Tallulah Gorge is one of Georgia’s most popular outdoor destinations. It’s a state park for hiking, biking, fishing, swimming, camping, and kayaking. The gorge itself is around 2 miles long. There is great hiking along the rim and down into the gorge creating several miles of trails. Through the trails you can see the dam, several waterfalls, a suspension bridge, and lots of diverse plants and wildlife. There are water release weekends in April and November. Kayakers flock to the park for the high-speed whitewater reaching up to 700 cubic feet per second. The gorge also has an interesting formation history. It started as the beach of an island hundreds of millions of years ago. The beach turned to sandstone over time. Then the Appalachian
Van Staal, C.R., Whalen, J.B., Valverde-Vaquero, P., Zagorevski, A., and Rogers, N. (2009) Pre-Carboniferous, Episodic Accretion-Related, Orogenesis along the Laurentian Margin of the Northern Appalachians. Geological Society, London, Special Publications, vol. 327, p. 271-316.
The St. Peter sandstone lies in an unconformity. It is 250 feet thick, it can be up to 500 feet thick and it fills erosional channels in the underlying strata. Buffalo Rock is an erosional remnant of Ordovician St. Peter Sandstone and overlying Pennsylvanian clastics. Sign for swift, turbulent, and deep water includes gravel bars and erosional features that are 180 feet above the current level of the river and massive cross bedded sand and gravel deposits along the river course.
The Bullfrog Valley gang was a notorious counterfeiting ring that operated in the wilderness of Pope County during the depression of the 1890’s.The gang’s origin and and methods were mysterious, but the New York Times reported ist demise on June 28, 1897.The remote valley, which follows Big Piney Creek from Long Pool to Booger Hollow, was named for Chief Bullfrog, a Cherokee Who, according to legend, settled there after his tribe’s forced removal from Georgia (the Trail of Tears by the Indian Removal Act of 1830. The Bullfrog Valley, an unincorporated community not typically recognized on current Arkansas state maps, is located along the Big Piney Creek near the community of Silex. According to Dumas, historically the
Yes this feature is the result of erosion and depositional processes however, it is not associated with the current water course. This feature may be the result of a Gilbert type delta that once occupied this area. Gilbert type deltas have three main components; topsets, foresets and bottomsets. Topsets are fluvial sediments (primarily sandur deposits) that were deposited on the subaerial delta surface. Erosive events occurring on the upper forslope can result in downslope channels and chutes. These features are then eroded by either strong currents or by debris flow resulting in these channels and chutes to become filled. Foresets are a combination of sand and gravel facies. The are deposited by gravitational processes on the delta foreslope and the grains tend to become finer and more angular downslope. Bottomsets consist of fine grained silts and clay and are deposited at the foot of the delta front.
This paper will review the origins and geology of the Stone Mountain monolith in North Georgia, the history of the area and people and groups who have utilized the site for social and commercial purposes.
Cuyahoga Valley National Park was formed the same way that most other valleys were. It is believed that long before the ice age occurred an ancient river carved through this area. This river left behind deposits that after millions of years transformed into the parks sandstone bedrock. As the ice age came into effect, this river froze and became part of a glacier that had an even bigger effect on the landscape of the valley. These glaciers scraped through northeastern Ohio and in the process left behind deposits that now make up the parks fertile soil (“Rock, Ice, and River”).
The world has been shaped by many events. Like a sculpture each piece was a result of an event that made it that way. The Snake River Canyon is no different, most of upper Utah and part southern Idaho show the scars of an event that rocked the landscape into what it is today. When researching and digging in the region you can find remnants of an old marine environment, from sediment deposits to river terraces hundreds of feet high. It’s confusing to think of the area as a giant lake with sandy beaches and powerful waves, but the overflow of this huge lake is what created most of the landscape you can see today. The great Bonneville flood was the world second largest flood, emptying over 32,000 square miles of lake volume. (Utah Geological Society) The flood that the this overfill caused carved through many areas and created the beautiful valley that can be seen there. However, this didn’t just happen over night. The pre-flood history, flood event, specific flood deposits all played an important role in shaping this large Geological marvel. Understanding what happened back then can give us a good glimpse into better understanding the region today, which can lead to better predicting and preserving for the future.
The Revolutionary War had many battles but none as short as the Battle of Fort Ticonderoga. In fact, the battle was over in less than twenty-four hours. Fort Ticonderoga was taken by American soldiers without a single shot fired. The weaponry seized from Fort Ticonderoga played a major role in strengthening the fire power of the American forces and helped save Boston from the British.
Providence Canyon was first made by farmers with water run-offs from their crops. Then, it started making ditches that would get deeper and wider, which turned into drop-offs and cliffs. Once it was made local people would drive there and have a picnic on the cliffs and explore the canyon. Now, government officials saw the economic value in Providence
Natural stone arches are geological formations that occur when rock is exposed to substantial amounts of erosion , which over time forces the rock into the shape of an arch. Stone arches are among the most diverse of rock formations, not only because of the large area where they are known to be found, but also their complex ways of forming. Although many factors contribute to making natural stone arches so enthralling, one key role keeps and hones our constant attention: each and every stone arch every formed will fall. Despite the things we do know about stone arches, they are continuously changing and teaching us new things about them as well as the world around us.
The Precambrian Shield Rocks found in the Brickworks was formed in an ancient sea more than 1.4 billion years ago. Over many years, the heat and pressure from plate tectonics slowly pushed the land into a mountain chain. During the Ordovician period (around 470- 448 million years ago), the mountain chains This layer of shale and limestone is called the Georgian Bay
and the importance of their history. It is the first monument to be added to the National Park
Canyonlands National Park, immense amounts of wilderness and rock, is located at the heart of the Colorado Plateau (Canyonlands National Park-Geology). Millions of years have formed specific features to the rock and surrounding wilderness that make it so special. Throughout the park, you will find that the sedimentary rock has formed many features such as hundreds of colorful canyons, mesas, buttes, fins, arches, and spires. The Green and Colorado rivers have played a major role in the formation of many of these features. These rivers cut through the park forming two massive canyons. This further splits the park into three distinct zones. “Island in the Sky” sits to the north while “The Maze” sits off to the west and “The Needles” to the east (Canyonlands National Park Information Guide). “Island in the Sky” serves as Canyonlands’ observation tower; it allows tourists to see overwhelming vistas of the rest of the land. “The Maze,” as hinted at by the name has been described as a “30 square mile puzzle in sandstone” (NPS: Nature & Science» Geology Resources Division). This section of the park often ranks as one of the most remote and inaccessible areas of the United States. Lastly, “The Needles” is known for its diversity in rock features. Throughout this land, features such as sculptured rock spires, arches, canyons, grabens, and potholes can be seen. The varying names hint at the diversity of the land as a whole. As said by The National Park Service’s Geology Resources Division, “Traces of the Anasazi can be found in almost every canyon in the Needles. Many of their stone and mud dwellings and storehouses are remarkably well-preserved. Tower Ruins, built high on a cliff ledge in a side canyon of Horse Canyon, is an outstanding ex...
With over two hundred miles of trails to travel, it is easy to see the tranquility of this distinguished place, and why so many noble men gave their lives protecting it. From tents to pull-through, private or public, and campgrounds there are plenty of options and places for you to park your camper or pitch your tent. Only five miles from the national park, Jackson Hole offers several nice hotels. Grand Teton National Park can be enjoyed by everyone with its forty-two mile scenic loop drive. If you do not want to drive, you can sign up for a scenic float trip that takes you straight through the heart of this magnificent mountain range on the Snake River. Another option you have to viewing the serenity of this place is through a scenic cruise on Jenny Lake. On this cruise you would spend approximately 1 hour learning about the history and geolo...
...These rocks include indurated conglomerates, coarse-grain granites, and Arkosic and breciated granites. Furthermore, there are evidences to indicate that faulting took place in the area. Hydrothermal and epithermal action must have intruded the rocks in the Goldfield area forming small stringers of quartz. There are also evidences of sedimentary rocks such as sandstones, limestone and conglomerates found near Roosevelt Lake (Eppinga, 2006).