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- W2090816988 abstract "I stated several years since § that the thick gravel-beds of the valley of the Wey below Guildford were underlaid by an old terrestrial surface, indicated by peat, trees, and sedimentary deposits,—that the remains of the extinct mammalia were usually associated with this old surface,—and that it was in mud and silt of this age that the nearly perfect skeleton was found on the Pease Marsh, as was also the other of the parallel valley of the River Mole. As the great end to which geological inquiry is now tending is that of the past physical conditions which the earth9s surface has undergone, and as the value of such inferences is wholly dependent on the accuracy with which observed facts may have been described, I am desirous of adding to the instances I before adduced respecting this ancient terrestrial surface, more particularly as the facts referred to have been represented in another way by Mr. P. J. Martin, in his “Additional Observations on the Anticlinal Line of the London and Hampshire Basins,” published in the Philosophical Magazine, March 1854. With reference to the phaenomcna of the Wealden area, considered physically, Mr. Martin is of opinion that “the key to the whole is in the conception of the cotemporaneity of upheaval and denudation,” and that “there is no drift that is not of the age of the denudation.” The circumstance that there should occur marl-beds, showing tranquil accumulations for long periods,—peat-bogs in old valleys, with trees of large growth,—and all now" @default.
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- W2090816988 date "1855-02-01" @default.
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- W2090816988 title "On Land-Surfaces beneath the Drift-Gravel" @default.
- W2090816988 doi "https://doi.org/10.1144/gsl.jgs.1855.011.01-02.23" @default.
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