Rocks Materials of the Solid Earth Flashcards
(96 cards)
The rock cycle is a good model for thinking about the transformation of one rock to another due to Earth processes. . Given the right conditions, any kind of rock can be transformed into any other kind of rock.
Rock Cycle
form when hot, molten rock crystallizes and solidifies
Igneous rocks
Completely or partly molten rock that is below Earth’s surface. It consists of a liquid
melt that contains gases (volatiles) such as water vapor, and it may contain solids (mineral crystals).
Magma
Completely or partly molten rock that is on the Earth’s surface
Lava
Molten rock cools and solidifies
Crystallization
When molten rock solidifies at the surface
Extrusive or Volcanic rock
Most magma loses its mobility before reaching Earth’s surface and eventually crystallizes deep below the surface.Igneous rocks that form at depth
Intrusive or Plutonic rock
If the molten material is cooled almost instantly, there is insufficient time for the ions to arrange themselves into a crystalline network. Solids produced in this manner consist of randomly distributed atoms.
Glass
Instant quenching sometimes occurs during violent volcanic eruptions that produce tiny shards of glass
Volcanic ash
Igneous rocks in which is composed almost entirely of light colored silicates such as quartz and potassium feldspar and contain about 10 percent dark silicate minerals
Granitic or Felsic
Rocks that contain at least 45 percent dark silicate minerals and calcium-rich plagioclase feldspar (but no quartz)
Basaltic or mafic
rocks with a composition between granitic and basaltic rocks and contain at least 25 percent dark silicate minerals, mainly amphibole, pyroxene, and biotite mica, with the other dominant mineral being plagioclase feldspar.
Andesitic or intermediate
Igneous rocks that has very low silica content and composed mostly of olivine minerals.
Ultramafic
the overall appearance of a rock, based on the size, shape, and arrangement of its mineral grains
Texture
Igneous rocks that form at Earth’s surface or as small intrusive masses within the upper crust, where cooling is relatively rapid. The crystals that make up fine-grained igneous rocks are so small which can be distinguished only with the aid of a polarizing microscope or other sophisticated techniques
Fine-grained texture
When large masses of magma slowly crystallize at great depth. Consist of a mass of intergrown crystals that are roughly equal in size and large enough so that the individual minerals can be identified without the aid of a microscope
Coarse-grained texture
developed when magma that has been slowly cooling and crystallising within the Earth’s crust is suddenly erupted at the surface, causing the remaining uncrystallised magma to cool rapidly.
Porphyritic texture
The large crystals in porphyritic rocks
Phenocryst
The matrix of smaller crystals wherein larger crystals are embedded.
Groundmass
Igneous rocks that have voids left by gas bubbles that escape as lava solidifies.
Vesicular texture
Nearly spherical openings as lava solidifies
Vesicles
Molten rock that is is quenched and cools quickly to become a solid.
Glassy texture
Formed from the consolidation of individual rock fragments ejected during explosive volcanic eruptions.
Pyroclastic (fragmental) texture
As magma cools, certain minerals crystallize first at relatively high temperatures. At successively lower temperatures, other minerals begin to crystallize.
Vowen’s reaction series