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caliche - tan hardpan caliche from the Mojave Desert - hand/display specimen

$ 4.32

Availability: 89 in stock

Description

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Tan hardpan caliche from the Mojave desert - hand/display specimen
Caliche underlies desert soils in a large part of the Western U.S. and in other arid areas. It is composed of calcium carbonate and can be tens of feet thick. An ideal caliche profile would have a
hardpan
at the surface progressing downward into a
platy
or
laminar layer
which overlies a
nodular zone
,
and then intercepts the bedrock. Since a caliche takes tens to hundreds of thousands of years to form, changes in climate disrupt this sequence and an ideal profile is seldom seen.
The term
caliche
is Spanish from the Latin
calx
for lime. It forms when calcium carbonate is leached from the overlying soil and accumulates some distance below the surface.
In the Mojave desert, a major period of calcium carbonate deposition appears to have occurred 20,000 years ago, forming a horizon below a depth of 100 cm during a period of greater rainfall than at present. As the climate dried, CaCO
3
precipitated to form caliche.
The mill for the Copper World Mine was at Valley Wells. The caliche there served as the roof of the mill workers' dugout cabins during the first 20 years of the 1900s, where, comfortable underground, they simply excavated under the caliche from the side of a ravine. In other parts of the Southwest, caliche posed a challenge for pioneers when they attempted to dig wells.
An example of this culturally interesting rock.
The field photo shows one of the mill workers' dugout cabins with a caliche roof.
Select a specimen:
When more than one specimen is shown, you can select a particular specimen by telling us what is in the photo with it - a black mechanical pencil, a silver and black pen, a silver and blue pen, or one of those plus some number of coins, or you can let us make the selection.
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