Volcanoes Volcano refers both to the opening in Earth’s crust through which molten rock, gases, and ash erupt and to the landform that develops around this opening. A volcanic eruption occurs when magma rises to the surface. The following three conditions allow magma to form: A decrease in pressure can lower the melting temperatures of materials in the asthenosphere. This takes place along a mid-ocean ridge rift valley where the lithosphere is thinner. An increase in temperature can cause materials in the asthenosphere to melt. This occurs at a hot spot, such as Hawaii. An increase in the amount of water in the asthenosphere can lower the melting temperatures of materials there. This occurs at subduction boundaries. Volcanoes are formed at subduction (convergent) boundaries: Water in the subducted rock is released into the asthenosphere. Water lowers melting temperatures leading to magma formation. Magma rises because it is less dense than surroundings. Some of the magma reaches Earth’s surface, and volcanoes form on the overriding plate. Volcanoes are formed at divergent boundaries: Below a rift, mantle material rises from deeper, hotter regions within the Earth Because of the rift, the pressure is lower than it is elsewhere in the mantle, lowering melting temps. Combination of high temperature and low pressure causes large amounts of magma to form Magma rises because it is less dense than surrounding materials Most of the magma that reaches Earth’s surface does so at divergent boundaries, along mid-ocean ridges. Most of Earth’s volcanic activity takes place under the oceans. In Iceland, the Mid-Atlantic Ridge rises above the surface. Thule, Iceland Volcanoes are formed over hot spots. A hot spot is an area of volcanic activity that results from plumes of hot solid material that have risen from deep within the Earth’s mantle. As the material rises, it melts at areas of lower pressure. A hot spot remains in the same place even as a lithospheric plate moves across it. Characteristics and types of magma. Characteristic Silica % Basaltic Andesitic Rhyolitic Least (about 50%) Intermediate (About 60%) Most (About 70%) Gas Content Least Intermediate Most Viscosity Least viscous Intermediate Most Eruption Type Rarely explosive Sometimes explosive Usually explosive Melting Temperature Highest Intermediate Lowest Location Rifts, oceanic hot spots Subduction boundaries Continental hot spots (Resistance to flow) Example Mount St. Helens Kilauea Yellowstone caldera Largest volcanic system in North America 1. Fill in the blanks: a. Magma that reaches the Earth’s surface is called lava. b. Lava with smooth, ropelike surfaces is called pahoehoe. c. Lava with rough jagged edges is called aa. d. When lava cools quickly underwater it forms rounded lumps called pillow lava. e. Solid fragments released from a volcano when trapped gas is ejected are called pyroclastic material. f. Pyroclastic material is classified by size. The smallest fragments are called ash, intermediate pieces are lapilli, and the largest pieces are called blocks and bombs. g. A dense superheated cloud of pyroclastic material flowing downhill with amazing speed is a pyroclastic flow. The eruption of Mount Vesuvius in A.D. 79 produced a pyroclastic flow that buried the Roman city of Pompeii. Volcano Type Volcano Shape Shield Broad base can support enormous height Cinder Cones Composite Description of lava discharge Basaltic lava flows long distances before hardening due to low viscosity Cone shaped mound with an oval base that tend to be smaller than other types Molten lava thrown into air hardens before it hits the ground Layers of materials from successive explosive eruptions accumulate around a vent Magma, water and gas explode in a massive cloud of superheated ash and stones Sketch of Volcano Fill in the table below to describe the formation of Crater Lake (a caldera). 1. A volcanic eruption partially The top of the cone collapsed inward, Over time, rainwater filled the caldera, emptied the magma chamber. forming a basin known as a caldera forming Crater Lake