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Earth Materials
refer to substances or objects extensively used in geological and biological processes on the surface of the planet.
Earth Material
Minerals, Rocks, Energy Sources, Soil and Water
Mineral
It is a naturally occurring, inorganic, homogeneous solid, with a definite chemical composition, and an ordered crystalline structure.
Characteristics of Minerals
Homogenous
Naturally formed
Inorganic Substance
Solid
Definable Chemical Composition
Crystalline Structure
Solidification
Freezing
Precipitation
dissolved in the water bond and separate out of the water
Solid-State Diffusion
movements through a solid and resulting to crystal lattice.
Biomineralization
animals produces minerals
Fumarolic Mineralization
precipitation directly from gases
Physical Properties of Minerals
Color
Streak
Luster
Crystal habit
Color
refers to certain wavelengths of light that are reflected by a mineral and is perceived by the observer
Streak
is the color of the powdered form of a mineral.
Luster
is the appearance of the mineral surface and is dependent on how it reflects light
Crystal habit
is the characteristic shape in which a mineral grows and is a projection of the mineral’s crystal structure.
Allochromatic minerals
color is not a reliable diagnostic property since small impurities may dramatically alter their color.
idiochromatic minerals
are strongly colored which drowns out any impurities in color.
Pseudochromatic minerals
Are false-colored minerals. Their colors are due to light diffraction.
Physical Properties of Minerals 2
Cleavage
Fracture
Hardness
Specific Gravity
Cleavage
is the tendency of some minerals to break along flat surfaces.
Fracture
is the pattern in which the mineral breaks aside from its planes of cleavage.
Hardness
is the resistance of the minerals to scratching.
Specific Gravity
is the ratio of a minerals’ weight to the weight of an equal volume of water.
Mohs Scale of Hardness
talc
gypsum
calcite
flurite
apatite
feldspar
quartz
topaz
corundum
diamond
Ionsdaleite
58% harder than diamond.
Solubility
refers the ability of a substance to dissolve in a solvent at a specified temperature.
Melting point
refers to the temperature at which solid turns into liquid.
Elements
Most of the minerals here are composed of only one element. Having knowledge about elements enables scientists to identify bonding possibilities and compounds that can be created.
Elements Example Minerals
copper, gold, silver, sulfur.
Sulfides
Minerals under these group are composed of a metal joined by a sulfur. Metallic luster is the characteristic that distinguish them.
Sulfides Example Materials
cinnabar(HgS), pyrite(FeS2)
Halides
These are nonmetal groups which consists of chlorine, fluorine, bromine, and iodine as their main chemical constituent.
Halides Example Materials
fluorite(CaF2), halite(NaCl), diabolite
Oxides and hydroxides
These are mineral groups composed of one or more metals joined with oxygen, water, or hydroxyl (OH)
Oxides and hydroxides Example Materials
cuprite(Cu2O),hematite(Fe2O3)
Nitrates, carbonates, borates
It is formed when a metal is combined with carbon, nitrogen and boron.
Nitrates, carbonates, borates Example Materials
malachite,nitratine, borax
Sulfates
One or more metal is combined with a sulfate compound (SO4)
Sulfates Example Materials
anhydrite (CaSO4)
Chromates, molybdate, tungstates
substituted the place of the sulfate group. These minerals are usually brightly colored, brittle and dense.
Chromates, molybdate, tungstates Example Materials
wulfenite(PbMoO4), scheelite(CaWO4)
Phosphates, arsenates, vanadates
One or metal is chemically combined with the Phosphates, arsenates, vanadates group.
Phosphates, arsenates, vanadates Example Materials
apatite, lazulite,vanadinite
Silicates
This is the largest mineral group. Minerals under this group have different amounts of silicon and oxygen
Silicates Example Materials
dioptase,labradorite