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 StatusLocally or Regionally Protected 1 Connections
Associated With
Source Beinn Eighe (Wikipedia)
Source Beinn Eighe (Wikipedia)
Caused By
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
In the Other Atlases
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
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.
Associated With: Quartzite, Lead paragraph
Unlike most other hills in the area it has a cap of Cambrian basal quartzite which gives the peaks of Beinn Eighe a distinctive light colour.
Associated With: Cambrian, Lead, age Cambrian
Unlike most other hills in the area it has a cap of Cambrian basal quartzite which gives the peaks of Beinn Eighe a distinctive light colour.
Associated With: Quartzite, Lead, rock Quartzite
Unlike most other hills in the area it has a cap of Cambrian basal quartzite which gives the peaks of Beinn Eighe a distinctive light colour.
Associated With: Sandstone, Article text, rock Sandstone
The younger Precambrian Torridonian Sandstone, which sits on top of the gneiss, forms the bulk of all of the Torridon Hills, including Beinn Eighe, and was formed around 800 million years ago from the sediment of rivers that flowed across the landscape of the gneiss.
View the SourceWikidata: Beinn Eighe
Wikidata Q3396296, class allow-list match (w-wdresolver-0926)View the Source Reader Challenges (0)
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