Allt Yr Esgair
Geology
The hill is formed from sandstones and mudstones of the Senni Formation (formerly the Senni Beds) of the Old Red Sandstone laid down during the Devonian period. The lower slopes are formed from mudstones and sandstones of the slightly older St. Maughans Formation. A number of small sandstone quarries, now disused, adorn the slopes. The hill probably stood out above the Usk Valley glacier ice during the ice age. At a late stage in de-glaciation, the cols at either end of the ridge at the villages of Pennorth and Bwlch are believed to have conveyed water from a greatly enlarged Llangorse Lake into the Usk catchment.
Access
Several bridleways run along the length of the hill giving access to walker, horseriders and mountain-bikers. The summit area and the woodland to the northeast are open access for walkers. A car park off the A40 road immediately south of the hill provides a convenient starting point for many walkers.
Archaeology
Allt yr Esgair's summit is crowned by an Iron Age hillfort, one of several in the Usk Valley.
The Roman road between the Roman fort of CICVCIVM at Y Gaer, Brecon and Gobannium at Abergavenny runs along the ridge and is followed by a modern-day bridleway.
See also
References
- ^ Ordnance Survey Explorer map OL13 'Brecon Beacons National Park: eastern area'
- ^ "Allt yr Esgair". hill-bagging.co.uk. Retrieved 23 June 2019.
- ^ British Geological Survey 1:50,000 map sheet 214 'Talgarth' & accompanying sheet explanation
- ^ "Allt-yr-Esgair Hillfort, Llangors; Allt yr Esgair Hillfort (92158)". Coflein. RCAHMW. 2015. Retrieved 22 January 2016.