Loading [MathJax]/extensions/mml2jax.js
Skip to main content
Library homepage
 

Text Color

Text Size

 

Margin Size

 

Font Type

Enable Dyslexic Font
Geosciences LibreTexts

Search

  • Filter Results
  • Location
  • Classification
    • Article type
    • Cover Page
    • License
    • Show TOC
    • Transcluded
    • Author
    • OER program or Publisher
    • Autonumber Section Headings
    • License Version
  • Include attachments
Searching in
About 1 results
  • https://geo.libretexts.org/Courses/Sierra_College/Physical_Geology_(Sierra_College_Edition)/16%3A_Groundwater/16.02%3A_Groundwater_Flow
    But if we drill a well through both the unconfined aquifer and the confining layer and into the confined aquifer, the water will rise above the top of the confined aquifer to the level of its potentio...But if we drill a well through both the unconfined aquifer and the confining layer and into the confined aquifer, the water will rise above the top of the confined aquifer to the level of its potentiometric surface (well B in Figure \(\PageIndex{2}\)). The stream in this scenario is the location with the lowest hydraulic potential, so the groundwater that flows to the lower parts of the aquifer has to flow upward to reach this location.

Support Center

How can we help?