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Vibratiosns of Earth produced by rapid release of energy |
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location directly above the focus, on the surface |
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- Body Waves-Primary & Secondary
- Surface waves
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Differences between magnitudes |
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Richter-Amplitude of largest seismic wave
Moment-Amout of displacement along fault
Mercalli Intensity-California buildings |
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Used to measure each station's distance from epicenter |
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Material saturated with water turns into a flow |
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Primary: Fast; through solid, liguid or gas |
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A. Wegener's continental drift |
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Definition
1915-Pangaea drifeted and broke along oceanic crust |
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Continental Drift evidence |
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Definition
- Fossils
- Rocks
- Ice Ages
- Climates
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Continental Drift objection |
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Inability to prove a mechanism |
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Definition
- Divergent (apart)-ocean ridges and seafloor spreading [pillow lava]
- Convergent (collide)-oceanic trench and lithosphere subduction [Japan]
- Transform (slide)-crust is neither created nor destroyed [San Andreas Fault]
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Where does new lithosphere form? |
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Definition
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Forces pull ocean crust apart at ridge crests |
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Convergent boundaries, lithosphere is descending into the mantle |
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Surface formed as oceanic lithosphere descends into mantle |
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Volcanoe produced by subduction of lithosphere |
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Age and magnetism of ocean floor rocks |
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Convergent Plate Boundaries |
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Definition
- Oceanic-Oceanic (O-O)-Oceanic slabs converge and form valcanoes
- Continental-Continental (C-C)-Subucting continental plates collide
- Oceanic-Continental (O-C)
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How do the Himalayas form? |
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Definition
Continental-Continental convergence |
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Rising plumes of mantle are beneath Hawaii and as the plates move, new islands are formed by the cooled hot rock |
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- Slab-pull slab-push
- Deposits minerals
- Distribution of earthquakes, volcanoes and mountains
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The study of folding (bending) and faulting (breaking) of rocks |
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Elastic, ductile and brittle deformation |
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Definition
- Elastic-Returns to original shape
- Ductile/Plastic-Permanent (folding)
- Brittle-Breaks (faulting)
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Structures formed by ductile/plastic deformation |
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Definition
- Anticlines-Shaped up, old rocks in center
- Synclines-Shaped down, young rocks in center
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Structure formed by brittle deformation |
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- Normal-Hanging wall moves down
- Reverse-Haning wall moves up (dips >45)
- Srike-Slip-Dominant displacement is horizontal to the strike
- Transform-Cuts through lithosphere (plate boundaries)
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Placing rocks/events in proper order |
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Principle of Superposition |
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Oldest rocks are on the bottom |
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Principle of Original Horizontality |
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Sed. layers are generally deposited in horizontal layers |
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Principle of Cross-Cutting |
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Definition
Younger features cut across older |
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Rock containing inclusion is younger |
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Tilted rocks overlaid by flat-lying rocks |
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Metamorphic or igneous rocks in contact with sed. strata |
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Strata on either side are parallel |
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Significance of unconformity |
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Break in the rock record produced by erosion or non-deposition of rocks |
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Element with same # protons, different # nuetrons |
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Time required for one half of radioactive nuclei to decay |
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