Geograph IrelandLatest Images by Gareth Evans
https://www.geograph.ie/
2024-03-19T13:15:48+00:00text/html2007-12-21T17:02:16+00:00https://www.geograph.ie/profile/20233Gareth Evans51.677951 -5.045517SM8902 : Angle bay looking towards Milford haven
https://www.geograph.ie/photo/637491
Near high tide. At low tide, an expanse of mud flat is exposed.text/html2007-12-21T16:51:24+00:00https://www.geograph.ie/profile/20233Gareth Evans52.596716 -2.862727SJ4100 : Disused barite workings, former Cothercott mine
https://www.geograph.ie/photo/637487
Immediately to the left of the figure a vein of barite is exposed. The openings lead into a still-open stope, or working, within the vein.text/html2007-12-18T17:08:31+00:00https://www.geograph.ie/profile/20233Gareth Evans52.586598 -2.905480SO3899 : Disused barite shaft, near Gatten Lodge
https://www.geograph.ie/photo/635863
Earl's Hill and Paulith Bank are the prominent hills in the backgroundtext/html2007-12-17T16:59:20+00:00https://www.geograph.ie/profile/20233Gareth Evans52.611258 -2.877929SJ4001 : Abandoned adit, Huglith copper/barite mine
https://www.geograph.ie/photo/635275
The adit holds water due to collapse of the entrance cutting. WARNING entry is dangerous - don't try it.text/html2007-12-17T16:50:41+00:00https://www.geograph.ie/profile/20233Gareth Evans52.624134 -2.910982SJ3803 : Maddox's Coppice
https://www.geograph.ie/photo/635266
Established planted woodland on the dip slope of the Stiperstones.text/html2007-12-15T22:57:19+00:00https://www.geograph.ie/profile/20233Gareth Evans52.626889 -2.891538SJ3903 : Habberley from Earl's Hill
https://www.geograph.ie/photo/633992
Habberley lies in a valley floored by early Ordovician mudrocks and overlain by glacial deposits. In the distance, the ground rises to the ridge of the Stiperstones, formed by resistant lower Ordovician quartz arenites.text/html2007-12-15T22:49:37+00:00https://www.geograph.ie/profile/20233Gareth Evans51.535980 -3.259921ST1282 : Taff Gorge from sandstone crag on Garth Hill
https://www.geograph.ie/photo/633985
Upper Carboniferous rocks underlie the foreground and have been mined historically for coal. The conspicuous settlement, Taff's Well, lies on alluvium and river terraces of the Taff. The wooded ridges either side of the gorge are of lower Carboniferous limestones which are currently quarried and have been mined historically for iron.