Loafing along Death Valley trails : $b a personal narrative of people and placesCaruthers, William
History
Loafing along Death Valley trails : $b a personal narrative of people and places
Caruthers, William
Death Valley (Calif. and Nev.)
He gave me a kind of _et-tu, Brute_ look and smiled.
“In the fall of 1882 I was driving a 12 mule team from the Eagle Borax
Works to Daggett. I met a man on a buckboard who asked if the team was
for sale. I told him to write Mr. McLaughlin. It took 15 days to make
the round trip and when I got back I met the same man. He showed me a
bill of sale for the team and hired me to drive it. He had an eight mule
team and a new red wagon, driven by a fellow named Webster. The man in
the buckboard was Borax Smith.
“Al Maynard, foreman for Smith and Coleman, was at work grubbing out
mesquite to plant alfalfa on what is now Furnace Creek Ranch. Maynard
told me to take the tongue out of the new wagon and put a trailer tongue
in it. ‘In the morning,’ he said, ‘hitch it to your wagon. Put a water
wagon behind your trailer, hook up those eight mules with your team and
go to Daggett.’
“That was the first time that a 20 mule team was driven out of Death
Valley. Webster was supposed to swamp for me. But when he saw his new
red wagon and mules hitched up with my outfit, he walked into the office
and quit his job.”
Chapter VI
Death Valley Geology
The pleasure of your trip through the Big Sink will be enhanced if you
know something about the structural features which are sure to arrest
your attention.
For undetermined ages Death Valley was desert. Then rivers and lakes.
Rivers dried. Lakes evaporated. Again, desert. It is believed that in
thousands of years there have been no changes other than those caused by
earthquakes and erosion.
It is no abuse of the superlative to say that the foremost authority
upon Death Valley geology is Doctor Levi Noble, who has studied it under
the auspices of the U.S. Geological Survey since 1917. He has ridden
over more of it than anyone and because of his studies, earlier
conclusions of geologists are scrapped today.
From a pamphlet published by the American Geological Society with the
permission of the U. S. Dept. of Interior, now out of print, I quote a
few passages which Doctor Noble, its author, once described to me as
“dull reading, even for scientists.”
“The southern Death Valley region contains rocks of at least eight
geologic systems whose aggregate thickness certainly exceeds 45,000 feet
for the stratified rocks alone.”
“The dissected playa or lake beds in Amargosa Valley between Shoshone
and Tecopa contain elephant remains that are Pleistocene....”
“Rainbow Mountain is one of the geological show places of the Death
Valley region.... Here the Amargosa river has cut a canyon 1000 feet
deep.... The mountain is made up of thrust slices of Cambrian and
pre-Cambrian rocks alternating with slices of Tertiary rocks, all of
which dip in general about 30 to 40 degrees eastward, but are also
anticlinally arched.”
Public-domain text, read in full here on John Shaqi.
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