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test 5
exam 5 tbc...
Question | Answer |
---|---|
What is the gradient of a stream that drops 80ft. on elevation over a distance of 3 miles? | ft/miles=80 ft./3 miles=26.667ft./miles |
artesian Spring | water rises to the surface due to pressure where the recharge area is at a higher elevation |
Natural Spring | groundwater flows freely where it intersects the water ta |
Hot springs | groundwater warmed (usually) by magma |
groundwater depletion(wells) | a. the water table around a well is lowered forming a cone of depression b. if pumping rates exceed recharge, the water table may be lowered permanently |
land subsidence | the structure of some aquifers is supported by the water in them. Removing water allows rock and sediment to compress resulting in subsidence of the land surface above |
saltwater intrusion | water in coastal aquifers often flows into the ocean. If pumping rates eliminate this flow, saltwater can flow freely into the aquifer |
caves | are natural underground cavities. Most are formed by the dissolution of limestone |
stalactites | hang from the ceiling |
stalagmites | grow up from the floor |
columns | stalactites and stalagmites that have grown together |
Karst Topography | landscapes shaped by dissolving power of groundwater |
Sinkholes | circular surface depressions |
Disappearing Streams | surface streams that drain under ground |
Geysers | deep groundwater changes to steam, increased pressure causes eruption of groundwater at surface |
Glacier | a moving body of ice that forms from the accumulation and compaction of snow |
alpine(valley)glaciers(mountain glaciers) | confined by surrounding mountains |
Cirque glaciers | create and occupy semicircular basins on mountainsides |
Valley glaciers | develop when a growing cirque glacier flows into preexisting stream valley |
Icecaps | cover the tops of mountains |
Continental ice sheet | an extremely large ice mass that blankets much or all of a continent |
zone of accumulation | where snow accumulates |
zone of wastage | loss of ice and snow |
calving | breaking off of large pieces (origin of icebergs) |
ablation | overall loss of snow and ice at glacier’s lower end |
basal slip | except in polar regions, most glaciers have liquid water at the bottom which they slide along |
glacial plucking | water at the base of the glacier seeps into bedrock fractures, freezes and expands, and breaks of large fragments |
glacial abrasion | rock fragments embedded in the bottom of a glacier scrape, polish and cut striations in the surface of the underlying bedrock |
cirque | depression carved out by a cirque glacier |
Tarn | cirque lake |
Arete | a sharp ridge between two valley glaciers |
Horn | a steep angular peak formed when three or more cirque glaciers erode a mountain |
Glacial Trough | wide, U-shaped valley |
Fracture zone | |
Roche Moutonee | rounded, asymmetrical mountains |
glacial till | poorly sorted sediment deposited directly from glacial ice |
glacial erratic | large, glacially transported rock |
moraine | deposited at the bottom or edges of a glacier. 1. lateral moraine 2. medial moraine 3. end moraine 4. ground moraine |
drumlin | egg shape hill |
stratified drift | Deposits from Glacial Meltwater Streams – well sorted stream deposits |
outwash | sediment deposited downstream of the glacier |
kettle lakes | form when large chunks of ice embedded in outwash |
kame | roundish hill of sediment that filled in an open space in the glacier |
eskers | sinuous ridges deposited by streams flowing in a glacier |
crustal depression and rebound | the weight of a glacier depresses the crust into the asthenosphere. When the glacier melts, the land rebounds |
milankovitch cycles | may have the effect of lowering solar radiation to polar latitudes allowing glaciers to form |
Plastic Flow | glacier’s ice crystals deform and slip past each other under pressure from overlying ice |
Glacial drift | any sediments of glacial origin |
milankovitch cycles process | a. earth’s orbit shifts from nearly circular to more elliptical b. change of the tilt of the earth’s axis c. precession |