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Nam-a̱lyiat

Wa̱i a̱lyiat
English: Ground-water flow paths vary greatly in length, depth, and traveltime from points of recharge to points of discharge in the groundwater system.
العربية: تدفق المياه السطحية ضمن المسارات يختلف بشكل كبير من حيث الطول و العمق و زمن المسير من نقطة الدخول لإالى نقطة الخروج في نظام المياه السطحية.
A̱tuk
A̱tyin Ground Water And Surface Water A Single Resource. U.S. Geological Survey Circular 1139, Figure 3.
A̱tyulyuut T.C. Winter, J.W. Harvey, O.L. Franke, and W.M. Alley
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Public domain
This image is in the public domain in the United States because it only contains materials that originally came from the United States Geological Survey, an agency of the United States Department of the Interior. For more information, see the official USGS copyright policy.

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Schematic of an aquifer showing confined zones, groundwater travel times, a spring and a well

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A̱swom (a̱sa̱khwot)

kpaat

1998

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