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Comprehensive vocabulary flashcards generated from lecture notes on magma formation, igneous rock types, textures, intrusive/extrusive settings, and general mineralogy.
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Igneous Rock
Rock that forms when hot molten rock (magma or lava) cools and freezes solid.
Magma
Molten rock located underground.
Lava
Molten rock located aboveground.
Volcano
A vent from which melt from inside the Earth spews out onto the planet's surface.
Pyroclastic Debris
Fragmented material that sprayed out of a volcano and landed on the ground or seafloor in solid form, which can cement together to form an igneous rock.
Phenocryst
A large or conspicuous crystal in a porphyritic rock, distinct from the groundmass
Extrusive Igneous Rock
Rock formed by the freezing of lava above ground, after it flows or explodes onto the surface and comes into contact with the atmosphere or ocean.
Intrusive Igneous Rock
Rock formed by the freezing of magma underground.
Wall Rock
The rock surrounding an igneous intrusion.
Magma Chamber
A space below ground filled with magma.
Geotherm
A graph showing how pressure and temperature interact inside the Earth, with temperature plotted on the x-axis and pressure on the y-axis.
Decompression Melting
Melting that takes place in locations where hot mantle rock rises to shallower depths (mantle plumes, beneath rifts, and beneath mid-ocean ridges), causing a decrease in pressure.
Volatiles
Substances (such as H2O or CO2) that evaporate easily and can exist in gaseous forms at Earth's surface.
Flux Melting
Melting that occurs when volatiles mix with hot, dry rock and break chemical bonds at the rock's melting point.
Heat-Transfer Melting
Melting that occurs when hot magma from the mantle is pushed to the surface and conducts heat to surrounding wall rock, causing it to melt.
Mafic Melts
Melts containing a high proportion of MgO and Fe2O3 relative to silica, with a SiO2 content of 46−52%.
Ultramafic Melts
Melts containing an extremely high proportion of MgO and Fe2O3 relative to silica, with a SiO2 content of 38−45%.
Felsic Melts
Melts containing relatively high proportions of SiO2 (67−76% SiO2) compared to MgO and Fe2O3; also called silicic melts.
Intermediate Melts
Melts whose chemical composition lies partway between mafic and felsic, containing 53−66% SiO2.
Partial Melting
The process by which only 2−30% of a source rock melts into magma because temperatures at sites of magma production do not get high enough to melt the entire rock.
Assimilation
The process of magma contamination in which blocks of wall rock fall into a magma chamber and dissolve.
Magma Mixing
The process where different magmas formed from different source rocks enter and mix within the same magma chamber.
Viscosity
A liquid's resistance to flow, which affects the speed of movement.
Fractional Crystallization
The process by which magma becomes progressively more felsic as it cools because mafic minerals crystallize first.
Lapilli
Pyroclastic particles measuring 2−64mm in diameter (marble-sized), consisting of frozen lava clots, pumice fragments, or ash clumps.
Ash
Tiny glass shards formed when volcanic spray immediately freezes and is carried by wind.
Pyroclastic Flow
A fast-moving avalanche that occurs when volcanic ash and debris mix with air and flow down the side of a volcano.
Intrusive Contact
The boundary between new intrusive igneous rock and the surrounding wall rock.
Dike
A tabular intrusion that cuts across pre-existing layering (bedding or foliation), radiating from a volcano or forming from rifting.
Sill
A tabular, horizontal sheet intrusion that injects between pre-existing rock layers.
Laccolith
A blister-shaped igneous intrusion formed when magma injects between underground layers and pushes the overlying layers up into a dome.
Pluton
An irregular or blob-shaped igneous intrusion ranging up to tens of kilometers wide.
Batholith
An immense intrusive complex formed by the intrusion of numerous plutons in a region.
Stoping
The process by which magma intrudes, where blocks of wall rock break off and sink into the magma.
Xenolith
A relict block of wall rock enclosed within intrusive rock after the magma freezes.
Phaneritic
A coarse-grained crystalline igneous texture in which individual mineral crystals are visible.
Aphanitic
A fine-grained crystalline igneous texture in which individual mineral grains are too small to see with the naked eye.
Porphyritic
An igneous rock texture consisting of large crystals (phenocrysts) surrounded by fine crystals (groundmass).
Pegmatite
A coarse-grained (phaneritic) igneous rock containing exceptionally large crystals up to tens of centimeters across, typically occurring in dike-shaped intrusions.
Vesicles
Open holes in igneous rock formed by gas bubbles preserved as magma cools and solidifies.
Obsidian
Vesicle-free felsic glass that is usually black or brown and fractures conchoidally.
Pumice
A felsic glass rock in which 75−90% of its volume consists of vesicles, formed from quickly cooled frothy lava.
Scoria
A mafic igneous rock with approximately 30% of its volume composed of large vesicles, generally more glassy than pumice.
Tuff
A fine-grained pyroclastic rock composed of volcanic ash or ash mixed with pumice lapilli.
Volcanic Agglomerate
An accumulation of volcanic bombs and other relatively large chunks of igneous rock.
Volcano Breccia
A pyroclastic rock consisting of fragments of volcanic debris that accumulated in the air or formed as solidifying lava broke up during flow.
Volcanic Arc
A chain of volcanoes developing along convergent plate boundaries, usually on the edge of the overriding plate.
Luster
The property describing the way a mineral surface scatters light.
Conchoidal Fracture
Smoothly curving, clamshell-shaped fracture surfaces produced when minerals (such as quartz) or glass break.