Seismic Activity Flashcards
- Earthquakes - Tsunamis
what is an earthquake?
a sudden shaking or trembling of the earth’s surface caused by the seismic waves or earthquake waves that are generated due to a sudden movement (sudden release of energy) in the Earth’s crust (shallow focus) or upper mantle (some shallow focus and all the intermediate and deep-focus earthquakes.
distribution of earthquakes
- The Pacific Ring of Fire accounts for about 68 per cent of all earthquakes.
- A second belt, known as the Alpine Belt (Himalayas and Alps). The energy released in earthquakes from this belt is about 15 per cent of the world total.
- Circum-Pacific Belt, which affects many populated coastal regions around the Pacific Ocean—for example, those of New Zealand, New Guinea, Japan, the Aleutian Islands, Alaska, and the western coasts of North and South America.
how do earthquakes form?
- ) Movements within the Earth’s crust cause stress to build up at points of weakness, causing the rocks to deform.
- ) When the stress finally exceeds the strength of the rock, the rock fractures along a fault often at a zone of existing weaknesses.
- ) The stored energy is suddenly released of intense vibration, or seismic waves spread out from the initial point of rapture. like a ripple on a pond (or a more violent one).
- )These waves are what makes the ground shake and contract large distances in all directions, near focus line, the waves can be very large, making them extremely destructive.
focus
the plate of origin of an earthquake inside the earth.
Epicenter
- point on the Earth’s surface vertically above the focus
- max charge is caused at the epicenter
isoseismic line
a line connecting all points on the surface of the earth where the intensity is the same.
what are the causes of earthquakes?
- plate tectonics
- slipping of the fault line
- human induced
- volcanic activity
causes of earthquakes - plate tectonics - divergent
As the plates move away from one another movement occurs which can create earthquakes. Further earthquakes can be generated as magma moves up through the ‘spreading ridge’.
divergent plate boundary magnitude
- small + frequent
- little risk due to this and their geographic location
divergent plate boundary - depth of focus
crust = thin
focus depth = shallow
divergent plate boundary example
- Mid Atlantic Ridge
- Eurasian plate moves eastward
- North American plate moves west
formation of earthquake - Transform
zone of friction is created as plates move past each other, this happens when the plates move in parallel direction or same direction.
transform - magnitude
high level of risk
depth - transform
shallow - intermediate
transform - example
San Andreas fault
- pacific plate moves north at a different speed to the North american plate
convergent - earthquake formaton
as one plate subducts friction is created. when the friction is overcome, the energy is released. these earthquakes have high potential to create tsunamis
convergent - magnitude
- earthquake focus is considerable in depth
- shallow earthquakes = movement of magma and subsidence occur at shallow depths
- large earthquakes associated with the benioff zone occur at considerable depths depending on the trajectory of the subducted plate boundary
convergent - depth of focus
- this area experiences a range of earthquakes
- most focused in an area names the Benioff zone
- some of the most largest and damaging earthquakes occur here.
- lower magnitude earthquakes are also frequent
convergent - example
Japan Tsunami 2011
- caused by earthquake
- Pacific plate subducted beneath the Eurasian plate
what are most earthquakes usually related to?
- compressional or tensional stresses built up at margins of the huge moving lithospheric plates.
what does the moving of the lithospheric plates cause~?
shallow earthquakes - sudden release of stress along a fault line, or fracture in the Earth’s crust
slipping of land along a fault line
sudden slipping of rock formations along faults are fractures in the Earth’s which happens due to the constant change in volume and density of rocks due to the intensity in temperature and pressure in the Earth’s interior.
how does volcanic activity cause earthquakes?
Caused by the consequent release of elastic strain energy both by tectonic faults and the movement of magma in volcanoes e.g. Mt St Helens eruption 1980.
foreshock
a mild earthquake preceding the violent shaking movement of an earthquake is known as a foreshock