Chapter 3 Flashcards

1
Q

Who came up with the Continental drift theory?

A

Alfred Wegner

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2
Q

Continental drift theory

How long ago would this have occurred?

A

Theory suggesting that all of Earth’s land had once been joined together into a single super-continent surrounded by an ocean

  • pangaea: the landmass
  • panthalassa: the surrounding ocean

-200 million years ago

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3
Q

What is the centrifugal theory?

A

Theory that believed the continents were slung toward the equator on the spinning Earth by a centrifugal effect
- inertia coupled with tidal drag on the continents (from the combined effects of the sun and moon) would account for the drifting continents

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4
Q

Is earth’s mantle a solid?

A

no it reacts to earthquakes, so it is a deformable mass

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5
Q

Seismic waves

A

low frequency waves generated during earth quakes

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6
Q

What are the types of seismic waves?

A

Surface waves: move along earth’s surface and the main reason for damage from earthquakes

Body waves: less dramatic, but very useful for analyzing earth’s interior surface

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7
Q

Types of Body waves?

A

P wave (primary wave): a compressional wave similar in behavior to a sound wave

S wave (secondary wave): a shear wave like that seen in a rope shaken side to side

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8
Q

Seismograpgh

A

instrument that senses and records earthquakes

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9
Q

Shadow zone

A

a wide band from which S waves were absent, would be found on the side of the Earth opposite the location of an earthquake
-existence of liquid core and shadow zone 1914, seismographic analysis

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10
Q

Mantle

A

core boundary

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11
Q

Crust

A

thin, relatively lightweight outermost layer

  • oceanic crust: thin and mostly basait
  • continental crust: granite
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12
Q

Mantle

A

beneath the crust, compose of 68% Earth’s mass and 83% volume

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13
Q

Core

A

intermost layer

-31.5% earth’s mass, 16% of its volume

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14
Q

Physical layers of the Earth

A

Lithosphere
Asthenosphere
Lower mantle
Core

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15
Q

Lithosphere

A

earth’s cool rigid outer layer

-Continental and oceanic crusts

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16
Q

Asthenosphere

A

hot, partially melted, slowly flowing layer of upper mantle

17
Q

Lower mantle

A

extends to the core

  • similar composition to the asthenosphere
  • hotter but due to rapidly increasing pressure the mantle below the asthenosphere does not melt
18
Q

Core

A

Two parts:

  • outer layer dense viscous liquid
  • inner layer solid
19
Q

William Thomson

A

Lord Kelvin
Earth is 80 million yrs old
-based on the rate at which the planet would have cooled from an original molten mass
*drying fruit model: earth shrunk as it cooled

20
Q

Radioactive decay

A

though most atoms are stable and do not change some forms of elements are unstable and give off heat when their nuclei break apart (decay)

  • radioactive particles ejected in process
  • released heat that contributed to Earth’s melting of the original mass
21
Q

Conduction

A

Internal heat journeys toward the surface

22
Q

Convection

A

heat that arises in the asthenosphere and mantle

- occurs when a fluid or semisolid is heated, expands, and becomes less dense and rises

23
Q

James Hutton

A

Uniformitarianism: all of Earth’s geological features and history could be explained by process identical to today’s and these processes must have been at work for a long time
- did not believe in the bibles concept of creation