Hazardous Earth Flashcards
(83 cards)
define a hazard
a threat (natural or human) that has the potential to cause loss of life, injury, property damage, socio-economic disruption or environmental degradation.
what two ways is the structure of the earth defined as?
Concentric structure defined in two ways - chemical composition and mechanical properties
what components are present in the chemical composition structure?
crust:
solid outer layer, silica-rich, 30-40 km thick in continental areas less dense, made of granite granite
oceanic crust denser but thinner (5-8 km) and made of basalt
Mantle:
Denser rock underneath crust, extending down 2900 km to core-mantle boundary (CMB), richer in iron and magnesium
Chemical changes occur in mantle transition zone (MTZ) from 410-660 km
what componants are present in the mechanical property system?
Lithosphere - cool, brittle outer shell, comprising crust and uppermost, rigid part of mantle. Broken into lithospheric plates (tectonic plates). Deeper into earth temperatures increase. At 1300 degrees mechanical properties change from elastic to plastic, making the base of the lithosphere. Most have continental and oceanic crust.
Asthenosphere - solid mantle rock, but hotter and under greater pressure so more ductile. Important role in tectonics allowing rigid plates to slide over it
Outer core - molten iron, convects, generating magnetic field
Inner core - iron but solid due to greater pressure despite being 5400 degrees
what are the role of convection currents and why are they important for geography?
Mantle convection fundamental to tectonics providing a mechanism by which earth cools over time through the formation and movement of plates at the surface
It was thought plates were moved by currents caused by heating but geologists now believe it is driven by cooling from above
how do convection currents work?
at subduction zones, slabs of cold oceanic crust become dense enough to sink into mantle (downwelling) - causes lithosphere to be stretched and thinned elsewhere (constructive plate margins), reducing pressure on underlying mantle rock causing it to upwell in response
upwelling thought to occur in thin column plumes rising from the core-mantle boundary - linked to subducted slabs reaching the bottom of the mantle
what is the disadvantage of convection currents
complex pattern and also not all understood yet
what did the theory of continental drift suggest?
1915 Wegener published theory of continental drift the idea that rather than being fixed the continents were moving
He proposed the 250Ma continents were joined into supercontinent (Pangaea) which broke up
what is the evidence for the continental drift theory?
Jigsaw fit - coastlines are complimentary
Geological fit - similar mountain chains/rock outcrops on either side of oceans
Ancient glaciations - glacial deposits and striations formed 300Ma suggest a single ice sheet once covered a massive land mass close to south pole
Fossil records - fossils found on either side of the oceans but nowhere else e.g. Mesosaurus in SA and Africa
what is the theory of sea-floor spreading?
1931 Holmes - ocean floor is continuously recycled, sinking in some areas and replaced elsewhere
1950s Hess proposed sea-floor spreading as a mechanism
how does paleomagnetism provide evidence for sea-floor spreading?
Iron-rich minerals in lava align with Earth’s magnetic field
Shows every few 100,000 years magnetic field reverses polarity
Vine and Matthews 1963 - rocks either side of the Carlsberg mid-ocean ridge mirrored each other in striped pattern of normal and reversed polarity - new ocean floor produced by volcanic activity at ridges and spreads as plates diverge
how does the age of sea rocks provide evidence for sea-floor spreading?
Gradually increases with distance each side of a mid-ocean ridge
Discovered in late 1960s due to deep-sea drilling project which dated rocks using fossils
why do theories change over time and what is the most recent theory?
With new evidence, ideas became more sophisticated and new theory of plate tectonics was created.
what is the global pattern of plates and plate boundaries?
1940s detailed maps of seismic activity showed most earthquakes concentrated in narrow bands with large aseismic areas in between. Volcanoes had a similar pattern - idea rigid lithosphere broken into plates
7 large and several smaller lithospheric plates - move over asthenosphere few cm per year
what is a convergent (collision) boundary?
plates move towards each other (no subduction)
what is a convergent (destructive) boundary?
plates move towards each other (denser plate subducts)
what is conservative (transform) boundary?
plates move alongside each other
what is a divergent (constructive) plate boundary?
plates move away from each other
what are the characteristics of divergent boundaries?
Sea floor spreading - plates pulled apart, lithosphere stretches and thins reducing pressure on asthenospheric mantle - upwells and partially melts - magma rises to form new crust
Mid ocean ridges (MORs) form 60,000km long chain of submarine volcanic mountains, warm, thin lithosphere over areas of upwelling
Transform faults - offset MORs every 50-500km, generating shallow earthquakes. Slow spreading MORs have central rift valley, formed where crust moves up along vertical faults as it spreads from ridge axis
Ridge push - MORs have higher elevation than surrounding ocean floor - plates slide down either side due to gravity pushing the rest of the plate away from ridge
what are the characteristics of C-O convergent boundaries?
Denser oceanic plate subducts beneath continental plate due to gravitational force, rigidity of plate allows it to bend elastically under stress causing deep ocean trenches
Sea-floor sediments scraped off oceanic plate create and accretionary wedge - adds new material to continent so grows laterally. Continental lithosphere folded and faulted produces fold and thrust mountains
Subducting oceanic lithosphere becomes more dense as it falls due to higher temperatures, pressure. Greater gravitational mass and increases capacity to pull - slap-pull (cold dense slab of oceanic lithosphere subducts into mantle pulling rest of plate with it)
Release of water from oceanic lithosphere into overlying wedge of mantle, lowering melting point and causing partial melting
Less dense magma rises through overlying continental lithosphere forming volcanoes
Earthquakes common due to faulting in subducting slab - Wadati-Benioff zone (sloping plane of earthquake foci) goes from trench down to 700 km
what are the characteristics of O-O boundaries?
Similar features and processes
Denser plate (older and cooler) subducts
Magma generation forms island arcs (chain of volcanic islands formed on overriding plate)
what are the characteristics of C-C boundaries?
Ocean has already been subducted and who continents collide
Continental lithosphere not sense enough to sink into mantle so no volcanoes or subduction
Folded and faulted into mountain chains (violent earthquakes) and intense pressure (metamorphism) e.g. Himalayas
what are the characteristics of conservative plate boundaries?
Jerky and sporadic movement
Frictional forces lock sections of boundary together along faults, building up strain energy.
When slips occur energy is released as earthquakes - no volcanic activity
E.g. San Andreas fault (Pacific-NA plate)
what are the factors that affect different types of volcano?
Eruptions (explosivity, materials ejected and size/shape of landforms) affected by: composition of magma/lava (high silica content are more viscous than mafic)
Convergent usually produce silicic magmas, divergent boundaries and hot spots mafic
Dissolved gas in magma affects the force of eruptions