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Geological Formation

Beinn Eighe

Inselbergs and Crystalline Monoliths

Beinn Eighe is a mountain massif in the Torridon area of Wester Ross, in Scotland's Northwest Highlands, south of Loch Maree, with its highest point, Ruadh-stac Mor, reaching 1,010 meters. Like its neighbors it stands on a foundation of ancient Lewisian gneiss overlaid by Precambrian Torridonian sandstone, but its summit ridge is capped by pale Cambrian quartzite, laid down around 540 million years ago as pure white sand under a warm tropical sea. That hard, brittle cap gives Beinn Eighe's peaks a distinctive light color that can be mistaken for snow, setting it apart from the darker sandstone summits around it.

Facts
Classification
Protected Status
Locally or Regionally Protected 1
Connections

Caused By

Orogeny, Processes

Wikidata P31 formation-type mapped to formative process Orogeny via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Beinn Eighe

In Discipline

Wikidata P31 formation-type mapped to discipline Geomorphology via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Beinn Eighe
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Found In

Also in Geography Atlas: where this subject is found.

Source Wikidata: Beinn Eighe
Sources
1. Beinn Eighe (Wikipedia)
Wikipedia article lead, protection designation
Quote, Wikipedia article lead, protection designation
ography has made it popular with both hillwalkers and climbers and the national nature reserve on its northern side makes it an accessible mountain for all visitors.
View the Source
Wikidata: Beinn Eighe
Wikidata Q3396296, class allow-list match (w-wdresolver-0926)View the Source
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