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Science Bowl-Geology

QuestionAnswer
aa A lava flow that solidifies with a spiny, rubbly surface
ablation or wastage the loss of glacial ice or snow by melting, evaporation, or breaking off into icebergs
abrasion grinding away of rock by friction and impact during transportation
absolute age or numerical age age given in years or some other unit of time
abyssal fan great fan-shaped deposit of sediment on the deep sea-floor at the base of many submarine canyons
abyssal plain very flat sediment-covered region of the deep-sea floor; usually at the base of the continental rise
accreted terrane terrane that did not form at its present site on a continent
accretionary wedge (subduction complex) a wedge of thrust-faulted and folded sediment scraped off a subducting plate by the overlaying plate
accumulation stage stage in the evolution of major mountain belts characterized by the accumulation of great thicknesses (several kilometers) of sedimentary of volcanic rocks
active continental margin a margin consisting of a continental shelf, a continental slope, and an oceanic trench
actualism the principle that the same processes and natural laws that operated in the past are those we can actually observe or infer from observations as operating at present. uniformitarianism has the same meaning as actualism for most geologists
advancing glacier glacier with a positive budget so that accumulation results in the lower edges being pushed outward and downward
aftershock small earthquake that follows a main shock
a horizon or zone of leaching the top layer of soil, characterized by the downward movement of water
alkali soil soil containing such a great quantity of sodium salts precipitated by evaporating ground water that it is generally unfit for plant growth
alluvial fan large fan-shaped pile of sediment that usually forms where a stream's velocity decreases as it emerges from a narrow canyon onto a flat plain at the foot of a mountain range
alpine glaciation glaciation of a mountainous area
amphibole group mineral group in which all members are double-chain silicates
amphibolite amphibole (hornblende), plagioclase schist
andesite fine-grained igneous rock of intermediate composition. Up to half of the rock is plagioclase feldspar with the rest being ferromagnesium minerals
angle of dip a vertical angle measured downward from the horizontal plane to an inclined plane
angular sharp-edged; lacking rounded edges or corners
angular unconformity unconformity in which younger srata overlie an erosion surface on tilted or folded layered rock
anorthosite crystalline rock composed almost entirely of calcium-rich plagioclase fledspar
antecedent stream stream that maintains its original course despite later deformation of the land
anticline an arched fold in which the rock layers usually dip away from the axis of the fold
aquifer a body of saturated rock or sediment through which water can more readily
arch (sea arch) bridge of rock left above an opening eroded in a headland of waves
Archean Eon the oldest eon of Earth's history
arete a sharp ridge that seperated adjacent glacially curved valleys
arid region an area with less that 25 cm of rain per year
arkose a sandstone in which more that 25% of the grains are feldspar
artesian well well where water rises above the aquifer
artificial recharge ground-water recharge increases by engineering techniques
aseismic ridge submarine ridge with which no earthquakes are associated
volcanic ash fine pyroclasts (less that 4 mm)
assimilation process where very hot magma melts country rock and assimilates the newly molten material
asthenosphere region made up of mantle beneath the lithosphere; behaves plastically
atoll circular reef surrounding a deeper lagoon
augite mineral of the pyroxene group found in mafic igneous rocks
aureole zone of contact metamorphism adjacent to a pluton
axial plane plane containing all of the hinge lines of a fold
backarc spreading type of sea-floor spreading that: moves an island arc away from a continent, tears an island arc in two, or splits the edge of a continent, forming a new sea floor
backshore upper part of the beach, landward of the high-water line
bajada broad, gently sloping, depositional surface formed at the base of a mountain range in a dry region by the coalescing of individual alluvial fans
bar ridge of sediment, usually sand or gravel, that has been deposited in the middle or along the banks of a streamby a decrease in stream velocity
barchan crescent shaped dune with the horns of the crescent pointing downwind
barrier island ridge of sand paralleling the shoreline and extending above sea level
barrier reef reef seperated from the shoreline by the deeper water of a lagoon
basal sliding movement in which the entire glacier slides along as a single body on its base over the underlying rock
basalt fine grained mafic, igneous rock composed predominantly of ferromagnesian minerals and with lesser amounts of calcium rich plagioclase feldspar
base level a theoretical downward limit for steam erosion of the Earth's surface
batholith large discordant pluton with an outcropping area greater than 100 square kilometers
bauxite principal ore of Al (Al2O3 * n H20)
baymouth bar ridge of sediment that cuts a bay off from the ocean
beach strip of sediment, usually sand but sometimes pebbles, boulders, or mud, that extends from the low-water line inland to a cliff or zone of permanent vegetation
beach face section of beach exposed to wave action
bedding arrangement of layers or beds of rock
bedding plane nearly flat surface separating two beds of sedimentary rock
bed load heavy or large sediment particles in a stream that travel near or on the stream bed
bedrock solid rock that underlies the soil
Benioff zone distinct earthquake zone that begins at an oceanic trench and slopes landward and downward into Earth at an angle of 30 or 60 degrees
bergschrund the crevasse that develops where a glacier is pulling away from a cirque wall
berm platform of wave-deposited sediment that is flat or slopes slightly landward
B horizon or zone of accumulation soil layer characterized by accumulation of material leached downward from the A horizon above
biochemical precipitated by the action of organisms
bioclastic limestone limestone consisting of fragments of shells, corals, and algae
biotite iron/magnesium-bearing mica
block large, angular pyroclast
blowout depression on the land surface caused by wind erosion
body wave seismic wave that travels through Earth's interior
bomb large spindle or lens shaped pyroclast
bottomset bed delta deposit formed from the finest silt and clay, which are carried far out to sea by river flow or by sediments sliding downhill on the sea floor
boulder sediment particle with a diameter greater than 256 mm
Bowen's reaction series sequence in which minerals crystallize from a cooling basaltic magma
braided stream stream that flows in a network of many interconnected rivulets around numerous bars
breaker wave that has become so steep that the crest of the wave topples forward, moving faster than the main body of the wave
breakwater offshore structure built to absorb the force of large breaking waves and provide quiet water near shore
brittle strain cracking or rupturing of a body under stress
butte narrow pinnacle of resistant rock with a flat top and very steep sides
calcareous containing calcium carbonate
calcite mineral with the formula CaCO3
caldera A volcanic depression much larger than the original crater
capacity (of stream) the total load that a stream can carry
capillary action the drawing of water upward into small openings as a result of surface tension
capillary fringe a thin zone near the water table in which capillary action causes water to rise above the zone of saturation
carbonaceous chondrite stony meteorite containing chondrules and composed mostly of serpentine and large quantities of organic materials
carbonic acid has formula H2CO3 and is a weak acid common in rain and surface waters
cave or cavern naturally formed underground chamber
cement the solid material that precipitates in the pore space of sediments, binding the grains together to form solid rock
cementation the chemical precipitation of material in the spaces between sediment grains, binding the grains together into a hard rock
Cenozoic Era the most recent of the eras (follows Mesozoic)
chain silicate structure silicate structure in which two of each tetrahedron's oxygen ions are shared with adjacent tetrahedrons, resulting in a chain
chalk very fine-grained bioclastic limestone
channel (Mars) feature on the surface of the planet Mars that closely resembles certain types of streams or channels on Earth
chaotic terrain (Mars) patch of jumbled and broken angular slabs and blocks on the surface of Mars
chemical sedimentary rock rock composed of material precipitated directly from solution
chemical weathering decomposition of rock resulting from exposure to water and atmospheric gases
chert hard, compact, fine-grained sedimentary rock formed almost entirely of siica
chill zone in an intrusion, the finer-grained rock adjacent to a contact with country rock
chondrule round silicate grain within some stony meteorites
C horizon soil layer composed of incompletely weathered parent material
cinder (volcanic) pyroclast approximately the size of a sand grain. Sometimes defined between 4 and 32 mm
cinder cone volcano constructed of loose rock fragments ejected from a central vent
circum-Pacific belt major belt around the edge of the Pacific ocean on which most composite volcanoes are located and where many Earthquakes occur
cirque steep-sided, amphitheater-like hollow carved into a mountain at the head of a glacial valley
clastic sedimentary rock sedimentary rock composed composed of fragments of preexisting rock
clastic texture arrangement of rock fragments bound into a rigid network by cement
clay sediment composed of particles with a diameter of 1/256 nm or less
clay mineral hydrous aluminum silicate that occurs as a platy grain of microscopic size with a sheet silicate structure
clay mineral group collective term for several clay minerals
cleavage ability of rock to break along preferred planes
coal sedimentary rock formed from the consolidation of plant material. Rich in carbon, usually black, and burns readily
coarse-grained rock rock in which most of the grains are larger than 1 mm for igneous and 2 mm for sedimentary
coast land near the sea, including the beach and a strip of land inland from the beach
coastal straightening the gradual straightening of an irregular shoreline by wave erosion of headlands and wave deposition in bays
cobble a sediment particle with a diameter of 64 to 256 mm
column a dripstone feature formed when a stalactite downward and a stalactite growing upward meet and join
columnar structure or columnar jointing volcanic rock in parallel, usually vertical columns, mostly 6-sided
comet small object in space, no more than a few kilometers in diameter. composed of frozen methane, frozen ammonia, and water ice, with small solid particles and dust imbedded in the ices
compaction loss in overall volume and pore space of a rock as the particles are packed closer together by the weight of overlying material
competence largest particle that a stream can carry
composite volcano or stratovolcano volcano constructed of alternating layers of pyroclastics and rock solidified from lava flows
compressive directed pressure directed pressure that tends to compress some portions of a body more than other portions
compressive stress stress due to a force pushing together on a body
conchoidal fracture curved fracture surfaces
concordant parallel to layering or earlier developed planar structures
concretion hard, rounded mass that develops when a considerable amount of cementing material precipitates locally in a rock, often around an organic nucleus
cone of depression depression of the water table formed around a well when water is pumped out; it is shaped like an inverted cone
confined aquifer or artesian aquifer aquifer completely filled with pressurized water and separated from the land surface by a relatively impermeable confining bed (such as shale)
confining pressure (also called geostatic or lithostatic pressure) pressure applied equally on all surfaces of a body
conglomerate coarse-grained sedimentary rock (grains coarser than 2 mm) formed by the cementation of rounded gravel
consolidation any process that forms firm, coherent rock from sediment or from liquid
contact boundary surface between two different types or ages of rocks
contact (thermal) metamorphism metamorphism under conditions in which high temperature is the dominant factor
continental crust thick, granitic crust under continents
continental drift concept suggesting that continents move over the Earth's surface
continental glaciation covering of a large region of a continent by a sheet of glacial ice
continental rise wedge of sediment that extends from the lower part of the continental slope to the deep sea floor
continental shelf submarine platform at the edge of a continent, inclined very gently seaward generally at an angle of less than 1 degree
continental slope relatively steep slop extending from a depth of 100 to 200 m at the edge of the continental shelf down oceanic depths
contour current bottom current that flows parallel to the slopes of the continental margin (along the contour rather than down the slope)
contour line line on a topographic map connecting points of equal elevation
convection (current) very slow circulation of a substance driven by differences in temperature and density within that substance
convergent plate boudary boundary between two plates that are moving toward each other
conquina limestone consisting of coarse shells
core central zone of the Earth
correlation determining time equivalency of rock units (rock units may be correlated within a region, a continent, and even between continents)
country rock any rock that was older than and intruded by igneous rock
crater (volcano) basinlike depression over a vent at the summit of a volcanic cone
Created by: 1150230574
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