Volcanoes Flashcards
Intrusive Rock is
Plutonic Rock
Magma Behavior determined by (3)
temp
composition
dissolved gases
Liquid
Melt
Solid in Lava are
Silicate
Volatiles are (3)
water vapor, co2, so2
Lava is
Extruded Magma
Aa Flow (2)
Basalatic lava
rough jagged blocks
Pahoehoe Flow (2)
basaltic lava
smooth surfaces
Another name for Pyroclastic Flow
Nuee Ardente
Nuee Ardente (3) generated by
collapse of eruption columns
Crater
a funnel-shaped depression at the summit of most volcanic cones, generally less than 1 km in diameter
Caldera
a volcanic crater that has a diameter of >1 kilometer and is produced by a collapse following a massive eruption
Volatiles
1-6 percent of total, water/co2
Bomb
hot lava greater than 2.5 inches, streamlined in air (meteor)
Hot temperature
decreases viscosity
Dissolved water
decreases viscosity by inhibiting formation of silica tetrahedra chains
Violence of Eruption
Gases expand near surface due to decreasing pressure; related to how easily gases escape
Silica Composition
Increases Viscosity
Tetrahedra
silicate structures linking together in chains early in crystallization process
Shield Volcanoes (3)
Large Area, Broad/dome shaped
Produced by MILD eruptions
Cinder Cones or
Scoria Cones
Composite Volcanoes or
Stratovolcanoes
Cinder Cones (3)
Small size/groups
Extensive Lava Fields
Steep Slope
Composite Volcanoes (3)
large/classic shape
symmetrical cone
layers of pyrcolastic debris
Volcanic Neck
remains of magma solidified in conduit
Volcanic Conduit
circular pathway from fissure to surface
Bowen’s Reaction Series
Minerals Crystallizes in systematic fashion based on melting points
Crystal Setting
earlier, dense minerals settle towards bottom
Magmatic Differentiations
one magma->two different magma
Assimilation
magma melts and incorporates other
Magma Mixing
Buoyant overtakes slow moving
Partial Melting
melt enriched in ions from lowest melting temperture minerals
Flow of Partial Melting
Ultramafic->Mafic->Intermediate->Felsic
Resurgent Dome
Magma bounces back up in caldera
Resurgent Dome Caldera
Yellowstone
Flood Basalt
eruptions from fissues
Large Igneous Province
Basalt Plateau
Composite Volcano Flow
Andesitic
Composite Volcano Location
Ring of Fire
Shield Volcano Location
Ocean
Shield Volcano Flow
Basaltic
Pipe
super long conduit
Divergent Plate Boundaries
Fluid/Basaltic Lava
Intraplate Volcanism has
mantle pumes
Superplumes are responsible for
flood basalts
remoting sensing devices test
silicon dioxide emissions
Igneous Rock goes to
Metamorphic Rock
Igneous to Metamorphic
heat and pressure
Sedimentary Rock goes to ___ via
Metamorphic via heat and pressure
Parasitic Cone
Flank Vent emitting lava/pyroclastic material
Fumaroles
flank vent emits gases
Calderas
circular, steep-sided depressions with a diameter >1 km
Crater Lake Calderas
Form from the collapse of the summit of a large composite volcano following an eruption; these calderas eventually fill with rainwater
Hawaiian type calderas
: Form gradually from the collapse of the summit of a shield volcano following the subterranean drainage of the central magma chamber
Yellowstone Calderas
Form from the collapse of a large area after the discharge of large volumes of silica-rich pumice and ash; these calderas tend to exhibit a complex history