Pine Mountain Range

Last updated
Pine Mountain Range
Pine Mountain
PineMtnRange.jpg
Looking at the Pine Mountain Range, northwest of Hamilton.
Highest point
Peak Dowdell's Knob
Elevation 1,395 ft (425 m)
Dimensions
Length50 mi (80 km)
Geography
CountryUnited States
Region Southern Rivers to Piedmont area of Georgia

The Pine Mountain Range is a long ridge in Meriwether County, Georgia, Harris County, Georgia, and Talbot County, Georgia. The highest altitudes in all three of these west Georgia counties can be found along the range. [1]

The Pine Mountain Range is part of a larger geological feature known as the Pine Mountain terrane, [2] which extends into eastern Alabama. The ridge in Georgia exceeds 1,100 feet (340 m) in elevation for a distance of about 20 miles (32 km). These are the highest elevations at so southerly a latitude in the eastern half of the continental United States. (The entire Pine Mountain terrane is geologically distinct from the Appalachian Range, which terminates farther north in Georgia and Alabama and has its own Pine Mountain in Kentucky and Tennessee.)

The Pine Mountain Range begins around Lake Harding, and runs northeast through Harris County. U.S. Route 27, as well as Georgia State Routes 190 and 354, cross the ridge south and east of the city of Pine Mountain. The ridge then parallels the Harris-Meriwether County line, where the highest point on the range, 1,395-foot (425 m) Dowdell's Knob, is found. President Franklin D. Roosevelt had a brick oven and picnic area constructed at this location for use during his many stays at his house in nearby Warm Springs. It then parallels the Talbot-Meriwether County line south of Manchester. At the extreme eastern end of the Pine Mountain Ridge, it is cut by the Flint River, forming the steep bluffs of Sprewell Bluff Park in Upson County.

F.D. Roosevelt State Park, the largest state park in Georgia, is found along the ridge in northern Harris County.

32°50′15″N84°48′56″W / 32.83750°N 84.81556°W / 32.83750; -84.81556

Related Research Articles

<span class="mw-page-title-main">Appalachian Mountains</span> Mountain range in eastern North America

The Appalachian Mountains, often called the Appalachians, are a mountain range in eastern to northeastern North America. Here, the term "Appalachian" refers to several different regions associated with the mountain range, and its surrounding terrain. The general definition used is one followed by the United States Geological Survey and the Geological Survey of Canada to describe the respective countries' physiographic regions. The US uses the term Appalachian Highlands and Canada uses the term Appalachian Uplands..

<span class="mw-page-title-main">Talbot County, Georgia</span> County in Georgia, United States

Talbot County is a county located in the west central portion of the U.S. state of Georgia. The 2020 census showed a population of 5,733. The county seat and largest city is Talbotton.

<span class="mw-page-title-main">Harris County, Georgia</span> County in Georgia, United States

Harris County is a county located in the west-central portion of the U.S. state of Georgia; its western border with the state of Alabama is formed by the Chattahoochee River. As of the 2020 census, the population was 34,668. The county seat is Hamilton. The largest city in the county is Pine Mountain, a resort town that is home to the Franklin D. Roosevelt State Park. Harris County was created on December 14, 1827, and named for Charles Harris, a Georgia judge and attorney.

<span class="mw-page-title-main">Pine Mountain, Harris County, Georgia</span> Town in Georgia, United States

Pine Mountain is a town in Harris and Meriwether counties in the U.S. state of Georgia. As of the 2020 census it had a population of 1,216.

<span class="mw-page-title-main">Manchester, Georgia</span> City in Georgia, United States

Manchester is a town in Meriwether and Talbot counties in the U.S. state of Georgia, although primarily in Meriwether. The population was 3,584 at the 2020 census, down from 4,230 in 2010. It is the most populous community in Meriwether County. CSX Transportation runs a railroad yard in Manchester.

<span class="mw-page-title-main">Warm Springs, Georgia</span> City in the United States

Warm Springs is a city in Meriwether County, Georgia, United States. The population was 465 at the 2020 census.

<span class="mw-page-title-main">Ouachita Mountains</span> Mountain range in Arkansas and Oklahoma, United States

The Ouachita Mountains, simply referred to as the Ouachitas, are a mountain range in western Arkansas and southeastern Oklahoma. They are formed by a thick succession of highly deformed Paleozoic strata constituting the Ouachita Fold and Thrust Belt, one of the important orogenic belts of North America. The Ouachitas continue in the subsurface to the northeast, where they make a poorly understood connection with the Appalachians and to the southwest, where they join with the Marathon uplift area of West Texas. Together with the Ozark Plateaus, the Ouachitas form the U.S. Interior Highlands. The highest natural point is Mount Magazine at 2,753 feet (839 m).

<span class="mw-page-title-main">Blue Ridge Mountains</span> Mountain range in the Eastern U.S.

The Blue Ridge Mountains are a physiographic province of the larger Appalachian Highlands range. The mountain range is located in the Eastern United States, and extends 550 miles southwest from southern Pennsylvania through Maryland, West Virginia, Virginia, North Carolina, South Carolina, Tennessee, and Georgia. This province consists of northern and southern physiographic regions, which divide near the Roanoke River gap. To the west of the Blue Ridge, between it and the bulk of the Appalachians, lies the Great Appalachian Valley, bordered on the west by the Ridge and Valley province of the Appalachian range.

<span class="mw-page-title-main">Wind River Range</span> Mountain subrange of the Rocky Mountains in Wyoming, United States

The Wind River Range is a mountain range of the Rocky Mountains in western Wyoming in the United States. The range runs roughly NW–SE for approximately 100 mi (160 km). The Continental Divide follows the crest of the range and includes Gannett Peak, which at 13,802 ft (4,207 m), is the highest peak in Wyoming; and also Fremont Peak at 13,750 ft (4,191 m), the third highest peak in Wyoming. There are more than 40 other named peaks in excess of 12,999 ft (3,962 m). With the exception of the Grand Teton in the Teton Range, the next 19 highest peaks in Wyoming after Gannett are also in the Winds.

<span class="mw-page-title-main">Transverse Ranges</span> Group of mountain ranges of southern California

The Transverse Ranges are a group of mountain ranges of southern California, in the Pacific Coast Ranges physiographic region in North America. The Transverse Ranges begin at the southern end of the California Coast Ranges and lie within Santa Barbara, Ventura, Los Angeles, San Bernardino, Riverside and Kern counties. The Peninsular Ranges lie to the south. The name Transverse Ranges is due to their east–west orientation, making them transverse to the general northwest–southeast orientation of most of California's coastal mountains.

<span class="mw-page-title-main">Cumberland Plateau</span> Plateau in the United States

The Cumberland Plateau is the southern part of the Appalachian Plateau in the Appalachian Mountains of the United States. It includes much of eastern Kentucky and Tennessee, and portions of northern Alabama and northwest Georgia. The terms "Allegheny Plateau" and the "Cumberland Plateau" both refer to the dissected plateau lands lying west of the main Appalachian Mountains. The terms stem from historical usage rather than geological difference, so there is no strict dividing line between the two. Two major rivers share the names of the plateaus, with the Allegheny River rising in the Allegheny Plateau and the Cumberland River rising in the Cumberland Plateau in Harlan County, Kentucky.

<span class="mw-page-title-main">Cumberland Mountains</span> Mountain range in the southeastern United States

The Cumberland Mountains are a mountain range in the southeastern section of the Appalachian Mountains. They are located in western Virginia, southwestern West Virginia, the eastern edges of Kentucky, and eastern middle Tennessee, including the Crab Orchard Mountains. Their highest peak, with an elevation of 4,223 feet (1,287 m) above mean sea level, is High Knob, which is located near Norton, Virginia.

<span class="mw-page-title-main">F. D. Roosevelt State Park</span> United States historic place

F.D. Roosevelt State Park is a 9,049 acres (36.62 km2) Georgia state park located near Pine Mountain and Warm Springs. The park is named for former U.S. President Franklin Delano Roosevelt, who sought a treatment for his paralytic illness in nearby Warm Springs at the Little White House. The park is located along the Pine Mountain Range. The western portion of the park, formerly named Pine Mountain State Park, was named a National Historic Landmark in 1997. F.D. Roosevelt State Park is Georgia's largest state park.

<span class="mw-page-title-main">Taconic orogeny</span> Mountain-building period that affected most of New England

The Taconic orogeny was a mountain building period that ended 440 million years ago and affected most of modern-day New England. A great mountain chain formed from eastern Canada down through what is now the Piedmont of the East coast of the United States. As the mountain chain eroded in the Silurian and Devonian periods, sediments from the mountain chain spread throughout the present-day Appalachians and midcontinental North America.

Pine Mountain, Georgia may refer to any of the following locations in the United States:

<span class="mw-page-title-main">Geology of Georgia (U.S. state)</span> Overview of the geology of the U.S. state of Georgia

The U.S. state of Georgia is commonly divided into four geologic regions that influence the location of the state's four traditional physiographic regions. The four geologic regions include the Appalachian foreland, Blue Ridge, Piedmont, and Coastal Plain. These four geologic regions commonly share names with and typically overlap the four physiographic regions of the state: the Appalachian Plateau and adjacent Valley and Ridge; the Blue Ridge; the Piedmont and the Coastal Plain.

The U.S. state of Tennessee is geographically diverse, with varying terrains and several distinct physiographic regions. Its landforms range from the Blue Ridge Mountains in the eastern part of the state to flat and fertile plains along the Mississippi River. The state is geographically, legally, culturally, and economically divided into three Grand Divisions: East Tennessee, Middle Tennessee, and West Tennessee.

<span class="mw-page-title-main">Georgia State Route 190</span> State highway in Georgia, United States

State Route 190 (SR 190) is a 16.7-mile-long (26.9 km) state highway that runs west–east mostly through F. D. Roosevelt State Park and Roosevelt's Little White House Historic Site. It is known as Scenic Heights Road and Pine Mountain Highway. It connects the Pine Mountain area and Manchester. It parallels the Pine Mountain Range for much of its length.

<span class="mw-page-title-main">Geology of North America</span> Overview of the geology of North America

The geology of North America is a subject of regional geology and covers the North American continent, the third-largest in the world. Geologic units and processes are investigated on a large scale to reach a synthesized picture of the geological development of the continent.

Coleoatchee Creek is a creek in Talbot County, Georgia. It rises at the base of Pine Mountain Range near the Meriwether County/Talbot County border. The creek has a very strong source, which continues to flow strongly in the severest droughts. The creek generally flows south through prime agricultural land to its junction with Big Lazer Creek south of Georgia Highway 36.

References

  1. WIlliamson, Kevin (2009-02-13). "Georgia Main Page".
  2. Hooper, Robert J.; Hatcher, Robert D. Jr. (1988-04-01). "Pine Mountain terrane, a complex window in the Georgia and Alabama Piedmont; evidence from the eastern termination". Geology. 16 (4): 307–310. Bibcode:1988Geo....16..307H. doi:10.1130/0091-7613(1988)016<0307:PMTACW>2.3.CO;2. ISSN   0091-7613.