User:LIUCMarco7/New sandbox

The Chatsworth Grit here is typically very coarse grained, with abundant pebble beds composed mainly of vein quartz, and the large scale sedimentary structures are clearly exposed – including examples of slumping and the development of finer grained flaggy beds. the large scale geological structures and geomorphology can be still seen in the skylines and the views along the edge; cloughs, stacks and large fallen blocks pass into thick deposits of head, which cover the lower slopes of this part of the Upper Derwent Valley.