/media/static/sites/homepage/assets/resource_carousel/css/flash.css/media/static/sites/homepage/assets/resource_carousel/assets.swftruejavascript:popout(%state%);true2/fake_tokenizer/5678javascript:trackingFcn(%module%, %page%);PREVNEXTPLAY ALLVIEW OPTIONSSHOW INFOHIDE INFOVIEW ALL SLIDESView All SlidesPOP-OUT PLAYERPRESENTATION MODEVIEW AS STAND-ALONE RESOURCESHOWHIDE NAVIGATIONPREVIOUS RESOURCENEXT RESOURCEPLAYPAUSEVOLUMEBACKSLIDES%low%-%high% OF %total%PREVIOUS PHOTONEXT PHOTOVIEW ALL PHOTOSVIEW FULL-SIZED IMAGE[ restricted access ]CANCELDOWNLOADCAPTIONS/SUBTITLESTERMS OF SERVICE]]>https://media.nationalgeographic.org/assets/photos/000/191/19125_r60x45.jpg?1f4d0cdc58dd818f31e272401c6d449cb4b5156ehttps://media.nationalgeographic.org/assets/photos/000/191/19125_r60x45.jpg?1f4d0cdc58dd818f31e272401c6d449cb4b5156ehttps://media.nationalgeographic.org/assets/photos/000/191/19125.jpghttps://media.nationalgeographic.org/assets/photos/000/191/19125.jpgIllustration by Tim Gunther
This illustration shows the two most common types of aquifers, confined aquifers and unconfined aquifers. An unconfined aquifer can receive water directly from the surface, while a confined aquifer is trapped between two layers of rock.
990743https://media.nationalgeographic.org/assets/photos/000/191/19125_r60x45.jpg?1f4d0cdc58dd818f31e272401c6d449cb4b5156ehttps://media.nationalgeographic.org/assets/photos/000/282/28260_r60x45.jpg?1f4d0cdc58dd818f31e272401c6d449cb4b5156ehttps://media.nationalgeographic.org/assets/photos/000/282/28260.jpgPhotograph by Richard Feren, MyShot
Kerid Crater, in Iceland, was formed by a collapsed magma chamber 6,500 years ago. The water level in the crater shows the top of the local water table. The water stored in the rocks beneath Kerid Crater forms an aquifer.
990743https://media.nationalgeographic.org/assets/photos/000/282/28260_r60x45.jpg?1f4d0cdc58dd818f31e272401c6d449cb4b5156ehttps://media.nationalgeographic.org/assets/photos/000/282/28261_c0-216-743-773_r60x45.jpg?476a82bb208fb9dee3029e54d474d5c0cd24d973https://media.nationalgeographic.org/assets/photos/000/282/28261.jpgPhotograph by Franc and Jean Shor
A girl draws water from the village well in Ayios Theodhoros, Greece. Aquifers store water for drinking, hygiene, and industry.