Around Coniston, Ashgill Quarry, Ashgill Beck and Torver Beck reveal a varied succession of Ordovician and Silurian marine rocks. Trilobites and brachiopods occur in shell-bearing beds, while younger mudstones preserve graptolite assemblages. These are separate upland exposures, with steep quarry faces and fast-changing stream conditions; arrange collecting permission and leave protected rock faces undisturbed. Silurian, Ordovician, Cuttings, Disused Quarries, Rating: ♦♦♦




