volcanic terraine Flashcards
naturally occuring landform where lave extruded from a magma chamber underground
volcano
zone of greatest seismic activity and consists of approximately 75% of the world’s volcano
pacific ring of fire (circum-pacific belt)
oceanic-oceanic crust collision
volcanic island arc
oceanic-continental crust collision
continental volcanic arc
continental-continental crust collision
volcanic plateau
formed by rising mantle plumes
hot spot
consists less than 50% of silica and least viscous magma
mafic (basaltic) magma
~60% silica content and intermediate viscosity magma
intermediate (andesitic) magma
~70% silica content and the most viscous magma
felsic (rhyolitic) magma
magma with rough jagged surface and sharp edges
AA
exhibit smooth ropy surface
pahoehoe
magma consists of blocks with slightly curved surface, smooth surface
block lava
outpourings of lava in the ocean floor
pillow lava
volcano with atleast 1 eruption in the last 10,000 years
active volcano
active volcano that is not erupting, supposed to erupt again
inactive volcano
volcano with no eruption for atleast 10,000 years, not expected to erupt again
dormant/extinct volcano
fissure eruption, the most calmest eruption, release free flowing basaltic magma
icelandic
characterised by effusive emission of highly fluid basalt lavas with low gas content, builds shield volcanoes
hawaiiin
short explosive burst by booming sounds.
strombolian
eruption with moderateley viscous magma, and so have thick, stubby flows
vulcanian
the largest and most violent of all types of volcanic erruptions
plinian
there is a single, usually small eruption. usually associated with fissure volcano belts
monogenetic
there is a sequence of eruptive event, often with a cyclic variation in lava types
polygenetic
mode of succession of wide sheets of volcanic rocks, built by repeated outpourings of basaltic lava
lava shield
central eruptions on a still smaller scale may give rise to simple straight-sided cones
lava cone
have no sign of a crator, but are gently sloping mounds, they may owe their shape to erosion although they never had pronounced craters but had lava welling right to the brim before solidification
lava mounds
viscous lava is extruded, it sags and spreads into convex dome-like bodies
cumulo-dome / mamelon
cumulo-domes or mamelons when they occur in the crater of a large volcano
tholoid
usually steep small cones
plug domes
produced as the last phase of an eruption of larger volcanoes
scoria cones
scoria volcanoes have no apparent crater
scoria mounds
they form in the interaction between lava flows and water
littoral cones
shallow volcanic craters with steep sides that is surrounded y tephra basalt
maars
ash, lapilli, blocks, and bombs
pyroclastic ejecta
tuffs and agglomerate
lithified deposits
nuee ardentes
volcanic clouds
welded tuff and ignimbrites
ash flow
volcanic ash + water
lahars