Geologic Time, Mass Wasting, & Rivers
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each of the black spaces below before clicking
on it to display the answer.
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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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Created by:
haleybaker
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