WA1 - Living with tectonic Hazards Flashcards
(18 cards)
Natural Hazard
A natural hazard is a perceived natural event that has the potential to threaten both life and property
Natural Event
- A natural event is a naturally occurring event that threatens human lives and causes damage to property
- A natural event in an uninhabited place becomes a hazard in a populated one
Natural Disaster
- A natural Disaster is the realisation of an hazard when it causes a significant impact on a vulnerable population
- A disaster is a sudden , calamitous event that causes serious disruption of the function of a community or a society causing widespread human and material damage .
Recording of a Disaster , criteria
- 10 or more people killed ,
- At least 100 affected
- A deceleration of a state of emergency by the relevant government
- A request by the national government for international assistance
Inner Core
1200KM
5000-7000
Solid State
Iron and Nickel , known as the NiFe layer
Outer Core
2300KM
3000-4000 *c
Liquid
Iron and Nickel in the Molten Layer
Lower Mantle
2900KM
800-3000*C
Solid and Molten state of Iron and MAGNESIUM
Upper Mantle + Aesthenosphere
150-250KM
less than 800*c
Liquid and Solid of IRON AND MAGNESIUM
Oceanic Crust
Thinner but denser than Continental Crust
5-8KM
Made up of basalt less than 200 Million years old
Continental Crust
Thicker but less than Continental Crust
35-70Km
Granite
4 Billion years old and found under shallow seas
How do tectonic Plates move
Tremendous heat found in Earth’s core causes rocks
in mantle to melt and become magma.
● Liquid mantle material, called magma, is intensely
heated and expands, rising up.
● Rising and spreading lava pulls the plates apart,
causing them to diverge as they are dragged along
and move away from each other.
● Then the magma cools and sinks, pulling the plates along.
● The sinking mantle material heats up again as it nears the core, creating a convection current and causing the whole process to
repeat.
Explain Oceanic-Oceanic Convergence
Associated landforms -> Oceanic trench and island arcs
Process -> Vulcanizing and subduction
The denser oceanic plate is subducted under the less dense plate which bends downward into the mantle , forming a trench . During the subduction , the crust mantle melts becoming magma , which gains heat and expands upwards and the magma cools and forms an island arc
After the subduction is complete , the plates are melted and destroyed , new plates are formed at divergent plate boundaries
What is a trench
A trench is a long narrow depression in the sea floor
Explain Continental-continental convergence
Associated Land forms -> Fold mountains by the process of folding
When two continental plates converge , they do not subduct due to their similar densities and hence push into one another , reason is its thickness
-The resultant compression force creates immense pressure which causes the rocks to buckle and fold-> This forming fold mountains
Explain Oceanic - Continental Convergence
Associated Landforms -> Oceanic trenches , Fold mountains , volcanoes
Oceanic plates subduct under the Continental plates as they are denser .
The downward movement of the plate dips into the mantle and may produce a deep oceanic trench , the downward movement of the oceanic plate may cause the melting of the mantle material above it , which produces magma that escapes through any leaks or fractures and when it escapes through the vents onto the surface , a volcano is formed
Explain Oceanic-Oceanic divergence
Associated landforms -> Mid oceanic ridges , and volcanic islands
Process - Sea floor spreading
As the two plates move apart they form fractures @ the boundary where magma then rises up from the zone of divergence cools and solidifies to form new sea floor known as a mid oceanic ridge , as the plates move apart the ridges move away and new ridges are formed , the youngest ridge is closest to the zone of divergence while the older ones are more spread apart
At various points in the mid oceanic ridge magma may build up and solidify to form undersea volcanoes that eventually grow above sea level to form volcanic islands
Sea floor map
Darker -> Normal polarity
Lighter -> Reversed polarity
Newer sea floor is closer to the mid oceanic ridge
Continental - Continental plate divergence
Associated landforms -> Rift valleys and block mountains + volcanoes