Paper 1 review Flashcards
How are fold mountains formed?
Tectonic plates converge
Driven by convection currents
Results in compression
Upfolding and uplift
Of sediment
To produce fold mountains
How ocean trenches and ridges are formed
Ocean trenches formed at converging plate boundaries by the subduction of one plate below the other causing a deep-sea trench. Ocean ridges are formed at divergent plate boundaries leading to the escape of magma which will produce ocean ridges
Conditions for braiding
Large input variations
High sediment load
Coarse sediment load
Steep slopes
Opposite for meandering
The Walker circulation
Trade winds
Piling of warm water
Upwelling of cold water
Active convection
Pressure
Dry and wet
Increasing slope stability
Afforestation: increases internal strength
Netting: contains debris or rocks
Pining: increases strength
Grading: reshaping to a specific slope
The role of water in movement
Rainsplash in terms of the kinetic energy of raindrops being enough to dislodge soil particles which, if there is a slope gradient, will move down. Bare surfaces needed. For sheetwash, smooth surfaces are needed where infiltration capacity is exceeded. Similar for rills but surface irregularities mean water flow is concentrated in channels. Soil heave, soil creep, solifluctuation and mudflows by wetting and drying
Factors influencing weathering
Temperature: freeze-thaw, insolation, salt crystal
Precipitation
Rock type and structure: greater in well jointed rocks will bedding planes
Pollution
Radiation balance
(incoming solar radiation + atmospheric counter radiation) - (reflected solar radiation + outgoing terrestrial radiation)
Daytime energy budget
Incoming solar radiation
Reflected solar radiation
Energy absorbed at surface
Sensible heat transfer
Latent heat transfer
Longwave radiation
How ocean currents affect wind belts
Winds across the sea cause surface currents
Trade winds pull surface water west-east
Coriolis deflects right so north
Westerlies push east (clockwise)
In southern hemisphere deflects left (counterclockwise)
Gyres due to circular flow
Wind drives these away from coasts
Winds from high to low pressure
Warm surface water in warm area
Exposes colder water
Sensible heat transfer
The transfer of heat into or out of an area by convection, conduction or advection changing temperature rather than phase
Latent heat transfer
Absorbed ore released by evaporation or condensation by a substance during a phase change
Abrasion
The wearing away of the river bed and bank by load
Most effective in upper course
Creates V-shaped channel
Hydraulic action
Force of flowing water to dislodge particles or fragments into the channel
Collapse and retreat of banks
Lateral erosion
Widens channel
Attrition
Constant collision and grinding of sediment, wearing down bedload
Impacts downstream efficiency and reduces size and friction
Solution
Removal of soluble minerals along with transportation
Eroded material dissolved and carried
River energy not important
In humid tropics, chemical weathering is efficient so solution is important
Reasons for different rates of weathering
Higher water content is faster
Result of lubrication of failures
Increase of pore water pressure reducing internal cohesion
Faster on steeper slopes
Rapid increase of strength
Particle by particle is slower
Rockfalls are fast due to lack of support
Vegetation influences movement
Suspension
Fine particles carried without touching channel
More turbulent means larger particles can be transported
Saltation
Skipping of rocks along river bed
Cumulative process
Traction
Sliding, rolling or hopping
Only occurs at high energy levels to move coarse bedload
Raindrop formation
Coalescence involves the merging of smaller water droplets in warm clouds to form larger raindrops
Hail
Updrafts carry water droplets to heights where temperatures are below freezing so they freeze upon contact with ice nuclei, forming hailstones
Dew
Formed when objects on the ground cool below dew point temperature causing water vapour in the air to condense
Snow
Form due to the direct transformation of water vapour into ice crystals
Temperature and humidity influence shape and size of snowflakes
Areas closer to poles or higher altitudes are more likely to experience snow