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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)
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- The upper slopes of Tarren y Gesail are primarily in the Garnedd-Wen Formation (en)
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- Tywyn to Dinas Mawddwy (en)
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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)
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- Garnedd-Wen Formation (en)
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- POINT(-3.9070999622345 52.635398864746)
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