Johnson City

Tennessee, United States
Also known as: Haynesville, Johnson’s Depot

Johnson City, city, Washington county, northeastern Tennessee, U.S. It lies in a valley in the southern Appalachian Mountains, about 100 miles (160 km) northeast of Knoxville and just west of Elizabethton. The area was settled in the 1760s. Originally a part of North Carolina, it was included in the Watauga Association, a form of self-government organized in 1772, and a few years later it was part of the short-lived state of Franklin. Following the arrival of the East Tennessee and Virginia Railroad in the mid-1850s, the settlement grew up around the railroad depot and was called Johnson’s Depot for Henry Johnson, an early settler and postmaster and later the city’s first mayor. In 1859 it was renamed Haynesville for Landon C. Haynes, later a Confederate senator, but was renamed for Johnson in 1861.

The economy is based on agriculture (livestock, corn [maize], and tobacco), services (including health care, finance, and telemarketing), and manufacturing (including water heaters, electronics, heating equipment, and automotive parts). The James H. Quillen Veterans Affairs Medical Center (known as Mountain Home) includes a lake and a cemetery. East Tennessee State University (1911) is in the city. The northern portion of Cherokee National Forest is to the south and west. Near the city are Rocky Mount, a restored 18th-century territorial capital, and the Tipton-Haynes Historic Site, an 18th-century home that includes a museum and a cave. The Appalachian Regional Fair is held in August in nearby Gray. Inc. 1869. Pop. (2000) 55,469; Johnson City Metro Area, 181,607; (2010) 63,152; Johnson City Metro Area, 198,716.

This article was most recently revised and updated by Kenneth Pletcher.
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Also called:
Appalachians

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Appalachian Mountains, great highland system of North America, the eastern counterpart of the Rocky Mountains. Extending for almost 2,000 miles (3,200 km) from the Canadian province of Newfoundland and Labrador to central Alabama in the United States, the Appalachian Mountains form a natural barrier between the eastern Coastal Plain and the vast Interior Lowlands of North America. As a result, they have played a vital role in the settlement and development of the entire continent. They combine a heritage of natural beauty and a distinctive regional culture with contemporary problems of economic deprivation and environmental deterioration.

Physical features

Physiography

The system may be divided into three large physiographic regions: northern, central, and southern Appalachia. These include such mountains as, in the northern area, the Shickshocks (French: Chic-Chocs) and the Notre Dame ranges in Quebec; the Long Range on the island of Newfoundland; the great monadnock (isolated hill of bedrock) of Mount Katahdin in Maine; the White Mountains of New Hampshire; and Vermont’s Green Mountains, which become the Berkshire Hills in Massachusetts, Connecticut, and eastern New York. New York’s Catskill Mountains are in central Appalachia, as are the beginnings of the Blue Ridge range in southern Pennsylvania and the Allegheny Mountains, which rise in southwestern New York and cover parts of western Pennsylvania, western Maryland, and eastern Ohio before merging into the third, or southern, region. This area includes the Alleghenies of West Virginia and Virginia; the Blue Ridge range, extending across Virginia and western North Carolina, the northwestern tip of South Carolina, and the northeastern corner of Georgia; the Unaka Mountains in southwestern Virginia, eastern Tennessee, and western North Carolina (of which the Great Smoky Mountains are a part); and the Cumberland Mountains of eastern Kentucky, southwestern West Virginia, southwestern Virginia, eastern Tennessee, and northern Alabama.

The highest elevations in the Appalachians are in the northern division, with Maine’s Mount Katahdin (5,268 feet [1,606 metres]), New Hampshire’s Mount Washington (6,288 feet), and other pinnacles in the White Mountains rising above 5,000 feet (1,525 metres), and in the southern region, where peaks of the North Carolina Black Mountains and the Tennessee–North Carolina Great Smoky Mountains rise above 6,000 feet (1,825 metres) and the entire system reaches its highest summit, on Mount Mitchell (6,684 feet [2,037 metres]).

A distinctive feature of the system is the Great Appalachian Valley. It includes the St. Lawrence River valley in Canada and the Kittatinny, Cumberland, Shenandoah, and Tennessee valleys in the United States; the latter is the site of the world-famous Tennessee Valley Authority (TVA), a government agency for natural resource conservation, power production, and regional development.

In the area known geologically as “New” Appalachia, especially where there are softer limestone rocks that yield to the constant solution by water and weak acids, numerous caves are a distinctive feature of the physiography. The chief caverns lie within or border the Great Valley region of Pennsylvania, Maryland, West Virginia, Virginia, and Tennessee. Caverns of the Shenandoah Valley in Virginia provide well-known and dramatic examples of underground passages, rooms, watercourses, formations, and other cave features that honeycomb much of the land below central and southern Appalachia.

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