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What is it and where is it formed? Quartz
is the most common
mineral in the Earth’s crust. Quartz is in
sandstones,
granites, and other
igneous rocks. It forms
veins in
the cracks of rocks. There is a lot of heat and water
where they form. Crystals are made when the quartz cools down. The way the crystal looks
depends on how hot it was when it was formed. Quartz is a part
of almost any kind of rock—igneous,
sedimentary, and
metamorphic. It can be found in layers or geodes, too. Geodes
are hollow rocks that are lined with crystals. |
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How and where is it mined? Quartz is mined
by surface mining most of the time. A backhoe is used to take
away the dirt and rock that is covering the vein. Only large
mines own and use heavy equipment all the time. The miners
might blast with explosives but they will use the littlest
amount that will get the job done. They don’t want to take a
chance of ruining the quartz with the blast. When the quartz
vein is uncovered, everything slows down so that the heavy
equipment won’t ruin the minerals. They will work by hand with
a pick and shovel once they can see the quartz. They might use
chisels, pry bars, and dentist tools to get the quartz out
without wrecking it. If it is damaged at all, it might not sell
for as much money. The quartz is taken out, wrapped in
newspaper, and put in some kind of box or pail until it can be
taken away to be cleaned. Quartz is mined in: Brazil and
the U.S.A. [Arkansas]. |
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What is it used for? Quartz is used in
radios, as crystal gems, sandpaper, soap, prisms, glass, paints,
clocks, watches, and computers. It is used for radar, radios,
and TVs because it conducts electricity. |
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Quartz is sometimes used as a crystal ball
for telling the future or for telling people what
diseases they have. |
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Pure quartz is clear. Many kinds
fluoresce. Mostly they make a white or green color. |
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Mineral Characteristic |
What the
mineralogists say |
Kid's Guide: What it REALLY
means! |
| Chemical Symbol |
SiO2 |
It
has oxygen and silicon in it. |
| Color |
Most
common are clear, white, or cloudy. |
There are lots of colors of quartz but the ones that are
seen most often are clear, white, or milky. |
| Streak |
White |
If
it was ground up into a powder, it would be white.
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| Transparency |
Transparent to opaque |
You
might see through some, find others blurry to look
through, or not see through some at all. It really has
to do with how much light can pass through them. |
| Luster |
Vitreous |
If
you shine a light on the mineral, it looks glassy. |
| Cleavage |
None |
If
you break the mineral, it will not split cleanly. |
| Fracture |
Conchoidal |
Pieces of mineral have a smooth, shell-like surface when
they are broken. |
| Magnetism |
None |
It will
not attract, or be attracted to, a magnet. |
| Hardness |
7 |
It
is toward the top of the Moh’s scale of hardness. It is
hard and can scratch glass which is hard. |
| Specific gravity |
2.65 |
It
is not very heavy. |
| Crystal Shape |
Hexagonal |
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Quartz is hard and is sometimes used to
test how hard other minerals are. You would use the quartz to
scratch other minerals. If it made a scratch mark, the mineral
would be softer than the quartz. If the mineral didn’t get
scratched, it would mean that the mineral was harder than the
quartz.
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Links:
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Citations:
Kolk, Melinda. veinofquartz.jpg. 1-Dec. Pics4Learning. 20 Dec
2005 <http://pics.tech4learning.com>.
“Many varieties of quartz.” Minerals-n-more.com. 24 Oct. 2005.
<http://www.minerals-n-more.com/Info_Quartz_Family.html>.
“Quartz.” Raintree Illustrated Science Encyclopedia. 1991 ed.
“Quartz.” World Book Encyclopedia. 2000 ed.
"Quartz." San Diego Natural History Museum. 21 Feb. 2006
<http://www.sdnhm.org/fieldguide/minerals/quartz.html>.
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