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28 Terms

1
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whats a hazard, natural hazard and disaster

  • A hazard is an event which has the potential to cause harm to the environment, people or the economy

  • A natural hazard is an event caused by environmental processes

  • A disaster occurs when harm actually occurs to the environment, people or the econom


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give me examples of Tectonicearthquakes,+ geological hazards, cllimate and meteorological hazards and Biological hazards

  • earthquakes, volcanic eruptions, landslides

  • Drought Blizzard/snowstorm/sandstorm Heatwave

  • pests and disease


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how natural hazards can be categorized

  • Magnitude - the strength/power of the event

  • Frequency - how often the event occurs

  • Size - the area covered by the hazard

  • Duration - the time a hazard event last


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what are tropical cyclones + their chracteristics

  • rotating, low-pressure systems (below 950mb) aka hurricanes, cyclones and typhoons

  • heavy rainfall high

  • wind speeds (over 119 kmph)

  • high waves and storm surge


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how magnitude of cyclone is measured

Saffir simpson scale 1-5

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whatr earthquakes +how do they happen

  • An earthquake is a sudden, violent shaking of the ground

  • Earthquakes are the result of pressure building when tectonic plates move


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what the focus + epicentre of an earth quake + how to measure magnitude

  • The epicentre is the point on the Earth's surface directly above the focus

  • The focus is the point at which the earthquake starts below the Earth's surface

  • Richter Scale or the Moment Magnitude Scal 4-10


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how do volcanoes form, where do they occur + where dey found

  • form when magma erupts onto the Earth's surface as lava

  • constructive (divergent) and destructive (convergent) pb’s

  • ctive volcanoes are located around the rim of the Pacific Ocean called the 'Ring of Fire


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what are hotspots

  • Hotspots occur away from plate boundaries and are plumes/columns of magma which escape through the Earth's crust


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Measuring eruption magnitude

  • magnitude of a volcanic eruption is measured on the Volcanic Explosivity Index (VEI)

  • weird circle..?


<ul><li><p>magnitude of a volcanic eruption is measured on the Volcanic Explosivity Index (VEI)</p></li><li><p>weird circle..?</p></li></ul><p></p>
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formation of tropical cyclone

  • Warm seawater (27°C or over) around the tropics

  • There are high levels of evaporation and condensation of water vapour from warm water leading to cumulonimbus cloud formation

  • The high levels of evaporation and condensation of water vapour provide energy for strong winds

  • Strong Coriolis Force close to the equator makes winds spin and moves them away from the equator

  • The tropical cyclones move westwards due to east-west winds in the tropics and strengthen as they move over warm waters


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Tropical cyclones require specific conditions to form

  • Sea surface temperatures over 27°C

  •   Between 5° and 30° north and south of the equator

  • Low wind shear

  • A deep layer of humid air

  • in low pressure area below 950mb


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features/ characteristics of tropical cyclone

  • Heavy rainfall High wind speeds (over 119 km/h)

  • Storm surges 

  • Calm eye

  • Highest winds and heaviest rain in the wall of the eye


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volcanic eruptuion n earthquakes take place give examples

  • at plate boundaries there are 4 of them

  • Constructive (divergent)

  • Destructive (convergent)

  • Collision

  • Conservative (transform)


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Constructive (divergent) plate boundary

  • At the constructive boundary, the plates are moving apart

  • The Mid-Atlantic Ridge is an example of a constructive plate boundary

  • Both volcanic eruptions and earthquakes can occur at this type of plate boundary


<ul><li><p>At the constructive boundary, the plates are moving apart</p></li><li><p> The Mid-Atlantic Ridge is an example of a constructive plate boundary </p></li><li><p>Both volcanic eruptions and earthquakes can occur at this type of plate boundary</p></li></ul><p></p>
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Destructive (convergent) plate boundary

  • At a destructive (convergent) plate boundary, the plates are moving together

  • The denser, heavier oceanic platesubducts under the lighter, less dense continental plat (E+V takes place here)


<ul><li><p>At a destructive (convergent) plate boundary, the plates are moving together </p></li><li><p>The denser, heavier oceanic platesubducts under the lighter, less dense continental plat (E+V takes place here)</p></li></ul><p></p>
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Collision boundary

  • At a collision boundary, two plates of similar density move towards each other

  • Neither is dense enough to subduct, so the land is pushed upwards

  • This process forms fold mountains such as the Himalayas

  • Earthquakes are the main hazard at this type of plate boundary


<ul><li><p>At a collision boundary, two plates of similar density move towards each other</p></li><li><p> Neither is dense enough to subduct, so the land is pushed upwards </p></li><li><p>This process forms fold mountains such as the Himalayas </p></li><li><p>Earthquakes are the main hazard at this type of plate boundary</p></li></ul><p></p>
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Conservative (transform) boundary

  • At a conservative (transform) boundary, the plates move past each other in opposite directions or in the same direction at different speeds

  • Earthquakes are the only hazard at this type of boundar


<ul><li><p>At a conservative (transform) boundary, the plates move past each other in opposite directions or in the same direction at different speeds</p></li><li><p> Earthquakes are the only hazard at this type of boundar</p></li></ul><p></p>
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at which plates do volcanoes often erupt in

  • Volcanoes occur at constructive (divergent),

  • destructive (convergent) plate boundaries

  • hot spot


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<p>Volcanoes at constructive boundarie</p>

Volcanoes at constructive boundarie

  • Constructive plate boundaries often occur under the sea/ocean

  • The lava escapes through the gap left as the plates move apart

  • The lava cools and hardens, forming a new crust

  • At constructive plate boundaries, the lava tends to be runny and eruptions are less explosive

  • These types of eruption form shield volcanoes, which have gently sloping side


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Volcanoes at destructive boundarie

  • The heavier, denser oceanic plate subducts under the lighter continental plate

  • In the subduction zone, the two plates come together, causing friction

  • Friction causes heat and the plate material melts, forming magma

  • The magma rises to the surface through cracks in the crust The cooling lava and ash build up, forming a volcan

  • At destructive plate boundaries, the lava tends to be sticky and produces explosive eruptions

  • These eruptions tend to form composite or stratovolcanoes 


<ul><li><p>The heavier, denser oceanic plate subducts under the lighter continental plate</p></li><li><p> In the subduction zone, the two plates come together, causing friction</p></li><li><p> Friction causes heat and the plate material melts, forming magma </p></li><li><p>The magma rises to the surface through cracks in the crust The cooling lava and ash build up, forming a volcan</p></li><li><p>At destructive plate boundaries, the lava tends to be sticky and produces explosive eruptions </p></li><li><p>These eruptions tend to form composite or stratovolcanoes&nbsp;</p></li></ul><p></p>
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Volcanoes at hot spots

  • At a hot spot, the tectonic plate passes over a plume of magma:

  • The magma rises to the surface through cracks in the crust

  • As the magma erupts and cools, this builds up

  • Eventually, due to the buildup of cooled lava, this may rise above the surface of the water, forming an island

  • As the tectonic plate moves slowly over the magma plume, a line of islands may form, e.g. Hawai


<ul><li><p>At a hot spot, the tectonic plate passes over a plume of magma: </p></li><li><p>The magma rises to the surface through cracks in the crust</p></li><li><p> As the magma erupts and cools, this builds up</p></li><li><p> Eventually, due to the buildup of cooled lava, this may rise above the surface of the water, forming an island </p></li><li><p>As the tectonic plate moves slowly over the magma plume, a line of islands may form, e.g. Hawai</p></li></ul><p></p>
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volcano primary hazards

  • The hazards from the volcanic eruption itself are primary hazards:

  • Ash Pyroclastic flow

  • Lava flow

  • Gas emissions

  • Volcanic bomb


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volcano secondary hazards

  • The hazards created that happen as a result of the primary hazards are secondary hazards:

  • Lahars Acidification

  • Landslide

  • s Climate change

  • Fires Flood


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at which plate boundaries are earth quakes stronger/weaker

  • Earthquakes happen at all plate boundaries

  • At a constructive (divergent) plate boundary, earthquakes tend to be weaker as the plates are moving apart

  • At destructive (convergent), collision and conservative (transform) plate boundaries, earthquakes tend to be stronger


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primary hazard of earth quakes

  • e ground shaking


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secondary hazard of earth quake

  • Collapse of buildings and other structures

  • Landslides

  • Gas leaks 

  • Fires

  • Soil liquefaction

  • Subsidence

  • Mudflows

  • Tsunam


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Earthquake sequence (how it happens)

  • As the tectonic plates move, they can get stuck

  • Pressure builds as the plates continue to try to move

  • Eventually, the plates jolt free, and the pressure is released as energy

  • The point at which the earthquake starts is the focus

  • The epicentre is the point directly above the focus on the Earth's surface

  • The energy passes through the Earth's crust as waves, which are the earthquake

  • Earthquakes can happen as a result of human activity, such as drilling into the crust or mining