Knowledge (XXG)

Fan Llia

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285:. Its southernmost slopes (around Cefn Perfedd) are formed in Plateau Beds Formation sandstones and an area in the north-east is underlain by sandstones and mudstones of the Senni Beds Formation. Rock exposures are infrequent − the hill being draped with glacial till and accumulations of peat. The most significant feature is a post-glacial landslip which extends from near the summit of Fan Dringarth down its eastern slopes almost to the 31: 254:
The hill has the form of a broad ridge aligned south-south-west to north-north-east peaking at an altitude of 632 m. It has a subsidiary top to the north which is known as
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Nuttall, John & Anne (1999). The Mountains of England & Wales - Volume 1: Wales (2nd edition ed.). Milnthorpe, Cumbria: Cicerone.
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and which may be responsible for the name of this subsidiary peak. Craig Cwm-du to the north hosted a small glacier in the ice age.
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and to the east by streams flowing into the Afon Dringarth, part of which has been impounded directly to the east of the hill as
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and which attains a height of 617 m. Its broad northern ridge is eventually truncated by the cliffs of Craig Cwm-du.
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car park at Blaen Llia (OS grid ref SN 926165) just off the minor road between the villages of
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British Geological Survey 1:50,000 map sheet 231 'Merthyr Tydfil' & accompanying memoir
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The hill is formed largely from sandstones of the Brownstones Formation of the
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Ordnance Survey Explorer map OL12 'Brecon Beacons National Park: western area'
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The hill is drained to the west by a number of streams flowing into the
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designated in 2005 in recognition of the area's geological heritage.
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The entire hill is designated as open country so walkers may
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interest are to be found on its flanks including several
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Index


Elevation
Prominence
Parent peak
Fan Fawr
Listing
HuMP
Hewitt
Nuttall
Coordinates
51°51′22″N 3°32′35″W / 51.8561°N 3.5430°W / 51.8561; -3.5430
Llia
Welsh
Powys
Wales
Parent range
Brecon Beacons
OS grid
SN937186
Topo map
OS
Fan Fawr
Fforest Fawr
Brecon Beacons National Park
Wales
Powys
archaeological
house platforms
Old Red Sandstone
Devonian period

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