* Your assessment is very important for improving the workof artificial intelligence, which forms the content of this project
Download Slide 1
Axial Seamount wikipedia , lookup
Mono–Inyo Craters wikipedia , lookup
Large igneous province wikipedia , lookup
Mount Garibaldi wikipedia , lookup
Llullaillaco wikipedia , lookup
Mount Pleasant Caldera wikipedia , lookup
Mount Meager massif wikipedia , lookup
Mount Pinatubo wikipedia , lookup
Itcha Range wikipedia , lookup
Olympus Mons wikipedia , lookup
Level Mountain wikipedia , lookup
Craters of the Moon National Monument and Preserve wikipedia , lookup
Cerro Blanco (volcano) wikipedia , lookup
Mount St. Helens wikipedia , lookup
Nevado del Ruiz wikipedia , lookup
Potrillo volcanic field wikipedia , lookup
Mount Vesuvius wikipedia , lookup
Cascade Volcanoes wikipedia , lookup
Mount Edziza volcanic complex wikipedia , lookup
Volcanology of Io wikipedia , lookup
Volcano (1997 film) wikipedia , lookup
Wells Gray-Clearwater volcanic field wikipedia , lookup
Shield volcano wikipedia , lookup
Mount Pelée wikipedia , lookup
Cerro Azul (Chile volcano) wikipedia , lookup
Earth Science 10-2 Factors Affecting Eruptions 1. The Primary factors that determine whether a volcano erupts explosively or quietly include characteristics of the magma and the amount of dissolved gases in the magma. Mount Saint Helens before and after eruption Viscosity • Viscosity o Is a substance’s resistance to flow o Viscosity is strongly affected by temp. o If lava cools and begins to harden, its Viscosity increases Continued… • Chemical composition – Chemical composition on magma has a more important effect on the type of eruption – Because of high silica content, rhyolitic lavas are very viscous and erupt explosively – Less silica has a calmer eruption Dissolved Gases • Vent – An opening to the surface – During explosive eruptions, the gases trapped in magma provide the force to propel molten rock out of the vent. – These gases are mostly water vapor and carbon dioxide Volcanic Material 1. Lava Flows a) Silica content and the temperature affect the characteristics of lava flows. b) Temperature differences produce 2 types of basaltic lava: pahoehoe and aa 2. Pahoehoe a) Is hotter, fast moving basaltic lava b) Pahoehoe forms relatively smooth skin that wrinkles as the still-molten lava continues to flow 3. Aa a) Is cooler, slower-moving basaltic lava b) Aa forms a surface of rough, jagged blocks with sharp, spiny projections 4. Gases a) Magmas contain varied amounts of dissolved gases held under pressure in the molten rock b) The gaseous portion of the magma is a small portion about 1 to 6% 5. Pyroclastic Materials a) Particles produced in volcanic eruptions are called pyroclastic materials b) The fragments ejected range in size from very fine dust and volcanic ash to pieces that weigh several tons Types of volcanoes 1. Anatomy of a volcano a) Volcanic activity usually begins when a fissure, or crack, develops in the crust b) Volcano- repeated eruptions of lava or pyroclastic material eventually build up a mountain c) Crater- steep-walled depression • The three main volcanic types of volcanoes are shield volcanoes, cinder cones, and composite cones. Volcano eruption types Shield volcano Cinder cones Composite cones 1. Shield volcanoes a) Are produced by the accumulation of fluid basaltic lavas. b) Shield volcanoes have a shape of a broad, slightly domed structure that resembles a warrior’s shield. 2. Cinder cones a) Ejected lava fragments that harden in the air build a cinder cone b) The shape of a cinder cone is determined by the steep-sided slope that forms as loose pyroclastic material builds up around the vent 3. Composite cones a) Is a large, nearly symmetrical volcano mountain composed of layers of both lava and pyroclastic deposits b) Most composite cones are located in a relatively narrow zone that rims the Pacific Ocean, the Ring of Fire How many of these Volcanoes are located in the U.S. 600 500 400 300 200 100 0 composite cinder shield • Volcanic landforms include calderas, volcanic necks, and lava plateaus • Long after eruptions have ended, these landforms can provide evidence of volcanic activity 1. Calderas a) A caldera is a depression in a volcanic mountain. b) Most calderas form in two ways: 1) By the collapse of the top of a composite volcano after an explosive eruption 2) From the collapse of the top of a shield volcano after the magma chamber drained 2. Volcanic necks a) Is a landform made of magma that hardened in a volcanoes pipe and later was exposed by erosion b) Weathering and erosion work constantly to wear away the volcanoes c) When a volcanoes activity ends, magma remaining in the pipe hardens to form igneous rock 3. Lave plateaus a) b) c) Is a volcanic landform produced by repeated eruptions of very fluid, basaltic lava Instead of building a cone the lava spreads out over a wide area The lava that forms the lava plateaus erupts through long cracks called fissures Volcanic Hazards • Volcano hazards include lava flows, volcanic ash, pyroclasitc flows, and mudflows. • Lahar – Occurs when water-soaked volcanic ash and rock slide rapidly downhill • Composite volcanoes are among the most dangerous. They can cause a lahar • An explosive eruption can also create a pyroclastic flow • Volcanoes usually give some warnings that an eruption is near • Usually most people settle near a volcano because of the fertile land from the ash