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*age of rocks/ geologic features/ events relative to each other *sequence of events |
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age of rocks, etc in yeras before present |
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*younger sediments are deposited atop older sediments *in an undisturbed sequence of sedimentary rocks older layers will occur deeper in the sequence |
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*sediments are deposited in essentially flat-laying layers *tilted layers indicate events after deposition |
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cross cutting relationships |
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*younger features cut across older features *faults, igneous intrusions |
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*rock unit containing inclusions formed after rock unit providing inclusions |
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*fossils succeed (follow)each other in a well defined order *fossils not randomly distributed through the rock record *fossil content of a sedimentary rock is charactersistic of the time when that rock formed |
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*(1800) *england *canal builder |
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*a gap in the geologic record *a buried erosional surface *a buried landscape |
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examples of simple uncomformities |
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*deposit sediment layer *lithify sediment *uplift/erode *subside/deposit new sediment *lithify new sediment *uplift |
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examples of angular uncomformity |
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basics of absolute dating one |
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*normally applied to igneous rocks (date the time when a particular crystal formed and radioactive elements within the crystal serve as internal "atomic clock" |
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*spontaneous ejection of capture of subatomic particles by an atomic nuclues |
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process of radioactive decay |
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*composition of nucleus changes *therefore one element changes into another *energy released |
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examples of radioactive decay |
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*alpha emission: nucleus ejects 2P+2N *beta emission: neutron ejects electron and turns into proton *electron capture: proton absorbs an electron and turns into neutron |
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elements with same number of protons but different number of neutrons |
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radioactive isotope that decays |
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what the parent isotope turns into |
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*time for half the quantity of a radioactive isotope to decay *geometric rate process |
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*linear rate- constant amount in a given time interval *geometric- constant fractions in given time interval |
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*orthoclase- KAlSi3O8 *contains K, NO Argon *contains some radioactive K-40. *K-40-----Ar40 half life 1.3 B.Y. |
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assumptions for radiometric dating for crystals |
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*know 1/2 life *invariant 1/2 life= basic principle for physics *parent isotope lost only through radioactive decay and no additional parent isotope added after the mineral forms *daughter isotope is formed only through radioactive decay of parent isotope and no daughter isotope lost from the crystal |
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applied assumptions to K-Ar method |
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*orthoclase crystal inside of granite *potassium gradually decays into Argon *heat up atoms and apply pressure *argon is out of there *no longer a closed crystal system |
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*choose an unaltered rock *use more than one radiometric dating method *date more than one mineral |
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C-14 radioactive isotope of carbon decays to N-14 *forms in upper atmosphere and its breathed in/consumed by organisms *1/2 life is 5730 yrs *normal stable carbon is C-12 *when alive organsims have constant C-14/C-12 ratio, after death ratio diminishes |
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*fragmentation and chemical decomposition of rock *physical (mechanical weathering) *chemical weathering |
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layer of weathered rock mineral fragments and soil that blankets most of earths surface (dirt) |
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*clay rich regolith formed from intense in place chemical weathering of bed rock *retains appearance and structure of the original rock *commonly red or orange *commin in west ga area |
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*combo of mineral grains, organic matter, water and air that supports plant growth *dark color.. organic matter |
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mechanical weathering process |
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*frost wedging--expansion of water to ice, cracks rocks apart. -talus (talus slope) **exfoliation/sheeting/unloading-- cracks form paralledl to land surface as overlying rock is stripped away *common in exhumed igneous intrusions |
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chemical decomposition of mineral into other minerals or non mineral substance |
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types of chemical weathering |
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*ionic dissociation *hydrolysis *oxidation |
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"dissolution" *minerals dissociate in water ex- halite, NaCl *major factor only for evaporite minerals |
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-main process for silicates *H or OH replace atoms w thin minerals *aided by acidic conditions *examples- calcite plus carbonic acid--- cations plus carbinate ions ** orthoclase feldspar plus carbonic acid-- kaolinite |
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combined iron metal with oxygen (iron oxides) *red color bc of iron being oxidized hematite |
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what controls the weathering rate? |
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*minerals *rock structure *climate |
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some are more resistant quartz- highly resistant calcite- dissolves in water |
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determining the rate fractures, porosity, etc |
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the most important factor of the wearthering rate (ex- water, wind, temp, humidity/rainfall) |
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*generates a lot of sediment *movement of rock or regolith downhill under the direct influence of gravity *important bc it could be deadly *expensive |
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*rock slide *slumping *flow *creep |
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occurs in unconsolidated material |
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*sediment and water moving as a fluid (mud flow) *ex- mud flow, debris flow, earth flow |
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very slow movement caused by cyclic expansion of the sediment and it could be a freeze/thaw or wetting/drying contraction of sediment |
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*oversteepening *water *vegetation loss *eathquakes |
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*river erosion *sea waves *construction/digging activity |
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*at the simplest level *adds weight or can weaken clays *running water can cause erosion *water pressure force pores or fractures open and decreases friction *"hydrolic jack" (bean can demo) |
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no roots to anchor your soil, no cover to absorb water |
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*rivers *gradient *velocity *discharge *alluvium |
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*slope of stream channel *controls velocity of flowing water |
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*speed of current *controls size of sediment particles that water can carry |
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*volume of water flowing past a point in a stream during a given time interval *measured in volume per unit time gallons per minute (GPM) cubic feet per second (CFS) |
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*detrital sediment deposited by running water *(sand gravel mud) |
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*flat floor of a valley built uo with flood deposits of alluvium *created by repeated flooding |
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*stram that wanders back and forth with broad looping curves *typically located of floodplain |
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*velocity of water *most important *meandering stream |
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former portion of the stream channel, now cut from stread water-filled |
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sediment choked stream, made of many intersecting channels |
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*bed load *suspended load *dissolved load |
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(coarsest sediment) bounced dragged, rolled along stream bed; sand and gravel *can even move boulders during large floods |
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(fine sed) carried suspended by moving water- silt and clay and mud |
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material chemically dissolved in H20 *chemically weathering products (Ca, Na, HCO3, SO4) *pollution (Ca, HCO3, Na) |
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*river/stream delta *alluvial fan *stream channel/floodplain |
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*located where a river mets the sea *river flows into the sea and velocity drops and sediment is deposited *as sediment is deposited, the river shifts position-- delta lobes |
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"delta on dry land" *delta forms when a stream exits a mountain valley *water velocity decreases |
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stream channel/floodplain |
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*point bars *braided streams- flow across comp sed channel *backswamp- flood plain away from channel (fine grain sediment like mud) *natural levees- on floodplain adjacent to channel (coarse sed) ridges of sand parallel to channel cross section |
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parallel to the river-small streams *prevent flooding by the river *built out of sed rock |
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*largest source of easily accessible fresh water *naturally purified *remains in ground for X period of time *occurs dispensed in tiny pores within rock and sed, not unergound rivers/lakes |
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*giant groundwater reservior *water constantly added to resevior *recharge- water constantly leaving underground *discharge= balance |
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measure of open space within material *determines amount of water that rock of sed can hold |
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ease with which a fluid can flow through a solid *determines how easily you can extract water from ground |
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water table and related terms |
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*unsaturated zone *saturated zone *water table |
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area of subsurface in which pores are not saturated with water |
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pores saturated with water |
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*boundaries between sat and unsat *level to which ground is filled up w water *rises and falls with changes in recharge and discharge *not always flat |
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*gaining streams *losing strams |
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*streams receive water from undre ground *most streams are gaining streams *naturally all streams are gaining |
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*stream that loses water into undergound *found in deserts, arid climates, a lot of bedrock |
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aquifers and related terms |
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*aquifer *confining layer *unconfined layer *unconfined aquifer *confined aquifer *artesian well *perched aquifer *well *spring *seep |
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a water saturated geologiv unit that can transmit significant amounts of water units normal hydrologys conditions *rock alluvium saprolite etc *useable amounts of water |
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a low permeability unit that acts as a barrier to groundwater flow |
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(water table aquifer) *an aquifer bounded on its top surface by the water table |
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an aquifer capped by a confining layer (also referred to as an artesian aquifer) |
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*a well in which water rises above the top of aquifer *occur in confined and unconfined aquifers *flowing well |
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a small aquifer above main water table |
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a hole dug or drilled below water table to extract water |
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a location of concentrated groundwater discharge |
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a location of deffused groundwater discharge |
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*mostly metamorphic rock *AL-NJ (includes west ga) *metamorphoc rocks overlain by saprolite *wells |
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metamorphic rocks (piedmont) |
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*saprolite= high porosity low perm *bedrock= low porosity, fractures so high perm |
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*10 ft to 60 ft *dug, bored (augured) *2ft- 4ft diameter |
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*80 feet to 600 feet deep *drilled *6 in diamter well |
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*karst- provence of slovenia *landscape underlain by water- soluble bed rock |
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*limestone (most), gypsum, rocksalt *features-caves, sinkholesm losing streams *subsurface erosion- water dissolves bedrock, few to no surface streams *large springs |
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