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Chapter 6 Lesson 3.   Earth’s plates bend and break under pressure. Earthquakes p. 246.

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Presentation on theme: "Chapter 6 Lesson 3.   Earth’s plates bend and break under pressure. Earthquakes p. 246."— Presentation transcript:

1 Chapter 6 Lesson 3

2   Earth’s plates bend and break under pressure. Earthquakes p. 246

3 Vocabulary Fault –a break in the Earth’s crust where rocks can slide past each other. Earthquake-The snap and slide of rocks as energy is released in Earth’s crust. Focus-The point inside Earth where an earthquake begins Epicenter-The point on Earth’s surface directly above the focus of an earthquake

4   A fault is the term used when rocks break. A fault is a break in the Earth’s crust where rocks can slide past each other.   Most faults form along plate boundaries but can also form within a plate. Fault

5   The point inside the Earth where the earthquake begins.   It can be near the surface or deep within the Earth. Focus

6   Plates move; pressure builds up.   Rocks bend and stretch. If they snap, they release energy suddenly in the form of an earthquake. Earthquakes p. 246

7   The point on the Earth’s surface directly above the focus of the earthquake Epicenter

8   P waves-Primary waves-  Travel through the interior.  Energy travels away from the focus.  P waves are the fastest waves and are the first to be detected.  They compress and expand the ground. (like an accordion) Earthquake Waves

9   S waves-Secondary waves-  Travel through the interior  These waves travel across the direction that the P waves are moving.  They move up and down and side to side. Earthquake Waves

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12   -Surface waves travel along the Earth’s surface.  Some shake the ground from side to side.  Some roll like ocean waves.  Both of these cause most of the damage done to buildings that is done by an earthquake. Earthquake Waves

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14   Seismographs measure and record motion caused by an earthquake’s energy waves. Measuring Earthquake Strength and Damage p. 250

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16   Seismographs measure and record motion caused by an earthquake’s energy waves.   The time between the arrival of the P and the S waves is recorded. The more time that elapses, the further away is the epicenter. Measuring Earthquake Strength and Damage p. 250

17 Richter Scale

18   1935, Charles Richter developed a scale to measure earthquake strength.   Uses the size of waves recorded on a seismograph to determine how strong an earthquake is.   Scale estimates the amount of energy released by an earthquake.   2.0 is minor   4.0 can be felt but causes little damage.   6.0 or greater can cause major damage. Richter Scale

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20   Measures the distance rock along the fault moves. This is used to determine the energy released.   Numbers are similar to the Richter scale but is believed to be more accurate.   Measures earthquake strength. Moment Magnitude Scale

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22   Measures damage caused.   Uses Roman numerals.   XII means buildings were completely destroyed. Mercalli Intensity Scale

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24   When an earthquake happens under the ocean the sea floor will rise and fall.   The movement of water can cause a giant wall of water (May be more than 30m.)   May cause massive damage to buildings near shore. Tsunami

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29 Volcanoes

30  Some mountains are formed when rocks at convergent boundaries are deformed and lifted.

31 Volcanoes  Some mountains are volcanoes and are formed when molten rock, or magma is pushed to the surface and builds up.

32 Volcanoes  Most volcanoes are along the boundaries of plates.

33 Volcanoes  Some form along divergent boundaries where plates are pulling apart and magma rises to the surface.

34 Volcanoes  Some form along convergent boundaries where oceanic crust is pushed down.

35 3 Types of Volcanoes  Shield  Cinder Cone  Composite

36 Shield Volcano

37  Formed by NON-EXPLOSIVE eruptions  Layer after layer builds up slowly.  Broad, slightly dome shaped  May erupt many times

38 Shield Volcano

39 Cinder Cone Volcano  Formed by EXPOLSIVE eruptions, composed of ash and rock thrown out of vent  Erode quickly  Steep sides  Erupt for a short period of time.  Few are taller than 300m or 1000 ft.

40 Cinder Cone Volcano

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42 Composite Volcanoes  Formed by a mixture of explosive and non explosive eruptions  May erupt off and on for many years.

43 Compostie Volcano

44 Composite Volcano \

45 Hawaiian Volcanoes

46  These volcanoes are NOT formed at plate boundaries.

47 Hawaiian Volcanoes  Sometimes magma occurs at another area of a plate, called a hot spot.

48 Hawaiian Volcanoes The magma pushes up, and if it erupts above the surface, it can form a volcano.

49 Hawaiian Volcanoes  As the plates move over the hot spot, the volcano that was formed stops erupting and a series of new volcanoes may form.

50 Hawaiian Volcanoes  If the hot spot lies under the oceanic crust, the series of volcanoes may become a chain of islands.

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52 Hawaiian Volcanoes  The youngest island, Hawai’i, has three active volcanoes.  They have been constantly erupting since 1983.

53 Hawai’iOahu Kauai

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