plate tectonics the dynamic interior of the earth

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Plate Tectonics The Dynamic Interior of the Earth

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Page 1: Plate Tectonics The Dynamic Interior of the Earth

Plate TectonicsThe Dynamic Interior of the Earth

Page 2: Plate Tectonics The Dynamic Interior of the Earth

Review of Earth’s Interior:

1. Name, in order going from the center of the Earth to where we live, the four major layers of the Earth.

2. What composes the lithosphere?3. How do the two layers closest to the center of

the Earth differ in their composition?4. Describe how scientists determine the

composition of the different layers of the Earth.

Page 3: Plate Tectonics The Dynamic Interior of the Earth

If you look at a map of the world, do you notice anything interesting about the shapes of the continents?

Page 4: Plate Tectonics The Dynamic Interior of the Earth

Plate Tectonics

•https://www.youtube.com/watch?v=_5q8hzF9VVE• The Earth’s crust is divided into 12

major plates which are moved in various directions.• This plate motion causes them to

collide, pull apart, or scrape against each other.

Page 5: Plate Tectonics The Dynamic Interior of the Earth
Page 6: Plate Tectonics The Dynamic Interior of the Earth

Plate Tectonics• The plate

interactions cause the Earth structures (mountains, trenches, etc.).• Tectonic:

deformation of the crust because of a plate interaction.

Page 7: Plate Tectonics The Dynamic Interior of the Earth

What are tectonic plates made of?• Plates are made of

rigid lithosphere.• Remember - The

lithosphere is made up of the crust and the upper part of the mantle.

Page 8: Plate Tectonics The Dynamic Interior of the Earth

Theory of Continental Drift• Proposed by Alfred

Wegener in early 1900’s.• He hypothesized

that the continents were once joined together in a single large land mass he called Pangaea

Page 9: Plate Tectonics The Dynamic Interior of the Earth

Theory of Continental Drift• Pangaea split apart

and the continents moved gradually to their present positions• Process is known as

Continental Drift

Page 10: Plate Tectonics The Dynamic Interior of the Earth

Pangaea, about 200 million years ago, before it began breaking up.Wegener named the southern portion of Pangaea Gondwana, and the northern portion Laurasia.

Page 11: Plate Tectonics The Dynamic Interior of the Earth

The continents about 70 million years ago. Notice that the breakup of Pangaea formed the Atlantic Ocean. India’s eventual collision with Eurasia would form the Himalayan Mountains.

Page 12: Plate Tectonics The Dynamic Interior of the Earth

Learning Check

•What layer of the Earth composes the tectonic plates?• How many “major” plates make up the

Earth?•Who developed the theory of plate

tectonics?• Describe Pangaea.

Page 13: Plate Tectonics The Dynamic Interior of the Earth

Evidence of Continental Drift

1. Continents fit together like a puzzle.• Ex. - The Atlantic

coastlines of Africa and South America.

Page 14: Plate Tectonics The Dynamic Interior of the Earth

More Evidence…

2. Fossils of several plants and animals of the same species found on different continents.

Ex. Mesosaurus

Page 15: Plate Tectonics The Dynamic Interior of the Earth

Some More Evidence3. Rock and Mountain

Correlation. Identical rocks and mountain structures have been found on either side of the ocean.

• The order of rock layers in South America, Africa, India, Antarctica, and Australia show remarkable similarities.

Page 16: Plate Tectonics The Dynamic Interior of the Earth

Last Piece of Evidence4. Ancient climate information.• Coal has been found in cold regions and

glacial evidence has been found in warm climates.

Page 17: Plate Tectonics The Dynamic Interior of the Earth

Another Learning Check…

1. Explain at least 3 pieces of evidence used to support Wegener’s theory of continental drift.

Page 18: Plate Tectonics The Dynamic Interior of the Earth

Was Wegener Correct?• Everyone agreed that

Wegener’s evidence was compelling. But wouldn’t we feel the movement?• Also, wouldn’t there be

evidence to show that the continents were still moving today?• Wegener was a

meteorologist and his theory was not well accepted. (He died on an expedition in Greenland collecting ice samples)

Page 19: Plate Tectonics The Dynamic Interior of the Earth

Holes in Wegener’s Theory…

• One reason scientists had a hard time with Wegener’s theory is that there was no mechanism for the continents motion.

Page 20: Plate Tectonics The Dynamic Interior of the Earth

Sea Floor Spreading• Henry Hess• 1960’s• Using new

technology, radar, he discovered that the seafloor has both trenches and mid-ocean ridges.• Proposed the sea-

floor spreading theory.

Page 21: Plate Tectonics The Dynamic Interior of the Earth

Sea Floor Spreading• Hess proposed that hot, less dense material

below Earth’s crust rises toward the surface at the mid-ocean ridges.• Then, it flows sideways, carrying the seafloor

away from the ridge in both directions.

Page 22: Plate Tectonics The Dynamic Interior of the Earth

Sea Floor Spreading• As the seafloor spreads apart at a mid-

ocean ridge, new seafloor is created.• The older seafloor moves away from the

ridge in opposite directions.• This helped explain how the crust could

move—something that the continental drift hypothesis could not do. • https://

www.youtube.com/watch?v=hmMlspNoZMs

Page 23: Plate Tectonics The Dynamic Interior of the Earth

Evidence of Seafloor Spreading• In 1968, scientists

aboard the research ship Glomar Challenger began gathering information about the rocks on the seafloor. • Scientists found that

the youngest rocks are located at the mid-ocean ridges.

Page 24: Plate Tectonics The Dynamic Interior of the Earth

Age of Seafloor Rocks