changes within the earths surface changes within the earths surface

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CHANGES WITHIN THE EARTHS SURFACE

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Page 1: CHANGES WITHIN THE EARTHS SURFACE CHANGES WITHIN THE EARTHS SURFACE

CHANGES WITHIN THE EARTHS

SURFACE

CHANGES WITHIN THE EARTHS

SURFACE

Page 2: CHANGES WITHIN THE EARTHS SURFACE CHANGES WITHIN THE EARTHS SURFACE

The Earth’s LayersThe Earth’s Layers 1. Core - center

Inner - solid/ outer-liquid

2. Mantle thick layer of rock 3. Crust

rocky surface area

1. Core - center Inner - solid/ outer-

liquid 2. Mantle thick layer of rock 3. Crust

rocky surface area

QuickTime™ and aSorenson Video 3 decompressorare needed to see this picture.

QuickTime™ and aSorenson Video 3 decompressorare needed to see this picture.

Page 3: CHANGES WITHIN THE EARTHS SURFACE CHANGES WITHIN THE EARTHS SURFACE

Land, Air and WaterLand, Air and Water Lithosphere --surface material (soil, rock, and other landforms)

Atmosphere -- substances above the surface (air and water)

Biosphere -- plants, animals, and other living things

Continents -- 7 separate Relief -- difference in elevation

Lithosphere --surface material (soil, rock, and other landforms)

Atmosphere -- substances above the surface (air and water)

Biosphere -- plants, animals, and other living things

Continents -- 7 separate Relief -- difference in elevation

Page 4: CHANGES WITHIN THE EARTHS SURFACE CHANGES WITHIN THE EARTHS SURFACE

Plate TectonicsPlate Tectonics

Movement and shifting of the plates

THERE ARE 4 TYPES OF PLATE MOVEMENT

Movement and shifting of the plates

THERE ARE 4 TYPES OF PLATE MOVEMENT

QuickTime™ and aSorenson Video 3 decompressorare needed to see this picture.

QuickTime™ and aSorenson Video 3 decompressorare needed to see this picture.

Page 5: CHANGES WITHIN THE EARTHS SURFACE CHANGES WITHIN THE EARTHS SURFACE

4 Types of Movement4 Types of Movement

Subduction -- heavier plate slides down toward the mantle

Sea - Floor Spreading -- Magma comes from underneath and moves it away

Converging -- collide and create Mt.

Faulting -- plates slip or grind past each other

Subduction -- heavier plate slides down toward the mantle

Sea - Floor Spreading -- Magma comes from underneath and moves it away

Converging -- collide and create Mt.

Faulting -- plates slip or grind past each other

Page 6: CHANGES WITHIN THE EARTHS SURFACE CHANGES WITHIN THE EARTHS SURFACE

Changes on the Surface -

sect. 3

Changes on the Surface -

sect. 3 Weathering - break down at or near the Earth’s surface

1. Mechanical -- rock is actually broken or weakened physically

Example--frost wedging 2. Chemical -- Alters rocks chemical make

up a. Carbonic Acid -- dissolves rock b. Acid rain -- chemicals combine

with water

Weathering - break down at or near the Earth’s surface

1. Mechanical -- rock is actually broken or weakened physically

Example--frost wedging 2. Chemical -- Alters rocks chemical make

up a. Carbonic Acid -- dissolves rock b. Acid rain -- chemicals combine

with water

Page 7: CHANGES WITHIN THE EARTHS SURFACE CHANGES WITHIN THE EARTHS SURFACE

EROSIONEROSION

Movement of weathered materials including gravel, soil, and sand

Agents -- water, wind and glaciers

Movement of weathered materials including gravel, soil, and sand

Agents -- water, wind and glaciers

Page 8: CHANGES WITHIN THE EARTHS SURFACE CHANGES WITHIN THE EARTHS SURFACE

WaterWater

Carries sediment away and this will grind away at the rock

Flood plain -- forms on the sides of rivers

Delta -- flat, low-lying plain formed at the mouth of the river, where the river enters the lake

Carries sediment away and this will grind away at the rock

Flood plain -- forms on the sides of rivers

Delta -- flat, low-lying plain formed at the mouth of the river, where the river enters the lake

Page 9: CHANGES WITHIN THE EARTHS SURFACE CHANGES WITHIN THE EARTHS SURFACE

GlaciersGlaciers

Huge slow moving sheets of ice

4 ice ages Moraines -- piles of rock and debris left by glaciers

Huge slow moving sheets of ice

4 ice ages Moraines -- piles of rock and debris left by glaciers