causes of climate change: variation in sun's radiation, changes in composition of atmosphere, changes in earth's surface, variations in earth's orbit
eccentricity: changes in earth's orbit from circular to elliptical - 100,000 year cycle
precession: changes in the tilt of the earth's axis - 23,000 year cycle
obliquity: changes in the wobble of the earth's axis - 14,000 year cycle
ozone forms naturally in the stratosphere
ozone forms in the troposphere due to chemical reactions with other gases
acid precipitation: precipitation that combines with pollutants that turn the precipitation acidic
main sources of acid precipitation: sulphuroxides, nitrogenoxides
effects of acid precipitation: slowed tree growth, reduces fish population, erodes materials
positive feedback: a process in a system that encourages the continuation of the original process
climate models: solving a series of mathematical equations that includes greeenhousegases, solarradiation and other climatological components
climate change impact on humans: food production, tourism and human health
impacts of climate change on biodiversity: bleaching of corals, loss of flora and fauna, extinction risk for polar bears
relationship between humans and environment: humans are simply one component of the natural world, humans live separately from nature
relationship with nature dictated our actions: living in harmony with nature, or exploiting nature for economic gain
precautionary principle: when there is a risk involved to either humans or the environment, we must act even if there is still uncertainty about the risk. it is our social responsibility to protect people and the environment from harm
issues preventing growth of wind farms: habitat disruption, appearance, noise
implications of large hydroelectric projects: loss of land due to flooding, displaced population, leaching, destruction of habitats
The Richter Scale was a measure of the strength of a wave 100 kms from the epicentre
the moment magnitude scale (M) is determined by: area of rock ruptured along a fault, distance of movement along a fault, strength of rock at focus
the modified mercalli intensity scale: qualitative scale based on damage to property and people
earthquake processes: friction along plate exerts stress, when the stress exceeds the strength of the rocks there is sudden movement along a fault, this rupture starts at the focus and propagates as seismic waves
fault types are distinguished by the direction of displacement of the rock
two types of faults: strike slip and dip slip
strike slip faults: displacement is horizontal
dip slip faults: displacement is verticle
best example of strike slip fault is: san andreas fault
three types of dip slip faults: reverse fault, thrust fault, normal fault
reverse fault: the hanging wall is moved up relative to footwall at an angle above 45 degrees
thrust fault: the hanging wall moves up relative to the footwall but at an angle less than 45 degrees
normal fault: the hanging wall has moved down relative to the footwall
footwall: where miners place their feet
hanging wall: where miners place their lanterns
fault activity: active, potentially active, or inactive
active: movement within the last 11,600 years
potentially active: movement within the last 2.6 million years
inactive: no movement during the past 2.6 million years
tectonic creep: the extremely slow movement of rock along a fracture caused by stress
body waves: P and S waves
P waves: primary or compressional, move in push pull motion FAST - can travel through solids or liquids