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features of a stratovolcano
steepsided, viscous lava, explosive, layers of ash and lava, destructive plates
features of shieldvolcano
gently sloping sides, runny and thin lava, less explosive, frequent eruptions, conservative plates
dangers of volcano
lava, ash, pyroclastic flow, lahars, volcanic bombs
opportunities of volcano
beauty, jobs from tourism, mining, fertile land, geothermal energy,
reducing impacts of volcano
thermal imagery and temperature can predict, hazard mapping and risk zones
hazards of earthquake
ground shakes, landslides, building fall, tsunamis, fires, infrastructure destroyed
why people still live near earthquake(applies to volcano too)
employment, sentiment, friends and family, cannot afford to move, confidence in protection methods, don’t think risk is high enough/will happen
reducing impacts of an earthquake
prediction, seisometers, preparation, early warning drills, protection - steel frames means buildings can sway, deep foundations means less likely to collapse, shock absorbers absorb tremors, shatteproof windows less likely to be injured by glass breaking
types of erosion
erosion is the wearing away of rock by natural processes
hydraulic action, water forces its way into cracks and causes pressure which makes the cracks bigger and large pieces of rock fall off
abrasion, rocks carried by water wear bed and banks down thru a sandpaper action
attrition, material in load hits other material and gets smaller and more rounded
solution, minerals in rocks get dissolved
types of transportation
transportation is the movement of eroded material in a rive
traction, large material rolled along river bed, not enough strength to pick up
saltation, load bounces along river bed
suspension, material held up and carried in river flow
solution, river carries dissolved sediment
deposition
river loses energy as it gets slower, puts load down on bed banks floodplain
v shaped valley formation
vertical erosion occurs due to low discharge
weathering attacks valley sides
gravity pulls weathered material into river
increased load = increased erosion
further vertical erosion and erosion of sides
steep v shaped valley formed
Waterfalls and gorges
hard rock lies over soft rock
soft rock erodes quicker as less resistant
steep gradient and waterfall created
rock is undercut
plunge pool formed below
rock collapses under own weight
waterfall retreats
over time steep sided valley - gorge - forms
potholes
hollows in river bed
sediment scours bed
depressions exist
eddies(swirls) form
pebbles spin and erode downwards#
hollow/pothole formed
meander and oxbow lake
water flows faster on outside bend of river, as deeper water = less friction
erosion occurs here
inner bend is shallower, slower water due to increased friction
deposition occurs here
helicoidal flow takes neroded material to shallwo side
slip off slope formed on inner bend, river cliff other side
bend gets more pronounced as this continues
neck of meander narrows
when water levels high, river cuts across meander
new chaneel formed with loop
sediment deposited on inner bend where loop connects
loop is cut off from river and oxbow lake forms
floodplains and levees
floodplain is flat land next to river in lower course formed by lateral erosion and deposition. levees are mounds of deposited sediment
when a river floods it deposits load on floodplain as energy lost
biggest deposited first
sediment builds up and forms mounds
levees, or large natural embankments close to the channel form
made of sand, silt and clay - alluvium
delta
depositional landform at river mouth, when river meets sea must slow down
depositionn occurs
if material not washed away builds up and blocks channel
delta formed as channel splits in varies different ways
topset, foreset, bottomset beds, with going from coursest and shortest to finest and furthest
arcuate is fan shapeed, birds foot is lots channels jutting into sea, curspate is a arrow channel with sides eroded
causes of flooding
heavy consistent rain, rapid snowmelt, steep slopes, saturated ground, deforestation, urbanisation
impacts of flooding
food shortages, injury and death, property damage, power cuts, contamination of water, ecosystems destroyed
managing flooding - hard engineering
barriers and floodwalls, embankments, levees all allow river to hold more water before flooding
canals and waterways increase chanel and control where water goes,
dredging and straightening removes meanders, crosses faster and more channel
dams control flow by blocking
managing flooding - soft
afforestation, water interception thru trees
water allowed to flow into less valuable areas such as washlands
land use zones, certain buildings allowed at certain distances relative to how valuable it is and risk
opportunities of a river
agriculture, trade, HEP, jobs thru tourism, transport, domestic uses such as cooking cleaning washing drinking
what affects a coasts shape
rock type, coastal defences, power of waves
what affects wave energy
wind speed, distance of open water where wind is blowing - fetch - length of time wind has been blowing
destructive waves and beach formed
high energy, high, strong backwash and weak swash, destroys beach, drags material back, steep beach
constructive waves and beach formed
flat, low, low energy, strong swash and weak backwash, deposition and gently sloping beach
cove formation
concordant coastline, layers of rock parallel to coastline, hard rock eroded slowly, breaks through to soft rock, erodes more, cove formed
headlands and bays
discordant coastline, alternating layers of soft and hard rock perpendicular to coastline
soft rock less resistant so eroded quicker
hard rock more resistant so eroded slower
headlands and bays formed, headland are bits of hard rock jutting out, bays between them where soft rock eroded
wave cut platforms and cliffs
water erodes the base of cliff of the coast at high water mark
wave-cut notch formed, wave has undercut rock
further erosion makes cliff above unstable
cliff collapses, waves carry away eroded material
wave cut platform forms
process repeats, cliff and coast retreat
caves arches stacks and stumps
happens on a headland, waves are refracted and attack sides of healand
attacks any weaknesses/cracks, opens up a large crack through hydraulic action
grows into a cave through widening of crack and erosion
gets larger, breaks through headland to form arch
arch foundation gets thinner and wider due to erosion and weathering
arch collapses and forms a stack
eroded and forms a stump
process of longshore drift
waves approach beach at angle due to prevailing wind, swash approaches at this angle
waves hit coastline and travel up beach, swash moves sand in this direction
backwash comes straight back down the beach due to gravity so moves sand back down
process repeats, material moved along beach in zig-zag manner
spit formation
material is moved along beach through longshore drift
Once they reach a headland/change in coast shape, material is deposited in calmer water here
more deposition occurs as result of higher friction
spit extends in length, marshes develop behind it with salt loving plants’ roots keeping mud together
wind may change direction and form hooked end
fully extended when force of tide prevents any more deposition
sand dune formation
A loose sand hill stabilised by vegetation. Needs constructive waves for deposition, large supply of sand, high tidal range, marram grass and obstacles
Windblown sand is deposited against an obstruction such as driftwood
More sand particles are caught
Dunes grow in size
Vegetation begins to grow e.g. marram grass, more stable
traps more and gets larger over time
dunes get bigger and bigger, as more and more plants grow, with organic matter growing. embryo → fore → yellow → grey → mature
coral reefs - location and characteristics
diverse underwater ecosystem, made of coral polyp and exoskeleton of limestone, algae live inside with symbiotic relationship (respiration and photosynthesis). grows upwards, located 30 degrees north and south
coral reefs conditions required
warm water between 18-27 - encourages year round growth
shallow water not more than 60m deep - sunlight can penetrate
water free from sediment - not damage coral
plentiful supply of oxygen and plankton - so organisms can grow and food supply
calm water - prevents destruction of coral
alkaline water 8 and above - acidic water kills coral
coral reef opportunities
habitats for species, sea food, tourism, coastal protection, medicinal compounds, shells can be used in jewellery
coral reefs threats and management
pollution from sunscreen, overfishing, used in jewellery, damage from tourists trampling, sand and limestone used in construction
reduce greenhouse gases, marine protected areas, reef restoration projects, public awareness campaigns, coral safe sunscreen
mangroves location and characteristics
shrubs/trees that grow on coast in equatorial conditions, adapted to salty conditions, 30 N and S. densely packed trees with aerial roots and shiny leaves grow in shallow muddy water
mangrove conditions needed to survive
temp above 20 degrees, temp range max 5
gentle wave action, no strong currents
high salinity
large tidal range
low shore slope
mangrove value
used for coastal protection from storms and erosion, food, fuel, tourism, medicinal compounds
mangrove hazards and management
pollution, increased salinity due to climate change, cleared for better beach view, converted to rice paddies, overharvested for fuel
protected areas, education, restoration campaigns, penalties
opportunities of the coast
agriculture - flat and fertile land
jobs and local income for fishermen
tourism as people want to go to sandy beaches
hazards of the coast
erosion, land retreats, things at risk
mass movements like rock falls cause death
flooding destroys crops
tsunamis destroy livelihoods
hurricanes and storms, PTSD
managing coastal erosion
sea walls and rock armour, gabions reflect wave energy/ absorb wave energy
groynes prevent longshore drift, sand remains on beach, friction, absorb wave energy
cliff regrading, cuts cliffs and gentle slopes to stop slumping
beach replenishment, place sand and pebbles on beach
managed retreat, low value areas allowed to be eroded to protect land in other areas
dangers of a tropical storm
death/injury
habitats destroyed
floods destroy homes
infrastructure destroyed
evacuation and homelessness
stevenson screen location and reasons
white, reflects sunlight to prevent instruments inside heating up
slats, allow air to circulate freely for accurate temperature and humidity
elevated, prevent it from being distorted from ground heat and protect it from being damaged
in the open, away from buildings which give off heat and trees which cause shadow, away from public/fenced to prevent tampering with
cloud types
cirrus = high, alto = medium, stratus = layers, cumulus = heaped, nimbus = rain and dark
rainforest ecosystem
high biodiversity, 50-80% of worlds species
not very fertile soil, constantly leached, but nutrients rapidly cycled due to high decomposition. top layer is fertile, but no build up
ground 0m, shrub 10m, under canopy 15m, canopy blocks sunlight, 30m, emergent = 45m
hot desert ecosystem
low biodiversity as few plants can grow there
little plant growth due to extreme temps and low water
lack of organic matter so soil is lacking in nutrients, course and sandy