the western coast [of Great Britain] don't refer to it as such."

Seabed

The seabed under the Celtic Sea is referred to as the Celtic Shelf, part of the continental shelf of Europe. The northeast portion has a depth of between 90 and(-) 100 m, increasing towards Saint George's Channel. In the opposite direction, sand ridges pointing southwest have a similar height, separated by troughs approximately 50 m deeper. These ridges were formed by tidal effects when the sea level was lower. South of 50°N,

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