There are actually six geographic sub-regions, three in both the uplands and the lowlands.

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Transcription:

6 Regions of AR

Although Arkansas is most easily divided into two distinct geographical regions, the northwestern uplands and the southeastern lowlands, this description does not accurately portray the state's geographical complexity. There are actually six geographic sub-regions, three in both the uplands and the lowlands. The northwestern uplands are made up of three distinctive sub-regions: The Ozark Mountains, the Arkansas River Valley, and the Ouachita Mountains. The southeastern lowlands are comprised of the Gulf Coastal Plain (The Timberlands), the Mississippi Alluvial Plain (the Delta), and Crowley's Ridge

The Ozark Region The Ozark Region of Arkansas is located in the extreme northern and western portions of the state. This area is marked by flat-topped mountains, or plateaus, which have been eroded over millions of years.

The Ozark surface features were created as water eroded the plateau. This process took millions of years and shaped the Ozarks into its present rugged shape. Caves, such as Blanchard Springs Caverns, were formed by streams flowing through cracks in the limestone. These streams carved mountains out of the plateau. They made bluffs, waterfalls, and natural dams. Rivers have carved deep valleys into the high, flat plateaus here. These mountains are more than two thousand feet higher than the lowlands of the southeastern half of the state.

The Arkansas River Valley The Arkansas River Valley is the area carved by the river long ago. This 40mile wide trough divides the Ozark and Ouachita Mountains. Most of Arkansas's larger cities can be found in the river valley - Fort Smith, Little Rock, and several others.

A series of valleys between the Ozark and Ouachita mountains through which the Arkansas River flows.

Ouachita Mountains The Ouachita Mountains lie south of the river valley. These mountains run east to west and are largely covered in pine trees. The soil here is even worse than that of the Ozarks. There are many unusual features here including Hot Springs and the diamond crater at Murfreesboro.

The Ouachitas are located in the western part of the state. Long, narrow ridges that run from east to west characterize this region. Within its boundaries lie the communities of Hot Springs, and part of Little Rock and Mena. Sandy soil allows pine trees to grow on the south slopes of the Ouachita and hardwoods grow on the north faces.

Delta/Mississippi Alluvial Plain The Delta, or Mississippi Alluvial Plain, covers the eastern portion of Arkansas. Here the Mississippi and numerous other rivers have deposited rich soils over millions of years. This area has swamps, prairies, and rich farmland where the soil is very deep. Today this region is the primary agricultural part of Arkansas.

When the Gulf of Mexico receded from the Delta millions of years ago, its geological deposits were removed by rivers and replaced by deep layers of sand, silt and clay. Flat bottomlands characterize the area and today, it is a major agricultural region. Powerful rivers, the Arkansas, White and Mississippi, flow through the area and often cause floods.

The Gulf Coastal Plain The southern part of Arkansas is part of the Gulf Coastal Plain. This area was once covered by the Gulf of Mexico and emerged from the sea 50 million to 100 million years ago. Today there is much agriculture and timber in this area, as well as oil and natural gas deposits.

The lowland region has some hills, but most of the area is flat. Rivers and lakes are found in the region. The Arkansas oil industry is headquartered here. Sandy, rolling hills harbor pine trees and hardwood bottoms are found along rivers. Wildlife such as deer, beaver and wading birds are abundant.

Crowley s Ridge Crowley's Ridge divides the eastern part of Arkansas. The ridge is composed of loess (windblown soil) and runs for 150 miles north from Helena. It varies in height from 250 to 500 feet above sea level. Crowley's ridge was originally an island between the Mississippi and Ohio rivers. When these rivers shifted their courses millions of years ago, Crowley's ridge was left behind as a long, low hilly formation. Most of the major cities of the Arkansas Delta can be found on or near Crowley's Ridge.