Tectonics
Thursday 22nd May
The earth as a scotch egg
The crust of
our earth is
very shallow
like the
breadcrumb
layer of the
scotch egg. It
is what w...
Cross Section of the Earth Crust – very thin like the
breadcrumbs of our scotch egg.
6-70km thick
Mantle – very high
temps...
Distribution of Earthquakes and Volcanoes
Distributed on the plate boundaries
Mostly on the coasts or in the ocean
Around ...
Convection
Currents
Mantle
Crust
Why the plates move
• Magma from the earths core is super heated and rises towards the cr...
Oceanic and Continental Crust
Continental Crust:
• 25 -100km thick
• Less dense
• Bigger crystals
• More easily eroded
• Y...
Divergent Plate Boundaries
The plates moving apart in this way is
known as sea floor spreading.
It is the reason for Iceland's existence and
the reas...
Convergent Plate Boundary – two
continental crusts
Convergent Plate Boundaries – one
oceanic, one continental crust
It is on convergent plate boundaries that you find the deepest ocean
trenches and some of the most active volcanoes in the...
Conservative Plate Boundaries
The San Andreas Fault in California is
the best known example of a
constructive plate margin.
The can also be found near F...
Type of plate
boundary
Diagram Description of
changes
EQ/Volcano
activity
Examples
Convergent
•Oceanic plate forced
downwa...
Measuring Earthquakes
Richter Scale
Measures strength using numbers
No upper limit
Mercalli Scale
Measures effects using r...
How do earthquakes happen?
1) Pressure builds up at plate boundaries.
2) The plates cannot move though due to
friction, an...
Silicon Valley, home of IBM and Apple. 23,000 jobs and
700,000 people. On the San Andreas Fault. There has not
been a larg...
The Soufriere Hills on the island of Montserrat erupted in 1995 in one of the most devastating
eruptions ever seen. It ent...
Sorrento and the Island of Capri in Italy.
Massive tourist destination and people are attracted because
of the beautiful b...
Mount Etna in Italy, Europe's most active volcano but ‘safe’ enough for tourists to go and watch.
Many farmers also grow o...
Iceland straddles the Mid Atlantic ridge; a divergent plate boundary. The magma near the surface
heats water in the rock c...
Haiti - LIC Earthquake Case Study
Effects Responses
• The main port was closed after severe damage to
the docks and a cran...
Iceland – HIC Volcano Case Study
Causes
•Iceland lies on a divergent plate boundary between the North American and Eurasia...
Prediction - Volcanoes
Volcanoes can be monitored to predict eruptions with:
• GPS - to see if the ground is rising up as ...
Prevention - Volcanoes
Once an eruption has happened it is possible to prevent it from having major
effects on the local p...
Prediction - Earthquakes
Earthquakes are much harder to predict because they happen underground
so are not visible. Method...
Planning for Earthquakes
Because so little warning can be given it is
better to plan for the worse to limit the effects
su...
Tectonics
Tectonics
Tectonics
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Tectonics

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EDEXCEL A GSCE Geography revision Unit 2 - Tectonics

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Tectonics

  1. 1. Tectonics Thursday 22nd May
  2. 2. The earth as a scotch egg The crust of our earth is very shallow like the breadcrumb layer of the scotch egg. It is what we live on. The mantle is like the meaty bit of our scotch egg. It is the largest section and is made of liquid rock called magma. It is underneath the crust and behaves a bit like jam The outer core is what lies beneath the mantle. This is the white of our egg. This is also liquid rock but moves very slowly because it is under so much pressure. The inner core of the earth is solid because of the pressure. It is also hotter than the surface of the sun
  3. 3. Cross Section of the Earth Crust – very thin like the breadcrumbs of our scotch egg. 6-70km thick Mantle – very high temps. Looks like jam! Between 5000 and 1300oC Outer Core – Liquid made mostly of iron Inner Core – Solid made of iron. Up to 5500oC
  4. 4. Distribution of Earthquakes and Volcanoes Distributed on the plate boundaries Mostly on the coasts or in the ocean Around the edge of the pacific and through the middle of the Atlantic With the exception of Hawaii which is on a hotspot
  5. 5. Convection Currents Mantle Crust Why the plates move • Magma from the earths core is super heated and rises towards the crust • As it rises and travels away from the core it begins to cool • When it reaches the crust it is forced sideways and because it is not colder, sinks back down again towards the core. • Where is spreads out you will find divergent boundaries and where is sinks downwards it full down crust from a convergent boundary.
  6. 6. Oceanic and Continental Crust Continental Crust: • 25 -100km thick • Less dense • Bigger crystals • More easily eroded • Youngest Oceanic Crust: • 5 -10km thick • More dense • Tiny crystals • Very hard rock • Very old rock
  7. 7. Divergent Plate Boundaries
  8. 8. The plates moving apart in this way is known as sea floor spreading. It is the reason for Iceland's existence and the reason why volcanoes are present there. The island of Sursey, off the coast of iceland erupted in 1963. Before then there had been no land in that place.
  9. 9. Convergent Plate Boundary – two continental crusts
  10. 10. Convergent Plate Boundaries – one oceanic, one continental crust
  11. 11. It is on convergent plate boundaries that you find the deepest ocean trenches and some of the most active volcanoes in the world. The Cascade Mountain range is off the west coast of America and is a line of volcanic mountains caused by the convergent plate margin. Because a lot of earthquakes occur under the ocean it is only destructive plate margins that cause tsunamis.
  12. 12. Conservative Plate Boundaries
  13. 13. The San Andreas Fault in California is the best known example of a constructive plate margin. The can also be found near Fiji, Israel, South Island in New Zealand and Sumatra in Indonesia.
  14. 14. Type of plate boundary Diagram Description of changes EQ/Volcano activity Examples Convergent •Oceanic plate forced downwards into the mantle forming a subduction zone. •Deep trench formed •Continental plate forced up into mountain range Constructive Conservative Pacific and North American Plates along the San Andreas Fault •Two plates move away from each other •New oceanic crust is created forming mid- oceanic ridges with volcanoes Two plates move sideways past each other – land is neither formed nor destroyed. •Heat from the mantle and friction from contact between the two plates causes violent earthquakes to be triggered. •These can also cause tsunamis •The melting plate creates magma which rises to the surface to form volcanoes •Where magma builds up above the surface, volcanoes form. •In the ocean these quite often show as islands Plates do not tend to move past each other smoothly. Friction is created and they tend to get stuck. Pressure builds until the plate flips forward creating violent EQ’s Pacific ring of Fire Japanese Island Arc New Zealand Iceland Great Rift Valley Africa
  15. 15. Measuring Earthquakes Richter Scale Measures strength using numbers No upper limit Mercalli Scale Measures effects using roman numerals. Limited because there is only so much damage that can be done
  16. 16. How do earthquakes happen? 1) Pressure builds up at plate boundaries. 2) The plates cannot move though due to friction, and pressure continues to build. 3) Suddenly the crust breaks along a fault. 4) The plates spring apart. 5) Stored energy is released in a few seconds from the focus, and travels out from the epicentre as seismic waves on the surface.
  17. 17. Silicon Valley, home of IBM and Apple. 23,000 jobs and 700,000 people. On the San Andreas Fault. There has not been a large earthquake here for over 30 years.
  18. 18. The Soufriere Hills on the island of Montserrat erupted in 1995 in one of the most devastating eruptions ever seen. It entirely covered the capital city of Plymouth in ash and closed the airport. It was known that the island was highly volcanic but no-one wanted to leave the island even after the eruption. Their families and their livelihoods were there and they had nowhere else to go.
  19. 19. Sorrento and the Island of Capri in Italy. Massive tourist destination and people are attracted because of the beautiful beaches and amazing weather. It also has a historic interest with many people coming to visit Pompeii; the ancient roman port that got destroyed by the volcano in 79AD. Across the bay from Mt Vesuvius It has not erupted violently for over 50 years.
  20. 20. Mount Etna in Italy, Europe's most active volcano but ‘safe’ enough for tourists to go and watch. Many farmers also grow olives, grapes and citrus fruits because the volcanic ash produces extremely fertile soil here. Siciliy is quite a poor area of Italy too with a very close knit community.
  21. 21. Iceland straddles the Mid Atlantic ridge; a divergent plate boundary. The magma near the surface heats water in the rock causing warm pools of water to rise up. People visit Iceland to bathe in these pools. The hot water can also be harnessed for geothermal energy. This is extremely environmentally friendly and renewable.
  22. 22. Haiti - LIC Earthquake Case Study Effects Responses • The main port was closed after severe damage to the docks and a crane. • Some roads are impassable - either because of earthquake damage, or because they are blocked by rubble or smashed vehicles. • Between 500,000 and 700,000 people are believed to have been left homeless • Even before the earthquake only half of Haitians had access to clean water. Now most of the remaining water supply been cut off. • Eight hospitals or health centres in the capital collapsed or suffered severe damage. • US engineers and dive teams fixed piers, cranes, and buildings. • Around 3,000 UN troops and police worked to clear some of the major roads. • More than 500 makeshift camps have been identified by the Haitian government, which has requested large tents be set up as reception centres for the homeless. • On 20 January, 755,000 litres of water were provided to 151,000 people. • Field hospitals have been set up by teams from Russia, Israel, Colombia, Jordan and Brazil. Causes • Haiti is located on a conservative plate margin between the Caribbean and North America plate which are slowly moving past each other. • 7.0 magnitude which stuck on Tuesday 12th January at 16:53 (Haiti Time)
  23. 23. Iceland – HIC Volcano Case Study Causes •Iceland lies on a divergent plate boundary between the North American and Eurasian plates which are moving apart at a rate of 2cm per year. •As they move apart, lava wells up in the gap in between towards the surface. •As this process continues and consecutive lava eruptions cool and build up, volcanoes are created. Effects •The cloud of ash went 20,000ft into the atmosphere and blew on westerly winds cross Europe. •95,000 flights had to be cancelled in the UK as the ash was at the height that plans normally fly at. •The flight ban was imposed because in the high temperatures of an engine turbine, ash can turn to molten glass and cripple the engine. •The airline industry said its losses soared to over £650 million •Other transport companies benefitted as passengers looked for alternatives to flying. •Eurostar in particular saw a huge demand from and said it carried 50,000 extra passengers just on one day alone. •Kenyan farmers were forced to dump stocks of fresh food and flowers destined for European consumers which cost the Kenyan economy $3.8m a day as a result of flight cancellations to Europe. •Locally 700 farmers around the volcano were evacuated due to the melting ice cap on top of the mountain which caused flooding and property to be washed away. Responses •Some 60 volunteers and staff of the Icelandic Red Cross provided food for the farming population living in the vicinity of the glacier. •Some 700 people were evacuated from the disaster zone three times in the past month. •A 24-hour emergency information hotline was also activated. Red Cross volunteers are also providing meals twice a day in Heimaland, as most people have not been able to stock up on food.
  24. 24. Prediction - Volcanoes Volcanoes can be monitored to predict eruptions with: • GPS - to see if the ground is rising up as magma approaches the surface • Gas sampling – changes to gases coming out of the volcano might mean an eruption is coming • Geothermal monitoring – the ground gets hotter as magma rises to the surface • Seismic monitoring – to ‘listen’ to the rising blobs of magma as they force their way upwards and cause small earthquakes • Looking at historical records to see if there is a past pattern of eruptions that might be repeated.
  25. 25. Prevention - Volcanoes Once an eruption has happened it is possible to prevent it from having major effects on the local people by; • Spraying the lava with water to cool it down and stop it flowing • Putting concrete barriers in the path of lava forcing it away from villages • Setting off explosive to divert the lava flow • Digging ditches to funnel it away from homes
  26. 26. Prediction - Earthquakes Earthquakes are much harder to predict because they happen underground so are not visible. Methods used to predict earthquakes include; • Noting strange animal behaviour – cats, dogs, birds and snakes are known to behave differently before an earthquake • Monitoring electrical discharges – there is some evidence that these increase before an earthquake. Some scientists believe that they appear in the sky as a rainbow glow, known as earthquake lights. • Recording minor tremors as these could be small foreshocks
  27. 27. Planning for Earthquakes Because so little warning can be given it is better to plan for the worse to limit the effects such as; • Providing education for local residence who are taught how to react • Have an emergency kit ready including a torch, bottled water, first aid kit and tinned food. • Design buildings that can withstand earthquakes by having flexible steel frames; shutters can be used to cover windows that might shatter; rubberised foundations can be used to absorb the energy of a quake • Planning regulations so buildings are not built too high.
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