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A critical Examination of the first Principles of Geology in a Series of Essays / By G. B. Greenough
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pulverize them to the finest degree ima- ginable, and mix them as confusedly together as possible, and let them fall through a dry fluid, such as the air, they will settle just in the same confused state as they were; if you permit them to sub- side through water, they will settle more or less in parallel strata. Indeed it re- quires twenty or thirty times the quantity of water to earth to make this layer-like subsidence tolerably apparent even in the mixture of but three or four bodies; but the greater quantity of water you use, and the finer you pulverize the sub- stances, the more apparent and regularthe strata will be. (P. 269.)

According to Werner, strata are fromfour to six feet apart in the older form-ations, but less distant in the newer.

Hutchinson observes a , that in the mid-u land counties of England the strata are commonly thin near the surface, and be- come gradually thicker in proportion toa Hutchinsons Works, vol. xii. p. 264.