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Plate Boundaries Chart/Notes
Plate Boundaries Chart/Notes

CONVERGENT BOUNDARIES
CONVERGENT BOUNDARIES

... creating new ocean floor Continental Rifting The process that causes continental crust to extend and thin. Rift Valley deep valley formed on land where two plates move apart and magma rises to Earth's surface ...
Pre-visit Lesson: Grades 3-5 - Washington State Parks and
Pre-visit Lesson: Grades 3-5 - Washington State Parks and

... forming mountains. This theory can be shown through a simple demonstration. Using a few colors of play dough or craft foam you can demonstrate the various movements of tectonic plates and the layering of the earth. While introducing the idea that earth’s crust is made up of many separate plates all ...
Period 8 Volcanism
Period 8 Volcanism

...  (Note: this is also true of water - its structure is much like ice, with many ...
Earthquakes, Volcanoes, Tsunamis
Earthquakes, Volcanoes, Tsunamis

... o How can the public can prepare for earthquakes and volcanoes? Unfortunately for you and your research team, the President would like for you to write a report with answers to these questions by the end of four weeks, or he will cut all of your funding! You have your laptop, cellular phone and mode ...
World Geography - San Diego Unified School District
World Geography - San Diego Unified School District

...  The ring of fire  Volcanoes  Plate boundaries are where tectonic plates collide and separate past each other  Magma to travel upward through the crust  The ring of fire contains nearly 75 % of the worlds active land volcanoes http://my.hrw.com/sh2/sh07_10/student/tabpages/hq7c/c13/s01/vc06/hq7 ...
Oceanic Crust - River Dell Regional School District
Oceanic Crust - River Dell Regional School District

... • E.g. The Andes ...
Plate Tectonics Virtual Lab
Plate Tectonics Virtual Lab

... Question 1: Is there a relationship between the locations of earthquake epicenters, volcanoes, and plate boundaries? If so, describe the relationship. Earthquakes occur along fault lines, which are all the types of plate boundaries. Volcanoes are located along converging plate boundaries and divergi ...
Hot Rocks and Oil: Are Volcanic Margins the New Frontier?
Hot Rocks and Oil: Are Volcanic Margins the New Frontier?

... ISSUES WITH VOLCANIC ROCKS AND EXPLORATION In order to get an oil or gas prospect one needs what is known as the ‘5 steps to heaven’. 1. Reservoir – the rock mass that has void space to host the hydrocarbon. 2. Seal – a rock that is impermeable to the migration of hydrocarbons. 3. Trap – a structur ...
Geography and Society – First Discussions
Geography and Society – First Discussions

... o Summarize the major points of the Theory of Plate Tectonics. o Explain how data collected on the magnetism, depth, and the age of oceanic crust support the Theory of Plate Tectonics. o Explain how the distribution of earthquakes, volcanoes, and the Hawaiian Island chain relate to plate tectonics. ...
No Slide Title
No Slide Title

... • When the top of a mantle plume reaches the base of the lithosphere, the mantle rock spreads out and “pools” under the lithosphere. • Because pressure on the rock is low at this shallow depth, the rock melts. • Large volumes of magma are released onto the ocean floor. ...
Full Text
Full Text

... throw as the volcano is approached is caused by an interaction of the regional stress field with that set up by the volcano mass. For faults to be reoriented there must be a ductile layer below the volcano (hot crust at mid -ocean ridge, weak sedimentary strata, etc.), Increased volcano mass and siz ...
volcano - cloudfront.net
volcano - cloudfront.net

... • When the top of a mantle plume reaches the base of the lithosphere, the mantle rock spreads out and “pools” under the lithosphere. • Because pressure on the rock is low at this shallow depth, the rock melts. • Large volumes of magma are released onto the ocean floor. ...
deep structure of kamchatka northern volcanic group
deep structure of kamchatka northern volcanic group

... seismic sounding data). The center of mantle low velocity anomaly is located near the latitude of Tolbachinskyi cones. Its lower boundary corresponds to 130km to 140km depth with a P-wave velocity reduction of 4% to 5%. Presumably this anomaly corresponds to a mantle magma source, though no asthenos ...
Mount Etna`s
Mount Etna`s

... 530 active volcanoes of the world are divided into three major types according to their positions on or between these plates. The first and most numerous type is found along the rift zones, where two plates are moving apart. The best examples are the long midocean ridges. Forces beneath the plates r ...
Sigmundsson pages
Sigmundsson pages

... when two of these plates diverge. Divergent plate movements cause a buildup of tensional stress that is released in a process known as rifting. This consists of periods of large-scale faulting (the slippage of adjacent rock masses at fractures in Earth’s crust) and/or volcanic and magmatic activity. ...
Subsurface structure of the “petit
Subsurface structure of the “petit

You Will Discover
You Will Discover

... In physical weathering, only the size of rocks is changed. Large rocks are broken into smaller pieces of the same kind of rock. Water is one cause of physical weathering. Water flowing in rivers and streams and in ocean waves carries particles of rock, soil, and sand. The particles scrape against ea ...
plate tectonic study guide
plate tectonic study guide

... The old oceanic crust then goes to the asthenosphere where it melts and recycles back to the mid-ocean ridge. 22. Where do most faults occur? (at transform boundary- earthquakes) - a fault is a break in the Earth’s crust mainly occurs at transform boundaries -a lot of earthquakes happen at fault lin ...
Geology study cards
Geology study cards

Chapter 21.2 PPT - Madison County Schools
Chapter 21.2 PPT - Madison County Schools

... • focus: the location within Earth along a fault at which the first motion of an earthquake occurs • epicenter: the point on Earth’s surface directly above ...
66KB - NZQA
66KB - NZQA

... magma (fire fountain). The magma cools quickly in the air forming Scoria, which contains vesicles due to the trapped gases. The scoria builds up to form steep sided cones Both volcanoes are formed by hot spots where magma from the mantle rises towards the surface and forces its way through the overl ...
131KB - NZQA
131KB - NZQA

... magma (fire fountain). The magma cools quickly in the air forming Scoria, which contains vesicles due to the trapped gases. The scoria builds up to form steep sided cones Both volcanoes are formed by hot spots where magma from the mantle rises towards the surface and forces its way through the overl ...
Figure 8-21 Distribution of Lava Flow for the Model
Figure 8-21 Distribution of Lava Flow for the Model

... (2) The hazard map includes five phenomena: lava flow, tephra fall, volcanic bomb; pyroclastic flow and lahar; (3) Among the five types, ash fall has larger impact areas; therefore, the scale of background map is different from other four types. (4) The target users are the staff in the Civil Defens ...
Assessment 3.2 – Plate Tectonics
Assessment 3.2 – Plate Tectonics

... or directly away from each other but rather two tectonic plates grind past each other in a horizontal direction is what type of plate boundary? a. Convergent b. Divergent c. Transform d. Reform 4. What geological feature can be created by a divergent boundary? a. Mountain Chains b. Volcanoes c. Eart ...
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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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