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27 Cards in this Set

  • Front
  • Back
What are the products of eruptions (3)
Lava flows, pyroclastic debris, volcanic gases
How are lava flows determined by viscosity?
Low: Easily flows; High: resists flows (cliffs)
Low viscocity is characteristic of basaltic or rhyolitic lava?
Basaltic.
High viscocity is characteristic of basaltic or rhyolitic lava?
Andesitic (intermediate) and Rhyolitic (heavy). There's a higher level of silica in these.
What makes lava domes?
Rhyolitic lava flows
Lava flows in relation to silica, temp, gas, and crystals:
High: More silica, cool, gas-poor, and crystal-rich; Low: less silica, hot lava, gas-rich, crystal poor
Three types of Basaltic lava flows (3)
Pahoehoe, columnar jointing, pillow lavas
Pryoclastic Debris: Volcanic Ash
powder-sized glass fragments, bad to breathe and bad for planes
Pyroclastic Debris: Pumice / Scoria
gas filled rock that solified at vent
Is pumice felsic or mafic?
Felsic
Is scoria felsic or mafic?
Mafic
Volcanisclastic Debris: Lapilli
pea to plum-sized
Volcanisclastic Debris: Blocks
apple to refrigerator-sized, chunks from walls of vent
Volcanisclastic Debris: Bombs
apple to fridge size, lava that solidifies in the air
Volcanisclastic Debris: Tuff
Lithified Ash and lapilli (ash that's solified, looks homogenous)
Volcanisclastic Debris: Tephra
ash that's not solidified
Pryoclastic flow
gravity-driven avalanche of hot ash and lapilli-- moves incredibly quickly
Lahar
fast-moving flow of ash-rich debris and water
Volcanic gases (4)
Up to 9% of magma may be gas: water, carbon dioxide, sulfur dioxide, hydrogen sulfide.
Caldera
is the falling of the mountain into the void created by the lack of magma. The resurgent dome is residual magma.
Shield Volcano
low-viscosity basalt flows
Cinder cones
cone-shaped piles of tephra
Stratovolcanoes
alternating layers of lava flows and tephra
Eruption style: effusive
produces lava flows
Eruption style: explosive
produces pyroclastic debris
Three basaltic eruption styles
Vulcanian, strombolian, and hawaiian
Rhyolitic eruption style
Plinian