GCSE Geography AQA - Restless Earth
These are revision cards for GCSE geography AQA, I'm making ones for restless earth, the coastal zone, rocks, tourism, population and urban. In some parts its hard to describe processes without pictures, so just try to imagine it! These include case studies :)
- Created by: Jenny Hoper
- Created on: 09-06-12 09:00
Structure of the Earth
Continental Crust:
- 30 - 50km thick
- Over 1500 mil years old
- Mainly granite, silicon, O2, aluminium
- Can't sink, can't be destroyed, 2.6 density
Oceanic Crust:
- 6 - 10km thick
- Less than 200 mil years old
- Mainly bascut, silicon, magnesium, O2
- Can sink, can be destroyed, 3.0 density
Inner core < outer core < mantle < oceanic crust < continental crust
Plate Margins
- Constructive plate margins - 2 plates move away from each other, magma rises to surface to form volcanic islands, volcanoes & earthquakes
- Collision zones - 2 cont. plates move towards each other, neither can be destroyed so form fold mountains, no volcanoes but some earthquakes
- Destructive plate margins/subduction zones - 2 plates move towards each other, heavier oceanic crust sinks below cont. crust, causes deep sea trenches, volcanoes & earthquakes
- Conservative plate margins - 2 plates move sideways next to each other, same direction or different directions, violent earthquakes
Fold Mountains & Ocean Trenches
Fold mountains:
- many places e.g. Alps, Himalayas, Carcasas
- Rivers carry sediment into sea between 2 plates, sediments build on sea bed
- Geosycline filled with sediment, compression as plates move towards each other
- Continued compression from 2 plates, sediments folded into fold mountains
Ocean trenches:
- found in subduction zones, edge of Pacific ocean e.g. Peru-Chile trench
- Oceanic plate sinks below cont. crust, causes a trench
Shield & Composite Volcanoes
Volcanoes found in long narrow belts e.g. 'Pacific Ring of Fire' & mid Atlantic ocean, south Europe & centre of Pacific ocean
Shield volcanoes:
- Constructive plate margins
- Lava - runny, basic, hot
- Cone - wide base, gentle slopes made of lava
- e.g. Mauna Loa, Hawaii; Hekla & Heimaey, Iceland
Composite volcanoes:
- Destructive plate margins
- Lava - acidic, sets quickly
- Cone - tall, narrow base, steep sides made of layers of lava & ash
- Pyroclastic flows, secondary cones
- e.g. Mt St Helens, USA; Pinatubo, Philippines
Earthquakes
- Caused by sudden release of pressure due to movement along faults
- Most occur along plate margins, strongest at destructive, constructive & conservative
- Plates suddenly lurch, point where pressure is released called the focus
- At destructive plate margins focus is deep & sinking of subducting plate & its subsequent melting can trigger strong earthquakes
- Longitudinal & transverse waves, surface of focus called the epicentre
Plate Margin Case Studies
- Constructive - Mid-Atlantic Ridge, Iceland
- Destructive/subduction - Nazca & South American plate boundaries, Andes mountains (fold mountains), Peru-Chile Trench (8km deep, 45,00km long from Panama to Tierra del Fuego)
- Collision - Indo-Australian & Eurasian plate boundaries, Himalayas
- Conservative - Pacific plate (faster) & North American plate (slower), San Andreas Fault
Fold Mountains - The Alps
- Why is human activity hard? - relief high & steep, accessibility hard; narrow mountain valleys, making roads/railways hard; soil is stony, thin & infertile; colder, windier & wetter as you go up
Human activity:
- Forests - timber from coniferous forests main building material & winter fuel, pulp & paper
- Farming - on south-facing slopes are warmer, transhumance - seasonal movement of animals, summer cattle on higher alp, fodder grows on valley floor, winter cattle to valley floor, feed on fodder; new techology - cable cars carry milk to valley floor, turn milk into butter & cheese
- HEP - Hydro-electric Power, power generated from fast-moving rivers due to steep slopes, precipitation & melting glaciers; cheap, renewable, used by sawmills etc, supplies with electricity
- Tourism - skiing, snowboarding, e.g. St Montz Chomonix; glacial lakes, scenery e.g. Interlaken
- Safety - building tunnels & shelters along roads from avalanches, expensive, needs technology
Mount Pinatubo
- 9th June 1991, not erupted since 1380; largest eruption of 20C, near city of Manila, destructive plate margin; Philippines plate (oceanic) & Eurasian plate (cont.)
- Primary effects - 200,000 homes destroyed, local hospital, schools & factories, contaminated water, unusable roads & bridges, ash ruined harvest of 1991, 6 died as direct result of eruption
- Secondary effects - planting in 1992 impossible, over 1 mil animals died, farmers forced to city, disease like malara & diarrhoea, 1991 & 1993 monsoon rains - flooding & lahars, lowered world temps & blocked sun, 700 died from disease/lahars
- Immediate responses - many didn't believe it would happen, fled with panic to refugee camps, emergency aid from Japan - food, medicine, blankets, April - June 1991 early warning signs, evacuation of 58,000, 15,000 at Clark Air Base
- Long term responses - Nov 1991 US abandoned CAB, Aeta tribe returned to slopes, Japan granted materials for rehabilitation, people from Angeles stayed in refugee camps due to lahars, 10 years later CAB now a thriving tourist resort, 1993 Clark Development Corporation for Aeta, 7 industries
Pinatubo - predicting & preparing
Predicting:
- Magma moving causes small earthquakes, measure using seismomenters, recorded 2 months before eruption
- Ground temps increased - heat seeking cameras
- Bulging lava dome - tiltmeasures by CAB
- Gurgling magma, gas & steam
- GPS - detect movement
Preparing:
- Forecast eruption, predict how powerful it will be
- Evacuate those in danger area, provide transport, accommodation & food
- Train more emergency service teams
- 2nd April, first evacuation of 2,000 people
- Organise emergency supplies & water
Yellowstone Supervolcano
Supervolcano characteristics:
- erupts at least 1000km3 of material
- formed by boiling reservoir of magma, grows to enormouse size & colossal pressure
- when it erupts & collapses, it causes a huge depession called a caldera
Facts: north-west Wyoming, USA; 55km by 65km; recurrence interval of 600,000 years; geysers, mud pits & hot springs; ground risen by 70cm in some places
Local effects - devastating for 100 mile radius; pyroclastic flows for 50-100 miles at 500 mph; ash rise 80,000 feet, then 20-30 feet would fall; 400,000 people at risk; inhaling ash is dangerous; animals & crops die; day turns to night
National effects - north-west USA devastated; ash particles stay in air for years, crops fail for 6 years, biggest supplier of grain so big consequences
International effects - severe air traffic disruption; global temps & climates effected; ash particles in air for 6 years
Kobe Earthquake
Location - epicentre on Awaji Island in Osaka Bay off coast of Kobe, south Japan
Magnitude & duration - Philippine plate under Eurasian plate along Nokima fault, 7.2 Richter scale, 20 seconds
Date & time - Jan 17th 1995, 5:46 am
Primary effects - 200,000 buildings destroyed; bullet train bridges collapsed; 120/150 quays destroyed; 1km of Hanshin Expressway collapsed; almost every house flattened
Secondary effects - electricity, water, gas supplies cut off; fires; massive traffic jams help up emergency crews; 230,000 homeless; Panasonic & Mitsubshi temporarily closed; 5,500 dead & 40,000 injured
Immediate responses - Hanshin Expressway still closed; hospitals struggled to cate for everyone
Long term responses - all services working by July; fire areas by Aug; total damage £56 bn, Sept 1996 H. Expressway open again, buildings further apart, flexible steel frames, rubber blocks
Sichuan Earthquake
Location - Sichuan country, central China, epicentre in Wenchuan
Magnitude & duration - Indian Plate & Eurasian plate along Longmenshan fault; 7.9 Richter scale, 120 seconds
Date & time - May 12th 2008 at 2:28 pm
Primary effects - 8,700 dead initially, 374,000 injured; 5-10 mil homeless; 5 million buildings collapsed, Juyuan school in Dujiangyuan 900 pupils killed; communications stopped
Secondary effects - 69,000 dead, 18,000 missing; landslides blocked roads & rivers; fear of flooding; £75 bn damage
Immediate responses - 20 helicopters bring relief & rescue; army troops parachuted & hiked to worst areas; clean water, food supplies & tents
Long term responses - teams from Japan, Russia & South Korea helped; donation of £100 mil from Red Cross, went to running camps
Indian Ocean Tsunami
Location - epicentre in Sumatra
Magnitude - 9.1 Richter scale, 10m vertical displacement of seabed along 750 mile fault line
Date - 26 Dec 2004
Effects - highest wave 25m; 220,000 died, 650,000 injured; 2 mil homeless; tourist resorts damaged, affected local economy, many foriegn nationals died
Responses - rescue services & emergency teams swamped by scale of disaster; wounds turned gangerous; fresh water, water purification tablets, food, sheeting & tents from whole world; £75 million from UK, build 20,000 new homes; Indian Ocean Tsunami Warning System set up in June 2006
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