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*WIND -strong wind and long "fetch" have larger waves |
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longshore current/transport |
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gravitation interaction among Earth, moon, sun and oceans |
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sun, moon, and earth line up -higher high tides and lower low tides |
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sun,earth, and moon form right angle (moon is above the earth) -lower high tides, higher low tides |
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*magnify effects of tides, waves, etc *normal part of beach evolution |
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*formation of a beach *a natural beach is not destroyed by "beach erosion" *Beach is lost only when structures are employed to lock the shoreline in place |
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*action of waves on shoreline- removal of all but coarsest sediment (SAND) *as shoreline moves, beach moves with it |
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causes of shoreline retreat |
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*global sea-level rise *land subsidence *sand starvation |
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*present rate: 2mm per year and four feet of lateral shoreline movement *10-25 cm over a century |
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*examples- east texas and lousiana *Louisiana losing 25 mi^2 of land per year |
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*hard stabalization *soft stabalization *move out of the way |
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*build hard, immovable structure to anchor beach *structures are seawall and groin/jetty |
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soft stabalization (beach replenishment) |
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*add sand to beach *advantages-save beach and buildings *disadvantages-expensive and has a short lifespan |
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*stress *strain *britle deformation *ductile deformation *fault *joint *strike and dip *dip *strike |
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response of rock to stress |
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breakable, faulting (rock breaks) |
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a break in a rock along movement |
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a break in a rock along NO movement |
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describes the orientation of a planier feature (could be tilted, folded rock layers) |
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tells you the downward tilt of a feature; measured as an angle below horizontal |
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compass direction of the intersection of a tilted plane with the horizontal |
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ductile deformation again |
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*(folds) *anticline- "A" up rock layers *synticline- "U" shaped rock layers *folds result from compression/shortening |
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brittle deformation again |
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*(faulting) *dip/slip faults-motion parallel to the dip direction, has both vertical and horizontal movement |
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*volcanic eruptions *nuclear weapons testing *elastic rebound |
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*rocks bend elastically as stress applied *faulting releases elastic strain instantly *earthquake waves radiate out from fault break *aftershocks as fault strain fully dissipater |
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magnitude and intensity- scale (1902) |
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*subjective *based on eyewitnesses accounts, damage 1-barely felt 6-felt by all, slight damage 12-total destruction |
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m=log10(X/T)+lamda *m-magnitude *X-amplitude of ground motion *T-period of ground motion *lamda-distance correction function *m=6-7:serious *m=7-8:major *m=8-9:massive |
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*similar to richter scale *more accurate and consistent *based on: physical prop of affected rock, surface area of fault rupture, amount of fault slip |
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*point of earth's surface is vertically straight above the focus(earthquake) |
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weight that shows motion of disturbance within the earth |
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*secondary waves *shear waves *motion within wave is perpindicular to direction of travel *travel through solid only |
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*analogues to waves on water surface *propogate along free surface *circular ground motion (groud-roll) |
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*almost impossible to make precise predictions *uncertainties of decades to centuries *earthquake precursors *"seismic gap" method |
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*tilting or swelling of ground *groundwater pressure change *electromagnetic field changes *animal behavior |
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paper with pen that shows the disturbance of the earthquake |
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damage control of earthquakes |
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*build flexible structures, anchor structures to bedrock *no heavy roofs *problems with soft sediments *Loma Prieta-earthquake *no heavy roofs |
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problems with soft sediments |
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*liquification-(anchorage,ak) sed. liquifies *amplification (oakland, ca) sed is weaker, movement (Loma Prieta) |
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*(tidal waves) *off shore earthquakes create waves in the sea *waves propogate out of the epicenter *can be huge when hit land |
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*abrupt jump to high velocity material several km deep *deeper earthquake waves travel faster than shallow *we can infer that the crust is underlain by denser mantle |
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*earth behaves like a giant magnet *earths interior too hot to contain magnetic minerals *field most likely generated by rotation of solid inner core within liquid core |
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*polarity of earths magnetic field spontaneously reverses *intervals of a few 10000 years to millions of year (avg-250000yrs) *last reversal=780000 years ago *reversals recorded in minerals that act as natural compasses, esp iron rich igneous minerals |
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*1908-1912: alfred wegener-proposed hypothesis of cont drift *1950s-1960s=mapping of ocean floor, leads to theory of plate tectonics |
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*cont drift- all of the continuity fit together like a jigsaw puzzle; |
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evidence of plate tectonics |
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*distribution of fossils *paleo climate info=ancient climate *united glaciacion=combine all continents into antarctica |
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important steps to theory |
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*look at sea floor *poor resolution of earthquakes *evidence of sea floor (structure, age, magnetic) |
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*polar wandering, heat flow, realtime |
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*mid ocean ridge (block faulting) normal fault-ridge being pulled apart *large mtn chain *intense volcanic activity *seafloor spreading @ ridge= crustal expansion apart |
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*not older than 180 million years *covered by sed. layers *youngest sea floor coincides with mid ocean ridge |
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*theory of plate tectonics- earths lithosphere divided into discrete plates that are in motion relative to each other *interactions between plates are the main cause of volcanism, earthquakes, mtn bldg and other geo phenom *plate motion is driven by thermal convection in the mantle |
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plates pull apart, gap filled with lava, build new ocean crust |
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locations of divergent boundaries |
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*midocean ridges (most) *cont drift (a few) -ocean floor=basalt |
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located in the eastern part of africa *linear drift-red sea and gulf of aden |
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*plates ram together, subduction zone, ocean trench, volcanoes, ocean crust destroyed |
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types of convergent boundaries |
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*oceanic/cont and oceanic/oceanic, cont collision. west side of pacific is oceanic convergent, east side= cont drift, himalaya=cont collision |
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*(san andres fault, ca) *plates slide horizontal *links segments of divided boundaries, earthquake hazards |
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*earth is dynamic, constant crustal motion, and crustal deformation, thermal uplift (fault) |
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*isostacy- earths crust floats on top of mantle, lighter cont. crust floats higher, thicker cont. crust floats higher *thermal effects- hot mantle may up crust, important at mid ocean |
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assertion of earths lower atmosphere and oceans have warmed during past |
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metereological phenomenon |
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*climatical evidence clearly tells us the earth is warmer now than it was 10 years ago, 50 years ago, 100 yrs ago, or 10000 yrs ago *causes of climate change poorly understood |
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*some argue that the earth is warmer bc of human activities and that therefore we need to change our ways *others argue- the earth isnt warmer, observed warming is natural |
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*complex balance of forces *atmospheric- circulation patterns, greenhouse gasses *oceanic-circular patterns, greenhouse gas source/sink *geological-position of continents, volcanic gasses/dust *astronomical (orbital) |
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*as atmospheric, oceanic, geological, and astronomical change, earth's climate changes *earths climate has changed dramatically during the very recent geologic past |
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entrapment of heat by certain atmospheric gasses(greenhouse gasses) |
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*glasses that are transparent to sunlight but trap heat (infra-red) energy (H2o,CO2,CH4,others) |
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*sunlight (light energy)-passes through atmosphere,absorbed by ground, ground warms up *heat energy from ground radiated back into atmospheric *heat absorbed by greenhouse gasses *atmosphere warms up |
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*normal part of earths climate *keeps eart 60 degrees *without= 15 degrees |
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*ice cores *tree rings *lake and ocean sediment *cave sediment |
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*greenland and antarctica *trapped atmospheric gasses *snow depth *dust, contamination |
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Pleistocene era (1.65 my-10K yrs ago) *numerous advances and retreats of continental glaciers in northern hemisphere |
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most important of measuring past temps |
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*ice cores *ocean sediment |
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