[On the Origin of Species by Charles Darwin]@TWC D-Link bookOn the Origin of Species CHAPTER XII 34/45
Southward of the Asiatic continent, on the opposite side of the equator, we know, from the excellent researches of Dr.J.Haast and Dr.Hector, that in New Zealand immense glaciers formerly descended to a low level; and the same plants, found by Dr. Hooker on widely separated mountains in this island tell the same story of a former cold period.
From facts communicated to me by the Rev.W.B. Clarke, it appears also that there are traces of former glacial action on the mountains of the south-eastern corner of Australia. Looking to America: in the northern half, ice-borne fragments of rock have been observed on the eastern side of the continent, as far south as latitude 36 and 37 degrees, and on the shores of the Pacific, where the climate is now so different, as far south as latitude 46 degrees. Erratic boulders have, also, been noticed on the Rocky Mountains.
In the Cordillera of South America, nearly under the equator, glaciers once extended far below their present level.
In central Chile I examined a vast mound of detritus with great boulders, crossing the Portillo valley, which, there can hardly be a doubt, once formed a huge moraine; and Mr.D.Forbes informs me that he found in various parts of the Cordillera, from latitude 13 to 30 degrees south, at about the height of 12,000 feet, deeply-furrowed rocks, resembling those with which he was familiar in Norway, and likewise great masses of detritus, including grooved pebbles.
Along this whole space of the Cordillera true glaciers do not now exist even at much more considerable heights.
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