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
The late Prof. Alexander Winchell, a man who did not hesitate to
express his convictions, thus bears similar testimony:--"There has been
no continental glacier. There has been no uniform southerly movement of
glacier masses. There has been no persistent declivity as a _sine qua
non_, down which glacier movements have taken place. The continuity of
the supposed continental glacier was interrupted in the regions of the
dry and treeless plains of the west; and in the interior and Pacific
belts of the continent within the United States, ancient glaciation was
restricted to the elevated slopes."[170] He might have added that the
St. Lawrence valley was submerged and received the ends of Appalachian
and Adirondack glaciers on the south-east, and those of Laurentide
glaciers on the north-west.
[170] Nov., 1890.
My friend Prof. Claypole, who, however, has some hesitation, fearing,
I presume, to be cast out of the synagogue for heresy, ventures to
say,[171] "We deduce from the facts and arguments stated above, that
all the observations of glacial action in the northern hemisphere are
explicable by assuming the existence of enormous and confluent[172]
glacier-systems in and about the high lands of Europe, Asia, and
America, which high lands became, therefore, glacial radiants, and shed
their load of ice in all directions over the lower adjacent ground,
along the lines of easiest flow; that this theory does no violence
to the analogy of the existing order of things, requiring merely
an enlargement of actual glaciers by the intensification of actual
conditions : that abundant evidence can be obtained, as, for example,
from Switzerland, that the present glacier system of the earth was
once of sufficient magnitude to produce all the observed phenomena;
that the most important glacial radiants in the northern hemisphere
were, in North America, the district round Hudson Bay, New England
and the Adirondacks, with certain areas in the western Cordilleras,
and in Europe the Norwegian Dovrefelds and the Alps, Asia apparently
possessing none of commensurate importance; that it satisfactorily
explains, also, the previously puzzling absence of glacial action
over the great plain of Siberia, the coldest portion of the northern
temperate zone; that the belief in a vast polar ice cap, thousands of
feet thick, covering the whole Arctic region, and extending almost
continuously down to low latitudes, is an assumption doing violence to
observed physical facts and to probability, that it is not required to
account for the phenomena, and is, in fact, contradictory to some of
them."
[171] _American Geologist_, Feb., 1889.
[172] The term "confluent" is not necessary here. The glaciers of all
mountain chains may be said to be more or less confluent in the nevé,
from which individual glaciers radiate.
Public-domain text, read in full here on John Shaqi.
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