Tectonics Flashcards

(49 cards)

1
Q

Why does the west coast of South America show a full range of earthquake depths?

A

Because the Nazca Plate is subducting beneath the South American Plate, producing shallow, intermediate and deep‑focus earthquakes.

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2
Q

What types of earthquake depths occur along the Peru–Chile trench?

A

Shallow, intermediate and deep‑focus earthquakes.

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3
Q

Where are shallow‑focus earthquakes most commonly found?

A

Mostly on plate boundaries

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4
Q

Which type of earthquake is most common worldwide?

A

Shallow‑focus earthquakes

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5
Q

Where are deep‑focus earthquakes typically found?

A

In regions with long, steep subduction zones, such as Japan and the Philippines.

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6
Q

Which country experiences the greatest range of earthquake depths?

A

Japan, one of the world’s most seismically active regions

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7
Q

In which three tectonic settings are volcanoes found?

A

Constructive boundaries,
Destructive boundaries,
Hotspots

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8
Q

What causes volcanic activity at hotspots?

A

The plate moves over a mantle plume, producing effusive, non violent eruptions

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9
Q

Do conservative margins produce volcanoes? Why?

A

No - because the plates slide past each other and do not create magma

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10
Q

Why are volcanoes rare at continental - continental destructive margins?

A

No subduction occurs so magma is not typically generated

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11
Q

What happens at a destructive oceanic - continental plate margin

A

Plates collide, the oceanic plate is subducted, causing explosive and destructive volcanoes and very violent earthquakes

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12
Q

What is formed at a destructive oceanic - continental plate margin

A

A mountain belt forms when plates collide

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13
Q

Why do conservative margins not produce volcanoes

A

conservative margins do no produce volcanoes because plates slide past each other without subduction or magma generation

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14
Q

Where are volcanoes found

A

Volcanoes are mainly found along plate boundaries and in certain active regions such as Asia and Iceland

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15
Q

Mid plate hotspot earthquakes

A

Minor up to magnitude 5.0-6.0

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16
Q

Mid plate Hotspot volcanoes

A

effusive nonviolent

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17
Q

Conservative continental - continental earthquakes

A

very violent up to magnitude 8

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18
Q

Conservative continental - continental volcanoes

A

none

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19
Q

Mid plate hotspot movement

A

plate moves over a rising plume of hot magma

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20
Q

Constructive oceanic - oceanic volcanoes

A

effusive non violent

21
Q

Constructive oceanic - oceanic earthquakes

A

minor up to magnitude 5.0-6.0

22
Q

constructive oceanic - oceanic movement

A

plates move apart

23
Q

destructive continental - continental volcanoes

A

very rare, but devastating

24
Q

destructive continental - continental earthquakes

A

very violent up to magnitude 8

25
destructive oceanic - continental volcanoes
explosive, destructive
26
destructive oceanic - continental earthquakes
very violent up to magnitude 9.0
27
destructive oceanic - continental movement
plates collide, oceanic plate subducts
28
What happened in the 1970s
Geologists accepted that - the lithosphere is divided into tectonic plates - plates move because of convection currents, ridge push and slab pull - interactions at plate boundaries explain earthquakes, volcanoes and mountain building
29
What is happening today (plate tectonic theory)
Continents are still moving at a few centimetres per year Plate tectonics explain global distribution of earthquakes, volcanoes and mountain ranges
30
What happened in the 1960s (Dan McKenzie)
Showed that the lithosphere is made of plates that move due to mantle convection His research helped form the foundation of modern Plate Tectonics Theory
31
What happened in the 1960s
Discovered symmetrical patterns of magnetics stripes on either side of mid ocean ridges These stripes showed Earth's magnetic field had reversed many times. Provided strong evidence supporting seafloor spreading
32
What happened in the 1940s
Hess proposed that magma rises from the mantle at mid ocean ridges As magma cools, new crust forms and spreads outwards This process explains how continents move This idea became known as Seafloor Spreading
33
What happened in 1912
Wegener proposed the idea of Continental Drift He suggested continents were once joined and have since drifted apart Evidence included - Matching coastlines (e.g., South America + Africa) - Fossils found on separate continents - Similar rocks and mountain ranges His theory lacked a mechanism, so it was not widely accepted at the time
34
What is the plate tectonic theory timeline
250 million years ago - Pangaea 1912 - Alfred Wegener (Continental Drift Theory) 1940s - Harry Hess (Seafloor Spreading) 1960S - Vine and Matthews (Magnetic Stripes Evidence) 1960S - Dan McKenzie (Plate Movement) 1970S - Modern Plate Tectonics Established Today - Earth's Lithosphere
35
How fast do tectonic plates move today
A few centimetres per year
36
What did Dan McKenzie discover in the 1960s
That the lithosphere is made of moving tectonic plates driven by mantle convection
37
What evidence did Vine and Matthews discover
Magnetic stripes on the ocean floor, showing polarity reversals
38
Who proposed the idea of Seafloor Spreading
Harry Hess
39
Why was Wegener's theory initially rejected
He couldn't explain how continents moved
40
Characteristics of the continental crust
Thick Underlies continents Made mainly of granite Lower density than oceanic crust
41
Characteristics of the oceanic crust
Thin Underlies ocean basins Made mainly of basalt Denser than continental crust
42
Why is continental crust less dense than oceanic crust
Because it is made mainly of granite rather than basalt
43
Characteristics of the lithosphere
The rigid outer layer of the Earth Made of the crust + upper mantle Around 100 km deep on average It is broken into tectonic plates which are always moving (slowly)
44
What two continents did Pangaea split into
Laurasia (north) and Gondwanaland (south)
45
What is continental crust made of and what is its density like?
Granite; it is thick and has a lower density than oceanic crust
46
What were Wegener's five pieces of evidence for continental drift
Jigsaw fit Geological fit Tectonic fit Glacial deposits Fossil evidence
47
What is the lithosphere
The rigid surface layer of Earth made of the crust and upper mantle, about 100km deep
48
What is oceanic crust made of and what is its density like
Basalt it is thin and denser than continental crust
49