. The Quarterly journal of the Geological Society of London. Surface of Water 331 Ft. Surface, or WaUr S21 Ft Surface of miter 396Ft. Fig. 21. Jjcwehwater Scale 7inch to 1 mile. Jjdkes with their svrmdings, deptJisin feet. Mintern Bros. Lith. Vol XXX PI X PLANS AM) SECTIONS TO ILLUSTRATE PAPER ON THE ORIGIN 01 SOME OF THE LAKE-BASINS OF CUMBERLAND in <.,,. OF THE LAKE-BASINS OF CUMBERLAND. 103 Fig. 17. Plan of Derwentwater, \ 18. „ Bassenthwaite Lake, .,, , ,« • • i ix7 t I lines along which the sections run. 20. „ Urunimock Water, ° 21. „ Loweswater, J Discussion.
. The Quarterly journal of the Geological Society of London. Surface of Water 331 Ft. Surface, or WaUr S21 Ft Surface of miter 396Ft. Fig. 21. Jjcwehwater Scale 7inch to 1 mile. Jjdkes with their svrmdings, deptJisin feet. Mintern Bros. Lith. Vol XXX PI X PLANS AM) SECTIONS TO ILLUSTRATE PAPER ON THE ORIGIN 01 SOME OF THE LAKE-BASINS OF CUMBERLAND in <.,,. OF THE LAKE-BASINS OF CUMBERLAND. 103 Fig. 17. Plan of Derwentwater, \ 18. „ Bassenthwaite Lake, .,, , ,« • • i ix7 t I lines along which the sections run. 20. „ Urunimock Water, ° 21. „ Loweswater, J Discussion. Mr. Campbell said that he had listened with great pleasure to theable paper of the author. He was not himself acquainted with theLake-district; but he knew many similar districts in which similarphenomena existed. He agreed with the authors conclusion, thatthese lake-basins were the result of glacial erosion. But if icecould do so much, it might have done more. In confirmation of theauthors views, Mr. Campbell said that in the Caucasus there arevery few lakes. He had found no glacial phenomena in the wholerange, except one small moraine near the only lake in Daghestan. Mr. Evans inquired what effect the varying hardness of the strata,their trend and dip, might have had
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Keywords: ., bookcentury1800, bookdecade1840, bookidquarte, booksubjectgeology
