Tectonic Processes & Hazards Flashcards

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1
Q

What is a Divergent Plate boundary

A

Two plates moving away from each other. They are mostly in the sea & around mid-ocean ridges.

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2
Q

What is a Convergent Plate boundary

A

Where two plates move against each other. These actively form collision locations with plate material subducting into the mantle.

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3
Q

What is a Conservative Plate boundary

A

Where one plates slides against another. Movement is horizontal and lithosphere is neither created nor subducted.

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4
Q

What is the Lithosphere

A

Surface layer of Earth composed of the crust and upper mantle (100km deep on average). The lithosphere is broken into huge sections (tectonic plates)

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5
Q

Zone of Friction

A

As plates slide or move against each other this ‘zone of friction’ is created.

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6
Q

Passive continental margins

A

Where there if no collision or subduction taking place, and therefore tectonic activity is minimal here.

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7
Q

Characteristics of an Active Subduction zone

A

high magmatic activity, a narrow continental shelf with active seismicity.

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8
Q

What will happen between an oceanic plate and continental plate converging towards each other?

A

The oceanic plate will subduct underneath the oceanic plate creating a ‘subduction zone’ as its denser.

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9
Q

How may surface volcanism form at destructive plate boundaries?

A

volcanoes might appear at the ocean floor of Earth’s surface, typically appearing above the magma that forms directly above down-thrust plates.

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10
Q

What will happen between two continental plates converging towards each other?

A

Both plates move upwards creating ‘fold mountains’ such as the Himalayas.

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11
Q

What is a rift volcano

A

Created by two plates diverging from each other at the site of a mic-ocean ridge commonly. They tend to be less explosive and more effusive especially when in deep ocean.

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12
Q

What is a hotspot volcano

A

found away from boundaries of volcanoes but are fed by underlying mantle plumes that are unusually hot comparing with the surrounding mantle. (e.g. Hawaii).

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13
Q

Define the aesthenosphere

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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14
Q

What type of rocks generally make up oceanic and continental crusts?

A

continental crusts commonly are made up of granite, and oceanic crusts are primarily compose basalt.

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15
Q

What from the Earth’s core drives the creation of convection currents?

A

Radioactive decay in the core.

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16
Q

Seafloor spreading

A

The continuous input of magma at divergent plate boundaries, creating new crust. This commonly happens in mid-ocean ridges.

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17
Q

Rift Valleys

A

Two continental plates moving apart resulting in the reconstruction of paleomagnetic reversals. (palaeomagnetism)

18
Q

Define Palaeomagnetism

A

results from the zone of magma ‘locking in’ the Earth’s magnetic polarity when it cools. Scientists can use this tool to determine historic periods of tectonic activity through reconstructing relative plate motions.

19
Q

Define a subduction zone

A

where two plates moving together (one oceanic and the other continental) have differing density making the oceanic plate slide underneath. This destroys crust as it melts.

20
Q

What is a locked fault

A

Enormous stress built up and can be held for hundreds of years. This may lead up to severely high magnitude Earthquakes.

21
Q

Define a Benioff zone

A

area of seismicity corresponding with the slab being thrust downwards in the subduction zone.

22
Q

What is the hypocentre

A

Focus point within the ground where the strain energy of the earthquake stored in the rock is first released.

23
Q

What is the focal length

A

The distance between the epicentre on the surface and the hypocentre.

24
Q

Define a fault

A

A fracture in the rocks that makes up the Earth’s crust.

25
Q

What is a Primary Wave

A

vibrations caused by compression. They spread quickly from the fault at a rate around 8km/s.

26
Q

What is a Secondary Wave

A

Waves that move more slowly around 4km/s. They vibrate at right angle to the direction of travel and cannot go through liquids (unlike P waves).

27
Q

What is a Love Wave

A

Surface waves (restricted to horizontal movement), with a high amplitude. These are also the slowest wave type.

28
Q

Define lateral spreading

A

land adjacent to any sloping land sliding under low-friction conditions across a liquefied soil layer.

29
Q

Soil liquefication

A

Water-saturated material can temporarily lose normal strength and behave liquid-like under the pressure of strong shaking.

30
Q

Epicentre

A

The location on the Earth’s surface that is directly above the Earthquake focus.

31
Q

tsunami

A

initiated by earthquakes, landslides, and sometimes volcanic eruptions.

32
Q

How fast can tsunamis travel?

A

up to 600km in deep water

33
Q

What are the properties of tsunami waves

A

In deep water tsunami waves are not very noticeable, until they reach more shallow waters to rise on average 0.5-5m in height.

34
Q

Define a Pyroclastic Flow

A

frothing of molten magma in the vent of the volcano. The bubbles burst explosively to eject hot gases and pyroclastic material, which contains glass shards, crystals, and ash etc. They can be up to 1000C.

35
Q

Define a Tephra

A

When a volcano ejects material such as rock fragments into the atmosphere. It may vary in size from ‘bombs (>32mm in diameter), to fine dust (<4mm).

36
Q

What determines the threat of a Lava flow

A

The viscosity of the lava is determined by the amount of silicon dioxide it contains. On steep slopes some lava flows can reach 15m/s.

37
Q

Volcanic Gases

A

Gases are associated with explosive eruptions and lava flows. The mix normally includes water vapour, sulphur dioxide, hydrogen and carbon dioxide.

38
Q

What makes volcanic gases extremely dangerous (c02)

A

C02 is colourless and odourless, and when it accumulates in valleys undetected, it has caused high levels of deaths.

39
Q

Lahars

A

volcanic mudflows generally composed of fine sand and silt material. The degree of hazard varies depending on the steepness of slopes., volume of material, and particle size.

40
Q

How may lahars be associated with secondary hazards

A

As a secondary hazard they can be associated with heavy rainfall as old tephra deposits on steep slopes can be re-mobilised into mudflows.

41
Q

Jökulhlaups

A

Glacial outburst triggered from a volcanic eruption due to land alterations or the temperature creating a dramatic release of liquid.