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P6.2 Plate Techtonics

P6.2 Plate Techtonics

Assessment

Presentation

Science

11th Grade

Medium

NGSS
HS-ESS1-5, HS-ESS2-1

Standards-aligned

Created by

Amanda Petyko

Used 15+ times

FREE Resource

8 Slides • 7 Questions

1

P6.2 Plate Techtonics

By Amanda Petyko

2

Some text here about the topic of discussion.

Some minerals in igneous rocks develop a slight magnetism in alignment with Earth’s magnetic field at the time of their formation. Also, scientists have discovered the polarity of Earth’s magnetic field has periodically reversed and the North Magnetic Pole becomes the South Magnetic Pole, while the South Magnetic Pole becomes the North Magnetic Pole.​

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Scientists looked at the new rock formed at the bottom of the ocean and saw igneous rocks that had recorded the magnetic field of the Earth.

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The ancient magnetism, called paleomagnetism, present in rocks on the ocean floor can be used to determine the rate at which the plates are separating and, consequently, the time when they began to separate. Where plates separate along the mid-ocean ridge, magma from the mantle rises to the surface and creates new ocean floor. As the magma cools, the minerals assume magnetism equal to the magnetic field at that time.

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5

Multiple Choice

Question image

Which "stripe" of seafloor is the oldest?

1

Dark red

2

Orange

3

Peach

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Multiple Choice

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How do we know those stripes are present on the sea floor?

1

You see the lava coming up from the mantle.

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They are magnetized differently.

3

The rocks are colored different.

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Multiple Choice

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How many magnetic reversals have happened according to this data?

1

6

2

5

3

4

4

3

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Records of the magnetic polarity reversals have been determined from the oceanic crust across sections of the mid-ocean ridges in the Pacific, South Atlantic, and North Atlantic oceans.​

This shows spreading from the last 2 million years.​

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Multiple Choice

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Which ocean has spread the greatest distance during the last 2 million years?

1

The first one (Pacific Ocean)

2

The middle one (South Atlantic Ocean)

3

The last one (North Atlantic Ocean)

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More evidence to support Plate Tectonic Theory...

Hawaiian Islands

Researchers have proposed that a rising plume of mantle material has formed a hot spot below the island of Hawaii. It is believed that the position of this hot spot within the Earth has remained constant during a very long period of time. In the past, as the Pacific plate has moved over the hot spot, the successive volcanic islands of the Hawaiian chain have been built.

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Poll

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Kauai = 3.8 - 5.6 myo

Oahu = 2.2 - 3.3 myo

Molokai = 1.3 - 1.8 myo

Maui = less than 1.0 myo

Hawaii = 0.7 - present

Which island is the oldest?

Kauai

Oahu

Molokai

Maui

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Multiple Choice

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Kauai = 3.8 - 5.6 myo

Oahu = 2.2 - 3.3 myo

Molokai = 1.3 - 1.8 myo

Maui = less than 1.0 myo

Hawaii = 0.7 - present

Which island currently under the hot spot?

1

Oahu

2

Hawaii

3

Molokai

4

Maui

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Multiple Choice

Which tectonic plate is moving over the hot spot that formed the Hawaiian Islands?

1

The Atlantic Plate

2

The Indian Plate

3

The Pacific Plate

4

The North American Plate

P6.2 Plate Techtonics

By Amanda Petyko

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