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200 pt 300 pt 400 pt 500 pt 100 pt 200 pt 300 pt 400 pt 500 pt 100 pt 200pt 300 pt 400 pt 500 pt 100 pt 200 pt 300 pt 400 pt 500 pt 100 pt 200 pt 300 pt 400 pt 500 pt 100 pt Mechanical Weathering Chemical Weathering Rates of Weathering Soil Soil Conservati

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Mechanical Weathering. Chemical Weathering. Rates of Weathering. Soil. Soil Conservation. 100 pt. 100 pt. 100 pt. 100 pt. 100 pt. 200 pt. 200 pt. 200pt. 200 pt. 200 pt. 300 pt. 300 pt. 300 pt. 300 pt. 300 pt. 400 pt. 400 pt. 400 pt. 400 pt. 400 pt. 500 pt. 500 pt. - PowerPoint PPT Presentation

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MechanicalWeathering

ChemicalWeathering

Rates of Weathering

SoilSoil

Conservation

Page 2: 200 pt

Frost action where water seeps into cracks, freezes, and breaks

rock during cold weather

Page 3: 200 pt

Ice Wedging

Page 4: 200 pt

The part of plants that gets into cracks, grows, expands, and

breaks rock

Page 5: 200 pt

Roots

Page 6: 200 pt

The process when rocks and sand rub, scratch, and wear away other

rocks

Page 7: 200 pt

Abrasion

Page 8: 200 pt

Abrasion caused by rocks falling on other rocks

Page 9: 200 pt

Gravity

Page 10: 200 pt

True or False: Mechanical weathering changes the rock’s

composition

Page 11: 200 pt

False

Page 12: 200 pt

True or False: Over time, water can dissolve the minerals of

rocks.

Page 13: 200 pt

True

Page 14: 200 pt

A type of chemical weathering caused by polluted precipitation.

Page 15: 200 pt

Acid Rain

Page 16: 200 pt

These living things produce acids that break down rock over time.

Page 17: 200 pt

Lichens

Page 18: 200 pt

Chemical weathering that occurs when air reacts with iron in rocks

to create rust.

Page 19: 200 pt

Oxidation

Page 20: 200 pt

True or False: Wind abrasion is a form of chemical weathering.

Page 21: 200 pt

False

Page 22: 200 pt

True or False: Water can be both a mechanical & chemical

weathering agent.

Page 23: 200 pt

True

Page 24: 200 pt

The rate (or time it takes) for rocks to weather depends on

climate, elevation, and _______________ (what the rock

is made of).

Page 25: 200 pt

Composition

Page 26: 200 pt

Rocks in __________ climates will weather away faster because

they are exposed to more ice, wind, and precipitation.

Page 27: 200 pt

Colder/cooler/higher

Page 28: 200 pt

_____________ Weathering happens faster in warm, humid

climates

Page 29: 200 pt

Chemical

Page 30: 200 pt

True or False: The less rock that is exposed, the more it will

weather away.

Page 31: 200 pt

False

Page 32: 200 pt

Devil’s Tower (where the softer part of the volcano weathered away but left the harder rock

behind) is an example of __________ weathering.

Page 33: 200 pt

Differential

Page 34: 200 pt

The source (or beginning) of the soil is the __________ rock

Page 35: 200 pt

parent

Page 36: 200 pt

The dark soil found in Horizon A full of nutrients from decaying

plants and animals

Page 37: 200 pt

Humus

Page 38: 200 pt

This is found in Horizon R (bottom layer) and has not been

weathered at all

Page 39: 200 pt

Bedrock

Page 40: 200 pt

___________ occurs in Horizon E when water drains nutrients

down into this layer

Page 41: 200 pt

Leaching

Page 42: 200 pt

This type of soil sediment has the smallest grain size and water will

NOT move through it easily (Sand, Clay, or Silt)

Page 43: 200 pt

Clay

Page 44: 200 pt

True or False: Desert soil is best for growing crops

Page 45: 200 pt

False

Page 46: 200 pt

A conservation technique where old harvested plants are left to

lay on top of the soil

Page 47: 200 pt

No-till farming

Page 48: 200 pt

Planting rows of crops across the slope of a hill to hold create less

soil erosion

Page 49: 200 pt

Contour Plowing

Page 50: 200 pt

Planting crops in different fields each year so that nutrients have

time to be replenished

Page 51: 200 pt

Crop Rotation

Page 52: 200 pt

Why is soil worth protecting?

Page 53: 200 pt

We rely on soil to live!