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• The circulation of water between the hydrosphere, solid earth, and atmosphere. • Powered by the sun • 97% of the Earth’s water is in the ocean |
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Where is water mainly sourced from? |
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Groundwater and surface runoff |
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What are the two types of base level? |
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• Ultimate: the ocean • Local/temporary: waterfall, dam • Raising base level causes deposition • Lowering base level causes erosion |
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• Maintain the exact velocity required to transport materials and neither erode or deposit. • A natural state for streams |
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amount of material a stream can carry |
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the largest size material that is carried |
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• Material dissolved in the water • Supplied mostly by groundwater |
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• Carries largest amount • Sand, silt, and clay • Velocity decides what size material will be carried and what will be deposited |
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• Largest material • Bounces along the bottom • Only moves when water is forceful |
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• Generally well sorted • Velocity separates the particles by size (sorting) • Bars: sand and gravel deposited in a channel. |
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Stream sediments are known as |
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• Intermittent streams depositing large amounts of sediment onto a valley floor in the shape of a fan • Common in deserts |
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• Formed when a stream or river enters a body of water with lower energy, and deposit its sediments • Can produce large volumes of coarse sediment • Great Oil and Gas Reservoirs Ex: Gulf of Mexico |
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• Valleys that flood from meandering streams • Consist of silt, sand and gravel • Large flat areas plains with multiple old stream channels • Sediment deposited during the formation of floodplains create natural levees |
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• Rapid down-cutting in resistant rocks • Rapids and waterfalls (young features) are common • Vertical walls • More vertical erosion |
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Stream processes: uplift of land |
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• Increases gradient and stream flow • Stream starts to erode: both headward and downward to bedrock |
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create new floodplain level |
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erosion into current channel and steals its flow. |
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• One of the most valuable resources • About 1% of freshwater is underground • Largest supply of freshwater |
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Where does groundwater generally accumulate? |
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• Area above the water table • Lots of water, but hard to collect because of how it attaches to rocks and soil |
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• Below top of water table • Completely saturated • Varies seasonally due the quantity, distribution, and timing of precipitation • Streams interact with the groundwater system |
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• Streams that gain water from groundwater |
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• Streams that lose water to groundwater |
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• Percentage of void space in rock and sediment • Stores fluid |
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• The ability to transmit water through the pores of sediment or material |
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• The layers of material that prevent water flow |
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• Sediments or material that transmits water freely |
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• Where the water table meets the Earth’s surface |
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• Most common way of retrieving GW • Used for agriculture, and drinking water • Wells must break through the water table |
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What results in a cone of depression? |
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• When the water table is lowered away from the well, its called drawdown |
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• Wells that flow to the surface • Water rises above the top of the aquifer • An aquitard must both be present |
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Problems associates with GW withdrawl |
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• Water table height is effected by amount of water going into and coming out of aquifer • Severe droughts and over usage of wells can cause long term decreases in water table height |
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GW removed more that replaced, it can cause the ground to sink |
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• Form when more water is frozen than melts each year • 2% of the earth’s water is in glaciers • If all glaciers melted, sea level would dramatically rise • Glaciers are a strong erosional force, like a bulldozer |
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• Slow moving glaciers located in old stream valleys • Ice bound by rock walls that flow from an upward point • These form many features of classic glacier landforms |
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• Much larger than valley glaciers • Two currently exist N. Pole/Greenland and Antartica • Flow into ice shelves: flat masses of ice that extend toward the sea |
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• Small ice sheet glaciers, that cover upland and plateaus and bury landscape |
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• Flow from ice caps and ice sheets outward through mountains toward the sea. Like localized valley glaciers dumping into sea |
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• When valley glaciers merge at base of large mountains |
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• Mass of ice slips along ground • Melted water causes ice to move over rock • Caused by heat from in the earth |
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• Does not flow, is brittle and cracks • Forms crevasses from glacier moving over rough terrain |
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Rates of glacier movement |
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• Some glaciers move at unnoticeable rates (cm/day), while others move up to several meters a day • Quick movements by glaciers are called surges |
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• Area defined above the snowline • Where ice and snow collect and form |
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• Located generally below snowline • Where glaciers lose ice and snow due to melting • Ice can break off in a process called calving which produces icebergs |
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• Water flows into cracks of rocks and freezes • Glacier lifts, picks up and moves rocks • Can move very large rocks |
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• Caused by rock movement sliding over rock, “sanding” it down • Produces rock flour and glacial striations |
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The sediments deposited by glaciers. |
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Till and Stratified drift |
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• Sediment deposited when ice melts. • Melting ice can’t sort sediments. • Characterized by very poorly sorted, polished and scratched sediments. |
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• Sorted from glacial melt water according to shape and size • Layered and better sorted than till • Consists mostly of sand and gravel |
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Glacial theory and the ice age |
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• Last ice age was about 18,000 years ago • Climate changes come from variations in the earth’s orbit and tilt of the axis |
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