File:Kinharvie Burn with Auchengray Hill in the background - geograph.org.uk - 714365.jpg
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Kinharvie_Burn_with_Auchengray_Hill_in_the_background_-_geograph.org.uk_-_714365.jpg (640 × 480 pixels, file size: 103 KB, MIME type: image/jpeg)
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DescriptionKinharvie Burn with Auchengray Hill in the background - geograph.org.uk - 714365.jpg |
English: Kinharvie Burn with Auchengray Hill in the background From an internet source: The Criffel Hills and Kinharvie Burn itself were well known to the Scottish mineralogists of the 19th century. In particular, Jameson, Dudgeon and Heddle all published localities for sphene and allanite for which the area is famous. They were also aware of the occurrence of manganese minerals which were very difficult to analyse at that time. Modern analytical techniques have shown that the 'psilomelane' of Kinharvie Burn is romanèchite and this is only the third confirmed Scottish locality. |
Date | |
Source | From geograph.org.uk |
Author | Darrin Antrobus |
Attribution (required by the license) InfoField | Darrin Antrobus / Kinharvie Burn with Auchengray Hill in the background / |
InfoField | Darrin Antrobus / Kinharvie Burn with Auchengray Hill in the background |
Camera location | 54° 58′ 25″ N, 3° 40′ 42″ W | View this and other nearby images on: OpenStreetMap | 54.973640; -3.678400 |
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Object location | 54° 58′ 27″ N, 3° 40′ 42″ W | View this and other nearby images on: OpenStreetMap | 54.974270; -3.678400 |
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This image was taken from the Geograph project collection. See this photograph's page on the Geograph website for the photographer's contact details. The copyright on this image is owned by Darrin Antrobus and is licensed for reuse under the Creative Commons Attribution-ShareAlike 2.0 license.
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Attribution: Darrin Antrobus
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current | 01:39, 19 February 2011 | 640 × 480 (103 KB) | GeographBot (talk | contribs) | == {{int:filedesc}} == {{Information |description={{en|1=Kinharvie Burn with Auchengray Hill in the background From an internet source: The Criffel Hills and Kinharvie Burn itself were well known to the Scottish mineralogists of the 19th century. In part |
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