“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.”

“None of the geologic terms in common use appear exactly to fit this mosaic of large tightly packed individual blocks of different ages occupying a definite zone above a major thrust fault.”