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Published byCrystal Wilkinson Modified over 9 years ago
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Volcanic Landforms Processes and Hazards
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Volcanic Landforms 1.Intrusive Igneous Forms 2.Extrusive – Basalt Landforms 3.Extrusive – Composite volcanoes 4.Extrusive – Rhyolite landforms
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1. Intrusive Igneous Forms Magma solidified at great depth (so mineral sizes are large) Plutons (individual magma chambers) Batholiths (merged magma chambers)
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Pluton seen because of glacial erosion, Chile
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Brandberg, Western Namibia Intrusive igneous rocks are often more resistant to erosion, so they are topographic highs
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Plutons (individual magma chambers) Batholiths (merged magma chambers) Laccolith (bubble up strata) Dikes – vertical magma cutting through Sill – horizontal magma inserted between Large Small
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Dike, Spanish Peaks, Colorado more resistant than surrounding sediment, so stand out
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Dike, Picture Gorge
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Shiprock (Tse bi Dahi, Rock With Wings), New Mexico is the classic example of a volcanic neck (base of composite volcano, so deep that is intrusive rock) Over time, the less resistant rock (i.e., pyroclasts and less consolidated lava flows) comprising the flank of the volcano is eroded away leaving the resistant neck exposed in relief. Volcanic Neck. Dike
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Classroom Resource Tse bi Dahi Rock With Wings Shiprock Volcanic Neck
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Viscosity Organization Extrusive – Basalt Landforms Extrusive – Composite volcanoes Extrusive – Rhyolite landforms
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More Viscous = More Explosive Classroom Resource
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2. Extrusive – Basalt Landforms Basalt Flow Flood Basalts Cinder Cone Shield Volcano Shield & Cinder Cone – from basalt eruptions Later: Composite volcano
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Basalt flows will travel great distances and slope angles will reflect low viscosity.
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Classroom Resources Recent Hawaii Eruptions (NPS) A year of pahoehoe Spatter Cone
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Low viscosity releases trapped gases easily, so not explosive.
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Classroom Resources Etna Tourist Office No Lives Lost
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Different Textures, Same Basalt Rock Pahoehoe a’a
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Lava Tubes – so fluid that inside keeps moving & creates caves Classroom Resource Lava tube breakout
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Lava Tube, Hawaii near Flagstaff, AZ Mt St. Helens, OR
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Buries old topography
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Cinder Cones SP Crater, AZ
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Cinder drops out (like hour glass)
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Cinder Cone Developing
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Largest drop out first
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Largest Clasts: Volcanic Bombs Classroom Resource Cinder Cone Bombs
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Crater: depression at top formed by force of eruption
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Owens Valley, Calif
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Very common in Arizona: especially S.F. Volcanic Field
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Sunset Crater, AZ
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Shield Volcanoes Isabela Island, Galapagos
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Hawaii built from Shield Volcanoes
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Weight of new lava has depressed the crust around Hawai’i Moat ~ 5000 m Below Sea Level
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Mauna Loa: note gentle profile from fluid basalt flows
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Mauna Kea
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Often have Summit Caldera – from collapse as lava flows away
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3. Extrusive – Composite Volcanoes Mt Ararat, Armenia
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Sit above Subduction Zones Fuji Egmont
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Extraordinarily Dangerous from Nova
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Future Disaster: Popocatepetl, next to Mexico City & Puebla
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Composite Volcano
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Online Animations Volcanic Hazards http://serc.carleton.edu/NAGTWorkshops/vis ualization/collections/volcano.html
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Classroom Resources Nuee Ardente (also called glowing avalanche, pyroclastic flow) Set to music (www.mvo.ms) Soufriere, Montserrat
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Nuee Ardente (Glowing Avalanche or pyroclastic flow)
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Pompeii, Italy Mt. Vesuvius
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Volcanic Ash
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Debris Avalanche
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Mt St. Helens Before Eruption
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Classroom Resource Lahaar, Mt St. Helens Fly Over
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Mt Mazama (could be Rainier)
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Caldera – from collapse after lava has “evacuated” from magma chamber Crater Lake
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Mt Hood (my bet to go next)
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Mount Pinatubo
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Classroom Resources
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Arizona has San Francisco Peaks & Mt Baldy
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Classroom Resource San Francisco Peaks (made by Simpkin, ASU)
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4. Extrusive – Rhyolite Landforms Small Eruptions: Rhyolite Domes, Mt Elden Rhyolite so viscous has trouble flowing, so piles up in dome shape
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Many Rhyolite Domes near Mono Lake, Calif
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Mammoth Lakes, still active evidence: carbon dioxide
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Classroom Resources After major eruption of composite volcano, will often start to rebuild with rhyolite domes
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Arizona has many rhyolite caldera super eruptions (17-27 myr ago) Superstition Mtns Chiricahua Mtns
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Toba – almost did us in
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Imagery seen in this presentation is courtesy of Ron Dorn and other ASU colleagues, students and colleagues in other academic departments, individual illustrations in scholarly journals such as Science and Nature, scholarly societies such as the Association of American Geographers, city, state governments, other countries government websites and U.S. government agencies such as NASA, USGS, NRCS, Library of Congress, U.S. Fish and Wildlife Service USAID and NOAA.c
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