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the imbedding of organic remains in deposits formed upon the land, I shall next consider the including of the same in deposits formed under water. It will be convenient to divide this branch of our subject into three parts; considering, first, the various modes whereby the relics of _terrestrial_ species may be buried in subaqueous formations; secondly, the modes whereby animals and plants inhabiting _fresh water_ may be so entombed; thirdly, how _marine_ species may become preserved in new strata. The phenomena above enumerated demand a fuller share of attention than those previously examined, since the deposits which originate upon dry land are insignificant in thickness, superficial extent, and durability, when contrasted with those of subaqueous origin. At the same time, the study of the latter is beset with greater difficulties; for we are here concerned with the results of processes much farther removed from the sphere of ordinary observation. There is, indeed, no circumstance which so seriously impedes the acquisition of just views in our science as an habitual disregard of the important fact, that the reproductive effects of the principal agents of change are confined to another element--to that larger portion of the globe, from which by our very organization we are almost entirely excluded.[1059] _Imbedding of Terrestrial Plants._ When a tree falls into a river from the undermining of the banks or from being washed in by a torrent or flood, it floats on the surface, not because the woody portion is specifically lighter than water, but because it is full of pores containing air. When soaked for a considerable time, the water makes its way into these pores, and the wood becomes _waterlogged_ and sinks. The time required for this process varies in different woods; but several kinds may be drifted to great distances, sometimes across the ocean, before they lose their buoyancy. _Wood sunk to a great depth in the sea._--If wood be sunk to vast depths in the sea, it may be impregnated with water suddenly. Captain Scoresby informs us, in his Account of the Arctic Regions, that on one occasion a whale, on being harpooned, ran out all the lines in the boat, which it then dragged under water, to the depth of several thousand feet, the men having just time to escape to a piece of ice. When the fish returned to the surface "to blow," it was struck a second time, and soon afterwards killed. The moment it expire
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