The Earth's Surface 

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Structure of the earth

  • [[The crust[[
      * The crust is the outside layer
      * Made of solid rock
      * Oceans and continents lie on top of the crust
  • ]]The mantle]]
      * The mantle lies under the crust
      * Made of magma
      * The magma is moved around by convection currents
  • {{The core{{
      * The centre of the earth
      * Made of iron and nickle
      * Hottest part => 6000 degrees
      * Can be divided into the inner core and the outer core

Plates

  • The earths crust is broken into plates
  • Plates with land on top = continentalplatescontinental plates
  • Plates with ocean on top = oceanicplatesoceanic plates
  • The line where two plates meet = plateboundaryplate boundary
Convection currents
  • The plates lie on top of the mantle
  • Magma in the mantle is moved around by convection currents = causes plates to move
  • Plates can
      * CollideCollide
      * SeparateSeparate
      * SlideSlide

Plate tectonics

The study of plates and their movement is called platetectonicsplate tectonics

PangaeaPangaea: All the continents joined together

  • Pangaea then broke up by continentaldriftcontinental drift
  • Proof: Mid-Atlantic Ridge
What happens at each of the plate boundaries?
Plates collide
  • DestructiveDestructive boundaries
  • Crust is destroyeddestroyed
  • SubductionSubduction: Heavier plate (oceanic) is pushed under the lighter plate (continental)
  • Colliding plates cause:
      * FoldmountainsFold mountains
      * EarthquakesEarthquakes
      * VolcanoesVolcanoes
  • Example:
      * The Andes
Plates separate
  • ConstructiveConstructive boundary
  • New crust is formedformed
  • Plates move apart and magma moves in to fill the gap, which cools and hardens to form new crust
      * When this happens under the sea it’s called seafloorspreadingsea-floor spreading
  • Separating plates cause:
      * VolcanicmountainsVolcanic mountains
      * VolcanicislandsVolcanic islands
  • Example:
      * The Iceland
Plates slide
  • PassivePassive boundary
  • Crust is neithercreatedordestroyedneither created or destroyed
  • Plates lock and release a huge amount when the pressurepressure is released
  • Sliding plates cause:
      * EarthquakesEarthquakes
      * FaultlineFault line
  • Example:
      * San Andreas Fault

Volcanic Activity

Ringoffire:Ring of fire: the edge of the pacific where most volcanic activity happens

Volcanic activity causes:

  • MidoceanicridgesMid-oceanic ridges
  • VolcanicislandVolcanic island
  • VolcanicmountainsVolcanic mountains

Mid-oceanic ridges

Hot molten magma rises up from the mantle, through the cracks in the crust. This mama cools, hardens and builds up, forming a ridge of rock

Example:

  • The MidAtlanticRidgeMid-Atlantic Ridge
  • Where the South American Plate from the African/Eurasian Plate

Volcanic island

When underwater mountains rise above the surface of the ocean

Example:

  • IcelandIceland

Volcanic mountain

Formed when magma rises up from a magma chamber through a vent to reach the Earth’s surface. When magma reaches the surface of the earth it’s called lava.

When lava, hot ash and rocks are throw into the air from the vent we call it an eruption. After many eruptions, layers of material build up around the vent to form a a cone shaped volcanic mountain or volcano.

Parts of a volcano

 Volcano

Example:

  • Mount St Helens, USA
Types of volcano:
  • %%Active%%
      * Erupt regularly
      * Example: Mount St Helens, USA
  • DormantDormant
      * Might not erupt for a long time but might erupt again
      * Mount Vesuvius, Italy
  • ==Extinct==
      * Extinct volcanoes will not erupt again
      * Croghan Hill, Co. Offaly
Socio-economic effects of volcanoes

SocioeconomicSocio-economic: to do with both social factors and economic factors and how they relate to eachother

%%Positive effects:%%

  • The soils near volcanoes are richinmineralsrich in minerals and are very suitable for agricultureagriculture. This means that people can farm and sell more produce
      * Campania in Italy has very fertile soils as it lies next to mount Vesuvius
  • Volcanic regions are very good touristtourist sites
  • Water heated underground by volcanic activity can be used to make geothermalenergygeothermal energy to heat peoples home’s
      * Geothermal energy is very popular in IcelandIceland

==Negative effects:==

  • SulfurdioxideSulfur dioxide is produced by volcanoes and can poison people nearby and can cause acidrainacid rain
  • Lava flow burns everything in it’s path and can result in huge lossoflifeloss of life
  • When volcanic matter mixes with rain or snow it can result in a laharlahar
Volcanic activity in Ireland
  • Evidence for extinct Irish volcanoes 450 million years ago:
      * The Giant’s Causeway: Igneous rock
      * Lambay Island, Co. Dublin

Case Study: Volcanic activity in Iceland

The physical landscape, social and economic activities are very influenced by volcanic activity as Iceland is located on the MidAtlanticRidgeMid-Atlantic Ridge

Geothermal energy
  • GeothermalenergyGeothermal energy is one of the cheapescheapest and most sustainablesustainable forms of energy
  • SteamSteam from geothermal energy is used to create electricitelectricity which provides factories, offices and houses with power
  • WaterWater heated by geothermal energy can be used to heathomesheat homes
Agriculture
  • Iceland is self-sufficient in the production of meat
  • Selfsufficient:Self sufficient: does’t need to import products
  • Crops are grown in greenhousesgreenhouses that are heated by geothermalenergygeothermal energy
  • Water is used sustainablysustainably
  • Ireland doesn’t receive much daylight in winter, however cheapgeothermalenergycheap geothermal energy can be used to create artificiallightartificial light in greenhouses
Tourism
  • Natural tourist attractions:
      * BlacksandbeachesBlack sand beaches
      * GeysersGeysers
      * GeothermalspasGeothermal spas
  • %%Positive impacts%%
      * Tourism provides jobsjobs
  • ==Negative impacts==
      * SoilerosionSoil erosion and litter from tourists

Case Study: Natural disaster: Mount St Helens

%%Short-term responses%%
  • As the volcano was monitoredmonitored and predicted to erupt, people were evacuatedevacuated
  • AshAsh took 10 weeks and millions of dollars to remove
      * Provided 200,000 jobsjobs
  • ElectricityElectricity was restored
^^Long term responses^^
  • Millions of treestrees were replantedreplanted
  • Farmers were given compensationcompensation for their losses
  • Government gave money to rebuilddamagedbuildingsrebuild damaged buildings and transporttransport

Earthquakes

  • Earthquakes are sudden tremourstremours in the Earth’s crust
  • Caused by releasedpressurereleased pressure of collidingcolliding or slidingplatessliding plates
  • Earthquake
  • Smaller tremors after an earthquake are called aftershocksaftershocks

Measuring earthquakes

  • SeismologistSeismologist: A person who studies earthquake activity
  • SeismographSeismograph: Used to measure tremors in the earth’s crust
  • RichterRichter scale: A scale ranging between 1-10, each unit is 10 times stronger than the one before it
  • MomentmagnitudescaleMoment magnitude scale: Mw

Damage caused by earthquakes

  • LossoflifeLoss of life
  • Building can collapsecollapse or get damageddamaged
  • Damage to electricity lines or gas pipes can cause firesfires
  • Damage to sewerssewers and water supplies can spread diseasedisease
  • When bridgesbridges, roadsroads and railwaysrailways are broken it can effect transporttransport in and out of the area
  • LandslidesLandslides and avalanchesavalanches can be triggered
  • TsunamiTsunami: huge wave caused by an earthquake underwater
How to reduce the damage caused by earthquakes
  • Earthquake resistant buildings
      * ShockabsorbersShock absorbers
      * ReinforcingwallswithsteelReinforcing walls with steel
      * TunedmassdampersTuned mass dampers
  • Earthquake and tsunami drills
  • Early-warning systems

Case study: Earthquake in Japan

On March 11 2011 an 8.9 earthquake hit Japan which also caused a tsunami

%%Short term responses%%
  • After the earthquake a tsunamiwarningtsunami warning was issued and coastal areas were evacuatedevacuated
  • People living near the nuclear power plant were checked for signs of radiationradiation
  • TemporarycampsTemporary camps were set up for the homelesshomeless
  • DebrisDebris was cleaned up
  • Other countries offered emergencyaidemergency aid
^^Long term responses^^
  • Electricity and water supplies were restored
  • Roads and airports were repaired
  • Houses and other building were repaired or rebuilt

Fold mountains

When two plates collide with each other a fold mountain forms

  • Heavier plate sinks under the lighter plate
  • Lighter plate bucklesbuckles because it has nowhere to go making foldmountainsfold mountains

or

  • If two lighter plates collide they both buckleupwardsbuckle upwards

Example:

  • The Andes

Periods of folding

AlpineAlpine
  • Highest mountains
  • 30-35 million years ago
  • Examples:
      * The Alps
      * The Andes
      * Himalayas
@@Armorican@@
  • When Eurasian and African plate collided
  • 250 million years ago
  • Examples:
      * MacGillycuddy’s Reeks
      * Black forest, Germany
==Caledonian==
  • When Eurasian Plate and American plate collided
  • 400 million years ago
  • Examples:
      * Dublin and Wicklow mountains

Mountains and people

Tourism
  • People are attracted to the beautifulscenerybeautiful scenery
  • LeisureactivitiesLeisure activities
      * Hill walking
      * Skiing
      * Rock climbing
  • Provides employmentemployment
  • PollutionPollution and littering
Farming
  • CattleCattle and sheepsheep
  • Difficult to use machinerymachinery
Forestry
  • Forestry is usually the only suitable economic activity
  • Felling of trees can cause soil erosionerosion and landslideslandslides

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