Locations at risk from tectonic hazards Flashcards
The global distribution of earthquakes
- the main earthquake zones are found along plate boundaries
-about 70% of all earthquakes are found in the ring of fire in the pacific ocean
-most powerful earthquakes are on convergent plate boundaries - ## rare intra-plate earthquakes can occur due to things such as old fault lines
the global distribution of volcanoes
- around 500 active volcanoes around the world
- around 50 erupt each year but the strength of a volcano is determined by how much gas is dissolved in the magma and how easily that gas can escape
distribution of divergent boundaries
- most clearly displayed at mid-ocean ridges
- at these locations there are many large numbers of shallow focus low mag earthquakes.
- most are under the sea
divergent boundaries and earthquakes
- new oceanic crust which is thinner and denser than the continental is created
- earthquakes here are frequent, small and typically low hazard risk due to them being normally in the ocean and they do not typically trigger tsunamis
conservative boundaries and earthquakes
- more risk
- san andreas fault is a good example- in california
- the pacific plate moving north is creating friction against the north american plate thats moving north at a different speed
convergent boundaries and earthquakes
- typically when one plate subducts under the other strain builds over time in the subduction zone and the friction between the two rock masses is overcome releasing energy.
convergent boundaries and volcanoes
- when a subduction zone is created by the oceanic plate being thrust underneath the continental due to the continentals buoyancy.
- volcanoes typically appear above the magma that forms directly above down-thrust plates
- create composite volcanoes which are more violent- andesitic magma which is very runny and viscious
divergent boundaries and volcanoes
- create rift volcanoes where plates diverge from one and other
- shield volcanoes which are less violent- basaltic magma which is thicker and less viscious
hotspot volcanoes
- found in the middle of tectonic plates
- due to mantle plumes - area in the mantle from which heat rises as a hot thermal plume from deep in the earth
- high heat and low pressure at the base of the lithosphere enable melting of the rock.
- magma rises and escapes through cracks in the earths crust and erupts to form a volcano
- as the tectonic plates move over the stationary mantle plume the volcanoes move away and a new one forms in its place
- the old volcanoes cool and subside creating islands
- example of chain volcanoes can be seen in the hawaiian islands
explain plate tectonic theory
a theory explained more than 60 years ago to explain large scale movements of the lithosphere
-based around evidence such as sea-floor spreading, ocean topography and paleomagnetism
what is paleomagnetism
- results from the iron in a zone of magma lining up with the earths polarity at the time of cooling
- scientists can then use this to determine historic periods of large-scale tectonic activity through the reconstruction of relative plate motions
what are convection currents
- thought to be a possible driving force for the movement of plate tectonics
- The heat from the core is transferred to the mantle. Liquid rock, close to the core, is heated and rises. When it reaches the crust it is forced sideways as often it can not pass through the crust. The friction between the convection current and the crust causes the tectonic plate to move. The liquid rock then sinks back towards the core as it cools. The process then repeats.
what is sea floor spreading
-the formation of fresh areas of oceanic crust which occurs through the upwelling of magma at mid-ocean ridges and its subsequent outward movement on either side.
what is a benioff zone
- an area of seismicity corresponding with the slab being thrust downwards in a subduction zone
- the different speeds and movements of rock at this point produce numerous earthquakes
- it is the site of intermediate/deep-focused earthquakes
what is a locked fault
- a fault that is not slipping because the frictional resistance on the fault is greater than the stress across the fault- its stuck
- these faults can store massive amounts of energy for long periods of time and is eventually released in a large magnitude earthquake
- the 2004 indian ocean tsunami was the result of a mega-thrust locked fault