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-**Geography Summer Exam Revision**+====== ​Geography Summer Exam Revision ​====== 
 + 
 + 
 + 
 + __ Plate Tectonics:​__ 
 + 
  
-Geography Summer Exam Revision 
  
-Plate Tectonics: 
  
 Plates: Below are examples which you need to learn for the test. Plates: Below are examples which you need to learn for the test.
  
-Colliding: The Himalayas are an example of the collision of two continental plates+Colliding: ​<color #00a2e8>The Himalayas are an example of the collision of two continental plates</​color>​
  
-Separating: Mid-Atlantic Ridge+Separating: ​<color #ff7f27>Mid-Atlantic Ridge</​color>​
  
-Sliding Past Each Other: San Andreas Fault +Sliding Past Each Other: ​<color #ffaec9>San Andreas Fault</​color> ​
  
  
-Structure Of The Earth+//Structure Of The Earth//
  
-Plate: ​                    ​ +  - Plate: ​                  
-Plate Boundary: Where plates meet +  ​- ​Plate Boundary: Where plates meet 
-Crust: The thin outer layer of the earth +  ​- ​Crust: The thin outer layer of the earth 
-Mantle: Consists of both hot molten and semi-hot molten rock known as magma. It moves around in very slow currents. +  ​- ​Mantle: Consists of both hot molten and semi-hot molten rock known as magma. It moves around in very slow currents. 
-Outer Core: Consists of liquid nickel and iron (molten) +  ​- ​Outer Core: Consists of liquid nickel and iron (molten) 
-Inner Core: The solid centre of the earth.+  ​- ​Inner Core: The solid centre of the earth.
  
-Convection Currents+//Convection Currents//
  
-The earth'​s core heats the magma up towards the earth'​s crust. +The earth'​s core heats the <color #ed1c24>magma</​color> ​up towards the <color #ed1c24>earth'​s crust</​color>​
-As the magma rises it begins to cool. +As the magma <color #ed1c24>rises</​color> ​it begins to <color #ed1c24>cool</​color>​
-The cool magma becomes heavier and heavier causing it to sink back towards the earths core or magma chamber+The cool magma becomes heavier and heavier causing it to <color #ed1c24>sink</​color> ​back towards the earths ​<color #ed1c24>core.</​color> ​ 
-This circular ​movement ​causes a continuous movement of magma (convection currents) in the mantle. ​+This circular ​motion ​causes a continuous movement of magma (convection currents) in the <color #ed1c24>mantle</​color>​
 Convection currents cause tectonic plates to move very slowly. Convection currents cause tectonic plates to move very slowly.
  
-Earthquakes 
  
-The four parts of an earthquake are: 
  
-Focus (the point within the earth where an earthquake rupture starts) +__Earthquakes__
-Epicentre (point on surface directly above focus) +
-Shock Waves (waves that transmit energy released by earthquakes,​ spread out in circles from core focus)) +
-Fault (large crack in the earths crust)+
  
 +//The four parts of an earthquake are://
  
 +  - Focus (the point within the earth where an earthquake rupture starts)
 +  - Epicentre (point on surface directly above focus)
 +  - Shock Waves (waves that transmit energy released by earthquakes,​ spread out in circles from core focus))
 +  - Fault (large crack in the earths crust)
  
-Case Study: Chile 
  
-300km from capitol Santiago 
-35km from the pacific ocean 
-8.8 on the magnitude scale 
-More than 500 people left dead 
-Damage cost was $30 billion 
-Central towns hit by t-sunmai waves 
-Febuary 10th 2010 
-More than 400,00 severely damaged/​destroyed ​ 
  
-Volcanos+//Case Study: Chile//
  
-Formation of a volcano+  -  <color #​22b14c>​300km</​color>​ from capitol Santiago 
 +  -  <color #​22b14c>​35km</​color>​ from the pacific ocean 
 +  -  <color #​22b14c>​8.8</​color>​ on the magnitude scale 
 +  -  More than <color #​22b14c>​500</​color>​ people left dead 
 +  -  Damage cost was <color #​22b14c>​$30</​color>​ billion 
 +  -  Central towns hit by t-sunmai waves 
 +  -  Febuary 10th 2010 
 +  -  More than <color #​22b14c>​400,​00</​color>​ severely damaged/​destroyed ​
  
-When two volcanos separate or collide, magma can rise from the mantle. 
-It fills the space in the crust -vent in an eruption 
-Magma cools and hardens at the surface. This is called lava 
-Layers of ash and lava build up around the vent 
-This forms a cone shaped mountain with a crater 
  
-Mass Movement 
  
-Sea+__Volcanos__ 
 + 
 +//Formation of a volcano// 
 + 
 +  * When two volcanos separate or collide, magma can rise from the mantle. 
 +  * It fills the space in the crust -vent in an eruption 
 +  * Magma cools and hardens at the surface. This is called lava 
 +  * Layers of ash and lava build up around the vent 
 +  * This forms a cone shaped mountain with a crater 
 + 
 +__Mass Movement__ 
 + 
 +4 aspects that affect mass movement are: 
 +  - <color #​fff200>​Water</​color>​ - Water makes the regolith (material) heavier, causing it to move faster down slopes 
 +  - <color #​ff7f27>​Vegetation</​color>​ - Roots of tree's and plants help keep the soil together, helping to prevent mass movement 
 +  - <color #​ed1c24>​Human Interaction</​color>​ - Humans speed up mass movement when they makes hills/​slopes more unstable ex. roads/​quarry 
 +  - <color #​00a2e8>​Slope or Gradient</​color>​ - The steeper the gradient, the faster loose regolith can travel down it 
 + 
 + 
 +__Sea__
  
 Form of erosion -  Form of erosion - 
 +
 +__River__
 +
 +Form of deposition - 
 +
 +__Process of Erosion + Deposition__
 +
 +//​Erosion://​
 +  * <color #​c3c3c3>​Hydraulic Action</​color>:​ Motion of water hitting the surface
 +  * <color #​b5e61d>​Abrasion</​color>:​ Scraping/​wearing away of rocks
 +  * <color #​ff7f27>​Attrition</​color>:​ Impact of rock grains hitting of each other 
 +  * <color #​ffaec9>​Solution</​color>:​ Minerals are dissolved in water and carried along
 +
 +//​Deposition://​
 +
 +__Maps__
 +
 +  * line number to the right
 +  * key on back of map 
 +  * always has to be exact
  
  
geography/summer_exam_revision.1652376084.txt.gz · Last modified: 2022/05/12 17:21 by shane