Unit 1 Geography- Restless earth
- 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
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
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)
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.
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!
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
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)
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
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.
Mt Pinatubo- 1991- Base Details
- Eurasian and Philippines plate
- Destructive PB
- 611 Years dormant
- Philiappines
- LEDC
- Andesitic
- Oceanic crust
- Plinian erupition
- VEI- 6
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
Eyjafjallajokull- 2010- Base Details
- Eurasian and North American plate
- Contstructive PB
- 90 years dormant
- Iceland
- MEDC
- Basaltic
- Core
- Volcanian eruption/ Strombolian eruption
- VEI= 4
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.
Monitoring Volcanoes and Quakes- disaster manageme
Disaster event - Emergancy response
- fire crews, medical staff, rescue team, army support, food supplies, shelter protection
Relief- Mend Scars
- Loss management, support network
Reconstruction-Rebuild
- learn from mistakes, using modern technologies in construction
Migration- Rescue the impact
- Relocate people away, strengthen structers, planning restrictions
Preparedness-Being ready
- Governments, Comminuties, individuals
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
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
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
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
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
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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