Abstract
The pebble-bed in the Trias of Budleigh Salterton has attracted much notice, but I am not aware that its materials have been compared with those of the corresponding bed in the Bunter group of the English Midlands. For this purpose I recently spent a short time at the former place, and think the results worth placing on record. I select for comparison the pebble-bed on the more northern part of the wild Staffordshire moorland called Cannock Chase, with which I happen to be especially familiar. The points of resemblance shall be noted first, those of difference afterwards.

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