Chapter 5 Lesson 2 The Moving Crust

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Presentation transcript:

Chapter 5 Lesson 2 The Moving Crust Pgs. 110-117

The large sections that make up Earth’s crust and upper mantle are called tectonic plates.

When plates slowly ram into each other, they can form bended rock layers, called folds. Folded Mountains

A long, narrow crack in Earth’s crust is called a fault.

Tall landforms caused by folding or faulting are called mountains.

If the rock in Earth’s crust suddenly shakes, an earthquake occurs.

Underwater earthquakes can cause huge ocean waves, called tsunamis.

The source of an earthquake creates seismic waves that travel outward.

A tool that graphs seismic waves as wavy lines is called a seismograph.

The magnitude of an earthquake is how strong the earthquake is **The magnitude of an earthquake is how strong the earthquake is. The Richter Scale is how the magnitude of earthquakes are rated.

Seismic waves travel at different speeds along Earth’s surface and through Earth’s interior.

A mountain that forms around an opening in Earth’s crust is a volcano.

Most volcanoes form near plate edges.

A volcano is produced by melted rock, called magma, which erupts onto the surface as lava.

Some volcanoes form over thin places in Earth’s crust, called hot spots.

In the Pacific Ocean, an example of volcanoes that formed over a hot spot is the Hawaiian Islands.

**A volcanic eruption can send out melted rock (lava), gases, ash, or rocks into the air.

There are small earthquakes in Hawaii, but not real strong ones because strong earthquakes occur near plate boundaries.