Groundwater Flashcards
GROUND WATER ZONES
- Unsaturated zone - water is present
- water table - top of zone of saturation
- zone of saturation - ground water and water pressure great to allow wells
Active Margin features
tectonic activity
earthquake and volcanoes
narrow shelf
steep slopes
passive margin features
no tectonic activity
wide continental shelf
gradual slope
smooth transition to abyssal plain
ROCK FLOUR
ACT AS A FINE GRIT THA TPOLISHES THE SURFACE OF BEDROCK SMOOTH
GLACIAL STRIATIONS
LARGE FRAGMENT SCRAPE OVER SURFACE CREATING ELONGATE GROOVES
ACCUMULATION > ablation
advance (positive feedback)
accumulation < ablation
retreat (negative feedback)
cirque
Bowl-shaped feature – represents where the head of the glacier eroded the mountain by plucking rock away from it
hanging valley
Tributary valley – with a waterfall plunging into the main valley
A small glacier that forms within a cirque basin, generally high on theside of a mountain.
cirque
A crack or series of cracks that open in the surface of a moving glacier inresponse to differential stresses caused by glacier flow. They range in shape from linearto arcuate, in length from feet to miles. Their orientation may be in any direction withrespect to the glacier flow. The deepest crevasses may exceed 100 feet
crevasse
An elongated ridge of glacial sediment sculpted by ice moving over the bed of aglacier. Generally, the down-glacier end is oval or rounded and the up-glacier end tapers.The shape is often compared to an inverted, blunt-ended canoe. Although not commonin Alaska, drumlins cover parts of the Eastern and Midwestern United States
Drumlin
A rock of unspecified shape and size, transported a significant distance from itsorigin by a glacier or iceberg and deposited by melting of the ice. Erratics range frompebble-size to larger than a house and usually are of a different composition that thebedrock or sediment on which they are deposited
erratic
A meandering, water-deposited, generally steep-sided sediment ridge that formswithin a subglacial or englacial stream channel. Its floor can be bedrock, sediment, orice. Subsequent melting of the glacier exposes the deposit. Generally composed ofstratified sand and gravel, eskers can range from feet to miles in length and may exceed100 feet in height
Esker
Reducing emissions from electric power
Substituting less carbon-intensive fuels
Renewable energy
Increased end-use energy efficiency
Nuclear energy
Carbon capture and requestion