Freezing Lava Beds near Medicine Lake, Siskiyou County, Northern
California. (M. S. Baker, _Sierra Club Bulletin_, 1899. Vol. II., page
318.)--"One other feature of the lava region must be mentioned--the ice
caves. There are several of these known, and very likely many more
remain undiscovered. Those located along the edge of the lava, near the
cinder cone, I have known to contain ice and water as late as August.
The largest I have seen is on the Mayfield Road, about twenty miles
east of Bartles. It is situated in the barren lava, and in one of the
warmest localities of the region,--and there are few cool spots in the
lava anywhere. One enters the cave by crawling down a hole none too
large. The instant the interior is reached the temperature falls in a
surprising way. Not more than ten feet below the surface of the hot
rocks is a bed of ice, covered by a foot or so of ice water. The body
of ice was perhaps twelve or fifteen feet long, by five feet across
in the widest places. This cave is formed by a fissure that extends a
distance of twenty miles from the ice cave to Pittville, and nearly
coincides with the 4000 foot level, as shown in the map. Along the
southeastern half of this earth fissure the southwest wall has faulted,
leaving a cliff, which, in places, must be nearly 200 feet high."
Freezing Shafts, Montana.--Mr. Robert Butler, of San José, Cal., has
given me much information about glacières in Montana. He visited one
miners' shaft which is situated about 80 kilometers up the Rosebud
River from Rosebud Station on the Northern Pacific R. R., and about 10
kilometers northeast of the Cheyenne Indian Agency. It is on the north
slope of the Little Wolf Mountains, near the summit, at the head of
Greenleaf Creek. The canyon and surrounding slopes are covered with
a dense growth of pine. The rock has the appearance of scoriæ caused
by the burning of immense beds of coal in recent geological times. The
rock is broken into comparatively small pieces. The altitude is some
1200 meters. The forest, the volcanic ash and the altitude, besides
the loose rock formation, makes this place a natural ice house. Ten or
twelve years ago three prospectors, looking for silver, sunk a shaft
here. At a depth of about 4 meters it began to grow cold, and at 6
meters they found ice and imagined they could feel an upward draught.
Being ignorant and superstitious, they became frightened and abandoned
the shaft. During the winter, the snow fills the shaft half full of
ice, which then remains over through the summer. There is a general
report and belief among those who have visited the well, that it
freezes in summer and thaws in winter. There are thousands of mining
shafts in Montana, and if they are on the north slope of a mountain
of considerable altitude and under a dense forest and not too deep,
they generally have ice at the bottom during the summer. It is also
said to be nothing new for a miner in following crevices to find them
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