Page:Quarterly Journal of the Geological Society of London, vol. 31.djvu/835

Rh

the north-eastern border of Derbyshire a low range of hills, rising from the plateau of the Magnesian limestone, is somewhat abruptly cut through by a short ravine known as Creswell Crags (fig. 1). It is about a third of a mile in length, running nearly east



and west, and is bounded on either side by beautifully wooded cliffs, which in places are some 50 or 60 feet high. The limestone is the Lower Permian, and is very hard and massive here, with an easterly dip, which is rather difficult to trace. On either side of the ravine the crags are much fissured, the fissures now and then forming tolerable-sized caverns, opening some 15 feet or less above the level of a sheet of water that has been formed by the damming up of a small stream flowing between the crags from W. to E. Some years ago I had formed a strong wish to examine the fissures in this locality, but until lately could never find the opportunity. Last April, however, I was enabled to pay a preliminary visit to the spot. A very brief inspection sufficed to show me that it was one well worth careful exploration; and in answer to an application to His Grace the Duke of Portland, he very kindly gave me leave to carry on the work.

On the southern side of the ravine there is a cavern (Fissure C) with a large mouth; but it contracts at a very short distance in, where it has been walled up to keep out foxes, many smaller fissures being similarly protected in the locality. In this cavern, in a small hole I made for testing at the entrance, I obtained, about 3 or 4 inches below the surtace, a fine piece of the leg-bone of Rhinoceros tichorhinus.