Tectonics :) Flashcards

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1
Q

What is the lithosphere

A

the rigid outer part of the earth, consisting of the crust and upper mantle.

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2
Q

What is the asthenosphere

A

the upper layer of the earth’s mantle, below the lithosphere, in which there is relatively low resistance to plastic flow and convection is thought to occur

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3
Q

What are convection currents

A

Convection currents describe the rising, spreading, and sinking of gas, liquid, or molten material caused by the application of heat. They move the tectonic plates

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4
Q

Describe the structure of the earths layers

A

The earth is made up of three different layers: the crust, the mantle and the outer and inner core

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5
Q

Describe the different crusts

A
  • Oceanic crust
    (5-10km thick, dense)
  • Continental crust
    (20-70km thick, less dense)
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6
Q

Describe what the mantle is

A

the region of the earth’s interior between the crust and the core, believed to consist of hot, dense silicate rocks

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7
Q

Describe what the inner and outer cores are like.

A

The inner core is under intense pressure, which keeps it solid despite high temperatures. Outer Core. The outer core, which is liquid, is about 1300 miles (2092 km) thick.

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8
Q

What are the three different types of plate boundary?

A
  • Destructive
    (plates moving into each other) (volcano)
  • Conservative
    (slipping past each other) (faults)
  • Divergent
    (moving away from each other) (rift valleys)
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9
Q

Explain what a rift valley is

A

A rift valley is a lowland region that forms where Earth’s tectonic plates move apart

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10
Q

What is a subduction zone

A

a region in which a portion of a tectonic plate sinks beneath another plate into the Earth’s interior. oceanic under continental

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11
Q

what is slab pull

A

the force due to the weight of the cold, dense sinking tectonic plate. helps pull down the oceanic plate under the continental plate

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12
Q

What is ridge push

A

magma rises as the plates move apart. The magma cools to form new plate material. As it cools It becomes denser and slides down away from the ridge. This causes other plates to move away from each other.

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13
Q

what is palaeomagnetism

A

Palaeomagnetism is the study of the Earth’s magnetic field preserved in rocks. The discovery that some minerals, at the time of their formation, can become magnetised parallel to the Earth’s magnetic field

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14
Q

What is the evidence for plate tectonics

A
  • South America and Africa would fit nicely together
    -Fossils of animals on one continent found on another continent (mesosaurus)
  • Coal found in Antarctica and UK (can only be made in tropical conditions)
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15
Q

describe the distribution of earthquakes and volcanos

A

tend to follow patterns around the plate boundaries apart from hotspots like Hawaii.

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16
Q

How do we measure earthquakes

A

with seismograph and with the richter scale (1-10)

17
Q

how do we measure volcanos

A

with the volcanic explosivity index (VEI)

18
Q

What are the primary effects of earthquakes

A

Primary effects of an earthquake can include the ground shaking, buildings collapsing, and the ground splitting

19
Q

What are the secondary effects of an earthquake

A

ground settlement, lateral ground displacement, liquefaction, landslides and rock falls, tsunamis, floods, fires and falling debris.

20
Q

describe liquefaction

A

Liquefaction takes place when loosely packed, water-logged sediments at or near the ground surface lose their strength in response to strong ground shaking. The buildings tend to sink/collapse

21
Q

What are the different types of volcano

A
  • composite
    (The lava of a composite volcano is acidic and is of high viscosity, calmer)
  • shield
    (The basaltic lava of a shield volcano is runny and is of low viscosity, violent)
  • cinder cones
    (violent lava)
  • lava domes
    (viscous lava calmer)
22
Q

Primary effects of volcanic eruptions

A

Pyroclastic Flows, Lava Flows, Volcanic Bombs and Tephra, Lahars

23
Q

secondary effect of volcanic eruptions

A

Widespread ash-fall or gas impact (acid rain) may lead to agricultural hardships including crop failure, loss of livestock and contamination of water supplies which, in turn, may trigger famine and related diseases.

24
Q

what is a lahar

A

A lahar is a destructive mudflow or debris flow composed of a mixture of volcanic ash, rocks, and water.

25
Q

what is a volcanic bomb and tephra

A

volcanos eject large rocks, called volcanic bombs, along with smaller rock fragments, ash, and dust, known as tephra

26
Q

why do volcanos erupt

A

Deep within the Earth, it is so hot that some rocks slowly melt and become a thick flowing substance called magma. Since it is lighter than the solid rock around it, magma rises and collects in magma chambers. Eventually, some of the magma pushes through vents and fissures to the Earth’s surface

27
Q

how can we predict tectonic hazards

A
  • Seismic activity (seismograph)
  • Seismic hazard zoning (understanding and mapping areas vulnerable from previous events)
  • Earthquake precursors (signs/patterns observed before an earthquake, foreshocks, animal behaviour)
  • Volcanic monitoring (gas emission measurements, ground deformation studies)
28
Q

How can we mitigate tectonic hazards

A
  • land-use planning (restricting development in high-risk zones, promoting safer construction practices)
  • building design and retrofitting (earthquake-resistant buildings, reinforced foundations and shock-absorbing materials)
  • Early warning systems (alerts to the population)
  • Education (educate people on the matter)
29
Q

How can we monitor tectonic hazards

A
  • global monitoring networks (networks of monitoring facilities providing real-time data on tectonic activity)
  • Remote sensing (satellite imagery and aerial surveys)
  • Seismic monitoring
  • volcano monitoring techniques (gas sampling, thermal imaging, ground temperature measurements)