Dating in cornwall england
No place in England is more than 75 miles (120 km) from the sea, and even the farthest points in the country are no more than a day’s journey by road or rail from London.
Deep deposits of sand, gravel, and glacial mud left by the retreating glaciers further altered the landscape.
The Cumbrian Mountains, which include the famous Lake District, reach 3,210 feet (978 metres) at Scafell Pike, the highest point in England.
Slate covers most of the northern portion of the mountains, and thick beds of lava are found in the southern part.
Between these regions lie bands of sandstones and limestones of different geologic periods, many of them relicts of primeval times when large parts of central and southern England were submerged below warm seas.
Geologic forces lifted and folded some of these rocks to form the spine of northern England—the Pennines, which rise to 2,930 feet (893 metres) at Cross Fell.
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Erosion by rain, river, and tides and subsidence in parts of eastern England subsequently shaped the hills and the coastline.