Cam Loch, Sutherland
| Cam Loch, Sutherland | |
|---|---|
 Looking from Suilven, past the middle summit of Meall Meadhonach to Cam Loch in the distance. | |
  Cam Loch, Sutherland Location in Sutherland | |
| Location | NC21331348 |
| Coordinates | 58°04′26″N 5°01′51″W / 58.0740°N 5.0308°WCoordinates: 58°04′26″N 5°01′51″W / 58.0740°N 5.0308°W |
| Type | freshwater loch |
| Primary inflows | |
| Primary outflows | |
| Max. length | 4.18 km (2.60 mi)[1] |
| Max. width | 0.917 km (0.570 mi)[1] |
| Surface area | 253 ha (630 acres)[2] |
| Average depth | 38 ft (12 m)[1] |
| Max. depth | 122 ft (37 m)[1] |
| Water volume | 1,025,740,415.89 cu ft (29,045,734.000 m3)[1] |
| Shore length1 | 17 km (11 mi) [2] |
| Surface elevation | 124 m (407 ft)[2] |
| Max. temperature | 56.2 °F (13.4 °C) |
| 1 Shore length is not a well-defined measure. | |
Cam Loch (the crooked loch)[3] is an irregularly-shaped freshwater loch, about 5 km long, on a north-west to south-east orientation, located slightly north of the village of Elphin, in the Assynt district of Sutherland, Scotland.[1][2][4] The loch is located in an area along with neighbouring Coigach, as the Assynt-Coigach National Scenic Area,[5] one of 40 such areas in Scotland.[6]
Geography[]
Located immediately to the south-west of Cam Loch, and at a slightly lower level, is Loch Veyatie, which is roughly parallel to it.[4] The two lochs are connected by Abhainn Mhòr, which consists of extensions of the two lochs with a waterfall between them. The loch is overlooked by the twin peaks of Cùl Mòr at 849m to the south-west. Directly south of the loch is Canisp at 847m. To the south-east, is the steep-sides ridge that forms the mountain of Suilven at 723m. Cam Loch sits in an area of wilderness landscape of moorland, bogs, and lochs and lochans. It is an area that holds several large lochs, for example the irregular-shaped , directly to the west.
Cam Loch is fed by inflows from Loch Urigill and Loch Borralan via the River Ledbeg.[7] The loch drains via Abhainn Mhòr, into Loch Veyatie, that is part of the Fionn Loch Drainage System, that drains into , that in turn is drained by the into the sea.[7]
Interglacial site[]
Cam Loch is internationally important as one of the most intensively studied late glacial sites in Scotland, in studies by members of the Freshwater Biological Association.[8] It is a reference site for the stratigraphy of the late glacial in north-west Scotland and used to compare paleoecological research with sites elsewhere in the United Kingdom and Western Europe.[8] The sediments preserved on the loch bed are important for reconstructing the late glacial period between 13000 and 10000 BP.[8] The evidence provided by the sediment shows a rapid and marked climatic change during that period.[8] Due to richness of the evidence, the loch has been intensively studied over the years.[8] The sediments have been studied for their inorganic and organic geochemistry, pollen stratigraphy and diatom stratigraphy.[8]
Bibliography[]
Inorganic geochemistry[]
- Pennington, Winifred; Sackin, M. J. (September 1975). "I. Numerical Analysis". New Phytologist. 75 (2): 419–453. doi:10.1111/j.1469-8137.1975.tb01405.x.
- Pennington, Winifred (October 1975). "A chronostratigraphic comparison of Late-Weichselian and Late-Devensian subdivisions, illustrated by two radiocarbon-dated profiles from western Britain". Boreas. 4 (3): 157–171. doi:10.1111/j.1502-3885.1975.tb00687.x.
- Pennington, W. (1977). "Lake Sediments and the Lateglacial Environment in Northern Scotland". Studies in the Scottish Lateglacial Environment: 119–141. doi:10.1016/B978-0-08-020498-7.50013-3. ISBN 9780080204987.
Organic geochemistry[]
- Cranwell, P.A. (September 1981). "Diagenesis of free and bound lipids in terrestrial detritus deposited in a lacustrine sediment". Organic Geochemistry. 3 (3): 79–89. doi:10.1016/0146-6380(81)90002-4.
- Cranwell, P.A. (1977). "Organic geochemistry of Cam Loch (Sutherland) sediments". Chemical Geology. 20: 205–221. Bibcode:1977ChGeo..20..205C. doi:10.1016/0009-2541(77)90044-4.
- Pennington, W. (1977). "Lake Sediments and the Lateglacial Environment in Northern Scotland". Studies in the Scottish Lateglacial Environment: 119–141. doi:10.1016/B978-0-08-020498-7.50013-3. ISBN 9780080204987.
Pollen stratigraphy[]
- Pennington, Winifred (October 1975). "A chronostratigraphic comparison of Late-Weichselian and Late-Devensian subdivisions, illustrated by two radiocarbon-dated profiles from western Britain". Boreas. 4 (3): 157–171. doi:10.1111/j.1502-3885.1975.tb00687.x.
- Pennington, W. (1977). "Lake Sediments and the Lateglacial Environment in Northern Scotland". Studies in the Scottish Lateglacial Environment: 119–141. doi:10.1016/B978-0-08-020498-7.50013-3. ISBN 9780080204987.
Diatom stratigraphy[]
- Haworth, Elizabeth Y. (July 1976). "Two Late-Glacial (Late Devensian) Diatom Assemblage Profiles from Northern Scotland". The New Phytologist. Wiley. 77 (1): 227–256. doi:10.1111/j.1469-8137.1976.tb01516.x. JSTOR 2433656.
- Pennington, W. (1977). "Lake Sediments and the Lateglacial Environment in Northern Scotland". Studies in the Scottish Lateglacial Environment: 119–141. doi:10.1016/B978-0-08-020498-7.50013-3. ISBN 9780080204987.
Gallery[]
- Images of Cam Loch and surrounding areas
The Cam Loch Looking across the southern part of the Loch. Cul Mor is in the distance on the right, with Cul Beag and Ben More Coigach on the left.
Cam Loch From the Lochinver/Ledmore path with Suilven in the background.
The Cam Loch Looking across the broad middle part of the loch, from where the Elphin to Lochinver path leaves the loch and heads inland. Cul Mor is beyond.
Cam Loch. From path to Suilven from Elphin.
View over Cam Loch towards Suilven
References[]
- ^ a b c d e f John, Murray; Lawrence, Pullar. Bathymetrical Survey of the Fresh-Water Lochs of Scotland, 1897–1909 Lochs of the Kirkaig Basin Volume II – Cam Loch. National Library of Scotland. p. 161. Retrieved 20 January 2022.
This article incorporates text from this source, which is in the public domain.
- ^ a b c d "Cam Loch". Centre for Ecology and Hydrology. Scotland and Northern Ireland Forum for Environmental Research (SNIFFER). Retrieved 20 January 2022.
- ^ The New Statistical Account of Scotland: Sutherland, Caithness, Orkney, Shetland, General index. Vol. XV. Edinburgh, London: W. Blackwood and Sons. 1845. p. 107.
- ^ a b Gittings, Bruce; Munro, David. "Cam Loch". The Gazetteer for Scotland. School of GeoSciences, University of Edinburgh and The Royal Scottish Geographical Society. Retrieved 21 January 2022.
- ^ "Assynt-Coigach National Scenic Area". NatureScot. Retrieved 2 October 2020.
- ^ "National Scenic Areas". NatureScot. Retrieved 2 October 2020.
- ^ a b Yu, Ge (1995). Lake Status Records from Europe: Data Base Documentation. World Data Center-A for Paleoclimatology, NOAA Paleoclimatology Program. p. 262.
- ^ a b c d e f Birks, H.J.B. (6 December 2012). "Cam Loch". In Gordon, J. E.; Sutherland, D. G. (eds.). Quaternary of Scotland. Springer Science & Business Media. p. 134. ISBN 978-94-011-1500-1.
This article incorporates text from this source, which is in the - Freshwater lochs of Scotland
- Kirkaig Basin
- Sites of Special Scientific Interest in Scotland