File:Linn of Tummel - geograph.org.uk - 835865.jpg

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Linn_of_Tummel_-_geograph.org.uk_-_835865.jpg (640 × 480 pixels, file size: 92 KB, MIME type: image/jpeg)

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English: Linn of Tummel Though still a spectacular waterfall today, the water flow was tempered somewhat with the completion of the hydro-electric scheme in the Tummel area in 1950. The volume of water flowing down the River Tummel was reduced when the majority of the flow was diverted through a pipe connecting the eastern end of Loch Tummel with the Clunie Power Station, and with the construction of the artificial Loch Faskally immediately below the Falls, the water level at this point rose.
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Source From geograph.org.uk
Author Euan Nelson
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Euan Nelson / Linn of Tummel / 
Euan Nelson / Linn of Tummel
Camera location56° 43′ 05″ N, 3° 47′ 01″ W  Heading=337° Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo
Object location56° 43′ 05″ N, 3° 47′ 00″ W  Heading=337° 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: Euan Nelson
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Under the following conditions:
  • attribution – You must give appropriate credit, provide a link to the license, and indicate if changes were made. You may do so in any reasonable manner, but not in any way that suggests the licensor endorses you or your use.
  • share alike – If you remix, transform, or build upon the material, you must distribute your contributions under the same or compatible license as the original.

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current19:45, 20 February 2011Thumbnail for version as of 19:45, 20 February 2011640 × 480 (92 KB)GeographBot (talk | contribs)== {{int:filedesc}} == {{Information |description={{en|1=Linn of Tummel Though still a spectacular waterfall today, the water flow was tempered somewhat with the completion of the hydro-electric scheme in the Tummel area in 1950. The volume of water flow

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