HAZARDS - volcanoes Flashcards
pyroclastic flow
mixture of hot rock, lava, ash and gasses which erupt from a volcano and move rapidly along the ground
tephra
rock fragments ejected during the volcanic eruption
nuée ardente
dense rapid moving cloud of ash, hot gasses and lava fragments - type of pyroclastic flow
primary hazards of a volcano
pyroclastic flow, lava flow, tephra, nuée ardente
secondary hazards of a volcano
acid rain, lahars, tsunamis
lahars
destructive mudflow - ash and other volcanic materials mixed with water.
spatial distribution of earthquakes
95% of plate boundaries are associated with constructive and destructive plate boundaries. 5% are intraplate.
what are the three factors that increase the viscosity of magma?
low temperature
high silica content
low volume of dissolved gas
what are the characteristics of high viscosity magma?
thick, cooler magma = violent eruptions as it blocks vents
what are the characterisitics of low wiscosity magma
hot, runny magma
less pressure so gasses can escape and vents are not blocked.
less violent eruptions
basaltic magma
-high temperature, low silica content = LOW viscosity =
-non-violent eruptions
-found at constructive plate boundaries
(balsamic vinagar is runny)
rhyolitic
-low temperature, high silica content =thick HIGH viscosity magma
-violent eruptions
-found at destructive margins
(Ryan is chilled out and slow)
andesitic
low temp, high silica = HIGH viscosity - VERY explosive - affects large areas - basaltic and continental crust at subduction zone - destructive margin (Andrea is even slower than Ryan)
how is the magnitude of volcanoes measured?
VEI volcano explosivity index 0-8 = based on the amount of material ejected and how high it is blasted.
frequency
depends on the volcano
- constructive - basaltic lava = frequent with smaller mag.
- destructive - rhyolitic lava = every 100,000 yrs with larger mag