Volcanic Eruptions - MAGMAS Flashcards
Volcanoes are mostly found along
convergent boundaries
Much magmas are expelled along
divergent boundaries
the type of ____and consequent type of _____ of a volcano depends on the _____ it is formed
magma ; eruption ; tectonic setting
what are the three types of magma
basaltic, andesitic, rhyolitic
what is a magma
a magma is an extremely hot mixture of solid, gas, and liquid, located under Earth’s surface
what is the solid part of the magma
crystals
what are the gaseous part of the magma
H2O, CO2, SO2
what is the liquid part of the magma
molten rock
what type of magma are formed in an oceanic-oceanic subduction zone
basaltic or andesitic magma
what type of magma are formed in an oceanic-continental subduction
andesitic or rhyolitic
what type of magma is found in oceanic hotspot
basaltic magma
what type of magma is found in continental hot spot
rhyolitic magma
how does continental hotspot produce rhyolitic magma?
silica-poor basalt still rises toward the surface; as the magma rises, it melts its way trough thick, silica-rich continental crust forming shallow silica-rich (rhyolitic) magma chambers
silica content of basaltic magma
48-52%
silica content of andesite/dacite magma
52-68%
silica content of rhyolite magma
68-77% or >66%
silica content of ultramafic magma
<45%
t or f: as silica content increases, the silica structure of the magma becomes more 3D
T
t or f: high temperature magma have high viscosity
F (low viscosity)
the viscosity of magma increases with ____ SiO2 and ______ tempeature
increasing ; decreasing
they are the least viscous type of magma
basaltic magma
why are basaltic magmas least viscous?
they form in the upper mantle where the temperature is high and the SiO2 content is low
t or f: basaltic magmas are formed in the deep and hot upper mantle while andesite and rhyolitic magmas form at much shallower and cooler depths
T
t of f: magmas evolve in different ways, one process can’t explain the entirety of its evolution
T
t or f: overtime, a volcano may extrude lavas that are uniform in composition
F (vary in composition)