File:Loch Kinord - geograph.org.uk - 903441.jpg

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English: Loch Kinord Loch Kinord and the nearby Loch Davan were both formed when the last glaciers melted here more than 10.000 years ago. They are textbook examples of kettle holes. These were formed when large blocks of ice became separated from the melting glacier and were buried by sand and gravel. When that ice finally melted, the sand and gravel that once lay on top of the ice collapsed, leaving a hollow (kettle hole) on the ground surface which later filled with water. The lochs are relatively shallow. Loch Kinord has an average depth of about 2 metres. The shallow depth means that light can penetrate to the loch floor. Consequently, the loch has a rich flora with many species of aquatic plants recorded.
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Source From geograph.org.uk
Author Nigel Corby
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Nigel Corby / Loch Kinord / 
Nigel Corby / Loch Kinord
Camera location57° 05′ 06″ N, 2° 55′ 12″ W  Heading=180° Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo
Object location57° 04′ 59″ N, 2° 55′ 11″ W  Heading=180° Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo

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This file is licensed under the Creative Commons Attribution-Share Alike 2.0 Generic license.
Attribution: Nigel Corby
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current19:57, 21 February 2011Thumbnail for version as of 19:57, 21 February 2011640 × 427 (89 KB)GeographBot (talk | contribs)== {{int:filedesc}} == {{Information |description={{en|1=Loch Kinord Loch Kinord and the nearby Loch Davan were both formed when the last glaciers melted here more than 10.000 years ago. They are textbook examples of kettle holes. These were formed when

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