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be seen, some of them quite tilled with quartz-pebbles, and 
forming a conglomerate ; they have a general dip to the north- 
west. Though not seen in absolute contact, there can be no 
doubt the two series of beds do not conform together. Still 
proceeding southwards about a mile, opposite the situation 
occupied by the old Pompocali, are the picturesque crags of 
Etchell. They are formed from the same gritstone already 
mentioned, are of a yellow colour, and have become 
much rounded by exposure. A short distance above and 
beyond the crags, the Permian Limestone is worked for 
agricultural purposes. 
Westward from these points the Gritstone may be 
traced, and is found to correspond exactly with the various 
beds of the Third Millstone Grits, already described as 
stretching from Harewood and Eccup eastward. The great 
Fault which reaches from Meanwood to Kiddall Hall, and there 
passes beneath the limestone, has brought the Upper or 
Rough Eock into apposition with the Coal-measures on the 
south. The Fault appears to be continued two or three 
miles still further eastwards along the edge of Bramham 
Park. North of the Fault, near the park, the limestone has 
been so much abraded that a considerable expanse of the 
grit rock beneath is now at the surface. Three or four 
quarries have been opened in the grit to obtain stone for 
building purposes. In one, outside the boundary wall of the 
park, a good section is exposed, showing the limestone 
superimposed on the grit, with a small bed of fine sand, 
mostly white and very falsely-bedded, dividing the two. The 
gritstone, of which about twenty feet are exposed, is white, 
in thick massive beds. It is quartzose, and contains many 
rounded pebbles of the same material. In some cases it is 
very soft, and may be ground into sand between the fingers ; 
usually it is a good building stone. The upper surface is 
very uneven, and has evidently been subject to the action of 
