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Sinkhole

Sinkhole

A sinkhole is a hole in the ground that forms when water dissolves surface rock

Grades

6 - 12+

Subjects

Chemistry, Earth Science, Geography, Geology, Physical Geography

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Morgan Stanley

A sinkhole is a hole in the ground that forms when water dissolves surface rock. Often, this surface rock is limestone, which is easily eroded, or worn away, by the movement of water.

In a landscape where limestone sits underneath the soil, water from rainfall collects in cracks in the stone. These cracks are called joints. Slowly, as the limestone dissolves and is carried away, the joints widen until the ground above them becomes unstable and collapses. The collapse often happens very suddenly and without very much warning. Water collects in these collapsed sections, forming sinkholes.

Sinkholes also form when the roofs of caves collapse. Sinkholes are often funnel-shaped, with the wide end open at the surface and the narrow end at the bottom of the pool.

Sinkholes vary from shallow holes about 1 meter (3 feet) deep, to pits more than 50 meters (165 feet) deep. Water can drain through a sinkhole into an underground channel or a cave. When mud or debris plugs one of these underground caves, it fills with water to become a lake or a pond.

Sinkholes occur naturally, especially where there is abundant rainfall, and the rock beneath the surface soil is limestone. For instance, a cenote (pronounced "seh-NOH-tay") is a type of sinkhole that forms when the roof of an underground cave collapses, exposing the water to the surface. Cenotes are very common on the Yucatan Peninsula of Mexico. There are more than 2,000 cenotes on the Yucatan, and they are a main source of fresh water for people there. Ancient Mayans believed cenotes were passageways to the underworld.

People can create sinkholes when building roads, aquifers, or other types of construction. Altering land in these ways can weaken the underlying rock and make it more susceptible to sinkholes. Sinkholes can open up in the middle of busy streets or in neighborhoods, especially during heavy rainfall.

The land surrounding the Dead Sea in the Middle East is prone to sinkholes because of the prevalence of rock salt, which is easily dissolved by water. Tourists who are unaware of sinkholes and even scientists studying sinkholes have been injured by falling into them.

Fast Fact

Daisetta Sinkhole
Some parts of the United States are very susceptible to sinkholes. In May 2008, a large sinkhole formed in Daisetta, Texas, a suburb of Houston. The sinkhole formed when an underground mound of rock salt collapsed. The sinkhole swallowed several cars, oil drilling equipment, and oil tanks. In one day, the Daisetta sinkhole had grown to 200 meters (656 feet) in diameter and 75 meters (246 feet) deep. Within a couple weeks a 23-meter (7-foot) deep lake had formed in the sinkhole, and a 2-meter (7-foot) alligator had taken up residence in the waters.

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Writers
Kim Rutledge
Melissa McDaniel
Santani Teng
Hilary Hall
Tara Ramroop
Erin Sprout
Jeff Hunt
Diane Boudreau
Hilary Costa
Illustrators
Mary Crooks, National Geographic Society
Tim Gunther
Editors
Jeannie Evers, Emdash Editing, Emdash Editing
Kara West
Educator Reviewer
Nancy Wynne
Producer
National Geographic Society
other
Last Updated

July 15, 2022

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