Chapter 4. The Earth s Surface: Shaping the crust

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Chapter 4 The Earth s Surface: Shaping the crust

Learning outcomes In this chapter you will learn: That the earth is made up of layers Why the earth is shaped as it is What plates are and how they move What happens when plates separate or meet How to describe an earthquake and a volcano that you have studied

The Solar System Earth: One of eight planets that make up the solar system Gets heat and energy from the Sun Only planet known to support life

The layers of the Earth The Earth is made up of three different layers: The Crust Outside layer Solid rock Oceans and continents The Mantle Sits under the crust Magma molten and semi-molten rock Convection currents The Core Centre of earth Hottest part Iron and nickel Exam hint: You need to be able to describe the layers of the Earth.

The Earth s crust Made up of plates Continental plates land on top Oceanic plates oceans on top Plate boundary place where plates meet Plates sit on magma in upper mantle Convection currents move magma Causes plates to move continental drift Plates collide, separate or slide past each other Plate tectonics the study of plates Exam hint: You must be able to explain what plates are and how they move.

The Earth s Crust Pangaea At one stage all the continents of the world were joined together. What was the name of the landmass they formed?

What happens at plate boundaries? Destructive boundaries Plates collide Crust destroyed Fold mountains Volcanic mountains Earthquakes Constructive boundaries Plates separate New land created Volcanic activity Volcanic mountains Volcanic islands Mid-ocean ridges Passive boundaries Plates slide past each other Earthquake activity Earthquakes Fault lines Exam hint: You need to know what happens when plates collide, separate or slide past each other.

Volcanic activity Occurs where plates separate or collide Most activity around edge of Pacific Plate Pacific Ring of Fire Landforms: Mid-ocean ridges Volcanic islands Volcanic mountains

Volcanic activity: Landforms Mid-ocean ridges Volcanic islands Volcanic mountains Magma rises from mantle Escapes through fissures in crust Cools and hardens Builds up Forms new land in ridge-like shape Mid-Atlantic Ridge Magma rises from mantle Escapes through fissures in crust Cools and hardens Builds up Forms new land in ridge-like shape Rises above surface of ocean Volcanic mountain Iceland Magma rises from magma chamber Escapes through vent Lava, hot ash, rocks, ash cloud Material builds up Forms a coneshaped mountain Crater at top Mount Vesuvius Exam hint: You need to be able to describe landforms created by volcanic activity and give examples.

Volcanic activity: Landforms

Types of volcano Three types of volcano: Active Erupt regularly Mount Etna Mount St. Helens Dormant Haven t erupted in long time Could erupt again Mount Vesuvius Extinct Haven t erupted in recorded history Croghan Hill, Offaly Exam hint: You must be able to describe the three types of volcano.

Effects of volcanoes Positive Negative Lava soils rich in minerals Tourist attractions Hot springs geysers Create new land Gases poison people, cause acid rain Lava flow burns everything in its path Loss of human life Cause lahars destroy towns and villages

Mount St. Helens Erupted 1980 March earthquake under mountain April large bulge noticed May volcano erupted Avalanche of rock and ash Ash cloud 10 miles high Eruption lasted nine hours Destruction within 300 km² 7,000 large animals killed Many smaller animals killed Surrounding forests destroyed 200 homes destroyed Mountain reduced by 400 metres Exam hint: You need to be able to describe a volcano you have studied and its effects.

Earthquakes Sudden tremors or vibrations in crust Plates collide or slide past each other Pressure builds along fault line Sudden release of pressure earthquake San Andreas fault line many earthquakes Exam hint: You may be asked to explain what earthquakes are and how they occur.

Earthquakes Focus point beneath surface Epicentre point on surface above focus Tremors strongest at epicentre Greatest damage at epicentre Aftershocks follow earthquakes Exam hint: You need to be able to describe the structure of an earthquake.

Study of earthquakes Seismologist studies earthquakes Seismographs used to measure tremors The Richter scale Show strength of earthquake Ranges from 1-12 Each unit 10 times stronger

Damage caused Loss of life Buildings damaged or collapse Electricity or gas supplies damaged Bridges, road, railway lines damaged Landslides or avalanches triggered Damage to sewers or water supplies Tsunamis and tidal waves triggered How can the damage caused by earthquakes be reduced? Exam hint: You may be asked to describe the damage that earthquakes can cause.

Earthquake in Japan 11 March, 2011 8.9 on Richter scale Triggered a tsunami 40 metres high 130,000 buildings collapsed 1 million buildings damaged 15,000 people died 4.4 million households no electricity or water Nuclear power plant damaged Cost 200 billion Exam hint: You may be asked to name an earthquake you have studied and the damage it caused.

Fold mountains Oceanic plate and continental plate collide Oceanic plate sinks under continental plate Continental plate buckles upwards Magma can move up and form volcanoes Andes Mountains Exam hint: You need to be able to describe how fold mountains are formed.

Fold mountains Two continental plates collide both buckle up Himalayas Indo- Australian and Eurasian plates collide An anticline is an upfold and a syncline is a down-fold

Periods of folding Alpine Highest mountains 30-35 million years ago Alps, Europe Andes, South America Rockies, North America Himalayas, Asia Alpine fold mountains Armorican Low mountains 250 million years ago Eurasian and African plates collided Macgillicuddy s Reeks The Galtees The Comeraghs Exam hint: You must be able to name different periods of folding and give examples of mountains they formed.

Sample answer (i) Name one example of a volcano. Answer: Mount St. Helens (ii) With reference to the diagram, explain how volcanoes occur.

Sample answer Answer: Volcanoes occur where plates separate or collide. Magma rises up from under the earth s surface. It escapes through a fissure or vent. When magma reaches the earth s surface it is known as lava. Lava, hot ash and rocks are thrown into the air. They eventually build up to form a volcanic mountain. (JC HL 2012 Q1B)