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the path water takes in our environment etiher through ground, plants, or atmostphere |
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hydrologic cycle can occur in ground by... |
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evaporation from soil, ground water, runoff |
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paths water can take from plants: |
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transpiration Animals: Respiration + perspiration (evapotranspiration) |
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path water cantake in the atmosphere:(3) |
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evaporation, precipitation, clouds |
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Global water Budjets: Oceans.. % Icecaps/glaciers.. ground and soil water.. rivers and lakes.. atmosphere.. |
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oceans 97.6 icecaps/galciers 1.9 ground and soil water .5 rivers and alkes .02 atmosphere .0001 |
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Run off and stream flows storage in: |
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an underground rock layer that holds water (not an underground lake) |
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precipitations- evapotranspiration +/- change in storage runn off is the movement of water over the surface of the land |
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the amount of runoff that goes into river and streams |
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cross-sectional area of stream X mean velocity of stream. 1mph is about 1.5 foot/sec |
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river flows at 30mph. depth is 5ft. width is 10 frt. what is the discharge? |
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5X10=50 velocity= 30X1.5= 45 45X50= 225cfs |
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discharge depends on gradient the larger the gradient the ____ the discharge |
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land area that contriubtes runoff to river system |
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boundary between drainage basins (the higher the elevation) |
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explain the stream network? stream of 1st order stream of 2nd order stream of 3rd order |
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the system of the main river channel plus its tributaries (heiarchial ranking system) 1st- no tributaries 2nd- merging or joining of two 1st order streams 3rd- merging of two 2nd order streams |
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when2 streams of same order merge the merged streams will be one order..(higher/lower) |
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when 2 sreams of different order merge the merged stram will be the same order as (higher/lower) stream |
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ground water runoff released over large periods of time (the avg. flow of a stream) |
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overland flow (the extra water running off land from a storm) |
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what influences the shape of hydrography? |
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a. size of basin b. type of surface c. shape of watershed d. slope e. intensity and duration of rain f. urbanization |
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pavement and concrete are impermeable to water so water must flow across surface |
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urban flood occur faster after the rain and are bigger in magnitude than ruralfloods |
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landform created by running WATER -fluvial processes have done more to shape our earth than any other process |
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the wearing away of land and soil through the process of running water (ex. gully and arroyos) |
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the placement of the material carried by running water (ex. deltas) |
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direct force of falling drops on base soil causing a geyserlike splashing in which soil particles are liften and then dropped into new positions |
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the removal of soil much faster than it can be formed (overgrazing, forest fires remove vegetation and erosion starts) ex- badlands (in s. dakota and colorado) |
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badlands are underlain by ____which do not allow water to seep through therefore the water must go as runoff and it erodes the surface features. |
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what are the 3 mechanisms of stream geology? |
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stream erosion stream transporation stream deposition |
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removal of material from the floor andsides of a channel |
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movemeent of the eroded particles thru... suspension (material help up by water) dissolved(mixed with the water (salt)) bed load: sand, gravel and cobbles move by rolling or sliding from water flow Stream deposition: depositing the material carried by the stream:occurs when there is a major change in stream discharge. |
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bouncing or skipping along stream bed |
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the slow reduction in the height of the headwater of a stream through time as the stream eroded away the surrounding materials there are 4 steps |
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what are william morris davis's 4 steps of stream gradiation? |
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1.stream established on land recently uplifted 2. gradiation in grogres (lake draining and deepening gorge 3.graded profile attained. beginning of floodplain. valley widening 4. flood plain widened to hold meanders |
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