Atoms to Minerals

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Created by:

awagner123  on January 9, 2011

Subjects:

earth science

Classes:

Wagner 8th grade

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Atoms to Minerals

Mineral
A naturally occurring, inorganic solid with a definite chemical composition.
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Mineral A naturally occurring, inorganic solid with a definite chemical composition.
Ag used in film developing
Cu used in electrical wiring
Gypsum used in drywall aka wall board
Phosphorous used in fertilizer
Halite rock salt also table salt
Graphite used in pencils
Calcite reacts with acid (HCl)
Calcite makes up limestone, which "saves PA from acid rain"
atom smallest part on an element with all of the characteristics of the element
molecule smallest part of a compound with all of the characteristics of the compound
compound combination of two or more elements in a specific ratio
proton (p+) positive charged atomic particle found in the nucleus
neutron (n) neutral atomic particle found in the nucleus
electron (e-) negatively charged atomic particle orbiting the nucleus (1836 times smaller than a proton)
isotope different types of atoms of the same chemical element, each having a different number of neutrons
ion An atom or a group of atoms that has acquired a net electric charge by gaining or losing one or more electrons.
covalent bond characterized by two non-metals sharing of pairs of electrons between atoms.
ionic bond type of bond that involves a metals and a nonmetal. The metal donates one or more electrons
metallic bond the bonding of metals to metals
John Dalton "Father of Modern Chemistry"
Niels Bohr Model of atom
40,000 How many pounds of minerals does a person use each year?
Silicates (SiO2) The most common mineral family in the Earth's crust
Oxygen The most common element in the Earth's surface
Silicon The second most common element in the Earth's surface
The Atomic Number also tell how many e- and p+ are in the atom
protons + neutrons= mass number use this formula to calculate # of n in atom
"Hoffman's Law" " Don't mess with the protons!"
Luster the shine or lack of shine of a mineral (either metallic or non-metallic)
Crystal Shape the way atoms align themselves to make flat planes
Streak color of mineral's powder
Cleavage the way a mineral breaks along a flat surface
Hardness resistance to being scratched
Friedrich Mohs developed a scale 1-10 using commonly known minerals
Fluorescence glows with UV light
Phosphorescence glows in dark
double refraction calcite exhibits this (seeing double)
radioactivity causes a Geiger counter to react
Metallic minerals usually leave a dark streak and have densities of 5g/cm3 or greater
Non-metallic minerals usually have a light or no-color streak and have densities less than 5g/cm3
Density = mass divided by volume (D=m/v) What is the equation for Density?

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