Tectonic Plate Boundaries Flashcards

1
Q

What are Tectonic Plates?

A

Upper, rigid parts of the Earth: lithosphere (heat transfer is by conduction)
Plates drift/ride on moving rock: asthenosphere (heat transfer is by convection)

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2
Q

How does earth keep balanced (stay the same size)?

A

some plates are destroyed

others are formed/enlarged

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3
Q

What are the three types of plate boundary?

A

divergent (oceanic ridge)
transform (transform fault)
convergent (trench, subduction zone)

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4
Q

What happens at divergent plate boundaries?

A

Fractures in lithosphere, plates move apart (extension)

magma rises, forming new crust

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5
Q

What are some examples of divergent plate boundaries?

A

MORs

continental rifts e.g. East African rift

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6
Q

What are the characteristics of divergent plate boundaries?

A

High heat flow
Rift valleys
Active mafic (basaltic) volcanism: fissure eruptions form ocean crust
Shallow, small earthquakes

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7
Q

What are some examples of convergent plate boundaries?

A

ocean-ocean subduction
ocean-continent subduction
continent-continent collision

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8
Q

At divergent boundaries, plates move away from each other - so why do topographic ridges form?

A

material is hottest at the ridge

rocks expand when hot -> less dense -> more buoyant

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9
Q

Why do divergent plate boundaries host only small, shallow earthquakes?

A

crust cools by conduction from ocean, only surface part is brittle enough to fracture in an earthquake

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10
Q

at a convergent plate boundary, which plate subducts? why?

A

denser plate subducted

older plate subducted in the case of two oceanic plates

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11
Q

What are the characteristics of subduction zones?

A

(1) Deep sea trench: depression in seafloor where oceanic plate bends and subduct e.g. Mariana Trench, 11 km deep (ocean-ocean subduction)
(2) Volcanic Arc: arc-shaped chain of volcanic islands (or continental volcanoes) e.g. cascade volcanic arc, Mt St Helens

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12
Q

What are the characteristics of convergent boundary earthquakes?

A

shallow to deep (0-660km deep)

small to very large (up to mag.9‐9.5 at subduction zones)

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13
Q

What happens at continental collision zones?

A

mountain building (orogeny) e.g. Mount Everest 8,848m

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14
Q

What are the “steps” that offset mid-ocean ridges?

A

Transform Boundaries

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15
Q

What happens at transform boundaries? What are the characteristics of transform boundaries?

A

Plates slide past each other

Shallow earthquakes, may be large (M8 but not M9)
Major vertical fractures and scarps
Features are offset horizontally
Usually no volcanic activity – no lithosphere created/destroyed

e.g. San Andreas fault

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16
Q

How can we measure plate motion?

A

(direction, speed relative to each other)
DIRECTION:
MOR orientation - perpendicular to plate motion
Transform fault orientation - parallel to plate motion

SPEED:
Mag. stripe width, age

17
Q

Can we directly measure plate motion?

A
Relatively speaking..
GPS satellites (& antennas) -> DIRECTION and SPEED
18
Q

How do plates move relative to the Earth’s interior?(“absolute” motion)

A

Plumes of hot mantle material rise from great depth and cause volcanism at the surface (e.g., Hawaii)

Hot spots (mantle plumes): remain stationary as plates drift over them and leave a track of volcanic islands showing how the plate has moved

19
Q

What is the distance between the youngest and the oldest Hawaiian islands?

A

around 500km

20
Q

What is the difference in age between the youngest and the oldest Hawaiian islands?

A

around 5 million years

21
Q

How fast is the Pacific Plate moving (cm/yr)?What direction?

A

Big Island -> Kauai: ~500 km
Age difference of volcanoes: ~5 million yrs

plate is moving north west at around 10cm/yr

22
Q

Which plates are moving faster?

A

Pacific, India-Australia, Philippine Sea plates

23
Q

Which plates are moving slower?

A

Antarctic, Africa, N. America, S. America

24
Q

What are the driving mechanisms for plate motion?

A

Convection in Earth’s interior -> Mantle drag

Gravity; Physical properties of plates (cooling, density change)

  • > Slab pull
  • > Ridge push