map attachmentsBlueskin Energy Wind Cluster

Porteous Hill

Landscape AssessmentLucas Associates landscape architects

2015print maps A4 portrait double-sided, bind on left

Blueskin Energy Wind Cluster | Porteous Hill landscape assessment

page 2location

Blueskin Bay

Porteous Hillthe site

north

Blueskin Energy Wind Cluster | Porteous Hill landscape assessment

page 3location

Blueskin Bay

Evansdale

Doctors Point

Hammond Hill

Kilmog Hill

Porteous Hillthe site

The information depicted in this map has been derived from numerous sources. It may not be complete, correct or up to date. This map is licensed by Landcare Research on an "as is" and "as available" basis and without any warranty of any kind, either express or implied. Landcare Research shall not be liable on any legal basis (including without limitation negligence) and expressly excludes all liability for loss or damage howsoever and whenever caused to a user of this map.

© Landcare Research NZ Limited 2014. Creative Commons Attribution 3.0 NZ License.

© Basemap data sourced from LINZ NZTopo Database. Crown Copyright Reserved.

4km3210

Scale: 1:100,000

Printed: 13:40:32 PM Thu, 18 Jun 2015

The information depicted in this map has been derived from numerous sources. It may not be complete, correct or up to date. This map is licensed by Landcare Research on an "as is" and "as available" basis and without any warranty of any kind, either express or implied. Landcare Research shall not be liable on any legal basis (including without limitation negligence) and expressly excludes all liability for loss or damage howsoever and whenever caused to a user of this map.

© Landcare Research NZ Limited 2014. Creative Commons Attribution 3.0 NZ License.

© Basemap data sourced from LINZ NZTopo Database. Crown Copyright Reserved.

4km3210

Scale: 1:100,000

Printed: 13:40:32 PM Thu, 18 Jun 2015

source: Landcare Research, Our Environment website

north

Heyward Point

Potato Point

Ōmimi

Guilds Hill

Brinns Point

Mopanui

Blueskin Energy Wind Cluster | Porteous Hill landscape assessment

page 4

coastal landscape preservation area

Porteous Hillthe siteCoast Road

Rail

SH1 Waitati-Waikouaiti Road

Coastal LandscapePreservation Area(CLPA)

source: Topo 50, CLPA - Dunedin District Plan

Blueskin Energy Wind Cluster | Porteous Hill landscape assessment

page 5

1

2

3

site location

source: Google Earth, aerial dated 2013

north

Porteous Hillthe site

CLPA

Blueskin Energy Wind Cluster | Porteous Hill landscape assessment

page 6

north

source: Google Earth, aerial dated 2013

the site withindicative turbine locations

1

2

3

site location

north

source: Google Earth, aerial dated 2013

Porteous Hillthe site

2 3 1

Blueskin Energy Wind Cluster | Porteous Hill landscape assessment

page 7geology

source: W.N. Benson Geological Map of Dunedin District

Porteous Hillthe site

Blueskin Energy Wind Cluster | Porteous Hill landscape assessment

page 8

Porteous28 September 2014Date Printed:

This map is a user generated static output from an Internet mapping site andis for reference only. Data layers that appear on this map may or may not be

accurate, current, or otherwise reliable.

THIS MAP IS NOT TO BE USED FOR NAVIGATION

Kilometers0.50

10,000SCALE 1:

Projection: NZGD_2000_New_Zealand_Transverse_Mercator

0.5

Legend

© CNES 2004-2010 / Spot Image

© GeographxCrown Copyright Reserved

Porteous

This map is a user generated static output from an Internet mapping site andis for reference only. Data layers that appear on this map may or may not be

accurate, current, or otherwise reliable.

THIS MAP IS NOT TO BE USED FOR NAVIGATION

Kilometers1.0

20,000

NZGD_2000_New_Zealand_Transverse_Mercator

Legend

© CNES 2004-2010 / Spot Image

© GeographxCrown Copyright Reserved

Landform Components

1. Rolling to easy rolling loess mantled slopes developed on olivine basalt (Porteous soils).

2. Strongly rolling to moderately steep colluvial slopes developed on dolerite and basaltic breccia.

3. Complex strongly rolling to moderately steep slopes with rippled or hummocky surfaces of slump earth�ow topography formed on Burnside and Abbotsford mudstones.

4. Steep to moderately steep basaltic hard rock slopes (Hammond Hill).

5. Isolated strongly rolling to steep basaltic hillocks.6. Smooth strongly rolling to rolling loess mantled

slopes developed on basalt.7. Complex rolling to strongly rolling slopes of

earth�ow topography formed largely on Burnside Formation mudstone.

8. Smooth rolling slopes on weathered basalt.9. Broken and slumped steep to moderately steep

slopes with steep to very steep basal sea cli�s cut into sedimentary strata.

10. Steep to moderately steep side slopes on basalt and basaltic colluvium.

11. Strongly rolling broken slopes underlain predominantly by basaltic breccia.

12. Rolling to strongly rolling sand dunes forming the sand spit south of Warrington.

13. Broken rolling to strongly rolling slopes of earth�ow topography developed predominantly on Concord Formation greensands.

14. Smooth rolling to strongly rolling slopes developed predominantly on Abbotsford mudstone.

15. Complex strongly rolling to moderately steep slope rippled or hummocky slopes of slump earth�ow topography formed predominantly on Abbotsford mudstone.

16. Smooth rolling slopes above a steep sea cli� and reef complex formed on phonolite.

Turbine location (25m radius)

Porteous Hill landform components Scale 1:20,000 @ A4

km1.00

12

10

11

7

8

9

16

13

14

15

6

3

4

55

12

Warrington

Omimi

Blueskin Bay

Porteous Hill(401m)

SH1

land typing

Porteous28 September 2014Date Printed:

This map is a user generated static output from an Internet mapping site andis for reference only. Data layers that appear on this map may or may not be

accurate, current, or otherwise reliable.

THIS MAP IS NOT TO BE USED FOR NAVIGATION

Kilometers0.50

10,000SCALE 1:

Projection: NZGD_2000_New_Zealand_Transverse_Mercator

0.5

Legend

© CNES 2004-2010 / Spot Image

© GeographxCrown Copyright Reserved

Porteous28 September 2014Date Printed:

This map is a user generated static output from an Internet mapping site andis for reference only. Data layers that appear on this map may or may not be

accurate, current, or otherwise reliable.

THIS MAP IS NOT TO BE USED FOR NAVIGATION

Kilometers1.00

20,000SCALE 1:

Projection: NZGD_2000_New_Zealand_Transverse_Mercator

1.0

Legend

© CNES 2004-2010 / Spot Image

© GeographxCrown Copyright Reserved

12

10

11

7

8

9

16

13

14

15

6

3

4

55

12

Key - Landform Components

1. Rolling to easy rolling loess mantled slopes developed on olivine basalt (Porteous soils).

2. Strongly rolling to moderately steep colluvial slopes developed on dolerite and basaltic breccia.

3. Complex strongly rolling to moderately steep slopes with rippled or hummocky surfaces of slump earthflow topography formed on Burnside and Abbotsford mudstones.

4. Steep to moderately steep basaltic hard rock slopes (Hammond Hill).

5. Isolated strongly rolling to steep basaltic hillocks.6. Smooth strongly rolling to rolling loess mantled

slopes developed on basalt.7. Complex rolling to strongly rolling slopes of

earthflow topography formed largely on Burnside Formation mudstone.

8. Smooth rolling slopes on weathered basalt.9. Broken and slumped steep to moderately steep

slopes with steep to very steep basal sea cliffs cut into sedimentary strata.

10. Steep to moderately steep side slopes on basalt and basaltic colluvium.

11. Strongly rolling broken slopes underlain predominantly by basaltic breccia.

12. Rolling to strongly rolling sand dunes forming the sand spit south of Warrington.

13. Broken rolling to strongly rolling slopes of earthflow topography developed predominantly on Concord Formation greensands.

14. Smooth rolling to strongly rolling slopes developed predominantly on Abbotsford mudstone.

15. Complex strongly rolling to moderately steep slope rippled or hummocky slopes of slump earthflow topography formed predominantly on Abbotsford mudstone.

16. Smooth rolling slopes above a steep sea cliff and reef complex formed on phonolite.

Turbine location (25m radius)

Porteous Hill landform components - Scale 1:20,000

Warrington

Omimi

Blueskin Bay

Porteous Hill(401m)

SH1

Landform Components

(30m radius)

Blueskin Energy Wind Cluster | Porteous Hill landscape assessment

page 9

Porteous28 September 2014Date Printed:

This map is a user generated static output from an Internet mapping site andis for reference only. Data layers that appear on this map may or may not be

accurate, current, or otherwise reliable.

THIS MAP IS NOT TO BE USED FOR NAVIGATION

Kilometers0.50

10,000SCALE 1:

Projection: NZGD_2000_New_Zealand_Transverse_Mercator

0.5

Legend

© CNES 2004-2010 / Spot Image

© GeographxCrown Copyright Reserved

Porteous

This map is a user generated static output from an Internet mapping site andis for reference only. Data layers that appear on this map may or may not be

accurate, current, or otherwise reliable.

THIS MAP IS NOT TO BE USED FOR NAVIGATION

Kilometers1.0

20,000

NZGD_2000_New_Zealand_Transverse_Mercator

Legend

© CNES 2004-2010 / Spot Image

© GeographxCrown Copyright Reserved

Landform Components

1. Rolling to easy rolling loess mantled slopes developed on olivine basalt (Porteous soils).

2. Strongly rolling to moderately steep colluvial slopes developed on dolerite and basaltic breccia.

3. Complex strongly rolling to moderately steep slopes with rippled or hummocky surfaces of slump earth�ow topography formed on Burnside and Abbotsford mudstones.

4. Steep to moderately steep basaltic hard rock slopes (Hammond Hill).

5. Isolated strongly rolling to steep basaltic hillocks.6. Smooth strongly rolling to rolling loess mantled

slopes developed on basalt.7. Complex rolling to strongly rolling slopes of

earth�ow topography formed largely on Burnside Formation mudstone.

8. Smooth rolling slopes on weathered basalt.9. Broken and slumped steep to moderately steep

slopes with steep to very steep basal sea cli�s cut into sedimentary strata.

10. Steep to moderately steep side slopes on basalt and basaltic colluvium.

11. Strongly rolling broken slopes underlain predominantly by basaltic breccia.

12. Rolling to strongly rolling sand dunes forming the sand spit south of Warrington.

13. Broken rolling to strongly rolling slopes of earth�ow topography developed predominantly on Concord Formation greensands.

14. Smooth rolling to strongly rolling slopes developed predominantly on Abbotsford mudstone.

15. Complex strongly rolling to moderately steep slope rippled or hummocky slopes of slump earth�ow topography formed predominantly on Abbotsford mudstone.

16. Smooth rolling slopes above a steep sea cli� and reef complex formed on phonolite.

Turbine location (25m radius)

Porteous Hill landform components Scale 1:20,000 @ A4

km1.00

12

10

11

7

8

9

16

13

14

15

6

3

4

55

12

Warrington

Omimi

Blueskin Bay

Porteous Hill(401m)

SH1

land typing

Blueskin Energy Wind Cluster | Porteous Hill landscape assessment

page 10

Porteous28 September 2014Date Printed:

This map is a user generated static output from an Internet mapping site andis for reference only. Data layers that appear on this map may or may not be

accurate, current, or otherwise reliable.

THIS MAP IS NOT TO BE USED FOR NAVIGATION

Kilometers0.50

10,000SCALE 1:

Projection: NZGD_2000_New_Zealand_Transverse_Mercator

0.5

Legend

© CNES 2004-2010 / Spot Image

© GeographxCrown Copyright Reserved

Porteous28 September 2014Date Printed:

This map is a user generated static output from an Internet mapping site andis for reference only. Data layers that appear on this map may or may not be

accurate, current, or otherwise reliable.

THIS MAP IS NOT TO BE USED FOR NAVIGATION

Kilometers1.00

20,000SCALE 1:

Projection: NZGD_2000_New_Zealand_Transverse_Mercator

1.0

Legend

© CNES 2004-2010 / Spot Image

© GeographxCrown Copyright Reserved

12

10

11

7

8

9

16

13

14

15

6

3

4

55

12

Key - Landform Components

1. Rolling to easy rolling loess mantled slopes developed on olivine basalt (Porteous soils).

2. Strongly rolling to moderately steep colluvial slopes developed on dolerite and basaltic breccia.

3. Complex strongly rolling to moderately steep slopes with rippled or hummocky surfaces of slump earthflow topography formed on Burnside and Abbotsford mudstones.

4. Steep to moderately steep basaltic hard rock slopes (Hammond Hill).

5. Isolated strongly rolling to steep basaltic hillocks.6. Smooth strongly rolling to rolling loess mantled

slopes developed on basalt.7. Complex rolling to strongly rolling slopes of

earthflow topography formed largely on Burnside Formation mudstone.

8. Smooth rolling slopes on weathered basalt.9. Broken and slumped steep to moderately steep

slopes with steep to very steep basal sea cliffs cut into sedimentary strata.

10. Steep to moderately steep side slopes on basalt and basaltic colluvium.

11. Strongly rolling broken slopes underlain predominantly by basaltic breccia.

12. Rolling to strongly rolling sand dunes forming the sand spit south of Warrington.

13. Broken rolling to strongly rolling slopes of earthflow topography developed predominantly on Concord Formation greensands.

14. Smooth rolling to strongly rolling slopes developed predominantly on Abbotsford mudstone.

15. Complex strongly rolling to moderately steep slope rippled or hummocky slopes of slump earthflow topography formed predominantly on Abbotsford mudstone.

16. Smooth rolling slopes above a steep sea cliff and reef complex formed on phonolite.

Turbine location (25m radius)

Porteous Hill landform components - Scale 1:20,000

Warrington

Omimi

Blueskin Bay

Porteous Hill(401m)

SH1

Porteous28 September 2014Date Printed:

This map is a user generated static output from an Internet mapping site andis for reference only. Data layers that appear on this map may or may not be

accurate, current, or otherwise reliable.

THIS MAP IS NOT TO BE USED FOR NAVIGATION

Kilometers0.50

10,000SCALE 1:

Projection: NZGD_2000_New_Zealand_Transverse_Mercator

0.5

Legend

© CNES 2004-2010 / Spot Image

© GeographxCrown Copyright Reserved

Porteous

This map is a user generated static output from an Internet mapping site andis for reference only. Data layers that appear on this map may or may not be

accurate, current, or otherwise reliable.

THIS MAP IS NOT TO BE USED FOR NAVIGATION

Kilometers1.0

20,000

NZGD_2000_New_Zealand_Transverse_Mercator

Legend

© CNES 2004-2010 / Spot Image

© GeographxCrown Copyright Reserved

Landform Components

1. Rolling to easy rolling loess mantled slopes developed on olivine basalt (Porteous soils).

2. Strongly rolling to moderately steep colluvial slopes developed on dolerite and basaltic breccia.

3. Complex strongly rolling to moderately steep slopes with rippled or hummocky surfaces of slump earth�ow topography formed on Burnside and Abbotsford mudstones.

4. Steep to moderately steep basaltic hard rock slopes (Hammond Hill).

5. Isolated strongly rolling to steep basaltic hillocks.6. Smooth strongly rolling to rolling loess mantled

slopes developed on basalt.7. Complex rolling to strongly rolling slopes of

earth�ow topography formed largely on Burnside Formation mudstone.

8. Smooth rolling slopes on weathered basalt.9. Broken and slumped steep to moderately steep

slopes with steep to very steep basal sea cli�s cut into sedimentary strata.

10. Steep to moderately steep side slopes on basalt and basaltic colluvium.

11. Strongly rolling broken slopes underlain predominantly by basaltic breccia.

12. Rolling to strongly rolling sand dunes forming the sand spit south of Warrington.

13. Broken rolling to strongly rolling slopes of earth�ow topography developed predominantly on Concord Formation greensands.

14. Smooth rolling to strongly rolling slopes developed predominantly on Abbotsford mudstone.

15. Complex strongly rolling to moderately steep slope rippled or hummocky slopes of slump earth�ow topography formed predominantly on Abbotsford mudstone.

16. Smooth rolling slopes above a steep sea cli� and reef complex formed on phonolite.

Turbine

Volcanic landform components

Deposition landform components

location (25m radius)

Porteous Hill landform components Scale 1:20,000 @ A4

km1.00

12

10

11

7

8

9

16

13

14

15

6

3

4

55

12

Warrington

Omimi

Guilds HillHammond Hill

Blueskin Bay

Porteous Hill(401m)

SH1

Porteous28 September 2014Date Printed:

This map is a user generated static output from an Internet mapping site andis for reference only. Data layers that appear on this map may or may not be

accurate, current, or otherwise reliable.

THIS MAP IS NOT TO BE USED FOR NAVIGATION

Kilometers0.50

10,000SCALE 1:

Projection: NZGD_2000_New_Zealand_Transverse_Mercator

0.5

Legend

© CNES 2004-2010 / Spot Image

© GeographxCrown Copyright Reserved

Porteous

This map is a user generated static output from an Internet mapping site andis for reference only. Data layers that appear on this map may or may not be

accurate, current, or otherwise reliable.

THIS MAP IS NOT TO BE USED FOR NAVIGATION

Kilometers1.0

20,000

NZGD_2000_New_Zealand_Transverse_Mercator

Legend

© CNES 2004-2010 / Spot Image

© GeographxCrown Copyright Reserved

Landform Components

1. Rolling to easy rolling loess mantled slopes developed on olivine basalt (Porteous soils).

2. Strongly rolling to moderately steep colluvial slopes developed on dolerite and basaltic breccia.

3. Complex strongly rolling to moderately steep slopes with rippled or hummocky surfaces of slump earth�ow topography formed on Burnside and Abbotsford mudstones.

4. Steep to moderately steep basaltic hard rock slopes (Hammond Hill).

5. Isolated strongly rolling to steep basaltic hillocks.6. Smooth strongly rolling to rolling loess mantled

slopes developed on basalt.7. Complex rolling to strongly rolling slopes of

earth�ow topography formed largely on Burnside Formation mudstone.

8. Smooth rolling slopes on weathered basalt.9. Broken and slumped steep to moderately steep

slopes with steep to very steep basal sea cli�s cut into sedimentary strata.

10. Steep to moderately steep side slopes on basalt and basaltic colluvium.

11. Strongly rolling broken slopes underlain predominantly by basaltic breccia.

12. Rolling to strongly rolling sand dunes forming the sand spit south of Warrington.

13. Broken rolling to strongly rolling slopes of earth�ow topography developed predominantly on Concord Formation greensands.

14. Smooth rolling to strongly rolling slopes developed predominantly on Abbotsford mudstone.

15. Complex strongly rolling to moderately steep slope rippled or hummocky slopes of slump earth�ow topography formed predominantly on Abbotsford mudstone.

16. Smooth rolling slopes above a steep sea cli� and reef complex formed on phonolite.

Turbine

Volcanic landform components

Deposition landform components

location (25m radius)

Porteous Hill landform components Scale 1:20,000 @ A4

km1.00

12

10

11

7

8

9

16

13

14

15

6

3

4

55

12

Warrington

Omimi

Guilds HillHammond Hill

Blueskin Bay

Porteous Hill(401m)

SH1

Porteous28 September 2014Date Printed:

This map is a user generated static output from an Internet mapping site andis for reference only. Data layers that appear on this map may or may not be

accurate, current, or otherwise reliable.

THIS MAP IS NOT TO BE USED FOR NAVIGATION

Kilometers0.50

10,000SCALE 1:

Projection: NZGD_2000_New_Zealand_Transverse_Mercator

0.5

Legend

© CNES 2004-2010 / Spot Image

© GeographxCrown Copyright Reserved

Porteous

This map is a user generated static output from an Internet mapping site andis for reference only. Data layers that appear on this map may or may not be

accurate, current, or otherwise reliable.

THIS MAP IS NOT TO BE USED FOR NAVIGATION

Kilometers1.0

20,000

NZGD_2000_New_Zealand_Transverse_Mercator

Legend

© CNES 2004-2010 / Spot Image

© GeographxCrown Copyright Reserved

Landform Components

1. Rolling to easy rolling loess mantled slopes developed on olivine basalt (Porteous soils).

2. Strongly rolling to moderately steep colluvial slopes developed on dolerite and basaltic breccia.

3. Complex strongly rolling to moderately steep slopes with rippled or hummocky surfaces of slump earth�ow topography formed on Burnside and Abbotsford mudstones.

4. Steep to moderately steep basaltic hard rock slopes (Hammond Hill).

5. Isolated strongly rolling to steep basaltic hillocks.6. Smooth strongly rolling to rolling loess mantled

slopes developed on basalt.7. Complex rolling to strongly rolling slopes of

earth�ow topography formed largely on Burnside Formation mudstone.

8. Smooth rolling slopes on weathered basalt.9. Broken and slumped steep to moderately steep

slopes with steep to very steep basal sea cli�s cut into sedimentary strata.

10. Steep to moderately steep side slopes on basalt and basaltic colluvium.

11. Strongly rolling broken slopes underlain predominantly by basaltic breccia.

12. Rolling to strongly rolling sand dunes forming the sand spit south of Warrington.

13. Broken rolling to strongly rolling slopes of earth�ow topography developed predominantly on Concord Formation greensands.

14. Smooth rolling to strongly rolling slopes developed predominantly on Abbotsford mudstone.

15. Complex strongly rolling to moderately steep slope rippled or hummocky slopes of slump earth�ow topography formed predominantly on Abbotsford mudstone.

16. Smooth rolling slopes above a steep sea cli� and reef complex formed on phonolite.

Turbine

Volcanic landform components

Deposition landform components

location (25m radius)

Porteous Hill landform components Scale 1:20,000 @ A4

km1.00

12

10

11

7

8

9

16

13

14

15

6

3

4

55

12

Warrington

Omimi

Guilds HillHammond Hill

Blueskin Bay

Porteous Hill(401m)

SH1

Porteous28 September 2014Date Printed:

This map is a user generated static output from an Internet mapping site andis for reference only. Data layers that appear on this map may or may not be

accurate, current, or otherwise reliable.

THIS MAP IS NOT TO BE USED FOR NAVIGATION

Kilometers0.50

10,000SCALE 1:

Projection: NZGD_2000_New_Zealand_Transverse_Mercator

0.5

Legend

© CNES 2004-2010 / Spot Image

© GeographxCrown Copyright Reserved

Porteous

This map is a user generated static output from an Internet mapping site andis for reference only. Data layers that appear on this map may or may not be

accurate, current, or otherwise reliable.

THIS MAP IS NOT TO BE USED FOR NAVIGATION

Kilometers1.0

20,000

NZGD_2000_New_Zealand_Transverse_Mercator

Legend

© CNES 2004-2010 / Spot Image

© GeographxCrown Copyright Reserved

Landform Components

1. Rolling to easy rolling loess mantled slopes developed on olivine basalt (Porteous soils).

2. Strongly rolling to moderately steep colluvial slopes developed on dolerite and basaltic breccia.

3. Complex strongly rolling to moderately steep slopes with rippled or hummocky surfaces of slump earth�ow topography formed on Burnside and Abbotsford mudstones.

4. Steep to moderately steep basaltic hard rock slopes (Hammond Hill).

5. Isolated strongly rolling to steep basaltic hillocks.6. Smooth strongly rolling to rolling loess mantled

slopes developed on basalt.7. Complex rolling to strongly rolling slopes of

earth�ow topography formed largely on Burnside Formation mudstone.

8. Smooth rolling slopes on weathered basalt.9. Broken and slumped steep to moderately steep

slopes with steep to very steep basal sea cli�s cut into sedimentary strata.

10. Steep to moderately steep side slopes on basalt and basaltic colluvium.

11. Strongly rolling broken slopes underlain predominantly by basaltic breccia.

12. Rolling to strongly rolling sand dunes forming the sand spit south of Warrington.

13. Broken rolling to strongly rolling slopes of earth�ow topography developed predominantly on Concord Formation greensands.

14. Smooth rolling to strongly rolling slopes developed predominantly on Abbotsford mudstone.

15. Complex strongly rolling to moderately steep slope rippled or hummocky slopes of slump earth�ow topography formed predominantly on Abbotsford mudstone.

16. Smooth rolling slopes above a steep sea cli� and reef complex formed on phonolite.

Turbine

Volcanic landform components

Deposition landform components

location (25m radius)

Porteous Hill landform components Scale 1:20,000 @ A4

km1.00

12

10

11

7

8

9

16

13

14

15

6

3

4

55

12

Warrington

Omimi

Guilds HillHammond Hill

Blueskin Bay

Porteous Hill(401m)

SH1

Porteous28 September 2014Date Printed:

This map is a user generated static output from an Internet mapping site andis for reference only. Data layers that appear on this map may or may not be

accurate, current, or otherwise reliable.

THIS MAP IS NOT TO BE USED FOR NAVIGATION

Kilometers0.50

10,000SCALE 1:

Projection: NZGD_2000_New_Zealand_Transverse_Mercator

0.5

Legend

© CNES 2004-2010 / Spot Image

© GeographxCrown Copyright Reserved

Porteous

This map is a user generated static output from an Internet mapping site andis for reference only. Data layers that appear on this map may or may not be

accurate, current, or otherwise reliable.

THIS MAP IS NOT TO BE USED FOR NAVIGATION

Kilometers1.0

20,000

NZGD_2000_New_Zealand_Transverse_Mercator

Legend

© CNES 2004-2010 / Spot Image

© GeographxCrown Copyright Reserved

Landform Components

1. Rolling to easy rolling loess mantled slopes developed on olivine basalt (Porteous soils).

2. Strongly rolling to moderately steep colluvial slopes developed on dolerite and basaltic breccia.

3. Complex strongly rolling to moderately steep slopes with rippled or hummocky surfaces of slump earth�ow topography formed on Burnside and Abbotsford mudstones.

4. Steep to moderately steep basaltic hard rock slopes (Hammond Hill).

5. Isolated strongly rolling to steep basaltic hillocks.6. Smooth strongly rolling to rolling loess mantled

slopes developed on basalt.7. Complex rolling to strongly rolling slopes of

earth�ow topography formed largely on Burnside Formation mudstone.

8. Smooth rolling slopes on weathered basalt.9. Broken and slumped steep to moderately steep

slopes with steep to very steep basal sea cli�s cut into sedimentary strata.

10. Steep to moderately steep side slopes on basalt and basaltic colluvium.

11. Strongly rolling broken slopes underlain predominantly by basaltic breccia.

12. Rolling to strongly rolling sand dunes forming the sand spit south of Warrington.

13. Broken rolling to strongly rolling slopes of earth�ow topography developed predominantly on Concord Formation greensands.

14. Smooth rolling to strongly rolling slopes developed predominantly on Abbotsford mudstone.

15. Complex strongly rolling to moderately steep slope rippled or hummocky slopes of slump earth�ow topography formed predominantly on Abbotsford mudstone.

16. Smooth rolling slopes above a steep sea cli� and reef complex formed on phonolite.

Turbine

Volcanic landform components

Deposition landform components

location (25m radius)

Porteous Hill landform components Scale 1:20,000 @ A4

km1.00

12

10

11

7

8

9

16

13

14

15

6

3

4

55

12

Warrington

Omimi

Guilds HillHammond Hill

Blueskin Bay

Porteous Hill(401m)

SH1

Porteous28 September 2014Date Printed:

This map is a user generated static output from an Internet mapping site andis for reference only. Data layers that appear on this map may or may not be

accurate, current, or otherwise reliable.

THIS MAP IS NOT TO BE USED FOR NAVIGATION

Kilometers0.50

10,000SCALE 1:

Projection: NZGD_2000_New_Zealand_Transverse_Mercator

0.5

Legend

© CNES 2004-2010 / Spot Image

© GeographxCrown Copyright Reserved

Porteous

This map is a user generated static output from an Internet mapping site andis for reference only. Data layers that appear on this map may or may not be

accurate, current, or otherwise reliable.

THIS MAP IS NOT TO BE USED FOR NAVIGATION

Kilometers1.0

20,000

NZGD_2000_New_Zealand_Transverse_Mercator

Legend

© CNES 2004-2010 / Spot Image

© GeographxCrown Copyright Reserved

Landform Components

1. Rolling to easy rolling loess mantled slopes developed on olivine basalt (Porteous soils).

2. Strongly rolling to moderately steep colluvial slopes developed on dolerite and basaltic breccia.

3. Complex strongly rolling to moderately steep slopes with rippled or hummocky surfaces of slump earth�ow topography formed on Burnside and Abbotsford mudstones.

4. Steep to moderately steep basaltic hard rock slopes (Hammond Hill).

5. Isolated strongly rolling to steep basaltic hillocks.6. Smooth strongly rolling to rolling loess mantled

slopes developed on basalt.7. Complex rolling to strongly rolling slopes of

earth�ow topography formed largely on Burnside Formation mudstone.

8. Smooth rolling slopes on weathered basalt.9. Broken and slumped steep to moderately steep

slopes with steep to very steep basal sea cli�s cut into sedimentary strata.

10. Steep to moderately steep side slopes on basalt and basaltic colluvium.

11. Strongly rolling broken slopes underlain predominantly by basaltic breccia.

12. Rolling to strongly rolling sand dunes forming the sand spit south of Warrington.

13. Broken rolling to strongly rolling slopes of earth�ow topography developed predominantly on Concord Formation greensands.

14. Smooth rolling to strongly rolling slopes developed predominantly on Abbotsford mudstone.

15. Complex strongly rolling to moderately steep slope rippled or hummocky slopes of slump earth�ow topography formed predominantly on Abbotsford mudstone.

16. Smooth rolling slopes above a steep sea cli� and reef complex formed on phonolite.

Turbine

Volcanic landform components

Deposition landform components

location (25m radius)

Porteous Hill landform components Scale 1:20,000 @ A4

km1.00

12

10

11

7

8

9

16

13

14

15

6

3

4

55

12

Warrington

Omimi

Guilds HillHammond Hill

Blueskin Bay

Porteous Hill(401m)

SH1

Porteous28 September 2014Date Printed:

This map is a user generated static output from an Internet mapping site andis for reference only. Data layers that appear on this map may or may not be

accurate, current, or otherwise reliable.

THIS MAP IS NOT TO BE USED FOR NAVIGATION

Kilometers0.50

10,000SCALE 1:

Projection: NZGD_2000_New_Zealand_Transverse_Mercator

0.5

Legend

© CNES 2004-2010 / Spot Image

© GeographxCrown Copyright Reserved

Porteous

This map is a user generated static output from an Internet mapping site andis for reference only. Data layers that appear on this map may or may not be

accurate, current, or otherwise reliable.

THIS MAP IS NOT TO BE USED FOR NAVIGATION

Kilometers1.0

20,000

NZGD_2000_New_Zealand_Transverse_Mercator

Legend

© CNES 2004-2010 / Spot Image

© GeographxCrown Copyright Reserved

Landform Components

1. Rolling to easy rolling loess mantled slopes developed on olivine basalt (Porteous soils).

2. Strongly rolling to moderately steep colluvial slopes developed on dolerite and basaltic breccia.

3. Complex strongly rolling to moderately steep slopes with rippled or hummocky surfaces of slump earth�ow topography formed on Burnside and Abbotsford mudstones.

4. Steep to moderately steep basaltic hard rock slopes (Hammond Hill).

5. Isolated strongly rolling to steep basaltic hillocks.6. Smooth strongly rolling to rolling loess mantled

slopes developed on basalt.7. Complex rolling to strongly rolling slopes of

earth�ow topography formed largely on Burnside Formation mudstone.

8. Smooth rolling slopes on weathered basalt.9. Broken and slumped steep to moderately steep

slopes with steep to very steep basal sea cli�s cut into sedimentary strata.

10. Steep to moderately steep side slopes on basalt and basaltic colluvium.

11. Strongly rolling broken slopes underlain predominantly by basaltic breccia.

12. Rolling to strongly rolling sand dunes forming the sand spit south of Warrington.

13. Broken rolling to strongly rolling slopes of earth�ow topography developed predominantly on Concord Formation greensands.

14. Smooth rolling to strongly rolling slopes developed predominantly on Abbotsford mudstone.

15. Complex strongly rolling to moderately steep slope rippled or hummocky slopes of slump earth�ow topography formed predominantly on Abbotsford mudstone.

16. Smooth rolling slopes above a steep sea cli� and reef complex formed on phonolite.

Turbine

Volcanic landform components

Deposition landform components

location (25m radius)

Porteous Hill landform components Scale 1:20,000 @ A4

km1.00

12

10

11

7

8

9

16

13

14

15

6

3

4

55

12

Warrington

Omimi

Guilds HillHammond Hill

Blueskin Bay

Porteous Hill(401m)

SH1

Porteous28 September 2014Date Printed:

This map is a user generated static output from an Internet mapping site andis for reference only. Data layers that appear on this map may or may not be

accurate, current, or otherwise reliable.

THIS MAP IS NOT TO BE USED FOR NAVIGATION

Kilometers0.50

10,000SCALE 1:

Projection: NZGD_2000_New_Zealand_Transverse_Mercator

0.5

Legend

© CNES 2004-2010 / Spot Image

© GeographxCrown Copyright Reserved

Porteous

This map is a user generated static output from an Internet mapping site andis for reference only. Data layers that appear on this map may or may not be

accurate, current, or otherwise reliable.

THIS MAP IS NOT TO BE USED FOR NAVIGATION

Kilometers1.0

20,000

NZGD_2000_New_Zealand_Transverse_Mercator

Legend

© CNES 2004-2010 / Spot Image

© GeographxCrown Copyright Reserved

Landform Components

1. Rolling to easy rolling loess mantled slopes developed on olivine basalt (Porteous soils).

2. Strongly rolling to moderately steep colluvial slopes developed on dolerite and basaltic breccia.

3. Complex strongly rolling to moderately steep slopes with rippled or hummocky surfaces of slump earth�ow topography formed on Burnside and Abbotsford mudstones.

4. Steep to moderately steep basaltic hard rock slopes (Hammond Hill).

5. Isolated strongly rolling to steep basaltic hillocks.6. Smooth strongly rolling to rolling loess mantled

slopes developed on basalt.7. Complex rolling to strongly rolling slopes of

earth�ow topography formed largely on Burnside Formation mudstone.

8. Smooth rolling slopes on weathered basalt.9. Broken and slumped steep to moderately steep

slopes with steep to very steep basal sea cli�s cut into sedimentary strata.

10. Steep to moderately steep side slopes on basalt and basaltic colluvium.

11. Strongly rolling broken slopes underlain predominantly by basaltic breccia.

12. Rolling to strongly rolling sand dunes forming the sand spit south of Warrington.

13. Broken rolling to strongly rolling slopes of earth�ow topography developed predominantly on Concord Formation greensands.

14. Smooth rolling to strongly rolling slopes developed predominantly on Abbotsford mudstone.

15. Complex strongly rolling to moderately steep slope rippled or hummocky slopes of slump earth�ow topography formed predominantly on Abbotsford mudstone.

16. Smooth rolling slopes above a steep sea cli� and reef complex formed on phonolite.

Turbine

Volcanic landform components

Deposition landform components

location (25m radius)

Porteous Hill landform components Scale 1:20,000 @ A4

km1.00

12

10

11

7

8

9

16

13

14

15

6

3

4

55

12

Warrington

Omimi

Guilds HillHammond Hill

Blueskin Bay

Porteous Hill(401m)

SH1

Porteous28 September 2014Date Printed:

This map is a user generated static output from an Internet mapping site andis for reference only. Data layers that appear on this map may or may not be

accurate, current, or otherwise reliable.

THIS MAP IS NOT TO BE USED FOR NAVIGATION

Kilometers0.50

10,000SCALE 1:

Projection: NZGD_2000_New_Zealand_Transverse_Mercator

0.5

Legend

© CNES 2004-2010 / Spot Image

© GeographxCrown Copyright Reserved

Porteous

This map is a user generated static output from an Internet mapping site andis for reference only. Data layers that appear on this map may or may not be

accurate, current, or otherwise reliable.

THIS MAP IS NOT TO BE USED FOR NAVIGATION

Kilometers1.0

20,000

NZGD_2000_New_Zealand_Transverse_Mercator

Legend

© CNES 2004-2010 / Spot Image

© GeographxCrown Copyright Reserved

Landform Components

1. Rolling to easy rolling loess mantled slopes developed on olivine basalt (Porteous soils).

2. Strongly rolling to moderately steep colluvial slopes developed on dolerite and basaltic breccia.

3. Complex strongly rolling to moderately steep slopes with rippled or hummocky surfaces of slump earth�ow topography formed on Burnside and Abbotsford mudstones.

4. Steep to moderately steep basaltic hard rock slopes (Hammond Hill).

5. Isolated strongly rolling to steep basaltic hillocks.6. Smooth strongly rolling to rolling loess mantled

slopes developed on basalt.7. Complex rolling to strongly rolling slopes of

earth�ow topography formed largely on Burnside Formation mudstone.

8. Smooth rolling slopes on weathered basalt.9. Broken and slumped steep to moderately steep

slopes with steep to very steep basal sea cli�s cut into sedimentary strata.

10. Steep to moderately steep side slopes on basalt and basaltic colluvium.

11. Strongly rolling broken slopes underlain predominantly by basaltic breccia.

12. Rolling to strongly rolling sand dunes forming the sand spit south of Warrington.

13. Broken rolling to strongly rolling slopes of earth�ow topography developed predominantly on Concord Formation greensands.

14. Smooth rolling to strongly rolling slopes developed predominantly on Abbotsford mudstone.

15. Complex strongly rolling to moderately steep slope rippled or hummocky slopes of slump earth�ow topography formed predominantly on Abbotsford mudstone.

16. Smooth rolling slopes above a steep sea cli� and reef complex formed on phonolite.

Turbine

Volcanic landform components

Deposition landform components

location (25m radius)

Porteous Hill landform components Scale 1:20,000 @ A4

km1.00

12

10

11

7

8

9

16

13

14

15

6

3

4

55

12

Warrington

Omimi

Guilds HillHammond Hill

Blueskin Bay

Porteous Hill(401m)

SH1

Porteous28 September 2014Date Printed:

This map is a user generated static output from an Internet mapping site andis for reference only. Data layers that appear on this map may or may not be

accurate, current, or otherwise reliable.

THIS MAP IS NOT TO BE USED FOR NAVIGATION

Kilometers0.50

10,000SCALE 1:

Projection: NZGD_2000_New_Zealand_Transverse_Mercator

0.5

Legend

© CNES 2004-2010 / Spot Image

© GeographxCrown Copyright Reserved

Porteous

This map is a user generated static output from an Internet mapping site andis for reference only. Data layers that appear on this map may or may not be

accurate, current, or otherwise reliable.

THIS MAP IS NOT TO BE USED FOR NAVIGATION

Kilometers1.0

20,000

NZGD_2000_New_Zealand_Transverse_Mercator

Legend

© CNES 2004-2010 / Spot Image

© GeographxCrown Copyright Reserved

Landform Components

1. Rolling to easy rolling loess mantled slopes developed on olivine basalt (Porteous soils).

2. Strongly rolling to moderately steep colluvial slopes developed on dolerite and basaltic breccia.

3. Complex strongly rolling to moderately steep slopes with rippled or hummocky surfaces of slump earth�ow topography formed on Burnside and Abbotsford mudstones.

4. Steep to moderately steep basaltic hard rock slopes (Hammond Hill).

5. Isolated strongly rolling to steep basaltic hillocks.6. Smooth strongly rolling to rolling loess mantled

slopes developed on basalt.7. Complex rolling to strongly rolling slopes of

earth�ow topography formed largely on Burnside Formation mudstone.

8. Smooth rolling slopes on weathered basalt.9. Broken and slumped steep to moderately steep

slopes with steep to very steep basal sea cli�s cut into sedimentary strata.

10. Steep to moderately steep side slopes on basalt and basaltic colluvium.

11. Strongly rolling broken slopes underlain predominantly by basaltic breccia.

12. Rolling to strongly rolling sand dunes forming the sand spit south of Warrington.

13. Broken rolling to strongly rolling slopes of earth�ow topography developed predominantly on Concord Formation greensands.

14. Smooth rolling to strongly rolling slopes developed predominantly on Abbotsford mudstone.

15. Complex strongly rolling to moderately steep slope rippled or hummocky slopes of slump earth�ow topography formed predominantly on Abbotsford mudstone.

16. Smooth rolling slopes above a steep sea cli� and reef complex formed on phonolite.

Turbine

Volcanic landform components

Deposition landform components

location (25m radius)

Porteous Hill landform components Scale 1:20,000 @ A4

km1.00

12

10

11

7

8

9

16

13

14

15

6

3

4

55

12

Warrington

Omimi

Guilds HillHammond Hill

Blueskin Bay

Porteous Hill(401m)

SH1

Porteous28 September 2014Date Printed:

This map is a user generated static output from an Internet mapping site andis for reference only. Data layers that appear on this map may or may not be

accurate, current, or otherwise reliable.

THIS MAP IS NOT TO BE USED FOR NAVIGATION

Kilometers0.50

10,000SCALE 1:

Projection: NZGD_2000_New_Zealand_Transverse_Mercator

0.5

Legend

© CNES 2004-2010 / Spot Image

© GeographxCrown Copyright Reserved

Porteous

This map is a user generated static output from an Internet mapping site andis for reference only. Data layers that appear on this map may or may not be

accurate, current, or otherwise reliable.

THIS MAP IS NOT TO BE USED FOR NAVIGATION

Kilometers1.0

20,000

NZGD_2000_New_Zealand_Transverse_Mercator

Legend

© CNES 2004-2010 / Spot Image

© GeographxCrown Copyright Reserved

Landform Components

1. Rolling to easy rolling loess mantled slopes developed on olivine basalt (Porteous soils).

2. Strongly rolling to moderately steep colluvial slopes developed on dolerite and basaltic breccia.

3. Complex strongly rolling to moderately steep slopes with rippled or hummocky surfaces of slump earth�ow topography formed on Burnside and Abbotsford mudstones.

4. Steep to moderately steep basaltic hard rock slopes (Hammond Hill).

5. Isolated strongly rolling to steep basaltic hillocks.6. Smooth strongly rolling to rolling loess mantled

slopes developed on basalt.7. Complex rolling to strongly rolling slopes of

earth�ow topography formed largely on Burnside Formation mudstone.

8. Smooth rolling slopes on weathered basalt.9. Broken and slumped steep to moderately steep

slopes with steep to very steep basal sea cli�s cut into sedimentary strata.

10. Steep to moderately steep side slopes on basalt and basaltic colluvium.

11. Strongly rolling broken slopes underlain predominantly by basaltic breccia.

12. Rolling to strongly rolling sand dunes forming the sand spit south of Warrington.

13. Broken rolling to strongly rolling slopes of earth�ow topography developed predominantly on Concord Formation greensands.

14. Smooth rolling to strongly rolling slopes developed predominantly on Abbotsford mudstone.

15. Complex strongly rolling to moderately steep slope rippled or hummocky slopes of slump earth�ow topography formed predominantly on Abbotsford mudstone.

16. Smooth rolling slopes above a steep sea cli� and reef complex formed on phonolite.

Turbine

Volcanic landform components

Deposition landform components

location (25m radius)

Porteous Hill landform components Scale 1:20,000 @ A4

km1.00

12

10

11

7

8

9

16

13

14

15

6

3

4

55

12

Warrington

Omimi

Guilds HillHammond Hill

Blueskin Bay

Porteous Hill(401m)

SH1

Porteous28 September 2014Date Printed:

This map is a user generated static output from an Internet mapping site andis for reference only. Data layers that appear on this map may or may not be

accurate, current, or otherwise reliable.

THIS MAP IS NOT TO BE USED FOR NAVIGATION

Kilometers0.50

10,000SCALE 1:

Projection: NZGD_2000_New_Zealand_Transverse_Mercator

0.5

Legend

© CNES 2004-2010 / Spot Image

© GeographxCrown Copyright Reserved

Porteous

This map is a user generated static output from an Internet mapping site andis for reference only. Data layers that appear on this map may or may not be

accurate, current, or otherwise reliable.

THIS MAP IS NOT TO BE USED FOR NAVIGATION

Kilometers1.0

20,000

NZGD_2000_New_Zealand_Transverse_Mercator

Legend

© CNES 2004-2010 / Spot Image

© GeographxCrown Copyright Reserved

Landform Components

1. Rolling to easy rolling loess mantled slopes developed on olivine basalt (Porteous soils).

2. Strongly rolling to moderately steep colluvial slopes developed on dolerite and basaltic breccia.

3. Complex strongly rolling to moderately steep slopes with rippled or hummocky surfaces of slump earth�ow topography formed on Burnside and Abbotsford mudstones.

4. Steep to moderately steep basaltic hard rock slopes (Hammond Hill).

5. Isolated strongly rolling to steep basaltic hillocks.6. Smooth strongly rolling to rolling loess mantled

slopes developed on basalt.7. Complex rolling to strongly rolling slopes of

earth�ow topography formed largely on Burnside Formation mudstone.

8. Smooth rolling slopes on weathered basalt.9. Broken and slumped steep to moderately steep

slopes with steep to very steep basal sea cli�s cut into sedimentary strata.

10. Steep to moderately steep side slopes on basalt and basaltic colluvium.

11. Strongly rolling broken slopes underlain predominantly by basaltic breccia.

12. Rolling to strongly rolling sand dunes forming the sand spit south of Warrington.

13. Broken rolling to strongly rolling slopes of earth�ow topography developed predominantly on Concord Formation greensands.

14. Smooth rolling to strongly rolling slopes developed predominantly on Abbotsford mudstone.

15. Complex strongly rolling to moderately steep slope rippled or hummocky slopes of slump earth�ow topography formed predominantly on Abbotsford mudstone.

16. Smooth rolling slopes above a steep sea cli� and reef complex formed on phonolite.

Turbine

Volcanic landform components

Deposition landform components

location (25m radius)

Porteous Hill landform components Scale 1:20,000 @ A4

km1.00

12

10

11

7

8

9

16

13

14

15

6

3

4

55

12

Warrington

Omimi

Guilds HillHammond Hill

Blueskin Bay

Porteous Hill(401m)

SH1

Porteous28 September 2014Date Printed:

This map is a user generated static output from an Internet mapping site andis for reference only. Data layers that appear on this map may or may not be

accurate, current, or otherwise reliable.

THIS MAP IS NOT TO BE USED FOR NAVIGATION

Kilometers0.50

10,000SCALE 1:

Projection: NZGD_2000_New_Zealand_Transverse_Mercator

0.5

Legend

© CNES 2004-2010 / Spot Image

© GeographxCrown Copyright Reserved

Porteous

This map is a user generated static output from an Internet mapping site andis for reference only. Data layers that appear on this map may or may not be

accurate, current, or otherwise reliable.

THIS MAP IS NOT TO BE USED FOR NAVIGATION

Kilometers1.0

20,000

NZGD_2000_New_Zealand_Transverse_Mercator

Legend

© CNES 2004-2010 / Spot Image

© GeographxCrown Copyright Reserved

Landform Components

1. Rolling to easy rolling loess mantled slopes developed on olivine basalt (Porteous soils).

2. Strongly rolling to moderately steep colluvial slopes developed on dolerite and basaltic breccia.

3. Complex strongly rolling to moderately steep slopes with rippled or hummocky surfaces of slump earth�ow topography formed on Burnside and Abbotsford mudstones.

4. Steep to moderately steep basaltic hard rock slopes (Hammond Hill).

5. Isolated strongly rolling to steep basaltic hillocks.6. Smooth strongly rolling to rolling loess mantled

slopes developed on basalt.7. Complex rolling to strongly rolling slopes of

earth�ow topography formed largely on Burnside Formation mudstone.

8. Smooth rolling slopes on weathered basalt.9. Broken and slumped steep to moderately steep

slopes with steep to very steep basal sea cli�s cut into sedimentary strata.

10. Steep to moderately steep side slopes on basalt and basaltic colluvium.

11. Strongly rolling broken slopes underlain predominantly by basaltic breccia.

12. Rolling to strongly rolling sand dunes forming the sand spit south of Warrington.

13. Broken rolling to strongly rolling slopes of earth�ow topography developed predominantly on Concord Formation greensands.

14. Smooth rolling to strongly rolling slopes developed predominantly on Abbotsford mudstone.

15. Complex strongly rolling to moderately steep slope rippled or hummocky slopes of slump earth�ow topography formed predominantly on Abbotsford mudstone.

16. Smooth rolling slopes above a steep sea cli� and reef complex formed on phonolite.

Turbine

Volcanic landform components

Deposition landform components

location (25m radius)

Porteous Hill landform components Scale 1:20,000 @ A4

km1.00

12

10

11

7

8

9

16

13

14

15

6

3

4

55

12

Warrington

Omimi

Guilds HillHammond Hill

Blueskin Bay

Porteous Hill(401m)

SH1

Porteous28 September 2014Date Printed:

This map is a user generated static output from an Internet mapping site andis for reference only. Data layers that appear on this map may or may not be

accurate, current, or otherwise reliable.

THIS MAP IS NOT TO BE USED FOR NAVIGATION

Kilometers0.50

10,000SCALE 1:

Projection: NZGD_2000_New_Zealand_Transverse_Mercator

0.5

Legend

© CNES 2004-2010 / Spot Image

© GeographxCrown Copyright Reserved

Porteous

This map is a user generated static output from an Internet mapping site andis for reference only. Data layers that appear on this map may or may not be

accurate, current, or otherwise reliable.

THIS MAP IS NOT TO BE USED FOR NAVIGATION

Kilometers1.0

20,000

NZGD_2000_New_Zealand_Transverse_Mercator

Legend

© CNES 2004-2010 / Spot Image

© GeographxCrown Copyright Reserved

Landform Components

1. Rolling to easy rolling loess mantled slopes developed on olivine basalt (Porteous soils).

2. Strongly rolling to moderately steep colluvial slopes developed on dolerite and basaltic breccia.

3. Complex strongly rolling to moderately steep slopes with rippled or hummocky surfaces of slump earth�ow topography formed on Burnside and Abbotsford mudstones.

4. Steep to moderately steep basaltic hard rock slopes (Hammond Hill).

5. Isolated strongly rolling to steep basaltic hillocks.6. Smooth strongly rolling to rolling loess mantled

slopes developed on basalt.7. Complex rolling to strongly rolling slopes of

earth�ow topography formed largely on Burnside Formation mudstone.

8. Smooth rolling slopes on weathered basalt.9. Broken and slumped steep to moderately steep

slopes with steep to very steep basal sea cli�s cut into sedimentary strata.

10. Steep to moderately steep side slopes on basalt and basaltic colluvium.

11. Strongly rolling broken slopes underlain predominantly by basaltic breccia.

12. Rolling to strongly rolling sand dunes forming the sand spit south of Warrington.

13. Broken rolling to strongly rolling slopes of earth�ow topography developed predominantly on Concord Formation greensands.

14. Smooth rolling to strongly rolling slopes developed predominantly on Abbotsford mudstone.

15. Complex strongly rolling to moderately steep slope rippled or hummocky slopes of slump earth�ow topography formed predominantly on Abbotsford mudstone.

16. Smooth rolling slopes above a steep sea cli� and reef complex formed on phonolite.

Turbine

Volcanic landform components

Deposition landform components

location (25m radius)

Porteous Hill landform components Scale 1:20,000 @ A4

km1.00

12

10

11

7

8

9

16

13

14

15

6

3

4

55

12

Warrington

Omimi

Guilds HillHammond Hill

Blueskin Bay

Porteous Hill(401m)

SH1

Porteous28 September 2014Date Printed:

This map is a user generated static output from an Internet mapping site andis for reference only. Data layers that appear on this map may or may not be

accurate, current, or otherwise reliable.

THIS MAP IS NOT TO BE USED FOR NAVIGATION

Kilometers0.50

10,000SCALE 1:

Projection: NZGD_2000_New_Zealand_Transverse_Mercator

0.5

Legend

© CNES 2004-2010 / Spot Image

© GeographxCrown Copyright Reserved

Porteous

This map is a user generated static output from an Internet mapping site andis for reference only. Data layers that appear on this map may or may not be

accurate, current, or otherwise reliable.

THIS MAP IS NOT TO BE USED FOR NAVIGATION

Kilometers1.0

20,000

NZGD_2000_New_Zealand_Transverse_Mercator

Legend

© CNES 2004-2010 / Spot Image

© GeographxCrown Copyright Reserved

Landform Components

1. Rolling to easy rolling loess mantled slopes developed on olivine basalt (Porteous soils).

2. Strongly rolling to moderately steep colluvial slopes developed on dolerite and basaltic breccia.

3. Complex strongly rolling to moderately steep slopes with rippled or hummocky surfaces of slump earth�ow topography formed on Burnside and Abbotsford mudstones.

4. Steep to moderately steep basaltic hard rock slopes (Hammond Hill).

5. Isolated strongly rolling to steep basaltic hillocks.6. Smooth strongly rolling to rolling loess mantled

slopes developed on basalt.7. Complex rolling to strongly rolling slopes of

earth�ow topography formed largely on Burnside Formation mudstone.

8. Smooth rolling slopes on weathered basalt.9. Broken and slumped steep to moderately steep

slopes with steep to very steep basal sea cli�s cut into sedimentary strata.

10. Steep to moderately steep side slopes on basalt and basaltic colluvium.

11. Strongly rolling broken slopes underlain predominantly by basaltic breccia.

12. Rolling to strongly rolling sand dunes forming the sand spit south of Warrington.

13. Broken rolling to strongly rolling slopes of earth�ow topography developed predominantly on Concord Formation greensands.

14. Smooth rolling to strongly rolling slopes developed predominantly on Abbotsford mudstone.

15. Complex strongly rolling to moderately steep slope rippled or hummocky slopes of slump earth�ow topography formed predominantly on Abbotsford mudstone.

16. Smooth rolling slopes above a steep sea cli� and reef complex formed on phonolite.

Turbine

Volcanic landform components

Deposition landform components

location (25m radius)

Porteous Hill landform components Scale 1:20,000 @ A4

km1.00

12

10

11

7

8

9

16

13

14

15

6

3

4

55

12

Warrington

Omimi

Guilds HillHammond Hill

Blueskin Bay

Porteous Hill(401m)

SH1

Porteous28 September 2014Date Printed:

This map is a user generated static output from an Internet mapping site andis for reference only. Data layers that appear on this map may or may not be

accurate, current, or otherwise reliable.

THIS MAP IS NOT TO BE USED FOR NAVIGATION

Kilometers0.50

10,000SCALE 1:

Projection: NZGD_2000_New_Zealand_Transverse_Mercator

0.5

Legend

© CNES 2004-2010 / Spot Image

© GeographxCrown Copyright Reserved

Porteous

This map is a user generated static output from an Internet mapping site andis for reference only. Data layers that appear on this map may or may not be

accurate, current, or otherwise reliable.

THIS MAP IS NOT TO BE USED FOR NAVIGATION

Kilometers1.0

20,000

NZGD_2000_New_Zealand_Transverse_Mercator

Legend

© CNES 2004-2010 / Spot Image

© GeographxCrown Copyright Reserved

Landform Components

1. Rolling to easy rolling loess mantled slopes developed on olivine basalt (Porteous soils).

2. Strongly rolling to moderately steep colluvial slopes developed on dolerite and basaltic breccia.

3. Complex strongly rolling to moderately steep slopes with rippled or hummocky surfaces of slump earth�ow topography formed on Burnside and Abbotsford mudstones.

4. Steep to moderately steep basaltic hard rock slopes (Hammond Hill).

5. Isolated strongly rolling to steep basaltic hillocks.6. Smooth strongly rolling to rolling loess mantled

slopes developed on basalt.7. Complex rolling to strongly rolling slopes of

earth�ow topography formed largely on Burnside Formation mudstone.

8. Smooth rolling slopes on weathered basalt.9. Broken and slumped steep to moderately steep

slopes with steep to very steep basal sea cli�s cut into sedimentary strata.

10. Steep to moderately steep side slopes on basalt and basaltic colluvium.

11. Strongly rolling broken slopes underlain predominantly by basaltic breccia.

12. Rolling to strongly rolling sand dunes forming the sand spit south of Warrington.

13. Broken rolling to strongly rolling slopes of earth�ow topography developed predominantly on Concord Formation greensands.

14. Smooth rolling to strongly rolling slopes developed predominantly on Abbotsford mudstone.

15. Complex strongly rolling to moderately steep slope rippled or hummocky slopes of slump earth�ow topography formed predominantly on Abbotsford mudstone.

16. Smooth rolling slopes above a steep sea cli� and reef complex formed on phonolite.

Turbine

Volcanic landform components

Deposition landform components

location (25m radius)

Porteous Hill landform components Scale 1:20,000 @ A4

km1.00

12

10

11

7

8

9

16

13

14

15

6

3

4

55

12

Warrington

Omimi

Guilds HillHammond Hill

Blueskin Bay

Porteous Hill(401m)

SH1

Porteous28 September 2014Date Printed:

This map is a user generated static output from an Internet mapping site andis for reference only. Data layers that appear on this map may or may not be

accurate, current, or otherwise reliable.

THIS MAP IS NOT TO BE USED FOR NAVIGATION

Kilometers0.50

10,000SCALE 1:

Projection: NZGD_2000_New_Zealand_Transverse_Mercator

0.5

Legend

© CNES 2004-2010 / Spot Image

© GeographxCrown Copyright Reserved

Porteous

This map is a user generated static output from an Internet mapping site andis for reference only. Data layers that appear on this map may or may not be

accurate, current, or otherwise reliable.

THIS MAP IS NOT TO BE USED FOR NAVIGATION

Kilometers1.0

20,000

NZGD_2000_New_Zealand_Transverse_Mercator

Legend

© CNES 2004-2010 / Spot Image

© GeographxCrown Copyright Reserved

Landform Components

1. Rolling to easy rolling loess mantled slopes developed on olivine basalt (Porteous soils).

2. Strongly rolling to moderately steep colluvial slopes developed on dolerite and basaltic breccia.

3. Complex strongly rolling to moderately steep slopes with rippled or hummocky surfaces of slump earth�ow topography formed on Burnside and Abbotsford mudstones.

4. Steep to moderately steep basaltic hard rock slopes (Hammond Hill).

5. Isolated strongly rolling to steep basaltic hillocks.6. Smooth strongly rolling to rolling loess mantled

slopes developed on basalt.7. Complex rolling to strongly rolling slopes of

earth�ow topography formed largely on Burnside Formation mudstone.

8. Smooth rolling slopes on weathered basalt.9. Broken and slumped steep to moderately steep

slopes with steep to very steep basal sea cli�s cut into sedimentary strata.

10. Steep to moderately steep side slopes on basalt and basaltic colluvium.

11. Strongly rolling broken slopes underlain predominantly by basaltic breccia.

12. Rolling to strongly rolling sand dunes forming the sand spit south of Warrington.

13. Broken rolling to strongly rolling slopes of earth�ow topography developed predominantly on Concord Formation greensands.

14. Smooth rolling to strongly rolling slopes developed predominantly on Abbotsford mudstone.

15. Complex strongly rolling to moderately steep slope rippled or hummocky slopes of slump earth�ow topography formed predominantly on Abbotsford mudstone.

16. Smooth rolling slopes above a steep sea cli� and reef complex formed on phonolite.

Turbine

Volcanic landform components

Deposition landform components

location (25m radius)

Porteous Hill landform components Scale 1:20,000 @ A4

km1.00

12

10

11

7

8

9

16

13

14

15

6

3

4

55

12

Warrington

Omimi

Guilds HillHammond Hill

Blueskin Bay

Porteous Hill(401m)

SH1

Landform Components

3D Views from Google Earth

view from Blueskin Bay overlooking the site

view from Omimi overlooking the site

view from Warrington overlooking the site

(30m radius)

land typing

1.

2.

3.

4.

5.6.

7.

9.

12.

13.

14.

15.

8.

10.

11.

16.

Blueskin Energy Wind Cluster | Porteous Hill landscape assessment

page 11

Porteous28 September 2014Date Printed:

This map is a user generated static output from an Internet mapping site andis for reference only. Data layers that appear on this map may or may not be

accurate, current, or otherwise reliable.

THIS MAP IS NOT TO BE USED FOR NAVIGATION

Kilometers0.50

10,000SCALE 1:

Projection: NZGD_2000_New_Zealand_Transverse_Mercator

0.5

Legend

© CNES 2004-2010 / Spot Image

© GeographxCrown Copyright Reserved

Porteous

This map is a user generated static output from an Internet mapping site andis for reference only. Data layers that appear on this map may or may not be

accurate, current, or otherwise reliable.

THIS MAP IS NOT TO BE USED FOR NAVIGATION

Kilometers1.0

20,000

NZGD_2000_New_Zealand_Transverse_Mercator

Legend

© CNES 2004-2010 / Spot Image

© GeographxCrown Copyright Reserved

Landform Components

1. Rolling to easy rolling loess mantled slopes developed on olivine basalt (Porteous soils).

2. Strongly rolling to moderately steep colluvial slopes developed on dolerite and basaltic breccia.

3. Complex strongly rolling to moderately steep slopes with rippled or hummocky surfaces of slump earth�ow topography formed on Burnside and Abbotsford mudstones.

4. Steep to moderately steep basaltic hard rock slopes (Hammond Hill).

5. Isolated strongly rolling to steep basaltic hillocks.6. Smooth strongly rolling to rolling loess mantled

slopes developed on basalt.7. Complex rolling to strongly rolling slopes of

earth�ow topography formed largely on Burnside Formation mudstone.

8. Smooth rolling slopes on weathered basalt.9. Broken and slumped steep to moderately steep

slopes with steep to very steep basal sea cli�s cut into sedimentary strata.

10. Steep to moderately steep side slopes on basalt and basaltic colluvium.

11. Strongly rolling broken slopes underlain predominantly by basaltic breccia.

12. Rolling to strongly rolling sand dunes forming the sand spit south of Warrington.

13. Broken rolling to strongly rolling slopes of earth�ow topography developed predominantly on Concord Formation greensands.

14. Smooth rolling to strongly rolling slopes developed predominantly on Abbotsford mudstone.

15. Complex strongly rolling to moderately steep slope rippled or hummocky slopes of slump earth�ow topography formed predominantly on Abbotsford mudstone.

16. Smooth rolling slopes above a steep sea cli� and reef complex formed on phonolite.

Turbine

Volcanic landform components

Deposition landform components

location (25m radius)

Porteous Hill landform components Scale 1:20,000 @ A4

km1.00

12

10

11

7

8

9

16

13

14

15

6

3

4

55

12

Warrington

Omimi

Guilds HillHammond Hill

Blueskin Bay

Porteous Hill(401m)

SH1

land typing

Blueskin Energy Wind Cluster | Porteous Hill landscape assessment

page 12vegetation

800m6004002000

Scale: 1:25,000LegendVegetation

Exotic GrasslandHerbaceous(Wetlands)

Native ShrublandExotic Scrub

Native Forest turbinesExotic Forest

1

23

Slaughterhouse Bush

800m6004002000

Scale: 1:25,000LegendVegetation

Exotic GrasslandHerbaceous(Wetlands)

Native ShrublandExotic Scrub

Native Forest turbinesExotic Forest

1

23

Slaughterhouse Bush

source: Landcare Research, Our Environment website, LCBD4 June 2014

Blueskin Energy Wind Cluster | Porteous Hill landscape assessment

page 13house sites

139 Pryde Road

58 Reservoir Road110 Porteous Road

2100 Waikouaiti-Waitati Road

2142 Waikouaiti-Waitati Road

2197Waikouaiti-Waitati Road

22 Pryde Road 90 Pryde Road

2

2

3

LEGENDsite (24ha)

turbines

houses within 1.5 km of cluster

1

139 Pryde Road

58 Reservoir Road110 Porteous Road

2100 Waikouaiti-Waitati Road

2142 Waikouaiti-Waitati Road

2197Waikouaiti-Waitati Road

22 Pryde Road 90 Pryde Road

2

2

3

LEGENDsite (24ha)

turbines

houses within 1.5 km of cluster

1

139 Pryde Road

58 Reservoir Road110 Porteous Road

2100 Waikouaiti-Waitati Road

2142 Waikouaiti-Waitati Road

2197Waikouaiti-Waitati Road

22 Pryde Road 90 Pryde Road

2

2

3

LEGENDsite (24ha)

turbines

houses within 1.5 km of cluster

1

Blueskin Energy Wind Cluster | Porteous Hill landscape assessment

page 14alternative sites considered

source: Google Earth, aerial dated 2013

north