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Tectonics - Chapter 1 (Plate Boundaries (Divergent (Constructive)…
Tectonics - Chapter 1
Plate Boundaries
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Divergent (Constructive)
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Shallow Focus ,Low magnitude
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Earthquakes
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Stages Of An Earthquake
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4: The Brittle Crust then rebounds either side of the fractures which is the ground shaking (earthquake)
Seismic Waves
Priamary (P Waves)
Vibrations caused by Compressions like a shunt through a connected line - spreading at about 8km/sec
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Secondary Hazards
Tsunamis
Most distinctive Earthquake causes secondary impact- Caused by seabed displacement where apart of the sea floor drops often due to an earthquake creating a displacement of water and a series of tsunami wave
Characteristics: Long wavelengths, typically 150-1000km, Low Amplitude (Wave height) 0.5-5m, Fast Velocities of uptown 600 KpH in deep water
Liquefaction
When Highly saturated Ground/Soil substantially loses strength and stiffness in response to an applied stress such as an earthquake
Effect: Building and Structual Loss, Take out supply networks , ground tilting (60 degrees in Japan
Landslides
Earthquakes often occurring mountainous locations and landslides, avalanches and rockfalls can cause huge damage in areas with significant relief- studies show that below a magnitude 4 landslides are very rare
Effect: Building Structural damage, Loss of life and Environmental damage
Volcanoes
Primary Hazards
Pyroclastic Flows
Result from the frothing of molten magma in the vent of the volcano. The bubbles burst explosively to eject hot gases and pyroclastic material, which contains glass shards, pumice, crystals and ash of uptown 1000 degrees C
Tephra
When a volcano erupts it all sometimes eject solid material such as rock fragments into the atmosphere that can be f significant size causing extensive damage
Lava Flows
If Fast moving can endanger human life with the viscosity decent on the salon dioxide, on steep slopes speed scan reach uptown 15m/sec burnins all in its path
Volcanic Gases
Many types of gases such as sulphur dioxide and carbon dioxide a colourless odourless gases can be emitted in large volumes. The high density of some of these gases causes them to sink and can accumulate in valleys posing a danger to inhabitants.
Secondary Hazards
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Jokulhlaups
type of catastrophic glacial outburst flood . They are. hazard to people and infrastructure and can cause widespread landform modifications occur when a volcano erupts under a glacier melting the ice that the suddenly bursts through