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Chp 7.2 Volcanic Eruptions and Features. What controls volcanic eruptions?. Composition of Magma Based on percentage of silica and oxygen present in the magma. High Silica: Thicker and slower moving. Usually thick and sticky. Viscosity:
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What controls volcanic eruptions? • Composition of Magma • Based on percentage of silica and oxygen present in the magma. • High Silica: • Thicker and slower moving. • Usually thick and sticky. • Viscosity: • Is a physical property that describes the material’s resistance to flow. • Low Silica: • Low percentage of silica and more Fe and Mg. • Thin and runny.
Dissolved Gases and Temperature • Higher temperature of magma, the more easily it flows. • Gases: H2O(v), CO2, SO2, H2S • The more gases the greater the chance of an explosive eruption.
Types of Magma and Lava • Basaltic Magma and Lava • Low percentage of silica. • Low viscosity. • Much thinner, more fluid magma • Tend to pour from the vent and run down the sides of the volcano in a non-explosive eruption. • Pahoehoe lava cools develops ropelike patterns. • Aa lava is stiff, and slow moving. • Underwater eruption forms bubble-like pillow lava.
Granitic Magma and Lava • High percentage of silica. • High viscosity, flows slowly. • Sticky and lumpy. • Trap gases, builds up pressure and produces explosive eruptions.
Types of Volcanoes • Shield volcano: • Is a huge, gently sloping volcanic landform that is mainly composed of basaltic lava. • Develop as layer upon layer of gently flowing basaltic lava piles up.
Cinder Cone Volcanoes • Is mainly composed of solid fragments known as Tephra. • Includes fragments of volcanic rock or lava. • Explosive volcanic eruptions. • When lava erupts from the vent, it cools quickly in the air.
Composite Volcanoes • Is mainly composed of alternating layers of lava and tephra. • Quiet and explosive volcanic eruptions due to the composition of magma • Tall mountains.
Volcanoes in California • Form at a convergent plate boundary • Part of a volcanic arc. • Form where the Juan de Fuca Plate subducts beneath the N. American Plate
Intrusive Igneous Features • Batholiths • Largest intrusive igneous features. • Magma slowly cools and solidifies before reaching the surface. • Many kilometers in width and length and several kilometers thick.
Dikes and Sills • Magma squeezes into cracks in rocks below the surface. • Magma that cuts across rock layers and hardens is called dike. • Magma that is parallel to rock layers and hardens is called sill.
Volcanic Neck • Hardened magma inside the vent is eroded by water and wind. • The cone is much softer than the igneous rock in the vent, so it erodes first.
Lava Domes • Rounded volcanic feature that forms when highly viscous lava erupts from the vent. • Lava piles up. • When gases accumulate, pressure increases within the lava dome, gas, lava and solid materials are ejected in the air.
Lava Tubes • A hollow tube that forms when lava flows through a channel, cools and hardens on the surface. • Often underground. • Magma flows to the sea.
Caldera • Is a large, circular depression. • Forms when the top of the volcano collapses and becomes wedged into the nearly empty magma chamber. • The chamber becomes filled with water, forming lakes and landscapes. • Usually the largest eruptions on Earth.