Hazards Flashcards
Lithosphere
The solid top layer of crust in which plates are formed, consists of crust and upper mantle
Asthenosphere
Soft plastic like rock in the upper mantle just below the lithosphere
Core temp of earth
5000-7000 degrees c
Evidence of tectonic theory
Jigsaw fit Glacial deposits fossil evidence geological fit tectonic fit
thickness of continental crust
35 - 40 km
thickness of oceanic crust
7 - 10 km
slab pull
when the oceanic crust is pulled into the mantle - at subduction zones (so destructive plate margins)
ridge push
(constructive margins) where magma forces upwards, pushing plates apart
age of continental crust
2 billion
age of oceanic crust
no more than 200 million
types of destructive boundry
collision
oceanic/oceanic
oceanic/continental
density of continental crust
2.7g/cm3
example of a fault line
san andreas
density of oceanic crust
2.9g/cm3
potential cost of an earthquake along the san andreas fault
$33 billion
mineral content of continental
Si Al and oxygen
mineral content of oceanic
Si Mg and oxygen
what plate boundary do fault lines form
conservative
what plates are involved in the san andreas fault
pacific and north american
why are conservative boundaries the most deadly
little warning given and very powerful
landforms associated with constructive boundaries
mid ocean ridge
rift valleys
example of a rift valley
east african rift valley
landforms of an oceanic/continental destructive boundary
oceanic trench
composite volcanoes
earthquakes
fold mountains
features of oceanic/oceanic destructive boundary
earthquakes n tsunamis
ocean trenches
island arcs
which plate subducts in an oceanic/oceanic destructive boundary
the faster moving or marginally denser
example of collision fold mountains
himalayas
features of collision boundaries
powerful earthquakes
fold mountains
example of island arc
caribbean islands
example of oceanic/continental destructive boundary fold mountains
the andes in south america
types of volcano
composite
shield
Why is a continental/continental boundary a collision?
Bc they cannot subduct
Features of a composite volcano
Narrow base Steep sides High Viscous lava Ash
Volcanic hazard types
Lava flows Gases Lahars Ash fallout Pyroclastic flows Acid rain
Features of a shield volcano
Wide base
Non viscous lava
Steam
Gentle slopes
Hazard
a natural event which does (or have the potential to) cause people harm
Lava flows
A mass of flowing or solidified lava
least hazardous
Gases emitted in a volcanic eruption
sulphur dioxide and carbon monoxide are the main ones
Lahars
kinda like mudflows, a mix of water and ash that flows like a river and sets like concrete
Ash fallout
Rain of airborne ash from an eruption
Pyroclastic flows
Flows at high speeds consisting of ash and lava
Most deadly
Acid rain
Gases released from eruption mix with atmospheric water
hazard risk
the probability that a natural hazard may take place
Monitoring volcanoes
Gas emissions
Seismic activity
Geological observations
Gas emission monitoring volcanoes
Sulphur dioxide emitted before eruption it’s easily detectable
Seismic monitoring volcanoes
Seismographs put activity on Richter scale
Geological monitoring volcanoes
Tilt meter measures changes in slope
EDM measures horizontal movement
geophisical hazard
driven by the earth’s own internal energy forces
atmospheric hazard
driven by processes at work in the atmosphere
hydrological hazard
driven by water bodies, mainly the oceans
hazard perception
the way we see and react to hazards, it’s determined by economic and cultural factors
fatalist response
the losses are accepted as inevitable as there is little we can do to control the hazard - may be due to lack of alternatives (economic)
prediction response
as technology increases, the methods of predicting hazards are better
adaptation and adjustment response
natural events are inevitable so by adjusting our lives, the losses can be reduced
This is a realistic n cost effective response for governments
frequency
how often the hazard occurs
magnitude
how strong the hazard is
relief phase
immediate
search and rescue
what does the park model show
the country can improve after an event
rehabilitation phase
weeks or months
infrastructure restores
temporary structures
to allow the reconstruction phase to begin as quickly as possible
reconstruction phase
restoring to the same or better quality of life as before the event
spell the volcanic case study
Eyjafjallajokull
plates involved in icelandic eruption
american plate moved west while eurasian plate moved east at a rate of 2.5cm/year
plate boundary of icelandic volcano
constructive
when was the icelandic eruption
april 2010
rating of icelandic eruption on the vei
4
how thick was the ice cap that melted due to the icelandic eruption
150m thick causing widespread flooding
how many tonnes of co2 was emitted per day into the atmosphere by the icelandic volcano
30 000 tonnes
how much money did airlines and associated businesses lose due to the icelandic eruption
£130 million per day
what percentage of kenya’s economy was discarded due to the icelandic eruption
20% (based on the export of cut flowers and green veg)
how much did shares in air travel and tourism agencies drop by due to the icelandic volcano
4%
how much money did london’s tourism lose due to the icelandic volcano
£120 million
how many farms were destroyed due to the icelandic volcano
20
how many people were evacuated due to the icelandic eruption
800
what was distributed to prevent people choking on ash in the icelandic eruption
face masks
name two short term responses to the icelandic volcano
immediate grounding of air traffic and cut off parts of roads and bridges to prevent further damage from lahars and lava flows
how much did the EU spend in researching the dangers of flying in ash following the icelandic eruption
€6 million
what did the french red cross do to help after the icelandic eruption
set up two emergency shelters to help 400 people
what did the netherlands red cross do after the icelandic eruption
gave 1500 beds for stranded people
why did we study the icelandic volcano
it is hemispheric in scale
what earthquake did i study
nepal
why did i study the nepal earthquake
the magnitude and poor country
what number on the richter scale was the nepal earthquake
7.9
where was the epicentre of the nepal earthquake
between the capital of kathmandu and the city of pokhara
what is the gdp of nepal
$2465/year
which plates were involved in the nepal earthquake
eurasian plate moving towards the indo-australian plate
how rich is nepal
157/185
what tropical storm did i study for a mic
hurricane sandy
where did hurricane sandy begin
western caribbean on 22nd october 2012
where did hurricane sandy move to after developing in western caribbean
travelled north hitting haiti and cuba before hitting the east coast of america
why did i study hurricane sandy
unusual location - too far north
name some factors that influence people’s perception of a hazard
Socio-Economic status Personality Religion / ethnic background Level of Education Past experience Occupation
3 main ways to perceive a hazard
Fear- feel vulnerable
Adaptation- prepare- prevent and protect
Fatalism- part of the area- God’s will
two internal energy sources
Primordial Heat
Radiogenic Heat
primordial heat
Heat left over from Earth’s formation
radiogenic heat
Heat produced by the decay of isotopes like Uranium 238
By far the greatest source, but slowly diminishing
Explain Alfred Wagner’s theory (1912)
Continental Drift- 300 million years ago Pangea existed
Formation of shield volcanoes
Plates move apart
Magma rises to surface, cools = new crust
Sea floor spreading
Layers built by eruptions
shield volcano boundary
constructive
shield volcano example
Eyjafjallajokull, Iceland
formation of composite volcano
Plates move towards eachother Oceanic, denser, subducts Beinoff Zone Less dense molten material rises Layers of ash and lava build
composite volcano boundary
destructive
composite volcano example
Mount Etna, Italy
volcanoes in rift valleys formation
Brittle crust fractures
Areas drop down between parallel faults
Thin crust- forms magma
Magma forces its’ way to the surface
volcanos in hotspots formation
Concentration of radioactive elements below crust
Plume of magma rises
Breaks through surface
vei
volcanic explosivity index Logarithmic scale (0-8) measuring magnitude of eruption by height of eruption column and volume of tephra erupted
disadvantages of the vei
Doesn’t consider climate impact
Ash, lava and lava bombs all treated alike
location of icelandic volcano
Southern Iceland, beneath an ice cap
icelandic volcano how high was the ash plume
11km
where was the dominant lava flow of the icelandic volcano
to the west
why wash the ash from the icelandic volcano distributed at a high velocity
due to the jetstreams above iceland
seismicity
Earth shaking, which can be human induced through fracking, mining and reservoir construction