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5th Year Geography Earthquakes

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1 5th Year Geography Earthquakes
10/11/2018 Leaving Certificate Geography Unit 1.4 : Earthquakes Mr. McMahon 10/11/2018 Mr.C.McMahon Mr.C.McMahon

2 Learning Outcomes You will learn….
What an earthquake is. Why they occur. How their global pattern is explained by the location of fault lines. How earthquake zones are located and measured. How they are predicted. How earthquakes impact upon the landscape and human populations. 10/11/2018 Mr.C.McMahon

3 Earthquakes-The Past Ten Years
Place Richter Scale Casualties 2004 Sumatra Indian Ocean 9.1 230,000 2008 Sichuan Province China 7.9 87,587 2005 Pakistan 7.6 86,000 2010 Japan 6.8 12,690 (14,000 unaccounted for) 10/11/2018 Mr.C.McMahon

4 What is an Earthquake ? Damage Decreases From Epicentre Scarp
10/11/2018 Mr.C.McMahon

5 What Causes Earthquakes?
The plates of the crust are constantly moving. Sometimes plates jam or stick together. This creates a build up of energy when one or both plates slip releasing seismic waves that can violently shake the surface above. 10/11/2018 Mr.C.McMahon

6 Key Concepts Focus: The point where an earthquake begins in earth’s crust. Earthquakes can be shallow or deep focus. Epicentre: The point on the surface that is the worst affected by a quake. Damage lessens the further one moves from the epicentre. 10/11/2018 New Zealand Earthquake 2011 Mr.C.McMahon

7 The Global Distribution of Earthquakes
5th Year Geography Earthquakes 10/11/2018 The Global Distribution of Earthquakes 10/11/2018 Mr.C.McMahon Mr.C.McMahon

8 Location of Earthquakes
Earthquakes do no occur randomly. Their location is based on plate boundaries. Earthquakes occur at convergent, divergent and transform boundaries. 10/11/2018 Mr.C.McMahon

9 Transform Fault. California USA. Rifting: East Africa
The Subduction zone of Japan is the most earthquake prone area in the world. Transform Fault. California USA. Rifting: East Africa Divergent: Mid Atlantic Ridge. Convergent: Columbia -Chile 10/11/2018 Mr.C.McMahon

10 Seismic waves Primary (P) waves: Fast waves that compress then expand molten material 10/11/2018 Mr.C.McMahon

11 Secondary (S) waves are slow as they have to travel through solid rock.
10/11/2018 Mr.C.McMahon

12 Earthquake Waves 10/11/2018 Mr.C.McMahon

13 Surface Waves: The slowest waves that expend their energy on the surface causing anything on it to move up and down. Principle. Energy from waves is absorbed by material as it travels through them. Thus the father a wave travels the more energy they expend. 10/11/2018 Mr.C.McMahon

14 Measuring Earthquakes
The Seismograph Three are needed for a full set of data Horizontal measuring waves North-South Horizontal- East to West. Vertical Movement 10/11/2018 Mr.C.McMahon

15 The Richter Scale Logarithmic Scale.
Each unit is 10 times the wave activity of the previous for example a force 8 is 10 times greater than a force 7. The force is measured at a greater rate of 30. 10/11/2018 Mr.C.McMahon

16 Predicting Earthquakes
Earthquake zones are identified. Predictions based on timeframes. Seismologist Identify seismic gaps- points between plates where earthquakes are likely to begin. 10/11/2018 Mr.C.McMahon

17 Early Warning Systems Early Warning systems based on modern communication systems are being developed. Monitoring animal behaviour. 10/11/2018 Mr.C.McMahon

18 10/11/2018 Mr.C.McMahon

19 Destruction by Earthquakes
Destruction by earthquakes depends on the following. The depth of the focus The population density around the epicentre. Economic development and the standard of buildings. Overlying Topography 10/11/2018 Mr.C.McMahon

20 Soil Liquefaction Liquefaction is the process of soil, clay and sand turning into a sludge. During an earthquake ground water mixes with the soil types to produce a material like quicksand. This undermines the foundations of bridges, roads, dams etc…. Consequences ? 10/11/2018 Mr.C.McMahon

21 Other Dangers Falling Debris Flooding Burst gas and sewage mains.
Spread of disease Disruption to emergency services Tsunamis 10/11/2018 Mr.C.McMahon

22 Tsunami Giant waves that are generated when an earthquake occurs on the sea floor. See Indian ocean Earthquake- Tusnami animation Wikipedia 10/11/2018 Mr.C.McMahon

23 Limiting Earthquake Damage
Retro- fitting of Old Buildings. The development of advanced warning systems Tapered frames to increase a buildings frames integrity The use of shock absorbers in a buildings columns and foundations. 10/11/2018 Mr.C.McMahon

24 Case Study: The Haiti Earthquake
5th Year Geography Earthquakes 10/11/2018 Case Study: The Haiti Earthquake Tuesday 12th January 2010. Measured 7.0 Richter Scale Focus at 13 KM Epicentre 13KM from the capital Port Au Prince 10/11/2018 Mr.C.McMahon Mr.C.McMahon

25 Haitian Earthquake Map
5th Year Geography Earthquakes 10/11/2018 Haitian Earthquake Map 10/11/2018 Mr.C.McMahon Mr.C.McMahon

26 Case Study: The Japan Earthquake
5th Year Geography Earthquakes 10/11/2018 Case Study: The Japan Earthquake Struck on March 11th 2010 Richter Scale 9.0 Epicentre 60KM from the coast triggered Giant Tsunami Over 12,690 dead and 14,000 unaccounted for. 10/11/2018 Mr.C.McMahon Mr.C.McMahon

27 Japan Earthquake Map http://www.youtube.com/watch?v=hOe8PMoKdI8
10/11/2018 Mr.C.McMahon

28 Key Concepts Earthquake Focus Epicentre Seismology Seismograph
Richter scale Magnitude P Waves Q Waves S Waves Earthquake Prediction Early Warning Systems Scarp Tsunami Tremor Aftershocks 10/11/2018 Mr.C.McMahon


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