Dating in mid wales
In the face of constant change, Wales continues to seek both greater independence and a distinct place in an integrated Europe.
Wales is bounded by the Dee estuary and Liverpool Bay to the north, the Irish Sea to the west, the Severn estuary and the Bristol Channel to the south, and England to the east.
The country stretches some 130 miles (210 km) from north to south, and its east-west width varies, reaching 90 miles (145 km) across in the north, narrowing to about 40 miles (65 km) in the centre, and widening again to more than 100 miles (160 km) across the southern portion.
Glaciers during the Pleistocene Epoch (about 2,600,000 to 11,700 years ago) carved much of the Welsh landscape into deeply dissected mountains, plateaus, and hills, including the north-south–trending Cambrian Mountains, a region of plateaus and hills that are themselves fragmented by rivers.
However, glaciers during the Pleistocene blanketed most of the landscape with till (boulder clay), scraped up and carried along by the underside of the great ice sheets, so that few soils can now be directly related to their parent rock.
Acidic, leached podzol soils and brown earths predominate throughout Wales.
Many of them have been pounded by the sea into spectacular steplike cliffs.
Anglesey (Môn), the largest island in England and Wales, lies off the northwestern coast and is linked to the mainland by road and rail bridges.
The varied coastline of Wales measures about 600 miles (970 km).
Other plateaus give way to coastal flats that are estuarine in origin.
Wales consists of six traditional regions—the rugged central heartland, the North Wales lowlands and Isle of Anglesey county, the Cardigan coast (Ceredigion county), the southwestern lowlands, industrial South Wales, and the Welsh borderland.