Plate Tectonics Flashcards

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1
Q

Inner Core

A

800 miles thick (iron & nickel in solid state)

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2
Q

Outer Core

A

1,400 miles thick (iron and nickel in liquid state)

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3
Q

Mantle

A

1,800 miles thick (flows with consistency of asphalt)

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4
Q

Continental Plate

A

5-25 miles thick

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5
Q

Oceanic Plate

A

3-5 miles thick

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6
Q

Divergent Plate Margin

A

Spreading Motion - Constructive Effect - Ridge Topography - Volcanic Activity

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7
Q

Convergent Plate Margin

A

Subduction Motion - Destructive Effect - Trench Topography - Volcanic Activity and Earthquakes

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8
Q

Transform Plate Margin

A

Lateral Sliding Motion (Slides Paralel) - Conservative Effect - No Major Topography - No Volcanic Activity but Earthquakes are present within crust

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9
Q

Deep Sea Trench

A

in the deepest parts of the ocean; these are long, narrow depressions along the sea floor which are formed due to tectonic activity (the movement of the Earth’s lithosphere)

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10
Q

Volcanic Arc

A

a LONG chain of many volcanoes that forms above a SUBDUCTION ZONE.

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11
Q

Ring of Fire

A

a large area around the Pacific Ocean that has active earthquakes, volcanic eruptions and tectonic plate boundaries that fringe the Pacific Basin.

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12
Q

Subduction Zone

A

a convergent plate boundary where the Earth’s crusts meet and one expands underthe other because it’s denser.

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13
Q

Fold Mountains

A

mountains that are formed by two or more tectonic plates when they are pushed together by the Earth’s crusts.

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14
Q

Block Mountains

A

a mountain formed by natural faults in the Earth’s crust. A mountain formed when crustal plates move away from each other.

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15
Q

Plate Boundaries/Margins

A

the boundary of one of the plates that forms the upper layer (lithosphere) and together cover the surface of the Earth.

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16
Q

Two types of Layers That the Earth is Made of

A

Compositional (chemical) & Mechanical Layers

17
Q

Three Mechanical Layers

A

Lithosphere - Asthenosphere - Mesosphere

18
Q

Creator of Plate Tectonics Theory

A

Alfred Wegener

19
Q

Pangea

A

a notion that around 335 millions years prior to now, there existed an ancient supercontinent based off the evidence of continental drift and fossil evidence.

20
Q

Plate Tectonics Theory

A

a notion that the outermost mechanical layer (the lithosphere) or Earth’s crust is divided into many plates which shift across the earth’s surface

21
Q

Evidence of the Plate Tectonics Theory

A

Our planet is always forming and reshaping itself from beneath ( magma rising )

The locations of earthquakes and volcanoes around the world follow a similar pattern to that of which Wegener theorised, an outline of the plates beneath us

Fossils of tropical species for example were found in less than tropical areas of the world, proving Wegener’s point of the world being one supercontinent at a time in prehistory.

22
Q

Three Types of Plate Boundaries

A

Convergent

Divergent

Transform

23
Q

Sima

A

The lower layer of the Earth’s crust, it is dense and heavy

24
Q

Sial

A

Found on the upper part of the earth’s crust and is very light.

25
Q

Difference between Sima and Sial

A

Sima is the lower layer of the Earth’s crust, it is dense and heavy while sial is found on the upper part of the earth’s crust and it is much lighter than sima.

26
Q

Acidic Lava

A

Comes from composite volcanoes and it is viscous (sticky) it also moves slowly and traps gases.

27
Q

Basic Lava

A

Comes from shield volcanoes and it runs faster than acid lava. Doesn’t. trap gases.

28
Q

Features Formed by Active Plate Margins

A

Deep sea trenches

Volcanoes

Mountains

29
Q

Three Signs of Plate Tectonics

A

The locations of volcanoes and earthquakes around the world follow a pattern that was theorised by Alfred Wegener.

Fossils of tropical animals were found in regions that don’t host a tropical climate which proves the theory of Pangea.

The planet is always reshaping and forming itself from beneath the Earth’s surface.

30
Q

Formation of Fold Mountains

A

Fold mountains are formed when two tectonic plates shift and collide causing the earth to rise and form hills and mountains.