Pen-y-crug

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Ramparts of Pen-y-crug hill fort Pen-y-crug hillfort - geograph.org.uk - 374823.jpg
Ramparts of Pen-y-crug hill fort

Pen-y-crug is a hill in the Brecon Beacons National Park in the county of Powys, south Wales. It is commonly referred to locally as simply 'The Crug' (pronounced cree-g).[ citation needed ] The Welsh name signifies 'top of the mound'. It slopes are moderately gently on three sides; only to the west do they steepen somewhat. Its flat trig point adorned summit at 331m overlooks the valley of the River Usk to the south. To the southeast are panoramic views over Brecon whilst eastwards are the Black Mountains and south the Brecon Beacons. [1]

Contents

Geology

Trig point at the summit of Pen-y-crug Trig point at Pen-y-crug summit.jpg
Trig point at the summit of Pen-y-crug

The hill is formed from sandstones and mudstones of the St. Maughans Formation of the Old Red Sandstone laid down during the Devonian period. The lower slopes are formed from mudstones and sandstones of the Raglan Mudstone Formation of late Silurian age. A number of small sandstone quarries, now disused, adorn the upper slopes. The hill probably stood out above the Usk Valley glacier ice at times during the ice age. [2]

Access

A bridleway runs northwestwards over the northern and eastern slopes of the hill from the B4520 road on the northern edge of Brecon giving access to walkers, horseriders and mountain-bikers. A public footpath also leads to the summit from the edge of Brecon via Maen-du Well. The upper slopes are open access for walkers. A small car park off the minor road to its north provides a convenient starting point for many walkers.

Archaeology

LIDAR showing the Iron Age hillfort

The summit is crowned by an impressive Iron Age hillfort, one of several in the Usk Valley. [3]

There are the remains of a brick and tile works dating from Victorian times on its southeastern flank.

See also

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This article describes the geology of the Brecon Beacons National Park in mid/south Wales. The area gained national park status in 1957 with the designated area of 1,344 km2 (519 sq mi) including mountain massifs to both the east and west of the Brecon Beacons proper. The geology of the national park consists of a thick succession of sedimentary rocks laid down from the late Ordovician through the Silurian and Devonian to the late Carboniferous period. The rock sequence most closely associated with the park is the Old Red Sandstone from which most of its mountains are formed. The older parts of the succession, in the northwest, were folded and faulted during the Caledonian orogeny. Further faulting and folding, particularly in the south of the park is associated with the Variscan orogeny.

References

  1. Ordnance Survey Explorer map OL12 'Brecon Beacons National Park: western area'
  2. British Geological Survey 1:50,000 map sheet 213 'Brecon' & accompanying sheet explanation
  3. "Pen-y-Crug; Pen-y-Crug Hillfort (92058)". Coflein. RCAHMW. 16 December 2014. Retrieved 27 January 2016.

51°57′46″N3°24′51″W / 51.9627°N 3.4142°W / 51.9627; -3.4142