the solid earth. earth’s structure core mantle crust

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The Solid Earth

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Page 1: The Solid Earth. Earth’s Structure Core Mantle Crust

The Solid Earth

Page 2: The Solid Earth. Earth’s Structure Core Mantle Crust

Earth’s Structure

• Core

• Mantle

• Crust

Page 3: The Solid Earth. Earth’s Structure Core Mantle Crust

Earth’s Structure

Page 4: The Solid Earth. Earth’s Structure Core Mantle Crust

Earth’s Structure

Page 5: The Solid Earth. Earth’s Structure Core Mantle Crust

Core

• Innermost portion of the earth

• Inner core is VERY hot, but solid

• Outer core is liquid molten material

Page 6: The Solid Earth. Earth’s Structure Core Mantle Crust

Mantle

• Surrounds the core

• Most is solid rock, but under the outermost part is a zone of hot, partly melted rock that flows like soft plastic called the asthenosphere

Page 7: The Solid Earth. Earth’s Structure Core Mantle Crust

Crust

• Outermost and thinnest layer

• Continental crust-under continents

• Oceanic crust-under the oceans (71% of the crust)

Page 8: The Solid Earth. Earth’s Structure Core Mantle Crust

Internal Earth Processes

• 2 kinds of movement of the earth– Convection cells: large volumes of heated

rock that move following a pattern similar to the atmosphere (warmer is less dense)

– Mantle plumes: mantle rock flows slowly upward, reaching the surface and spreading out (oceanic ridge)

Page 9: The Solid Earth. Earth’s Structure Core Mantle Crust

Convection Currents

Page 10: The Solid Earth. Earth’s Structure Core Mantle Crust

Mantle Plume

Page 11: The Solid Earth. Earth’s Structure Core Mantle Crust

Plate Tectonics

• Tectonic plates (~60miles thick) consist of continental and oceanic crust and rigid outermost part of the mantle-called the lithosphere

• Plates move constantly supported by the flowing asthenosphere

• Produces mountains, oceanic ridges, trenches, etc.

Page 12: The Solid Earth. Earth’s Structure Core Mantle Crust

Plate Movment

Page 13: The Solid Earth. Earth’s Structure Core Mantle Crust

Plate Tectonics

Page 14: The Solid Earth. Earth’s Structure Core Mantle Crust

3 Types of Plate Boundaries

• Divergent plate boundary: plates move apart from each other

• Convergent plate boundary: plates moving toward each other (earthquakes)

• Transform Fault: plates slide past each other

Page 15: The Solid Earth. Earth’s Structure Core Mantle Crust

Divergent Plate Boundary

Page 16: The Solid Earth. Earth’s Structure Core Mantle Crust

Convergent Plate Boundary

Page 17: The Solid Earth. Earth’s Structure Core Mantle Crust

Transform Fault

• http://www.youtube.com/watch?v=QDqskltCixA

Page 18: The Solid Earth. Earth’s Structure Core Mantle Crust

External Earth Processes

• Geologic changes based directly or indirectly on energy from the sun and gravity– Erosion– Weathering

Page 19: The Solid Earth. Earth’s Structure Core Mantle Crust

Erosion

Page 20: The Solid Earth. Earth’s Structure Core Mantle Crust

Erosion

• Material is dissolved, loosened, or worn away from one part of the earth’s surface and deposited in other places– Streams– Wind– Human activities that accelerate erosion (acid

rain)

Page 21: The Solid Earth. Earth’s Structure Core Mantle Crust

Weathering

• Produces loosened materials that can be eroded

• Two types– Mechanical (frost)– chemical

Page 22: The Solid Earth. Earth’s Structure Core Mantle Crust

Minerals

• An element or inorganic compound that occurs naturally (solid)– Can be an element (gold)– Can be a combination of elements (salt,

quartz)

Page 23: The Solid Earth. Earth’s Structure Core Mantle Crust

Rocks

• Material that makes up a large, natural continuous part of the crust– Most consist of 2 or more minerals

Page 24: The Solid Earth. Earth’s Structure Core Mantle Crust

Three main Rock Types

• Igneous

• Sedimentary

• Metamorphic

Page 25: The Solid Earth. Earth’s Structure Core Mantle Crust

Igneous

• Formed when magma (molten lava) wells up, cools, and hardens; most of the earth’s crust– Granite– Lava

Page 26: The Solid Earth. Earth’s Structure Core Mantle Crust

Igneous

Page 27: The Solid Earth. Earth’s Structure Core Mantle Crust

Sedimentary

• Formed from sediment that is weathered into smaller pieces, transported, and deposited into a body of water, pressed together, forming layers– Sandstone– limestone

Page 28: The Solid Earth. Earth’s Structure Core Mantle Crust

Sedimentary

Page 29: The Solid Earth. Earth’s Structure Core Mantle Crust

Metamorphic

• Formed when preexisting rock partially melts, or is subjected to high pressure– Slate– marble

Page 30: The Solid Earth. Earth’s Structure Core Mantle Crust

Metamorphic

Page 31: The Solid Earth. Earth’s Structure Core Mantle Crust

Rock Cycle

Page 32: The Solid Earth. Earth’s Structure Core Mantle Crust

Natural Hazards-Earthquakes

• Stress in the earth’s crust cause a fracture in solid rock, producing a fault

• Energy is released as shock waves moving outward from the focus– Focus: point of initial movement– Epicenter: point on the surface directly above

the focus

Page 33: The Solid Earth. Earth’s Structure Core Mantle Crust

Earthquakes

Page 34: The Solid Earth. Earth’s Structure Core Mantle Crust

Earthquakes

• Magnitude measured by the Richter Scale• Seismograph measures amplitude of vibrations

(each unit represents an amplitude that is 10X greater than the one before it) ex. An earthquake of 6.0 is 100x greater than a 4.0– Insignificant <4.0– Minor 4.0-4.9– Damaging 5.0-5.9– Destructive 6.0-6.9– Major 7.0-7.9– Great >8.0

Page 35: The Solid Earth. Earth’s Structure Core Mantle Crust

Seismogram

Page 36: The Solid Earth. Earth’s Structure Core Mantle Crust

Earthquakes

• Aftershocks can last up to 4 months• Foreshocks can occur seconds to weeks before

main shock• Primary Effects: shaking, permanent ground

displacement, damage to infrastructure• Secondary Effects: rock slides, urban fires,

flooding, tsunamis• http://www.youtube.com/watch?

v=g15sZ_d2WUY

Page 37: The Solid Earth. Earth’s Structure Core Mantle Crust

Natural Hazards-Volcanoes

• Magma reaching the earth’s surface• Can release:

– Ejecta (rocks, debris)– Liquid lava– Gases (water vapor, carbon dioxide, sulfur dioxide)

• Concentrated where there is seismic activity• Gases can remain in the atmosphere for up to 3 years,

causing a cooling effect by as much as 1oF• http://www.youtube.com/watch?v=bgRnVhbfIKQ

• http://www.youtube.com/watch?v=Hec9yK-QQ4o

Page 38: The Solid Earth. Earth’s Structure Core Mantle Crust

Volcanoes

Page 39: The Solid Earth. Earth’s Structure Core Mantle Crust

Earthquake/Volcanic Activity