forces of change

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Forces Of Change Chapter 2 Section 2

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Chapter 2 Section 2. Forces Of Change. - PowerPoint PPT Presentation

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Page 1: Forces Of Change

Forces Of Change

Chapter 2 Section 2

Page 2: Forces Of Change

• In 1906 the booming city of San Francisco was destroyed by an earthquake that measured 8.6 on the Richter scale. Over 400 people were killed, and 28,000 buildings were reduced to rubble. Another slightly less forceful earthquake struck the city in 1989, doing far less damage and claiming 67 lives. Most people remember it because it interrupted the World Series for 12 days while damages were repaired in Oakland and San Francisco.

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Earth’s Structure• A Layered Planet The earth is composed of three

layers: the core, the mantle, and the crust.- The inner core is about 4,000 miles (about 6,430

km) below the surface. - The outer core is about 1,400 miles (about 2,250

km) thick. - Both are made of iron and nickel. - The mantle is made of hot, dense rock. - It releases 80 percent of the heat generated from

the earth’s interior.

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Page 5: Forces Of Change

Plate Movement• Many scientists believe that all the

continents once were joined and have broken apart and drifted. This theory is called continental drift.

• Plates move gradually. As they move, they come together and pull apart.

• This movement pushes up mountains, creates volcanoes, and produces earthquakes.

• These activities are called plate tectonics.

2.1 explain internal and external physical forces that impact Earth

Page 6: Forces Of Change

Colliding and Spreading Plates

• One way that mountain ranges form is in a process called subduction, when a sea plate collides with and dives beneath a continental plate.

• Continents grow in a process called accretion, when pieces of the earth’s crust come together slowly as a sea plate slides under a continental plate.

• When two sea plates collide, they may create a chain of islands.

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Page 8: Forces Of Change

Folds and Faults• When plates squeeze the earth’s surface, they

create folds or bends in layers of rock.

Page 9: Forces Of Change

When the layers grind or slide past each other, they create cracks known as faults.

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Earthquakes• Sudden, violent movements along the fault lines are

called earthquakes.

Page 11: Forces Of Change

• The Ring of Fire is a zone of earthquake and volcanic activity surrounding the Pacific Ocean.

• Cities in this area, like San Francisco and Los Angeles, are prone to severe earthquakes.

Page 12: Forces Of Change

Volcanic Eruptions• Volcanoes are mountains formed by

magma that has broken through the earth’s crust.

• Volcanoes often rise along plate boundaries.

• They also occur when especially hot places deep inside the earth blast their magma to the surface.

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Page 14: Forces Of Change

External Forces of Change Weathering

• Physical weathering occurs when large masses of rock are broken down into smaller pieces. Chemical weathering changes the chemical composition of rocks.

Page 15: Forces Of Change

Wind Erosion

• The movement of dust, sand, and soil from one place to another is called wind erosion.

• It can devastate some areas and bring mineral riches to the soil in

other places.

Page 16: Forces Of Change

Glacial Erosion• Glaciers are large bodies of ice that

move slowly across the earth’s surface.• As they move, they carry along rocks

and soil.• Sheet glaciers are flat, broad sheets

of ice. • Mountain glaciers are located in high

mountain valleys.

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Page 18: Forces Of Change

Water Erosion• Rain, rivers, streams, and

oceans wear away soil and rock in a phenomenon called water erosion.

• Water erosion often forms valleys and canyons.

Page 19: Forces Of Change