place

Aber Dinlle Fault

Geology of GwyneddUnited Kingdom geology stubsWales geography stubs

The Aber Dinlle Fault is a SW-NE trending fault in North Wales. It forms part of the Menai Strait Fault System, with the Berw and Dinorwic Faults. It lies close to the epicentre of the 1984 Llŷn Peninsula earthquake, although it is not thought to have been responsible for that event. The fault was active during deposition of Ordovician rocks in the Welsh Basin. It was reactivated as a normal fault in the Carboniferous with a downthrow to the northwest and again reactivated as a reverse fault during Late Carboniferous inversion associated with the Variscan Orogeny.

Excerpt from the Wikipedia article Aber Dinlle Fault (License: CC BY-SA 3.0, Authors).

Aber Dinlle Fault
A4244,

Geographical coordinates (GPS) Address Nearby Places
placeShow on map

Wikipedia: Aber Dinlle FaultContinue reading on Wikipedia

Geographical coordinates (GPS)

Latitude Longitude
N 53.18 ° E -4.13 °
placeShow on map

Address

A4244
LL57 4UU , Pentir
Wales, United Kingdom
mapOpen on Google Maps

Share experience

Nearby Places

Mynydd Llandygai
Mynydd Llandygai

Mynydd Llandygái (also spelt Mynydd Llandegai, [ˌmənɨðˌɬandəˈɡai] ; from Welsh mynydd "mountain", Llandygai "Church of St Tegai") is a small, partly forested hill in Gwynedd, North Wales. It forms the start of the Glyderau ridge. It is also the name of the quarry village at the base of the hill situated at the edge of Snowdonia National Park at grid reference SH600656. The village lies at about 1,000 feet (300 m) above sea level and gets strong winds and above average rainfall. Many of the houses are spread along long roads rather than clustered around a point, giving the village a somewhat decentralised feel. However the village is distinguished by two parallel rows of semi-detached quarrymen's cottages constructed during the 19th century for workers of Penrhyn Quarry, which mined slate. The first mention of housing on the site can be found in the census of 1841. Each of the houses was provided with an area of land (approximately 1 acre) sufficient to feed the family. This arrangement is clearly visible on the map of the area. This can be contrasted with the situation in the South Wales coalfields or in the industrial Midlands where no such provision was made for the workers. Originally named Douglas Hill, the name was changed in the 1930s after the inhabitants decided that they did not want to associate with the name Douglas, namely part of the Penrhyn family surname. (See Baron Penrhyn.) Physically the village has changed little since it was originally built. The area to the south is mountainous and there are a number of slate and stone quarries in the vicinity.