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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
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
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
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
how magnitude of cyclone is measured
Saffir simpson scale 1-5
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
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
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
what are hotspots
Hotspots occur away from plate boundaries and are plumes/columns of magma which escape through the Earth's crust
Measuring eruption magnitude
magnitude of a volcanic eruption is measured on the Volcanic Explosivity Index (VEI)
weird circle..?

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
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
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
volcanic eruptuion n earthquakes take place give examples
at plate boundaries there are 4 of them
Constructive (divergent)
Destructive (convergent)
Collision
Conservative (transform)
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

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)

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

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

at which plates do volcanoes often erupt in
Volcanoes occur at constructive (divergent),
destructive (convergent) plate boundaries
hot spot

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
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

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

volcano primary hazards
The hazards from the volcanic eruption itself are primary hazards:
Ash Pyroclastic flow
Lava flow
Gas emissions
Volcanic bomb
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
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
primary hazard of earth quakes
e ground shaking
secondary hazard of earth quake
Collapse of buildings and other structures
Landslides
Gas leaks
Fires
Soil liquefaction
Subsidence
Mudflows
Tsunam
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