It Is A Mass Of Lava Presenting To The Gray Sage
Plain Of Shasta Valley A Bold Craggy Front Two Thousand Feet High.
Its summit lies at an elevation of five thousand five hundred feet
above the sea, and has several square
Miles of comparatively level
surface, where bunchgrass grows and the snow does not lie deep, thus
allowing the hardy sheep to pick up a living through the winter months
when deep snows have driven them down from the lofty ridges of Shasta.
From here it might be well to leave the immediate base of the mountain
for a few days and visit the Lava Beds made famous by the Modoc War.
They lie about forty miles to the northeastward, on the south shore of
Rhett or Tule[7] Lake, at an elevation above sea level of about forty-five hundred feet. They are a portion of a flow of dense black
vesicular lava, dipping northeastward at a low angle, but little
changed as yet by the weather, and about as destitute of soil as a
glacial pavement. The surface, though smooth in a general way as seen
from a distance, is dotted with hillocks and rough crater-like pits,
and traversed by a network of yawning fissures, forming a combination
of topographical conditions of very striking character. The way lies
by Mount Bremer, over stretches of gray sage plains, interrupted by
rough lava slopes timbered with juniper and yellow pine, and with here
and there a green meadow and a stream.
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