Paleomagnetism Flashcards

1
Q

At which geographic pole is the southern magnetic pole located?

A

The southern magnetic pole is currently located at the geographic north pole.

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2
Q

Geographic (True) north is located

A

On Earth’s spin axis

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3
Q

Current declination of earth’s north geomagnetic pole

A

NOT the same as true north.

Current difference is about 11.5 degrees.

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4
Q

What happens to your compass as you approach true magnetic north?

A

It becomes more erratic.

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5
Q

Where on earth is the magnetic inclination horizontal?

A

At the equator

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6
Q

Where on earth is the magnetic inclination horizontal?

A

At the geomagnetic poles

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7
Q

Where would a rock with this magnetic inclination have formed?

A

The northern hemisphere near the equator

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8
Q

Where would a rock with this magnetic inclination have formed?

A

At the northern hemisphere near the poles

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9
Q

How did this plate move?

A

In the southern hemisphere towards the equator.

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10
Q

How do magnetic inclinations change with location on earth?

A
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11
Q

Is the earth a permanent magnet?

A

No the interior is below the curie point of ferromagnetic materials.

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12
Q

geodynamo

A

The mechanism by which the earth shares it’s magnetic field

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13
Q

What sustains earth’s geodynamo?

A

It is sustained by a moving electric current caused by thermal convection in the liquid outer core.

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14
Q

Is earth’s actual magnetic field dipole or non dipole?

A

It is a combination of both, though it behaves mostly like a dipole.

If you remove the dipole firled, there are splotches of non-dipole fields

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15
Q

Evidence of earth’s magnetic field

A

Historic record of variable magnetic north wrt geographic north

Fossil traces of magnetic field in the past

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16
Q

Curie temperature

A

The temperature at which certain magnetic materials undergo a sharp change in their magnetic properties.

17
Q

Thermal remnant magnetization

A

mineral grains fix their magnetic directions as the material cools.

18
Q

What rocks show past magnetic inclinations?

A

Igneous rocks: Rocks cool and hold the geomagnetic field at the time of formation

Sedimentary rocks: Erosion of magnetic materials become suspended in water and become alligned at the time of settlng of the sediments

19
Q

Apparent positions of magnetic poles in the past

A

not consistant with current poles.

20
Q

True polar wanderer

A

Fixed continents.

Poles move relative to the continents

Recreation of paleopoles on separate continents should look similar.

21
Q

Apparent polar wanders

A

Continental drift

continents move relative to the poles

Recreation of paleo paths is a unique path.

22
Q
A