I. I ntroduction . The area here termed the Central Mendips comprises that part of the Mendip Hills which lies between Cheddar and Shepton Mallet. This paper deals only with the Palæozoic rocks, which occupy the greater part of the area, and appear in inliers among the Mesozoic rocks on the south. The eastern, western, and northern boundaries of the area are artificial, the lines cutting across the geological structures. I wish to express my indebtedness to Dr. Stanley Smith for his unfailing help in the field and laboratory and in the compilation of this paper; to Prof. S. H. Reynolds and Dr. T. F. Sibly for much advice and helpful criticism; to the Department of Scientific and Industrial Research for a maintenance grant; to the Colston Research Society for defraying certain expenses; and, finally, to all others who have in any way helped me. The area was first surveyed by Sir Henry T. De la Beche, over eighty years ago, and his results were embodied in the 1-inch Geological Survey Map, Sheet XIX, O.S. (1845), as also in the Survey Memoir of 1846 [3]. His account of the structure and stratigraphy is remarkably accurate, and forms the basis of all subsequent work. Except for the publication of William Sanders's geological map in 1862, which was the first large-scale map of the area, no works of importance appeared for more than twenty years after De la Beche's Memoir, until Bristow & Woodward [2] wrote an article dealing with prospects of coal south