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Geological Formation

Stac Pollaidh

Inselbergs and Crystalline Monoliths

Stac Pollaidh is a mountain in the Northwest Highlands of Scotland, its rocky crest built of Torridonian sandstone and carved into numerous pinnacles and steep gullies. During the last Ice Age its ridge stood above the surrounding ice sheet as a nunatak, while glacial movement smoothed the flanks below. It reaches 612 meters with a topographic prominence of nearly 440 meters, and its name blends the Norse word for pool river with Scottish Gaelic usage.

Facts
Classification
Protected Status
National Park or Reserve 1
Protected Status
International Treaty Protected Area 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: Stac Pollaidh

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: Stac Pollaidh
In the Other Atlases

Found In

Also in Geography Atlas: where this subject is found.

Source Wikidata: Stac Pollaidh
Sources
1. UNEP-WCMC and IUCN, World Database on Protected Areas: WDPA protected areas at the location of Stac Pollaidh
UNEP-WCMC and IUCN, World Database on Protected Areas
  • WDPA feature: Assynt - Coigach
    "desig_eng": "National Scenic Area"
  • WDPA feature: Inverpolly
    "desig_eng": "Emerald Network"
View the Source
Wikidata: Stac Pollaidh
Wikidata Q3396239, class allow-list match (w-wdresolver-0926)View the Source
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