Volcanoes 1: Igneous Rocks and Making Magma
volcano: a hole in the Earth’s crust where molten rock, rock fragments, and hot gas emerge from Earth’s crust and mantle
magma reaches the surface through fractures and is extruded as lava or explodes as pyroclastic material
magma: created by melting pre-existing rock below Earth’s surface
gases: dissolved in magma, low pressure near surface allows escape
mostly H2O and CO2 (also SO2, H2S, HCl, and others)
pyroclastic material: fragments or rock blasted up into the air
pyro=fire, clast=fragments = fire fragments
lava: melted rock at the Earth’s surface
melt + crystals + bubbles
magma: melted rock below Earth’s surface
melt + crystals + bubbles
ignis=fire, so fire rocks
one of the 3 types of rocks
other two are metamorphic and sedimentary
crystallize from melted material (magma or lava)
form at volcanoes
extrusive igneous rocks: form on surface from cooled and crystallized lava
intrusive igneous rocks: form beneath the surface from cooled and crystallized magma
magma cooled very slowly deep below the surface
formation takes years to centuries (possibly millenia)
lava cooled quickly on surface
formation takes days to months
felsic igneous rock features:
light colored
form the continental crust
common rock types = granite (intrusive) or rhyolite (extrusive)
intermediate igneous rock features:
intermediate colored
form the continental crust
common rock types = diorite (intrusive) or andesite (extrusive)
mafic igneous rock features:
dark colored
form oceanic crust
common rock types = gabbro (intrusive) or basalt (extrusive)
at depth, rock is under high pressure and high temperature
3 ways:
increase temperature
hotter things melt
decrease pressure
move it to lower pressure
called “decompression melting” (temperature stays the same)
add water or other volatiles
lowers melting temperature
pose a threat (loss of life)
destroy ecosystems
avoid them
we can predict them
aftermath can be worse than initial eruption
air quality
volcano: a hole in the Earth’s crust where molten rock, rock fragments, and hot gas emerge from Earth’s crust and mantle
magma reaches the surface through fractures and is extruded as lava or explodes as pyroclastic material
magma: created by melting pre-existing rock below Earth’s surface
gases: dissolved in magma, low pressure near surface allows escape
mostly H2O and CO2 (also SO2, H2S, HCl, and others)
pyroclastic material: fragments or rock blasted up into the air
pyro=fire, clast=fragments = fire fragments
lava: melted rock at the Earth’s surface
melt + crystals + bubbles
magma: melted rock below Earth’s surface
melt + crystals + bubbles
ignis=fire, so fire rocks
one of the 3 types of rocks
other two are metamorphic and sedimentary
crystallize from melted material (magma or lava)
form at volcanoes
extrusive igneous rocks: form on surface from cooled and crystallized lava
intrusive igneous rocks: form beneath the surface from cooled and crystallized magma
magma cooled very slowly deep below the surface
formation takes years to centuries (possibly millenia)
lava cooled quickly on surface
formation takes days to months
felsic igneous rock features:
light colored
form the continental crust
common rock types = granite (intrusive) or rhyolite (extrusive)
intermediate igneous rock features:
intermediate colored
form the continental crust
common rock types = diorite (intrusive) or andesite (extrusive)
mafic igneous rock features:
dark colored
form oceanic crust
common rock types = gabbro (intrusive) or basalt (extrusive)
at depth, rock is under high pressure and high temperature
3 ways:
increase temperature
hotter things melt
decrease pressure
move it to lower pressure
called “decompression melting” (temperature stays the same)
add water or other volatiles
lowers melting temperature
pose a threat (loss of life)
destroy ecosystems
avoid them
we can predict them
aftermath can be worse than initial eruption
air quality