... between Green Ore [NG 357900 150200] and Stoke St. Michael [NG 366500 147000], 5 km north of Shepton Mallet [NG 362000 143500], as the most likely catchment area for the hot springs. Edmunds & Miles (1991) reviewed the evidence for the residence of the thermal waters in the Carboniferous Limestone...

..., Avonmouth; CH, Cheddar; CL, Clevedon; PH, Portishead; RS, Radstock; SH, Shepton Mallet; TW, Tortworth; WL, Wells; WM, Weston-super-Mare. overthrust pieces of Lower Carboniferous rocks, completely surrounded by Upper Carboniferous rocks. Sibly (1912) successfully interpreted the Vobster inlier (see Fig. 2...

... and limestones. The Downside Stone is best seen in the Shepton Mallet area ( Green & Welch, 1965 ), where it is overlain by the Charmouth Mudstone Formation (Pylle Clay Member of Bristow et al . 1999 ). Most of the Downside Stone is of planorbis – bucklandi Zone age (Hettangian–Sinemurian...

... Ankylosauromorpha), but this has not been supported in a recent global analysis of ornithischian phylogeny ( Butler et al . 2008 ). Reports of S. harrisonii from the Rhaetian Westbury Formation of Shepton Mallet, Somerset ( Storrs 1994 ), Lower Jurassic Kayenta Formation of Arizona, USA ( Padian 1989...

... to him half a ton of matrix from another fissure he had discovered, that at Windsor Hill near Shepton Mallet. Kiihne recovered over 2000 bones and teeth of the mammal-like reptile Oligokyphus from the fissure, which he dated on the invertebrate content as Liassic. (Ktihne 1956). Oligokyphus was the only...

... Mallet, England. This locality is also a fissure-fill deposit formed in Carboniferous limestone but is Charmouthian (Pliensbachian) and thus younger than the St. Bride’s fissures (Kühne 1956 ). The Mendip adult Oligokyphus specimens comprise two size morphs (Kühne 1956...