Title: Evidence Supporting Crustal Plate Movement Earth Science High School
1Evidence Supporting Crustal Plate MovementEarth
ScienceHigh School
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2Teacher Page
- Content Earth Science
- Grade level High School
- Creator Lisa Boulden
- MAP Standard
- Identify evidence of Crustal Plate movement
- Use journal for notes and questions
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3Crust of the Earth (Write in your journal)
- How would you define the Earths crust?
- All of the solid Earth
- What are the two types of crust?
- 1. Continental crust
- Where would you find continental crust?
- The majority of the continental crust is found
above sea level. - 2. Oceanic Crust
- Where would you find oceanic crust?
- Below sea level.
4Characteristics
5- Plate Tectonics
- What does it mean???
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7In your journalBased on the picture of plate
tectonics explain in your own words what you
think has occurred.
8Plate tectonics is...
- slow horizontal movement of the continents over
thousands of years - caused by the movement of crustal plates
- resulting in the present continent locations
9Evidence to support plate movement
- List two ideas you would present to support the
theory of plate movement. - Volcanic activity
- Earthquakes
- Islands
- Mountains
- The mid ocean ridge
- Past theories such as Pangea
- fossil and climate clues
- rocks
- continental shorelines matching up
10Volcanic Activity
11Supporting Evidence for Volcanic Activity
- Volcanoes occur at diverging plate boundaries and
convergent plate boundaries - Diverging plate boundaries the boundary between
two plates that are spreading apart - Lava flows up through the crack that develops
when the plates move apart - Convergent plate boundaries the boundary between
two plates that are moving toward each other - Lava is forced to the surface at the point where
one plate pushes under the other
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13Supporting Evidence Earthquakes
- Rocks break and move along faults
- Fault movement is caused from the constant motion
of the Earths crust - This movement puts stress on the rock
- The stress causes rocks to bend, compress, and
stretch like rubber bands - Resulting in vibrations within the Earth, known
as Earthquakes
14Islands
15Supporting evidence for islands
- As a plate begins its descent, a continuous
series of earthquakes is created - Magmas are melted and rise toward the surface
- If the upper plate is oceanic, the volcanoes pile
up until they poke through the surface of the
ocean and form an elegant arc of islands
16Islands continued
- Eventually these magmas make their way up into
the leading edge of the overriding plate, where
they add material to the crust and build
volcanoes above it
17Mountains
18Supporting evidence for mountains
- When two continents carried on converging plates
ram into each other, they crumple and fold under
the enormous pressure, creating great mountain
ranges
19Mid Ocean Ridges
20Supporting evidence for the mid ocean ridge
- the Mid-Ocean Ridge is a continuous range of
undersea mountains more than 12,000 feet high and
1,200 miles wide winding through 40,000 miles of
the worlds oceans - two plates are pulling apart from each other as
hot magma (liquid rock) emerges from the mantle
and oozes forth as lava to fill the crack
continuously created by plate separation
21PangeaThe Original Supercontinent
22Supporting evidence for fossil and climate clues
- Fossils of the same fresh water/land reptile
found in South America and Africa - The fossil Glossopteris (a fern) was found in
Africa, Australia, India, South America, and
Antarectia, a wide variety of climates would
indicate that they were once similar - Fossils of warm weather plants were found in
Greenland, which has a cold climate
23Supporting evidence for rocks
- Similar rock structures are found on different
continents - Part of the Appalachian Mountains of the eastern
United States are similar to those found in
Greenland and western Europe - South America and western Africa have rock
structures that are very similar
24Supporting evidence for continental shorelines
matching up
- parallelism of opposite shores
- Continents appear to fit together like puzzle
pieces - Continental shelf matches up better than the
actual shorelines - How would you test the theory that the continent
fit together at one time?
25Putting it all together (in your notes)
- Your job is to use the information you have
learned about continental drift and the movement
of crustal plates to persuade a nonbeliever of
Pangea that at one time our continents were one
large land mass. You must provide supporting
evidence to back your persuasion.