Geology: The Science of the Earth's CrustMiller, William J. (William John)
Philosophy
Geology: The Science of the Earth's Crust
Miller, William J. (William John)
Geology
Brief descriptions of a few typical carefully studied earthquakes
during recent years will serve to make the main features of earthquakes
still clearer to the reader.
The violent Japanese earthquake of 1891 was caused by the sinking of
a block of earth forty miles long from two to thirty feet below that
on the other side of a fault fracture. There was also considerable
horizontal shifting, and cracks developed in the adjacent region. A
distinct fault scarp, fifteen to twenty feet high, developed, and in
some cases extended right across cultivated fields.
[Illustration: Fig. 13.--Map of the United States, showing the large
areas over which three of the greatest of our earthquakes were actually
felt by people. These earthquakes were recorded in many parts of the
world by delicate instruments: New Madrid, 1811; Charleston, 1886; San
Francisco, 1906.]
[Illustration: Fig. 14.--Sketch map showing the trace of the great
fault fracture along which a renewed sudden movement of as much as
twenty feet took place to cause the San Francisco earthquake of 1906.
(After U. S. Geological Survey.)]
The San Francisco earthquake of 1906 was produced by renewed movement
along the great fault which extends lengthwise through the Coast Range
Mountains for several hundred miles. It is literally correct to say
that, for 250 miles along this great earth fracture, one part of the
Coast Range instantaneously slipped from two to twenty-two feet past
the other. More or less of the movement extended at least several
thousand feet down into the earth. In this case both sides slipped and
the movement was very largely horizontal rather than vertical. The
land on the east side of the fault moved south and that on the west
side moved north, the amount diminishing away from the fault on each
side so that some miles out the actual crustal movement was only a few
inches. When one thinks of the tremendous volumes of earth material
involved in this shifting of the earth's crust, is it any wonder
that such destructive earthquake waves were produced? Many buildings
were wrecked, several hundred people were killed, the disastrous San
Francisco fire resulted, water mains were broken, and fences and roads
crossed by the fault were dislocated as much as fifteen to twenty feet.
[Illustration: Plate 5.--Swift Current Valley in Glacier National Park,
Montana. This was once a deep V-shaped canyon carved out (eroded)
by stream action. Then a great valley glacier slowly plowed its way
through it during the Ice Age and, by ice erosion, the present nearly
straight U-shaped canyon has resulted. (_Photo by Campbell, U. S.
Geological Survey._)]
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