Chapter 12 Flashcards

1
Q

The transfer of heat through matter by molecular activity

A

Conduction

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2
Q

The transfer of heat by the mass movement or circulation of a substance

A

Convection

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3
Q

The innermost layer of Earth based on composition. It is thought to be largely an iron-nickel alloy with minor amounts of oxygen, silicon, and sulfur

A

Core

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4
Q

The gradual increase in temperature with depth in the crust. The average is 30 degrees C per kilometer in the upper crust

A

Geothermal Gradient

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5
Q

The solid innermost layer of earth, about 1216 kilometers in radius

A

Inner core

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6
Q

The rigid outer layer of Earth, including the crust and upper mantle

A

Lithosphere

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7
Q

Lies between the transition zone and the liquid core, contains the mineral perovskite, is the earths largest layer occupying 56% of the volume of the planet

A

Lower mantle

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8
Q

The solid rocky shell that extends from the base of the crust to a depth of 2900 kilometers

A

Mantle

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9
Q

A field that surrounds the Earth because of Earths convection currents in earths liquid iron core

A

Magnetic field

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10
Q

A subdivision of the mantle situated below the lithosphere. This zone of weak material exists below a depth of about 100 kilometers and in some regions extends as deep as 700 kilometers. The rock within this zone is easily deformed.

A

Asthenosphere

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11
Q

The part of the mantle that extends from the core-mantle boundary to a depth of 660 kilometers. Also known as lower mantle

A

Mesosphere

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12
Q

The boundary separating the crust and the mantle, discernible by an increase in seismic velocity

A

Moho

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13
Q

A layer beneath the mantle about 2270 kilometers thick, which has the properties of a liquid

A

Outer core

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14
Q

The zones between 105 and 140 degrees distance from an earthquake epicenter, which direct waves do not penetrate because of refraction by Earth’s core

A

Shadow zones

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15
Q

When seismic wave hits a boundary between different Earth materials and waves are reflected back toward surface

A

Seismic reflection

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16
Q

The bending of seismic waves while passing through the Earth

A

Seismic refraction

17
Q

The actual shape of the earth, which is rough and oblate, or slightly squashed; the earths circumference is longer around the equator than it is along the meridians

A

Geoid

18
Q

The paths of the seismic waves

A

Seismic Rays

19
Q

Boundary layer between the rocky mantle and the liquid iron outer core; large variations in composition and temperature

A

D” layer