tropical cyclones, volcanic eruptions, earthquakes Flashcards

1
Q

conditions tropical cyclones

A
  • deep layer of humid, warm (>27°c), and unstable air
  • supply of energy (heat moisture) from sea surface
  • circulatory motion of air, anti-clockwise in northern hemisphere, encouraged by coriolis force
    -wind shear encourages circulatory motion
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2
Q

What is a hotspot and what happens at it?

A
  • hotspots are locations beneath the earth’s crust where strong and rising currents of magma (known as plumes) occur
  • where the crust above a plume is weak, volcanic activity occurs, e.g. hawaiian islands
  • this also happens away from the edge of a plate boundary as there is a weakness in the crust
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3
Q

describe how tectonic plates cause movement in plate boundaries?

A
  • tectonic plates move due to convection currents in the earth’s mantle, caused by heat from core.
  • constructive boundaries : plates move apart, allowing magma to rise, form new crust
  • destructive boundaries : oceanic plate forced under continental plate due to subduction, creates earthquakes and volcanoes.
  • conservative boundaries : plates slide past each other causing friction, leading to earthquakes
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4
Q

explain how earthquakes are caused?

A
  • caused by the movement of tectonic plates
  • e.g example, at a conservative plate boundary
    two plates sliding past each other
  • there is neither rising magma here, nor subduction so no volcanoes
  • instead, the friction gives rise to earthquakes
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5
Q

constructive plate boundary:

A

-two plates moving apart, e.g. in oceans
- magma (molten rock) rises to the crust to fill the gap, creates new crust through submarine volcanoes
- happens along the mid-ocean ridge in atlantic ocean

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6
Q

state the similarities and differencesof 2 types of volcanoes

A

shield volcano:
-not as dangerousnot very explosive (but lava flows out)
-low viscosity
-frequent but not big eruptions

composite volcano: (strato)
-dangerous and explosive
-high viscosity
-not as frequent eruption

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7
Q

destructive plate boundary:

A

-two plates moving towards each other, meeting head on
- the edge of one plate margin is being destroyed as it plunges beneath the other plate it is
- this is known as subduction
- molten rocks rise to the surface to form volcanoes
- friction between the two plates creates earthquakes

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8
Q

conservative plate boundary:

A
  • two plates sliding past each other
  • there is neither rising magma here, nor subduction so there are no volcanoes
  • instead, friction gives rise to earthquakes
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9
Q

collision plate boundary:

A
  • two plates meet head on (due of equal density and strength)
  • sediments between two plates are squeezed upwards
  • results in formation of fold mountains
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10
Q

tropical cyclones causes

A

starts when high temperatures cause air to rise from sea
rising air - causes local thunderstorms
small storms come together - create strong flow of warm, rapidly rising air
produces area of increasingly low pressure

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11
Q

what happens at the center (eye)?

A

there is a subsiding air with calm conditions, cloud skies. surrounding the eye is the eye wall where the most destructive energy occurs.

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12
Q
A
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