Some Salient Points in the Science of the EarthDawson, John William, Sir
Science
Some Salient Points in the Science of the Earth
Dawson, John William, Sir
Geology; Paleontology
Still another question of great cosmic interest relates to the possible
alternation of glacial conditions in the northern and southern
hemispheres. There is evidence of drift in the southern part of South
America, similar to that in the north; but was it deposited at the same
time? If we could be sure that it was not, many difficulties would be
removed. The southern hemisphere is at present emphatically the ocean
hemisphere; the northern, the land hemisphere. Perhaps these conditions
may be capable of being reversed, in which case the periods of
depression in the south may have corresponded with those of elevation
in the north. One thing which we know is, that there is a polar ice
ring, not an ice cap, for we do not know what is within its edges at
the South Pole, about 2,000 miles in diameter, and this in the only
circumstances in which it can exist, namely, surrounded by a vast ocean
furnishing it with abundant aqueous vapour. We also know that from this
ice ring radiate glaciers, carrying _débris_, with which the sea bottom
is strown half way to the equator. If continents were elevated out of
the Southern Ocean, we should probably have on their surfaces glacial
deposits more widespread and continuous than any remaining on the
continents of the northern hemisphere, and like some of them thinning
out to a terminal edge or border, instead of a terminal moraine like
that of a glacier.[176] Thus we may say with some truth that the
southern hemisphere is now passing through one phase of the Glacial
period.
[176] This is now admitted by Chamberlain and others to be the case
with the oldest boulder clay on the American continent.
Public-domain text, read in full here on John Shaqi.
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