Tectonics Flashcards

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1
Q

What is a natural hazard?

A

A natural hazard is an event that threatens people or has the potential to cause damage, destruction and death.

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2
Q

If an HIC is impacted it will cope better because:

A
  • government stable + democratic + has agencies to help in emergencies
  • technology can predict events e.g USA has USGs. Technology can protect buildings.
  • Planning laws prevent buildings in dangerous areas
  • Agencies that can act quickly to help an area e.g army, fire crew
  • Better education
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3
Q

What are the 4 layers of the earth (inside to out)?

A
  1. Inner core
  2. Outer core
  3. Mantle
  4. Crust
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4
Q

What are convection currents?

A

They take place in the mantle where the hot core causes magma to rise in the mantle and sink back down to the core when it cools. Convection builds pressure and carries the plates with it.

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5
Q

What is slab pull?

A

The denser plate sinks back into the mantle under the influence of gravity. It pulls the rest of the plate along behind it.

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6
Q

What is ridge push?

A

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

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7
Q

What is continental drift?

A

The movement between land/continents.

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8
Q

What is the proof for continental drift?

A

The apparent fit of continents, the correlation of fossils on earth, the rock and rock type correlation, paleoclimate data.

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9
Q

Which boundary type is divergent?

A

Constructive

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10
Q

Which boundary types are conservative?

A

sideways or transform

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11
Q

Which boundary types are convergent?

A

Destructive or collision

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12
Q

Describe a destructive plate boundary:

A

It is found where convection currents push a continental plate and oceanic plate towards each other. The oceanic plates subducts under the continental because it is denser. Where two plates intersect a deep trench forms. Earthquakes occur at varying depths along the subduction zone where the lates stick and pressure builds up. When the plate has descended below 100km it starts to melt due to rising temperature and pressure as it moves into the mantle. The magma is now less dense than the surrounding rock and rises through the gaps in the continental plate. Most of the molten rock cools and solidifies in huge sponge-like magma chambers far below the Earth’s surface. If it reaches the surface, there is an explosive eruption of gases, ash and lava.

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13
Q

Describe a constructive plate boundary:

A

It is found where two plates move apart and a new crust is formed at the boundary. The plates are being pulled apart through convection currents. Initially rift valleys form on sea floor. Magma rises from the mantle to fill the gap between the separating plates forming submarine volcanoes which in time may grow above sea level. A midge ocean ridge develops at this point. As the basaltic magma cools it adds new land to separating plates.

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14
Q

Describe a conservative plate boundary:

A

They occur where two plates move parallel or nearly parallel to each other. Crustal roc are neither created or destroyed here. The boundary between the plates is characterised by pronounced transform faults. As the plates move past each other they stick building pressure. Suddenly when there is a release of pressure the plate jerks forward and energy is released in the form of seismic waves causing an earthquake.

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15
Q

Describe a collision plate boundary:

A

Two continental plates move towards each other and collide. Neither plate can be created or destroyed here so they are forced upwards or downwards. The upwards section makes fold mountains and the downwards section makes mountain roots. There are high magnitude earthquakes at collision plate boundaries because of the massive build up of friction and pressure. However no plate is being destroyed. magma is not created, so no volcano formed.

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16
Q

Example of destructive plate boundary:

A

Nazca plate subducts under south American

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17
Q

Example of constructive plate boundary:

A

Atlantic sea floor is spreading where North American and Eurasian plates moving apart.
Or
Surtsey, south of Iceland

18
Q

Example of conservative plate boundary:

A

The San Andreas fault in California.

19
Q

Example of collision plate boundary:

A

Himalayas

20
Q

What is magma and what is lava

A

Molten rock underground and Magma that reaches the surface

21
Q

What is the name to the rock which is formed from cooled lava?

A

Igneous

22
Q

What type of rock is basalt?

A

Found at shield volcano
Formed from lava at low viscosity
No holes - heavier rock

23
Q

What type of rock is Pumice/Scoria?

A

Found at composite volcanoes
Formed from lava with high viscosity
Lots of holes - light rock

24
Q

Describe composite volcano:

A

Lava is viscous and sticky
Formed at destructive/compressional plate boundary
Explosive
Lava doesn’t travel very far - sticky
Shape of volcano is steep

25
Q

Describe a shield volcano:

A

Lava is not viscous
Formed at constructive plate boundary
Non explosive
Lava can travel a long distance
Shape of volcano is gently sloping sides

26
Q

What is Lahar:

A

These are a mixture of volcanic ash rocks and other debris mixed with either hot or cold water. They can destroy whole towns and many move too fast for people to out run.

27
Q

What is tephra:

A

This is anything blown out of the volcano into the air. It can vary in size from tiny ash particles to chunks of rock the size of cars.

28
Q

What is a land slide:

A

A section of the volcano slides/falls down the side of the mountain

29
Q

What is Jokulhlaup:

A

A glacial outburst, when a glacier that is on top of a volcano melts due to a volcanic eruption

30
Q

What are primary impacts:

A

Immediate impacts from tectonic hazards

31
Q

What are secondary impacts:

A

Impacts which happens later on often as a result of the primary effects

32
Q

Examples of primary impacts:

A
  • People are injured and killed by collapsed buildings or pyroclastic flows
  • Infrastructure such as water, gas, and electricity cables are broken
  • Roads, railways, airports are damaged
  • Leaking gas can be ignited causing fires
33
Q

Examples of secondary impacts:

A
  • People left homeless can die from exposure
  • Tourists put off/unable to visit area
  • Blocked transport
  • Repairs and construction can be expensive so can weaken country’s economy
  • Shortage of clean water and lack of sanitation can spread diseases
  • Businesses reduced and unemployment increases, money spent repairing damage so economy slows
34
Q

How do earthquakes happen:

A

Earthquakes occur on all 4 types of plate boundaries. They occur when two plates try to slip past each other in different directions. The plates do not always move smoothly alongside each other and mat stick. The rocks are put under a great deal of stress and often bend. When this happens pressure builds up. Eventually when the stress is too great, the rock suddenly snap back across the fault line and tension is released from inside the crust. Energy in the form of seismic waves radiates out in all directions, causing the ground to shake The point inside the crust where the pressure is released is called the FOCUS. The point on the Earth’s surface above the focus is called the epicentre. The waves are felt most strongly at the epicentre, becoming less strong as they travel further away.

35
Q

What does the Mercalli scale measure?

A

The amount of damage = gives the indication of intensity of earthquake. Refers to effects on humans, buildings, landscapes.

36
Q

What does the Richter scale measure?

A

The measurements of the earthquake waves from instruments e.g seismographs

37
Q

The closer the waves are to the focus…

A

the more energy they have and the bigger the magnitude they are

38
Q

Reasons why people still live at risk of tectonic hazards:

A
  • Job opportunities
  • Tourism
  • Fertile soil
  • Can’t afford to move
  • Chances of hazard very slim
  • Cheap geothermal power
  • Places well prepared
  • Minerals are rich
39
Q

4 ways tectonic hazards can be managed:

A

Monitoring
Prediction
Planning/Prevention
Protection

40
Q

What are pyroclastic flows

A

Mixtures of hot, dry ash, rock and gas from volcanic eruptions. They travel at about 80km per hour and range from 200-700 degrees Celsius.