Geology of Groundwater Occurence Flashcards

1
Q

All surface-water features (streams, lakes, reservoirs, wetlands, and estuaries) interact with ___________

A

ground water

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2
Q

Hydrogeologist is concerned with the distribution of earth material as
they affect_______________ of the earth.

A

porosity and hydraulic conductivity

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3
Q
  • is a gently sloping plain consisting of alluvium.
  • It is normally delimited by uplands on either side that rise above the
    level of the valley to varying heights.
A

Alluvial Valleys

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4
Q

During mountain-building episodes, the uplift of mountain masses will result in _________ being formed.

A

intermontane basins

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5
Q

__________can also be created by down-dropping of large
crustal pieces along faults.

A

Fault-block valleys

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6
Q

Coarse gravel is deposited in the___________, sand and fine gravel form ______ along banks, and silt and clay come to rest on the floodplain.

A

stream channel; natural levees

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7
Q

Clastic sedimentary rocks are typically composed of_____
Chemically precipitated sedimentary rocks are primarily ______
Coal and lignite can also be considered to be sedimentary deposits, with the original sediments being _______

A
  • silicate, carbonate, or clay minerals.
  • limestone, dolomite, salt, or gypsum
  • organic matter
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8
Q

_____________of sedimentary rocks can create very complex hydrogeologic systems, in which determination of the locations of
recharge and discharge zones and flow systems is confounded.

A

Folding and faulting

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9
Q

intrusions of sediment that are forced into rock fractures

A

Clastic Dikes

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10
Q

Faults in consolidated rock units can act either as pathways for water movement or as
flow barriers. If there has been little displacement along the fault, then the fault is more likely to develop fracture permeability because there is less opportunity for the formation of soft, ground-up rock, called ____________ to form between the moving surfaces

A

gouge,

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11
Q

Hydraulic conductivity of clastic sedimentary rocks, based on , is a ___________________
function Of the ________________ of the original sediment. The same factors

A

primary permeability; grain Size, Shape, and Sorting

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12
Q

Clastic limestones have high ____

A

primary porosity

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13
Q

Chemically precipitated rocks pan be very low porosity and permeability if the they are ___________

A

crystalline

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14
Q

Bedding plane can be zone of low primary porosity and permeability (T o F)

A

F

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15
Q

__________, or shafts leading from surface streams, can carry surface water under-
ground into caverns. Swallow holes can drain an entire stream or only a small portion of one,

A

Swallow holes

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16
Q

Caves above water table

A

Vadose Cave

17
Q

Caves Below water table

A

Phreatic Cave

18
Q

Caves at the water table

A

water-table cave

19
Q

3 conceptual models for carbonate aquifers

A

Diffuse-Flow
Free-flow
Confined-Flow

20
Q

have had little solutional activity directed toward opening
large channels; these are to some extent homogeneous.

A

diffuse flow

21
Q

controlled by the orientation of the beding planes and fractures that determine the locations of solutional conduits, but not by
confining beds.

A

Free-flow

22
Q

have solution openings in the carbonate units, but low-permeability noncarbonate beds exert control over the direction of
-water movement.

A

Confined-Flow

23
Q

Hindrance to Ground water exploration

A

Complex Stratigraphy

24
Q

Desert areas receive ______of precipitation or less each year-

A

25 cm

25
Q

Vast bedrock aquifers are known to occur in the sedimentary basins
of Egypt, Jordan, and Saudi Arabia (Harshbarger 1968). The Sahara
Desert is underlain by the_________, a sandstone up to 3000 ft
(900 m) thick.

A

Nubian aquifer

26
Q

They are regional features, bounded on the continental side by
highlands and seaward by a coastline.

A

Coastal Plain Aquifers

27
Q

Aquifers located next to tidal bodies are subjected to short-term
fluctuations in the head, due to the tide.

A

Tidal Effect

28
Q
A