EARTHSC 2GG3 (Post-Midterm)

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Last updated 2:58 AM on 6/17/26
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64 Terms

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What are the causes of slope failure?

  • Imbalance between friction and gravity forces as object moves downslope

  • Slope steepness (gravity overcomes friction)

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Joints

  • cracks which are common in bedrock near earth’s surface

  • create planes of weakness

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What causes joints to grow?

  • increasing slope angle

  • overburden removal

  • ice/root wedging

  • daily temperature changes

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How are joints positioned in sedimentary rocks?

perpendicular to bedding

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How are joints positioned in igneous rocks?

can be either perp or parallel to the surface

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Exfoliation joint

onion skin-looking joint from erosion bringing igneous rocks to the surface

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Planes of weakness

  • surfaces with less strength compared to material around it

  • e.g. wet clay/sand layers, joints, (Ex)foliation joints (foliation is metamorphic)

  • also influenced by slope orientation

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Cohesion

  • weak electrical charges attracting grains to each other

  • promoted by small amounts of water

  • overcome by too much water

<ul><li><p>weak electrical charges attracting grains to each other</p></li><li><p>promoted by small amounts of water</p></li><li><p>overcome by too much water</p></li></ul><p></p>
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Angle of repose

  • Steepest angle maintained to horizontal by cones of loose material on flat surfaces

  • 30 - 37 deg for dry sand/gravel (higher when damp)

  • up to 45 deg for irregular gravel

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Creep

  • slow, gradual downslope movement

  • common in temperate areas due to repeated expansion and contraction

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Solifluction

  • creep in areas with permafrost

  • active layer slides downslope in overlapping sheets

  • methane and CO2 release

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Slump

  • mass wasting where rocks/sediment stay mostly coherent during movement

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Translational slump

slump where failure surface is planar

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Rotational slump

slump where failure surface is concave

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Head scarp

exposed, upslope edge of failure surface

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Toe

downslope edge of slump rock

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Mudflows & debris flows

  • Non-coherent flows of rock and sediment (higher water content)

  • can move up to 100 km/h

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Mudflow

flow containing slurry of mud, and finer materials

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Debris flow

flow containing mixture of mud and large rocks

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Underwater slides

  • sediment dispersing, forming turbulent cloud under water

  • caused by earthquakes/large disturbances and hotspot volcanoes

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Rockfalls

  • a mass free-falling down a cliff/steep slope (often vertical)

  • caused by joints/fracturs in rocks

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Frost wedging

  • splitting of rock through pressure exerted when water freezes

  • dominant process causing rockfalls in cold regions

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Rock slides & Strurzstroms

  • the largest and most destructive landslides

  • speeds up to 100-300 km/h

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Rock slide

extremely rapid downslope movement of large volumes of rock and debris

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Sturzstroms

  • aka rock avalanches

  • begin as rock slides then break up, taking on air and water

  • mechanism unclear

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Fluidization

  • flowing as a fluid composed of rock fragments suspended in air

  • potential theory for Sturzstroms

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Leda clay

  • aka quick clay

  • Water saturated mud deposited in salty water composed of clay flakes with large pore spaces between the flakes

  • highly unstable (glacial melting)

  • liquifies when disturbed

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Weather disasters

  • Storms, hurricanes, and floods mainly driven by solar energy instead of energy from within the earth

  • main E source is the sun

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Watch

  • issued when the drivers/signs of an event are present

  • high probability that event might happen

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Warning

issued when we are sure the event will take place

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Lapse rate

change of temp with altitude; ~6.5 °C/km

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Troposphere

  • part of atm heated by IR radiation from earth's land and water

  • where we live

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Stratosphere

  • part of atm heated by ozone absorbing UV light

  • temp increases with heigh

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Mesosphere

  • part of atm that cools due to lack of ozone

  • temp decreases with height

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Thermosphere

part of atm where high-energy radiation is absorbed by gases

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What happens to air pressure and density with altitude?

They decrease with increasing altitude

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Coriolis effect

  • shifting of wind movement path to the right due to earth's rotation

  • Speed of rotation decreases with latitude

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Which direction do air masses curve in the N Hem?

they curve to the right

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Which direction do air masses curve in the S Hem?

they curve to the left

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Cyclone

air flows upward and counter-clockwise

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Anticyclone

air flows downward and clockwise

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Hadley cells

  • Air rises at 0°C and sinks at ~25° N and S lat

  • These cells are when tropical air warms, rises, and flows towards poles

    • Then subtropical air cools, sinks, and flows back towards equator

  • Control of rainfall in low latitudes

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Trade winds

  • Trade winds: result as Hadley cell air flows toward equator

    • N hem surface winds curve southwest

    • S hem surfacer winds curve northwest

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Intertropical Convergence Zone (ITCZ)

  • where N and S hems trade winds converge

  • N hem summer → shifts N of equator

  • S hem summer → shifts S of equator

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Air pressure zones

  • More land mass is in N hem, more water in S hem

  • Southern hem has more buffering from water, resulting in less significant seasonal changes

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Pressure in Northern winter

cold polar high pressure zones with cold air flowing off continents and rising in Icelandic and Aleutian lows

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Pressure in Northern summer

highs pressure over ocean with onshore flow of moist air and monsoons

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Front

  • When two different air masses meet with different temperature or moisture or both

  • Warmer air has potential to hold more moisture than cold air

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Cold front

  • cold air from north wedges under warmer air, forcing it upwards

  • Warm air cools down by force → thunderstorms and rain

<ul><li><p>cold air from north wedges under warmer air, forcing it upwards</p></li><li><p><span>Warm air cools down by force → thunderstorms and rain</span></p></li></ul><p></p>
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Warm front

warm air runs up and over colder air (more gradual since cold air is not 'moving') → cloud formation, rain not likely

<p>warm air runs up and over colder air (more gradual since cold air is not 'moving') → cloud formation, rain not likely</p>
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How to make a single-cell thunderstorm

  • warm, humid air rises, forming clouds

  • rain/ice too heavy → condensation

  • warm updraft stops when enough has fallen

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Supercell thunderstorm

  • same as a single cell storm but much larger and can rotate

  • Updraft and rotation combined lead to powerful tornadoes

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Wall cloud

lower part of column, where updrafts are strongest

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Anvil cloud

above the wall cloud, lots of lighting activity

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How do tornadoes form?

  • Descend from wall cloud within supercell storm

  • Most tornadoes are formed within supercell storms

  • ~30% of supercell storms produce tornadoes

  • Supercell formation -> watch

  • Funnel cloud descends -> warning

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Tornado track

swath of destruction on the ground (focused destruction); path it takes across the ground

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Enhanced Fujita Scale

  • Not based on wind speed (hard to track)

  • Classed based on worst damage caused by tornado

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