Valley Region of the Appalachian Mountains Essay example

Found in the Appalachian Region, the Juniata Formation extends from central-southern Pennsylvania to Tennessee (Davies 2010). Though the thickness of the Juniata Formation is far from constant across its lateral extent, it is approximately 2000 feet thick in northern Pennsylvannia and thins towards the southwest (Crowder 1980). Named for the Juniata River running through southern Pennsylvania, this formation consists of sediments from the Taconic Orogeny in the late Ordovician period (Crowder 1980). Figure one displays the characteristic layers of alternating red sandstones and shales, which are divided into three distinct units (Darton

Hess, D. (2011). Mcknight's Physical Geography; A Landscapes Appreciation. (10th ed.). Upper Saddle River, NJ: Pearson Education, Inc

When a person is in a stressful situation on instinct they have two options, fight or flight. In war the same is true. War is not always bayonets and bullets, it’s the decisions you make during times of hardship. A soldier has to make the decision whether to keep fighting for what they believe in no matter what the stakes or to flee. In December of 1777, George Washington and his troops arrived at Valley Forge. Since the summer of 1775, all has gone well for the Continental Army. More recently Washington was presumably unable to stop General Howe and his British soldiers from claiming the national capital of Philadelphia. With Howe and his army of approximately 18,000 comfortably quartered in Philadelphia,

The Appalachian region is one of the most valuable areas of the United States. It is rich in many natural aspects and is home to some of the hardest working citizens in this country. Unfortunately, Appalachia is also home to a variety of harsh social problems including severe drug abuse and a gripping poverty facing a large portion of Appalachian citizens. The two of these issues seem to go hand in hand in many cases, so the solution of one could also lead to the solution of the other. Appalachians have always had a history of handling their own problems, these drastic social problems are no different.

The third region is the Appalachian Plateau this is the smallest region and is locate in North Western Georgia. It is only 300 miles long and consist of narrow valleys, ridges, and mountains including Lookout Mountain.

The Appalachian Mountains run through North Carolina and was formed about 480 million years ago during the Ordovician Period. Another North Carolina feature is the Great Smoky Mountains,The Great Smoky Mountains are a mountain range, along the Tennessee to North Carolina and borders the southeastern United States. There are many more land forms such as The Piedmont. The Piedmont, is a plateau area located in the southeastern part of the United States, and runs through North Carolina . It sits between the Atlantic Coastal Plain and the main Appalachian Mountains.North Carolina has a warm climate and it averages 5 inches of snow a year. Although, this also is different across the state. Along the coast, most areas get less than 2 inches of snow each

In Uneven Ground, the author Ronald D. Eller narrates the economic, political, and social change of Appalachia after World War II. He writes “persistent unemployment and poverty set Appalachia off as a social and economic problem area long before social critic Michael Harrington drew attention to the region as part of the “other America” in 1962.”(pp.2) Some of the structural problems stated by Eller include problems of land abuse, political corruption, economic shortsightedness, and the loss of community and culture; personally view the economic myopia as being the most daunting.

This area is also known as the Appalachian Mountains.

One of the major things noticeable from the cross section is that quite a few of the rock layers are over turned, where the older rock layers are above the newer rock layers. This is seen in the contact between the Quartz Monzonite of Papoose Flat and the Campito Formation which is also a disconformity. Next there is some fault zones separating the Camptio, Poleta, and Harkless formations. We then see some more overturned layers with the contacts between Saline Spring Valley Formation (lower and upper members) above the Mule Spring Formation along with some inferred folding. With a normal fault separating the inferred folding event, we see where the overturning occurs. In between the Cambrian layers we see Tertiary Basalt nonconformities also being folded, thus with that we know that the folding event was more recent than the formation of the Basalt. Next there is a large Basalt field with a spot of the Harkless formation. Again we see over tuning as the Basalt field ends there are the Devonian and Mississippian rock Layers on top of the basalt. Separating these overturned layers from the Harkless Formation and the Saline valley Formation (upper member), which are not overturned, is a thrust fault. From this information, there was a major stress event sometime after the Tertiary period causing the rock layers to fold and overturn. And from this stress event and from the folding, normal and thrust faults are formed. Finally we see that there were alluvial and landslide deposits from the Quaternary after the folding, faulting, and over

Proof of volcanic activity related to the break-up of Australia and Antarctica is seen at Bunbury, which is located 150km south of Perth, at the point where the basalt is of early Cretaceous, also on the middle Jurassic Kangaroo Island. However, evidence of Cenozoic eruptions is only seen in Eastern Highland. All through the Cenozoic, hot spot volcanic event transpire (Sutherland et al., 1985). Most of these events follow the Miocene (Stephenson et al., 1980) with recent eruptions close to the southern and northern margin of volcanic zone at southeast of South Australia and north Queensland respectively.

Pennsylvania is a state situated in the middle-Atlantic regions and north eastern part of United States. The Appalachian Mountains passes in the middle of Pennsylvania. It is the sixth densely populated, 33rd largest and 6th known state from 50 united states. It is one of original 13 colonies, William Penn was the one founded Pennsylvania as a haven for his associated Quakers. Philadelphia, Pennsylvania capital, was the location of the both first and the second Continental Congresses in the year 1774 and 1775, the end of which brought the Announcement of Independence, leading to the American Revolution. Pennsylvania became the second state after the war, where Delaware was the first, to approve the United States Constitution. Pennsylvania

Virginia also has three regions, which is divided by mountains. The first region is the Appalachian region, which is the north-west region until the Appalachian Mountains. Directly East of the Appalachian is the Blue Ridge

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

This chapter tells and explains the literature of Appalachia and includes important literature that’s came out of the region. It talks about many fiction tales Appalachia has to share and offer to the rest of the country. Many could say there myths or tall tales. They also explained how the lack of education decreased some literature and was a setback. Even with that being said they are many published writers from the region and plenty of great books to read. Other than just published books there a lot of poems that are famous and are very well written. Drama and theater are also two parts of Appalachian literature. I can relate to that because both of my roommates are in those programs. When I told them I was taking this class

Fault structure is the aftermath of a slipping event in the lithosphere that produces high velocity compression waves that can be imaged as they travel through and across the surface of the lithosphere. These waves affect and change, or in other words add complexity to the structure of the lithosphere within the fault zone. This