WATER WARS: A look at Gallatin Valley Water Controversies

Stop 5:
Day Ranch

Stop 6:
Fish Creek

Stop 7:
Other Considerations



Glossary of Terms

A - B - C - D - E - F - G - H - I - J - K - L - M - N - O - P - Q - R - S - T - U - V - W - X - Y - Z

alluvium: the detrital materials eroded, transported and deposited by streams and rivers.

aquifer: a permeable body of rock capable of yielding quantities of groundwater to wells or springs

aquitard: a bed of low permeability adjacent to an aquifer; may serve as a storage unit for groundwater although it does not yield water readily

Archean: a term meaning ancient, which has been applied to the oldest rocks of the Precambrian.

basement: a set of rocks, usually of igneous or metamorphic rock, that is overlain by younger sedimentary strata. A crustal layer beneath a sedimentary one. The ancient continental igneous rock base that lies beneath Precambrian rocks.

bench: a terrace of level earth or rock that is raised and norrow and that breaks the continuity of a slope

braided river: complex tangle of converging and diverging stream channels separated by sand bars or islands. Characteristic of flood plains where amount of debris is large in relation to discharge .

crystalline rock: a rock made up of minerals in a clearly crystalline state; igneous or metamorphic rock as opposed to sedimentary rock

depositional environment: the environment in which materials were laid, placed or thrown down; specifically the constructive process of accumulation into beds, veins or irregular masses of any kind of loose, solid rock material by any kind of natural agent.

gneiss: a variety of rocks with a banded or coarsely foliated structure formed by regional metamorphism

groundwater: the water contained in interconnected pores located below the water table in an unconfined aquifer or located in a confined aquifer

grain size: average size of mineral particles composing a rock or sediment

impermeable: a rock or unit in which water can not flow thorough

paleotopography: the topography given to an area in geologic past

permeable: a porous formation or rock through which hydrocarbon fluids or water can flow

pore: an opening or channel way in rock or soil

porosity: the ratio of the volume of void spaces in a rock or sediment to the total volume of the rock or sediment

Quaternary: the second period of the Cenozoic geologic era, following the Tertiary, and including the last 2-3 million years

sediment: a mass of organic or inorganic solid fragmented material, or the solid fragment itself, that comes from weathering of a rock and is carried by, suspended in, or dropped by air, water or ice; or a mass that is accumulated by any natural agent that forms in layers on the earth's surface such as sand, gravel, silt, mud, fill or loess. A solid material that is not in solution and either is distributed through the liquid or has settle out of the liquid

stratigraphy: a branch of geology concerned with form, arrangement, geographic distribution, chronological succession, classification, correlation and mutual relationships of rock strata, especially sedimentary

surface water: water found in ponds, lakes, inland seas, streams and rivers

terrace: a horizontal or gently sloping embankment of earth along the contours of a slope to reduce erosion, control runoff or conserve moisture. A long narrow, nearly level surface bounded by a steeper descending slope on one side and by a steeper ascending slope on the other side.

Tertiary: the older major subdivision of the Cenozoic era, extending from the end of the Cretaceous to the beginning of the Quaternary, from 70,000,000 to 2,000,000 years ago

thin section: made by grinding down a slice of rock which has been glued to a glass slide until it reaches a thickness of about 0.03mm (30 microns).  At this thickness most minerals become more or less transparent and can therefore be studied by a microscope using transmitted light (http://www.gly.bris.ac.uk/www/teach/opmin/mins.html)

unconformity: the relation between adjacent rock strata whose time of deposition was separated by a period of non-deposition or erosion; a break in the stratigraphic sequence



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