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Earth`s Interior
Earth`s Interior

... order (oldest to youngest), but without absolute ages. We use a number of principles and laws to do this: • Law of Original Horizontality – Sedimentary units and lava flows are deposited horizontally. • Law of Superposition – the layer below is older ...
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Slide 1

... c. Ba/La (Windows) d. Galapagos ...
SCIENCE TEST1 (VWILLIAMSSCIENCETEST1)
SCIENCE TEST1 (VWILLIAMSSCIENCETEST1)

... C. hot water. D. clay. 17. What causes the MOST erosion on Earth? A. running water B. wind C. chemical action D. glaciers 18. Which one of the following is MOST LIKELY to make a rock break open? A. dew evaporating on the rock B. tree leaves decaying on the rock C. snow melting in a crack in the rock ...
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... (rock fragments) - called cinders – Moderately explosive ...
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VOLCANOES - SchoolRack

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Igneous Rocks Magma • molten rock material consisting of liquid
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... Basaltic, Basic or Mafic • very hot (900-1200°C) • very fluid • low SiO2 (silica) content (~50%) • mafic (magnesium and iron rich) minerals • volatile gases are low • produces “flowing” volcanoes: lava flows Silicic, Felsic, Acidic or Granitic • less than 850°C • highly viscous • high SiO2 content ( ...
Igneous Rocks - Crafton Hills College
Igneous Rocks - Crafton Hills College

... Basaltic, Basic or Mafic • very hot (900-1200°C) • very fluid • low SiO2 (silica) content (~50%) • mafic (magnesium and iron rich) minerals • volatile gases are low • produces “flowing” volcanoes: lava flows Silicic, Felsic, Acidic or Granitic • less than 850°C • highly viscous • high SiO2 content ( ...
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... Volcanoes are found throughout the world. Typically they form where tectonic plates come together. Examples include the volcanoes in the area known as the Pacific Ring of Fire which encircles the Pacific Ocean basin. They also may form where thin spots occur in the earth’s crust such as under Yellow ...
earthquakes and volcanoes - Didattica Orizzonte Scuola
earthquakes and volcanoes - Didattica Orizzonte Scuola

... 6959m. It is located in the Andes Mountains between Chile and Argentina. The mountain was created by the subduction of the Nazca Plate beneath the South American plate during the geologically recent Andean orogeny. It is not an active volcano. ...
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The Restless Earth Unit Study Guide 1. What is the outermost layer

and benefits - of volcanic eruptions
and benefits - of volcanic eruptions

... the incandescent torrent rushing into water, a crater being there formed, surrounded by a heap of black sand. This horse shoe heap was 75 feet high above sea level, and the front of it had broken down on the ocean side, revealing a section of bedded sands over a rock wall beneath... The material was ...
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Lithosphere Part 2

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Mountain Building-Folding and Faulting

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Unit 3 Plate Tectonics Study Guide with answers

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... Mountain ranges and other large scale features of the Earth have puzzled geologists and geophysicists for centuries. The fact that many mountain ranges contain oceanic rocks that formed miles below sea-level, and that land living species seemed to be able to walk across the oceans, as evidenced by t ...
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4. What are two examples of hot spots from the

... continents. More than a hundred hotspots beneath the Earth's crust have been active during the past 10 million years. Most of these are located under plate interiors (for example, the African Plate), but some occur near diverging plate boundaries. Some are concentrated near the mid-oceanic ridge sys ...
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Hot Spot Volcanoes

... These isolated areas of volcanic activity are not associated with plate boundaries These volcanoes are found both on continents and out in the ocean ...


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Chapter 12 Vocabulary and Study Guide Volcanoes 1) acid rain

... and core that forms volcanoes when melted rock is forced upwards and breaks through the crust. Mantle plumes are these areas of hot, upwelling mantle. A hot spot develops above the mantle plume. Hotspots may be far from tectonic plate boundaries. A volcanic hotspot is where lava pushes up from under ...
Geobattleships - Earth Learning Idea
Geobattleships - Earth Learning Idea

... are taken to mark the boundaries of tectonic plates in the Earth’s lithosphere (the lithosphere is the crust plus uppermost mantle). ...
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Deadly quakes help renew the planet

... Indonesia and has studied the archipelago, says historical evidence from earlier tsunamis suggests that the huge waves can distribute rich sediments from river systems across coastal plains, making the soil richer. "It brings fertile soils into the lowlands," he says. "In time, a more fertile jungle ...
Geohazards Name: Period: Date: _____
Geohazards Name: Period: Date: _____

... Essential Question: Where are the common locations of geohazards and how do they occur? Geohazards can be defined as events related to the geological state and processes that may cause loss of lives as well as material and environmental damages. These geohazards arise from global geological processe ...
Earth Systems 3209 - Heritage Collegiate
Earth Systems 3209 - Heritage Collegiate

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Notebook #4 Catastrophic Events Affect Diversity GT
Notebook #4 Catastrophic Events Affect Diversity GT

... * During the Precambrian time volcanic activity was one of the most natural events, but lava flows, ash clouds in the atmosphere, and heat made conditions for life forms extremely difficult. Those simple life forms often did not survive these conditions. ...
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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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