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What causes earthquakes? What causes volcanoes to form? How do earthquakes and volcanoes change Earth’s surface? Earthquakes and Volcanoes

Lesson 2 Reading Guide - KC

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Earthquakes and Volcanoes. What causes earthquakes? What causes volcanoes to form? How do earthquakes and volcanoes change Earth ’ s surface?. Lesson 2 Reading Guide - KC. Earthquakes and Volcanoes. lava flow volcanic ash caldera. earthquake fault mid-ocean ridge hot spot. - PowerPoint PPT Presentation

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Page 1: Lesson 2 Reading Guide - KC

• What causes earthquakes?• What causes volcanoes to form?• How do earthquakes and volcanoes

change Earth’s surface?

Earthquakes and Volcanoes

Page 2: Lesson 2 Reading Guide - KC

• earthquake• fault• mid-ocean ridge• hot spot

Earthquakes and Volcanoes

• lava flow• volcanic ash• caldera

Page 3: Lesson 2 Reading Guide - KC

• Because tectonic plates move very slowly, most changes to Earth’s surface take a long time.

• But some changes occur very quickly and violently.

• An earthquake is the rupture and sudden movement of rocks along a break or a crack in Earth’s crust.

Earthquakes

Page 4: Lesson 2 Reading Guide - KC

An earthquake can change Earth’s surface quickly and dramatically.

Dr. Roger Hutchinson/NOAA

Page 5: Lesson 2 Reading Guide - KC

• The surface along which the crust moves is called a fault.

• When pieces of crust slide past each other, energy is released, causing the ground to shake.

Earthquakes (cont.)

Photograph by N.J. Silberling, USGS Photo Library, Denver, CO

Page 6: Lesson 2 Reading Guide - KC

• Most earthquakes begin in the lithosphere within about 100 km of Earth’s surface.

• The focus is the area beneath Earth’s surface where rock that is under stress breaks, triggering an earthquake.

• The point on the surface directly above the focus is called the epicenter.

Earthquakes

Page 7: Lesson 2 Reading Guide - KC

• Earthquakes release energy in the form of vibrations or waves.

• Body waves move through the Earth's interior traveling much more quickly than surface waves.

• Surface waves move over Earth's surface.

Earthquakes

Page 8: Lesson 2 Reading Guide - KC

• Primary or P waves are the first energy waves that arrive after an earthquake occurs. They travel through both solids and liquids in a push-pull, linear motion, similar to an earthworm.

• Secondary or S waves are the second energy wave that travels through the interior of Earth. They can only travel through solids in an up and down motion.

Earthquakes-Types of Body Waves

Page 9: Lesson 2 Reading Guide - KC

• Love or L waves: originate at the epicenter of an earthquake and arrive after the secondary waves. They are responsible for the most damage

• Rayleigh waves are a second type of surface wave that arrive at a location distant from the epicenter. They travel in a backwards elliptical motion.

Earthquakes-Types of Surface Waves

Page 10: Lesson 2 Reading Guide - KC

Most earthquakes occur near plate boundaries, though some occur very far from plate boundaries.

Page 11: Lesson 2 Reading Guide - KC

• Earthquakes can create new landforms such as mountains.

• Compression and tension forces produce ridges and mountains as Earth’s crust moves vertically.

Earthquakes (cont.)

Page 12: Lesson 2 Reading Guide - KC

• Liquefaction refers to when extreme shaking causes ground that is made up of loose sediment to behave more like a liquid than a solid.

• Earthquakes can trigger landslides, which bring rocks and soil from the tops of mountains into valleys.

Earthquakes (cont.)

Page 13: Lesson 2 Reading Guide - KC

Earthquakes that happen underwater can cause tsunamis—huge ocean waves created by movement at a fault.

Earthquakes (cont.)

Page 14: Lesson 2 Reading Guide - KC

• Volcanoes are landforms that form when magma erupts onto Earth’s surface as lava.

• Volcanoes can occur at divergent and convergent plate boundaries and at hot spots.

• There are approximately 1,500 active volcanoes on Earth.

Volcanoes

Page 15: Lesson 2 Reading Guide - KC

The mountains that form as lava from a volcano at a divergent boundary builds up and cools are called mid-ocean ridges.

Page 16: Lesson 2 Reading Guide - KC

At some convergent boundaries, one tectonic plate sinks, melts the mantle, and forms magma that erupts onto the plate that does not sink.

Page 17: Lesson 2 Reading Guide - KC

• Hot spots are locations where volcanoes form far from plate boundaries.

• When a hot spot is under oceanic crust, it will form islands such as the Hawaiian Islands.

• When a hotspot is under continental crust, it will form a geyser like Old Faithful at Yellowstone National Park in Wyoming.

Volcanoes (cont.)

Page 18: Lesson 2 Reading Guide - KC

• Because magma is hot, it is also less dense than the rock material around it.

• Rising magma and great pressure caused by dissolved gases eventually erupt through cracks in Earth’s surface, creating a volcano.

Volcanoes (cont.)

Page 19: Lesson 2 Reading Guide - KC

Most of Earth’s largest volcanoes are located at convergent plate boundaries.

Page 20: Lesson 2 Reading Guide - KC

• When melted mantle material erupts, it flows over Earth’s surface, creating long streams of molten rock called lava flows.

• The lava eventually cools and solidifies, forming solid rock.

Volcanoes (cont.)

Royalty-Free/CORBIS

Page 21: Lesson 2 Reading Guide - KC

• At convergent plate boundaries, part of the continental crust can become mixed with magma from the mantle.

• When this mixture of molten materials erupts, it does not flow as easily as lava made only of melted mantle.

• Instead of forming lava flows, it often solidifies in the atmosphere, where it breaks into small pieces of lava called volcanic ash.

Volcanoes (cont.)

Page 22: Lesson 2 Reading Guide - KC

• Eruptions that eject ash high into the atmosphere are called explosive eruptions.

• Lava also can be produced during these eruptions.

Volcanoes (cont.)

Page 23: Lesson 2 Reading Guide - KC

Before a volcano erupts, magma builds up in the crust in a reservoir called a magma chamber.

Page 24: Lesson 2 Reading Guide - KC

• Shield volcanoes form after basaltic lava flows have occurred over time.

• Shield volcanoes tend to be large with gentle slopes, such as Mauna Loa in Hawaii.

J.S. Griggs/U.S. Geological Survey

Page 25: Lesson 2 Reading Guide - KC

• Composite volcanoes form as lava flows and ash layers deposited by explosive eruptions build up.

• Composite volcanoes often have steep sides and a cone shape.

PhotoLink/Getty Images

Page 26: Lesson 2 Reading Guide - KC

Sometimes the surface above the chamber collapses, creating a large depression in the center of the volcano called a caldera.

P.W. Lipman, U.S. Geological Survey

Page 27: Lesson 2 Reading Guide - KC

• Volcanic ash and gases from explosive eruptions can blow high into the atmosphere, blocking sunlight.

• This can cause the temperature of the atmosphere near Earth’s surface to decrease.

P.W. Lipman, U.S. Geological Survey

Page 28: Lesson 2 Reading Guide - KC

• Earthquakes occur when movement along a fault occurs. Earthquakes occur mostly along plate boundaries. They can cause great damage.

• Volcanoes form at two types of plate boundaries. Lava cools and builds up, forming volcanoes and other landforms.

Page 29: Lesson 2 Reading Guide - KC

• Earthquakes and volcanoes change the surface by building mountains, covering land with lava, and shifting the surface along faults.

Page 30: Lesson 2 Reading Guide - KC

27. Which happens when extreme shaking causes sediment to behave more like a liquid than a solid?A. compressionB. eruption C. liquefaction D. tsunami

Page 31: Lesson 2 Reading Guide - KC

A. mid-ocean ridgeB. lava flowC. faultD. caldera

28. Which is a long stream of molten rock which eventually cools, solidifies, and builds up over time as flat layers?

Page 32: Lesson 2 Reading Guide - KC

A. calderaB. compositeC. mid-oceanD. shield

29. Which type of volcano often has steep sides and is cone shaped?

Page 33: Lesson 2 Reading Guide - KC

30. Earthquakes occur and volcanoes erupt only near plate boundaries.

31. Volcanoes erupt melted rock.

Do you agree or disagree?