rocks Flashcards
types of rocks
Igneous
Sedimentary
Metamorphic
rock cycle
All rocks on Earth are locked into a system of cycling and re-cycling.
Sedimentary rocks
Rocks that are formed from erosion, deposition, and cementation.
Igneous
rocks that are formed from melting and cooling
Metamorphic
rocks that are formed by changing temperature and pressure
Intrusive Igneous rocks
Slow cooling deep beneath the Earth’s surface allows crystals to grow to a large size (1/8” or more). These crystals are easily visible
Extrusive Igneous rocks
Rapid cooling near or at the Earth’s surface produces many small crystals that are not readily seen by the unaided eye. Typically volcanic in origin, and Cooling may be so rapid that crystals do not have a chance to form and instead a glass is produced.
Granite
a coarse to medium-grained rock that forms from the cooling of magma deep within the Earth (intrusive). It is made up mainly of varying amounts of the minerals: quartz, orthoclase, muscovite, biotite and hornblende. The name is from the Latin granum, for “grains”.
PEGMATITES
classified as intrusive igneous rocks, but there is a difference. They are VERY coarse grained and strictly speaking are not crystallizing out of a magma.
Diorite
very similar to granite, but is distinguished in the hand specimen by the absence of visible quartz.
Generally it has a salt and pepper appearance
Gabbro
a coarse-grained rock that is high is iron & magnesium-bearing minerals (pyroxenes, amphiboles, plagioclase feldspar, olivene). The rocks will be dark in color, somewhat heavier than granitic rocks and devoid of quartz.
Peridotite
or DUNITE is composed of 90-100% olivine. As a result it is characteristically olive-greens in color.
This material is thought to have originated in the upper mantle of the Earth.
RHYOLITE
name comes from the Greek rhyo, from rhyax, “stream of lava”. It is formed when molten rock with the same composition as a high silica granite oozes to the Earth’s surface; and therefore cools quickly so only microscopic-
ANDESITE
is the fine-grained equivalent of DIORITE. It tends to be a darker gray than rhyolite and is often porphyritic, with visible hornblende.
BASALT
occurs as thin to massive lava. flows, sometimes accumulating to thicknesses of thousands of feet and covering thousands of square miles.
dark, fine-grained and often vesicular (having gas pockets). The pockets may be filled with secondary minerals