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Fan Bwlch Chwyth

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The entire hill is open country across which the walker can wander at will. A bridleway runs south-eastward from the minor road between
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road. The bridleway follows, in part at least, the vehicular track (no public vehicular access) to the disused quarry.
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The hill is formed from sandstones and mudstones of the Senni Beds Formation and Brownstones Formation of the
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British Geological Survey 1:50,000 map sheet 231 'Brecon' & accompanying sheet explanation
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Ordnance Survey Explorer map OL12 'Brecon Beacons National Park: western area'
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when a minor glacier grew at this spot. It has left a couple of arcuate
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This face is much the steepest and has its origins in the
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face has been quarried. The quarry is designated as a
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Index


Elevation
Prominence
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Coordinates
51°52′57″N 3°34′53″W / 51.88250°N 3.58139°W / 51.88250; -3.58139
Powys
Wales
Parent range
Brecon Beacons
OS grid
SN912217
Fforest Fawr
Brecon Beacons National Park
Powys
trig point
Old Red Sandstone
Devonian period
fault
ice ages
moraines
glaciated rock
site of special scientific interest
Heol Senni
A4067
images of Fan Bwlch Chwyth on Geograph website
Categories
Mountains and hills of Powys
Fforest Fawr

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