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Geologic Time, Mass Wasting, & Rivers

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Term
Definition
principle of uniformitarianism   processes happening now happened before; large changes require a long time  
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principle of original horizontality   sediment deposited horizontally; tilted rocks deformed by tectonics  
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principle of superposition   younger formations on top  
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principle of lateral continuity   form in lateral sheets; erosion dissects once continuous layers  
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principle of cross-cutting relations   younger features cut older features  
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principle of inclusions   inclusions always older than enclosing material; must be present to be included  
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principle of fossil succession   index fossils determine time range  
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disconformity   erosion, lack of deposition  
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angular unconformity   relationship is angular  
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non-conformity   sedimentary deposited on top of eroded igneous or metamorphic rocks  
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relative dating   based on order of formation; younger or older  
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absolute dating   actual number of years  
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Hadean Eon   first; formation of Earth, molten core goes to center, oceans formed, meteorites  
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Archean Eon   second; continents, lithosphere formed, meteorites stop, rock record survives, mats of cyanobacteria  
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Proterozoic Eon   third; multi-cellular vertebrates appear  
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Phanerozoic Eon   fourth; Permian extinction @ beginning; hard-shelled organisms (better records), Pangaea rifts apart  
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Mesozoic Era/Jurassic and Triassic Period   Subduction sutures terrenes onto continent, collision build up Rockies, feathered birds, ancestors of mammals  
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Mesozoic Era/Cretaceous Period   seas flood continents, modern fish, flowers  
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K-T boundary event   Cretaceous-Tertiary, meteorite impacts, blots out sun -stops photosynthesis; evidence: plankton-free clay, iridium rich clay, micro tektites, buried crater visible  
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geologic column order   eon - era - period - epoch  
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classification of mass-movements   type of material, rate of movement, nature of mass, immediate surrondings  
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slides   rotational/slump: concave; translational: whole block slides down  
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falls   one chunk drops  
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flows   debri flows: muddy, granular, lahar-style; creep: air freezes, grains pulled out, air warms, grains pulled down  
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factors of slope stability (8)   water (adds weight, lubricates); steepen slope; remove base/top; add material to top (pipes, adds water); remove vegetation; tilted bedding planes; composition of slope; preexisting weaknesses  
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base level   level below which stream cannot erode  
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discharge   cfs  
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bedload   sediment being transported  
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gradient   slope  
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sinuosity   curviness  
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too much discharge   increase sinuosity, decrease gradient - lower discharge meandering stream  
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too much sediment   decrease sinuosity, braided stream  
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