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Lecture 14 Summary
Lecture 14 Summary

... in diameter that was ejected from a volcano during an for Volcanic Lava explosive eruption. Types Volcanic bombs - lava fragments that were ejected while viscous (partially molten) and larger than 64 mm in diameter. ...
Cascade Range Volcanoes
Cascade Range Volcanoes

... collapse •Hillman Peak Highest point on the rim of the caldera Wizard Island. A small cinder cone volcano. ...
Volcanoes - SchoolRack
Volcanoes - SchoolRack

... rock-forming substance, gases, water from the mantle • -called lava on surface • -lava forms solid rock when cooled ...
Chapter 9 Section 1 Notes
Chapter 9 Section 1 Notes

... 1. _________________________eruptions are the most common type of eruption. 2. These eruptions produce relatively calm flows of ______________. Explosive Eruptions 1. ________________________ eruptions are much rarer than nonexplosive eruptions. 2. During an explosive eruption, clouds of hot debris, ...
Igneous Rocks - Occurrence and Classification
Igneous Rocks - Occurrence and Classification

... Vulcanian - short, violent, relatively small explosion of viscous magma (usually andesite, dacite, or rhyolite). Pelean - explosive outbursts that generate pyroclastic flows, dense mixtures of hot volcanic fragments and gas. Plinian - caused by the fragmentation of gassy magma, and are usually assoc ...
Volcano and extrusive igneous rock notes
Volcano and extrusive igneous rock notes

... • a crater is the bowl-shaped feature at the top of a volcano where the vent is located. • a fissure is a crack in the side of a volcano through which magma can flow. These might be circular and concentric with the crater, or (more commonly) radial, extending like spokes away from the crater. • a ca ...
volcanoes
volcanoes

... Volcanoes are classified as active or inactive. Inactive volcanoes are older and have usually erupted many times. A volcano is described as active if it is currently erupting or expected to erupt eventually. Eruption Stage A volcanic eruption occurs when lava, gasses, and other subterranean matter c ...
Volcanic Landforms
Volcanic Landforms

... Some volcanic landforms are formed when lava flows build up mountains and plateaus on Earth’s surface. Volcanic eruptions create landforms made of lava, ash, and other materials. These landforms include shield volcanoes, composite volcanoes, cinder cone volcanoes, and lava plateaus. At some places o ...
Types of Volcanoes
Types of Volcanoes

... fine-grained rock. However, andesite is usually light to medium gray in color. Andesite is one of the most common volcanic rocks and can contain olivine, a green mineral. There are different stages of volcanic activity as well as a variety of rocks manufactured through volcanic eruptions. Most peopl ...
VOLCANOES
VOLCANOES

... bubbles start to form from the gas dissolved in the magma. The gas bubbles exert tremendous pressure. This pressure helps to bring the magma to the surface and forces it in the air, sometimes to great heights. ...
3-2 Notes: Volcanoes Eruptions • Volcano
3-2 Notes: Volcanoes Eruptions • Volcano

... • In AD 79, Mt. Vesuvius erupted and buried the town of Pompeii in a deadly pyroclastic flow, killing almost ________ people immediately. Volcanoes Form Along Plate Boundaries • Volcanoes are common along tectonic plate boundaries at subduction zones and _________________ boundaries. • Volcanoes can ...
LAVA FLOW—A SILENT VOLCANIC HAZARD IN HAWAII Thursday
LAVA FLOW—A SILENT VOLCANIC HAZARD IN HAWAII Thursday

... Thursday, October 30, to provide security to the Big Island community that was being threatened by the slow-moving river of molten lava creeping slowly towards the town's center. ...
Directed Reading
Directed Reading

... gently sloping sides b. structure that is formed from lava and pyroclastic material ejected during a volcanic eruption c. volcano that is rarely more than a few hundred meters high and has steep slope angles that can be close to 40° d. volcano that is made from alternating layers of hardened lava fl ...
Volcanoes - SD43 Teacher Sites
Volcanoes - SD43 Teacher Sites

... intermittent (hundreds or thousands of years of inactivity separating a few years of activity.) • Most Complex • Formed by melting of crust when colliding with other rock surfaces (subduction) • Can be very large because of their long lives and resistance to erosion. ...
Volcanoes and Other Igneous Activity
Volcanoes and Other Igneous Activity

... – Fed by massive mantle plumes – Caused by flood basalts – Discharge over Columbia River Basalts time through long fissures (cracks). – Create large plateaus. ...
Volcano Vocabulary
Volcano Vocabulary

... Hot Springs ...
Volcano Vocabulary
Volcano Vocabulary

... Hot Springs ...
Typical shield volcano Mauna Loa, Hawaii
Typical shield volcano Mauna Loa, Hawaii

... Example: Mauna Loa on Hawaii ...
• Once magma reaches the surface, it is called lava. • An example of
• Once magma reaches the surface, it is called lava. • An example of

... A weak spot in the crust where magma comes to the surface is a volcano. How well a liquid flows depends on its viscosity. A long tube that connects a magma chamber to the surface is called a pipe. A volcano that is no longer likely to erupt is said to be extinct. A huge hole left behind when a volca ...
Lecture 12
Lecture 12

... (composite volcanoes) •  Alternating andesitic lava flows and layers of explosively ejected pyroclastics. •  Magma is intermediate, making the lava viscous and difficult to erupt •  Explosive eruptions due to buildup of gases. ...
Volcanoes - geographylyndon
Volcanoes - geographylyndon

... lava and ash (other volcanoes just consist of lava). • The eruptions from these volcanoes may be a pyroclastic flow rather than a lava flow. A pyroclastic flow is a mixture of hot steam, ash, rock and dust. • A pyroclastic flow can roll down the sides of a volcano at very high speeds and with temper ...
Volcano Notes - MrTestaScienceClass
Volcano Notes - MrTestaScienceClass

...  Thicker, viscous  Difficult for gases to escape, so pressure builds up ...
Section 6.1 Volcanic eruptions
Section 6.1 Volcanic eruptions

...  Thicker, viscous  Difficult for gases to escape, so pressure builds up ...
Student Science Volcano Project
Student Science Volcano Project

... active volcano in Indonesia than anywhere else on Earth 130! Perhaps the most dangerous volcano in called Merapi, or "Mountain of Fire" on the island of Java. Since 1548, Merapi has erupted violently 68 times. In 1998, it became active again, and people began to evaluate. When the island of Krakatau ...
Landforms at plate margins – Volcanoes and supervolcanoes
Landforms at plate margins – Volcanoes and supervolcanoes

... A volcano is a cone-shaped mountain formed by surface eruptions from a magma chamber inside the Earth. The magma that reaches the surface in an eruption is called lava, and is one of the many different products that can be thrown out, including ash, cinders, pumice, dust, gases and steam. The world ...
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Silverthrone Caldera



The Silverthrone Caldera is a potentially active caldera complex in southwestern British Columbia, Canada, located over 350 kilometres (220 mi) northwest of the city of Vancouver and about 50 kilometres (31 mi) west of Mount Waddington in the Pacific Ranges of the Coast Mountains. The caldera is one of the largest of the few calderas in western Canada, measuring about 30 kilometres (19 mi) long (north-south) and 20 kilometres (12 mi) wide (east-west). Mount Silverthrone, an eroded lava dome on the caldera's northern flank that is 2,864 metres (9,396 ft) high may be the highest volcano in Canada.The main glaciers in the Silverthrone area are the Pashleth, Kingcome, Trudel, Klinaklini and Silverthrone glaciers. Most of the caldera lies in the Ha-Iltzuk Icefield, which is the largest icefield in the southern half of the Coast Mountains; it is one of the five icefields in southwestern British Columbia that thinned between the mid-1980s and 1999 due to global warming. Nearly half of the icefield is drained by the Klinaklini Glacier, which feeds the Klinaklini River.The Silverthrone Caldera is very remote and rarely visited or studied by geoscientists, such as volcanologists. It can be reached by helicopter or — with major difficulty — by hiking along one of the several river valleys extending from the British Columbia Coast or from the Interior Plateau.
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