14 relations: Caledonian orogeny, Carmarthenshire, Church Stretton, Cymru Terrane, England, Fault (geology), Fold (geology), Pembrokeshire, Powys, Shropshire, Terrane, Variscan orogeny, Wales, Wrekin Terrane.
The Caledonian orogeny was a mountain building era recorded in the northern parts of Ireland and Britain, the Scandinavian Mountains, Svalbard, eastern Greenland and parts of north-central Europe.
Carmarthenshire (Sir Gaerfyrddin; or informally Sir Gâr) is a unitary authority in the southwest of Wales and is the largest of the thirteen historic counties of Wales.
Church Stretton is a small town in Shropshire, England, south of Shrewsbury and north of Ludlow.
The Cymru Terrane is one of five inferred fault bounded terranes that make up the basement rocks of the southern United Kingdom.
England is a country that is part of the United Kingdom.
In geology, a fault is a planar fracture or discontinuity in a volume of rock, across which there has been significant displacement as a result of rock-mass movement.
A geological fold occurs when one or a stack of originally flat and planar surfaces, such as sedimentary strata, are bent or curved as a result of permanent deformation.
Pembrokeshire (or; Sir Benfro) is a county in the southwest of Wales.
Powys is a principal area, a county and one of the preserved counties of Wales.
Shropshire (alternatively Salop; abbreviated, in print only, Shrops; demonym Salopian) is a county in the West Midlands of England, bordering Wales to the west, Cheshire to the north, Staffordshire to the east, and Worcestershire and Herefordshire to the south.
A terrane in geology, in full a tectonostratigraphic terrane, is a fragment of crustal material formed on, or broken off from, one tectonic plate and accreted or "sutured" to crust lying on another plate.
The Variscan or Hercynian orogeny is a geologic mountain-building event caused by Late Paleozoic continental collision between Euramerica (Laurussia) and Gondwana to form the supercontinent of Pangaea.
Wales (Cymru) is a country that is part of the United Kingdom and the island of Great Britain.
The Wrekin Terrane is one of five inferred fault bounded terranes that make up the basement rocks of the southern United Kingdom.