Usòrò:Groundwater flow.svg

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Mmẹkụwátá

Nkówá
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.
Ǹgụ́ụ̀bọ̀chị̀
Mkpọlọ́gwụ̀ Ground Water And Surface Water A Single Resource. U.S. Geological Survey Circular 1139, Figure 3.
Odé ákwụ́kwọ́ T.C. Winter, J.W. Harvey, O.L. Franke, and W.M. Alley
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Nkwényé

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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Nkowapụta

Tinye nkọwa otu ahịrị ihe faịlụ a na-anochi anya ya.
Schematic of an aquifer showing confined zones, groundwater travel times, a spring and a well

Ihe ndị egosiri na faịlụ a

depicts Bekee

aquifer Bekee

Ịta nke usòrò

Bìri èhì/ogè k'ị hụ òtù ụ̀fa dị̀ m̀gbè ahụ̀.

Èhì/OgèMbọ-akaÓgólógó na asaáÒjìèmeNkwute
dị ùgbu â09:10, 9 Mee 2013NvóÁká màkà otù ȯ dị nà 09:10, 9 Mee 2013645 × 400 (86 KB)Mwtoews

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