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Geological Formation

Sarn Badrig

Coastal and Reef Features

Sarn Badrig, also spelled Sarn Padrig, is one of several roughly parallel shingle reefs extending under the sea in Cardigan Bay off the west coast of Wales. The causeway is made of glacial deposits left behind by receding ice sheets at the end of the last ice age. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/

Connections

Caused By

Sedimentation, Processes

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

Source Wikidata: Sarn Badrig

In Discipline

Oceanography, Disciplines

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

Source Wikidata: Sarn Badrig
In the Other Atlases
Sources
Sarn Badrig (Wikipedia)
Lead section
Quote, Lead section
Sarn Badrig, also spelled Sarn Padrig (Welsh for 'St. Patrick's causeway'), is one of several more or less parallel shingle reefs extending under the sea in Cardigan Bay on the west coast of Wales.
View the Source
Wikidata: Sarn Badrig
Wikidata Q7424321, class allow-list match (w-wdresolver-0926)View the Source
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