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Earth and Space Science Part 3
Earth and Space Science Part 3

... floor where plates are moving apart. Volcanic mountains add to the continental crust when they form on land. They also enrich the soil. ...
Mountains and Volcanoes
Mountains and Volcanoes

... • Magma is thick and sticky. • Water from descending plate heats up and forms steam. • Steam increases pressure in volcano, which causes it to explode. • ex) Mount St. Helens, Washington Mount St Helens, 1980 ...
Chapter 29: Formation of Rocks
Chapter 29: Formation of Rocks

... Solid rock melts and becomes magma under certain conditions that lower the melting point of the material. ...
Composite volcanoes
Composite volcanoes

... viscous (thick) magma. • When very viscous magma rises to the surface, it usually clogs the craterpipe, and gas in the craterpipe gets locked up. • Therefore, the pressure will increase resulting in an explosive eruption. ...
Volcano Characteristics
Volcano Characteristics

... you live near a volcano? What are the chances that it will erupt in your lifetime? If you don’t live near one, could a volcanic eruption elsewhere cloud the skies above where you live? ...
Chapter 6
Chapter 6

... thinner than continental crust ...
Ch 12 Vocabulary - Taylor County Schools
Ch 12 Vocabulary - Taylor County Schools

... that arises in the middle of a tectonic plate. Hot spots do not move. Pyroclasts – Material expelled from a volcano that cools and becomes solid as it falls to Earth. Volcanic blocks – Chunks of solid material ripped away from the opening of the volcano and expelled into the air. ...
Volcanoes
Volcanoes

... • Asthenosphere is extremely rich in ferromagnesian (ultramafic) and a melt from it is mafic (or ultramafic) • Basalt is emplaced as new seafloor at the spreading ridge or a rift • Rift systems in continental crust may melt granitic crust and produce andesite or rhyolite lavas – A bimodal suite of e ...
File
File

... spreading, mid-ocean ridges, subduction zones, earthquakes and volcanoes, mountain ranges) that occur on or near the Earth’s surface. • Explain why tectonic plates move using the concept of heat flowing through mantle convection, coupled with the cooling and sinking of aging ocean plates that result ...
Chapter 5
Chapter 5

Science Unit - Western Springs College
Science Unit - Western Springs College

Volcanic activity
Volcanic activity

... Types of volcanoes  Shield volcano  Mountain w/ broad gently sloping sides that forms when basaltic rock is layered  Cinder cone volcanoes  Forms when material is ejected high in to the air and piles up around a vent  Has steep sides  More explosive  Composite volcanoes  Much larger than ci ...
PPT
PPT

... California ...
10/12/09 Volcanoes and Plate TectonicsCh
10/12/09 Volcanoes and Plate TectonicsCh

... A volcano forms above a hot spot when magma erupts through the crust and reaches the surface. As the plate moves, new _______________________________ will form over the Hot Spot. ...
Ch 12 Vocabulary - Taylor County Schools
Ch 12 Vocabulary - Taylor County Schools

... mountain ranges with a rift valley between them that extends around Earth on the . Formed at a plate boundary. ...
Science Study Guide What is the hot molten rock
Science Study Guide What is the hot molten rock

Earthquakes and Volcanoes
Earthquakes and Volcanoes

... eldest daughter, Kate, elected to attend Indiana University where she is now a freshman. She recounted the following to her mother and me. During Freshman Orientation Week, all departments gathered together in trade show fashion to present their particular curriculums. Students were invited to visit ...
Plate Boundaries
Plate Boundaries

Volcanos - High View School
Volcanos - High View School

... Why do some volcanos erupt with explosions and some don’t? Some volcanos are explosive and others are not. If the magma is thin and runny, the gas can easily escape from it. When this type of magma erupts, the larva just flows out of and down the sides of the volcano. When magma is thicker or has a ...
Volcanoes - Mr. Cramer
Volcanoes - Mr. Cramer

...  Magma - molten mixture of rock, gasses, and water from the mantle  Lava- magma that reaches the surface ...
Ch 10.1 Volcano Notes
Ch 10.1 Volcano Notes

Quiz #2 - University of Hawaii at Hilo
Quiz #2 - University of Hawaii at Hilo

... At or near tectonic plate boundaries There is no preferred location ...
VOLCANOES
VOLCANOES

... 5. The primary source of hazards related to volcanic eruptions are the products of eruptions: lava flows, pyroclastic flows, lahars (volcanic mudflows), ash falls, toxic gases (mainly SO2), and phreatic eruptions. 6. A volcanic eruption can have a global impact on climate and atmospheric chemistry t ...
CHAPTER 5 VOLCANOES Important Concepts 1. Most magmas
CHAPTER 5 VOLCANOES Important Concepts 1. Most magmas

... 5. The primary source of hazards related to volcanic eruptions are the products of eruptions: lava flows, pyroclastic flows, lahars (volcanic mudflows), ash falls, toxic gases (mainly SO2), and phreatic eruptions. 6. A volcanic eruption can have a global impact on climate and atmospheric chemistry t ...
Y10GeUA3_2 Tectnic Nov16_7 PP
Y10GeUA3_2 Tectnic Nov16_7 PP

... in that area are predominantly the most immediate or near the center of the issue, and stable so it does not represent a risk for the populations and economic activities in its area of influence. Variations in the levels of the parameters derived from the monitoring indicating that the volcano is ab ...
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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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