Blue Ridge Mountains Essay

Situated right at the heart of the Chattahoochee Valley, along the banks of the Chattahoochee River, the charming city of Columbus Georgia is home to roughly two-hundred-thousand of the half-million residents of the combined Columbus-Auburn-Opelika metro area. As the second largest city in Georgia (on its own) and a much larger city

Some major rivers in Georgia include the Chattahoochee River, the Savannah River, and the Suwannee River. A few land features around Georgia are the Atlantic coastal plains which stretch from Massachusetts to the Florida Peninsula, then around the Gulf of Mexico, the Piedmont, which has a hilly landscape in the north, but if you travel southeast, the hills begin rolling near 400 feet below sea level, and the Blue Ridge Mountains that “Rise at 2,000 to 5,000 feet above sea level,” according to “The Geography of Georgia.”

The Chattahoochee River is located in Georgia and flows southwesterly towards Alabama. Evidence indicates that humans have been inhabitants of the Chattahoochee River for an extremely long period.

The Great Plains are located between the South and Midwest regions to the east and the Rocky Mountains to the west. The Great Plains Indians were dictated by climate, land,

Next, he adds, “The Georgia low country had such a long and deep agricultural history…” (Stewart xvii). In school, teachers do not go into much detail regarding the agricultural history of coastal Georgia. It is often overlooked, even though it is one of the main reasons that Georgia was settled and a large part of Georgia’s history.

The beauty of Arkansas did not magically appear overnight. In the words of Albert Einstein, “Look deep into nature, and then you will understand everything better”(“Albert Einstein Quotes”). The geography of Arkansas is made of six different areas. The Ozark Mountains, Ouachita Mountains, Arkansas River Valley make up the northwestern half of the great state of Arkansas. The Mississippi Delta, West Gulf Coastal plains, and Crowley's Ridge make up the southeastern half of the state of Arkansas. Three of these areas have been chosen to compare the similarities and differences based on their creation, foliage and climate. The areas chosen are the mystical Ozark Mountains, the stunning Ouachita mountains and the breathtaking Arkansas River Valley areas.

Appalachia is a region extending from Mississippi to New York and includes eleven states within its official

When the Ouachita Mountains were created, the sediment carried by rivers was sent downward and eroded again. Swamps overfilled with clay and plant remains ended up buried. These remains become valuable products of the valley today- coal and natural gas. This region varies between narrow ridges and flat-topped mountains with rolling or hilly plains split by the river. The Arkansas River was an important means of transportation between the mountains. Present day Batesville, Fort Smith, Clarksville, Russellville, Morrilton, and part of Conway are within this

Nestled between the rolling hills of North Georgia is the little town of Ringgold, Georgia. This town, although small in size, has had a significant historical impact in the region. It has also started admirable patriotic traditions emulated by cities surrounding the town. From its role in the Civil War to its modern day impact on local culture and tradition, the town of Ringgold has remained a trailblazer for the local area.

Appalachia Mountains are rich in natural resources, containing an abundant number of coal, timber, oil, gas, and water (Daugneaux 1981). These natural resources have historically influenced the economic characteristics of the region. The region's economy has been highly dependent on mining, forestry, agriculture, chemical industries, and heavy industry, among which coal mining appears to be the largest financial contributor to the economy (Appalachia's Economy). However, the mining practice used to extract coal in Appalachia called

• Georgia is the fastest growing economy in the Caucasus region. Objectives include increasing defense capabilities, improving infrastructure, and establishing energy security.

the leading manufacturing sector of the United States in the years before the Civil War. Georgia's entrepreneurs began to experiment in factory-based industry between 1809 and 1820, but they

Stone mountain has remained a very influential monument of Georgia; a gem of what may say to the state’s tourism and a landmark of American history throughout the ages. Stonewall Jackson, Robert E. Lee , and Jefferson Davis on top of their valuable steeds represent the Confederate nation and its tie with Stone mountain as they are carved meticulously in the world’s largest exposed granite; however, the peaceful serenity of the lake and nature that envelops the mountain and its visitors remained a very important ceremonial location for native americans. The complete history of Stone Mountain is interwoven into the treads of historical events that have occurred throughout and even before the great nation , United States of America, was formed. Currently, it’s one of the most famous attractions in Georgia known for the breathtaking view of metropolitan Atlanta at the peak of the mountain. It is clear as rich as the beauty of stone mountain is,undeniably, it has a strong historical importance to American history and exquisite backround.

Bibb County, in central Georgia, was formed December 9, 1822. Geologically, Bibb County is located on the fall line where the southern Piedmont meets the Coastal Plain. Before the arrival of European settlers, the area had been a center of a series of Native American civilizations. The county sits on 249.76 square miles of land and there are approximately 622 people per square mile.

The Piedmont is located between the Coastal Plain and the Mountain regions, in the middle region of the state. The origins of Piedmont are French, meaning “foot of the mountain”, because it’s located at the base of the Appalachians Mountains. From the western Coastal Plane to the mountains, the elevations range from about 300 feet to near 1,500 feet (Seaman 2006). The fall line, or fault zone, lies between the Coastal Plain and the Piedmont. The rivers that flow along the fault line are formed from shoals, low waterfalls and rapids. As the rivers flow from the Piedmont to the coastal Plain the rocks become younger and softer. The streams below the fall line are usually lethargic and smooth-flowing. The streams above the fall line are gravelly and shallow, making boating difficult. As for the land, the Piedmont is called a plateau because it is high and mostly flat. Most geologist separate the Piedmont into two different areas because the rock suites are so different. The eastern part, known as the Carolina Slate Belt and then the western part, known as the Inner piedmont. My main area of focus will be the Carolina Slate Belt, with attention to the ancient