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What is it and where is it formed? Hematite is a
mineral
that is often found where there used to be water, hot springs, or volcanoes.
Hematite is an ore of iron which means that iron is in it. It is formed in
igneous,
sedimentary, and
metamorphic rocks but mainly in
granite and limestone. |
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How and where is it mined? Hematite is mined using
underground mining. It is mined in England, Mexico, Australia, Canada, and
Brazil. |
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What is it used for?
Hematite is sometimes used as a
gemstone. Ground up hematite is red or reddish brown
and is used for dying things. Is also used in paints. |
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Interesting! Chinese doctors sometimes use hematite to
cure sickness. |
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Mineral Characteristic |
What the
mineralogists say |
Kid's Guide: What it REALLY
means! |
| Chemical Symbol |
Fe2O3 |
Hematite has iron and oxygen in it. |
| Color |
Mostly
black or red |
These are the most common colors of hematite. |
| Streak |
Red |
If
you crushed hematite, the dust that was formed would be red. |
| Transparency |
Opaque |
You can’t see through it. |
| Luster |
Metallic or earthy |
If
you shine a light on this mineral, it might be glossy or dull. |
| Cleavage |
None |
When broken, it doesn’t have a pattern to how it splits. |
| Fracture |
Jagged |
If
broken, the pieces would look jagged and uneven. |
| Magnetism |
Yes |
It
will attract and be attracted to a magnet if it is heated. |
| Hardness |
5-6 |
Only something as hard as a steel file will scratch this. It is hard. |
| Specific gravity |
5.3 |
Slightly heavier than most metals. |
| Crystal Shape |
Hexagonal |
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Hematite was found
on Mars, a planet that used to have more
water. |
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Links:
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Citations:
Fuller,
Sue. Rocks & Minerals. London: Dorling Kindersley, 1995.
"Hematite." 24 Oct. 2005 <http://webmineral.com/data/Hematite.shtml>.
"Hematite." 3 Nov. 2005 <http://mineral.galleries.com/minerals/oxides/hematite/hematite.htm>.
“Iron
Ore: Hematite, Magnetite & Taconite.” 21 Oct. 2005.
<http://www.mii.org/Minerals/photoiron.html.
Pellant, Chris. Rocks and
Minerals.
New
York: Dorling Kindersley, 1992.
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