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What question does relative dating ask? |
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In what order did geological events happen? |
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What are the principles of relative age dating? |
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Superposition Original Horizontality Cross-cutting relationships Inclusions Unconformities Angular unconformity Disconformity Nonconformity |
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• Developed by Nicolaus Steno in 1669 • In an undeformed sequence of sedimentary rocks the oldest rocks are on the bottom |
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• Layers of sediment are generally deposited in a horizontal position • Rock layers that are flat have not been disturbed |
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Cross cutting relationships |
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• Younger features cut across older feature |
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• An inclusion is a piece of rock within another rock • Rock containing the inclusion is younger |
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• An unconformity is a break in the rock record produced by erosion and/or non-deposition of rock units |
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• Tilted rocks are overlain by flat-lying rocks |
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• Strata on either side of the unconformity are parallel |
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• Metamorphic or igneous rocks in contact with sedimentary strata |
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Traces or remains of prehistoric life now preserved in rock |
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What rocks are fossils found in? |
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What do fossils aid in the interpretation of? |
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geologic, geographic, and environmental past |
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Conditions favoring preservation |
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• Rapid burial • Possession of hard parts (skeleton, shell, etc.) |
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• Fossil organisms succeed one another in a definite and determinable order • Most any time period can be recognized by its fossil content • Matching of rocks of similar ages in different regions is known as correlation • Correlation often relies upon fossils |
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• Unstable isotopes emit particles and energy in a process known as radioactive decay • Radioactive decay occurs at known rates and using this you can determine the age of certain types of rocks. |
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unstable radioactive isotope |
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results from the decay of a parent |
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the time required for one-half (50%) of the parent to change to daughter product |
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What tells us the age of the sample? |
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Comparing the ratio of parent to daughter |
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Sources of error in radiometric age dating |
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• No parent or daughter is added or subtracted • No daughter product at start • Decay is consistent with time |
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How do you avoid error in radiometric dating? |
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only fresh, unweathered rock samples should be used |
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Sources of error in detrital and metamorphic rocks |
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Definition
• Detrital sedimentary rocks are not the same age as the rock in which they formed • Metamorphic rock age may not necessarily represent the time when the rock formed |
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a) Precambrian time b) Phanerozoic |
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• Eon: the greatest amount of time • Era • Period • Epoch: smallest amount of time |
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• Almost 4 billion years of time prior to the Phanerozoic Comprised of • Proterozoic Eon: 540 to 2500 MYA • Archean Eon: 2500 to 3800 MYA • Hadean Eon: 3800 to 4500 MYA |
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• “Visible life” • Most of earth’s history is preserved here. Comprised of • Paleozoic Era: 570 to 245 MYA • Mesozoic Era 245 to 66 MYA • Cenozoic Era: 66 MYA to present |
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570 to 245 MYA • Dominant large animals: Amphibians/fish • Continents mostly together, similar animals and plant species, flat-few mountain ranges, large, warm, clear, shallow seas. • Appalachians form 350 to 400 MYA. |
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Periods in the Palezoic era |
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• Cambrian (oldest), • Ordovician, • Silurian, • Devonian, • Mississippi, • Pennsylvanian, • Permian (youngest) |
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245 to 66 MYA • Dominant large animals: Reptiles/dinosaurs • The continents began pulling apart, • More diversity in plant and animal species. • Increased mountain building and with that, lots of sediment from erosion. • Pangaea begins to breakup at about 200 MYA. • Rocky Mountains form 66 to 120 MYA. |
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Periods in the Mezzezoic era |
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• Triassic, • Jurassic, • Cretaceous |
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66 MYA to present • Dominant large animals: Mammals • Mountain building begins to slow • Lots of erosion of existing mountains. • Himalayas form 45 MYA. |
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Quantenary Period composed of two Epochs |
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• Pleistocene (oldest), • Recent (less than 10,000 years) |
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Crustal deformation happens through |
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the force applied to rocks • Compressional stress: shortening of a rock body • Tensional stress: stretching of a rock body • Shear: tearing and twisting of a rock body |
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the response of a rock to stress, deformation • Generally involves a change in shape of the rock |
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Elastic deformation Ductile/Plastic deformation Brittle deformation |
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• Changes in shape of rock are reversible (deform it, remove the stress and it returns to its original shape Ex: a rubber band, San Andreas fault |
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Ductile/Plastic deformation |
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• Changes in shape of rock are permanent and not reversible (like folding) Ex: Silly putty pulled slowly or warm taffy |
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• Rocks break once the elastic limit is surpassed • They will fracture (rupture) if the rock is brittle Ex: Silly putty pulled quickly or a dry stick |
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• Measurements used to find the orientation of a rock unit or fault surface • Important tool for geologic maps |
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• Compass direction, level/horizontal direction on the bedding or fault plane |
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• Angle of inclination, max. angle perpendicular to strike. Ex: Follows natural flow direction of water on surface |
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Axial plane Axis Limb Limb dip angle Plunging Double Plunging |
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i) Anticline ii) Syncline iii) Monocline iv) Domes and basins |
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• Uplifted strata in which layers slope away from the axis of the fold or central ridge • When eroded, oldest rocks are in middle and dip away from axis |
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A trough in folded strata with beds that slope toward the axis of the downfold • When eroded youngest rocks are in middle and dip toward axis |
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Step-like folds in horizontally sedimentary strata |
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• Dome: upwarped, circular fold, dip away from center • Basin: downwarped, circular fold, dip toward center |
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A faulting displaces or offsets normally continuous features: a bedding plane, a road, a stream. |
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Normal fault Thrust (low angle) or reverse fault (high angle) Strike slip fault |
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• Tensional setting • Hanging wall is pulled below the footwall |
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• Compressional setting • Hanging wall is pushed above the footwall |
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• Horizontal movement along a fault-line. • Right lateral vs. left lateral (relative motion) |
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• Fractures across which no displacement or offset has occurred. • Columnar joints are a very special (6-sided) type of joint system found typically in basaltic lava flows |
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• An Earthquake is a sudden movement of the Earth’s crust, which originates at or below the surface • Invaluable for studying the interior of the Earth |
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• Tectonic activity • Volcanic eruptions • Bomb testing |
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Small earthquakes that can precede a major earthquake. |
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Smaller earthquakes that follow the main earthquake. Very common |
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An instrument that records earthquakes |
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The zone within the Earth (at depth) where rock displacement produces an earthquake |
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On the Earth’s surface, directly above the focus of an earthquake |
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Properties of seismic waves |
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Definition
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• Move through the material by compressing it • Highest velocity of all seismic waves • Reaches seismographs first |
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• Velocity is less than P waves • Does not travel through liquids |
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• Travel along surface of the Earth • Behave like S waves • Causes intense ground motion during an earthquake • Slower than P or S waves |
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Locating epicenter on an earthquake |
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Definition
• Location found by using a series of seismographs • Determination of elapsed time between arrival of first P wave and first S wave • Use a time-distance graph to determine distance to the epicenter from seismic station • Triangulate using 3 or more stations to get location |
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How do do you measure an earthquake? |
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Definition
Modified Mercalli Intensity Scale Richter Scale c) Seismic moment |
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Modified Mercalli Intensity Scale |
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Definition
• Measures earthquake intensity: Subjective degree of shaking • Depends energy released and distance to epicenter • Type of ground material (soft, hard) • Describes damage to structures • Ranges from I (only felt by a few) to XII (total destruction) |
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• Measures earthquake magnitude • Measures energy released at source of earthquake • Use amplitude of wave taken from seismograph • Logarithmic scale used to express magnitude. Each number on Richter Scale has 32 times more energy |
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• Used for the largest earthquakes • Uses rock properties as well as more distant seismographs • Near seismographs may be max’d out. |
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Earthquakes and plate tectonics |
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• Mostly near plate boundaries • Three main plate boundaries: Divergent (smallest), Transform (medium) and Convergent (largest). |
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• Earthquakes are shallow, more frequent • Generally low magnitudes |
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• Continental transform-medium magnitudes, thick, cool crust-San Andreas Fault Zone • Oceanic transform- mostly near MOR, thin, plastic, warm crust-lower magnitudes |
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• Largest magnitudes • Commonly in subduction zones • The largest earthquakes on earth: 1960 Chile 9.4 |
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Types of earthquake destruction |
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Definition
Ground motion Tsunami Landslides and ground instability Fires Seiches |
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seismic sea waves • Earthquakes under the ocean but on/near seafloor • Waves travel at 400-500 mph in open ocean • Low height in open ocean (less than 1m) • When entering shallow water, they rapidly decelerate and build in height from momentum • First sign can be withdrawal of water from coast; a few minutes later the crest arrives |
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Landslides and ground instability |
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• Commonly triggers landslides • Liquefaction: stable high-fluid content soil turns fluid-like, mostly where loose fill has been added |
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• Sloshing in lakes may cause dams to break |
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Past patterns From trenching Foreshocks and Ground tilt/bulge Changes in animal behavior |
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• Originally measured by lowering lines overboard • Sonar invented in the 1920s • Reflects sound waves off the ocean floor |
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