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... 3. What is the name of the ocean floor where two tectonic plates are moving apart? Ridge or a chain of volcanoes. 4. How did the continents move into their current location? This is due to the movement of the tectonic plates. The magma in the mantle moves the plates, which in turn moves the continen ...
... 3. What is the name of the ocean floor where two tectonic plates are moving apart? Ridge or a chain of volcanoes. 4. How did the continents move into their current location? This is due to the movement of the tectonic plates. The magma in the mantle moves the plates, which in turn moves the continen ...
Where Volcanoes Are Located - CK
... Why does melting occur at convergent plate boundaries? The subducting plate heats up as it sinks into the mantle. Also, water is mixed in with the sediments lying on top of the subducting plate. This water lowers the melting point of the mantle material, which increases melting. Volcanoes at converg ...
... Why does melting occur at convergent plate boundaries? The subducting plate heats up as it sinks into the mantle. Also, water is mixed in with the sediments lying on top of the subducting plate. This water lowers the melting point of the mantle material, which increases melting. Volcanoes at converg ...
Seafloor Spreading
... Plate tectonics is a theory that the Earth’s Crust is broken into sections (plates) that move around the Asthenosphere. The Lithosphere is made up of the crust and part of the upper mantle. Plates can move together as Convergent Boundaries. Convection Currents are the energy in the mantle that force ...
... Plate tectonics is a theory that the Earth’s Crust is broken into sections (plates) that move around the Asthenosphere. The Lithosphere is made up of the crust and part of the upper mantle. Plates can move together as Convergent Boundaries. Convection Currents are the energy in the mantle that force ...
Programme title: Awesome Forces video conference
... Investigate natural forces at work around the planet. The BBC science website is an excellent starting point for images, information, and film clips on the Earth’s surface and interior, as well as historical tectonic and volcanic events. Explore in particular the ‘Surface & interior’ topic. bbc.co.u ...
... Investigate natural forces at work around the planet. The BBC science website is an excellent starting point for images, information, and film clips on the Earth’s surface and interior, as well as historical tectonic and volcanic events. Explore in particular the ‘Surface & interior’ topic. bbc.co.u ...
Rapid Changes in Earth`s Surface
... many ways. Flowing lava and ejections of cinder, pumice, and ash build up to create volcanic mountains. A powerful eruption can destroy trees many kilometers away as hot gases and ash flow from the volcano. Ash can be sent high into Earth’s atmosphere. The ash from a volcanic eruption forms very fer ...
... many ways. Flowing lava and ejections of cinder, pumice, and ash build up to create volcanic mountains. A powerful eruption can destroy trees many kilometers away as hot gases and ash flow from the volcano. Ash can be sent high into Earth’s atmosphere. The ash from a volcanic eruption forms very fer ...
Carbon Dioxide & Lake Nios
... CO2 it becomes deadly because it displaces the Oxygen that we need for respiration. •Lake Nios, Cameroon, is a very deep lake within a volcanic crater. •The lake is so deep that hydrostatic pressure forces CO2 to remain at the lake bottom. •When the pressure of the CO2 exceeds a certain limit the ga ...
... CO2 it becomes deadly because it displaces the Oxygen that we need for respiration. •Lake Nios, Cameroon, is a very deep lake within a volcanic crater. •The lake is so deep that hydrostatic pressure forces CO2 to remain at the lake bottom. •When the pressure of the CO2 exceeds a certain limit the ga ...
The Restless Earth - Heathcote School & Science College
... Tectonic plate margin where rising magma adds plate boundary new material to the diverging plates. Destructive Tectonic plate margins where oceanic plate is plate boundary subducted. Convection currents ...
... Tectonic plate margin where rising magma adds plate boundary new material to the diverging plates. Destructive Tectonic plate margins where oceanic plate is plate boundary subducted. Convection currents ...
Lecture11_volcanic_landforms
... high gas content. Like soda, the gas is dissolved within the magma when the magma is under pressure. Gas bubbles and froth on surface of the lava, similar to bubbles on top of soda. Obsidian flow, Long Valley Caldera, California, was created by crustal collapse associated with an explosive eruption ...
... high gas content. Like soda, the gas is dissolved within the magma when the magma is under pressure. Gas bubbles and froth on surface of the lava, similar to bubbles on top of soda. Obsidian flow, Long Valley Caldera, California, was created by crustal collapse associated with an explosive eruption ...
Deep magma feeding system of Fuji volcano, Japan
... strong upwelling flow in the mantle and its connection to the voluminous lower crustal magma chamber. The velocity perturbations in the upper mantle and lower crust beneath Fuji volcano are much greater than other volcanoes in Izu arc (e.g., Hakone, Izu Oshima) and those in North Japan arc (e.g., Az ...
... strong upwelling flow in the mantle and its connection to the voluminous lower crustal magma chamber. The velocity perturbations in the upper mantle and lower crust beneath Fuji volcano are much greater than other volcanoes in Izu arc (e.g., Hakone, Izu Oshima) and those in North Japan arc (e.g., Az ...
Volcanoes
... along mid-ocean ridges where the two plates are pulling apart – Ex: Volcanoes along the Great Rift Valley in Africa ...
... along mid-ocean ridges where the two plates are pulling apart – Ex: Volcanoes along the Great Rift Valley in Africa ...
Volcanoes
... two oceanic plates converge • Ex: Japan, New Zealand, Caribbean Islands, Philippines ...
... two oceanic plates converge • Ex: Japan, New Zealand, Caribbean Islands, Philippines ...
Plate Tectonics and Volcanoes
... Background Information for the Teacher Most volcanoes occur along diverging plate boundaries, such as the mid-ocean ridge, or in subduction zones around the edges of oceans. Exceptions to this pattern are volcanoes that form at “hot spots”. Volcanoes at Diverging Plate Boundaries – form along the mi ...
... Background Information for the Teacher Most volcanoes occur along diverging plate boundaries, such as the mid-ocean ridge, or in subduction zones around the edges of oceans. Exceptions to this pattern are volcanoes that form at “hot spots”. Volcanoes at Diverging Plate Boundaries – form along the mi ...
Quiz Four (2:00 to 2:05 PM) - University of South Alabama
... explosion (exciting). When filled with water they are called crater lakes. ...
... explosion (exciting). When filled with water they are called crater lakes. ...
UNIT 2 Metamorphism and tectonic plates: Metamorphism is a
... the continental plate is built up from the sediments in an accretionary prism and magma from volcanic arcs. This produces an orogen on the continent. (Ex. Andes). Eventually, the continental plate will reach the trench and join the oceanic plate. Volcanoes created by this process have very acidic an ...
... the continental plate is built up from the sediments in an accretionary prism and magma from volcanic arcs. This produces an orogen on the continent. (Ex. Andes). Eventually, the continental plate will reach the trench and join the oceanic plate. Volcanoes created by this process have very acidic an ...
volcanoes
... VOLCANO - Weak spot in the crust where magma has come to surface. MAGMA CHAMBER - Pocket beneath a volcano where Magma Collects. [MC] HOT SPOT - Area where magma from deep in the mantle MELTS through crust above it. EXTINCT - A volcano that is UNLIKELY to erupt again. ISLAND ARC - String of ISLANDS ...
... VOLCANO - Weak spot in the crust where magma has come to surface. MAGMA CHAMBER - Pocket beneath a volcano where Magma Collects. [MC] HOT SPOT - Area where magma from deep in the mantle MELTS through crust above it. EXTINCT - A volcano that is UNLIKELY to erupt again. ISLAND ARC - String of ISLANDS ...
Geology Final Exam Review 1st Semester What drives Earth`s rock
... 2. What are the textures of igneous rocks? a. Describe what causes the different textures. 3. Tell the differences between gabbro and granite. 4. List the 3 main compositional types of igneous rocks. a. Describe the mineral differences for each type. 5. List the 3 main types of volcanoes. a. Describ ...
... 2. What are the textures of igneous rocks? a. Describe what causes the different textures. 3. Tell the differences between gabbro and granite. 4. List the 3 main compositional types of igneous rocks. a. Describe the mineral differences for each type. 5. List the 3 main types of volcanoes. a. Describ ...
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.