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19.
American Stores Tower
PI-60 Building Stones of Downtown
Salt Lake City, A Walking Tour
Rockville
Granite is a coarse-grained granite containing larger crystals of
white feldspar with smaller crystals of quartz and black mica. Photo
courtesy of Terry Boerboom, Minnesota Geological Survey.
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299 South Main Street
Completed in early 1998, this 24-story, flat-topped structure is
partially covered by three different building stones. (The flat
top was designed for a helicopter landing pad.)
The black rock, "Cold Spring Black" (trade name), was quarried
near Alma in Quebec, Canada; the dark gray diorite, "Academy Black,"
was quarried northeast of Fresno, California in the Sierra Nevada
foothills; and the light gray granite, "Rockville White," was quarried
near the small town of Rockville, Minnesota.
Dark gray and black granite-like rocks called "black granite"
in the building stone industry are usually diorite or gabbro to
geologists. Diorite is dark gray to blackish-gray igneous rock mainly
composed of sodium-rich plagioclase feldspar, hornblende, pyroxene,
and a small amount of quartz. Gabbro is dark-colored, coarse-grained
igneous rock characteristically composed of calcium-rich plagioclase
feldspar, pyroxene, and possibly olivine.
"Cold Spring Black" is a mafic (contains iron and magnesium) metamorphic
rock that most likely formed during the early Precambrian over 2.5
billion years ago. Originally, it was probably a gabbro that was
later subjected to low-temperature, low-pressure metamorphism as
it was uplifted.
"Academy Black" contains crystals of hornblende and pyroxene interlocking
with smaller crystals of plagioclase feldspar. It is part of the
Knowles Granodiorite which formed during the early Cretaceous Period
around 110 million years ago.
"Rockville White" comes from the approximately 1.8 billion-year-old
Rockville Granite. The Rockville Granite is one of several granite
bodies located in east-central Minnesota. This granite has been
quarried since the early 1900s and varies in color from a dominantly
pink to a dominantly white stone. It is coarse grained and consists
of larger crystals of pale pink to white feldspar with smaller crystals
of quartz and black mica.
Cross 300 South and Main Street and continue south down the
west side of Main Street until you reach the Frank E. Moss United
States Courthouse.
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