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Volcanoes!
Volcanoes!

... Steeper, form in clusters (on sides of shield/composite) ...
Volcanoes
Volcanoes

... the volcano, swept down the river valleys on the side of the edifice and destroyed Armero and Chinchina. The footage of rescue efforts after the lahar were devastating and heartbreaking. Sadly, this disaster was mostly preventable as the citizens of these towns could have had at least an hour's warn ...
Types of Volcanoes Dangers from Composite Cones Pyroclastic
Types of Volcanoes Dangers from Composite Cones Pyroclastic

... twisted and braided rope. aa flow – rough, jagged blocks with sharp edges. Melted rhyolitic rock flows very slowly. ...
lesson 24 effects of ash fall
lesson 24 effects of ash fall

... Magma is buoyont, and lighter than the solid rock that surrounds it, which is why it rises. ...
QR-Volcanoes 59 points Using separate pieces of paper, answer
QR-Volcanoes 59 points Using separate pieces of paper, answer

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Volcanoes
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-1- 1. Distinguish between intrusive and extrusive igneous rocks. 2
-1- 1. Distinguish between intrusive and extrusive igneous rocks. 2

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volcanoes-notes

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7.3 Volcanoes continued

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why live enar a volcano

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Science 1 Notes: Volcanoes
Science 1 Notes: Volcanoes

... stone is used as a cleaner. B. Intrusive igneous rocks (plutonic) are formed when magma cools slowly beneath the earth’s surface. We only see this rock when the layers of rock above it are eroded away. The Sierra Nevada Mountain range was formed from a large pool of magma that cooled below the earth ...
Ch 3 Sec 4: Volcanic Landforms
Ch 3 Sec 4: 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. Landforms formed when lava flows build up: 1. shield volcanoes- At some places on Earth’s surface, thin layers of lava p ...
Earth Science - Mr.E Science
Earth Science - Mr.E Science

... – Crater - a bowl-shaped area around a volcano's central vent. – Pyroclastic Flow -an explosive fast-moving current of hot gas and rock (1800 0F) hurls out ash, cinders, and bombs. ...
Volcanoes - Pacific Disaster Net
Volcanoes - Pacific Disaster Net

... gas bubbles can escape from it, leading to more violent eruptions. However, if water is present during the eruption, even highly fluid magma can erupt explosively - these hydrovolcanic eruptions lead to violent steam explosions, fragmenting the magma into fine-grained ash. ...
Introduction to volcano characteristics and activity
Introduction to volcano characteristics and activity

... pyroclastic material, formed by collapse of the volcanic column or collapse of accumulated viscous lava. They are deadly and few have survived a direct hit by one. Volcanic mudflows, also more commonly known as lahars, their Indonesian name where they are common. Lined to steep sided cones, they for ...
Answers to the 13-2 two column notes
Answers to the 13-2 two column notes

... Caldera (Define and example)It is when a magma chamber empties and the volcanic cone collapses to leave a large , basin shaped depression called a caldera. Mount Mazama in Oregon erupted and formed a caldera that later filled with water and is now called Crater Lake. ...
THIS Volcano powerpoint
THIS Volcano powerpoint

... the simplest type of volcano. They are built from particles and blobs of congealed lava ejected from a single vent. As the gas-charged lava is blown violently into the air, it breaks into small fragments that solidify and fall as cinders around the vent to form a circular or oval cone. These are the ...
Hot Spot
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... he people who live near Italy’s Mount Vesuvius (veh-SOO-veeuhs) must be ready to leave the area at any time. Why? Vesuvius, a huge volcano, may soon erupt, or explode. That means big trouble for those people—all 2 million of them! ...
Volcanoes - BrainPOP
Volcanoes - BrainPOP

... 1. Which of the following is an opinion about volcanic activity? a. Volcanoes are made of hardened lava b. A large number of volcanoes can be found along the edge of the Pacific Ocean c. The 1991 eruption of Mt. Pinatubo was the scariest volcanic event in history d. Shield volcanoes can actually cre ...
Shapes of igneous bodies
Shapes of igneous bodies

... Extrusive bodies – Pyroclastic Landforms Pyroclastic Deposits include – volcaniclastic – formed by volcano (process irrelevant) - pyroclastic – formed from magma/lava aerially expelled from vent - lahar – volcanic debris mixed with water/melting ice or snow Pyroclastic Fall Deposits – material falls ...
6VolcanicT2 - Arizona State University
6VolcanicT2 - Arizona State University

... Imagery seen in this presentation is courtesy of Ron Dorn and other ASU colleagues, students and colleagues in other academic departments, individual illustrations in scholarly journals such as Science and Nature, scholarly societies such as the Association of American ...
Notes 13.2 Studying the composition of rocks, scientists determine
Notes 13.2 Studying the composition of rocks, scientists determine

...  Made of pyroclastic material o COMPOSITE VOLCANO Made of alternating layer of hardened lava flows and pyroclastic material.  During quiet eruption, lava flows cover the side of the cone  During explosive eruption, large amts of pyroclastic material builds up around the vent.  Quiet-explosive-q ...
File
File

... 4. Rocks are classified by what they are made of and how they form. Igneous rocks always begin as magma. What are the two main types of igneous rocks, and what is the main difference between them? How does each type form into solid rock? ...
Volcanoes
Volcanoes

... • Composite volcanoes – AKA stratovolcanoes – Moderately to steeply sloping – Constructed of alternating layers of pyroclastic debris and solidified lava flows – Composed primarily of intermediate composition volcanic rocks (i.e., andesite) – Most common type of volcano at convergent plate boundarie ...
Geysers: Types: cone (has a cone of “geyserite” around a small vent
Geysers: Types: cone (has a cone of “geyserite” around a small vent

... II. Felt only by a few persons at rest, especially on upper floors of buildings. III. Felt quite noticeably by persons indoors, especially on upper floors of buildings. Many people do not recognize it as an earthquake. Standing motor cars may rock slightly. Vibrations similar to the passing of a tru ...
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Mount St. Helens



Mount St. Helens or Louwala-Clough (known as Lawetlat'la to the indigenous Cowlitz people, and Loowit to the Klickitat) is an active stratovolcano located in Skamania County, Washington, in the Pacific Northwest region of the United States. It is 96 miles (154 km) south of Seattle, Washington, and 50 miles (80 km) northeast of Portland, Oregon. Mount St. Helens takes its English name from the British diplomat Lord St Helens, a friend of explorer George Vancouver who made a survey of the area in the late 18th century. The volcano is located in the Cascade Range and is part of the Cascade Volcanic Arc, a segment of the Pacific Ring of Fire that includes over 160 active volcanoes. This volcano is well known for its ash explosions and pyroclastic flows.Mount St. Helens is most notorious for its catastrophic eruption on May 18, 1980, at 8:32 a.m. PDT, the deadliest and most economically destructive volcanic event in the history of the United States. Fifty-seven people were killed; 250 homes, 47 bridges, 15 miles (24 km) of railways, and 185 miles (298 km) of highway were destroyed. A massive debris avalanche triggered by an earthquake measuring 5.1 on the Richter scale caused an eruption that reduced the elevation of the mountain's summit from 9,677 ft (2,950 m) to 8,363 ft (2,549 m), replacing it with a 1 mile (1.6 km) wide horseshoe-shaped crater. The debris avalanche was up to 0.7 cubic miles (2.9 km3) in volume. The Mount St. Helens National Volcanic Monument was created to preserve the volcano and allow for its aftermath to be scientifically studied.As with most other volcanoes in the Cascade Range, Mount St. Helens is a large eruptive cone consisting of lava rock interlayered with ash, pumice, and other deposits. The mountain includes layers of basalt and andesite through which several domes of dacite lava have erupted. The largest of the dacite domes formed the previous summit, and off its northern flank sat the smaller Goat Rocks dome. Both were destroyed in the 1980 eruption.
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