weathering and erosion. mechanical weathering chemical weathering

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Weathering and Erosion

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Page 1: Weathering and Erosion. Mechanical Weathering Chemical Weathering

Weathering and Erosion

Page 2: Weathering and Erosion. Mechanical Weathering Chemical Weathering

Mechanical WeatheringChemical Weathering

Page 3: Weathering and Erosion. Mechanical Weathering Chemical Weathering

Examine the illustration below that shows volcanic mountain formation. Note that the volcanoes bring new

rock to the surface.

Page 4: Weathering and Erosion. Mechanical Weathering Chemical Weathering

Weathering

• Mechanical or chemical weathering is a surface process that breaks rocks into smaller pieces.

• Freezing• Thawing• Oxygen in the air• Plants• Animals• Weather

Page 5: Weathering and Erosion. Mechanical Weathering Chemical Weathering

Mechanical Weathering

• Breaks rocks into smaller pieces without changing them chemically.

• The small pieces are identical in composition to the original rock.

• Ice wedging • Living beings

Page 6: Weathering and Erosion. Mechanical Weathering Chemical Weathering

Ice Wedging

• The freezing and thawing cycle breaks up rocks.

• Ice wedging occurs when water seeps into rock cracks and freezes. Interestingly, water EXPANDS when it freezes. As the water freezes in the rock crack, sections of rock are broken off. Ice wedging is common in areas where the climate includes a cold season.

Page 7: Weathering and Erosion. Mechanical Weathering Chemical Weathering

Ice WedgingNote how the water can freeze and expand in rock

cracks.

Page 8: Weathering and Erosion. Mechanical Weathering Chemical Weathering

Plants and animals

• Plants grow in inconvenient places. Their roots grow into cracks in rocks where water collects.

• Roots become thicker and longer exerting pressure and wedging rock apart.

Page 9: Weathering and Erosion. Mechanical Weathering Chemical Weathering

Note that the roots are creating large cracks in the rock.

Page 10: Weathering and Erosion. Mechanical Weathering Chemical Weathering

Plants and animals

• Gophers and prairie dogs weather rock, burrowing in the ground.

• When they burrow through sediment, they break the rocks.

Page 11: Weathering and Erosion. Mechanical Weathering Chemical Weathering

Prairie dogs burrowing into the soil. Note the small rocks that are now exposed

Page 12: Weathering and Erosion. Mechanical Weathering Chemical Weathering

Interest Scientific Fact:

• Earthworms are a major factor in the weathering of rock. Earthworms tunnel through the soil looking for food. As they tunnel, they bring rock flakes to the surface and expose covered rock to the weathering effects of air and water.

Page 13: Weathering and Erosion. Mechanical Weathering Chemical Weathering

Earthworms

Page 14: Weathering and Erosion. Mechanical Weathering Chemical Weathering

Abrasion

• Abrasion is the grinding of rocks. Abrasion may occur because of the action of wind, running water, waves, and gravity.

• Wind, running water, and waves push smaller particles of rock into other rock eventually causing pieces to chip away. Rocks fall and tumble as gravity pulls them down hill. When this happens, the rocks chip or break apart.

Page 15: Weathering and Erosion. Mechanical Weathering Chemical Weathering

Note how the wind has weathered the rock.

Page 16: Weathering and Erosion. Mechanical Weathering Chemical Weathering

Remember this:

Rocks are weathered when small pieces of rock are pushed across other rock or when a rock falls.

Page 17: Weathering and Erosion. Mechanical Weathering Chemical Weathering

Abrasion

Page 18: Weathering and Erosion. Mechanical Weathering Chemical Weathering

Abrasion

Abrasion occurs when small pieces of rocks are pushed into or across another rock. Over time this results in chipping or wearing down of the rocks. Rocks are weathered when small pieces of rock are pushed across other rock or when a rock falls.

Page 19: Weathering and Erosion. Mechanical Weathering Chemical Weathering

Abrasion

Page 20: Weathering and Erosion. Mechanical Weathering Chemical Weathering

Interesting Scientific Fact:

The Grand Canyon continues to be weathered by the action of the small grains of rock that are carried along by the Colorado River.

Page 21: Weathering and Erosion. Mechanical Weathering Chemical Weathering

Review 1

• Describe how rocks are mechanically weathering.

• Explain how carbonic acid weathers rocks.

• Describe how soil forms. What factors are important.

Page 22: Weathering and Erosion. Mechanical Weathering Chemical Weathering

Agents of Erosion

• Erosion is the wearing away and removal of rock and sediment.

• Agents:• Gravity• Ice• Wind• water

Page 23: Weathering and Erosion. Mechanical Weathering Chemical Weathering

Gravity

• Gravity is a force that pulls every object toward every other object.

• Gravity pulls everything on Earth toward its center.

• Mass movement is when gravity causes rock or sediment to move down a slope.

Page 24: Weathering and Erosion. Mechanical Weathering Chemical Weathering

Mass Movement

• Creep process in which sediments move slowly downhill.

• Common where freezing and thawing occur.

Page 25: Weathering and Erosion. Mechanical Weathering Chemical Weathering

Creep

Page 26: Weathering and Erosion. Mechanical Weathering Chemical Weathering

Mass Movement

• Slump occurs when a mass of rock or sediment moves downhill, leaving a curve scar.

Page 27: Weathering and Erosion. Mechanical Weathering Chemical Weathering

Slump

Page 28: Weathering and Erosion. Mechanical Weathering Chemical Weathering

SLUMPS

• Slumps are: • often clay-rich (cohesive unit) • slow to rapid • have spoon-shaped failure surfaces • show clear scarp face at head (top) • end in earthflows at toe (bottom)

Page 29: Weathering and Erosion. Mechanical Weathering Chemical Weathering

Slump

Page 30: Weathering and Erosion. Mechanical Weathering Chemical Weathering

Slump

Page 31: Weathering and Erosion. Mechanical Weathering Chemical Weathering

Mass Movement

• Rock Slides layers of rock break loose from slopes and slide to the bottom.

• Million of cubic meters of rock roaring down a mountain at speeds greater than 250 Km/h.

Page 32: Weathering and Erosion. Mechanical Weathering Chemical Weathering

Rock Slides

Page 33: Weathering and Erosion. Mechanical Weathering Chemical Weathering

Mass Movement

• Mudflows where heavy rains or melting snow and ice saturate sediments.

• Mudflows is a mass of wet sediment that flows downhill over the ground surface.

Page 34: Weathering and Erosion. Mechanical Weathering Chemical Weathering

Mudflows

Page 35: Weathering and Erosion. Mechanical Weathering Chemical Weathering

Mudflows

Page 36: Weathering and Erosion. Mechanical Weathering Chemical Weathering

Mudflows

Page 37: Weathering and Erosion. Mechanical Weathering Chemical Weathering

Ice

• Continental glaciers.• Valley glaciers.• Mountain glaciers.

• Ice can remove rock from mountaintops.• Ice forms cirques.• Ice can remove rock layers from land’s

surface.

Page 38: Weathering and Erosion. Mechanical Weathering Chemical Weathering

Ice

Page 39: Weathering and Erosion. Mechanical Weathering Chemical Weathering

Wind

• The erosion of the land by wind is called deflation.

• Deflation can lower the land’s surface by several meters.

• Abrasion is a form of erosion that can make pits in rocks and produce smooth, polished surfaces. ( deserts, cold regions with strong winds).

Page 40: Weathering and Erosion. Mechanical Weathering Chemical Weathering

Wind

Page 41: Weathering and Erosion. Mechanical Weathering Chemical Weathering

Water

• Water that flows over Earth’s surface is called runoff.

• Runoff causes erosion, especially if water is moving fast.

• Sheet erosion is a thin sheet of water can carry loose sediment grains with it, causing erosion of the land.

Page 42: Weathering and Erosion. Mechanical Weathering Chemical Weathering

Water

Page 43: Weathering and Erosion. Mechanical Weathering Chemical Weathering

Water