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Linn (geology)







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From Wikipedia, the free encyclopedia
 

(Redirected from Linn (geography))

Linn of Dee

InScotland and northern England, a Linn is a geographical water feature, a watercourse that has cut through a shelf of hard rock creating a narrow (usually), steep-sided crevice (fracture) through which it runs.

Typically one named after a river or area can have application even for more than one such feature.

The photograph of the Linn of Dee illustrates the attributes of a typical 'Linn'.

InGordon (1925) the author describing a walk down Glen Avon in the Cairngorms mentions two Linns on the River Avon - first:

A couple of miles below Faindouran Lodge the A'an is spanned by a bridge. Here the river is narrow, with foaming rapids and deep pools where salmon lie of a September day. Beside the Linn, on the damp granite ledges ...

— Gordon (1925) (p61)

Second:

At the Linn beside Inchrory the A'an thundered through its rocky gorge. Before midsummer salmon and grilse reach the deep pools of the Linn ...

— Gordon (1925) (p62-63)

A linn may also refer to a waterfall or a pool at the foot of a waterfall,[1] with the derivation a confusion of Scots Gaelic linne (pool) and Old English hlynn (torrent).[1]

Sources[edit]

References[edit]

Gazetteer for Scotland "Glossary:L". Retrieved 2 January 2008. England's Rock Art - Roughting Linn, Northumberland

Notes:


Retrieved from "https://en.wikipedia.org/w/index.php?title=Linn_(geology)&oldid=1227392571"

Categories: 
Fluvial landforms
Geography of Scotland
Geography of England
Hidden category: 
Articles containing Old English (ca. 450-1100)-language text
 



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