bellringer
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Bellringer. Describe the relationship between the silica content of magma and the resulting eruption of the volcano. Volcanic Landforms. Notes. Landforms from Lava and Ash. A shield volcano is a gently sloping mountain. Thin layers of lava build up slowly over a large area around a vent. - PowerPoint PPT PresentationTRANSCRIPT
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BellringerDescribe the relationship between the silica content of magma and the resulting eruption of the volcano.
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Volcanic Landforms
Notes
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Landforms from Lava and Ash
•A shield volcano is a gently sloping mountain. Thin layers of lava build up slowly over a large area around a vent.
•Examples include Mauna Kea, Hawai’i; some of the Galapagos Islands; Iceland; and Olympus Mons on Mars.
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Landforms from Lava and Ash
•A cinder cone is a steep, cone-shaped hill or small mountain. It forms when a volcano erupts explosively. Ashes, cinders, and bombs pile up around the vent. The tephra (rock pieces) are held together very loosely.
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Landforms from Lava and Ash
•A composite volcano is a tall, cone-shaped mountain. It forms when a volcano erupts quietly and then explosively, over and over again. Layers of lava are followed by layers of ash, cinders, and bombs.
•These volcanoes are also known as stratovolcanoes.
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http://dli.taftcollege.edu/streams/Geography/Animations/VolcanoTypes.html
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Landforms from Lava and Ash
•Sometimes lava forms a plateau instead of a mountain. A lava plateau is a high, level area. If forms when thin lava flows out of many long cracks.
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Landforms from Lava and Ash
•If a magma chamber empties, a volcano can collapse. This leaves a huge hole called a caldera. A caldera may fill with water and form a lake.
•Caldera is derived from the Latin calderia, which is usually translated as cauldron, or cooking pot.
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Landforms from Magma
•Sometimes, magma never breaches the surface of the crust, and instead, cools within it, forming intrusions of igneous (solid volcanic) rock that can eventually be exposed as weathering erodes away the surrounding rock.
•A volcanic neck (or volcanic plug) forms when magma hardens in the pipe of a volcano. Softer rock around the pipe erodes away, leaving just the neck standing. A volcanic neck looks like a giant tooth stuck into the ground.
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Landforms from Magma
•A dike forms when magma hardens across rock layers. A dike is a vertical, or up-and-down, igneous intrusion. When erosion exposes the dike, it leaves behind a long, thin ridge of igneous rock.
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Dike
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Volcanic neck and accompanying dike
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Landforms from Magma
•A batholith forms when a large amount of magma hardens inside the crust. A batholith is a large rock mass. It may become a part of a mountain range.
•A dome mountain forms when a batholith or smaller chunk of hardened magma is pushed up to the surface. The hardened magma forces the layers of rock above it to bend upward into a dome shape.
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Geothermal Activity
•Magma below the surface can heat underground water. The heating of underground water by magma is called geothermal activity. Geothermal activity is common where there are volcanoes.
•A hot spring forms when water heated by magma rises to the surface and collects in a natural pool.
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Natural geothermal hot springs in Iceland.
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Geothermal Activity
•A geyser forms when hot water and steam are trapped underground in a narrow crack. Pressure builds up until the hot water and steam erupt from the ground. This happens over and over again. Old Faithful is a geyser in Yellowstone National Park. It erupts about once and hour.
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Geothermal Activity
•Hot water from underground can be piped into homes to heat them. This is how many people in Iceland heat their homes. NO FOSSIL FUELS! 100% RENEWABLE.
•Steam from underground can be piped into electric power plants. In the power plants, the heat energy in the steam is turned into electric energy.
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