About: Garnedd-Wen Formation     Goto   Sponge   NotDistinct   Permalink

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The Garnedd-Wen Formation (also known as the Garnedd-Wen Beds) is an Ordovician lithostratigraphic group (a sequence of rock strata) in Mid Wales. The rock of the formation is a mixture of mudstones, siltstones, fine- to coarse-grained sandstones, greywackes and conglomerates. The formation extends from Dinas Mawddwy in the north-east to Tywyn in the south-west.

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  • Garnedd-Wen Formation (en)
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  • The Garnedd-Wen Formation (also known as the Garnedd-Wen Beds) is an Ordovician lithostratigraphic group (a sequence of rock strata) in Mid Wales. The rock of the formation is a mixture of mudstones, siltstones, fine- to coarse-grained sandstones, greywackes and conglomerates. The formation extends from Dinas Mawddwy in the north-east to Tywyn in the south-west. (en)
name
  • Garnedd-Wen Formation (en)
geo:lat
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foaf:depiction
  • http://commons.wikimedia.org/wiki/Special:FilePath/Tarren_y_Gesail_-_geograph.org.uk_-_736726.jpg
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  • Abercorris Group (en)
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  • The upper slopes of Tarren y Gesail are primarily in the Garnedd-Wen Formation (en)
country
  • Wales (en)
period
  • Ordovician (en)
region
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  • to (en)
type
georss:point
  • 52.6354 -3.9071
has abstract
  • The Garnedd-Wen Formation (also known as the Garnedd-Wen Beds) is an Ordovician lithostratigraphic group (a sequence of rock strata) in Mid Wales. The rock of the formation is a mixture of mudstones, siltstones, fine- to coarse-grained sandstones, greywackes and conglomerates. The formation extends from Dinas Mawddwy in the north-east to Tywyn in the south-west. (en)
extent
  • Tywyn to Dinas Mawddwy (en)
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otherlithology
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prilithology
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  • POINT(-3.9070999622345 52.635398864746)
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