Copy of `Iowa State University - Geology terms`
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Iowa State University - Geology terms
Category: Education > University
Date & country: 18/11/2013, USA Words: 782
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drainage divideThe line that separates one drainage basin from another.
driftGlacial deposits laid down directly by glaciers or laid down in lakes, ocean, or streams as result of glacial activity.
dripstoneCalcium carbonate deposited from solution as water enters a cave through the zone of aeration. Forms stalactites, stalagmites and other cave deposits.
drumlinStreamlined hill, largely of till, with blunt end pointing into direction from which ice moved. Occur in clusters called drumlin fields.
dry farmingFarming without irrigation in drylands.
drylandsA general term for semiarid and desert lands.
ductileStructural behavior in which a material deforms permanently without fracturing.
dust bowlAn area subject to dust storms, especially south central United States.
dust devilA small, dust-bearing whirlwind.
dust stormLarge volume of dust-sized particles lifted high into the atmosphere.
Earth systemSystem involving continuous interaction of the solid Earth, the atmosphere, the oceans and living things.
earthflowA form of slow, but perceptible, mass movement, with high content of water and rock debris. Lateral boundaries are well-defined and the terminus is lobed. With increasing moisture content grades into a mudflow.
eccentricity of the EarthA measure of the circularity of the Earth
elasticNon-permanent structural deformation during which the amount of deformation (strain) is proportional to the stress.
elastic reboundThe statement that movement along a fault is the result of an abrupt release of a progressively increasing elastic strain between the rocks on either side of the fault.
elasticityThe tendency for a body to return to its original shape and size when a stress is removed.
electronA fundamental unit of matter, negatively charged and disposed in a cloud surrounding the nucleus of an atom.
electron captureNuclear decay in which a proton in the nucleus acquires an electron from the outer cloud of the atom
electron shellA characteristic energy level with which an electron is associated. Electrons occupy discrete shells within the cloud surrounding an atom
elementsee chemical element
end morainesee terminal moraine.
eonThe primary division of geologic time which are, from oldest to youngest, the Hadean, Archean, Proterozoic, and Phanerozoic eons.
epicenterThe point on the Earth
epochA division of geologic time next shorter than a period. Example: the Pleistocene epoch is in the Quaternary period.
equilibrium lineOn a glacier the line separating the zone of accumulation from the zone of ablation .
eraA division of geologic time next smaller than the eon and larger than a period. Example: The Paleozoic era is in the Phanerozoic eon and includes, among others, the Devonian period.
erraticA stone or boulder, glacially transported from place of origin and left in an area of different bedrock composition.
eskerA winding ridge of stratified drift . Forms in a glacial tunnel and, when ice melts, stands as ridge up to 15 m high and kilometers in length.
eustatic change in sea levelA worldwide change in sea level, such as caused by melting glaciers.
eutrophicationThe process of aging of lakes by the addition of nutrients.
evaporiteA mineral or rock deposited directly from a solution (commonly seawater) during evaporation. For example, gypsum and halite are evaporite minerals.
exfoliationThe process by which concentric scales, plates, or shells of rock are stripped or spall from the bare surface of a large rock mass.
exfoliation domeA large dome-shaped form that develops in homogeneous crystalline rocks as the result of exfoliation.
exotic riverA river that is able to maintain its flow through a desert because of water received from outside the desert.
extrusivePertaining to igneous rocks or features formed from lava released on the Earth
faciessee metamorphic facies , sedimentary facies
failed riftA rift emanating from a plate triple junction along which minimal divergence has taken place.
fallWhen applied to mass movement of material refers to free fall of material moving without contact with the surface.
faultThe surface of rock rupture along which there has been differential movement of the rock on either side.
fault gougeSoft, uncemented, pulverized clay-like material found along some faults.
ferromagnesianContaining iron and magnesium, applied to the mafic minerals. Example: olivine.
fetchDistance over which wave-forming winds blow.
field capacitysee specific retention.
fiery cloudsee nu
firn(n
fissionThe spontaneous or induced splitting, by particle collision, of a heavy atomic nucleus into a pair of fragments plus some neutrons. Controlled induced fission can be used as a source of nuclear power.
fission track datingDating of minerals by fission tracks, damage tracks left in a mineral by spontaneous alpha emissions.
fissure eruptionAn eruption of lava that takes place from a fracture, usually without producing a cone.
fjordGlaciated valleys now flooded by the sea.
flash floodA flood that rises and falls very rapidly.
flashy streamA stream with a high, short flood peak and short lag time.
flintA variety of chert , often black because of included organic matter.
floodPeak flow that tops the banks of a stream channel.
flood recurrence intervalThe number of years of record plus 1 divided by the rank of each maximum annual flood.
floodplainArea bordering a stream over which water spreads when the stream tops its channel banks.
flowWhen applied to mass movement, refers to a chaotic movement of material in continuous contact with the ground surface, commonly involving a moderate to high amount of water.
flow foldingA fold formed in relatively fluid rocks that have flowed toward a synclinal trough.
flowstoneGeneral term for deposits formed by dripping and flowing water on walls and floors of caves.
fluid inclusionA tiny cavity in a crystal, commonly 1 to 100 microns in diameter, containing liquid and/or gas. Formed by the entrapment of fluid during the growth or subsequent deformation of the crystal.
focusThe point within the Earth which is the center of an earthquake, at which strain energy is first released and converted to elastic wave energy.
fold and thrust mountainsMountains, characterized by extensive folding and thrust faulting, that form at convergent plate boundaries on continents.
foliationA planar structure that develops in metamorphic rocks as a result of directed pressure.
foot wall blockThe body of rock that lies below an inclined fault plane. compare hanging wall block
foreset bedInclined layers of sediment deposited on the advancing margin of a growing delta or along the slip face of a sand dune.
foreshockA minor tremor that precedes an earthquake. An increase in seismicity may signal that a major release of strain energy is about to occur.
foreshoreLies between low and high tide marks.
formation waterThe water, held in pore volume in sedimentary rocks, that has persisted with little change in composition since it was buried with the sediment.
fossilEvidence in rock of the presence of past life, such as a dinosaur bone, an ancient clam shell, or the footprint of a long-extinct animal.
fossil fuelA hydrocarbon (coal or petroleum) that can be extracted from the Earth for use as a fuel. Fossil fuels are non-renewable energy sources.
fractional crystallizationA sequence of crystallization from magma in which the early-formed crystals are prevented from reacting with the remaining magma, resulting in a magma with an evolving chemical composition.
fragipanA dense layer of soil, containing silt and sand but no organic matter and little clay, whose extreme hardness and impermeability are due primarily to compaction. compare caliche , claypan, hardpan.
free oscillationA vibration of a body such as a bell or the Earth that continues without further influence after an initial event.
fringing reefA coral reef attached directly to the mainland.
frost wedgingA type of disintegration in which jointed rock is forced apart by the expansion of water as it freezes in fractures.
fusionThe combination of two light nuclei to form a heavier nucleus, with the accompanying release of energy. This is the source of energy in a hydrogen bomb. If it could be controlled, it could serve as an alternative to fission in nuclear power generation.
gabbroA coarse-grained igneous rock, chemically equivalent to a basalt.
gardeningThe constant and slow churning of the lunar regolith as the result of meteorite impacts.
geanticlineAn anticlinal structure presumed to form in the context of geosynclinal evolution. Not in current use since the development of plate tectonic theory.
geodeRoughly spherical, hollow or partially hollow accumulation of mineral matter. A few centimeters to nearly 0.5 m in diameter. Outer layer of chalcedony lined with crystals that project toward the hollow center. Crystals, often perfectly formed, usually quartz although calcite and dolomite and
geologic columnThe arrangement of rock units in the proper chronological order from youngest to oldest.
geologic time scaleThe chronological sequence of units of Earth time.
geologyThe science that deals with the study of the planet Earth
geosynclineA downwarping of the Earth
geothermal energyHeat extracted from the Earth for use as an power source.
geothermal gradientThe rate at which temperature increases with depth below the surface.
geyserA type of thermal spring which ejects water intermittently with considerable force.
glaciationThe formation, advance and retreat of glaciers and the results of these activities.
glacierA mass of ice, formed by the recrystallization of snow, that flows forward, or has flowed at some time in the past.
glacier iceIce with interlocking crystals that makes up the bulk of a glacier.
glassAn inorganic solid in which there is no crystalline structure .
glassyA texture of extrusive igneous rocks that develops as the result of rapid cooling, so that crystallization is inhibited.
global warmingThe prediction that climate will warm as a result of the addition to the atmosphere of humanly produced greenhouse gases.
gneissA coarse, foliated metamorphic rock in which bands of granular minerals (commonly quartz and feldspars) alternate with bands of flaky or elongate minerals (e.g., micas, pyroxenes). Generally less than 50% of the minerals are aligned in a parallel orientation.
gneissosityThe style of foliation typical of gneiss.
gougesee fault gouge
grabensee rift
graded beddingType of bedding sedimentary deposits in which individual beds become finer from bottom to top.
gradientSlope of a stream bed or hillside. The vertical distance of descent over horizontal distance of slope.
graniteLight colored, coarse grained, intrusive igneous rock characterized by the minerals orthoclase and quartz with lesser amounts of plagioclase feldspar and iron-magnesium minerals. Underlies large sections of the continents.
granitic beltA region of granitic rock, one of two characteristic regions within cratons .