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06 Volcanoes and earthquakes
06 Volcanoes and earthquakes

... that they cannot be felt by humans, though they can be detected by sensitive instruments called seismographs which measure earthquake strength or magnitude on the Richter Scale. Numbers on this scale range from 0 to 9, though no real upper limit exists. An earthquake whose magnitude is greater than ...
Mid-Term Review - Jeopardy 2012
Mid-Term Review - Jeopardy 2012

... main types of volcanoes? ...
Earthquakes and Volcanoes
Earthquakes and Volcanoes

... Locations of Volcanoes • Volcanic activity may occur under the ocean, at hot spots, along plate boundaries, and along the Ring of Fire. • Ring of Fire – active volcanoes around the edges of the Pacific Ocean • Under water eruptions (submarine eruptions) are 20x more frequent than eruptions on land • ...
Earthquakes and Volcanoes
Earthquakes and Volcanoes

... Locations of Volcanoes • Volcanic activity may occur under the ocean, at hot spots, along plate boundaries, and along the Ring of Fire. • Ring of Fire – active volcanoes around the edges of the Pacific Ocean • Under water eruptions (submarine eruptions) are 20x more frequent than eruptions on land • ...
Mass Extinctions
Mass Extinctions

... • Volcanic activity has been part of the nature of the changing planet • As continents collided and mountains built up, volcanoes formed • During the Precambrian time volcanic activity was one of the most natural events • Lava flows, ash clouds in the atmosphere, and heat made conditions for life ex ...
Ready Set Go for teachers
Ready Set Go for teachers

Chapter 13 Section 2
Chapter 13 Section 2

... Volcanic Eruptions Types of Magma/Lava • Mafic - describes magma or igneous rock that is rich in magnesium and iron and that is generally dark in color • Felsic - describes magma or igneous rock that is rich in feldspar and silica and that is generally light in color • Mafic rock commonly makes up t ...
Year 9 Revision
Year 9 Revision

Volcano Project
Volcano Project

... There are 3 basic types of volcanoes, some are explosive and some erupt quietly. Some are active for millions of years and others for only a few years. The type of volcanic structure and its location on Earth’s surface is determined by the type of magma it erupts. The type of magma is determined by ...
Volcanoes Part I: classification, deposits, and their distribution
Volcanoes Part I: classification, deposits, and their distribution

... 2/3 of all volcanoes are along the Ring of Fire that surrounds the Pacific Ocean. ...
File
File

... of eruption or which erupt at least once in every ten years. Active volcanoes are likely to be found in the following places (according to the order of appearance). - Divergent boundaries. E. g. Krafla, Loki, Hekla and Katla volcanoes in Iceland - Over Hot Spots. E. g. Mauna Loa, Mauna Kea and Kohal ...
Earth Science Notes NAME: Chapter Nine-Volcanoes
Earth Science Notes NAME: Chapter Nine-Volcanoes

Chapter 2 c Primary Structures e
Chapter 2 c Primary Structures e

... Tephra layers fine away from source ...
Name:___ANSWER KEY
Name:___ANSWER KEY

... b. how the use of sonar in World War 2 helped support the theory of plate tectonics. The use of sonar allowed for mapping of the ocean floor. It was there that the discovery of oceanic ridges, mountains, and volcanoes were found. ...
SUBDUCTION boundaries
SUBDUCTION boundaries

... oceanic plate goes under ...
http://kids - wikifuller
http://kids - wikifuller

... 4. Explain where the ring of fire can be found: ...
ttu_gs0001_000441.
ttu_gs0001_000441.

Geology Unit Study Guide
Geology Unit Study Guide

... 2. Who proposed the theory of continental drift? 3. Why was this theory not accepted? 4. What caused the tectonic plates to move? 5. What evidence did Wegener have that showed that Pangaea once existed? 6. How has technology aided in the support of continental drift? 7. What is the theory of plate t ...
magma chamber - Madison County Schools
magma chamber - Madison County Schools

... pressure on the magma decreases. This allows the gases in the magma to begin to bubble out. These gas bubbles take up more space than the dissolved gases. The bubbles force magma out of the vent, like the bubbles that force warm Coke out of a bottle. ...
Chapter 2 Notes
Chapter 2 Notes

... movement of rocks on both sides of fault ...
Volcanoes
Volcanoes

... oCommonly built from gravel size lava rock fragments called cinders oViolent eruptions, dangerous when close---High pressure gas bubbles causes thick lava to explode into the air, lava begins to cool as it rises and falls becoming very sticky oWhen lava hits the ground it sticks rather than flows oT ...
Volcano Reading and questions
Volcano Reading and questions

... ocean floor, creating volcanoes. The resulting volcanoes create a string of islands called an island arc. Volcanoes also occur where an oceanic plate is subducted beneath a continental plate. Some volcanoes result from “hot spots” in Earth’s mantle. A hot spot is an area where material from within t ...
Global Map-Essential Questions 1. Which plate boundary types
Global Map-Essential Questions 1. Which plate boundary types

... Most of the stickers on the map will be placed on or near subduction zones at convergent boundaries. Divergent boundaries (e.g., mid-ocean ridges) are major producers of volcanoes as well. ...
Where Are the Volcanoes?
Where Are the Volcanoes?

... large map as a class. Discuss the results. What patterns do students notice? Student should realize that volcanoes tend to be located in clusters. Introduce tectonic plates and plate boundaries at your discretion. Students may also realize that not all volcanoes are found only on land and that volca ...
HW 2: Plate Tectonics
HW 2: Plate Tectonics

... Attached is the map portion of a 3-dimensional diagram of three major tectonic plates (labeled plates 1 through 3) carrying two different continents: “Bella Casa” and “Mirabella”. The large arrows in the middle of the diagram indicate the direction of plate movement; the dashed lines represent the l ...
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Volcano



A volcano is a rupture on the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface.Earth's volcanoes occur because its crust is broken into 17 major, rigid tectonic plates that float on a hotter, softer layer in its mantle. Therefore, on Earth, volcanoes are generally found where tectonic plates are diverging or converging. For example, a mid-oceanic ridge, such as the Mid-Atlantic Ridge, has volcanoes caused by divergent tectonic plates pulling apart; the Pacific Ring of Fire has volcanoes caused by convergent tectonic plates coming together. Volcanoes can also form where there is stretching and thinning of the crust's interior plates, e.g., in the East African Rift and the Wells Gray-Clearwater volcanic field and Rio Grande Rift in North America. This type of volcanism falls under the umbrella of ""plate hypothesis"" volcanism. Volcanism away from plate boundaries has also been explained as mantle plumes. These so-called ""hotspots"", for example Hawaii, are postulated to arise from upwelling diapirs with magma from the core–mantle boundary, 3,000 km deep in the Earth. Volcanoes are usually not created where two tectonic plates slide past one another.Erupting volcanoes can pose many hazards, not only in the immediate vicinity of the eruption. One such hazard is that volcanic ash can be a threat to aircraft, in particular those with jet engines where ash particles can be melted by the high operating temperature; the melted particles then adhere to the turbine blades and alter their shape, disrupting the operation of the turbine. Large eruptions can affect temperature as ash and droplets of sulfuric acid obscure the sun and cool the Earth's lower atmosphere (or troposphere); however, they also absorb heat radiated up from the Earth, thereby warming the upper atmosphere (or stratosphere). Historically, so-called volcanic winters have caused catastrophic famines.
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