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Inside Earth 3.3 Volcanic Landforms
Inside Earth 3.3 Volcanic Landforms

... volcanoes? Describe one of them. ...
Volcanoes
Volcanoes

... Krakatau • Killed 36,000 people most were killed by a giant tsunami • Destroyed 160 villages • Fine ashes from the eruption were carried by upper level winds as far away as New York City • Volcanic dust lowered global temperatures for five years, this caused ...
Volcanoes I - Faculty Washington
Volcanoes I - Faculty Washington

... As a result of this lesson and the reading, you should be able to:  Define the following terms or phrases: Shield Volcano, Stratovolcano, Flood Basalts, Lahar, Pyroclastics, Lava.  Distinguish between the volcanism found over hot spots, subduction zones, and spreading centers in terms of their roc ...
QR-Volcanoes 59 points Using separate pieces of paper, answer
QR-Volcanoes 59 points Using separate pieces of paper, answer

... 1. List three factors that determine the nature of a volcanic eruption. What role does each play? 2. What is viscosity? How does the chemistry (concentration of SiO2) influence magma’s viscosity? How does temperature influence magma’s viscosity? 3. Why is a volcano fed by highly viscous magma likely ...
VOLCANOES form where molten rock is vented at Earth`s surface.
VOLCANOES form where molten rock is vented at Earth`s surface.

... A size comparison of the three types of volcanoes ...
Take a `Chance` on the volcano erupting
Take a `Chance` on the volcano erupting

... volcanoes! How much force does it take to set off a party popper ‘volcano’?’ N.B. We have recommended using 100g masses in this activity. To convert the mass in grams into the approximate force in Newtons, divide the ...
What is Lava? - Princeton ISD
What is Lava? - Princeton ISD

... • Nonexplosive Eruptions ...
Google Earth Volcano Lab
Google Earth Volcano Lab

... In this lab, you will be visiting many different volcanoes. As we learned, there are 3 different types of volcanoes that can be classified in different ways. Each volcano is unique. For every volcano you see, you will be asked to find the following information: ...
The Cascade Volcanoes - West Virginia University
The Cascade Volcanoes - West Virginia University

... Pyroclastic material - any volcanic material that is ejected from volcanic vents as loose or fragmental material; includes many specific terms that refer to shapes or sizes of particles (ash, bombs, pumice, cinders, etc.) Only 1/100th of the volume of large shield!! ...
Volcano types and projectiles
Volcano types and projectiles

... The vent on the top of a volcano is called a crater. A caldera is the remnants of a volcano whose cone has collapsed. Krakatau is the most well-known caldera, sporting a diameter of 6 km. ...
Slide 1
Slide 1

... Plutons- intrusive igneous rock bodies which are classified by shape, size, and their relationship to other surrounding rocks. -Batholiths-LARGEST plutons, irregularly shaped, coarsegrained igneous rocks. -Laccoliths-mushroom-shaped pluton with a round top and flat bottom. Relatively small -Sills-wh ...
The Ring of Fire - American Red Cross
The Ring of Fire - American Red Cross

... rub against each other. Around the Pacific Ocean plate, this pushing and rubbing sometimes causes earthquakes. It has also created a string of volcanoes that runs from New Zealand all the way around to the tip of South America — The Ring of Fire. This map shows the locations of some volcanoes on The ...
Section 9.1 How and where volcanoes form
Section 9.1 How and where volcanoes form

... rounded lumps of lava that crack forming pillow shapes because of the drastic temperature change in the ocean. ...
Volcanoes - Types and structure
Volcanoes - Types and structure

... These volcanoes are created at constructive margins. This is where two plates are moving apart from each other and magma moves to the surface through the gap. The emerging lava is more fluid and therefore the shape of the volcano is low and wide. This is why it is called a ‘shield’ volcano. ...
Chapter 12
Chapter 12

... Mt. Everest. Unlike Everest, Olympus Mons has a very gentle slope. It is up to 550 km at its base. ...
File
File

... Central vent filled from previous eruption ...
Eruption
Eruption

... This is the fiercest eruption of all because the gases and magma become trapped inside the volcano. This causes a huge explosion, which can be big enough to remove the top of the whole mountain! ...
Chapter 6 study guide
Chapter 6 study guide

... 9. If lava hardens quickly on the surface, what kind of texture will the igneous rock have? 10. If magma begins to harden slowly underground, then is forced up to the surface and continues to harden quickly, what kind of texture will the rock have? 11. Give an example of an igneous rock with fine te ...
Subject
Subject

...  Timeline of eruptions ...
Volcanoes SHOW
Volcanoes SHOW

... Combination of explosive activity (pyroclastic) and lava flows Responsible for most deaths of any type of volcano ex. Mount Saint Helens Mt. Pinatubo Mt. Fuji Mt. Vesuvius ...
Introduction to volcanoes, volcanic eruptions, and volcanic
Introduction to volcanoes, volcanic eruptions, and volcanic

... Lower viscosity basaltic lava (mafic) is ~45% to 54% silica ...
chapter 9 vocabulary terms
chapter 9 vocabulary terms

... Partial Melting (p. 273) – The process by which most igneous rocks melt. Since individual minerals have different melting points, most igneous rocks melt over a temperature range of a few hundred degrees. If the liquid is squeezed out after some melting has occurred, a melt with a higher silica cont ...
Volcanoes
Volcanoes

... that shoot small pieces of magma and ash into the air. O The magma then cools and hardens as it falls back to the Earth, forming a cinder cone. O In many cases, cinder cones form on the sides of a larger volcano. ...
Volcanoes
Volcanoes

... Dormant- are not currently erupting but are considered likely to do so. Mt. St Helens was dormant for 123 years before it erupted in 1980. ...
Volcanic Eruptions
Volcanic Eruptions

... • What causes these different types of volcanoes to form? • The different ways in which they erupt and the different materials that are erupted. ...
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Teide



Mount Teide (Spanish: Pico del Teide, IPA: [ˈpiko ðel ˈteiðe], ""Teide Peak"") is a volcano on Tenerife in the Canary Islands. Its 3,718-metre (12,198 ft) summit is the highest point in Spain and the highest point above sea level in the islands of the Atlantic. At 7,500 m (24,600 ft) from its base on the ocean floor, it is the third highest volcano on a volcanic ocean island in the world after Mauna Kea, Mauna Loa and others in Hawaii. Its elevation makes Tenerife the tenth highest island in the world. It remains active: its most recent eruption occurred in 1909 from the El Chinyero vent on the northwestern Santiago rift. The United Nations Committee for Disaster Mitigation designated Teide a Decade Volcano because of its history of destructive eruptions and its proximity to several large towns, of which the closest are Garachico, Icod de los Vinos and Puerto de la Cruz. Teide, Pico Viejo and Montaña Blanca form the Central Volcanic Complex of Tenerife.The volcano and its surroundings comprise Teide National Park, which has an area of 18,900 hectares (47,000 acres) and was named a World Heritage Site by UNESCO on June 28, 2007. It is one of the most visited national parks in the world, with a total of 2.8 million visitors, according to the Instituto Canario de Estadística (ISTAC). In 2013 it was the ninth most visited national park in the world. The Teide is the most visited natural wonder of Spain.
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