The Cwm Pennant Fault is a SSW-NNE trending normal fault system in North Wales. It forms part of the structures that bound the Snowdon graben. The main faults of the Cwm Pennant fault system throw down to the east. [1]
See also
References
- ^ Kokelaar, P. (1992). "Ordovician marine volcanic and sedimentary record of rifting and volcanotectonism: Snowdon, Wales, United Kingdom". Geological Society of America Bulletin. 104 (11): 1433–1455. doi: 10.1130/0016-7606(1992)104<1433:OMVASR>2.3.CO;2. Retrieved 18 December 2010.
52°58′N 4°13′W / 52.97°N 4.21°W
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The Cwm Pennant Fault is a SSW-NNE trending normal fault system in North Wales. It forms part of the structures that bound the Snowdon graben. The main faults of the Cwm Pennant fault system throw down to the east. [1]
See also
References
- ^ Kokelaar, P. (1992). "Ordovician marine volcanic and sedimentary record of rifting and volcanotectonism: Snowdon, Wales, United Kingdom". Geological Society of America Bulletin. 104 (11): 1433–1455. doi: 10.1130/0016-7606(1992)104<1433:OMVASR>2.3.CO;2. Retrieved 18 December 2010.
52°58′N 4°13′W / 52.97°N 4.21°W
|
| This article about a specific United Kingdom geological feature is a stub. You can help Wikipedia by expanding it. |
|
| This article about a location in Wales is a stub. You can help Wikipedia by expanding it. |