(_d._) _California._--Proceeding westwards into California, we are
again confronted with volcanic phenomena on a stupendous scale. The
coast range of mountains, which branches off from the Sierra Nevada at
Mount Pinos, on the south, is terminated near the northern extremity of
the State by a very lofty mountain of volcanic origin, called Mount
Shasta, which attains an elevation of 14,511 feet (see Fig. 25). This
mountain was first ascended by Clarence King in 1870,[4] and although
forming, as it were, a portion of the Pacific Coast Range, it really
rises from the plain in solitary grandeur, its summit covered by snow,
and originating several fine glaciers.
The summit of Mount Shasta is a nearly perfect cone, but from its
north-west side there juts out a large crater-cone just below the
snow-line, between which and the main mass of the mountain there exists
a deep depression filled with glacier ice. This secondary crater-cone
has been named Mount Shastina, and round its inner side the stream of
glacier ice winds itself, sometimes surmounting the rim of the crater,
and shooting down masses of ice into the great caldron. The length of
this glacier is about three miles, and its breadth about 4000 feet.
Another very lofty volcanic mountain is Mount Rainier, in the Washington
territory, consisting of three peaks of which the eastern possesses a
crater very perfect throughout its entire circumference. This mountain
appears to be formed mainly of trachytic matter. Proceeding further
north into British territory, several volcanic mountains near the
Pacific Coast are said to exhibit evidence of activity. Of these may be
mentioned Mount Edgecombe, in lat. 57°.3; Mount Fairweather, lat. 57°.20
which rises to a height of 14,932 feet; and Mount St. Elias, lat. 60°.5,
just within the divisional line between British and Russian territory,
and reaching an altitude of 16,860 feet. This, the loftiest of all the
volcanoes of the North American continent, except those of Mexico, may
be considered as the connecting link in the volcanic chain between the
continent and the Aleutian Islands.[5]
Public-domain text, read in full here on John Shaqi.
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