igneous rocks, minerals, and volcanos allan treiman lpi
TRANSCRIPT
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Igneous Rocks, Minerals, and Volcanos
Allan Treiman
LPI
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Plan of Talk
Tyrrany of Three– Three types of volcanos– Three types of lavas
Volcanos in terms of Lava Properties and Environments
Lava Properties in terms of Atoms Igneous Rocks and Minerals
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Three Types of Volcanos
Shield Composite /
Stratovolcano Cinder Cone
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But So Many More …
Caldera Complex ‘Super-Volcano’
Lava Plateau Dome Single Flow Tuff Ring And …
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What Controls the Shape of a Volcano?
Properties of lava– Viscosity of lava (runny or stiff) – Dissolved Gas - Explosive or Effusive– Solid grains in lava.
Volume of lava erupted Single or Multiple eruptions Environment around eruption
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Lava Properties: Viscosity Different sorts of lavas are stiffer or runnier What is lava?
– Molten material in the Earth– Solidifies at surface conditions
Many sorts of ‘lava’– Most common is silicate - abundant SiO4
4-
– Molten sulfur, carbonate, iron oxide– Mud is not lava on Earth (but “mud volcanos”)– Water is not lava on Earth (but is elsewhere)
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Silicate Lavas Large Range of Viscosity
– Basalt - as runny as motor oil – Andesite - stiffer than taffy– Rhyolite/Granite - like window glass
Depends on silica - SiO2 – Basalt: < 52% SiO2 in
chemical analysis– Andesite: 52 - 63% SiO2 – Dacite: 63 - 68 % SiO2 – Rhyolite: > 68 % SiO2
Andesite South Sister
SiO2 63.0 TiO2 1.15 Al2O3 16.24 Fe2O3 2.87 FeO 2.94 MnO 0.08 MgO 1.52 CaO 4.04 Na2O 4.86 K2O 2.00 P2O5 0.28 H2O 0.68 Sum 99.9
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Why does silica matter?
Si - O bonds much stronger than others Silica tetrahedra, SiO4
4- polymerize
In lava, single silica tetrahedra flow easily, like little balls
In lava, large silicate polymers flow poorly, like noodles
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Why does Water Matter? Force for explosive eruptions
– Water vapor bubbles out as magma nears surface
– No vapor, no explosion! Stiff water-rich magma makes
foam (pumice)& shards of glassy ash
Pumice + ash and water vapor can flow together as a ‘slurry’ = an ash flow
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Ash flow = pyroclasticflow = ‘nuee ardent’
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Caldera Complex “Super-Volcanos”
Valles Grandes, NM Caldera is 22 km across Rhyolite ash flows & domes Slope outside caldera ~2°
Yellowstone
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An Invisible Caldera Complex “Super-
Volcano”:Harney Basin
A shallow basin, slightly east of our field trip path.
Multiple Ash Flows – Devine Canyon: 9 mybp– Prater Creek: 8.4 mybp – Rattlesnake: 6.4 mybp
Nearly invisible under later basalts, and erosion
Typical of later cenozoic geology of Basin & Range!
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Crystals in Lava Solid crystals make lava more viscous What kinds of crystals?
– Olivine (Mg,Fe)2SiO4 - green, glassy
– Pyroxene (Ca,Mg,Fe)SiO3 - black/green, breaks on flat surfaces (cleavage)
– Feldspar - plagioclase (Ca, Na)(Al,Si)Si2O8 - clear-white-greenish, glassy, breaks on flat surfaces.
– Quartz - SiO2 - clear, glassy, curved fractures.
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Single Eruption Paricutin Cinder Cone - 1.4
km3 lava Columbia River, Grande
Ronde - to 750 km long, 2000 km3 lava
Yellowstone - Lava Creek Tuff (like at Valles Caldera) - ~1000 km3 ash
How much is a cubic kilometer?
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Many Eruptions Mauna Loa Shield -
~75,000 km3 lava Columbia River Basalts
~170,000 km3 lava Olympus Mons (Mars) -
~500,000 km3 volume Ontong-Java Plateau - ?
6,000,000 km3 lava
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Environment of Eruption
Into Air– Typical
Into Water– Maar Explosion– Tuff Ring– Pillow Lava
Into Ice– Tuya Buttes
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What Controls the Shape of a Volcano?
Properties of lava– Viscosity of lava (runny or stiff) – Dissolved Gas - Explosive or Effusive– Solid grains in lava.
Volume of lava erupted Single or Multiple eruptions Environment around eruption
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Cinder Cone
Paricutin, Mexico– 1943 - 1952