Unit 1 Geography- Restless earth

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  • Created by: jessb2000
  • Created on: 26-11-16 18:49

Tectonic plates


Convergant- When two plates collide- Oceanic will always go under- Eurasian and pacific

Divergant- when two plates are pulled apart- South American and African plate

Collision- when two continents collide- indo-Australian and Eurasian plate

Transform- Two plates slide past each other- Pacific plate and south American plate

Constructiv PB- Where two plates pull apart

Destructive PB- Where two different plates collide

Collision PB- Where two continental plates collide

Conservative PB- where two plates slide past each other

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Types of plate boundaries

Lithosphere- underside of the crust

Constructive- Where two plates rip apart

Destructive- Where two different plates collide

Collision- where two continental plates collide

Conservative- Where two plates slide past each other

Submarine Volcanoes- Underwater Eruptions

Ocean ridge- Raised seabeds pushed up by magma

Volcanic island- islands of volcanic origin

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East African Rift Valley- Continental division

  • A rising convection current creates a hot spot below the continental crust which weakens it causing the plates to diverge causing the land to split apart
  • As the continental crust splits the land begings to sink which forms a Rift Valley which has active volcanoes throughtout the length of the rift valley.
  • The rift valley can collect water which can form giant lakes or flooding with sea water (only if near the coast)
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Lava key terms

Lava lake- lava lakes are large volumes of molten lava which is usually basaltic and it is contained in a volcanic vent

Lava Pillars- Lava pillars are hollow inside which forms a pipe like channel between the top and the bottom of a lava flow. They are also common within collapsed sheet flow terrian.

Hydrothermal vents- fissure in a planets surface which the geothermal heated water issues. Commonly found near active volacnoes.

Pillow lava- pillow shape lava that has been formed underwater. Volcanic rocks that are characterized by thick sequences of discontinuious pillow shaped masses.

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Composite Volcano

  • Alternating layers of lava and ash
  • Destructive PB
  • 1200 degreese celcius- flows slowly as it is sticky
  • Steep with uneven sides
  • Rave but very violent!
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Shield Volcano

  • Layers of coolded down lava
  • Constructive PB
  • 3000 degreese celcius- flows very fast and is runny
  • low with gentle sloping sides
  • Frequent but not that violent
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Effects of volcanic activity

  • Wildlife deaths& hotsprings- CO2 kills squirrels- CO2+H2O= Carbonic acid, kills trees- sulphur causes 'stink'
  • Inital quake/explosion- Buildings fall, bridges, motroways,power cuts,fires begin,Ash collum, Human panic=injury.
  • Ash Fallout- Rains ash, settled on ground, turns day to night, deadly if breathed in.
  • Volcanic bombs- Destroy anything, cause fires, block roads, kill all species.
  • lava flows- Ignite houses, causes forest fires
  • Lahar and Lahar 2- ash+water= cement, flows like water-takes out bridges
  • Pyroclastic clouds- +300mph, 600 degrees C- Obliterates everything, Species get petrifed (turn to stone)
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Basaltic Lava

  • Constructive PB
  • Very Hot- 1200 Degreese C- runny
  • Low silica content
  • Longer time too cool-flows longer distances
  • Retains its gas
  • Gentle sloping landfomrs
  • Frequent but gentle
  • Lava and steam are ejected
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Andesitic Lava

  • Destructive PB
  • Less hot- 800 degreese C
  • Slow flow
  • High silica content
  • Soon cools- flows very short distances
  • Looses gasses quickly 
  • Viscious
  • Produces steep sides
  • Less frequent- Very violent
  • Ash rocks, gasses, steam and lava are ejected.
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Mt Pinatubo- 1991- Base Details

  • Eurasian and Philippines plate
  • Destructive PB
  • 611 Years dormant
  • Philiappines
  • LEDC
  • Andesitic
  • Oceanic crust
  • Plinian erupition
  • VEI- 6
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Mt Pinatubo- 1991- Effects

Primary

  • Quake and eruption(small)
  • Ash fallout- 50 miles
  • 2am, Main eruption
  • Pyroclastic clouds
  • Ash Collum
  • 20,000,000 tons of sulphur into the atmosphere.

Secondary

  • Darkness
  • Lahar-typhoon rain
  • SO2 reflects suns energy globally 2 degrees C drop in temp for 2 years

Management

  • Helicopter flyby
  • 14,000 evacuated
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Eyjafjallajokull- 2010- Base Details

  • Eurasian and North American plate
  • Contstructive PB
  • 90 years dormant
  • Iceland
  • MEDC
  • Basaltic
  • Core
  • Volcanian eruption/ Strombolian eruption
  • VEI= 4
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Eyjafjallajokull- 2010- Effects

Priamry

  • 3000 micro quakes
  • ash cloud- 17km high into the sky
  • lava flows
  • 7 month eruption

Secondary

  • if there was 3000 micro quakes- causes panic/chaos in the town
  • 17km ash cloud would impact on planes as they would be grounded- cant fly
  • People would inhale ash air- goes into lungs hardens them which would eventull kill them.
  • Six months to repir and get back to normal
  • ash on the road stops cars-emergancy services
  • ash in air causes it to become darker

Management

  • 22 March 2010- evacuation plan in place.
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Monitoring Volcanoes and Quakes- disaster manageme

Disaster event - Emergancy response

  • fire crews, medical staff, rescue team, army support, food supplies, shelter protection

ReliefMend Scars

  • Loss management, support network

Reconstruction-Rebuild

  • learn from mistakes, using modern technologies in construction

MigrationRescue the impact

  • Relocate people away, strengthen structers, planning restrictions

Preparedness-Being ready

  • Governments, Comminuties, individuals
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Sichuan China

  • LEDC
  • 12th May 2008 2:48pm
  • Collision PB
  • 7-7.9 richeter scale

Primary

  • 80% of houses collapsed
  • roads, train lines, factories,landslides, rock slides, schools, hospitals

Secondary

  • 70,000 deaths
  • 19,000 missing people
  • 5 million homeless
  • 245,000 injured
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Sichuan China- Secondary(urban area)/ short and lo

Secondary Effects- Urban Area

  • No work, landslides
  • Toxic clouds from factories
  • Rivers blocked, resures couldnt get anywhere
  • roads blocks- people slept in streets.

Short and long term responses

  • Abandoned settlements,
  • relocated survivers
  • Parachuted soilders in
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Kobe Japan

  • MEDC
  • 17th January 1995, 5:46am
  • Destructive PB
  • Shallow
  • 7.2 richter scale

Primary

  • 200,00 buildings collapsed
  • Bridges, train lines, quays, motorways/roads

Secondary

  • 5500 deaths- hypothermia, burnt, panicked
  • 230,000 homeless
  • 40,000 injured 
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Kobe Japan- Secondary urban area- Short and long t

Secondary effects- Urban Area

  • Electricity, gas, water supplies disrupted.
  • Traffic jams, delaying abulances and fire engines,
  • Broken pipes caused fires,
  • Buildings pancaked, flooors dropped down

Secondary effect- Economic

  • City council pay- roads motorways
  • Home insurance- building houses

Short and long term responses

  • Water, gas, phone services- fully operated by July
  • Commerical buildings- August
  • 7 months to repair everything
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Earthquakes-methods of building design

  • 'Birdcage' interlocks steel frame
  • outer panels flexibility attached to steel structure
  • Fire ressistant building materials
  • Roads to provide quick access for emergancy services
  • Rubber shock absobers to asorb earth eremors
  • Foundations sunk into bedrock avoiding clay
  • Open areas where people can assemble if evacuated
  • Automatic window shutters to prevent glass smashing
  • Steel frames that sway during earth movement
  • Computer controlled weights on roof to reduce movement
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Mercalli Vs Richter Scale

Richter Scale- a measure of how much the ground shakes, scale 1-9

Mercalli Scale- measure of the damage done, scale 1-12

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