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Dolostone is one of the most common rocks in our
neighborhood. People use it as gravel on
their paths and driveways. Road builders mix it with concrete and
asphalt, and railroads use it for ballast.
Dolostone formed in ancient seas, often in coral reefs, and it sometimes contains fossils. To learn more about dolostone, scroll farther down this page. |
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| Here's some dolostone gravel, dug out of a quarry near our home. | ||
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| This truck is
dumping a load of dolostone on our street. |
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| How to recognize dolostone | |
| Other rocks that look like dolostone | |
| Special things to look for | |
| Where dolostone came from | |
| How dolostone formed | |
| Other names for dolostone | |
| Links to Web sites about dolostone |
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Limestone:
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White
Marble:
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White Chert: Pieces of chalky white chert are often mixed with
dolostone gravel.
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Gray Slag:
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Look for fossils. The left arrow points to a piece of brachipod fossil. The right arrow points to a small coral fossil. |
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Look for masses of crystals. These quartz crystals filled an open space, or vug, within the dolostone rock. (The specimen is about an inch wide.) |
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Look for white and gray chert pieces in dolostone gravels. (Chert is harder than dolostone, looks smoother, and breaks to form sharp edges.) |
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Look for fools'
gold (pyrite or marcasite) crystals. The dark specks on these
rocks look like brassy metal under our Intel
Play QX3 computer microscope.
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The dolostone in our area was blasted out of huge quarries, like this one near Brookfield, Illinois. See the tiny dump trucks in this picture? Each one carries tons of crushed dolostone that will be used to make and repair roads and parking lots -- or mixed in concrete to build homes and offices. |
Our dolostone started out as skeletons of corals,
sponges, and other animals that lived in a shallow
sea that covered our area more than 400 million
years ago. The skeletons accumulated on the sea
floor as huge mounds, called reefs, and as layers
of sand- and mud-sized bits of skeleton.
These deposits could have formed limestone rock,
except that something happened to change their
chemistry. Sometime after burial, the "lime" in the
skeletons (the minerals calcite and aragonite)
changed into a new mineral, called dolomite.
So, instead of limestone, we have dolostone!
We use the scientific name "dolostone" for this
rock,
but it is also known by many other names:
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Here are some ways to classify dolostone
(by grouping it with similar types of rocks):
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Here's a Web site detailed information about the
types of reefs where our local dolostone formed:
< http://www.mpm.edu/reef/welcome.html
>
It includes a look a Thornton Quarry, which is
pretty close to our home:
< http://www.mpm.edu/reef/thornton-front.html
>
There are also fossilized Silurian-age reefs in Norway.
Visit one here:
< http://www.toyen.uio.no/palmus/galleri/montre/english/m_silurrev_e.htm
>
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Copyright 2001 Eric D. Gyllenhaal
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This page was created on March 12, 2001, and it was last updated on July 27, 2002.