Fold mountains Over millions of years the folding

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Fold mountains • Over millions of years, the folding of rocks creates a landform

Fold mountains • Over millions of years, the folding of rocks creates a landform called fold mountains. • The Himalayas, the Rocky Mountains and the Andes are examples of fold mountains.

Fold mountains • At convergent plate boundaries, the tectonic plates converge and collide. •

Fold mountains • At convergent plate boundaries, the tectonic plates converge and collide. • The compressional force creates immerse pressure. • Rock layers buckle and fold. (folding) • Results in the uplifting and compression of Earth’s crust, forming fold mountain

Fold mountains - Diagrams Buckle and fold – Fold Mountain Compressional Force

Fold mountains - Diagrams Buckle and fold – Fold Mountain Compressional Force

Fold mountains The Himalayas Peak : Mount Everest (between Nepal and Tibet) Elevation :

Fold mountains The Himalayas Peak : Mount Everest (between Nepal and Tibet) Elevation : 8, 848 metres

Fold mountains • Fold mountains are located along convergent plate boundaries

Fold mountains • Fold mountains are located along convergent plate boundaries

Fold mountains - Revision 1. Fig. 1 shows a landform. Identify the landformed as

Fold mountains - Revision 1. Fig. 1 shows a landform. Identify the landformed as a result of the convergence and explain its formation. [5 m]

Fold mountains - Revision 1. Fig. 1 shows a landform. Identify the landformed as

Fold mountains - Revision 1. Fig. 1 shows a landform. Identify the landformed as a result of the convergence and explain its formation. [5 m] • Fold mountain • At convergent plate boundaries, the tectonic plates converge and collide. • The compressional force creates immerse pressure • Rock layers buckle and fold. (folding) • Result in the uplifting and compression of Earth’s crust – forming fold mountain

Fold mountains - Revision 2. Fig. 2 shows a landform. Fold Mountain A Identify

Fold mountains - Revision 2. Fig. 2 shows a landform. Fold Mountain A Identify Fold mountain A, and explain its formation. [5 m]

Fold mountains - Revision 2. Fig. 2 shows a landform. Identify Fold mountain A,

Fold mountains - Revision 2. Fig. 2 shows a landform. Identify Fold mountain A, and explain its formation. [5 m] • Himalayas fold mountain • At convergent plate boundaries, Indian-Australian plate and Eurasian Plate converge and collide. • The compressional force creates immerse pressure • Rock layers buckle and fold. (folding) • Result in the uplifting and compression of Earth’s crust – forming the Huimalayas fold mountain

Rift valleys and block mountains • Rift valleys and block mountains are formed at

Rift valleys and block mountains • Rift valleys and block mountains are formed at divergent plate boundaries.

Rift valleys and block mountains • A fault is a fracture in the rocks

Rift valleys and block mountains • A fault is a fracture in the rocks along which the rocks are displaced. • The tensional forces result in parts of the crust being fractured. • This process is called faulting.

Rift valleys • A rift valley is a valley with steep sides formed along

Rift valleys • A rift valley is a valley with steep sides formed along fault lines. • E. g. East African Rift Valley

Rift valleys • It is formed at a divergent plate boundary when two plates

Rift valleys • It is formed at a divergent plate boundary when two plates move away from each other. • The central block of land subsides (sinks) between two parallel faults due to tensional forces. • A rift valley, which is a valley with steep sides is formed.

Block mountains • A block mountain is a block of land with steep sides.

Block mountains • A block mountain is a block of land with steep sides.

Block mountains • It is formed at a divergent plate boundary when two plates

Block mountains • It is formed at a divergent plate boundary when two plates move away from each other. • When the crusts on either side of the normal faults move apart, they sink and leave the central block standing higher than the rest. • This forms a block mountain, which is a block of land with steep sides.

Rift valleys and block mountains The East African Rift Valley Is formed from the

Rift valleys and block mountains The East African Rift Valley Is formed from the Nubian section of the African Plate and the Somalian section of the African Plate pulling away from one another.

Rift valleys and block mountains 3. Fig. 3 shows a landform. A Identify the

Rift valleys and block mountains 3. Fig. 3 shows a landform. A Identify the landformed as a result of the plate movement. Name landform A and explain its formation. [5]

Rift valleys and block mountains 3. Fig. 3 shows a landform. Identify the landformed

Rift valleys and block mountains 3. Fig. 3 shows a landform. Identify the landformed as a result of the plate movement. Name landform A and explain its formation. [7] • Rift Valley • East African Rift Valley • It is formed at a divergent plate boundary when African Plate move away from Somali sub-plate. • The central block of land subsides (sinks) between two parallel faults due to tensional forces. • East African Rift Valley, which is a valley with steep sides is formed.

Rift valleys and block mountains 4. With the help of well-annotated diagrams, explain the

Rift valleys and block mountains 4. With the help of well-annotated diagrams, explain the formation of a block mountain. [5 m]

Rift valleys and block mountains 5. With the aid of well-annotated diagrams, explain the

Rift valleys and block mountains 5. With the aid of well-annotated diagrams, explain the formation of a rift valley. [5]

What phenomena are found at plate boundaries and how are they formed? • An

What phenomena are found at plate boundaries and how are they formed? • An earthquake is a vibration in the earth’s crust caused by the sudden release of stored energy in the rocks found along fault lines.

Earthquakes • Extent of earthquakes - The Richter Scale is used to measure the

Earthquakes • Extent of earthquakes - The Richter Scale is used to measure the magnitude of an earthquake

Earthquakes • Apart from its magnitude, the extent of damage caused by an earthquake

Earthquakes • Apart from its magnitude, the extent of damage caused by an earthquake may vary based on other factors: - Population density time of occurrence level of preparedness distance from the epicentre type of soil

Earthquakes The distribution of the earth’s major earthquakes

Earthquakes The distribution of the earth’s major earthquakes

Earthquakes • Measuring earthquakes - A seismograph records the seismic waves released by an

Earthquakes • Measuring earthquakes - A seismograph records the seismic waves released by an earthquake.

Earthquakes Hazards associated with living in earthquakes zones - Threat of tsunamis - Disruption

Earthquakes Hazards associated with living in earthquakes zones - Threat of tsunamis - Disruption of services - Fires - Landslides - Destruction of properties - Destruction of infrastructure - Loss of lives

Hazards associated with earthquakes Threat of tsunamis • Tsunami refers to an usually large

Hazards associated with earthquakes Threat of tsunamis • Tsunami refers to an usually large sea wave. • Tsunamis may be formed by: - The movement of the sea floor during a large earthquake at subduction zones; - An underwater volcanic eruption; - An underwater landslide; and - A landslide above sea level which causes materials to plunge into the water.

Hazards associated with earthquakes

Hazards associated with earthquakes

Hazards associated with earthquakes • In 2004, a 9. 2 magnitude triggered a tsunami

Hazards associated with earthquakes • In 2004, a 9. 2 magnitude triggered a tsunami with waves spreading throughout the Indian Ocean. Aceh before and after the tsunami hit the area

Hazards associated with earthquakes The spread of the tsunami waves caused by the tsunami

Hazards associated with earthquakes The spread of the tsunami waves caused by the tsunami

Hazards associated with earthquakes Disruption of services • An earthquake can disrupt services such

Hazards associated with earthquakes Disruption of services • An earthquake can disrupt services such as the supply of electricity, gas and water. • The earthquake in Kobe, Japan, in 1995 disrupted electricity, gas and water supplies to about a million of Kobe city’s 1. 4 million residents. Fire • Earthquakes may rupture gas pipes and this can provide fuel to start fires. • For example, the earthquake in Kobe, Japan, in 1995 caused extensive fires.

Hazards associated with earthquakes Landslides • Landslides are rapid downslope movements of soil, rock

Hazards associated with earthquakes Landslides • Landslides are rapid downslope movements of soil, rock and vegetation. • Mudflows may also occur when there is heavy rainfall. Destruction of properties • Earthquakes can cause destruction to many homes. • People may be without homes after the disaster.

Hazards associated with earthquakes Destruction of infrastructure • Earthquakes may cause cracks to form

Hazards associated with earthquakes Destruction of infrastructure • Earthquakes may cause cracks to form in infrastructure such as roads and bridges. • Transportation can be disrupted as it is unsafe to use the damaged roads.

Hazards associated with earthquakes

Hazards associated with earthquakes