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26 Terms

1
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The state of equilibrium between the Earth's lithosphere and the underlying asthenosphere, maintained by the buoyancy of the lithosphere.

Isostasy

2
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First discovered isostasy and observed reduced deflection of plumb lines in the Andes.

George Everest

3
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The depth at which the weight of the crust is balanced by the buoyancy of the mantle.

Compensation depth

4
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The part of the crust directly beneath a mountain that extends deep into the mantle and has lower density, preventing sinking.

Root zone

5
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A model of isostasy that assumes the crust of constant density floats on a denser mantle, with higher elevation corresponding to deeper roots.

Airy-Heiskanen Model

6
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A model of isostasy that assumes topography varies inversely to density, with higher elevation corresponding to lower density of rocks.

Pratty-Hayford Model

7
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A model of isostasy that explains isostatic compensation as a regional phenomenon, with the crust behaving as an elastic material that bends downward due to topographic load.

Vening Meinesz Elastic Plate Model

8
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The process by which the lithosphere floats back to its original position after being pushed down by mountains or other features.

Isostatic rebound

9
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Uplift caused by a lowering of elevation after erosion of a mountain, resulting in a deeper root zone.

Overcompensation

10
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Subsidence caused by an increase in elevation due to additional load, resulting in a shallower root zone.

Undercompensation

11
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The angle formed between the magnetic north of a compass and the true geographical north.

Magnetic Declination

12
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Points on the Earth's surface with a common magnetic declination value.

Isogonic lines

13
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The angle formed between the Earth's surface and the planet's magnetic lines.

Magnetic Inclination

14
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The location with zero magnetic dip, present at the equator.

Aclinic line

15
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Property of materials that are repelled by a magnetic field, with all electron spins paired.

Diamagnetism

16
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Property of materials that are weakly attracted by a magnetic field, due to the presence of unpaired electrons.

Paramagnetism

17
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Property of materials that become magnetized and remain magnetized, with atomic magnetic moments parallel to the external magnetic field.

Ferromagnetism

18
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Property of materials with spins pointing in opposite directions, which may exist at low temperatures but vanishes at and above the NĂ©el temperature.

Antiferromagnetism

19
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Property of materials where the magnetic moments are unequal in magnitude, resulting in a spontaneous magnetization.

Ferrimagnetism

20
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The difference between the measured magnetic field of the Earth and that which would be expected from the International Geomagnetic Reference Field (IGRF).

Magnetic anomaly

21
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The alignment of minerals in the current magnetic field.

Induced magnetization

22
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The magnetization left behind in a ferromagnetic material after an external magnetic field is removed.

Remanence

23
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The ratio of the intensity of induced magnetization to that of remanent magnetization.

Königsberger ratio (Qn)

24
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A magnetometer composed of nickel-iron alloys that measures the strength of the magnetic field along its axis.

Flux-gate magnetometer

25
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A magnetometer that measures the frequency of precession of protons in a proton-rich liquid, proportional to the Earth's magnetic field.

Proton-precession magnetometer (PPM)

26
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A magnetometer that utilizes the Zeeman effect in vapors of alkali elements to measure the strength of the magnetic field.

Absorption-cell magnetometer