Catawba River in the context of "Wateree River"

The American bison (Bison bison; pl.: bison), commonly known as the American buffalo, or simply buffalo (not to be confused with true buffalo), is a species of bison that is endemic (or native) to North America. It is one of two extant species of bison, along with the European bison. Its historical range circa 9000 BC is referred to as the great bison belt, a tract of rich grassland spanning from Alaska south to the Gulf of Mexico, and east to the Atlantic Seaboard (nearly to the Atlantic tidewater in some areas), as far north as New York, south to Georgia, and according to some sources, further south to northern Florida, with sightings in North Carolina near Buffalo Ford on the Catawba River as late as 1750.

Two subspecies or ecotypes have been described: the plains bison (B. b. bison), smaller and with a more rounded hump; and the wood bison (B. b. athabascae), the larger of the two and having a taller, square hump. Furthermore, the plains bison has been suggested to consist of a northern plains (B. b. montanae) and a southern plains (B. b. bison) subspecies, bringing the total to three. However, this is generally not supported. The wood bison is one of the largest wild species of extant bovid in the world, surpassed only by the Asian gaur. Among extant land animals in North America, the bison is the heaviest and the longest, and the second tallest after the moose.

The Ridge-and-Valley Appalachians, also called the Ridge and Valley Province or the Valley and Ridge Appalachians, are a physiographic province of the larger Appalachian Highlands division. The physiographic province is divided into three sections: the Hudson Valley, the Central, and the Tennessee.

The river valleys were areas of indigenous settlements for thousands of years. In the historic period, the Cherokee people had towns along many of the rivers in western South Carolina and North Carolina, as well as on the western side of the Appalachian Mountains in present-day Tennessee. Similarly, the Catawba people occupied areas along the upper Catawba River in Western North Carolina, to the east of Cherokee County.

The Catawba, also known as Issa, Essa or Iswä but most commonly Iswa (Catawba: Ye Iswąˀ 'people of the river'), are a federally recognized tribe of Native Americans, known as the Catawba Indian Nation. Their current lands are in South Carolina, on the Catawba River, near the city of Rock Hill. Their territory once extended into North Carolina, as well, and they still have legal claim to some parcels of land in that state. They were once considered one of the most powerful Southeastern tribes in the Carolina Piedmont, as well as one of the most powerful tribes in the South as a whole, with other, smaller tribes merging into the Catawba as their post-contact numbers dwindled due to the effects of colonization on the region.

The Catawba were among the East Coast tribes who made selective alliances with some of the early European colonists, when these colonists agreed to help them in their ongoing conflicts with other tribes. These were primarily the tribes of different language families: the Iroquois, who ranged south from the Great Lakes area and New York; the Algonquian Shawnee and Lenape (Delaware); and the Iroquoian Cherokee, who fought for control over the large Ohio Valley (including what is in present-day West Virginia). During the American Revolutionary War the Catawba supported the American colonists against the British. Decimated by colonial smallpox epidemics, warfare and cultural disruption, the Catawba declined markedly in number in the late eighteenth and nineteenth centuries. Some Catawba continued to live in their homelands in South Carolina, while others joined the Choctaw or Cherokee, at least temporarily.

Catawba Falls is a series of waterfalls on the headwaters of the Catawba River, in McDowell County, near Old Fort, North Carolina.

Lake James is a large reservoir in the mountains of Western North Carolina which straddles the border between Burke and McDowell Counties. It is named for tobacco tycoon and benefactor of Duke University James Buchanan Duke. The lake, with surface elevation of 1200 ft (366 m), lies behind a series of 3 earthen dams. It was created by Duke Power between 1916 and 1923 as a hydro-electric project. It still generates power today and is the uppermost lake on the Catawba River system.

The Linville River is a river in western North Carolina, United States. The river begins in the slopes of Peak Mountain, Sugar Mountain and Flattop Mountain, in the Linville Gap area (also known as Tynecastle). As it goes south through Avery County, it passes through the communities of Grandfather, Linville, Pineola, Crossnore and finally at Linville Falls. After entering Burke County at the community of Linville Falls, the river becomes the centerpiece of the Linville Falls and the Linville Gorge, an area referred to as "the Grand Canyon of North Carolina." After approximately 30 miles (48 km), the river ends at Lake James and the Catawba River; the original confluence with the Catawba River has been flooded by the creation of the reservoir in 1923.

In 1975, North Carolina designated 13.0 miles (20.9 km) of the river as Linville State Natural River, including it in the state's Natural and Scenic Rivers System.

Morganton is a city in and the county seat of Burke County, North Carolina, United States. It is located in the foothills of the Blue Ridge Mountains along the Catawba River.

The population was 17,474 at the 2020 census. Morganton is approximately 75 miles (121 km) northwest of Charlotte and 57 miles (92 km) east of Asheville. It is one of the principal cities in the Hickory-Lenoir-Morganton, NC Metropolitan Statistical Area.

Mountain Island Lake is a lake northwest of Charlotte, North Carolina created in 1924 to coincide with the building of Mountain Island Hydroelectric Station. It is named after the mountain which appears as an island in the lake, and the surrounding area is identified by the lake's name. The shape of the lake follows the meander of the Catawba River's course, dammed near the Mount Holly Wastewater Plant. Full pond elevation is approximately 647.5 feet (197 m). The lake has around 3,281 acres (13 km) of surface area and 61 miles (98 km) of shoreline.