Physics · Groundwater Hydrology

The imaginary line or surface joining the static water levels in several wells excavated through a confined aquifer is known as the:

Verified Solution4 OptionsUpdated: October 2026👁️1 View

1Perched water table
2Cone of depression
3Hypsometric curve
4Piezometric surface✓

Correct answer

Piezometric surface

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The imaginary line or surface joining the static water levels in several wells excavated through a confined aquifer is known as the:

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The imaginary line or surface joining the static water levels in several wells excavated through a confined aquifer is known as the:

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