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Volcanoes and Volcanic Hazards. View From Space - Klyuchevskaya, Russia. Cleveland Volcano, Alaska. Mount Etna From Space. Mount Etna From Space. Mount Etna From Space. Mount Etna. Shiveluch, Russia. Magma – molten rock beneath the surface Lava – molten rock on the surface.
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Magma – molten rock beneath the surfaceLava – molten rock on the surface
Where Does Magma Come From? • Earth’s interior is hot (25 C/km near surface = 1000 C at 40 km) • Pressure inhibits melting • Mantle is solid • Never far below melting point • Volcanoes fed by small pockets 0-100 km deep • Rising hot material may melt • Water can lower melting point
Why Igneous Rock Classification Matters • Silica Content = Viscosity • Silica Content Governs Violence of Eruptions • Silica Poor (Basalt): Fluid lavas, generally little explosive activity • Intermediate Lavas (Andesite): Pasty lavas, explosive eruptions common • Silica-Rich Lavas (Rhyolite): Extremely viscous lava and explosive eruptions
Basalt (45-52% SiO2) • Slightly modified planetary raw material • Derived directly from mantle • Oceanic crust • Hot Spots and Flood Basalts • Oceanic volcanic arcs • Early stage of continental volcanic arcs • Rift zones with rapid spreading • Fluid lava with little explosive activity • Shield volcanoes, Cinder Cones
Andesite (52-66% SiO2) • Mixture of mantle material and continental crust • Continental volcanic chains • Pasty lava with significant explosive activity • Stratovolcanoes
Rhyolite (>66% SiO2) • Mostly remelted continental crust • Settings where magma has a long time to react with continental crust • Late stage of continental volcanic arcs • Slow-spreading Continental Rifts • Continental Hot Spots (Yellowstone) • Catasrtophic explosive activity common • Obsidian domes, magma chamber collapses
Some Igneous Rocks Are Named on Textural Criteria • Pumice - Porous • Obsidian - Glass • Tuff - Cemented Ash • Breccia - Cemented Fragments
Classes of Eruption Effusive • Icelandic • Hawaiian Explosive • Strombolian • Vulcanian • Plinian • Caldera-Forming (Ultra-Plinian) • Phreatic:
Lava Flows Pyroclastic Debris Bombs Lapilli Ash Mudflows Landslides Gases Steam Carbon Dioxide H2S SO2 HCl HF Products of Eruptions
Pollution SO2, HCl in Water Lava Flows Falling Ejecta Ash Falls Building Collapse Crop Destruction Mudflows Direct Damage (Colombia, 1985) Floods (Several Types) Blast (Mt. St. Helens, 1980) Pyroclastic Flow (St. Pierre, 1902) Gas (Lake Nyos, Cameroon, 1986) Environmental Hazards of Volcanoes
Nyiragongo, Congo • At least 34 eruptions since 1982 • Semi-permanent lava lake • Area accounts for 40% of Africa’s historic eruptions • Steep-sided but unusually fluid lava: unique • 1977: Lava lake drains at night, killing 70-hundreds • 2002: Lava invades city of Goma: 400,000 evacuated, 45 killed, 4500 buildings destroyed, 120,000 homeless