Geo - Tectonic plates Flashcards

(44 cards)

1
Q

tectonic plates

A
  • large slabs of solid rock that floats on the mantle
  • constantly move
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2
Q

layers of the earth

A
  1. crust
  2. mantle
  3. outer core
  4. inner core
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3
Q

crust

A
  • a layer of sand and rock
  • 5-50km thick
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4
Q

mantle

A
  • 2850km thick
  • reaches about half distance to the center of the earth
  • hot enough to liquify and become slow moving molten rock or magma
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5
Q

outer core

A
  • mass of molten iron
  • 2200km thick
  • surround the solid inner core
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6
Q

inner core

A
  • mass of iron
  • 3870oC
  • iron melts at this temp but immense pressure keeps it solid
  • 2400km in diameter
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7
Q

movement of plates

A

convection currents

core heats rock in mantle => hot semi-molten rock becomes less dense than its surrounding and rises => semi-molten rock reaches the crust above => semi-molten rock spreads out carrying the plates above it (conveyor belt) => semi-molten rock cools and sinks back down to be re-heated

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8
Q

2 types of crusts

A
  1. oceanic crust
  2. continental crust
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9
Q

oceanic crust

A
  • 6km (4 miles) thick
  • 200 million years old
  • made of basalt
  • density: 3g/cm
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10
Q

continental crust

A
  • 6 to 47 miles in thickness depending on location
  • 1 to 4 billion years old
  • made of granite
  • density: 2.6g/cm
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11
Q

where do earthquakes happen

A
  • margins / boundaries of tectonic plates
  • pacific ring of fire
  • hotspots (areas under the crust where magma is hotter than surrounding magma)
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12
Q

pacific ring of fire

A
  • string of tectonic activity
  • 90% of all earthquakes
  • 75% of all active volcanoes on Earth
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13
Q

4 types of plates boundaries / margins

A
  1. constructive boundaries
  2. conservative boundaries
  3. destructive boundaries
  4. destructive boundaries - collision zones
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14
Q

constructive boundaries

A

plates are moving apart (convection currents) => magma rises from the mantle => magma erupts to surface of earth (accompanied by earthquakes) => magma reaches the surface and cools => solidifies to form new crust of igneous rock => repeated

  • new rocks builds up to form a volcano
  • constructive boundaries tend to be found under the sea, eg. mid Atlantic
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15
Q

conservative plate boundary

A

slide in opposite direction / same direction different speed => plates move and create friction and get stuck => pressure builds => pressure releases and sends out huge amounts of energy => causes earthquake

  • earthquakes on conservative plates can be destructive bec occurs to earths surface
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16
Q

destructive boundaries

A
  • oceanic plate and continental plate

o.p and c.p collide => o.p forced beneath the c.p (subduction) => results in ocean trench => plate sinks into mantle and melts into magma => pressure builds up beneath earth surface => magma escapes thru weaknesses in rock and rises up thru a composition volcano (stratovolcano)

  • volcanic eruptions are often violent with steam, gas and ash
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17
Q

destructive boundaries - collision boundaries

A

2 continental plates collide => weigh the same so both are forced up => forms fold mountains

  • can be very powerful and destructive
  • landslides can be triggered by earthquakes
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18
Q

how are volcanoes formed

A
  • rupture in the crust of the earths
  • allows hot lava, volcanic ash and gases to escape from a magma chamber below the surface
  • volcanoes are most found where tectonic plates are diverging / converging and most are underwater
19
Q

main features of a volcanoes

A
  • ash cloud
  • pyroclastic flow
  • crater
  • main vent
  • lava flow
  • magma chamber
  • secondary vent
  • secondary cone
  • volcanic bombs
20
Q

2 types of volcanoes

A
  1. composite volcanoes
  2. shield volcanoes
21
Q

composite volcanoes

A
  • found at destructive plate margins
  • steep sides
  • made up of alternate layers of ash and lava
  • doesn’t flow far, sticky acidic lava
  • eruptions can be violent
22
Q

shield volcanoes

A
  • constructive plate margins
  • wide base
  • gentle sloping sides
  • lava is runny, flows a long way, basic (opposite acidic)
  • frequent eruptions
  • not violent
23
Q

why do people live near volcanoes

A
  1. geothermal energy
  2. tourism
  3. mining
  4. farming
24
Q

geothermal energy - volcanoes

A
  • energy created by using steam from underground
  • steam drives turbines in stations
  • energy for domestic and industrial use.
  • cheap and environmentally friendly
25
tourism - volcanoes
- scenery attracts tourists - creates many jobs for local people (tour guides, restaurants, hotel, gifts shops)
26
mining - volcanoes
- brings earths riches to the surfaces - minerals in lava underground can be mined when cooled (gold silver, diamonds, copper, zinc) - can be dangerous to work in
27
farming - volcanoes
- soil is mineral-rich and fertile - ideal for farming - will produce healthy crops and high yield harvests soil naturally contains - potash - nitrogen - sulphur
28
causes of earthquakes
- movement of the tectonic plates - seismic waves (shock waves like ripples on a pond) - more damage occurs near the epicenter (directly above the focus)
29
how do earthquakes happen
plates are constantly moving => friction the plates become stuck => pressure builds => pressure release and sends huge amounts of energy => earths surface shake violently (earthquake)
30
how are earthquakes measured
seismometers
31
seismometers
- detects seismic waves - recorded by a series of zig-zags - can determine time, location and intensity of an earthquake
32
Richter scale
- measures the magnitude of a tremor - scale of 1 to 10
33
factors of how severely a country is impacted
1. geographical location 2. level of development - predict / prepare for hazards 3. magnitude - scale of the hazard 4. natural factor 5. population distribution - lower no of deaths 6. time 7. education - allow more people to survive 8. frequency - how often hazard occurs
34
how do countries reduce the impacts of an earthquakes
3 P's 1. prediction 2. protection 3. preparation
35
prediction - 3 p's
- use of seismometers - can predict where and when they will happen
36
protection - 3 p's
- building adjustments - rubber shock absorbers - steel frames - assembly area - lightweight roof - safety glass
37
preparation - 3 p's
- earthquake drills
38
montserrat
location: the Caribbean area: 12km - 8km population: 11000 capital: Plymouth tectonic plates: Caribbean and north American plates, destructive plates volcano: Soufriere hills volcano, composite
39
cause of eruption - Montserrat
destructive plates ... oceanic plate and continental plate
40
info about eruption - montserrat
- began 18 July 1995 - Plymouth was evacuated bec pyroclastic flows and mudflows began occurring - built a huge lava dome, lava was sticky and couldn't flow - lava dome became unstable and collapsed - hot fast moving avalanches of lava blocks, gas and dust - pyroclastic flow travelled down mosquito ghaut - pyroclastic flow couldnt be controlled by the ghaut and spilled out of it - killed 19 people, several others were burned
41
primary effects - montserrat
- 2/3 island was covered in ash - couldnt aid to people - ash polluted the air - over populated the evacuation place - forest fires & tsunamis caused by pyroclastic flow made more damage - only airport was closed - poor sanitation
42
secondary effects- montserrat
- eruption destroyed two main industries; tourism and farming - ash covered field killed crops - farmers had no income - vegetation was destroyed by acid rain - polluted lakes and rivers, animal life almost impossible - population decreased, making it difficult for the country to recover (11,000 ppl to 4,000)
43
immediate / long term responses- montserrat
- MVO (montserrat volcano observatory) was set up to monitor the volcano / predict eruptions - scientists prevented progression in island for they believed another eruptions would have wiped out the whole island (no investment went to waste) - risk map was devised to show residents where it was safe on the island - 41 million dollars will donated by the British government to help the nation rebuild the island - 24 thousand was given to individual families as financial aid
44
why do people still live near the montserrat
- adventure tourism => tourists visit ruins and towns which are still buried in ash - geothermal energy => plans to increase geothermal energy - volcanic sand => exports sand for construction - beaches => distinctive 'black sand' - poverty => no income to move countries