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Robinson, Brett H.; Brooks, Robert R.; Kirkman, John H.; Gregg, Paul E.H.; Gremigni, Patrizia (1996). "Plant‐available elements in soils and their influence on the vegetation over ultramafic ("serpentine") rocks in New
Zealand".
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which forms the mountain. Ultramafic Rock weathers to this colour and plant growth is also stunted due to the soils high heavy metal content. The ultramafic rock formed in the Earth's
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McLintock, Alexander Hare; George
William Grindley, M. SC; Taonga, New Zealand Ministry for Culture and Heritage Te Manatu.
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was first identified on the mountain and named after it. Between 1850 and 1865 small deposits of
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were mined on the mountain leading to the building of New
Zealand's
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An encyclopaedia of New
Zealand, edited by A. H. McLintock, 1966
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This mountain, mountain range, or peak related article is a
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is a mountain in the
Richmond Range near the city of
298:History of mining on Dun Mountain (M. R. Johnston)
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243:Geological Society, London, Special Publications
88:. It is located between the catchments of the
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153:"Dun Mountain Trail gets government funding"
288:New Zealand Encyclopedia 1966: Dun Mountain
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100:. The mountain is named for its brown (
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112:in the Permian and is now part of the
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322:. You can help Knowledge by
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86:South Island
71:Dun Mountain
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63:New Zealand
363:Categories
187:2019-02-06
162:2019-02-06
139:References
271:129776536
224:0303-6758
50:Geography
41:Elevation
125:chromite
55:Location
251:Bibcode
90:Pelorus
77:in the
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129:copper
121:dunite
110:mantle
94:Maitai
75:Nelson
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