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Iowa State University - Geology terms
Category: Education > University
Date & country: 18/11/2013, USA Words: 782
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granitizationA metamorphic process by which solid rock is converted into granite by the addition or removal of material, without passing through a magmatic stage. compare metasomatism .
gravitational heatingPlanetary heating caused by the conversion of potential energy into heat. Associated with the iron catastrophe .
gravitational moistureWater in the zone of aeration that is moving down toward the zone of saturation.
graywacke() ) A variety of sandstone characterized by angular-shaped grains of quartz and feldspar, and small fragments of dark rock all
greenhouse gases Gases (primarily water and carbon dioxide, but also a variety of sulfur and nitrogen compounds and gaseous hydrocarbons) that trap the Sun
greenstoneAn altered or metamorphosed mafic igneous rock that owes its dark color to the presence of chlorite, epidote, or amphiboles.
greenstone beltA region of greenstones, one of two characteristic regions within cratons .
groinA wall built out from the shore, usually at perpendicular to it to trap sand carried by longshore currents .
grooveA broad, deep, generally straight furrow carved in bed rock by the abrasive action of debris embedded in a moving glacier. Larger and deeper than a glacial striation.
ground moraineTill deposited from main body of glacier during ablation.
ground waterWater beneath the Earth
ground water tablesee water table .
guyotsee seamount
habitA general term for the outward appearance of a mineral, defined by the relative sizes and arrangement of characteristic crystal faces.
HadeanThe oldest eon in Earth history, extending from the origin of the Earth to about 3.9 billion years ago.
half-lifeThe amount of time that it takes for one half of an original population of atoms of a radioactive isotope to decay.
hanging valleyA valley whose mouth is high above the floor of the main valley to which it is tributary. Usually, but not always, the result of mountain glaciation.
hanging wall blockThe body of rock that lies above an inclined fault plane. compare foot wall block
hardnessResistance of a mineral to scratching, determined on a comparative basis by the Mohs scale .
hardpanA general term for a relatively hard layer of soil at or just below the ground surface, cemented by silica, iron oxide, calcium carbonate, or organic matter. compare caliche , claypan, fragipan.
head(hydraulic head) The level to which ground water in the zone of saturation will rise.
heat flowThe amount of thermal energy leaving the Earth per cm2/sec.
heaveIn mass movement the upward motion of material by expansion as, for example, the heaving caused by freezing water.
hiatusA gap or interruption in the continuity of the geologic record either because the record was never formed or because it was destroyed by erosion. It represents the time interval spanned by an unconformity .
high level nuclear wasteRadioactive waste from defense activities of the U. S. government and from spent fuel rods from nuclear reactors.
hinge faultA fault along which there is increasing offset or separation along the strike of the fault plane, from an initial point of no separation.
hoodooA column or pillar of rock produced by differential weathering in a region of sporadic heavy rainfall, commonly facilitated by joints and by rock layers of varying hardness.
HookeA statement of elastic deformation, that strain is directly proportional to stress.
hornThe sharp spire of rock formed as glaciers in several cirques erode into a central mountain peak.
hot spotA region of high heat flow on the Earth
humusThe generally dark, more or less stable part of the organic matter in a soil, so well decomposed that the original sources cannot be identified.
hydraulic conductivityMeasure of permeability in Earth materials.
hydraulic gradientThe slope of the water table. Measured by the difference in elevation between two points on the slope of the water table and the distance of flow between them.
hydraulic head see head.
hydrographGraph of variation of stream flow over time.
hydrologic system(or hydrologic cycle) The pattern of water circulation from the ocean to the atmosphere to the land and back to the ocean.
hydrolysisA decomposition reaction involving water, in which hydrogen ions (H+) or hydroxyl ions (OH-) replace other ions. The result is a new residual mineral. Example: the addition of water to orthoclase produces kaolinite and releases K+ and silica into solution.
ice sheetA broad, mound-like mass of glacier ice that usually spreads radially outward from a central zone.
ice shelfA floating ice sheet extending across water from a land-based glacier.
icecapA small ice sheet.
igneous rockA rock that has crystallized from a molten state.
inclined bedding(cross-bedding) Bedding laid down at an angle to the horizontal, as in many sand dunes.
inclined foldA fold whose axial plane is inclined from the vertical, but in which the steeper of the two limbs is not overturned. compare overturned fold.
inclusion(xenolith) A fragment of older rock caught up in an igneous rock.
index fossilA fossil that identifies and dates the strata in which it is typically found. To be most useful, an index fossil must have broad, even worldwide distribution and must be restricted to a narrow stratigraphic range.
index mineral A mineral formed under a particular set of temperature and pressure conditions, thus characterizing a particular degree of metamorphism.
inertiaThe tendency of a body to resist acceleration . A moving body tends to keep moving at a constant speed in the same direction, and a stationary body tends to remain in one place, unless acted upon by an outside force.
inner coreThe solid innermost part of the core with a diameter of a little over 1,200 km.
intensityA measure of the size of an earthquake in terms of the damage it causes.
interlobate moraineRidge formed along junction of adjacent glacier lobes.
intrusivePertaining to igneous rocks or features formed by the emplacement of magma in pre-existing rock.
ionAn atom that has an electrical charge, by virtue of having gained or lost electrons. see cation, anion
ionic radiusThe effective distance from the center of an ion to the edge of its electron cloud.
ionic substitutionThe replacement of one or more ions in a crystal structure by others of similar size and electrical charge. Example: Fe2+ is interchangeable with Mg2+ in most ferromagnesian minerals.
iron catastropheThe period in the Hadean eon during which much of the iron in outer portions of the Earth migrated toward the center of the planet, producing the core and releasing large amounts of gravitational heat.
ironpanA hardpan in which iron oxides are the primary cementing agents.
island arcA curved belt of volcanic islands lying above a subduction zone. compare continental arc.
isochemical reactionA reaction in which chemical constituents of a rock are rearranged to form a new mineral assemblage, but no material is added to or lost from the rock as a whole. Applied generally to diagenetic or metamorphic environments.
isoclinal foldA fold in which the limbs are parallel.
isogradA line on a map joining points at which metamorphism took place under similar temperature and pressure conditions, as indicated by rocks belonging to the same metamorphic facies . Generally, the line separates two adjacent metamorphic zones, as indicated by specific .
isoseismal lineA line on a map joining points of equal earthquake intensity.
isostasyThe condition of equilibrium, comparable to floating, of units of the lithosphere above the asthenosphere .
isostatic change in sea levelA sea level change due to change in load on Earth
isotopeAtoms that differ in atomic mass number , but not in atomic number , are called isotopes. For example, oxygen (atomic number 8) may have an atomic mass number of 16, 17, or 18, depending on whether it has 8, 9, or 10 neutrons. It therefore has three isotopes.
jasperA red variety of chert , its color coming from minute particles of included hematite.
jet flowFlow in which fluid moves at high speed in jet-like surges as does water in free fall over a falls.
jettySimilar to a groin but built to keep sand out of a harbor entrance.
jointA surface of fracture in a rock, without displacement parallel to the fracture.
juvenile hydrothermal fluidA hot fluid, largely water, presumed to have been released from a magma.
kameStratified drift deposited in depressions and cavities in stagnant ice and left as irregular, steep sided hills when the ice is melts.
kame terraceStratified drift deposited between wasting glacier and adjacent valley wall. Stands as a terrace when glacier melts.
karstA landscape that develops from the action of ground water in areas of easily soluble rocks. Characterized by caves, underground drainage and sinkholes.
kettleDepression in ground surface formed by the melting of a block of glacier ice buried or partially buried by drift.
komatiiteAn ultramafic rock with a non-cumulate texture, presumed to be extrusive.
laccolithA concordant igneous intrusion with a flat floor and a convex upper surface, usually less than 8 km across and from a few meters to a few hundred meters thick at its thickest point.
lag timeThe delay in the response of stream flow between precipitation and flood peak.
laharA mudflow composed chiefly of pyroclastic material on the flanks of a volcano.
laminar flowFluid flow in which flow lines are distinct, and parallel and do not mix. compare turbulent flow .
lateral continuityThe extent of a rock unit over a considerable but definite area.
lateral moraineMoraine formed by valley glaciers along valley sides.
lateriteA highly weathered red soil rich in iron and aluminum oxides. Typically formed in a tropical to temperate climate where intense chemical weathering is common.
LaurasiaThe northern portion of the late Paleozoic supercontinent called Pangea.
lavaMolten rock that flows at the Earth
lava domeA steep-sided rounded extrusion of highly viscous lava squeezed out from a volcano and forming a dome-shaped or bulbous mass above and around the volcanic vent. The structure generally develops inside a volcanic crater.
lava flood(plateau basalt) A term applied to large areas of basaltic lava presumably extruded from fissures.
lava lakeA lake of lava, usually basaltic, in a volcanic caldera.
layered complexAn intrusive igneous body in which there are layers of varying mineral content.
leveesBanks of sand and silt along stream bank built by deposition in small increments during successive floods.
limestoneA sedimentary rock composed mostly of the mineral calcite, CaCO3.
linear duneLong, straight dune with slip faces on each side.
lineationA general term applying to any linear feature in a metamorphic rock.
liquefactionThe transformation of a soil from a solid to a liquid state as the result of increased pore pressure.
lithic sandstonesee graywacke.
lithificationThe process by which an unconsolidated deposit of sediments is converted in to solid rock. Compaction, cementation and recrystallization are involved.
lithophileSaid of an element that has a greater chemical affinity for silicate rocks than for sulfides or for a metallic state. Example: Aluminum.
lithosphereThe rigid outer shell of the Earth. It includes the crust and uppermost mantle and is on the order of 100 km in thickness.
lithostatic stressThe confining (non-directed) pressure imposed by the weight of overlying rock.
littoral currentsee longshore current.
loadOf a stream, the amount that it carries at any one time.
loessDeposits of wind-borne dust.