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Across
Across

... occurs; mid-ocean ridge is formed 9. Volcanoes made of only rock and ash 11. Process of changing rocks from one type to another 14. Inorganic, solid, naturally occurring substance with a definite chemical and crystal composition 15. Point under the surface where the earthquake begins 16. Moving smal ...
Document
Document

... --both violent & mild --both lava flows & tephra --andesitic lava / found “near” coasts --medium amount of silica --example = Mt. St. Helens & Andes ...
Basalt has a high melting point and is very runny (like honey) – in
Basalt has a high melting point and is very runny (like honey) – in

... and it flows like cold treacle. Because if flows more slowly than basalt, it forms volcanic cones with a much steeper shape, called cone volcanoes. Examples of cone volcanoes include Mt Taranaki and Mt Ruapehu. Rhyolite magma is the most viscous type of magma – it flows like tar. It is light in colo ...
File
File

... Not just one type  • What are volcanoes? • Where do they form? • How do they erupt? • What are the different types of volcanoes ...
Chapter 19
Chapter 19

Miscellaneous Earth`s Layers Volcanoes Earthquakes
Miscellaneous Earth`s Layers Volcanoes Earthquakes

... During an earthquake, why do S and P waves arrive at detection points at different times? ...
Unit 2-Earth History
Unit 2-Earth History

... of a volcano can be measured in millions of years, so a volcano that has not erupted in thousands of years would most likely be classified as dormant, rather than extinct. Finally, students may believe that volcanoes are only dangerous due to lava flows. In reality, pyroclastic flows, ash clouds, an ...
Volcanic Landforms
Volcanic Landforms

... essential feature of a composite volcano is a conduit system through which magma from a reservoir deep in the earth's crust rises to the surface. The volcano is built up by the accumulation of material erupted through the conduit and increases in size as lava, cinders, ash etc. are added to its slop ...
Volcanoes and Igneous Activity Earth - Chapter 4 - sir
Volcanoes and Igneous Activity Earth - Chapter 4 - sir

... Composite cone (stratovolcano) Most are located adjacent to the Pacific Ocean (e.g., Mount Fujiyama and Mount ...
Volcanoes and Other Igneous Activity - sir
Volcanoes and Other Igneous Activity - sir

... Viscosity is a measure of a material’s resistance to flow (e.g., higher viscosity materials flow with great difficulty) Factors affecting viscosity ...
Dark_Skies_2
Dark_Skies_2

... Pristine Atmosphere ...
Volcanoes PPT
Volcanoes PPT

... Chapter 18 ...
Volcanoes - GK
Volcanoes - GK

... in the bowl of hot water. 2. Lay the pegboard on top of a food serving tray to collect drips. 3. Weave the airline tubing into the pegboard from the top and back up through the bottom so that 2” or so of tubing is sticking up out of the pegboard. Remove the plunger. 4. Fill the syringe with your pre ...
Volcano Power Point
Volcano Power Point

... the vent and the collapse of material back into vent ...
Liquid Hot Magma.
Liquid Hot Magma.

... in the bowl of hot water. 2. Lay the pegboard on top of a food serving tray to collect drips. 3. Weave the airline tubing into the pegboard from the top and back up through the bottom so that 2” or so of tubing is sticking up out of the pegboard. Remove the plunger. 4. Fill the syringe with your pre ...
Volcanic
Volcanic

... Lava: Magma that reaches the surface and is exposed to the atmosphere. Vent: The path gas and magma use to escape the crust. ...
58 Earth Review Power Point 2011
58 Earth Review Power Point 2011

... C. Convergent D. Convergent with subduction C. large mountains D. Volcanoes, Small Mountains, and Deep Oceanic Trenches ...
QR-Volcanoes 59 points Using separate pieces of paper, answer
QR-Volcanoes 59 points Using separate pieces of paper, answer

... and caldera (assuming the volcano is dormant) 11. Extensive pyroclastic flow deposits are associated with which volcanic structure? 12. How to the eruptions that created the Columbia Plateau differ from eruptions that create large composite cones? 13. What is Shiprock, New Mexico, and how did it for ...
Name Date Z - SPS186.org
Name Date Z - SPS186.org

Volcano Jeopardy Round 1 Location, location, location! Most
Volcano Jeopardy Round 1 Location, location, location! Most

... b. What causes volcanoes that are located in the middle of a plate?  Hotspots c. Island arc volcanoes are formed along what type of boundary?  Subduction zone or convergent boundary d. Most volcanic activity on Earth can be found along what type of boundary?  Spreading centers or divergent bounda ...
Lesson Plan by : Laura Murphy, Arnone School Title : Volcanoes
Lesson Plan by : Laura Murphy, Arnone School Title : Volcanoes

... 1) Volcanoes are vents, or openings, in the Earth 2) They let heat from deep inside the Earth escape. 3) Volcanoes spout steam, ash, gases, and melted rock. 4) Earth has three layers: the crust, mantle, and the core. 5) Deep down, 3 to 25 miles, below the crust is a soft, hot layer (the mantel). 6) ...
Volcanic Hazards
Volcanic Hazards

... • One of the 19 active volcanoes in Japan • Erupted and killed ~15,000 people 200 years ago • Erupted violently on June 3, 1991 • Thousands of ash flows by the end of 1993, getting the dubious honor of the king of the ash flow centers • 44 people killed, including Harry Glicken, a U.S. volcanologist ...
Volcanoes-Help of Hindrance
Volcanoes-Help of Hindrance

Volcano Notes 2012
Volcano Notes 2012

... • Pyroclastic layers and lava flows of intermediate composition • Lahars: volcanic mudflow, rain or eruption • Steep-sided near top • Typical in continental and island volcanic arcs at convergent boundaries • Violent and dangerous eruptions ...
Volcano Notes
Volcano Notes

... nature than shield volcanoes. ...
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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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