tectonics Flashcards

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1
Q

where is there a constructive and collision plate boundary

A

between India and Australia

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2
Q

where is a transform plate boundary present

A

At New Zealand

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3
Q

what is the Benioff zone

A

A dipping flat zone where earthquakes are produced by the interaction of a down going oceanic crustal plate with a continental plate.

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4
Q

what is the subduction zone

A

the place where two lithospheric plates come together, one riding over the other. Most volcanoes on land occur parallel to and inland from the boundary between two plates

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5
Q

whats crustal fracturing

A

occurs when the Earths crust causes rock to break and fracture under stress and strain caused by seismic waves.

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6
Q

what are constructive/ divergent plate boundaries

A

where plates move apart from each other

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7
Q

what are destructive / convergent plate boundaries

A

where lithospheric plate boundaries move together

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8
Q

where are the majority of earthquakes and volcanoes found

A

on plate boundaries

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9
Q

where do we find Earthquakes with a magnitude of 9 or higher

A

where convergence of a oceanic plate and continental plate occurs (a destructive plate boundary with subduction)

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10
Q

what are earthquakes called in the middle of plates

A

intra-plate earthquakes

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11
Q

why do intra-plates earthquakes occur

A

They are associated with ancient faults (such as the Rhine Rift Valley) in which the solid crust can crack.
Large faults then may turn into new plate boundaries.

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12
Q

why do we find earthquakes at collision boundaries *

A

collisions of tectonic plates may also fracture the crust well away from the plate boundary which can yield large magnitude earthquakes.

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13
Q

what are hot spots?

A

volcanic activity near the centre of some plates.

This is either the result of the upwelling of hot molten material from the core/mantle boundary, such as the Hawaiian hotspots or may result from the top of a large mantle plume just under the crust such as seen in the Cape Verde Islands. It is also possible that large meteorite impacts create symmetrical hot spots on opposite sides of the planet when they collide with the Earth.

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14
Q

where are hotspots found

A

-Hawaii
-Cape Verde islands

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15
Q

what is convection

A

convection is created in the mantle by heat radiating outwards from the inner core

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16
Q

how is the internal structure of the Earth known

A

the internal structure of the earth is known based around how the different earthquake (seismic) waves travel through the solid and liquid layers of the Earth.

seismic waves revealed that there are complicated patterns of hot and cold areas

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17
Q

what is the mantle mostly made from

A

made mostly from peridotite which behaves like a viscous liquid under pressure.

consists of multiple layers with density and mineral differences

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18
Q

describe slab pull

A

slab pull is where denser oceanic plates are subducted at cold downwelling’s (there is also some suction force).

This subduction may cause the location of cooler mantle areas and the downward movement within the large scale convection pattern

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19
Q

why does the pacific plate move faster than the other plates

A

The Pacific plate has lots of subduction around its edge

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20
Q

how can plumes impact a countries location

A

they can push the crust up on a large scale.

The one currently under West Africa may have also caused the Atlantic Ocean and Iceland to form with the creation of mid Atlantic ridge, and split Scotland from North America and Africa from South America.

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21
Q

for the crust what is the:

-Structure
-Temperature
-Density
-Composition
-Physical state
-Seismic waves present

A

-Structure: oceanic= 7km thick, continental= 70 km thick

-Temperature: oceanic= 400 degrees C
-Density: oceanic= 3.3g/cm^3, continental= 2.7
-Composition: oceanic= basalt continental= granite
-Physical state: solid
-Seismic waves present: surface and body waves able to pass through

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22
Q

for the mantle what is the:

-Structure
-Temperature
-Density
-Composition
-Physical state
-Seismic waves present

A

-Structure: 700km to 2890km deep

-Temperature: 870 degrees c

-Density: 3.3-5.4 g/cm3

-Composition: peridotite, upper=olivine lower=magnesium silicate

-Physical state: phases of liquid and solid in layers

-Seismic waves present: body waves (both p and s) pass through at variable rates due to density changes.

23
Q

for the outer core what is the:

-Structure
-Temperature
-Density
-Composition
-Physical state
-Seismic waves present

A

-Structure: 2890km to 5150 km deep

-Temperature: 4400 to 6100 degrees c

-Density: 9.9 to 12.3 g/cm3

-Composition: 12% sulphur, 88% iron

-Physical state: liquid (+ generates a magnetic field)

-Seismic waves present: only p waves able to pass through, an S wave ‘shadow zone’ is created from about 105 degrees from the focal point

24
Q

for the inner core what is the:

-Structure
-Temperature
-Density
-Composition
-Physical state
-Seismic waves present

A

-Structure: 5150 km deep to centre

-Temperature: 7000 degrees c (radioactive decay)

-Density: 13.5 g/cm^3 (v dense)

-Composition: 20% nickel 80% iron

-Physical state: solid (+radiates heat)

-Seismic waves present: only P waves, their refraction at the core mantle boundary creates a ring ‘shadow zone between 105 and 140 degrees from the focal point

25
Q

what is a constructive/ divergent plate boundary

A

where two oceanic plates move apart.

sea floor spreading

convection in mantle occurs

26
Q

for the plate boundary type of constructive (divergent), what is the:

-seismic activity
-volcanic activity
-topography or bathymetry

A

-seismic activity: shallow focus; usually low magnitude (5-6)

-volcanic activity: effusive (not very explosive) eruptions, low VEI scale (1-3)

-topography or bathymetry: ocean ridge with central rift valley: faulting at right angles; volcanic isalnds

27
Q

for the plate boundary type of destructive (convergent) ocean and continent, what is the:

-seismic activity
-volcanic activity
-topography or bathymetry

A

-seismic activity: range of focal depths from 700km along the wadati-benioff zone: often high magnitude (8-9)

-volcanic activity: explosive (moderate to high VEI scale 5-6)

-topography or bathymetry: Island arc; oceanic trench; back arc and fore arc zones

28
Q

for the plate boundary type of destructive (convergent) ocean and ocean, what is the:

-seismic activity
-volcanic activity
-topography or bathymetry

A

-seismic activity: range of focal depths from shallow to 700km along Wadati Benioff zone: moderate to high magnitude

-volcanic activity: explosive (moderate to high VEI scale 5-6)

-topography or bathymetry: island arc; oceanic trench; back arc and forearc zones

29
Q

for the plate boundary type of Collison (convergent) continent and continent, what is the:

-seismic activity
-volcanic activity
-topography or bathymetry

A

-seismic activity: shallow to intermediate focal depth, moderate magnitude (6-8)

-volcanic activity: usually none

-topography or bathymetry: fold mountains and plateaus

30
Q

for the plate boundary type of transform (conservative), what is the:

-seismic activity
-volcanic activity
-topography or bathymetry

A

-seismic activity: shallow focus, usually moderate magnitude (6-8)

-volcanic activity: usually none, occasional fissure eruptions

-topography or bathymetry: ridges or scars on surface

31
Q

how do fossils confirm that tectonic plates move

A

places such Africa and South America have matching rock types. Fossils such as Cynognathus match across africa and south America

32
Q

how did evidence supporting the study of seismic waves and the location of focal points in the 1950s confirm that tectonic plates move

A

in 1950s the ocean floor was surveyed showing the presence of mid ocean ridges where new crusts were formed.

33
Q

how did evidence from The discovery in the 1960s of magnetic strips in the oceanic crust confirm that tectonic plates move

A

these palaemagnetic signals from past reversals of the Earth’s magnetic field and prove that new ocean crust is created by the process of sea-floor spreading at mid-ocean ridges. (seafloor spreading and palaeomagnetism occur at constructive margins, where new crust is being made)

34
Q

how does coal confirm that tectonic plates move

A

coal forms in tropical conditions however coal is found in the north sea

35
Q

where do we find the greatest friction and what is an example

A

at the wadati benioff zone within destructive plate boundaries.

due to this friction, there was a 9.5Mw earthquake in Chile, being the largest

36
Q

give an example of a transform (conservative) boundary where the highest level of stress is found

A

the San Andreas fault line created the largest earthquake at 7.6Mw for a conservative plate boundary

37
Q

what is the focus of an earthquake

A

the focus of an earthquake is where the stress is released, this sends earthquake (seismic ) waves in all directions, being strongest at the point above the focus which is the epicentre.

38
Q

where are lower magnitudes found

A

at constructive plate boundaries magnitude is lower as less friction is present.
E.g. the largest recent earthquake in Iceland was 6.5Mw in 2000, but they are normally lower

39
Q

what are body waves

A

both P and S waves

40
Q

-primary waves-

how fast are they:

what does it move through:

how destructive is the wave:

A

how fast are they: fastest type of wave, they arrive first

what does it move through: moves through solid rock and fluids. P waves are only able to move through the inner and outer core (not body waves)

how destructive is the wave: they are only damaging in the most powerful earthquakes

41
Q

-secondary waves-

how fast are they:

what does it move through:

how destructive is the wave:

A

how fast are they: slower than a P wave (travel 60% slower than a P wave)

what does it move through: they only travel through solids. Body waves are seen at both the mantle and the crust

how destructive is the wave: They do more damage than P waves

42
Q

-rayleigh waves-

how fast are they:

what does it move through:

how destructive is the wave:

A

how fast are they: 7800 miles per hour

what does it move through: only travels through the surface or crust

how destructive is the wave: responsible for most of the shaking felt by people

43
Q

-love waves-

how fast are they:

what does it move through:

how destructive is the wave:

A

how fast are they: slowest (last to arrive)

what does it move through: only travels through the surface of the crust

how destructive is the wave: cause the most damage

44
Q

In what way do primary waves move

A

primary waves push and pull in the direction of travel

45
Q

In what way do secondary waves move

A

secondary waves consist of an up and down movement

46
Q

what does magnitude measure

A

magnitude measures the amount of energy released at the epicentre

47
Q

how is earthquake magnitude measured

A

earthquake magnitude is measured using the moment magnitude scale (MMS)

MMS measures the energy released during an earthquake, it uses a logarithmic scale

48
Q

what does an earthquakes intensity measure

A

an earthquakes intensity is the effect on people, structures and the natural environment

49
Q

how is earthquake intensity meaured

A

by using the modified marcalli intensity scale which takes observations from people who experienced the earthquake

50
Q

what are the primary effects (direct results) of an earthquake

A

ground shaking- causes buildings, bridges, roads and infrastructure to collapse, killing or injuring those nearby

crustal fracturing- when energy is released during an earthquake causes the Earths crust to crack -leaving gaps

51
Q

what are the secondary effects of an earthquake

A

liquefaction- the violent shaking during an earthquake causes surface rocks to lose strength and become more liquid than solid. The subsoil loses its ability to support buildings. It can make rescue efforts more difficult and also disrupt underground power and gas lines.

landslides and avalanches- The ground shaking places stress on slopes, so they may fail (landslides, rockslides, mudslides and avalanches). This can lead to damage and injuries

tsunami- some underwater earthquakes generate tsunami that cause major problems for costal areas.

52
Q

what are landslides

A

landslides are where material loses cohesive strength and moves downwards under the influence of gravity- they occur when seismic waves loose shock

53
Q

give examples of where landslides have caused devastation

A

El Salvador, Central America