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oceanic plate goes down continental/crust plate converge or split |
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Large chunks of lithosphere 7 major and 7 minor Pacific Plate (most active) forms boundary between west coast and North American Plate |
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1912: Alfred Wegener Lithospheric Plates move on the Asthenosphere |
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All earth 225 million years ago Laurasia and Godwana (two islands) |
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Plates are moving apart Occurs in ocean basins Mantle convection, magma comes to surface, cools and forms new crust. Creates oceanic ridges (mid-atlantic ridge) |
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Plates are coming together Subduction zones - more dense subducts under less dense Metamorphic rock form |
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| Oceanic/Continental Boundary (converge) |
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Definition
melting crust forms volcanoes rocky mts/andes mts |
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| Oceanic/Oceanic Boundary (converge) |
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form trenches island arcs - aleutian islands. Marianas trench - deepest part of ocean |
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collision forms mountains alps/himalayas |
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plates slide laterally past each other sliding produces friction earthquakes faulting (san andreas) along mid ocean ridge |
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upwelling of magma from deep in earth remains stationary relative to plate movements Hawaii |
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broad profile effusive eruption largest Mauna Loa |
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stratovolcano layers of ash and lava oceanic crust denser plugs vent pressure builds |
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magma comes to surface mantle grows creates oceanridges (mid atlantic ridge) |
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| zone of volcanoes in pacific ocean along divergent boundary |
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1st - both land, curst, and ocean basins 2nd - specific landform (mountains, ocean ridge trenches) 3rd - detailed individual landforms |
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| craton (or part of the earth's crust) exposed at the surface) |
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| along ridge of fold of a fold |
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| along the bottom/ trough of a fold |
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| divergent boundary one side drops and creates a cliff |
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| Reverse Fault/Thrust Fault |
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| at convergent boundary compressed stress |
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| transform boundary that creates rift valleys |
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Horst - upward faulted blocks Graben - downward faulted blocks |
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Mountain building process Oceanic/continental - pacific coast of america oceanic/oceanic - volcanic islands continental/continental - european alps |
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seismology - study of measure with Richter scale Focus - where it starts Epicenter- surface location of focus Foreshock - before After shock - crust regaining equilibrium |
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P - compressional S - most destructive/shear wave L - slowest, cause most damage because they're on surface |
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| Plates dont move smoothly against each other the force exerted in movement moves back and with force |
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| vent at earth's surface through which erupted material comes out |
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| circular depression formed near summit |
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Lava - molten rocks and gases Pyroclasts - rock and clastic material associated with a violent eruption |
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| gentle eruption pours out on surface |
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| trapped gases leading to an explosive eruption/ thick magma |
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| divergent/convergent boundaries and hot spots |
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| steep volcanoes are 10s to 100s meters tall |
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| wide/largest & erupts effusively |
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violent eruption (pressure builds) strato volcano |
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| mud flow from melted snow w/ lava |
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| depression at summit due to loss of magma chamber |
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different materials weather at different rates Sedimentary (fastest) Metamorphic (slowest) |
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| parent material from which weathered regolith (rock fragments) and soil develop |
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| Geographic Orientation, Vegetation, Climate |
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Geo - determined on which side is exposed to elements Veg - stability Cli -determines type of weathering |
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frostaction - water gets into cracks, freezes and then expands Exfoliation - erosion removes mass. (creates sheets of rock) Crystallization - water vapor forms crystals. puts pressure on rock |
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| collection of broken rocks at the base of a mountain |
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spheroidal weathering - rounds corners, water penetrates joints and fractures them hydrolysis - water breaks down silica and weakens rock carbination - dissolves limestone, rain water hits rock turn to solution Oxidation - metals combine w/oxigen makes rust |
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| interaction of living organisms |
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| subsurface water dissolves rock creates a space between water table and surface |
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| Sinkholes/ Collapsed Sinkholes |
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SH - circular depression formed by solution process CSH - sinkhole collapse through the roof of an underground cave |
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| elongated depression from jointing of multiple collapsed sinkholes |
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| in limestone regions because easier to create - caves |
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stalagmites - from floor Stalactites - from ceiling Column - they join |
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down-slope movement of materia due to gravity Falls: rock fall or debris avalanche Slides: large movement of rock Flows: saturated soil. Water moves soild Creep: always ocurring |
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deflation: removal & lifting of individual parties desert pavement: small particles blow away larger stay Blowout depression: removes enough material to form a depression Abrasion: grinding of rocks Yardang: elongated ridges parallel to most effective wind direction Ventifacts: rocks with evidence of wind erosion |
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| turbulent winds hold light particles in air |
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| winds strong enough to move but not suspend |
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| Impact moves other grains |
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| perpendicular to winds due to impact of saltating particles |
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accumulated sand move with wind winward - gentle slope leeward - steep side |
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| crescent horn points to wind. often coastal |
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| crescent horns downwind in desert fringe |
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| many curved crescent shorter than longitudinal |
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| shifting winds multiple slipfaces |
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| conjoined crescents with horns downwind |
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flash floods - dry riverbed that can flood arroyos - dry channels filled with water during storms |
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| mouth of a canyon where it exits into a valley |
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| alluvial fans individually merging |
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| heavily eroded with little vegitation |
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| are that splits two rivers |
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| Boundary separating basins. (i.e. Mountain Ridge) |
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| separates largest basins. (i.e. Rock Mountain) |
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| tree most common & effective |
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| parallel ridges/ dipping or folded topography |
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| flow off mountain or volcano |
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| tree shaped on steep slopes |
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| water flows in right angles at faults & joints |
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| disrupted - usually glacial |
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Rule 1: when 2 streams of same order come together ill be next highest order Rule 2: 2 streams of different orders come together its the highest order |
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streams flow rate water/time controlled by: geometry of channel, viscosity, gradient, size of perimeter |
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| movement of solids in water |
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| solution chemical weathering. i.e. limestone |
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| fine material suspended in water |
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| current strong enough to move but not suspend |
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| linear features dont naturally occur rare |
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| stream transports sedmient intertwining channels |
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| gradual slope/broad flat sweeping curves |
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| outside of curve most erosion |
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| inner wave deposition of sediments |
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| cut off meander because it is easier to flow |
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| curve of lake drains & leaves |
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| Laminar Flow/Turbulent Flow |
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Lam - no mixing of sediments Turb - mixing of sediments in solution |
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| abrupt change in gradient to eliminate blockage/ resistan rock |
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1.Flood Plains 2.Delta 3.Alluvial Fans 4.Natural Leree |
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1 - low lying area surrounding a stream 2 - stream enters ocean 3 - delta on land drops sediment from mountain base 4 - blocks water flow |
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periods of high discharge water happens - rain, snow, hurricanes, levee failure flashflood - happens within minutes of storm return - describes magnitude, statistical probability |
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| required to pay for emergency services if attempt to cross in posted flood areas |
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| sediments mixed by wind temp is constant within depth |
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| temp colder as you go down |
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| near freezing. no mixing of sediments |
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| consists high water line, shore line, ocean less that 200ft deep |
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dissolved solids from crust varies 34-37% brine high than 35% brackish lower than 35% |
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global change in man sea level global warming 4-8in increase in the last century |
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Solar energy - prevailing wind, weather systems and climate atmospheric wind - generate ocean currents and waves climate regimes - influence coastal geomorphic coastal rock - rate of erosion & sediment production human activities - coastal change |
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| gravitational pull of moon and sun |
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| sun & moon are perpendicular small tidal range |
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| earth and moon are aligned. large tidal range (tidal wave is bigger) |
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| wind blows friction along water and transfers energy to water . energy moves as a wave |
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| wave hit not straight coastline. constant wave interaction straightens coast. |
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1.Waves in groups 2.Height of wave and wave crashes |
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| waves hit at angle to shore produces current parallel to coast |
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waves hit at angle to shore sand moves with waves and produces transport of sediments down the coast |
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| combination of longshore and beach drift |
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| fast moving water out to sea/ undertow |
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| wave action undercuts land |
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| various cliffs due to changing sea level |
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| erosion of less resistant rock |
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| erosion through less resistant rock erecting a bridge like feature |
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temporary location of sediment transported along shore stabilizes wave energy |
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| deposition of material at end of coast through littoral lift |
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| deposition at end of coast that has an enclosed bay |
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| sediment deposition connects main land to island sea stacks |
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| living organisms dying and they are the crustacean often around volcanic islands |
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| reef weathers away island |
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| in tropics with trees and shrubs where roots are out of water |
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| flows from within a U-shaped valley |
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| depression in mountain where snow can accumulate glacier forms and flow out |
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| glacier that has flowed out form a mountainous region |
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| glacier that flows directly to ocean |
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much larger than alpine constantly in motion Greenland and Antartica |
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| similar to water fall glacier travels off cliff |
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| large chunks of ice falling of tidal glaciers creating icebergs |
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| sudden forward movement w out warning |
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| vertical cracks in flowing glacier |
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| pressure liquifies bottom of glacier and it slides |
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| glacial retreat leaving behind valleys were the ice was |
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| u-shaped valley from tidal glacier (ocean fills the retreat) |
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| ice in cirque melts on leaves or glacial lave |
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| ridge where two glaciers flow away |
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| point where multiple glaciers flow away |
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| net loss of snow melting and snow gaining is equal |
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| line where transition from snow to ice |
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| net gain of snow is greater than net loss |
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| net loss of snow is greater than net gain |
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| general term for all glacial deposits both sorted and unsorted |
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| unlocal rock put in a location by glacier |
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| area of water melt at end of glacier like a delta |
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| large block of ice left behind from glacier |
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| glacier retreats till left behind |
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| erosional hill similar to a dune in shape polished by the side of a glacier |
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| sediment eroded by glacial movement that is deposited on the side of the glacier |
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| combination of 2 lateral moraines when two glaciers come together |
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