IV. Volcanoes
A. Basics
- general
- explosiveness depends on amount of gas and amount of silicon
- explosive
volcanoes are felsic or intermediate and contain lots of silicon
- gentle,
lava flow volcanoes are mafic or intermediate and contain little silicon
- felsic and intermediate explosive volcanoes
- high in silicon makes the magma very viscous (thick and gooey)
- light in
color
- explosive, composite or strato-volcanoes
- ash,
- pyroclastic flows, nuee ardente,
- tuff
- lahars
- mafic and intermediate volcanoes
- low in silicon
(<52%) makes the magma have low viscosity (thin and runny)
- dark in color
due to high iron and magnesium content
- gentle lava flows make shield
volcanoes
- more gas-rich lavas form cinder cones
B. Subduction related - usually felsic to intermediate
- general
- Cascade Range
- generally explosive strato-volcanoes
- produce light
colored, silicon rich, ash, tuff, pyroclastic rocks
- Mt. Shasta
- second and third highest Cascade peaks
- constructional edifice, largely
unaffected by glaciation
- Mt. Lassen
- ancestral Mt. Tehama
- erupted in 1914-1915
- Bumpass Hell geothermal area
- southern end of subduction zone
- region is also influenced by extension (cinder cones and lava flows)
C. Extension related
- general
- Basin and Range (last 28 my, mostly last 10my) extension
- stretches and thins crust (lithosphere)
- mafic volcanoes
- Medicine Lake Highlands
- shield volcano with minor cinder cones and spatter cones
- 700,000 years
- minor young silica-rich domes and flows
- Lava Flow National Monument (related to Medicine Lake)
- lava flows from vents on the north flank of the shield volcano
- extensive lava tubes
- Mojave desert
- young from north (10 my) to south
- mostly cinder cones and lava flows
- related to northward extension of rift zone?
- felsic and bimodal volcanoes
- Long Valley Caldera
- 3.6 my mafic flows
- 2 my felsic eruptions
- 760,000 major eruption
- Bishop Tuff
- caldera formation (2-3km deep, 17x32 km)
- 200,000 year recurrence interval?
- currently magma at 5-15km
- Mono-Inyo
- rhyolite and obsidian domes and flows
- Panum crater (650 years)
- Inyo craters (530 years)
- Coso volcanics
- 6 million years
- bimodal - mafic flows and felsic domes
- time/volume pattern
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