, analytical laboratories, and drilling service companies are available in Reno, Nevada (225 road km, 140 miles). Reno is the major supply center for exploration activity in Nevada. The nearest airport with commercial service is Reno, Nevada.

Access to the property is east from Fallon via paved highway US 50 for 64 km (39.8 miles) then north on state route 121 for 44 km (27.4 miles) then on a graveled road for about 25 km (15 miles) to the center of the property.

The highways are sufficient for transportation of exploration-size heavy equipment. A network of 4 wheel drive roads and ATV trails provide access to much of the property. Except for a few gravel mounds and sand dunes, all of the property is on a dry lake bed and is accessible by off-road drilling equipment using cross country travel. The playa surface is often muddy, especially in the spring and fall. Being essentially a salt pavement over mud, sinking a vehicle in the playa can occur even when the surface appears to be dry.

5.2 Climate and Physiography

The project area is located at an elevation of about 1030 meters (3380 feet) in the rain shadow of the Sierra Nevada Mountains in the Basin and Range physiographic province. The area has hot dry summers and cool winters. For Fallon, the average high temperature for July is 33.4°C (92.1°F) with an average low of 12°C (53.9°F); in December the average high is 7.7 °C (46°F) with an average low of -7.2°C (19.1°F). http://www.wrcc.dri.edu/cgi-bin/cliMAIN.pl?nvfall


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Total precipitation for Dixie Valley averages 111 mm (4.38 inches) per year with most of this falling in late spring. Rainfall in this environment is highly variable with long dry periods interspersed with major downpours from thunderstorms in the March – October time frame. The State of Nevada, Division of Water Resources website (http://water.nv.gov/mapping/et/et_general.cfm) shows the evapotranspiration potential calculated for shallow open water in Clayton Valley is 1740 mm (5.7 feet) per year for a net deficit of 1615 mm (5.3 ft.) per year.

The property is in relatively flat terrain consisting of playa, sand dunes, and alluvial fans dissected by dry stream channels. Elevations range from 1030 meters (3380 feet) on the playa floor to about 2070 meters (6800 feet) at the crest of the Stillwater Range. Vegetation is minimal consisting primarily of low growing desert shrubs with small forbs between them. The dominant plant on the alluvium is a variety of shad scale. Some small pinyon – juniper trees are found on the upper slopes.

Drilling and exploration access to any point on the property should be fairly easy when the playa is dry. Most points are accessible by ATV for exploration but this is discouraged by the BLM to avoid pioneering new roads.

5.3 Local Resources and Infrastructure

Other than county-maintained gravel roads and unimproved dirt trails, infrastructure on the property is negligible.

The Dixie Valley Geothermal Power plant located about 10 km to the north of the property produces about 63 megawatts of power at normal production levels. The northern Nevada power grid ties into this plant, offering an opportunity for electric power for any operations at this property.

Water quality studies of the springs on the west side of the valley show them to be of suffcient quality to use for drilling and other exploration uses. At this time, a specific source of exploration water has not been identified. As development proceeds, some exploration wells will likely be completed as water wells to provide operational water.

The footprint required for development of lithium brine or clay operation in Dixie Valley is not known at this time since neither the location nor size of the deposit nor the type of processing facility required is not yet known. The playa surface and adjacent low slopes offer plenty of room for facilities if needed. The BLM has demonstrated a willingness at several Nevada mines to swap low quality (for grazing and wildlife) land to be used for processing facilities and buildings for higher quality ranch land (purchased on the open market by the mining company).

Supplies, lodging, food, and fuel are available at Fallon, Lovelock or Austin, Nevada. Fallon and Lovelock also offer some heavy equipment operators for road and drill site construction.

Drill rigs would likely need to come from Fallon or the major regional hub for drilling at Elko, Nevada (416 road km, 259 road miles). In many cases, the drill rig will already be in the area working on other jobs so mobilization distances may be less.

http://water.nv.gov/mapping/et/et_general.cfm


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Mining is a common occupation in the area with several small-to moderate-sized mines opening and closing in the Hawthorne – Fallon – Lovelock area over the past several decades. A well-trained and experienced mining workforce pool is available in Nevada that will flow to where it is needed.

6.0 History

6.1 Regional Mining History

The area was likely prospected as early as the late 1840’s or early 1850’s. The main rush to the Comstock Lode in Virginia City, Nevada started about 1859. Prospectors fanned out from that camp and found several other base and precious metal camps in the western Sierra foothills and across the state. Mineralization at the Dixie Comstock mine was discovered in 1934 by prospectors panning the drainages on the eastern side of the Stillwater Range. The Stillwater Range also hosts small occurrences of other minerals, with copper, mercury, iron, and titanium being reported (Willden and Speed, 1974).

In addition to the hard rock mining, mining of salt and borates from numerous dry lake beds and “alkali springs” in the area took place to supply the larger camps (notably the Comstock / Virginia City District); salt was used for the vat leach mills and borax flux was used for the smelters. Dixie Valley was the site of the earliest commercial production of salt in Nevada. A “large amount” of salt was produced from the playa from 1861 to 1868. The salt was scraped from the surface with hoes and shipped to Virginia City and other districts as far away as Idaho via freight wagons. Construction of the Central Pacific railroad made the local production of salt uneconomic. Ten box car loads of borax were reportedly mined from the northern part of the playa in the early 1870’s (Papke, 1976).

6.2 Property History

Other than the exploitation of the playa crust for salt and borax, no other mining has occurred on the claims. Because of the active thermal springs on the western side of Dixie Valley, geothermal energy exploration was undertaken starting about 1974; these studies continue to the present.

Production drilling for the Caithness Dixie Valley geothermal plant, located about 18 km northeast of the center of the playa, started in 1994. It is currently producing about 66 megawatts of power. The active geothermal system extends about 30 km roughly north – south along the range front fault. The heat source appears to be simple very deep circulation into the crust; it is not related to igneous activity.

As far as is known, no other significant exploration has taken place on the current property.


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7.0 Geological Setting and Mineralization

7.1 Regional Geology

The Stillwater and Clan Alpine Ranges are composed of thrust sheets of Triassic and Jurassic age marine sedimentary rocks and Jurassic intrusive complexes that were accreted to the North American continent during the Cretaceous. These rocks have in turn been intruded by Cretaceous and Tertiary stocks and dikes and covered by their volcanic equivalents. In the southern Stillwater Range, an entire Tertiary caldera complex, including the sub-volcanic intrusive body is exposed.

These ranges are fault bounded, with the greatest movement along the Stillwater Range (west) side of the valley. Vertical displacement along this fault complex is at least 3,000 meters, as evidenced by volcanic rocks exposed near the top of range also being found beneath 1,500 to 2,000 meters of post-volcanic valley fill. These faults are still very active with earthquakes greater than magnitude 6 occurring in 1915 and 1954.

The most recent igneous activity is marked by relatively young basaltic cones scattered throughout the Walker Lane but not within or nearby Dixie Valley. The most spectacular geologically recent event was the eruption of the Long Valley Caldera (~740,000 years ago) when some 6.3 cubic kilometers (1.5 cubic miles) of ash blasted across the western US. The most recent volcanic activity in the western Nevada area was a series of glass and tuff eruptions known as the Mono – Inyo Volcanic chain with the last event occurring in about 1350 AD.

The tuffs for the Long Valley and Mono-Inyo eruptions are strongly enriched in lithium compared to world-wide averages and are likely the source rock for lithium brines in Nevada (Hofstra et al, 2013, Price et al, 2000).

7.2 Property Geology

Dixie Valley is a closed fault-bounded basin with the lowest elevation point (1031 m, 3383 ft.) in the Northern Great Basin on the Humboldt Salt Marsh playa. Age dating and other work at the Dixie Comstock Mine indicate gold mineralization occurred about 500,000 to 350,000 years ago along a range bounding structure that has been offset at least 100 meters since that time (Vikre, 1995). Faulting dated at about 11.1 to 15 million years before present resulted in at least an ancestral Dixie Valley existing from that time until the present. The basin is tectonically active with visible fault scarps formed during earthquakes in 1915 (Mw ~ 7.2) and 1954 (Mw ~ 6.9). With up to 6 meters of dip-slip offset along some of these scarps, it is clear that Dixie Valley is still subsiding.

In the area of the Humboldt Salt Marsh playa, the valley appears to be about 2,000 meters deep, primarily filled with poorly sorted coarse conglomerate, gravel, sand and silt with volcanic rocks, and tuff beds, and finer sediments in the lower third of the section (Blackwell et al, 2014). Multiple governmental, academic and industrial geophysical studies have been conducted in the valley to help guide geothermal exploration in other basins. However, many of the conclusions


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of these studies were shown to be incorrect by production drilling so studies continue to look for surface exploration methods that hold up better to drill testing.

Within the playa, the majority of the exposure is very fine lake bed clays and wind-blown sand. Outcrops of iron rich travertine and algal mound tufa are found around the springs to the west of the property. Due to the very early exploration stage of this property, NVEM has not conducted any new geologic mapping on the property.

At the end of the last ice age, water filled the central part of Dixie Valley to a depth of about 70 meters. Radiocarbon dating of tufa in Dixie Valley and adjacent valleys indicate high water stands at about 12,000 to 14,000 and 45,000 to 50,000 years ago. Hydrogen and oxygen isotope data indicates the vast majority of the water in Dixie Valley is ice age in origin, showing very little modern input into the basin (Blackwell et al 2003 and 2007).

7.3 Mineralization

Exposed mineralization is confined to salt crust on the playa surface and other locations in the valley. Since lithium brine is not well defined as “mineralization” in the conventional sense, it is hard to identify in outcrop exposures; it can only truly be identified in water via chemical analysis (Houston, 2011).

7.4 Alteration

Other than a few scabs of travertine and tufa, no outcropping alteration has been identified on the property. Again, the concepts of alteration and mineralization are different when applied to brines as compared to traditional hard rock mineral deposits. Alteration in this deposit class might well be finding beds of altered glass that are depleted in lithium when compared to unaltered glass and tuff. The alteration in this case would indicate not that metals or metal related fluids have passed through the rock but that fluids capable of mobilizing lithium out of the source rocks and carrying it away have passed through.


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Figure 6 Dixie Valley Project Generalized Geologic Map


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Figure 7 Dixie Valley Project Generalized Geologic Units

8.0 Deposit Type The main mineral target at Dixie Valley is a playa-related lithium brine deposit similar to productive playas in Clayton Valley, Nevada and several areas of South America. The Dixie Valley lithium project is a conceptual exploration play based on solid geologic information and favorable comparison to the lithium brine model.


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8.1 Exploration Model

The target model is a lithium brine model based on Clayton Valley, Nevada and several basins in South America. US Geological Survey Open File Report 2013-1006 lays out seven characteristics of lithium brine deposits (Bradley et al 2013).

The characteristics are:

1. Arid Climate

2. Closed Basin containing a playa or salar

3. Tectonically driven subsidence

4. Associated igneous or geothermal activity

5. Suitable lithium source rocks

6. One or more adequate aquifers

7. Sufficient time to concentrate brine.

The Dixie Valley Project is known to have all seven of these characteristics. How closely this project fits the model for a lithium brine deposit is not necessarily a warranty that an economic deposit will be found here but it is useful as a screening tool to guide exploration efforts.

Dixie Valley is arid: the State of Nevada Division of Water Resources website (www.water.nv.gov/mapping/et/et_general.cfm) shows a 1.3 meter (4.3 ft.) Net Irrigation Water Requirement (NIWR – the net of evapo-transpiration minus effective precipitation) for shallow open water and about 1 meter for low managed pasture grass. Isotopic studies (Blackwell et al 2014) indicate the majority of the water in the basin is of ice age origin, and what little modern precipitation that reaches the valley does not contribute significantly to the ground water.

Dixie Valley is a closed fault-bounded basin with the lowest elevation point (1031 m, 3383 ft.) in the Northern Great Basin on the Humboldt Salt Marsh playa. The basin is tectonically active with visible fault scarps formed during earthquakes in 1915 (Mw ~ 7.2) and 1954 (Mw ~ 6.9). With up to 6 meters of dip-slip offset along some of these scarps, it is clear that Dixie Valley is still subsiding. Given the valley has been a closed basin for at least 500,000 years and probably much longer, plenty of time has elapsed for evaporative concentration of lithium bearing geothermal and surface water.

Specific lithium-rich source rocks have not been clearly identified in this basin but Miocene age felsic ashflows are found in the ranges on all sides, along with shallow intrusive bodies of similar composition. Geothermal water in the basin contains up to 4.89 ppm Li and stream sediment samples from the Stillwater Range show values up to 88 ppm Li. Geologically recent volcanic ash from the Long Valley Caldera (Bishop Tuff) and Mono Craters are expected to be found within the catchment area of the basin and within the basin fill sediments. One major productive


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horizon in the Clayton Valley brine field is thought to be Bishop Tuff deposited and preserved in the basin (Zampirro, 2004).

The conceptual model is the following: as the basin goes through multiple wet and dry periods, lithium dissolved by deep circulating geothermal fluids or leached from local rock units by surface and near surface water is concentrated by evaporation beneath the playa. Heavier brines sink into the deeper levels of the basin or flow downward along tilted permeable beds, potentially forming subsurface pools of lithium-rich fluids.

At the Clayton Valley lithium operation, several different stratigraphic horizons produce lithium brines. These form distinct geologic units and can be correlated from hole to hole in different parts of the basin. One of the most prolific is the “Main Ash Aquifer” and is considered to correlate with the Bishop Tuff (Zampirro, 2004).

Brine exploration can be likened to oil exploration where specific geologic units will be productive while others may be barren or even dilute the target fluid. Drilling of production holes will likely be accomplished by commercial (municipal or irrigation) size water well equipment. These rigs are capable of drilling large diameter holes and casing the holes in such a way to pull from specific intervals and prevent flow from one aquifer to another.

Although the exploration model for this project is based on the Clayton Valley deposit and it is comparable geologically, it is not a sure thing that economic deposits of lithium will be found in this area. Dixie Valley has not been previously explored for lithium potential so by definition, it is not known what will be found.

9.0 Exploration

9.1 Surface Exploration

No formal surface exploration of the property has been conducted by Nevada Energy Metals at this point.

9.2 Geophysical Surveys

Dixie Valley has been used as a test case to develop and test geophysical methods for exploration and development of active geothermal systems. The majority of the detailed surveys were run over the producing steam field to the northwest of the property (Blackwell et al, 2014). Methods used included several types of gravity, magnetic, magnetotelluric, seismic, radiometric, and hyperspectral remote sensing. A detailed discussion of all of the methods and their results is beyond the scope of this report. Details are discussed in Blackwell et al (2003, 2007, and 2014).

Several gravity surveys were run in Dixie Valley from the mid-1970’s through 2013 by several groups with varying densities, goals, and methods. The map below is from a compilation published in Blackwell et al, 2014. The gravity data show a deep valley filled with alluvial debris that was deposited at a slightly slower rate than the subsidence rate of the valley. Gravity work, along with active and passive seismic studies, shows a predominantly trap-door style valley with


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a steep west side and more shallowly dipping pediment on the east. Several potential cross faults and structural disruptions are seen in the data. Structural bends and intersections are the apparent focus of geothermal fluid flow but production drill holes show a much more complicated pattern. These complications, at least partially, are the result of trying to hit high angle structures with vertical or near vertical wells.

A 940 square kilometer high resolution helicopter airborne magnetic survey was flown over the valley and adjacent ranges in 2002. East – west flight lines were spaced at 200 meters with north-south tie lines on 1000 meter spacing. Nominal instrument altitude was 120 meters AGL. Results of the survey were comparable with previous lower resolution ground and airborne surveys but improved resolution yielded greater detail. The survey was very effective in extending the trace of known surface faults under cover and identifying parallel faults under valley fill and pediment gravel. The magnetic anomalies are produced when rock units of different magnetic characteristics meet each other at fault contacts. These features can be seen in standard reduced to pole magnetic intensity plot but are enhanced in horizontal gradient plots. Hydrothermal alteration often destroys mafic (iron – magnesium) minerals in igneous rocks and derived sediments resulting in areas of lower magnetic intensity that may map these conduits. The drawback is the survey cannot tell if this alteration is the result of currently active or extinct geothermal systems.

Both magnetic and gravity data show the existence of “growth” faults where the amount of offset is greater at depth than in the near surface, indicating continuous slippage along the fault as the resulting basin was filled. Faults also do not continue forever along a specific plane, the energy that causes a single major fault can dissipate along a zone of smaller structures and then reform into a single strand, parallel or subparallel to the original structure but offset from the original trend. These “horsetails” are often the site of enhanced fluid flow because the single main structures squeeze closed while the network of smaller offset structures remains open. Because of the shallow depth, recent formation, and active fluid flow along faults in Dixie Valley, these features can be directly observed in the surface geology and indirectly in the geophysics.

From a lithium exploration standpoint, these zones of enhanced fluid flow can represent either sources of lithium-bearing water into an evaporative concentration process or drill targets where fracture-enhanced permeability will allow faster pumping rates.

Two seismic lines were run across the producing geothermal field north of the claim block. These lines support the trapdoor shape to the valley; beds on the western side of the valley dip to the east while beds on the east side dip west. The western beds dip more steeply than those on the east. The growth fault concept is also validated: deeper beds show steeper dips than the shallower beds. The implication for lithium brine exploration is the older, deeper beds will act as conduits directing heavier brines and lithium leached in situ from contained ash beds to the center of the valley, potentially forming a “bathtub” of concentrated brine.

Figures 8, 9, 10 and 11 are modified from Blackwell et al 2014.


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Figure 8 Dixie Valley Project Residual Gravity


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Figure 9 Dixie Valley Project Leveled Magnetics


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Figure 10 Dixie Valley Seismic Line Locations


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Figure 11 Dixie Valley Seismic Sections


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9.2 Geochemical Exploration

The geochemical work done in the valley and to a certain extent at the Dixie-Comstock Mine was directed to determining the age, origin, and potential temperature of the geothermal fluids. Lithium was not a metal of interest but was run on some of the geothermal fluids as a temperature indicator. Maximum lithium values reported in the geothermal fluids (wells and springs) are in the 4 to 5 ppm range with most in the 2 - 3 ppm range. This is about 2 orders of magnitude less than economic lithium brines at Clayton Valley but this degree of concentration has been reported in other basins. Lithium is apparently lost from production fluids after the heat has been extracted. At this point, the researchers have not offered an explanation of where it goes (Blackwell et al 2014).

Twenty two stream sediment samples from drainages in the Stillwater Range that flow into Dixie Valley averaged 45 ppm Li with a range of 10 to 88 ppm (USGS NURE and RASS geochemical databases). Leaching of lithium from volcanic ash and other rocks in the ranges around the basin is also a likely source of metal. In situ leaching and concentration of lithium in ash layers within the basin fill is also a potential exploration target.

Water balance calculations in Blackwell et al, 2014 (pp 57 – 60) indicate the basin is in a steady state, with evaporation essentially balanced with inflows of meteoric and geothermal water. Apparently, much of the precipitation falling in the Clan Alpine and Stillwater Ranges enters the basin as shallow ground water flowing through permeable beds in the alluvial fans rather than as runoff. Several artesian wells and springs are found on the margins of the valleys. Using major element geochemistry, Blackwell et al estimate the shallow ground water in Dixie Valley is about 10 to 25 percent geothermal fluid diluted by meteoric water. This steady state of inflow vs. evaporation is obviously an average since precipitation varies widely year to year. Shallow ground water in the basin has a colder isotopic signature than precipitation falling in the ranges. This indicates most of the water in the basin originally fell as snow during ice ages.

Soil samples collected and analyzed by the USGS in Dixie Valley returned lithium values >100 ppm in 27 of the 189 samples collected. The highest value was 540 ppm. These samples were taken from the playa crust and soils at a depth of 0 to 5 cm. (Hinkle et al 1995). The sampling was directed at detecting active geothermal systems thus the lines were laid out to test known fluid pathways. The higher values were collected to the east of the power plant with the highest of those over apparent structures. None of these samples were collected from the claim block but they do indicate that low to moderate levels of lithium in the springs and geothermal waters are concentrating in the playa salts and brines.


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Figure 12 USGS Soil Sample Results


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10.0 Drilling Although Dixie Valley has been the site of considerable drilling for geothermal energy exploration and development, none has been directed at lithium brine or minerals. Drilling at the Dixie-Comstock mine is confined to exploration of the vein system developed in a splay of the range front fault.

Some summary drill logs and other information from the geothermal drilling to help map basin geology and calibrate geophysical models are available in the public domain. However, most of this is for holes outside of the project area.

11.0 Sample Preparation, Analysis and Security Nevada Energy Metals has not yet collected any samples from the property. Sample handling protocol for any samples taken by Nevada Energy Metals will be in compliance with industry standards. Samples collected by employees or contractors will be placed in the appropriate container and marked in the field with the sample number and, where possible, a second sample number tag will be placed inside of the sample container as a check on the external number. Samples will be secured in locked vehicles or storage facilities until they are delivered to the analytical laboratory.

12.0 Data Verification No previous proprietary data has been identified or reviewed on this project area. All data used in the preparation of this report is derived from published reports. These reports are authored by reputable agencies or academics and are assumed to be factually accurate.

Information gleaned from 43-101 reports from adjacent properties is presumed to have been verified by the authors of those papers so will be used with attributions.

13.0 Mineral Processing and Metallurgy Not applicable at this point.

14.0 Mineral Resource Estimates Not applicable.

23.0 Adjacent Properties Other than the Dixie Comstock gold mine and the Caithness Geothermal Power Plant previously discussed, no significant claim blocks or mining operations are present in Dixie Valley.


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24.0 Other Relevant Data and Information The author is not aware of any other information about the project area that has not been discussed.

25.0 Interpretation and Conclusions Dixie Valley compares favorably with producing brine deposits in Clayton Valley, Nevada and similar operations in South America. Lithium is present in the geothermal fluids in the 2 – 5 ppm range, in playa silts and soil in the 30 – 530 ppm range, and in potential volcanic ash source beds. The district has all of the characteristics outlined in the USGS model for lithium brine deposits (Bradley 2013).

While based on solid but limited geologic information, at this point the Humboldt Salt Marsh lithium project is a conceptual exploration play. Essentially no exploration work for lithium has been done in this valley. A substantial body of geologic, geophysical and some geochemical work related to the active geothermal systems will serve as a base on which to build more detailed work. Gravity surveys have proven to be the most useful method in defining subsurface topography, and sufficient drilling data exists to calibrate three dimensional modeling of the data.

The majority of the drilling has been directed at the basin-bounding faults which host the geothermal fluids. The target for lithium exploration will be more towards the center of the basin where evaporative concentration of geothermal and meteoric water into brines and subsequent sinking of the denser brines into gravity traps may produce economic concentrations. Understanding (largely through geophysical surveys) of the subsurface topography and stratigraphy will be critical to identifying trapping features and drill targets. Initial work will also include auger or push rod type mud sampling to prove lithium has concentrated in evaporite minerals and interstitial fluids within the playa sediments.

26.0 Recommendations A phased exploration program should be undertaken at Dixie Valley Project to test the property for a lithium brine or clay deposit. Follow on work will be contingent on the results obtained in the previous efforts. If sufficient encouraging results are not obtained at any point in the process, subsequent plans should be revised.

The first phase is building the geologic infrastructure through data compilation, construction of base maps and GIS databases. Geologic reconnaissance and geochemical analysis of surface rock, mud, and sinter samples will also be conducted during this phase. Additional test auger sampling to collect lake bed material below sand dunes and alluvial cover may also be part of the initial program. The budget for this phase, including geologic supervision and preparation of all reports, is $35,000.

The second step in phase one would be to determine the sub-surface structure and topography in order to identify drill targets. This would require a geophysical survey using gravity, seismic or magnetotelluric techniques. Systematic shovel, auger, or push drilling to collect mud and/or


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water samples and geochemical analysis of these samples will also be part of this program. The budget for this phase of the project, including permitting if needed, geologic supervision, reporting, and interpretation, is $200,000.

Phase 2 would be to drill the best targets identified in the first two phases. This would be the most costly, both for the drill holes themselves and for the expensive water analysis that is required for brine testing. The budget for this phase is $2,265,000, including drilling, assays, permits, and reporting. Phase 2 would likely be broken into two campaigns to allow for results from the first effort to guide the second program.

The total proposed budget is $2,500,000, exclusive of land holding costs. Results of each phase or campaign will be used to modify the subsequent steps to insure the most cost-effective use of the exploration funds.


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27.0 References

Blackwell, David D., Wisian, Kenneth W., Richards, Maria C., Leidig, Mark, Smith, Richard, McKenna, Jason, 2003, Final Report Geothermal Resource Analysis and Structure of Basin and Range Systems, Especially Dixie Valley Field, Nevada, prepared for the U. S. Department of Energy, under DOE Idaho Operations Office Grant DE-FG07-011D13886, Southern Methodist University Department of Geological Sciences website.

Blackwell, David D., Smith, Richard P., and Richards, Maria C., 2007, Exploration and Development at Dixie Valley, Nevada: Summary of DOE studies. Proceedings, Thirty Second Workshop on Geothermal Reservoir Engineering Stanford University, Stanford California, January 22-24, 2007.

Blackwell, David D., Smith, Richard P., and Richards, Maria C., 2014, Editors, Description, Synthesis, and Interpretation of the Thermal Regime, Geology, Geochemistry, and Geophysics of the Dixie Valley, Nevada Geothermal System, Southern Methodist University Geothermal Laboratory. http://www.smu.edu/~/media/Site/Dedman/Academics/Programs/Geothermal%20Lab/Documents/Publications/DixieValleySynthesis.ashx?la=en.

Bradley, Dwight, Munk, LeaAnn, Jochens, Hillary, Hynek, Scott, and LaBay, Keith, 2013, A Preliminary Deposit Model for Lithium Brines, USGS Open File Report 2013-1006.

Coolbaugh, Mark F., 2016, Preliminary Structural Model, Teels Marsh, Mineral County, Nevada; Report for Dajin Resources made available on their website www.dajin.ca/teels-marsh/

Hinkle, M. E., Briggs, P.H., Motooka, J.M., and Knight, R.J., 1995, Analytical Results for Soil Samples and Plots of Results of R-Mode Factor Analysis of Soil and Soil-gas Data: Dixie Valley Known Geothermal Resource Area, Northern Dixie Valley, Nevada, USGS Open File Report 95-485.

Hofstra, A. H., Todorov, T. I., Mercer, C. N., Adams, D. T., and Marsh, E. E., 2013, Silicate Melt Inclusion Evidence for Extreme Pre-eruptive Enrichment and Post-eruptive Depletion of Lithium in Silicic Volcanic Rocks of the Western United States: Implications for the Origin of Lithium-rich Brines, Economic Geology, v. 108, pp. 1691-1701.

Houston, J., Butcher, A., Ehren, P., Evans, K., and Godfrey, L., 2011, The evaluation of Brine Prospects and the Requirement for Modifications to Filing Standards, Economic Geology, v. 106, pp. 1225-1239.

Hulen, Jeffrey B., 2008, Geology and Conceptual Modeling of the Silver Peak Geothermal Prospect, Esmeralda County, Nevada, Technical Report for Sierra Geothermal Power Corporation, http://gdr.openei.org/files/268/Silver%20Peak%20Geology%20Map%20and%20Model%20(Hulen)%20Jul%202008.pdf.

http://www.dajin.ca/teels-marsh/


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Munk, LeeAnn, Hynek, Scott, Boutt, David, and Bradley, Dwight, 2015, Geology, Geochemistry, and Hydrology of Lithium Brines: in Penell, W.M. and Garside, L.J., 2015, NEW CONCEPTS AND DISCOVERIES, Geological Society of Nevada 2015 Symposium Volume, pp. 515 - 519.

Price, Jonathon G., Lechler, Paul J., Lear, Michael B., and Giles, Tim F., 2000, Possible Volcanic Sources of Lithium in Brines in Clayton Valley, Nevada, in Cluer, J.K., Price, J.G., Struhsacker, E.M., Hardyman, R.F., and Morris, C.L., Geology and Ore deposits 2000; The Great Basin and Beyond: Geological Society of Nevada 2000 Symposium Proceedings, pp. 241-248.

Papke, Keith G., 1976, Evaporites and Brines in Nevada Playas, Nevada Bureau of Mines and Geology Bulletin 87.

Spanjers, Raymond P., 2015, Inferred Resource Estimate for Lithium, Clayton Valley South Project, Clayton Valley, Esmeralda County, Nevada, 43-101 Technical Report for Pure Energy Minerals.

Ross, Donald C., 1961, Geology and Mineral Deposits of Mineral County, Nevada; Nevada Bureau of Mines and Geology Bulletin 58.

Willden, Ronald and Speed, Robert C., 1974, Geology and Mineral Deposits of Churchill County, Nevada, Nevada Bureau of Mines and Geology Bulletin 83.

Zampirro, D., 2004, Hydrology of Clayton Valley Brine Deposits, Esmeralda County, Nevada in Castor, S.B., Papke, K.G., and Meeuwig, R.O., eds., BETTING ON INDUSTRIAL MINERALS: PROCEEDINGS OF THE 39TH FORUM ON THE GEOLOGY OF INDUSTRIAL MINERALS, RENO-SPARKS, NEVADA, MAY 18-24; Nevada Bureau of Mines and Geology Special Publication 33, pp. 271 -280.


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Appendix 1. Claim Names and Serial Numbers

Claim Serial Num Mer Twn Rng Sec Quad Location Date Last Assmt DV 1 NMC1126898 21 0220N 0350E 014 NE 6/2/2016 2 0 1 7 DV 2 NMC1126899 21 0220N 0350E 014 NE 6/2/2016 2 0 1 7 DV 3 NMC1126900 21 0220N 0350E 014 NE 6/2/2016 2 0 1 7 DV 4 NMC1126901 21 0220N 0350E 014 NE 6/2/2016 2 0 1 7 DV 5 NMC1126902 21 0220N 0350E 014 NE 6/2/2016 2 0 1 7 DV 6 NMC1126903 21 0220N 0350E 014 NE 6/2/2016 2 0 1 7 DV 7 NMC1126904 21 0220N 0350E 014 NE 6/2/2016 2 0 1 7 DV 8 NMC1126905 21 0220N 0350E 014 NE 6/2/2016 2 0 1 7 DV 9 NMC1126906 21 0220N 0350E 014 SE 6/2/2016 2 0 1 7 DV 10 NMC1126907 21 0220N 0350E 014 SE 6/2/2016 2 0 1 7 DV 11 NMC1126908 21 0220N 0350E 014 SE 6/2/2016 2 0 1 7 DV 12 NMC1126909 21 0220N 0350E 014 SE 6/2/2016 2 0 1 7 DV 13 NMC1126805 21 0220N 0350E 012 SE 4/29/2016 2 0 1 7 DV 14 NMC1126806 21 0220N 0350E 012 SE 4/29/2016 2 0 1 7 DV 15 NMC1126807 21 0220N 0350E 012 SE 4/29/2016 2 0 1 7 DV 16 NMC1126808 21 0220N 0350E 012 SE 4/29/2016 2 0 1 7 DV 17 NMC1126809 21 0220N 0350E 013 NW 4/29/2016 2 0 1 7 DV 18 NMC1126810 21 0220N 0350E 013 NW 4/29/2016 2 0 1 7 DV 19 NMC1126811 21 0220N 0350E 013 NW 4/29/2016 2 0 1 7 DV 20 NMC1126812 21 0220N 0350E 013 NW 4/29/2016 2 0 1 7 DV 21 NMC1126813 21 0220N 0350E 013 NW 4/29/2016 2 0 1 7 DV 22 NMC1126814 21 0220N 0350E 013 NW 4/29/2016 2 0 1 7 DV 23 NMC1126815 21 0220N 0350E 013 NW 4/29/2016 2 0 1 7 DV 24 NMC1126816 21 0220N 0350E 013 NW 4/29/2016 2 0 1 7 DV 25 NMC1126817 21 0220N 0350E 013 SW 4/29/2016 2 0 1 7 DV 26 NMC1126818 21 0220N 0350E 013 SW 4/29/2016 2 0 1 7 DV 27 NMC1126819 21 0220N 0350E 013 SW 4/29/2016 2 0 1 7 DV 28 NMC1126820 21 0220N 0350E 013 SW 4/29/2016 2 0 1 7 DV 29 NMC1126821 21 0220N 0350E 013 SW 4/29/2016 2 0 1 7 DV 30 NMC1126822 21 0220N 0350E 013 SW 4/29/2016 2 0 1 7 DV 31 NMC1126823 21 0220N 0350E 013 SW 4/29/2016 2 0 1 7 DV 32 NMC1126824 21 0220N 0350E 013 SW 4/29/2016 2 0 1 7 DV 33 NMC1126910 21 0220N 0350E 014 SE 6/2/2016 2 0 1 7 DV 34 NMC1126911 21 0220N 0350E 014 SE 6/2/2016 2 0 1 7 DV 35 NMC1126912 21 0220N 0350E 014 SE 6/2/2016 2 0 1 7 DV 36 NMC1126913 21 0220N 0350E 014 NW 6/2/2016 2 0 1 7 DV 37 NMC1126914 21 0220N 0350E 014 NW 6/2/2016 2 0 1 7


46

Claim Serial Num Mer Twn Rng Sec Quad Location Date Last Assmt DV 38 NMC1126915 21 0220N 0350E 014 NW 6/2/2016 2 0 1 7 DV 39 NMC1126916 21 0220N 0350E 014 NW 6/2/2016 2 0 1 7 DV 40 NMC1126917 21 0220N 0350E 014 NW 6/2/2016 2 0 1 7 DV 41 NMC1126918 21 0220N 0350E 014 NW 6/2/2016 2 0 1 7 DV 42 NMC1126919 21 0220N 0350E 014 NW 6/2/2016 2 0 1 7 DV 43 NMC1126920 21 0220N 0350E 014 NW 6/2/2016 2 0 1 7 DV 44 NMC1126921 21 0220N 0350E 014 NW 6/2/2016 2 0 1 7 DV 45 NMC1126825 21 0220N 0350E 012 SE 4/29/2016 2 0 1 7 DV 46 NMC1126826 21 0220N 0350E 012 SE 4/29/2016 2 0 1 7 DV 47 NMC1126827 21 0220N 0350E 012 SE 4/29/2016 2 0 1 7 DV 48 NMC1126828 21 0220N 0350E 012 SE 4/29/2016 2 0 1 7 DV 49 NMC1126829 21 0220N 0350E 013 NE 4/29/2016 2 0 1 7 DV 50 NMC1126830 21 0220N 0350E 013 NE 4/29/2016 2 0 1 7 DV 51 NMC1126831 21 0220N 0350E 013 NE 4/29/2016 2 0 1 7 DV 52 NMC1126832 21 0220N 0350E 013 NE 4/29/2016 2 0 1 7 DV 53 NMC1126833 21 0220N 0350E 013 NE 4/29/2016 2 0 1 7 DV 54 NMC1126834 21 0220N 0350E 013 NE 4/29/2016 2 0 1 7 DV 55 NMC1126835 21 0220N 0350E 013 NE 4/29/2016 2 0 1 7 DV 56 NMC1126836 21 0220N 0350E 013 NE 4/29/2016 2 0 1 7 DV 57 NMC1126837 21 0220N 0350E 013 SE 4/29/2016 2 0 1 7 DV 58 NMC1126838 21 0220N 0350E 013 SE 4/29/2016 2 0 1 7 DV 59 NMC1126839 21 0220N 0350E 013 SE 4/29/2016 2 0 1 7 DV 60 NMC1126840 21 0220N 0350E 013 SE 4/29/2016 2 0 1 7 DV 61 NMC1126841 21 0220N 0350E 013 SE 4/29/2016 2 0 1 7 DV 62 NMC1126842 21 0220N 0350E 013 SE 4/29/2016 2 0 1 7 DV 63 NMC1126843 21 0220N 0350E 013 SE 4/29/2016 2 0 1 7 DV 64 NMC1126844 21 0220N 0350E 013 SE 4/29/2016 2 0 1 7 DV 65 NMC1126922 21 0220N 0350E 014 SE 6/2/2016 2 0 1 7 DV 66 NMC1126923 21 0220N 0350E 014 SW 6/2/2016 2 0 1 7 DV 67 NMC1126924 21 0220N 0350E 014 SW 6/2/2016 2 0 1 7 DV 68 NMC1126925 21 0220N 0350E 014 SW 6/2/2016 2 0 1 7 DV 69 NMC1126926 21 0220N 0350E 014 SW 6/2/2016 2 0 1 7 DV 70 NMC1126927 21 0220N 0350E 014 SW 6/2/2016 2 0 1 7 DV 71 NMC1126928 21 0220N 0350E 014 SW 6/2/2016 2 0 1 7 DV 72 NMC1126929 21 0220N 0350E 014 SW 6/2/2016 2 0 1 7 DV 73 NMC1126930 21 0220N 0350E 023 NW 6/2/2016 2 0 1 7 DV 74 NMC1126931 21 0220N 0350E 023 NW 6/2/2016 2 0 1 7 DV 75 NMC1126932 21 0220N 0350E 023 NW 6/2/2016 2 0 1 7 DV 76 NMC1126933 21 0220N 0350E 023 NW 6/2/2016 2 0 1 7 DV 77 NMC1126934 21 0220N 0350E 015 NE 6/2/2016 2 0 1 7 DV 78 NMC1126935 21 0220N 0350E 015 NE 6/2/2016 2 0 1 7 DV 79 NMC1126936 21 0220N 0350E 015 NE 6/2/2016 2 0 1 7


47

Claim Serial Num Mer Twn Rng Sec Quad Location Date Last Assmt DV 80 NMC1126937 21 0220N 0350E 015 NE 6/2/2016 2 0 1 7 DV 81 NMC1126938 21 0220N 0350E 015 NE 6/2/2016 2 0 1 7 DV 82 NMC1126939 21 0220N 0350E 015 NE 6/2/2016 2 0 1 7 DV 83 NMC1126940 21 0220N 0350E 015 NE 6/2/2016 2 0 1 7 DV 84 NMC1126941 21 0220N 0350E 015 NE 6/2/2016 2 0 1 7 DV 85 NMC1126942 21 0220N 0350E 015 SE 6/2/2016 2 0 1 7 DV 86 NMC1126943 21 0220N 0350E 015 SE 6/2/2016 2 0 1 7 DV 87 NMC1126845 21 0220N 0360E 007 NW 4/29/2016 2 0 1 7 DV 88 NMC1126846 21 0220N 0360E 007 SW 4/29/2016 2 0 1 7 DV 89 NMC1126847 21 0220N 0360E 007 NW 4/29/2016 2 0 1 7 DV 90 NMC1126848 21 0220N 0360E 007 SW 4/29/2016 2 0 1 7 DV 91 NMC1126849 21 0220N 0360E 007 SW 4/29/2016 2 0 1 7 DV 92 NMC1126850 21 0220N 0360E 007 SW 4/29/2016 2 0 1 7 DV 93 NMC1126851 21 0220N 0360E 007 SW 4/29/2016 2 0 1 7 DV 94 NMC1126852 21 0220N 0360E 007 SW 4/29/2016 2 0 1 7 DV 95 NMC1126853 21 0220N 0360E 007 SW 4/29/2016 2 0 1 7 DV 96 NMC1126854 21 0220N 0360E 007 SW 4/29/2016 2 0 1 7 DV 97 NMC1126944 21 0220N 0350E 015 SE 6/2/2016 2 0 1 7 DV 98 NMC1126945 21 0220N 0350E 015 SE 6/2/2016 2 0 1 7 DV 99 NMC1126946 21 0220N 0350E 015 SE 6/2/2016 2 0 1 7 DV 100 NMC1126947 21 0220N 0350E 015 SE 6/2/2016 2 0 1 7 DV 101 NMC1126948 21 0220N 0350E 015 SE 6/2/2016 2 0 1 7 DV 102 NMC1126949 21 0220N 0350E 015 SE 6/2/2016 2 0 1 7 DV 103 NMC1126950 21 0220N 0350E 022 NE 6/2/2016 2 0 1 7 DV 104 NMC1126951 21 0220N 0350E 022 NE 6/2/2016 2 0 1 7 DV 105 NMC1126952 21 0220N 0350E 022 NE 6/2/2016 2 0 1 7 DV 106 NMC1126953 21 0220N 0350E 022 NE 6/2/2016 2 0 1 7 DV 107 NMC1126954 21 0220N 0350E 015 NW 6/2/2016 2 0 1 7 DV 108 NMC1126955 21 0220N 0350E 015 NW 6/2/2016 2 0 1 7 DV 109 NMC1126956 21 0220N 0350E 015 NW 6/2/2016 2 0 1 7 DV 110 NMC1126957 21 0220N 0350E 015 NW 6/2/2016 2 0 1 7 DV 111 NMC1126958 21 0220N 0350E 015 NW 6/2/2016 2 0 1 7 DV 112 NMC1126959 21 0220N 0350E 015 NW 6/2/2016 2 0 1 7 DV 113 NMC1126960 21 0220N 0350E 015 NW 6/2/2016 2 0 1 7 DV 114 NMC1126961 21 0220N 0350E 015 NW 6/2/2016 2 0 1 7 DV 115 NMC1126855 21 0220N 0360E 007 NE 4/29/2016 2 0 1 7 DV 116 NMC1126856 21 0220N 0360E 007 NE 4/29/2016 2 0 1 7 DV 117 NMC1126857 21 0220N 0360E 007 NE 4/29/2016 2 0 1 7 DV 118 NMC1126858 21 0220N 0360E 007 NE 4/29/2016 2 0 1 7 DV 119 NMC1126859 21 0220N 0360E 007 NE 4/29/2016 2 0 1 7 DV 120 NMC1126860 21 0220N 0360E 007 NE 4/29/2016 2 0 1 7 DV 121 NMC1126861 21 0220N 0360E 007 SE 4/29/2016 2 0 1 7


48

Claim Serial Num Mer Twn Rng Sec Quad Location Date Last Assmt DV 122 NMC1126862 21 0220N 0360E 007 SE 4/29/2016 2 0 1 7 DV 123 NMC1126863 21 0220N 0360E 007 SE 4/29/2016 2 0 1 7 DV 124 NMC1126864 21 0220N 0360E 007 SE 4/29/2016 2 0 1 7 DV 125 NMC1126865 21 0220N 0360E 007 SE 4/29/2016 2 0 1 7 DV 126 NMC1126866 21 0220N 0360E 007 SE 4/29/2016 2 0 1 7 DV 127 NMC1126867 21 0220N 0360E 007 SE 4/29/2016 2 0 1 7 DV 128 NMC1126868 21 0220N 0360E 007 SE 4/29/2016 2 0 1 7 DV 129 NMC1126962 21 0220N 0350E 015 SW 6/2/2016 2 0 1 7 DV 130 NMC1126963 21 0220N 0350E 015 SW 6/2/2016 2 0 1 7 DV 131 NMC1126964 21 0220N 0350E 015 SW 6/2/2016 2 0 1 7 DV 132 NMC1126965 21 0220N 0350E 015 SW 6/2/2016 2 0 1 7 DV 133 NMC1126966 21 0220N 0350E 015 SW 6/2/2016 2 0 1 7 DV 134 NMC1126967 21 0220N 0350E 015 SW 6/2/2016 2 0 1 7 DV 135 NMC1126968 21 0220N 0350E 015 SW 6/2/2016 2 0 1 7 DV 136 NMC1126969 21 0220N 0350E 015 SW 6/2/2016 2 0 1 7 DV 137 NMC1126970 21 0220N 0350E 022 NW 6/2/2016 2 0 1 7 DV 138 NMC1126971 21 0220N 0350E 022 NW 6/2/2016 2 0 1 7 DV 139 NMC1126972 21 0220N 0350E 022 NW 6/2/2016 2 0 1 7 DV 140 NMC1126973 21 0220N 0350E 022 NW 6/2/2016 2 0 1 7 DV 142 NMC1126974 21 0220N 0350E 023 NE 6/2/2016 2 0 1 7 DV 142 NMC1126975 21 0220N 0350E 023 NE 6/2/2016 2 0 1 7 DV 143 NMC1126976 21 0220N 0350E 023 NE 6/2/2016 2 0 1 7 DV 144 NMC1126977 21 0220N 0350E 023 NE 6/2/2016 2 0 1 7 DV 145 NMC1126869 21 0220N 0360E 024 NW 4/29/2016 2 0 1 7 DV 146 NMC1126870 21 0220N 0360E 024 NW 4/29/2016 2 0 1 7 DV 147 NMC1126871 21 0220N 0360E 018 NW 4/29/2016 2 0 1 7 DV 148 NMC1126872 21 0220N 0360E 018 NW 4/29/2016 2 0 1 7 DV 149 NMC1126873 21 0220N 0360E 018 NW 4/29/2016 2 0 1 7 DVB 1 NMC1127950 21 0220N 0350E 010 NW 6/2/2016 2 0 1 7 DVB 2 NMC1127951 21 0220N 0350E 010 NW 6/2/2016 2 0 1 7 DVB 3 NMC1127952 21 0220N 0350E 010 NW 6/2/2016 2 0 1 7 DVB 4 NMC1127953 21 0220N 0350E 010 NW 6/2/2016 2 0 1 7 DVB 5 NMC1127954 21 0220N 0350E 010 NW 6/2/2016 2 0 1 7 DVB 6 NMC1127955 21 0220N 0350E 010 NW 6/2/2016 2 0 1 7 DVB 7 NMC1127956 21 0220N 0350E 010 NW 6/2/2016 2 0 1 7 DVB 8 NMC1127957 21 0220N 0350E 010 NW 6/2/2016 2 0 1 7 DVB 9 NMC1127958 21 0220N 0350E 010 SW 6/2/2016 2 0 1 7 DVB 10 NMC1127959 21 0220N 0350E 010 SW 6/2/2016 2 0 1 7 DVB 11 NMC1127960 21 0220N 0350E 010 SW 6/2/2016 2 0 1 7 DVB 12 NMC1127961 21 0220N 0350E 010 SW 6/2/2016 2 0 1 7 DVB 13 NMC1127962 21 0220N 0350E 010 SW 6/2/2016 2 0 1 7 DVB 14 NMC1127963 21 0220N 0350E 010 SW 6/2/2016 2 0 1 7


49

Claim Serial Num Mer Twn Rng Sec Quad Location Date Last Assmt DVB 15 NMC1127964 21 0220N 0350E 010 SW 6/2/2016 2 0 1 7 DVB 20 NMC1127969 21 0220N 0350E 010 NE 6/2/2016 2 0 1 7 DVB 22 NMC1127970 21 0220N 0350E 010 NE 6/2/2016 2 0 1 7 DVB 23 NMC1127971 21 0220N 0350E 010 NE 6/2/2016 2 0 1 7 DVB 23 NMC1127972 21 0220N 0350E 010 NE 6/2/2016 2 0 1 7 DVB 24 NMC1127973 21 0220N 0350E 010 NE 6/2/2016 2 0 1 7 DVB 25 NMC1127974 21 0220N 0350E 010 NE 6/2/2016 2 0 1 7 DVB 26 NMC1127975 21 0220N 0350E 010 SE 6/2/2016 2 0 1 7 DVB 27 NMC1127976 21 0220N 0350E 010 SE 6/2/2016 2 0 1 7 DVB 28 NMC1127977 21 0220N 0350E 010 SE 6/2/2016 2 0 1 7 DVB 29 NMC1127978 21 0220N 0350E 010 SE 6/2/2016 2 0 1 7 DVB 30 NMC1127979 21 0220N 0350E 010 SE 6/2/2016 2 0 1 7 DVB 31 NMC1127980 21 0220N 0350E 010 SE 6/2/2016 2 0 1 7 DVB 32 NMC1127981 21 0220N 0350E 010 SE 6/2/2016 2 0 1 7 DVB 33 NMC1127982 21 0220N 0350E 011 NW 6/2/2016 2 0 1 7 DVB 34 NMC1127983 21 0220N 0350E 011 NW 6/2/2016 2 0 1 7 DVB 35 NMC1127984 21 0220N 0350E 011 NW 6/2/2016 2 0 1 7 DVB 36 NMC1127985 21 0220N 0350E 011 NW 6/2/2016 2 0 1 7 DVB 37 NMC1127986 21 0220N 0350E 011 NW 6/2/2016 2 0 1 7 DVB 38 NMC1127987 21 0220N 0350E 011 NW 6/2/2016 2 0 1 7 DVB 39 NMC1127988 21 0220N 0350E 011 NW 6/2/2016 2 0 1 7 DVB 40 NMC1127989 21 0220N 0350E 011 NW 6/2/2016 2 0 1 7 DVB 41 NMC1127990 21 0220N 0350E 011 SW 6/2/2016 2 0 1 7 DVB 42 NMC1127991 21 0220N 0350E 011 SW 6/2/2016 2 0 1 7 DVB 43 NMC1127992 21 0220N 0350E 011 SW 6/2/2016 2 0 1 7 DVB 44 NMC1127993 21 0220N 0350E 011 SW 6/2/2016 2 0 1 7 DVB 45 NMC1127994 21 0220N 0350E 011 SW 6/2/2016 2 0 1 7 DVB 46 NMC1127995 21 0220N 0350E 011 SW 6/2/2016 2 0 1 7 DVB 47 NMC1127996 21 0220N 0350E 011 SW 6/2/2016 2 0 1 7 DVB 48 NMC1127997 21 0220N 0350E 011 SW 6/2/2016 2 0 1 7 DVB 49 NMC1128067 21 0230N 0350E 013 NW 6/2/2016 2 0 1 7 DVB 50 NMC1128068 21 0230N 0350E 013 SW 6/2/2016 2 0 1 7 DVB 51 NMC1128069 21 0230N 0350E 013 SW 6/2/2016 2 0 1 7 DVB 52 NMC1128070 21 0230N 0350E 013 SW 6/2/2016 2 0 1 7 DVB 53 NMC1128071 21 0230N 0350E 013 SW 6/2/2016 2 0 1 7 DVB 54 NMC1128072 21 0230N 0350E 024 NW 6/2/2016 2 0 1 7 DVB 55 NMC1128073 21 0230N 0350E 024 NW 6/2/2016 2 0 1 7 DVB 56 NMC1128074 21 0230N 0350E 024 NW 6/2/2016 2 0 1 7 DVB 57 NMC1128075 21 0230N 0350E 024 NW 6/2/2016 2 0 1 7 DVB 58 NMC1128076 21 0230N 0350E 024 SW 6/2/2016 2 0 1 7 DVB 59 NMC1128077 21 0230N 0350E 024 SW 6/2/2016 2 0 1 7 DVB 60 NMC1128078 21 0230N 0350E 024 SW 6/2/2016 2 0 1 7


50

Claim Serial Num Mer Twn Rng Sec Quad Location Date Last Assmt DVB 61 NMC1128079 21 0230N 0350E 024 SW 6/2/2016 2 0 1 7 DVB 62 NMC1128080 21 0230N 0350E 025 NW 6/2/2016 2 0 1 7 DVB 63 NMC1128081 21 0230N 0350E 025 NW 6/2/2016 2 0 1 7 DVB 64 NMC1128082 21 0230N 0350E 025 NW 6/2/2016 2 0 1 7 DVB 65 NMC1128083 21 0230N 0350E 013 NE 6/3/2016 2 0 1 7 DVB 66 NMC1128084 21 0230N 0350E 013 NE 6/3/2016 2 0 1 7 DVB 67 NMC1128085 21 0230N 0350E 013 SE 6/3/2016 2 0 1 7 DVB 68 NMC1128086 21 0230N 0350E 013 SE 6/3/2016 2 0 1 7 DVB 69 NMC1128087 21 0230N 0350E 013 SE 6/3/2016 2 0 1 7 DVB 70 NMC1128088 21 0230N 0350E 013 SE 6/3/2016 2 0 1 7 DVB 71 NMC1128089 21 0230N 0350E 013 SE 6/3/2016 2 0 1 7 DVB 72 NMC1128090 21 0230N 0350E 013 SE 6/3/2016 2 0 1 7 DVB 73 NMC1128091 21 0230N 0350E 013 SE 6/3/2016 2 0 1 7 DVB 74 NMC1128092 21 0230N 0350E 013 SE 6/3/2016 2 0 1 7 DVB 75 NMC1128093 21 0230N 0350E 024 NE 6/3/2016 2 0 1 7 DVB 76 NMC1128094 21 0230N 0350E 024 NE 6/3/2016 2 0 1 7 DVB 77 NMC1128095 21 0230N 0350E 024 NE 6/3/2016 2 0 1 7 DVB 78 NMC1128096 21 0230N 0350E 024 NE 6/3/2016 2 0 1 7 DVB 79 NMC1128097 21 0230N 0350E 024 NE 6/3/2016 2 0 1 7 DVB 80 NMC1128098 21 0230N 0350E 024 NE 6/3/2016 2 0 1 7 DVB 81 NMC1128099 21 0230N 0350E 024 NE 6/3/2016 2 0 1 7 DVB 82 NMC1128100 21 0230N 0350E 024 NE 6/3/2016 2 0 1 7 DVB 83 NMC1128101 21 0230N 0350E 024 SE 6/3/2016 2 0 1 7 DVB 84 NMC1128102 21 0230N 0350E 024 SE 6/3/2016 2 0 1 7 DVB 85 NMC1128103 21 0230N 0350E 024 SE 6/3/2016 2 0 1 7 DVB 86 NMC1128104 21 0230N 0350E 024 SE 6/3/2016 2 0 1 7 DVB 87 NMC1128105 21 0230N 0350E 024 SE 6/3/2016 2 0 1 7 DVB 88 NMC1128106 21 0230N 0350E 024 SE 6/3/2016 2 0 1 7 DVB 89 NMC1128107 21 0230N 0350E 024 SE 6/2/2016 2 0 1 7 DVB 90 NMC1128108 21 0230N 0350E 024 SE 6/2/2016 2 0 1 7 DVB 91 NMC1128109 21 0230N 0350E 025 NE 6/2/2016 2 0 1 7 DVB 92 NMC1128110 21 0230N 0350E 025 NE 6/2/2016 2 0 1 7 DVB 93 NMC1128111 21 0230N 0350E 025 NE 6/2/2016 2 0 1 7 DVB 94 NMC1128112 21 0230N 0350E 025 NE 6/2/2016 2 0 1 7 DVB 95 NMC1128113 21 0230N 0350E 025 NE 6/2/2016 2 0 1 7 DVB 96 NMC1128114 21 0230N 0350E 025 NE 6/2/2016 2 0 1 7 DVB 97 NMC1128115 21 0230N 0360E 018 NW 6/3/2016 2 0 1 7 DVB 98 NMC1128116 21 0230N 0360E 018 NW 6/3/2016 2 0 1 7 DVB 99 NMC1128117 21 0230N 0360E 018 SW 6/3/2016 2 0 1 7 DVB 100 NMC1128118 21 0230N 0360E 018 SW 6/3/2016 2 0 1 7 DVB 101 NMC1128119 21 0230N 0360E 018 SW 6/3/2016 2 0 1 7 DVB 102 NMC1128120 21 0230N 0360E 018 SW 6/3/2016 2 0 1 7


51

Claim Serial Num Mer Twn Rng Sec Quad Location Date Last Assmt DVB 103 NMC1128121 21 0230N 0360E 018 SW 6/3/2016 2 0 1 7 DVB 104 NMC1128122 21 0230N 0360E 018 SW 6/3/2016 2 0 1 7 DVB 105 NMC1128123 21 0230N 0360E 018 SW 6/3/2016 2 0 1 7 DVB 106 NMC1128124 21 0230N 0360E 018 SW 6/3/2016 2 0 1 7 DVB 107 NMC1128125 21 0230N 0360E 019 NW 6/3/2016 2 0 1 7 DVB 108 NMC1128126 21 0230N 0360E 019 NW 6/3/2016 2 0 1 7 DVB 109 NMC1128127 21 0230N 0360E 019 NW 6/3/2016 2 0 1 7 DVB 110 NMC1128128 21 0230N 0360E 019 NW 6/3/2016 2 0 1 7 DVB 111 NMC1128129 21 0230N 0360E 019 NW 6/3/2016 2 0 1 7 DVB 112 NMC1128130 21 0230N 0360E 019 NW 6/3/2016 2 0 1 7 DVB 113 NMC1128131 21 0230N 0360E 019 NW 6/3/2016 2 0 1 7 DVB 114 NMC1128132 21 0230N 0360E 019 NW 6/3/2016 2 0 1 7 DVB 115 NMC1128133 21 0230N 0360E 019 SW 6/3/2016 2 0 1 7 DVB 116 NMC1128134 21 0230N 0360E 019 SW 6/3/2016 2 0 1 7 DVB 117 NMC1128135 21 0230N 0360E 019 SW 6/3/2016 2 0 1 7 DVB 118 NMC1128136 21 0230N 0360E 019 SW 6/3/2016 2 0 1 7 DVB 119 NMC1128137 21 0230N 0360E 019 SW 6/3/2016 2 0 1 7 DVB 120 NMC1128138 21 0230N 0360E 019 SW 6/3/2016 2 0 1 7 DVB 121 NMC1128139 21 0230N 0360E 019 SW 6/3/2016 2 0 1 7 DVB 122 NMC1128140 21 0230N 0360E 019 SW 6/3/2016 2 0 1 7 DVB 123 NMC1128141 21 0230N 0360E 030 NW 6/3/2016 2 0 1 7 DVB 124 NMC1128142 21 0230N 0360E 030 NW 6/3/2016 2 0 1 7 DVB 125 NMC1128143 21 0230N 0360E 030 NW 6/3/2016 2 0 1 7 DVB 126 NMC1128144 21 0230N 0360E 030 NW 6/3/2016 2 0 1 7 DVB 127 NMC1128145 21 0230N 0360E 030 NW 6/3/2016 2 0 1 7 DVB 128 NMC1128146 21 0230N 0360E 030 NW 6/3/2016 2 0 1 7 DVB 129 NMC1128147 21 0230N 0360E 018 NE 6/3/2016 2 0 1 7 DVB 130 NMC1128148 21 0230N 0360E 018 NE 6/3/2016 2 0 1 7 DVB 131 NMC1128149 21 0230N 0360E 018 SE 6/3/2016 2 0 1 7 DVB 132 NMC1128150 21 0230N 0360E 018 SE 6/3/2016 2 0 1 7 DVB 133 NMC1128151 21 0230N 0360E 018 SE 6/3/2016 2 0 1 7 DVB 134 NMC1128152 21 0230N 0360E 018 SE 6/3/2016 2 0 1 7 DVB 135 NMC1128153 21 0230N 0360E 018 SE 6/3/2016 2 0 1 7 DVB 136 NMC1128154 21 0230N 0360E 018 SE 6/3/2016 2 0 1 7 DVB 137 NMC1128155 21 0230N 0360E 018 SE 6/3/2016 2 0 1 7 DVB 138 NMC1128156 21 0230N 0360E 018 SE 6/3/2016 2 0 1 7 DVB 139 NMC1128157 21 0230N 0360E 019 NE 6/3/2016 2 0 1 7 DVB 140 NMC1128158 21 0230N 0360E 019 NE 6/3/2016 2 0 1 7 DVB 141 NMC1128159 21 0230N 0360E 019 NE 6/3/2016 2 0 1 7 DVB 142 NMC1128160 21 0230N 0360E 019 NE 6/3/2016 2 0 1 7 DVB 143 NMC1128161 21 0230N 0360E 019 NE 6/3/2016 2 0 1 7 DVB 144 NMC1128162 21 0230N 0360E 019 NE 6/3/2016 2 0 1 7


52

Claim Serial Num Mer Twn Rng Sec Quad Location Date Last Assmt DVB 145 NMC1128163 21 0230N 0360E 019 NE 6/3/2016 2 0 1 7 DVB 146 NMC1128164 21 0230N 0360E 019 NE 6/3/2016 2 0 1 7 DVB 147 NMC1128165 21 0230N 0360E 019 SE 6/3/2016 2 0 1 7 DVB 148 NMC1128166 21 0230N 0360E 019 SE 6/3/2016 2 0 1 7 DVB 149 NMC1128167 21 0230N 0360E 019 SE 6/3/2016 2 0 1 7 DVB 150 NMC1128168 21 0230N 0360E 019 SE 6/3/2016 2 0 1 7 DVB 151 NMC1128169 21 0230N 0360E 019 SE 6/3/2016 2 0 1 7 DVB 152 NMC1128170 21 0230N 0360E 019 SE 6/3/2016 2 0 1 7 DVB 153 NMC1128171 21 0230N 0360E 019 SE 6/3/2016 2 0 1 7 DVB 154 NMC1128172 21 0230N 0360E 019 SE 6/3/2016 2 0 1 7 DVB 155 NMC1128173 21 0230N 0360E 030 NE 6/3/2016 2 0 1 7 DVB 156 NMC1128174 21 0230N 0360E 030 NE 6/3/2016 2 0 1 7 DVB 157 NMC1128175 21 0230N 0360E 030 NE 6/3/2016 2 0 1 7 DVB 158 NMC1128176 21 0230N 0360E 030 NE 6/3/2016 2 0 1 7 DVB 159 NMC1128177 21 0230N 0360E 030 NE 6/3/2016 2 0 1 7 DVB 16 NMC1127965 21 0220N 0350E 010 SW 6/2/2016 2 0 1 7 DVB 160 NMC1128178 21 0230N 0360E 030 NE 6/3/2016 2 0 1 7 DVB 17 NMC1127966 21 0220N 0350E 010 NE 6/2/2016 2 0 1 7 DVB 18 NMC1127967 21 0220N 0350E 010 NE 6/2/2016 2 0 1 7 DVB 19 NMC1127968 21 0220N 0350E 010 NE 6/2/2016 2 0 1 7 DVC 1 NMC1128179 21 0230N 0360E 007 NE 6/3/2016 2 0 1 7 DVC 2 NMC1128180 21 0230N 0360E 007 NE 6/3/2016 2 0 1 7 DVC 3 NMC1128181 21 0230N 0360E 007 NE 6/3/2016 2 0 1 7 DVC 4 NMC1128182 21 0230N 0360E 007 NE 6/3/2016 2 0 1 7 DVC 5 NMC1128183 21 0230N 0360E 007 NE 6/3/2016 2 0 1 7 DVC 6 NMC1128184 21 0230N 0360E 007 NE 6/3/2016 2 0 1 7 DVC 7 NMC1128185 21 0230N 0360E 007 NE 6/3/2016 2 0 1 7 DVC 8 NMC1128186 21 0230N 0360E 007 NE 6/3/2016 2 0 1 7 DVC 9 NMC1128187 21 0230N 0360E 007 SE 6/3/2016 2 0 1 7 DVC 10 NMC1128188 21 0230N 0360E 007 SE 6/3/2016 2 0 1 7 DVC 11 NMC1128189 21 0230N 0360E 007 SE 6/3/2016 2 0 1 7 DVC 12 NMC1128190 21 0230N 0360E 007 SE 6/3/2016 2 0 1 7 DVC 13 NMC1128191 21 0230N 0360E 007 SE 6/3/2016 2 0 1 7 DVC 14 NMC1128192 21 0230N 0360E 007 SE 6/3/2016 2 0 1 7 DVC 15 NMC1128193 21 0230N 0360E 007 SE 6/3/2016 2 0 1 7 DVC 16 NMC1128194 21 0230N 0360E 007 SE 6/3/2016 2 0 1 7 DVC 17 NMC1128195 21 0230N 0360E 018 NE 6/3/2016 2 0 1 7 DVC 18 NMC1128196 21 0230N 0360E 018 NE 6/3/2016 2 0 1 7 DVC 19 NMC1128197 21 0230N 0360E 018 NE 6/3/2016 2 0 1 7 DVC 20 NMC1128198 21 0230N 0360E 018 NE 6/3/2016 2 0 1 7 DVC 21 NMC1128199 21 0230N 0360E 018 NE 6/3/2016 2 0 1 7 DVC 22 NMC1128200 21 0230N 0360E 018 NE 6/3/2016 2 0 1 7


53

Claim Serial Num Mer Twn Rng Sec Quad Location Date Last Assmt DVC 23 NMC1128201 21 0230N 0360E 008 NW 6/3/2016 2 0 1 7 DVC 24 NMC1128202 21 0230N 0360E 008 NW 6/3/2016 2 0 1 7 DVC 25 NMC1128203 21 0230N 0360E 008 NW 6/3/2016 2 0 1 7 DVC 26 NMC1128204 21 0230N 0360E 008 NW 6/3/2016 2 0 1 7 DVC 27 NMC1128205 21 0230N 0360E 008 NW 6/3/2016 2 0 1 7 DVC 28 NMC1128206 21 0230N 0360E 008 NW 6/3/2016 2 0 1 7 DVC 29 NMC1128207 21 0230N 0360E 008 NW 6/3/2016 2 0 1 7 DVC 30 NMC1128208 21 0230N 0360E 008 NW 6/3/2016 2 0 1 7 DVC 31 NMC1128209 21 0230N 0360E 008 NW 6/3/2016 2 0 1 7 DVC 32 NMC1128210 21 0230N 0360E 008 SW 6/3/2016 2 0 1 7 DVC 33 NMC1128211 21 0230N 0360E 008 SW 6/3/2016 2 0 1 7 DVC 34 NMC1128212 21 0230N 0360E 008 SW 6/3/2016 2 0 1 7 DVC 35 NMC1128213 21 0230N 0360E 008 SW 6/3/2016 2 0 1 7 DVC 36 NMC1128214 21 0230N 0360E 008 SW 6/3/2016 2 0 1 7 DVC 37 NMC1128215 21 0230N 0360E 008 SW 6/3/2016 2 0 1 7 DVC 38 NMC1128216 21 0230N 0360E 008 SW 6/3/2016 2 0 1 7 DVC 39 NMC1128217 21 0230N 0360E 017 NW 6/3/2016 2 0 1 7 DVC 40 NMC1128218 21 0230N 0360E 017 NW 6/3/2016 2 0 1 7 DVC 41 NMC1128219 21 0230N 0360E 017 NW 6/3/2016 2 0 1 7 DVC 42 NMC1128220 21 0230N 0360E 017 NW 6/3/2016 2 0 1 7 DVC 43 NMC1128221 21 0230N 0360E 017 NW 6/3/2016 2 0 1 7 DVC 44 NMC1128222 21 0230N 0360E 017 NW 6/3/2016 2 0 1 7 DVC 45 NMC1128223 21 0230N 0360E 008 NE 6/4/2016 2 0 1 7 DVC 46 NMC1128224 21 0230N 0360E 008 NE 6/4/2016 2 0 1 7 DVC 47 NMC1128225 21 0230N 0360E 008 NE 6/4/2016 2 0 1 7 DVC 48 NMC1128226 21 0230N 0360E 008 NE 6/4/2016 2 0 1 7 DVC 49 NMC1128227 21 0230N 0360E 008 NE 6/4/2016 2 0 1 7 DVC 50 NMC1128228 21 0230N 0360E 008 NE 6/4/2016 2 0 1 7 DVC 51 NMC1128229 21 0230N 0360E 008 NE 6/4/2016 2 0 1 7 DVC 52 NMC1128230 21 0230N 0360E 008 NE 6/4/2016 2 0 1 7 DVC 53 NMC1128231 21 0230N 0360E 008 SE 6/4/2016 2 0 1 7 DVC 54 NMC1128232 21 0230N 0360E 008 SE 6/4/2016 2 0 1 7 DVC 55 NMC1128233 21 0230N 0360E 008 SE 6/4/2016 2 0 1 7 DVC 56 NMC1128234 21 0230N 0360E 008 SE 6/4/2016 2 0 1 7 DVC 57 NMC1128235 21 0230N 0360E 008 SE 6/4/2016 2 0 1 7 DVC 58 NMC1128236 21 0230N 0360E 008 SE 6/4/2016 2 0 1 7 DVC 59 NMC1128237 21 0230N 0360E 008 SE 6/4/2016 2 0 1 7 DVC 60 NMC1128238 21 0230N 0360E 008 SE 6/4/2016 2 0 1 7 DVC 61 NMC1128239 21 0230N 0360E 017 NE 6/4/2016 2 0 1 7 DVC 62 NMC1128240 21 0230N 0360E 017 NE 6/4/2016 2 0 1 7 DVC 63 NMC1128241 21 0230N 0360E 017 NE 6/4/2016 2 0 1 7 DVC 64 NMC1128242 21 0230N 0360E 017 NE 6/4/2016 2 0 1 7


54

Claim Serial Num Mer Twn Rng Sec Quad Location Date Last Assmt DVC 65 NMC1128243 21 0230N 0360E 017 NE 6/4/2016 2 0 1 7 DVC 66 NMC1128244 21 0230N 0360E 017 NE 6/4/2016 2 0 1 7 DVC 67 NMC1128245 21 0230N 0360E 009 NW 6/4/2016 2 0 1 7 DVC 68 NMC1128246 21 0230N 0360E 009 NW 6/4/2016 2 0 1 7 DVC 69 NMC1128247 21 0230N 0360E 009 NW 6/4/2016 2 0 1 7 DVC 70 NMC1128248 21 0230N 0360E 009 NW 6/4/2016 2 0 1 7 DVC 71 NMC1128249 21 0230N 0360E 009 NW 6/4/2016 2 0 1 7 DVC 72 NMC1128250 21 0230N 0360E 009 NW 6/4/2016 2 0 1 7 DVC 73 NMC1128251 21 0230N 0360E 009 NW 6/4/2016 2 0 1 7 DVC 74 NMC1128252 21 0230N 0360E 009 NW 6/4/2016 2 0 1 7 DVC 75 NMC1128253 21 0230N 0360E 009 SW 6/4/2016 2 0 1 7 DVC 76 NMC1128254 21 0230N 0360E 009 SW 6/4/2016 2 0 1 7 DVC 77 NMC1128255 21 0230N 0360E 009 SW 6/4/2016 2 0 1 7 DVC 78 NMC1128256 21 0230N 0360E 009 SW 6/4/2016 2 0 1 7 DVC 79 NMC1128257 21 0230N 0360E 009 SW 6/4/2016 2 0 1 7 DVC 80 NMC1128258 21 0230N 0360E 009 SW 6/4/2016 2 0 1 7 DVC 81 NMC1128259 21 0230N 0360E 009 SW 6/4/2016 2 0 1 7 DVC 82 NMC1128260 21 0230N 0360E 009 SW 6/4/2016 2 0 1 7 DVC 83 NMC1128261 21 0230N 0360E 016 NW 6/4/2016 2 0 1 7 DVC 84 NMC1128262 21 0230N 0360E 016 NW 6/4/2016 2 0 1 7 DVC 85 NMC1128263 21 0230N 0360E 016 NW 6/4/2016 2 0 1 7 DVC 86 NMC1128264 21 0230N 0360E 016 NW 6/4/2016 2 0 1 7 DVC 87 NMC1128265 21 0230N 0360E 016 NW 6/4/2016 2 0 1 7 DVC 88 NMC1128266 21 0230N 0360E 016 NW 6/4/2016 2 0 1 7 DVC 89 NMC1128267 21 0230N 0360E 009 NE 6/4/2016 2 0 1 7 DVC 90 NMC1128268 21 0230N 0360E 009 NE 6/4/2016 2 0 1 7 DVC 91 NMC1128269 21 0230N 0360E 009 NE 6/4/2016 2 0 1 7 DVC 92 NMC1128270 21 0230N 0360E 009 NE 6/4/2016 2 0 1 7 DVC 93 NMC1128271 21 0230N 0360E 009 SE 6/4/2016 2 0 1 7 DVC 94 NMC1128272 21 0230N 0360E 009 SE 6/4/2016 2 0 1 7 DVC 95 NMC1128273 21 0230N 0360E 009 SE 6/4/2016 2 0 1 7 DVC 96 NMC1128274 21 0230N 0360E 009 SE 6/4/2016 2 0 1 7 DVC 97 NMC1128275 21 0230N 0360E 016 NE 6/4/2016 2 0 1 7 DVC 98 NMC1128276 21 0230N 0360E 016 NE 6/4/2016 2 0 1 7 DVC 99 NMC1128277 21 0230N 0360E 016 NE 6/4/2016 2 0 1 7 DVD 1 NMC1128343 21 0220N 0350E 011 NE 6/2/2016 2 0 1 7 DVD 2 NMC1128344 21 0220N 0350E 011 NE 6/2/2016 2 0 1 7 DVD 4 NMC1128346 21 0220N 0350E 011 NE 6/2/2016 2 0 1 7 DVD 5 NMC1128347 21 0220N 0350E 011 NE 6/2/2016 2 0 1 7 DVD 6 NMC1128348 21 0220N 0350E 011 NE 6/2/2016 2 0 1 7 DVD 7 NMC1128349 21 0220N 0350E 011 NE 6/2/2016 2 0 1 7 DVD 8 NMC1128350 21 0220N 0350E 011 NE 6/2/2016 2 0 1 7


55

Claim Serial Num Mer Twn Rng Sec Quad Location Date Last Assmt DVD 9 NMC1128351 21 0220N 0350E 011 SE 6/2/2016 2 0 1 7 DVD 10 NMC1128352 21 0220N 0350E 011 SE 6/2/2016 2 0 1 7 DVD 11 NMC1128353 21 0220N 0350E 011 SE 6/2/2016 2 0 1 7 DVD 12 NMC1128354 21 0220N 0350E 011 SE 6/2/2016 2 0 1 7 DVD 13 NMC1128355 21 0220N 0350E 011 SE 6/2/2016 2 0 1 7 DVD 14 NMC1128356 21 0220N 0350E 011 SE 6/2/2016 2 0 1 7 DVD 15 NMC1128357 21 0220N 0350E 011 SE 6/2/2016 2 0 1 7 DVD 16 NMC1128358 21 0220N 0350E 011 SE 6/2/2016 2 0 1 7 DVD 17 NMC1128278 21 0230N 0350E 025 NW 6/2/2016 2 0 1 7 DVD 18 NMC1128279 21 0230N 0350E 025 NW 6/2/2016 2 0 1 7 DVD 19 NMC1128280 21 0230N 0350E 025 SW 6/2/2016 2 0 1 7 DVD 20 NMC1128281 21 0230N 0350E 025 SW 6/2/2016 2 0 1 7 DVD 21 NMC1128282 21 0230N 0350E 025 SW 6/2/2016 2 0 1 7 DVD 22 NMC1128283 21 0230N 0350E 036 NW 6/2/2016 2 0 1 7 DVD 23 NMC1128284 21 0230N 0350E 036 NW 6/2/2016 2 0 1 7 DVD 24 NMC1128285 21 0230N 0350E 036 NW 6/2/2016 2 0 1 7 DVD 25 NMC1128286 21 0230N 0350E 036 NW 6/2/2016 2 0 1 7 DVD 26 NMC1128287 21 0230N 0350E 036 SW 6/2/2016 2 0 1 7 DVD 27 NMC1128288 21 0230N 0350E 036 SW 6/2/2016 2 0 1 7 DVD 28 NMC1128289 21 0230N 0350E 036 SW 6/2/2016 2 0 1 7 DVD 29 NMC1128290 21 0230N 0350E 036 SW 6/2/2016 2 0 1 7 DVD 3 NMC1128345 21 0220N 0350E 011 NE 6/2/2016 2 0 1 7 DVD 30 NMC1128359 21 0220N 0350E 001 NW 6/2/2016 2 0 1 7 DVD 31 NMC1128360 21 0220N 0350E 001 NW 6/2/2016 2 0 1 7 DVD 32 NMC1128361 21 0220N 0350E 001 NW 6/2/2016 2 0 1 7 DVD 33 NMC1128362 21 0220N 0350E 001 NW 6/2/2016 2 0 1 7 DVD 34 NMC1128363 21 0220N 0350E 001 SW 6/2/2016 2 0 1 7 DVD 35 NMC1128364 21 0220N 0350E 001 SW 6/2/2016 2 0 1 7 DVD 36 NMC1128365 21 0220N 0350E 001 SW 6/2/2016 2 0 1 7 DVD 37 NMC1128366 21 0220N 0350E 001 SW 6/2/2016 2 0 1 7 DVD 38 NMC1128367 21 0220N 0350E 012 NW 6/2/2016 2 0 1 7 DVD 39 NMC1128368 21 0220N 0350E 012 NW 6/2/2016 2 0 1 7 DVD 40 NMC1128369 21 0220N 0350E 012 NW 6/2/2016 2 0 1 7 DVD 41 NMC1128370 21 0220N 0350E 012 NW 6/2/2016 2 0 1 7 DVD 42 NMC1128371 21 0220N 0350E 012 NW 6/2/2016 2 0 1 7 DVD 43 NMC1128372 21 0220N 0350E 012 NW 6/2/2016 2 0 1 7 DVD 44 NMC1128373 21 0220N 0350E 012 NW 6/2/2016 2 0 1 7 DVD 45 NMC1128374 21 0220N 0350E 012 NW 6/2/2016 2 0 1 7 DVD 46 NMC1128375 21 0220N 0350E 012 SW 6/2/2016 2 0 1 7 DVD 47 NMC1128376 21 0220N 0350E 012 SW 6/2/2016 2 0 1 7 DVD 48 NMC1128377 21 0220N 0350E 012 SW 6/2/2016 2 0 1 7 DVD 49 NMC1128378 21 0220N 0350E 012 SW 6/2/2016 2 0 1 7


56

Claim Serial Num Mer Twn Rng Sec Quad Location Date Last Assmt DVD 50 NMC1128291 21 0230N 0350E 025 NE 6/2/2016 2 0 1 7 DVD 51 NMC1128292 21 0230N 0350E 025 NE 6/2/2016 2 0 1 7 DVD 52 NMC1128293 21 0230N 0350E 025 SE 6/2/2016 2 0 1 7 DVD 53 NMC1128294 21 0230N 0350E 025 SE 6/2/2016 2 0 1 7 DVD 54 NMC1128295 21 0230N 0350E 025 SE 6/2/2016 2 0 1 7 DVD 55 NMC1128296 21 0230N 0350E 025 SE 6/2/2016 2 0 1 7 DVD 56 NMC1128297 21 0230N 0350E 025 SE 6/2/2016 2 0 1 7 DVD 57 NMC1128298 21 0230N 0350E 025 SE 6/2/2016 2 0 1 7 DVD 58 NMC1128299 21 0230N 0350E 025 SE 6/2/2016 2 0 1 7 DVD 59 NMC1128300 21 0230N 0350E 025 SE 6/2/2016 2 0 1 7 DVD 60 NMC1128301 21 0230N 0350E 036 NE 6/2/2016 2 0 1 7 DVD 61 NMC1128302 21 0230N 0350E 036 NE 6/2/2016 2 0 1 7 DVD 62 NMC1128303 21 0230N 0350E 036 NE 6/2/2016 2 0 1 7 DVD 63 NMC1128304 21 0230N 0350E 036 NE 6/2/2016 2 0 1 7 DVD 64 NMC1128305 21 0230N 0350E 036 NE 6/2/2016 2 0 1 7 DVD 65 NMC1128306 21 0230N 0350E 036 NE 6/2/2016 2 0 1 7 DVD 66 NMC1128307 21 0230N 0350E 036 NE 6/2/2016 2 0 1 7 DVD 67 NMC1128308 21 0230N 0350E 036 NE 6/2/2016 2 0 1 7 DVD 68 NMC1128309 21 0230N 0350E 036 SE 6/2/2016 2 0 1 7 DVD 69 NMC1128310 21 0230N 0350E 036 SE 6/2/2016 2 0 1 7 DVD 70 NMC1128311 21 0230N 0350E 036 SE 6/2/2016 2 0 1 7 DVD 71 NMC1128312 21 0230N 0350E 036 SE 6/2/2016 2 0 1 7 DVD 72 NMC1128313 21 0230N 0350E 036 SE 6/2/2016 2 0 1 7 DVD 73 NMC1128314 21 0230N 0350E 036 SE 6/2/2016 2 0 1 7 DVD 74 NMC1128315 21 0230N 0350E 036 SE 6/2/2016 2 0 1 7 DVD 75 NMC1128316 21 0230N 0350E 036 SE 6/2/2016 2 0 1 7 DVD 76 NMC1128379 21 0220N 0350E 001 NE 6/2/2016 2 0 1 7 DVD 77 NMC1128380 21 0220N 0350E 001 NE 6/2/2016 2 0 1 7 DVD 78 NMC1128381 21 0220N 0350E 001 NE 6/2/2016 2 0 1 7 DVD 79 NMC1128382 21 0220N 0350E 001 NE 6/2/2016 2 0 1 7 DVD 80 NMC1128383 21 0220N 0350E 001 NE 6/2/2016 2 0 1 7 DVD 81 NMC1128384 21 0220N 0350E 001 NE 6/2/2016 2 0 1 7 DVD 82 NMC1128385 21 0220N 0350E 001 NE 6/2/2016 2 0 1 7 DVD 83 NMC1128386 21 0220N 0350E 001 NE 6/2/2016 2 0 1 7 DVD 84 NMC1128387 21 0220N 0350E 001 SE 6/2/2016 2 0 1 7 DVD 85 NMC1128388 21 0220N 0350E 001 SE 6/2/2016 2 0 1 7 DVD 86 NMC1128389 21 0220N 0350E 001 SE 6/2/2016 2 0 1 7 DVD 87 NMC1128390 21 0220N 0350E 001 SE 6/2/2016 2 0 1 7 DVD 88 NMC1128391 21 0220N 0350E 001 SE 6/2/2016 2 0 1 7 DVD 89 NMC1128392 21 0220N 0350E 001 SE 6/2/2016 2 0 1 7 DVD 90 NMC1128393 21 0220N 0350E 001 SE 6/2/2016 2 0 1 7 DVD 91 NMC1128394 21 0220N 0350E 001 SE 6/2/2016 2 0 1 7


57

Claim Serial Num Mer Twn Rng Sec Quad Location Date Last Assmt DVD 92 NMC1128395 21 0220N 0350E 012 NE 6/2/2016 2 0 1 7 DVD 93 NMC1128396 21 0220N 0350E 012 NE 6/2/2016 2 0 1 7 DVD 94 NMC1128397 21 0220N 0350E 012 NE 6/2/2016 2 0 1 7 DVD 95 NMC1128398 21 0220N 0350E 012 NE 6/2/2016 2 0 1 7 DVD 96 NMC1128399 21 0220N 0350E 012 NE 6/2/2016 2 0 1 7 DVD 97 NMC1128400 21 0220N 0350E 012 NE 6/2/2016 2 0 1 7 DVD 98 NMC1128401 21 0220N 0350E 012 NE 6/2/2016 2 0 1 7 DVD 99 NMC1128402 21 0220N 0350E 012 NE 6/2/2016 2 0 1 7 DVD 100 NMC1128403 21 0220N 0350E 012 SE 6/2/2016 2 0 1 7 DVD 101 NMC1128404 21 0220N 0350E 012 SE 6/2/2016 2 0 1 7 DVD 102 NMC1128405 21 0220N 0350E 012 SE 6/2/2016 2 0 1 7 DVD 103 NMC1128406 21 0220N 0350E 012 SE 6/2/2016 2 0 1 7 DVD 104 NMC1128317 21 0230N 0360E 030 NW 6/3/2016 2 0 1 7 DVD 105 NMC1128318 21 0230N 0360E 030 NW 6/3/2016 2 0 1 7 DVD 106 NMC1128319 21 0230N 0360E 030 SW 6/3/2016 2 0 1 7 DVD 107 NMC1128320 21 0230N 0360E 030 SW 6/3/2016 2 0 1 7 DVD 108 NMC1128321 21 0230N 0360E 030 SW 6/3/2016 2 0 1 7 DVD 109 NMC1128322 21 0230N 0360E 030 SW 6/3/2016 2 0 1 7 DVD 110 NMC1128323 21 0230N 0360E 030 SW 6/3/2016 2 0 1 7 DVD 111 NMC1128324 21 0230N 0360E 030 SW 6/3/2016 2 0 1 7 DVD 112 NMC1128325 21 0230N 0360E 030 SW 6/3/2016 2 0 1 7 DVD 113 NMC1128326 21 0230N 0360E 030 SW 6/3/2016 2 0 1 7 DVD 114 NMC1128327 21 0230N 0360E 031 NW 6/3/2016 2 0 1 7 DVD 115 NMC1128328 21 0230N 0360E 031 NW 6/3/2016 2 0 1 7 DVD 116 NMC1128329 21 0230N 0360E 031 NW 6/3/2016 2 0 1 7 DVD 117 NMC1128330 21 0230N 0360E 031 NW 6/3/2016 2 0 1 7 DVD 118 NMC1128331 21 0230N 0360E 031 NW 6/3/2016 2 0 1 7 DVD 119 NMC1128332 21 0230N 0360E 031 NW 6/3/2016 2 0 1 7 DVD 120 NMC1128333 21 0230N 0360E 031 NW 6/3/2016 2 0 1 7 DVD 121 NMC1128334 21 0230N 0360E 031 NW 6/3/2016 2 0 1 7 DVD 122 NMC1128335 21 0230N 0360E 031 SW 6/3/2016 2 0 1 7 DVD 123 NMC1128336 21 0230N 0360E 031 SW 6/3/2016 2 0 1 7 DVD 124 NMC1128337 21 0230N 0360E 031 SW 6/3/2016 2 0 1 7 DVD 125 NMC1128338 21 0230N 0360E 031 SW 6/3/2016 2 0 1 7 DVD 126 NMC1128339 21 0230N 0360E 031 SW 6/3/2016 2 0 1 7 DVD 127 NMC1128340 21 0230N 0360E 031 SW 6/3/2016 2 0 1 7 DVD 128 NMC1128341 21 0230N 0360E 031 SW 6/3/2016 2 0 1 7 DVD 129 NMC1128342 21 0230N 0360E 031 SW 6/3/2016 2 0 1 7 DVD 130 NMC1128407 21 0220N 0360E 006 NE 6/3/2016 2 0 1 7 DVD 131 NMC1128408 21 0220N 0360E 006 NW 6/3/2016 2 0 1 7 DVD 132 NMC1128409 21 0220N 0360E 006 NE 6/3/2016 2 0 1 7 DVD 133 NMC1128410 21 0220N 0360E 006 NW 6/3/2016 2 0 1 7


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Claim Serial Num Mer Twn Rng Sec Quad Location Date Last Assmt DVD 134 NMC1128411 21 0220N 0360E 006 NE 6/3/2016 2 0 1 7 DVD 135 NMC1128412 21 0220N 0360E 006 NW 6/3/2016 2 0 1 7 DVD 136 NMC1128413 21 0220N 0360E 006 NE 6/3/2016 2 0 1 7 DVD 137 NMC1128414 21 0220N 0360E 006 NW 6/3/2016 2 0 1 7 DVD 138 NMC1128415 21 0220N 0360E 006 NW 6/3/2016 2 0 1 7 DVD 139 NMC1128416 21 0220N 0360E 006 SW 6/3/2016 2 0 1 7 DVD 140 NMC1128417 21 0220N 0360E 006 NW 6/3/2016 2 0 1 7 DVD 141 NMC1128418 21 0220N 0360E 006 SW 6/3/2016 2 0 1 7 DVD 142 NMC1128419 21 0220N 0360E 006 NW 6/3/2016 2 0 1 7 DVD 143 NMC1128420 21 0220N 0360E 006 SW 6/3/2016 2 0 1 7 DVD 144 NMC1128421 21 0220N 0360E 006 NW 6/3/2016 2 0 1 7 DVD 145 NMC1128422 21 0220N 0360E 006 SW 6/3/2016 2 0 1 7 DVD 146 NMC1128423 21 0220N 0360E 007 NW 6/3/2016 2 0 1 7 DVD 147 NMC1128424 21 0220N 0360E 007 NW 6/3/2016 2 0 1 7 DVD 148 NMC1128425 21 0220N 0360E 007 NW 6/3/2016 2 0 1 7 DVD 149 NMC1128426 21 0220N 0360E 007 NW 6/3/2016 2 0 1 7 DVD 150 NMC1128427 21 0220N 0360E 007 NW 6/3/2016 2 0 1 7 DVD 151 NMC1128428 21 0220N 0360E 007 NW 6/3/2016 2 0 1 7