Volcanic Crisis: The Soufrière Hills Volcano, Montserrat
... in the rock, and even incorporated into minerals which make up the rock. As the plate descends into the hot mantle, this water is forced out, and upward. It invades the wedge of mantle rock between the two plates, causing the rock to melt. The resulting mix of molten rock and pressurized H2O forces ...
... in the rock, and even incorporated into minerals which make up the rock. As the plate descends into the hot mantle, this water is forced out, and upward. It invades the wedge of mantle rock between the two plates, causing the rock to melt. The resulting mix of molten rock and pressurized H2O forces ...
File - Ms. Fergus Science
... Finding the Epicenter: The Tortoise and the HareSeismographs are located all over the world. A seismograph station in Montana can pick up an earthquake occurring in California. If the earthquake is really strong, seismograph stations all over the world can also record this same earthquake. Why? Bec ...
... Finding the Epicenter: The Tortoise and the HareSeismographs are located all over the world. A seismograph station in Montana can pick up an earthquake occurring in California. If the earthquake is really strong, seismograph stations all over the world can also record this same earthquake. Why? Bec ...
Tectonic processes
... or two continental plates. When two oceanic plates move apart, magma rises to the sea floor and creates undersea volcanoes. Because the lava is under pressure from the ocean above and is not rich in dissolved gases, eruptions tend to be of a ■■ Figure 2.4: Constructive plate boundary between constan ...
... or two continental plates. When two oceanic plates move apart, magma rises to the sea floor and creates undersea volcanoes. Because the lava is under pressure from the ocean above and is not rich in dissolved gases, eruptions tend to be of a ■■ Figure 2.4: Constructive plate boundary between constan ...
Earth and Atmoshere Revision
... Explain why Los Angeles is preparing itself for a large earthquake. ...
... Explain why Los Angeles is preparing itself for a large earthquake. ...
tectonic plates.
... East Africa may be the site of the Earth's next major ocean. Plate interactions in the region provide scientists an opportunity to study first hand how the Atlantic may have begun to form about 200 million years ago. Geologists believe that, if spreading continues, the three plates that meet at the ...
... East Africa may be the site of the Earth's next major ocean. Plate interactions in the region provide scientists an opportunity to study first hand how the Atlantic may have begun to form about 200 million years ago. Geologists believe that, if spreading continues, the three plates that meet at the ...
Foundations of Social Studies GEOGRAPHY
... Geologic Hazards Geologic hazards are caused by the movement in the earth's plates. These events happen at or below the surface of the earth, but can have consequences that reach all the way into the highest parts of the atmosphere: Volcanoes occur when molten rock comes to the surface of the eart ...
... Geologic Hazards Geologic hazards are caused by the movement in the earth's plates. These events happen at or below the surface of the earth, but can have consequences that reach all the way into the highest parts of the atmosphere: Volcanoes occur when molten rock comes to the surface of the eart ...
unit cover page - Bremen High School District 228
... cannot observe them but only infer that they take place from other kinds of evidence. Identify the various features of the ocean floor which furnish evidence for plate tectonics: magnetic patterns, age, and topographical features. Identify the properties of rocks and minerals based on the physical a ...
... cannot observe them but only infer that they take place from other kinds of evidence. Identify the various features of the ocean floor which furnish evidence for plate tectonics: magnetic patterns, age, and topographical features. Identify the properties of rocks and minerals based on the physical a ...
Rocks from Lava
... before large crystals have time to form. That’s why extrusive igneous rocks usually have a smooth, sometimes glassy appearance. Extrusive igneous rocks can form in two ways. In one way, volcanoes erupt and shoot out lava and ash. Also, large cracks in Earth’s crust, called fissures, can open up. Whe ...
... before large crystals have time to form. That’s why extrusive igneous rocks usually have a smooth, sometimes glassy appearance. Extrusive igneous rocks can form in two ways. In one way, volcanoes erupt and shoot out lava and ash. Also, large cracks in Earth’s crust, called fissures, can open up. Whe ...
Plate Tectonics PowerPoint
... • The Earth is made up of 4 main layers (inner and outer core, mantle, and crust) • On the surface of the Earth are tectonic plates that slowly move around the globe • Plates are made of crust and upper mantle ...
... • The Earth is made up of 4 main layers (inner and outer core, mantle, and crust) • On the surface of the Earth are tectonic plates that slowly move around the globe • Plates are made of crust and upper mantle ...
Earthquakes and Volcanoes
... shape. They may even break, and the ends of the broken pieces may snap back. This snapping back is called elastic rebound. Rocks usually change shape, or deform, slowly over long periods of time. As they are strained, potential energy builds up in them. This energy is released suddenly by the action ...
... shape. They may even break, and the ends of the broken pieces may snap back. This snapping back is called elastic rebound. Rocks usually change shape, or deform, slowly over long periods of time. As they are strained, potential energy builds up in them. This energy is released suddenly by the action ...
Chapter 12.2 - Features of Plate Tectonics
... smoke and ask everywhere, found along plate boundaries Layers of ash and thick lava (magma outside Earth) form a tall cone. As magma reaches the surface, it cools, hardens and traps gases below. Pressure builds, eventually there is an eruption. 2. Shield volcanoes - these are not found at plat ...
... smoke and ask everywhere, found along plate boundaries Layers of ash and thick lava (magma outside Earth) form a tall cone. As magma reaches the surface, it cools, hardens and traps gases below. Pressure builds, eventually there is an eruption. 2. Shield volcanoes - these are not found at plat ...
Igneous Geology - Earth Science Teachers` Association
... Draw a magnified diagram to show crystal textures in a sample of Shap granite. Phenocrysts are the large crystals which you will find easy to recognise. Use labelling on your diagram to identify each separate mineral. Remember to add a ...
... Draw a magnified diagram to show crystal textures in a sample of Shap granite. Phenocrysts are the large crystals which you will find easy to recognise. Use labelling on your diagram to identify each separate mineral. Remember to add a ...
KCSE ONLINE GEOGRAPHY PP1 MARKING SCHEME SECTION A
... C(i)Weathering is the gradual breakdown and decomposition of rocks insitu(without movement) (2mks) (ii)-Frost action-occurs in areas with freezing temperatures.When the temperature rises ice melts and accumulates in cracks within the rocks.As it freezes water expands and widens the cracks leading t ...
... C(i)Weathering is the gradual breakdown and decomposition of rocks insitu(without movement) (2mks) (ii)-Frost action-occurs in areas with freezing temperatures.When the temperature rises ice melts and accumulates in cracks within the rocks.As it freezes water expands and widens the cracks leading t ...
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.