Magnetic Reversal

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description

Definition of Magnetic Reversal, Earth's Magnetic Field, Magnetic Compass, Magnetic Reversals as Proof of Seafloor Spreading...

Transcript of Magnetic Reversal

Page 1: Magnetic Reversal
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OBJECTIVES:

Define Magnetic Reversal

Provide an answer to

the question:

How does Magnetic

Reversal happen and how does it

prove seafloor spreading?

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What is

Magnetic Field

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The Earth’s Magnetic Field is generated in the very hot molten outer core and has existed since the birth of our planet.

It is a dipole, one that has a North Pole and a South Pole.

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The magnetic field is represented by magnetic field lines, which show the direction of the field at different points.

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A Magnetic Compass

Tells us directions on Earth

Proves that the Earth has a magnetic field

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What is Magnetic

Reversal

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Magnetic Reversal

A change in a planet’s magnetic field such that the positions of magnetic north and magnetic south are interchanged. The Earth’s field has alternated between periods of normal polarity, in which the direction of the field was the same as the present direction, and reverse polarity, in which the field was the opposite.

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Magnetic Reversal is also called magnetic ‘flip’ of the Earth. It happens when the North Pole is transformed into South Pole and the South Pole becomes the North Pole. This is due to the change in the direction of flow in the outer core.

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Magnetic Reversal as a Proof of Seafloor Spreading

Seafloor spreading was strengthened with the discovery that the magnetic rocks near the ridge follow a pattern aside from the fact that rocks near the ridge are remarkably younger than those fathers from the ridge.

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Magnetic reversals happened many times in the past. The occurrence of magnetic reversals can be explained through the magnetic patterns in magnetic rocks, especially those found in the ocean floor. When lava solidifies, iron bearing minerals crystallize. As these crystallize, the minerals behave like tiny compasses and align with the Earth’s magnetic field. So when magnetic reversal occurs, there is also a change in the polarity of the rocks. This allowed scientists to visualize the magnetic stripes in the ocean floor, and to construct a magnetic polarity time scale.

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Over the last 10 million years, there has been an average of 4 to 5 reversals per million years. New rocks are added to the ocean floor at the ridge with approximately equal amounts on both sides of the oceanic ridge. The stripes on both sides are of equal size and polarity which seemed to be mirror images across the ocean ridge.

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