Weathering Flashcards
(22 cards)
Erosion
Break down of rocks by moving agents that transport material away
(Sea/river/wind)
Freeze thaw (physical)
- Water enters cracks
- Temp falls (night) water freezes + expands (9% in volume)
- Pressure on rock
- Temp rises (day) melts + takes up less room
- More water enters, repeated, weakens, rock breaks into pieces
High rain, fluctuating temp +/- freezing
Exfoliation
- Hot (day) surface expands
- Cool (night) surface contracts
- Repeated, stress, weakens rock
- Outer layer breaks off, process again on layers underneath
High day temp, low night temp
Carbonation
- Rainwater combines with CO2 to form carbonic acid
- Attacks surface + soaks in joints
- Reacts with alkaline limestone to form calcium bicarbonate
- Carried away in solution (soluble)
High rain, high temp (doubles with 10°C rise)
Oxidation
- Oxygen (air) reacts with minerals (metal) in rock - iron
- Changes structure: expands + weakens rock
- Breaks down easily - rust
- Red brown colour, rock crumbles easily
High rain, high temp (doubles with 10°C rise)
Plants
- Roots move along crack + force apart rock
- Widen, weaken + disintegrate (mechanical)
- Release chemicals: carbonic acid (chemical)
High temps (summer) for growth and chemicals
Animals
- Burrow in rock, weakens + breaks down (mechanical)
2. Die, decompose, release chemicals (chemical)
Factors influencing type + rate of weathering
Many minerals, oxygen and water - CHEMICAL
Lines of weakness (bedding planes and cracks) - MORE LIKELY
Coarse grain (sandstone) - QUICKER than fine
Climatic conditions
Weathering rapid in humid tropical areas
Higher temp/rain (chemical) More trees/roots (biological) More animals (biological) More cracks (physical) Rapid decay (chemical) CO2 from decay - acidic rain (chemical) Rate doubles with 10°C rise (chemical)
Opportunities of natural environment (weathering)
Agriculture Tourism (rock climbing) Building (limestone, cement) Education Forestry
Weather and climate
Weather: day to day changes of earth’s atmosphere
Climate: average weather over period of time
Features of Stevenson screen
1.25m above ground - air temp
White - reflect sunlight
Downwards slats - air passes freely, wind doesn’t affect readings
Away from buildings - no effect of local relief
Grass - concrete absorbs heat
Max min thermometer, wet dry bulb thermometer + barometer
Rain gauge (precipitation)
Grass - avoid splashback
No trees/buildings - avoid shelter/water dripping
Remove bottle, empty into measuring cylinder, read at eye level
Every 2 hours/same time
Max min thermometer (highest/lowest temp)
Alcohol expands/contracts, affects mercury, pushes steel markers
Read lower end of index, work out difference, eye level
Reset with magnet
Diurnal temp range: highest - lowest
Wet + dry bulb thermometer (relative humidity)
Greater difference, less water vapour in air, drier air, lower relative humidity
Records air AND air as if 100% saturated (damp)
Read relative humidity off table
Barometer (air pressure, mb)
Pressure moves pointer around dial
High pressure on glass moves dial to high
Low pressure, moves to low
Wind vane (direction)
Record once an hour (changes frequently)
Arrow points in direction wind blows from
Anemometer (wind speed)
Cups rotate by air movement
Number of revolutions recorded on meter + automatically converted to km/h
Or Beaufont scale
Wind rose
Shows direction, frequency + strength (in month)
Strength = length of arm to centre Frequency = width of arm
Clouds and types
Visible mass of water droplets suspended in atmosphere
Air cools, condenses + can’t absorb any more water
Cumulus: heaped, bubbly, high tops
Stratus: sheet/layer
Cirrus: wispy, high altitude
Nimbus: rain bearer, grey/low
Estimate eights of cover by eye, less precise, shade circle segments
Convectional rainfall (cumulonimbus)
- Shortwave radiation from sun heats ground
- Long wavelength heats air above
- Transpiration + evaporation
- Air rises (humid)
- Cools + condenses (clouds)
- Water particles collide and get heavier, saturated, fall as rain
- Repeats
Weathering
Breakdown of rock by mechanical/physical/biological forces insitu (not removed)