The Appalachian Mountain Range

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Moonshine, hillbillies and a one of kind dialect is what comes to mind when most people think of the Appalachian Mountains and the Appalachia people in the eastern United States. Long identified by the population and commerce found in the area, the Appalachians are also an interesting geologic feature. Running from north to south, the Appalachian Mountain Range is one of the oldest ranges on planet Earth. Beginning to form nearly a billion years ago, the Appalachian Range extends from Alabama to Newfoundland. This paper will discuss the formation of the range in the Paleozoic Era. The different geologic features and patterns found in the northern and southern areas of the range. Finally, the Appalachia people, unique ecosystem and valuable resources found in the region. The Appalachian Mountains provide a unique place to study geological features and process.
The Appalachian Mountain chain is one of the oldest mountain ranges on the Earth. The Appalachians were formed over a series of mountain building events that took place during the Paleozoic Era. The first even was the formation of the Grenville Mountains during the formation of the supercontinent Rodinia (Jamestown). The Grenville Mountains were heavily eroded and became the base of the early Appalachians. Around 450 million years ago, uplift and folding created the Taconic Mountain range which would later become the Northern Appalachian Mountains. Ongoing collisions continued to create mountains to the north in present day Canada and to the south, the southern Appalachian Mountains and to the southwest, the Ozark Plateau and mountain range. The final mountain building event occurred 300 million years ago during the collision of plates forming the supercontinent Pangaea....

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