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a fold or depression shaped like a right-side-up bowl |
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an array of interconnecting streams that together drain an area |
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a film of water less than a few millimeters thick that covers the ground surface during heavy rains |
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Dentritic Drainage Network |
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like veins on a leaf or branches on a tree, gentle slopes, uniform rock type |
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flows out from central location, common around volcanoes or other conical features |
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Rectangular Drainage Network |
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streams join together at right angle because of a rectangular grid of fractures that breaks up the ground and localizes channels |
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drainage network that forms over valley-and-ridge sequences |
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the beginning point of a stream |
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a trough dug into the ground surface by flooding water |
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the flat land on either side of a stream that becomes covered with water during a flood |
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the elevated surface of an older floodplain into which a younger floodplain had cut down |
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the deepest part of a stream’s channel |
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a reach of stream containing many meanders (snake-like curves) |
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a sediment-choked stream consisting of entwined subchannels |
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streams made of rocks still attached to the Earth’s crust |
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stream channels cut down through resistant rock, can end up with channels having a shape based on rocks that are now eroded away |
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topography comes up around stream, which can erode at the same rate |
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chaotic twisting and swirling motion in flowing fluid |
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when a fluid flows in parallel layers, with no disruption between the layers |
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large particles, such as sand, pebbles, or cobbles that bounce or roll across a stream bed |
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tiny solid grains carried along by a stream without settling to the floor of the channel |
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ions dissolved in a stream’s water |
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sediments transported and deposited by streams |
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sediment transported by flowing water that is dropped when there is a sudden loss in water capacity, reduction in velocity |
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an event during which the volume of water in a stream becomes so great that is covers areas outside the stream’s normal channel |
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a location at the base of the lithosphere, at the top of a mantle plume, where temperatures can cause melting |
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the gradual widening of an ocean basin as new oceanic crust forms at a mid-ocean ridge axis and then moves away from the axis |
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an isolated submarine mountain |
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Carbonate Compensation Depth |
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line below which CaCO3 dissolves |
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driven mainly by wind and modified by the corriolis effect |
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driven mainly by gravity and the corriolis effect |
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subcircular current systems, in which water flows in a circular pattern |
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the force due to Earth’s rotation about the center of the Earth-Moon system |
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Sun, Moon, & Earth are aligned (highest, high tides) |
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Sun & Moon form 90 degree angle with the Earth (lowest, high tides) |
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a deposit of sand and gravel at the edge of the swash zone |
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the upward surge of water that flows up a beach slope when breakers crash onto the shore |
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a platform of rock, cut by wave erosion, at the low-tide line that was left behind a retreating cliff |
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a platform of rock, cut by wave erosion, at the low-tide line that was left behind a retreating cliff |
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a notch in a coastal cliff cut out by wave erosion |
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a coastal cliff that is cut by wave erosion |
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subsurface water that occurs below the water table within geologic formations that are saturated (pore spaces filled). This is not the same as soil moisture - there is often water trapped between grains of soil, but generally it will not flow to a well (held by capillary forces) |
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water passing through ground surface |
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water reaching the water table, level of water than can be produced from wells |
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the volume fraction of open spaces in a rock or soil |
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ease of ground water flow |
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geologic unit that is completely saturated by water, that stores and transmits water in usable quantities |
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geological unit with much lower transmissive properties than surrounding formation (aquiclude versus aquitard) |
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sediment or rock that transmits no water |
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sediment or rock that does not transmit water easily and therefore retards the motion of the water |
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one in which the upper surface of the aquifer is defined by the water table |
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an aquifer of limited lateral and vertical extent that is underlain by a confining layer |
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one in which the level to which water in the aquifer would rise in a pipe, emplaced in the ground and open at the bottom, is higher than where the top of the aquifer meets the overlying confining layer |
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a region above the water table that is also saturated, but within this zone water is held in place by suction |
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the region above the saturated zone |
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elevation of water table that tells you how much energy is available to drive flow |
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the abrupt rise or fall of air, without gaining or losing heat |
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short-term conditions, wind speed, temperature, humidity, precipitation, etc. |
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long-term conditions, seasonality, variability, average conditions, etc. |
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the reflectivity of an object |
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seasonal reversals in winds, leading to very wet and very dry seasons |
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trade winds die, water moves back to east, gets very warm offshore west US and SA, little or no upwelling |
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streams or sheets of recrystallized ice/snow that last through warm season, move under the influence of gravity |
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found in or near mountains, shape controlled by mountain topography, flow from high elevation to low elevation |
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cover vast expanses of continental areas, flow outward toward margins |
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most ice is close to melting, moves mainly by sliding at the bed |
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ice is well below melting point, frozen to underlying ground under most of the glacier, move mainly by internal deformation |
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Three Conditions For Glacier Formation |
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Definition
(1) local climate must be cold (2) enough snowfall for accumulation (3) gentle enough slope to avoid removal by sliding |
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rocks that are out of place, carried by glaciers |
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Definition
the abrupt release of energy due to slipping of rock masses (usually along a fault), leading to shaking of the ground |
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a measure of the amount of energy released |
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reversible. release the stress and the strain vanishes. |
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Term
Ductile and Brittle Strains |
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not reversible. release the stress and strain stops accumulating, but the rock does not return to its original shape. |
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Definition
smaller earthquakes that follow any large earthquake |
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Definition
(1) P-waves (primary, primus, "push") (2) S-waves (secondary, "side-to-side", slower) |
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Definition
(1) Rayleigh waves - up and down (kind of like waves on the ocean) (2) Love waves - side to side |
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a wave that propagates as a series of compressional and expansional vibrations is known as a compressional wave |
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a measure of how difficult a solid (or fluid) is to compress |
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a measure of how difficult a solid is to shear |
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shear waves. travel slower than P waves and arrive later. |
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seismic surface waves propagate only along the surface of the planet, they do not pass through the planet |
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Definition
create vibrations somewhat like those of S waves. makes rocks near the surface vibrate horizontally back and forth perpendicular to the direction of wave propagation |
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Definition
create vibrations that trace out circular paths aligned with wave propagation. resemble ocean waves with one major exception: the orbits rotate in the opposite direction. |
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lots of little, shallow earthquakes |
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strike slip, somewhat larger, rarer earthquakes, also generally shallow, sometimes intermediate |
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complex, many kinds of earthquakes normal faults, shallow quakes where plate is flexed |
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sensitive instruments designed to record the vibratory motion (strains) of passing seismic waves |
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long-wave radiation becomes trapped within Earth's atmosphere, helping to increase the heat stored |
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