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6. Volcano PowerPoint
6. Volcano PowerPoint

... Volcanoes are classified according to their form. The form of a volcanoes depends on the type of material that it is made up of. The nature of the extruded material (and the volcano itself) depends on the properties of the magma. Magma: Molten rock within the Earth. ...
Types of Magma - Teacher Notes
Types of Magma - Teacher Notes

... Viscosity • Viscosity – internal resistance to flow • Low Viscosity ...
Types of Magma - Dublin City Schools
Types of Magma - Dublin City Schools

... Andesitic Medium 3-4% Rhyolitic High ...
view the Lecture Presentation
view the Lecture Presentation

... Avalanches of hot ash (200Co–450oC) that race ...
Name: Date: Pd. Volcano Webquest Worksheet *1*Explore
Name: Date: Pd. Volcano Webquest Worksheet *1*Explore

... *2*List the types of volcanoes and give examples of each. Types of Volcanoes http://pubs.usgs.gov/gip/volc/types.html ...
Volcanoes
Volcanoes

... Volcanoes can create islands out of lava that rises from the ocean floor. Volcanic ash and lava make good soil. Volcanoes can also provide heat and power. Maybe some day we will get our power from volcanoes. ...
Exam 2 Review Sheet Handout Page
Exam 2 Review Sheet Handout Page

... 3) What is meant by mafic? Sialic or felsic? 4) What is Bowen’s Reaction Series? 5) What are the different igneous rocks and how does each relate to both texture and composition? Volcanism 1) What is meant by viscosity? How does it relate to magma composition and temperature? 2) How does viscosity r ...
Lahar in a jar - PRA Classical Academy for Homeschoolers
Lahar in a jar - PRA Classical Academy for Homeschoolers

... Earth's heat is released in Yellowstone by two main processes, conduction and convection: 1. Conduction is the movement of heat from hotter material to colder material. A common example of conduction is when heat from a stove is transferred through the bottom of a coffee pot to the liquid inside. Co ...
Volcanoes
Volcanoes

... • A circular pattern located around the pacific ocean along the plate boundaries where volcanoes are more common ...
Earth Science--Ch 9 Volcanoes Review Guide
Earth Science--Ch 9 Volcanoes Review Guide

... What is a hot spot?/ Where does most hot spot volcanic activity occur? Do hot spots move? What are the locations of some hot spots? What state was formed by a hot spot? ...
volcanoes - Catawba County Schools
volcanoes - Catawba County Schools

... • Name given to particles produced by eruption. They range in size from very fine dust to pieces that weigh several tons • Lapilli- range from small beads to walnuts (2-64 mm). Also called cinders • Blocks- anything larger than 64 mm and are made of hardened lava and bombs (which are pieces of semi- ...
Volcanoes
Volcanoes

... Mantle- The 2900-kilometer- (1800mile-) thick layer of Earth located below the crust. Crust- The very thin outermost layer of Earth. Magma- A body of molten rock found at depth, including any dissolved gases and crystals. Pyroclastic Materials- The volcanic rock ejected during an eruption, including ...
Crustal Deformation
Crustal Deformation

... 22. Where do Earthquakes usually occur? List some examples on the Earth. 23. Can earthquakes occur in the middle of a continent? If so, give a few examples. 24. Describe in detail the method seismologists use to locate an earthquake. Include P and S waves, travel time curves, and triangulation in yo ...
Hazards Chapter 3a
Hazards Chapter 3a

... people die or are displaced by them ...
Explosive Pyroclastic A volcano is a mountain formed beneath the
Explosive Pyroclastic A volcano is a mountain formed beneath the

... Explosive Pyroclastic A volcano is a mountain formed beneath the ground when the Earth’s crust meets the mantle and magma collects there until it rises to the surface because magma is less dense than the surrounding rock is. Then the magma becomes liquid. Shield, cinder cone, and composite volcanoes ...
Primary Later Phase (& KS3)
Primary Later Phase (& KS3)

... • Hot flows burning trees and buildings. ...
Volcanoes and Igneous Activity Earth - Chapter 4
Volcanoes and Igneous Activity Earth - Chapter 4

... Active - eruptions have occurred in historic times  Dormant - no historic eruptions have occurred ...
VOLCANOETYPES
VOLCANOETYPES

...  Sea Floor spreading zones → non-explosive (quiet- shield)  Hot spot → usually non-explosive, but can be explosive ...
Volcanic history HTML or RTF format, or link to related web page
Volcanic history HTML or RTF format, or link to related web page

... hot, similar to pyroclastic flows, most of those on Deception Island were probably relatively cold and contained water and/or steam at temperatures mainly below the boiling point of water. Any eruptions within or at low elevations around the margins of Port Foster are likely to be characterised by a ...
Volcanic Eruptions 2 - Earth Science > Home
Volcanic Eruptions 2 - Earth Science > Home

... Can Scientists Predict Volcanic Eruptions? Scientists cannot always predict where or when a volcano will erupt. However, by studying volcanoes, scientists have been able to identify some clues about when an eruption may happen. One way scientists predict volcanic eruptions is by studying the earthqu ...
2.4-Volcanic features
2.4-Volcanic features

... • the rapid melting of snow and ice by pyroclastic flows, •intense rainfall on loose volcanic rock deposits •breakout of a lake dammed by volcanic deposits. ...
Volcanoes I
Volcanoes I

... Volcanoes are classified according to their form. The form of a volcanoes depends on the type of material that it is made up of. The nature of the extruded material (and the volcano itself) depends on the properties of the magma. Magma: Molten rock within the Earth. ...
Skinner Chapter 7
Skinner Chapter 7

... 4. Water vapor and carbon dioxide together make up about half of all gases emitted from volcanoes. 5. Because of their low viscosities, basaltic lava flows move more quickly than pyroclastic flows. 6. Violent undersea eruptions can cause tsunamis. 7. A fissure eruption is a type of eruption in which ...
Volcanic Acid-Base Reaction
Volcanic Acid-Base Reaction

... Objective: In this activity, students will build a volcano by combining an acid and an alkaline substance. They will explore the properties of acids and bases and will learn to identify these substances in their environment. ...
Ch 3 Sec 4: Volcanic Landforms
Ch 3 Sec 4: Volcanic Landforms

... cracks and travel a long distance before cooling and hardening forming high level areas. Over millions of years, these layers of lava build up over a large area to form a lava plateau. Ex. Columbia Plateau An enormous eruption may empty a volcano’s main vent and magma chamber. With nothing to suppor ...
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Mount Pinatubo



Mount Pinatubo (Filipino: Bundok Pinatubo) is an active stratovolcano in the Cabusilan Mountains on the island of Luzon, near the tripoint of the Philippine provinces of Zambales, Tarlac, and Pampanga. Before the volcanic activities of 1991, its eruptive history was unknown to most people. It was heavily eroded, inconspicuous and obscured from view. It was covered with dense forest which supported a population of several thousand indigenous people, the Aetas, who fled to the mountains during the Spanish conquest of the Philippines.The volcano's Plinian / Ultra-Plinian eruption on 15 June 1991 produced the second largest terrestrial eruption of the 20th century after the 1912 eruption of Novarupta in the Alaska Peninsula.Complicating the eruption was the arrival of Typhoon Yunya (Diding), bringing a lethal mix of ash and rain to areas surrounding the volcano. Successful predictions at the onset of the climactic eruption led to the evacuation of tens of thousands of people from the surrounding areas, saving many lives, but the surrounding areas were severely damaged by pyroclastic flows, ash deposits, and subsequently, by the lahars caused by rainwaters re-mobilizing earlier volcanic deposits causing extensive destruction to infrastructure and changing the river systems months to years after the eruption.The effects of the eruption were felt worldwide. It ejected roughly 10,000,000,000 tonnes (1.1×1010 short tons) or 10 km3 (2.4 cu mi) of magma, and 20,000,000 tonnes (22,000,000 short tons) SO2, bringing vast quantities of minerals and metals to the surface environment. It injected more particulate into the stratosphere than any eruption since Krakatoa in 1883. Over the following months, the aerosols formed a global layer of sulfuric acid haze. Global temperatures dropped by about 0.5 °C (0.9 °F) in the years 1991-93, and ozone depletion temporarily increased substantially.
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