A is a area of flat land. Plains are one of the major , or types of land, on Earth. They cover more than one-third of the world’s land area. Plains exist on every .
Many plains, such as the that stretch across much of central North America, are . A grassland is a where grass is the main type of .
In North America, —those in places with warm summers and cold winters—are often called . In areas with little rain and , short grasses grow. In areas that receive more rain and snow, tall grasses can grow 1.5 meters (5 feet) high. However, most have been under and are now or .
The Great Plains have supported a wide variety of cultures for thou of years. The so-called “” are actually more than two tribes. Communities include , native to the Canadian of Alberta; , whose center today is in the U.S. state of Wyoming; and , many of whom live today in the Mexican state of Coahuila.
In Asia and eastern Europe, temperate grasslands are called . Steppes usually do not receive enough rain for tall grasses and trees to grow.
Tropical grasslands are called . Savannas exist in places that are warm throughout the year. They often have scattered trees. Savannas such as the stretch across much of central Africa. They are also found in Australia, South America, and southern North America.
Not all plains are grasslands. Some, such as Mexico’s Tabasco Plain, are . Forested plains have different types of trees, shrubs, and other vegetation.
can also be plains. Parts of the Sahara, a great desert in North Africa, are plains.
In the , where the ground is frozen, plains are called . Despite the cold, many plants survive here, including shrubs and .
Plain Formation
Plains form in many different ways. Some plains form as ice and water , or wears away, the dirt and on higher land. Water and ice carry the bits of dirt, rock, and other material, called , down hillsides to be elsewhere. As layer upon layer of this sediment is laid down, plains form.
activity can also form plains. form when pushes up from below ground and flows across the land. The earth in a lava plain is often much darker than the surrounding . The dark earth is a result of the lava, mostly a dark-colored called , broken down into tiny particles over millions of years.
The movement of rivers sometimes forms plains. Many rivers run through . As rivers move from side to side, they gradually erode the valley, creating broad plains.
As a river floods, it overflows its . The flood carries , sand, and other sediment out over the land. After the water withdraws, the sediment remains. If a river floods repeatedly, over time this sediment will build up into a . Flood plains are often rich in and create farmland. The flood plain surrounding Africa’s Nile River has helped Egyptian for thousands of years.
form at the base of . Water carrying sediment flows downhill until it hits flat land. There, it spreads out, depositing the sediment in the shape of a fan. The Huang He River in China has created an alluvial plain that covers about 409,500 square kilometers (158,000 square miles). Because much of the sediment the Huang He carries is yellowish in color, it is also called the Yellow River.
Many rivers deposit their sediment in the ocean. As the sediment builds up, it might eventually rise above , forming a . The Atlantic Coastal Plain stretches along much of the eastern coast of North America. These broad underwater plains slope gently down beneath the water.
are found at the bottom of the ocean. These plains are 5,000 to 7,000 meters (16,400 to 23,000 feet) below sea level, so scientists have a hard time studying them. But scientists say abyssal plains are among the flattest, smoothest places on Earth.
Fast Fact
Plains on Other Planets Plains can be found on other planets. Mercury has large stretches of plains, and scientists have landed several probes on the boulder-covered plains of Mars.
Fast Fact
Thundering Hooves The Great Plains of North America once supported about 50 million bison, which are sometimes called buffalo. The bison roamed in vast herds, feeding on the prairie grasses. They were hunted to near-extinction in the 1800s.
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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
August 22, 2025
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