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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/

Facts
Classification
Protected Status
International Treaty Protected Area 1
Connections

Caused By

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

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

Found In

Also in Geography Atlas: where this subject is found.

Source Wikidata: Sarn Badrig
Sources
1. UNEP-WCMC and IUCN, World Database on Protected Areas: WDPA protected areas at the location of Sarn Badrig
UNEP-WCMC and IUCN, World Database on Protected AreasWDPA feature: Pen Llŷn a`r Sarnau/ Lleyn Peninsula and the Sarnau
Quote, WDPA feature: Pen Llŷn a`r Sarnau/ Lleyn Peninsula and the Sarnau
"desig_eng": "Emerald Network"
View the Source
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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