tectonics Flashcards

1
Q

who proposed the idea of continental drift

A

Alfred Wegener, 1912 Pangaea
- Asserted Pangaea had broken into pieces were still moving apart - related to the spinning Earth

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2
Q

what is density

A

mass per unit volume

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3
Q

what is the density stratification like on earth

A

denser substances towards the center

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4
Q

what kind of waves do earthquakes generate

A

seismic waves

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5
Q

2 types of seismic waves

A

surface waves - travel along Earth’s surface
body waves - travel through Earth

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6
Q

2 types of body waves

A
  • P wave - compressional wave – refracted at density boundaries (travel 2x as fast as S waves in solids )
  • S wave – shear wave – cannot pass through liquids
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7
Q

what is used to detect and record arrival times and intensity of seismic waves

A

seismograph

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8
Q

what did Oldham discover

A

“shadow zones” - different waves bend different ways in dense and less dense zones – able to get an idea of planet structure

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9
Q

crust characteristics

A

Earth’s rocky shell ~ 2-75 miles
- form shifting slabs of rock called tectonic plates

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10
Q

2 types of crust

A

Oceanic – basalt
Continental – granite

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11
Q

upper mantle characteristics

A

~400 miles thick
- The rigid top ~40 miles

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12
Q

lower mantle characteristics

A

~ 1400 miles thick
- extends to core – similar composition to asthenosphere, but does not melt due to rapid pressure increase – increases melting point

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13
Q

mantle characteristics

A

Oxygen, iron, magnesium, silicon - ~68% of Earth’s mass, 83% of volume

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14
Q

outer core characteristics

A

~1,400 miles thick
- Mostly iron and nickel

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15
Q

inner core characteristics

A

~ 1,500 miles in diameter
- Mostly iron

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16
Q

what factors determine the behaviour of the rock

A

temperature, pressure, rate at which stress is applied

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17
Q

Lithosphere characteristics

A

~ 44-125 miles depth
- crust + uppermost cool and rigid portion of mantle
- floats on (and is supported by) the denser deformable asthenosphere

18
Q

Asthenosphere characteristics

A

~ 400 miles depth
- hot, partially melted, slowly flowing

19
Q

upper core characteristics

A

dense, viscous liquid

20
Q

inner core characteritics

A

solid, ~6 times denser than crust

21
Q

what is earths internal heat maintained by

A

radioactive decay
- Heat transfer occurs via conduction (solid materials) + convection (fluids like the mantle)

22
Q

what is buoyancy

A

Things sink until the same proportion of their volume is submerged – continents do this

23
Q

what is Isostatic equilibrium

A

erosion of a top of a mountain causes their roots to rise to get equilibrium – cause continental crust to get thinner

24
Q

crustal rock vs asthenosphere differences

A
  • crustal rock is rigid and does not flow at surface temperatures
  • Ships adjust to weight changes via buoyancy, but crustal rock cannot
25
Q

what is a fault

A

When the force of uplift/down-bending exceeds mechanical strength of adjacent rock – the rock will fracture - adjacent rock fragments move vertically toward each other

26
Q

what are the 3 historical debates over Earth’s age

A
  • James Hutton – uniformitarianism
  • Controversy with biblical school of thought – catastrophism
  • Darwin and Wallace – biological evolution
27
Q

Some interesting observations that led to the sea floor spreading hypothesis

A
  • Many earthquake lines correspond with ocean ridges
  • Seismographs indicated deformable, non-rigid layer in North Atlantic upper mantle - shows how tectonic plates can move
  • Radiometric dating shows that the ocean floor is about 200 million years old - very young compared to Earth’s age
  • Ocean floor sediments thickest at edge of Atlantic, thinnest near ‘Mid-Atlantic Ridge’
28
Q

what are Mid-ocean ridges

A

spreading centers where oceanic crust forms

29
Q

what are Subduction zones

A

areas where oceanic crust recycled into mantle

30
Q

what is the sea floor spreading hypothesis and the key observations that support it

A

explains how new oceanic crust forms and moves across the ocean floor
- Spreading centers were hot
- New oceanic crust cooled and so shrunk in volume and become denser as move from center
- The ocean was thus deeper father from the spreading center

31
Q

what are plate tectonics a combination of

A

Seafloor spreading + continental drift = plate tectonics

32
Q

who proposed the idea of continental drift

A

Wilson, 1965

33
Q

what are tectonic plates and how are they formed

A
  • Earth’s lithosphere is divided into separate plates that float on the asthenosphere
  • they move over the semi-fluid, deformable asthenosphere
  • Heat from Earth’s interior causes the asthenosphere to expand, become less dense, and rise
  • Rising material lifts and cracks the crust, creating the edges of tectonic plates.
34
Q

3 ways that tectonic plates interact at plate boundaries

A
  • Divergent
  • Convergent
  • Transform
35
Q

divergent plate interaction

A

plates move apart
- where ocean basins are formed (mid-ocean ridge systems)
- can also get continental divergence (rift valley)

36
Q

Convergent plate interaction and its 3 types

A

plates collide and one moves underneath the other
- Ocean to ocean convergence = Trench, Island arc systems
- Ocean to continent convergence = Trench, Volcanoes
- Continent to continent convergence = Mountains, Earthquakes

37
Q

Transform plate interaction

A

plates move aside each other

38
Q

what are mantle plumes

A

continent-sized columns of superheated mantle e.g. Deccan Traps, India; Pacific Northwest
- remain relatively stationary under moving plates

39
Q

what are Hotspots

A

relatively narrow plumes of magma e.g. Hawai’i; Yellowstone
- remain relatively stationary under moving plates

40
Q

what happens when an oceanic plate moves over a hot spot

A

Formation of a volcanic island chain