button to main menu  Otley's Guide 1823 (8th edn 1849)

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Page 212:-
In conclusion, we append some remarks by Mr. Westall, prefacing his Views of the Caves - a series of effective and accurate aquatints, which have not been sufficiently appreciated:
  geolmorphology
  limestone caves

'The rocks in which these Caves are formed are composed of coarse limestone and marble, of various kinds of and colours, which generally run in horizontal strata, from three to six feet wide: the lowest is of a very fine quality, particularly the black, of which there is a fine vein in Yordas Cave, but it is more difficult to be got at than at Dent, where it is worked with great success.
'This bed of calcareous rock is probably connected with that in Derbyshire, as the same kind of marine petrifactions of animals, no longer known to exist, occur in both. It is called transition or mountain limestone, and caves are found in the same kind of rock in various parts of the world.
'These Caves are supposed to be formed by water forcing its way through natural fissures, and carrying the softer or broken parts of the rock with it, as streams are found invariably to run through them all.'

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KIRKBY LONSDALE BRIDGE.- SOUTH VIEW
T. BINNS [del]

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button -- "Kirkby Lonsdale Bridge" -- Devil's Bridge

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