Test 2 Flashcards
viscosity
resistance to flow
How is viscosity related to silica content?
more silica=higher resistance to flow
Basaltic lava
relatively little silica
very hot
fast moving
lava tube
as basaltic lava cools, eventually molten lava only moves through tunnel-like passage ways
Pahoehoe
basaltic lava flows that whose surface is warm and pasty wrinkle into smooth glassy, rope-like ridges
a’a’
if the flow becomes too viscous to make rope-like ridges, it breaks into a jumble of sharp, angular fragments
pillow lava
basaltic lava that cools rapidly in the ocean
andesitic lava
slow moving
lumpy flow with a bulbous snout
blocky lava
andesitic lava flow
Rhyolitic lava
most viscous most felsic coolest rarely flows more than 1-2 km broken and blocky
pyroclastic debris
fragmental igneous material erupted from a volcano
lava fountains
gas pressure drives columns of basaltic lava into the air
lapilli
solidified pea to golf ball sized fragments of glassy lava
blocks
apple to refrigerator sized fragments of already solid lava from the walls of the vent ejected by an eruption
pumice lapilli
frothy lava breaks into marble-sized chunks
Tuff
pyroclastic debris from andesitic or rhyolitic eruptions that has been buried and transformed into rock
lahar
volcanic debris that mixes with water and flows away from the volcano
crater
circular, bowl-like depression occurs at the top of a volcano
caldera
large crater
shield volcano
broad gentle domes
form from magma with low viscosity
Cinder cones
cone-shaped piles of basaltic lapilli and block
slope is determined by the max slop the magma can be deposited at
stratovolcanoes
large, tall volcanoes consisting of layers of lava, pyroclastic debris, and volcaniclastic debris
Effusive eruptions
lava pours out from a vent or fissure
convective cloud
huge plume of ash that rises from a large explosion rises skyward
column collapse
gravity pulls a substantial amount back down around the volcano
volcanoes at continental rifts
both basaltic and explosive rhyolitic volcanoes
oceanic hot-spot volcanoes
basaltic volcanoes on the ocean floor
continental hot-spot volcanoes
both basaltic and rhyolitic pyroclastic debris
flood-basalt
huge amounts of low-viscosity mafic lava erupted from fissures and spread out in vast sheets
jointing
natural cracks in rocks
exfoliation joints
lie parallel to the mountain faces
talus
rock rubble at the base of the slope
erosion
breaking off and removal of rock or sediment
strips away overburden
salt wedging
in arid climates, dissolved salt in groundwater precipitates into open pore spaces in rocks, forming crystals that push apart the surrounding rock
Thermal expansion
forest fires heat up rocks and as the surface cools the outer layers can break off
Dissolution
water flowing over rock slowly dissolves minerals
hydrolysis
water chemically reacts with minerals and breaks them down
hydration
the absorption of water causes some rocks to swell and weaken