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53 Cards in this Set

  • Front
  • Back
mineralogy
the branch of geology that studies the composition, structure, appearance, stability, occurrence, and associations of minerals.
mineral
a naturally occurring, solid crystalline substance, generally inorganic, with a specific chemical composition.
atom
smallest unit of an element that retains the physical and chemical properties of that element.
nucleus
center of every atom, contains almost all of the mass of the atom, has protons and neutrons.
proton
positive electrical charge
neutron
electrically neutral, uncharged.
electrons
cloud of moving particles, negative electrical charge, has a mass so small that it is conventionally taken to be zero.
atomic number
number of protons in the nucleus of an atom
atomic mass
sum of the masses of its protons and neutrons.
isotopes
atoms with different numbers of neutrons.
chemical reactions
interactions of the atoms of two or more chemical elements in certain fixed proportions that produce chemical compounds.
electron sharing
mechanism by which a covalent bond is formed between the elements in a chemical reaction
electron transfer
mechanism by which an ionic bond is formed between the elements in a chemical reaction.
cation
positively charged ion.
anion
negatively charged ion
ionic bond
bond between atoms formed by electrical attraction between ions of the opposite charge.
covalent bonds
bond between atoms in which the outer electrons are shared.
metallic bond
covalent bond in which freely mobile electrons are shared and dispersed among ions of metallic elements, which have the tendency to lose electrons and pack together as cations.
crystallization
growth of a solid from a gas or liquid whose constituent atoms come together in the proper chemical proportions and ordered three dimensional arrangement.
crystal
an ordered 3d array of atoms in which the basic arrangement is repeated in all directions.
precipitate
to drop out of a saturated solution as crystals
polymorphs
one of two or more alternative possible crystal structures for a single chemical compound.
hardness
measure of the ease with which the surface of a mineral hardness based on the ability of one mineral to scratch another.
Mohs scale of hardness
an empirical, ascending scale of mineral hardness based on the ability of one mineral to scratch another.
cleavage
tendency of a crystal to break along flat planar surfaces.
fracture
tendency of a crystal to break along irregular surfaces other than cleavage planes.
luster
how the surface of a mineral reflects light
color
imparted by light-either transmitted through or reflected by crystals or irregular masses.
streak
color of the fine deposit of mineral dust left on an abrasive surface, such as tile or glazed porcelain, when a mineral is scraped across it.
density
mass per unit volume
specific gravity
weight of a mineral divided by the weight of an equal volume of pure water at four degrees Celsius.
crystal habit
shape in which its individual crystals or aggregates of crystsal grow
rock
naturally occurring solid aggregate of minerals, or, in some cases, nonmineral solid matter.
texture
describes the sizes and shapes of its mineral crystals and the way they are put together.
igneous rocks
rocks formed by the solidification of molten rock.
sedimentary rock
rocks formed as the burial products of layers of sediments.
metamorphic rocks
rocks formed by the transformation of preexisting solid rocks under the influence of high pressure and temperature.
intrusive igneous rocks
a rock formed by the solidification of a magma, before or after it reaches the surface.
extrusive igneous rocks
form from rapidly cooled magmas that erupt at the surface through volcanoes.
sediments
layers of loose particles, such as sand, silt, and the shells of organisms.
weathering
chemical and physical processes that break up and decay rocks into fragments of various sizes.
siliciclastic sediments
physically deposited particles.
chemical and biochemical sediments
new chemical substances that form by precipitation when some of a rock's components dissolve during weathering and are carried in river waters to the sea.
lithification
process that converts sediments into solid rock, and it occurs either by compaction or cementation.
bedding
the formation of parallel layers of sediment as particles settle to the bottom of the sea, a river, or a land surface.
regional metamorphism
occurs where high pressures and temperatures extend over large regions, as happens where plates collide, takes place over large areas.
contact metamorphism
where high temperatures are restricted to smaller areas, such as the rocks near and in contact with an intrusion
foliation
wavy or flat planes produced when the rock was structurally deformed into folds.
rock cycle
the set of geologic processes that convert each type of rock into the other two types.
ores
rich deposits of minerals from which valuable metals can be recovered profitably.
hydrothermal solutions
a hot solution formed around bodies of molten rock when circulating groundwater comes into contact with a hot intrusion, reacts with it, and carries off significant quantities of elements and ions released by the reaction.
vein deposits (veins)
sheetlike deposits of precipitated minerals in the fractures and joints
erosion
set of processes that loosen soil and rock and move them to the spot where they are deposited as layers of sediment.