LIVERMORE
VALLEY LITHOPHILES
Gem
and Mineral Society
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STATE FOSSIL
The saber-toothed cat (Smilodon
californicus) was adopted by the Legislature as the official
State Fossil in 1973. Since it was adopted the name has been
changed to Smilodon fatalis, this change was made because
the fossil had already been identified from an earlier find
and named C. fatalis. As with all scientific names the earlier
name takes presidents over any newer names. Fossil evidence
indicates that this member of the cat family with 8-inch upper
canine teeth was about a foot shorter than a modern lion,
but weighed nearly twice as much. This meat-eater was very
common in California and lived here until 10,000 years ago.
Sabertoothed cats roamed most of North America, Europe and
South America. They lived during the Pleistocene age of geologic
history, which means they were here when the indigenous -
people of North America lived here. Fossil bones of Smilodon
fatalis have been found in abundance preserved in the tar
pits of Rancho La Brea in Los Angeles, but have also been
found locally at a quarry in Danville, California. In early
textbooks, encyclopedias, coloring books and other children's
books the fossil was listed as a Sabertoothed Tiger, it was
NOT a tiger, but a cat, this has now been corrected in most
books.
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STATE MINERAL
As one might expect, gold
is the official state mineral and was so designated in 1965.
In the four years following the discovery of gold by James
Marshall in January of 1848, California's population swelled
from 14,000 to 250,000 people. Miners came from all over
the world and extracted 28,280,711 fine ounces of gold from
1850-1859 which would be worth approximately $10,000,000,000
today. Although production is much lower, present day prospectors
can still pan for gold in California's streams. Today there
is still about 80% of the gold remaining in the gold-fields
of California's 'Mother-Lode'. Gold in its purest form has
a color of gold-yellow, hence its name. Gold is a very malleable
mineral with a hardness of 2.5; one ounce of gold can be
pounded into a sheet so thin that it will cover a football
field and you can shine a light through it. It is 19.3 times
as heavy as water. It can form crystals that are octahedrons,
dodecahedrons, cubes, as well as dendrites and massive.
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STATE ROCK
California has a greater number
of minerals and a wider variety of rock types than does any
other state. Serpentine (Serpentinite), a shiny, green and blue rock found
throughout California, was named the official State Rock in
1965. It contains the state's principal deposits of chromite,
magnesite, and cinnabar. California was the first state to
designate a State Rock. The minerals in the serpentine family
contain mostly magnesium and silicon, but also can contain
iron and aluminum. The rock is composed of several minerals
including several forms of asbestos. You can find serpentine
through out the Coast Mountain Range from the northern to
the southern part of the state. California will never rid
its air of some forms of asbestos because of the minerals
in serpentine.The rock should be called Serpentinite and not Serpentine, Serpentine is a mineral group.
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STATE GEMSTONE
Benitoite was designated the
official State Gemstone in 1985. Sometimes called the "blue
diamond", it was first discovered near the headwaters of the
San Benito River in 1907. It received its name because it
was found in San Benito County. The gem is extremely rare
and ranges in color from a light transparent blue to a dark
vivid sapphire blue, and occasionally it is found in a violet
shade. It is a Barium Titanium Silicate, has a hardness of
6-6.5 and a density of 3.65, and has an intense blue fluorescence
under SW UV light. It occurs in glaucophane schist in a serpentine
body. Associated minerals include; neptunite, natrolite, joaquinite,
albite, Jonesite , fresnoite and 26 other minerals. Benitoite
was first described by Dr. George Lauderback from U. C. Berkeley.
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STATE SOIL
The San Joaquin Soil was designated
as the official state soil in 1997. The first documentation
of San Joaquin Soil was made in 1900. The soil is listed as
a reddish brown, sandy loam about 14 inches thick. The subsoil
is a sticky and very plastic brownish red sandy clay loam
about 10 inches thick. Which in turn is resting on a red or
brownish red hardpan. There are more than 1500 soil series
recognized in California. One reason for the cataloging of
these soils is for the planning of crop types and the water
use for those crops. Another reason is to determine what types
of construction the soils can support. In 1983, the type location
for the San Joaquin soil was relocated to a site north of
Lodi, California, in San Joaquin County. At that time, a preserved
5 foot profile section of the San Joaquin soil was sent to
the Netherlands World Soil Museum in Wageningen, Holland.
Samples are also on file with "Benchmark Soils" a national
listing of soil series considered representative of soils
in Major Land Resource Areas (MLRA) in the United States.
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