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GEOG 203: FINAL EXAM

Alexander VonHumboldt
father of biogeography saw vegetation as a whole, rather than small parts of botany
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abiotic
impact of physical environment
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biotic
impact of biology; inherent characteristics barrier of transportation
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Niche Concept
habitat(s) a particular plant/animal is most suited for; range environmental variable (x), species response (y) zone of optimum zone of stress zone of intolerance
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chipmunk distribution case
2 species can live in same areas, but one takes over 1 section and the other takes over the other section and they are very mildly mixed in the middle; based on biotic characteristics
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mountain vegetation
more like tundra at top middle--low trees bottom tropical (Costa Rica)
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population
...
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community
populations interacting together -combination of species
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ecosystem
communities and environment interacting together -climate factors and living things; varying sizes; overlap **DYNAMIC
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photosynthesis
fundamental process of turning water and carbon dioxide into glucose, water, & oxygen
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biome
ecosystems interacting formed by temperature & precipitation similarities
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biodiversity
many types of flora/fauna highest in warmer/wetter regions: tropical rainforest
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all organisms need
water sunlight/heat/energy
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island diversity
increases with size decreases with distance from mainland
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latitudinal gradient affect on biodiversity
higher latitudes= lower biodiversity; more in southern hemisphere than northern hemisphere
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history of ecosystems
65million years ago: Tertiary pd=mostly warm, rainforests 1.6million years ago: Quaternary pd=mostly cold, glacial forests fragmented over time b/c tectonic plate movement
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invasive exotic species
species not native to land better at competing & stay around Kudzu Chinese Tallow Tamarisk
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anthropogenic disturbances
people-caused
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disturbance
mass even that kills vegetation resets succession maintains habitats maintains species diversity create landscape patterns
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succession
recovery of vegetation after a disturbance
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climax vegetation
self-replacing community (instead of new, more developed/evolved species)
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serotinous cones
cones only open with heat & distribute seeds
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forest fire frequency
humans decrease natural fires; must prescribe fires to maintain some habitats/species
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denudation
processes that degrade or strip down the landscape; anything that causes weathering/erosion
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relief
change in geomorphology/elevation
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geomorphology
science of landforms origin, elevation, form, spatial distribution
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landforms are consequences of
tectonic plate movement denudational processes wear down/rearrange (erosion & deposition)
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differential weathering
everything weathers at a different rate b/c everything is composed differently
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ridges
formed by resistant rocks such as sandstone; have steeper angled slopes
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valleys
formed by less resistant rocks like shale
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resisting framework
rocks that are in place on the landscape, often having been uplifted to high elevations by plate tectonic processes
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karst
geological formation shaped by the dissolution of a layer of soluble bedrock (limestone) features sinkholes; limited surface water cockpit karst (like mattress egg shells) tower kart (rapid rates of weathering in humid envt--China)
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mass wasting
slope movement/mass movement soil, sand, regolith, & rock move downslope under the force of gravity/cohesion/friction **gravity as an agent of denudation
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erosion
wearing away
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deposition
drop-off after being carried away
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ingredients for mass wasting
big, steep mountain great tectonic activity, shattered rocks (loose rocks) climate: occasional heavy winter rainstorms; vegetation=drought-tolerant; don't lose much water; mountain climate fire
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colluvium
deposit that is a consequence of mass-wasting example=rocks at mountain bottom typically unsorted
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angle of repose
maximum slope where "safe" from mass wasting
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factor of safety
how likely a slope is to fail =strength/stress best further away from 1
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talus slope
type of colluvium; fragment of rock broken off
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debris avalanche
increases speed with slide; breaks apart and becomes fluid
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creep slide
slow movement; evident by leaning of items on hillside
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solifluction lobe (Sweden)
ice top layer falls out; soil moving down slope atop permafrost; slow tundra environment
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Huascaran, Andes 1970
jumped 1000ft ridge; Yungay town in lowlands covered by debris
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gradient
angle of stream slope
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velocity
speed/flow rate of stream rapidness; greatest at coastal plains b/c turbulence is low
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discharge
volume of stream width*depth*velocity=Q
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cross-sectional area
area in section of a stream (width/depth)
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hydrograph
bar graph of amount of rainfall during event
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hyetograph
line graph of discharge during/after rainfall event flashy for urban areas; subdued for rural areas (due to amount of vegetation in the way flow)
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drainage basin
collection area for water (first order basin nested inside 2nd order basin...) sloping landscapes
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dendritic drainage pattern
efficient water delivery
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trelis drainage pattern
on valleys
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parallel drainage pattern
eroded down rapidly
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deranged drainage pattern
glaciers melt back
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watershed
line separating drainage basins; usually for smaller streams Continental Divide=major
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hydraulic action
water's movement picking up rocks; power
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abrasion
water scrapes because of contact (stream pushes load along bed)
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solution
dissolved load in stream
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base level
gravity/streams cut down to this; ultimate=sea level
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load
what streams carry bed=bottom suspended=within, tumbling dissolved=within but unseen
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alluvium
stream deposition as velocity decliens along stream bed & along middle & sides of stream
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point bar
arc where stream meanders
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undercut bank
where stream begins to form closed horseshoe
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oxbow lake
created when stream cuts off "longer" route horseshoe shape
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alluvial fans
fluvial and mass wasting denudation dry areas stream sorts load & settles at mountain base like a fan
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delta
stream slows toward ocean/gulf stream deposits alluvium near coast & settles at mouth of river expands coastline slowly birdfoot or delta/triangle-shaped
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