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Geological Formation

Isles of Scilly

Islands and Archipelagos

The Isles of Scilly are a small archipelago off the southwestern tip of Cornwall, England, in the United Kingdom. One of the islands, St Agnes, lies more than four miles further south than Lizard Point, the southernmost point of the British mainland, and holds Troy Town, the UK's southernmost inhabited settlement. The archipelago had a population of about 2,100 at the 2021 census, concentrated mainly on St Mary's, and has held its own local authority, the Council of the Isles of Scilly, since 1890.

Facts
Classification
Protected Status
National Park or Reserve 1
Connections

Associated With

Granite, Materials
Source Isles of Scilly (Wikipedia)
Permian, Eras
Source Isles of Scilly (Wikipedia)

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: Isles of Scilly
In the Other Atlases

Found In

Also in Geography Atlas: where this subject is found.

Source Wikidata: Isles of Scilly
Sources
1. Wikidata: Isles of Scilly
  • Wikidata Q180209, class allow-list match (w-wdresolver-0926)
  • Wikidata P1435 heritage-designation or P3425 Natura 2000 claim on the formation's own item (w-bbfill-earth2-0926)
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Isles of Scilly (Wikipedia)
  • Lead section
    The Isles of Scilly (, SIL-ee; Cornish: Syllan) are a small archipelago in Cornwall, England, approximately 45 km (28 mi) south-west of Land's End. One of the islands, St Agnes, is over four miles (six kilometres) further south than the most southerly point of the British mainland at Lizard Point, and has the southernmost inhabited settlement in Cornwall and the UK, Troy Town.
  • Associated With: Permian, Article text, age Permian
    All the islands of Scilly are all composed of granite rock of Early Permian age, an exposed part of the Cornubian batholith.
  • Associated With: Granite, Article text, rock Granite
    All the islands of Scilly are all composed of granite rock of Early Permian age, an exposed part of the Cornubian batholith.
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