Fforest (Carmarthenshire)
Encyclopedia
Fforest is the name applied to a small upland area adjoining the Vale of Towy, some 4 km north of the town of Llandovery
in Carmarthenshire
, Wales
. Stretching for a distance of 4 km from southwest to northeast the area rises to two separate summits either side of a broad saddle; one at 297m in the south and a second one to the northeast crowned by a triangulation pillar which attains a height of 341m. The ridge is privately owned hence there is no public access to any part of it though it is encircled by public roads and paths. The hills are formed from silty grey mudstone
s of uppermost/latest Ordovician
age ascribed to the Yr Allt Formation.
Llandovery
Llandovery is a market town in Carmarthenshire, Wales, lying on the River Tywi and the A40 road.The town is served by Llandovery railway station, where there is a park and ride to Llanelli and Shrewsbury via the Heart of Wales Line...
in Carmarthenshire
Carmarthenshire
Carmarthenshire is a unitary authority in the south west of Wales and one of thirteen historic counties. It is the 3rd largest in Wales. Its three largest towns are Llanelli, Carmarthen and Ammanford...
, Wales
Wales
Wales is a country that is part of the United Kingdom and the island of Great Britain, bordered by England to its east and the Atlantic Ocean and Irish Sea to its west. It has a population of three million, and a total area of 20,779 km²...
. Stretching for a distance of 4 km from southwest to northeast the area rises to two separate summits either side of a broad saddle; one at 297m in the south and a second one to the northeast crowned by a triangulation pillar which attains a height of 341m. The ridge is privately owned hence there is no public access to any part of it though it is encircled by public roads and paths. The hills are formed from silty grey mudstone
Mudstone
Mudstone is a fine grained sedimentary rock whose original constituents were clays or muds. Grain size is up to 0.0625 mm with individual grains too small to be distinguished without a microscope. With increased pressure over time the platey clay minerals may become aligned, with the...
s of uppermost/latest Ordovician
Ordovician
The Ordovician is a geologic period and system, the second of six of the Paleozoic Era, and covers the time between 488.3±1.7 to 443.7±1.5 million years ago . It follows the Cambrian Period and is followed by the Silurian Period...
age ascribed to the Yr Allt Formation.