---
source: https://iinventedlight.com/library/notes/artesian-wells.md
title: "Artesian wells: groundwater that rises on its own"
license: CC-BY-4.0
license_url: https://creativecommons.org/licenses/by/4.0/
source_license: "US government work, public domain; restated in our own words"
attribution: "Summary by iinventedlight (AI-assisted). Sources: USGS, Artesian Water and Artesian Wells, US government work, public domain; USGS, Aquifers and Groundwater, US government work, public domain."
author: "iinventedlight (synthesis of cited sources); text drafted with AI assistance"
date: 2026-11-04
status: published
checked_on: 2026-11-04
as_of: 2026-11-04
confidence: medium
untested: "No observation or experiment was done; only the fetched government pages were read."
category: coverage-gaps
topic_area: "earth science: groundwater"
tags: ['usgs', 'groundwater', 'aquifers', 'wells']
sources:
  - id: S1
    title: "Artesian Water and Artesian Wells"
    publisher: USGS
    url: https://www.usgs.gov/special-topics/water-science-school/science/artesian-water-and-artesian-wells
    accessed: 2026-11-04
    license: "US government work, public domain"
  - id: S2
    title: "Aquifers and Groundwater"
    publisher: USGS
    url: https://www.usgs.gov/special-topics/water-science-school/science/aquifers-and-groundwater
    accessed: 2026-11-04
    license: "US government work, public domain"
---
# Artesian wells: groundwater that rises on its own

**Answer:** Artesian water is really not different from other groundwater, except that it flows to the land surface because pressure in the rocks underground forces it to the surface. An artesian well is drilled into a confined aquifer, and a flowing artesian well delivers water to the land surface naturally.

## Confined vs. unconfined aquifers

- The upper layer of an aquifer system is generally the unconfined aquifer, which does not have a confining layer of solid material above it.
- The water table is the height to which water rises in a well in an unconfined aquifer.
- In some locations there can exist confined aquifers below the unconfined aquifers. They have layers of solid material above and below them and are thus under pressure from the rock weight.
- An impermeable, confining layer separates the confined and unconfined aquifer.

## How confined aquifers recharge

For water to recharge a confined aquifer, it must seep down from the surface at a distance away and travel somewhat horizontally into the aquifer.

## The capillary fringe

Above the water table lies the capillary fringe, where all the spaces and voids are full of water held up by surface tension with the rocks and mineral grains.

## Is "artesian" water special?

USGS asks whether bottled "artesian-well drinking water" is different from other water. Its answer is that artesian water is really not different from other groundwater; having water flow to the surface naturally is just a handy way to tap groundwater resources.

## Claims
- id: C1
  claim: Artesian wells can flow to the surface because of underground pressure.
  source: S1
  evidence: "Artesian wells can be sometimes flow to the land surface naturally because of underground pressure."
- id: C2
  claim: Confined aquifers can exist below unconfined aquifers.
  source: S1
  evidence: "In some locations there can exist confined aquifers below the unconfined aquifers."
- id: C3
  claim: Artesian wells are drilled into a confined aquifer.
  source: S2
  evidence: "which are drilled into a confined aquifer"

## Sources
- [S1] Artesian Water and Artesian Wells. USGS. https://www.usgs.gov/special-topics/water-science-school/science/artesian-water-and-artesian-wells . License: US government work, public domain. Accessed 2026-11-04.
- [S2] Aquifers and Groundwater. USGS. https://www.usgs.gov/special-topics/water-science-school/science/aquifers-and-groundwater . License: US government work, public domain. Accessed 2026-11-04.

License: this note is CC BY 4.0 (https://creativecommons.org/licenses/by/4.0/). Summary by iinventedlight (AI-assisted).