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Volcanos and Plate Tectonics Chapter 7.1. Introduction 1.Introduction a.While scientists cannot directly measure earth’s interior temperatures, they can.

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Presentation on theme: "Volcanos and Plate Tectonics Chapter 7.1. Introduction 1.Introduction a.While scientists cannot directly measure earth’s interior temperatures, they can."— Presentation transcript:

1 Volcanos and Plate Tectonics Chapter 7.1

2 Introduction 1.Introduction a.While scientists cannot directly measure earth’s interior temperatures, they can estimate them using seismic wave analysis, heat flow near the surface of the earth, and computer modeling.

3 Introduction b.Most of the rocks in the lower part of the mantel are kept below their melting point due to the temperature and pressure in that zone. i.Due to this high pressure, most of the rock in the asthenosphere is also kept solid.

4 Introduction ii.However, sometimes this rock will melt and form magma. 1.Magma is liquid rock produced inside of the earth, and is formed when mantle material flows to areas of lower pressure faster than it can lower its temperature by heat flow, or when liquids such as water are added to the mantle material.

5 Volcanism 2.Volcanism a.Volcanism is any activity that results in the movement of magma toward or onto the earth’s surface.

6 Volcanism b.When rock melts in the earth, pockets of magma are formed and continue to melt rock around it. As this rock melts, it also expands and becomes less dense which causes it to move through the more dense crustal rock toward the surface of the earth.

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8 Volcanism c.Most magma forms at plate boundaries, usually oceanic – continental. i.When the mantle material subducts, it allows water to come in contact with the asthenosphere which causes the rock to melt.

9 Volcanism d.Lava is magma that breaks through to the earth’s surface. i.A vent is the opening through which the molten rock flows. ii.A volcano is the structure formed by the vent and the volcanic material that builds up on the earth’s surface around the vent.

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11 Major Volcanic Zones 1.Major Volcanic Zones a.Most active volcanos and earthquakes occur in zones near both convergent and divergent boundaries of the lithospheric plates. b.One of the three major earthquake zones is the Pacific Ring of Fire.

12 Major Volcanic Zones i.This zone includes areas in North America, South America, Asia, and the islands of the western Pacific Ocean. ii.This increased volcanic and earthquake activity is caused by subducting plates encircling the Pacific Ocean.

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14 Major Volcanic Zones iii.Many island arcs are also formed in this area. 1.Island arcs are formed by magma breaking through the earth’s surface and cooling to form solid rock. As this is occurring, the plate continues to move and create a new volcanic island and island arcs.

15 Major Volcanic Zones 4.A mid-ocean ridge is a place where a large amount of magma surfaces due to plate moving apart from each other. The surfacing magma hardens and forms new lithosphere and underwater volcanos.

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17 Major Volcanic Zones a.Iceland is an example of the Mid-Atlantic Ridge that is above sea-level. i.One half of Iceland is on the North American plate and is moving westward while the other half is on the Eurasian plate and is moving Eastward. ii.The middle of Iceland is cut by large fissures. 1.Fissures are cracks through which lava flows.

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19 Major Volcanic Zones 1.Hot spots are areas of volcanism within the lithospheric plate a.Hot spots occur where magma makes its way to the earth’s surface within the interiors of lithospheric plates. b.At a hot spot, the lithospheric plate continues to move while the hot spot stays in place. Hot spots create volcanic chains of islands such as the Hawaiian Islands.

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