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Geo midterms
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Mineralogy
is concerned with all aspects of mineral.
Mineral
is a naturally solid and inorganic substance which forms the earth.
Smoky
Quartz
is a mineral that is composed of silicon and oxygen (SiO2).
Crystalline
structure
means that the atoms inside the mineral are arranged in a symmetrical manner.
Obsidian
is also called as volcanic glass and has no internal structure. It is not considered a mineral.
Fixed
or
variable
chemical
composition
means that each mineral has its own chemical composition.
Quartz
in the form of
amethyst
has a fixed chemical composition.
Color
should not be relied upon.
Luster
is how the surface of the mineral
reflects
light.
Streak
is the color of the mineral as a powder.
Cleavage
is the direction of the weakness of a mineral.
Fracture
is the breakage of the mineral.
Hardness
is the strength of the mineral to resist scraping and puncture.
Talc
is the softest mineral.
Diamond
is the hardest mineral.
Crystal
shape
means that all minerals are crystalline but some doesn't have the opportunity to show their crystal form.
Acid reaction
distuingish small number of minerals with some properties.
Magnetism
is the reaction when a small magnet reacts to the mineral.
Magnetite
is the most common mineral that is magnetic.
Specific
gravity
is the density of the mineral.
Feldspar
is the most abundant group of minerals on earth.
Petrology
is the study of rocks.
Igneous
rocks
are formed by solidification of molten magma.
Aphanitic
fine-grained, less than 1mm, grains not seen with the unaided eye.
Phaneritic
coarse-grained, visible crystal and 1 to 10 mm.
Pegmatitic
very coarse grained, 1 cm.
Porphyritic
composed of both large and fine-grained crystals.
Vesicular
rocks that have vesicles resembling a sponge.
Pyroclastic
fragmented angular grains ejected during the eruption.
Glassy
when lava cools quickly.
Intrusive igneous
rocks
crystallize below the earth's surface.
Extrusive
igneous
rocks
erupt into the surface resulting in small crystals as the cooling take place quickly.
Granite
is a hard igneous rock made of clearly visible crystals of various minerals.
Basalt
is a dark-colored fine-grained igneous rock.
Pumice
is a light igneous rock with thousands of tiny bubbles.
Sedimentary
rocks
are from pre-existing rocks or pieces of once living organisms.
Clastic sedimentary
rocks are from accumulation and lithification of mechanical weathering debris.
Chemical
sedimentary rocks form when dissolved materials precipitate from solutions.
Organic
sedimentary rocks form from accumulation of plant or animals debris.
Metamorphic
rocks have been modified by heat, pressure, and chemical process.
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