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Volcanoes and Plate Tectonics
“an opening in the Earth’s crust through which an eruption takes place”
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Three Types of Volcanoes!
Cinder Cones
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Cinder Cone
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Inside a Cinder Cone
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Cinder Cone Steep sloped sides (angles close to 40°)
Relative to other volcanoes – small few hundreds of meters high Small explosive eruptions Made up of pyroclastic material (ash and tephra)
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Shield
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Montserrat Volcano eruption
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Shield Volcanoes The volcano have a very broad base, with gently sloping side (like a ‘shield’) Quiet eruptions Made up of layers of hot, mafic (basaltic) lava Hawaii is a good example of a shield volcano
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Composite
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Mount Saint Helens May 15, 1980
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Mount Saint Helens May
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Mount Saint Helens May 18, 1980 Eruption
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Mount Saint Helens May
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Mt. St. Helens devastation
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Mount Saint Helens September 10, 1980
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Mount Saint Helens September 24, 1984
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Mount Saint Helens (from Spirit Lake) May 15, 1980
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Mount Saint Helens (from Spirit Lake) May 19,1982
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Popocatepetl composite volcano in Mexico is on the Ring of Fire
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Composite Volcanoes Steep sloped sides Very tall, 1000s of meters
Very explosive eruptions, sometimes quiet eruptions (alternating for the most part) Made up of alternating layers of lava flows and silica rich (granitic) pyroclastic material. Mt. St. Helens is a good example of a composite volcano
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Volcanoes (cont.) Kinds of Eruptions:
Quiet: Shield Volcanoes – broad base, low angle slope Pillow lava – lava that occurs in mid-ocean ridges Basalt Plateaus – lava spreading evenly over a large area
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Volcanoes (cont.) Kinds of Eruptions:
Rift Eruptions – Opening in the crust “spreading centers”: sea floor spreading (ocean) rift valley (continent) Lava ‘oozes’ out because of its mafic or basaltic composition
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Areas of Volcanic Activity (kinds of eruptions)
Same regions as Earthquakes, which often serve as warning signs that a volcanic eruption might occur. Ring of Fire – around the rim of Pacific Ocean, subduction zone Ocean Ridge system Hotspots
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Volcanoes (cont.) Kinds of Eruptions:
Ring of Fire – Subduction boundary Eruptions – Cinder cones and Composite Volcanoes Explosive eruptions, usually young mountain chains – like around the Ring of Fire
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Hot Spots Hot Spots – a place in the mantle where great amounts of heat are rising through the lithosphere. Causes of Hot Spots are still unknown – the source of the heat or ‘spot’ remains in the same location while the plate moves over it. For example: Hawaii
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Hot Spots
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Hot Spots
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Thermal signature of the Hawaiian Islands
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Plutonic – Igneous Rocks
When masses of magma cools beneath the surface, it forms the cores of mountains. These ‘igneous intrusions’ are called Plutons. Plutons have different names depending on their size and shape.
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Plutonic – Igneous Rocks
Small intrusive igneous formations are: Dikes Sills Volcanic Necks Laccoliths…
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Plutonic – Igneous Rocks
Laccolith – magma that bulges upward and formed dome mountains. (Henry Mountains, Utah and Black Hills, South Dakota) Batholith – a LARGE body (> 100 km3) of intrusive igneous rock. Forms the core of most major mountain ranges (Sierra Nevada) Stock – small batholith, less than100 km3
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Volcanoes
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Ruby Mountains Batholith
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La Paz Batholith
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East side of Sierra Batholith
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Granite Dome - Texas
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