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mineralogy
study of minerals
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mineral
any naturally occuring inorganic solid that possesses an orderly crystalline structure & well defined chemical composition; occurs in nature, is solide, orderly repetitive structure that can be expressed in a chemical formula
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rock
any solid mass of mineral or mineral like matter that occurs naturally as part of our planet
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aggregate
several different items like minerals in one rock (granite is a rock made up of several minerals)
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atom
smallest particule that cannot be chemically split
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make up of atoms
# of protons and neutrons in the center usually the same # with electrons that surround the atom also usually the same amount
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valence electrons
interact with other atoms to form chemical bonds
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atomic mass
the number of protons in an atom that determines its chemical nature
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element
group of the same kind of atom (90 natural & 23 synthesized)
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chemical compound
elements that join with others to form a mineral
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octet rule
atoms tend to gain, lose or share electrons until they are surrounded by 8 valence electrons
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chemical bond
transfer of sharing of electrons that allows each atom to attain a full valence shell of electrons
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ionic bonds
electrons are transferred between the atoms
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covalent bond
electrons are shared between the atoms
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metallic bond
electrons are shared among all the atoms in the element
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mass number
total number of protons and neurtons in an atom
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isotopes
an atom ith the same # of protons to make an element but a different number of neutrons
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radioactive decay
the nuclei changes through random process becoming unstable isotope radiating energy & emit particles is used to measure age of fossils, rocks and minerals
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optical property
used in identification of minerals and is luster, light transmission, color and streak of a mineral
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luster
the appearance or quality of light that is reflected from the surface of the mineral (how the light hits the mineral)
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metallic luster
appears to look like it is a metal
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submetallic luster
is not as shiny as metal as if freshly broken, has a dull or tarnished appearance from the exposure to air
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nonmetallic luster
described as having vitreous (glasy look), dull (earth luster like soil), pearly luster (like inside of clam shell) or silky luster (as if coated in oil)
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opaque
no light will go through the sample
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translucent
you see light through but no image can be seen through the sample
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transparent
both light and image can be seen through the sample
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color
the color of the sample can be misleading especailly for those that have several tints such as quartz
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streak
the color of the powdered mineral that is obtained by rubbing the sample across a streak plate (unglazed porcelain piece) can help identfy the color of the mineral as will always have same streak color no matter the color of actual sample & distinguishes between metallic luster and nonmetallic luster
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crystal shape (habit)
the shape of the crystall or aggregate of crystals
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hardness
the resistance to abrasion or scratching
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mohs scale
gives # value of hardness with diamond having the hardest of 10 and talc having the lowest of 1
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cleavage
the tendecy of a mineral to break along planes of weak bonding, with a # of cleavage directions and angles at which they meet
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fracture
having a chemical bond that equally or nearly so strong in all directions
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irregular fracture
produces uneven surface
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conchoidal fracture
breaks into smooth, curved surfaces like broken glass
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splintery fracture
breaks into splinters
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fibrous fracture
breaks into fibers
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density
mass per unit volume
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specific gravity
is used to describe the density, unit less # representing ratio of minerals weight to the weight of an equal volume of water
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other properties of minerals
the taste, feel, smell, magnetic and ability to interact with acid
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double refraction
when a transparent piece is placed over letters they appear to be seen twice
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rock forming minerals
the minerals of the earth's surface
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economic minerals
those used extensively in the manufactur of products
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8 elements that are in bulk of rock forming minerals 98% of the continental crust by weight
- oxygen
- silicon
- aluminum
- iron
- calcium
- sodium
- potassium
- magnesium
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silicates
they are made up of oxygen and silion that are the basic building blocks of the group
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nonsilicates
other mineral groups they are far less abundant
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silicate minerals
contain oxygen and silicon plus 1 or more additional elements
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silicon oxygen tetrahedron
4 oxygen atoms that surround the smaller silicon atom
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mineral resources
earth's storehouse of useful materials that can be recovered for use
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reserves
already idenified deposits from which minerals can be extracted profitably
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ore
useful metallic minerals that can be mined for profit
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why is silica the major component of magma
it is abundant and can crystallize at any tempature depending on the othe chemicals with it
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