Earth Science-2 Flashcards

(55 cards)

1
Q

Geologic process of Earth describe the natural forces that influence the shape and structure of the planet.

A

Geologic Process of the Earth

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2
Q

formed, located or occurring beneath the surface of the earth.

A

Endogenic Process –

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3
Q

– forces within the earth that cause the ground to move

A

Endogenic Forces

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4
Q

– when the land is shaped by endogenic forces

A

Endogenic Processes

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5
Q

The Main Endogenic Process

A

Folding and faulting

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6
Q

– two forces push towards each other from the opposite sides

A

Folding

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7
Q

– fracturing and displacement of more brittle rock strata along a fault plane

A

Faulting

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8
Q

Types of Faulting

A

Normal fault (convergence)
Reverse fault (divergence)
Tear fault (transform)

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9
Q

Other endogenic (subsequent)

A

Other Endogenic Subsequent
Volcanism (volcanic activity)
Metamorphism
Earthquake (seismic activity)

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10
Q

– volcanism or magmatism (also known as volcanic activity or igneous activity)
Two types of volcanism:

A

Volcanism

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11
Q

when magma is forced into the rocks that make up the earth’s crust

A

Intrusive Volcanism

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12
Q

– are the result of magma coming from deep within the earth to surface

A

Extrusive Volcanism

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13
Q

Result of volcanism – igneous rock

A

Andesite
Granite
Pumice

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14
Q

an endogenic process which occurs when there is pressure and heat applied to geologic structures which leads to metamorphic rock

A

Metamorphism –

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15
Q

Result of metamorphism
Slate
Marble
Amphibolite

A

Slate
Marble
Amphibolite

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16
Q

– seismic activity is an sudden shaking or vibration in the earth’s crust

A

Earthquakes

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17
Q

– activities or phenomena occur on the earth’s surface

A

Exogenic process

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18
Q

–process that breaks down rock in to smaller pieces

A

Weathering

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19
Q

happens when rock is physically broken into smaller pieces

A

Physical weathering

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20
Q

Factors that affect physical weathering

A

Iced wedging
Release of pressure
Growth of plants
Animals
Abrasion

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21
Q

– process of breaking down through chemical changes

A

Chemical weathering

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22
Q

Factors that affect chemical weathering

A

Water
Oxygen
Carbon dioxide
Living organisms
Acid rain

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23
Q

– rock particles carried away by wind, water, ice, & gravity

24
Q

– changes the shape of coastline

A

Erosion by water

25
– can erode the land
Erosion by ice
26
– carries dust, sand, and volcanic ash from one place to another
Erosion by wind
27
– pulls any loose bits down the side of the hill or mountain
Erosion by gravity
28
– natural process in which a material is carried to the bottom of bodies of water and forms to solid
Sedimentation
29
– is the movement of rock, soil, and downward due to the action of gravity
Mass wasting
30
Factors that triggered mass wasting
Over-steepened slope Water Earthquake Vegetation removal
31
– in 1956, observed and presupposed that shapes of continents on both sides of the atlantic ocean seem to connect to each other
Abraham Ortelius
32
– 1912, geophysicist developed and hypothesized the continental drift theory
Alfred Wegener
33
– proposed the existence of Tethys sea, the only recognized body of water
Eduard Suess
34
– massive land mass
Pangaea
35
Two giant continents:
Laurasia and Gondwanaland
36
– a genus extinct of seed ferns
Glossopteris
37
Tillites – glacial deposits from rock strata in areas that were once covered with snow
Tillites
38
– fossil fuel originated from the chemically altered remains of prehistoric vegetation
Coal
39
Evidences to support the continental drift theory:
•Similarity of fossils found in different continents Presence of tillites in areas whose present climates do not suggest •glacial formation •Presence of coal in polar regions •Continuity of rock layers found in different continents •Similarity of rock types in different continents
40
7 continents
: Russia Asia South America North America Africa Australia Antarctica
41
– birth of plate tectonic theory
1940
42
– suggested that the idea of mantle convection as the driving force for the movement of continents
Arthur Holmes
43
as a substance is heated, its density decreases and rises to the surface until it cools and sank again
Thermal Convection
44
– to specify that heat is actually radiating from the mantle
Mantle Convection
45
: Oceanic lithosphere: Continental lithosphere:
ocean & seas land
46
7 Major Plates
Pacific plate Eurasian plate North American plate South American plate Indo-Australian plate Antarctic plate African plate
47
where plates meet
Convergent –
48
moves away from each other
Divergent –
49
slides past each other
Transform –
50
Movement of plates results in crustal deformation (folding & faulting)
Crustal Deformation
51
Folding – resulting from the compression of rock Faulting – forms cracks or fractures on the rocks Compressional stress – cause two rocks to squeeze Example: himalayan mountains Tensional stress – a rock pulled apart Example: mid atlantic ridge, great african rift valley Shear stress – deformation of a material by slippage along place Example: small ponds, deep trench, sea floor
Folding
52
– forms cracks or fractures on the rocks
Faulting
53
– cause two rocks to squeeze Example: himalayan mountains
Compressional stress
54
– a rock pulled apart Example: mid atlantic ridge, great african rift valley
Tensional stress
55
deformation of a material by slippage along place Example: small ponds, deep trench, sea floor
Shear stress