EARTH'S ROCKS Flashcards
aggregation of different
mineral constituents which
form the earth’s crust
rocks
are scientists who study a planet’s
solid features, like soil, rocks, and
minerals
Geologists
process in which rocks are
continuously transformed
between the three rock types
igneous, sedimentary and
metamorphic
Geological
classification
Sedimentary rocks
Igneous rocks
Metamorphic rocks
Physical classification
Stratified rocks
Unstratified rocks
Foliated rocks
Chemical
classification
Argillaceous rocks
Calcareous rocks
Siliceous rocks
Physical classification and Chemical classification of sedimentary
Stratified rocks & Argillaceous rocks
Physical classification and Chemical classification of igneous rocks
Unstratified rocks & Calcareous rocks
Physical classification and Chemical classification of metamorphic rocks
Foliated rocks & Siliceous rocks
➢from the word ignis, which means “fire” in Latin
Igneous rocks
the word ignis, which means
“fire” in Latin
are formed by the solidification of magma below the earth’s surface
Igneous rocks
molten rock that is
underground and lava for
molten rock that breaks
through the Earth’s surface
Magma
process that turns any
rock into magma
Melting
requires extremely high
temperatures, which only
occur far beneath the
earth’s surface
Melting
the process that hardens
magma and turns it into
igneous rock
Cooling
can occur either underneath or
on the earth’s surface
Cooling
2 types of igneous rocks
Intrusive Igneous Rocks
Extrusive Igneous Rocks
➢also called plutonic rocks
➢cool slowly without ever reaching the surface
Intrusive Igneous Rocks
➢have large crystals that are usually visible without a
microscope
➢surface is known as a phaneritic texture
Intrusive Igneous Rocks
Intrusive Igneous Rocks suface is known as a
phaneritic texture
best-known phaneritic rock is
granite
extreme type of phaneritic rock is called
pegmatite
have a huge variety of crystal shapes and sizes,
including some larger than a human hand
Pegmatite
- extreme igneous rocks
- form during the final stage of a magma’s crystallization
Pegmatites