Mammoth Cave National Park Research Paper

12. In the Figure 5 profile, the coastline is within a few kilometers of the western end of the vertical cross section. From the coastline, water depth increases very gradually to about 40 m at 140 km from shore (western end of the profile). This segment of the vertical cross-section resembles the continental [(rise)(slope)(shelf)]

Similar to how other gorges are created, it was the energy of the river water rushing from the melting glacier that was able to cut into the surface of the bedrock. Streams carved through

There is an abundant amount of history buried inside the walls of Little Cottonwood Canyon. This mountain range has existed since the Ice Age which was roughly 14,000-30,000 years ago. Consequently, the Ice Age and Lake Bonneville created a Delta at the base of the canyon and a long creek that carves its way down the mountain (Wilkerson 1987). It also created Cirques; which is a crescent formed slope on the faces of the mountains (Richmond 1964). Little Cottonwood Canyon also lies on an active fault, the Wasatch fault, and it has been active for the past 15 million years. This fault in the last 6000 years has had around 19 major earthquakes that instigated a large movement of about 6-10 feet of

This article talks about the study of the Dunbar Cave in Montgomery County, Tennessee to learn more about the varied ways that the cave was used by people. Many of the artifacts that was in the cave linked its usage time to be from the Late Paleo-Indian to the Mississippian period. The article define dark-zone cave art as “the decorations in the areas of the caves that is beyond the reach of external lights”. Mug Glyph Cave art was found in the 12th Unnamed Cave in Tennessee and since then sixty-nine other caves that had dark-zone cave art were found. The artifacts and chronological data from these sites indicates that the tradition of cave art began 6000 years ago.

Ten thousand years ago, mammoths once inhabited the land we now call home. Where we eat and shop, where we sleep and go to class was once home to these beasts. Standing over fourteen feet tall and with tusks over sixteen feet long these animals found the area now known as Waco their home. I did not know that mammoths even inhabited the Texas, and even more surprised that they lived here in Waco. There are many incredible things that happen here in Waco, and the Waco Mammoth National Park is one of them. This newly sanctioned national park is beautiful and with its incredible history it attracts the attention of thousands of tourists every year. For this park, I analyzed, the quality of the tour and for the tour guide to be informative, if the price of the park is worth the money,

Louis, there is the Meramec Cavern. Tourists are allowed to enter the cave and there are informational and educational kiosks that provide the user with background information on the history of the cave such as how it was formed, who it was founded by, the reason the founder took and interest in the cave, and why the cave is significant. You can also take a tour through the cave which lasts around an hour and a half. This tour takes you throughout the entire cave. A major part of the tour is when you arrive at what seems to be a pool of water at the end of the cave. The tour guide then shows you that the pool comes out on the other side of a rock wall. This pool was used by Jesse James to stash his stolen goods and hideout from the police. The Meramec Cavern also offers ziplining outside the cave and a small river that you can canoe or kayak

Powerful forces of the earth cause a landmass to slide under the water. The hot water from the floor of the ocean then melted the rock from the land, forming granite rocks (U.S. Department of the Interior). Mesozoic volcanic and sedimentary rock are scattered through Sierra Nevada Batholith, which covered most of the park during the Jurassic and Cretaceous times (Harris). Weathering and the batholithic makeup impact the exterior of the landforms within these national parks. Yosemite National Park has a very similar geological history compared to the Sequoia and King Canyon National parks, due to the fact that they all lie in the Sierra Nevada’s peak and western slopes (Harris). When it comes to lithospheric extension in the Death Valley Region, during the time of rapid growth, the plates in this region rapidly expanded. In the region of the Sequoia and King Canyon national park the plates did not expand rapidly, thus indicating that more extension occurred in the Sequoia and Kings Canyon region (Jones). Under the surface, there are many marble caves that are endemic to the area (U.S. Department of the Interior). It is clear that natural forces like these have the ability to create beautiful and interesting geology. The description of the tectonic plates would be an ocean continent subduction zone (U.S. Department of the Interior | U.S. Geological Survey). This occurs because of the above process. A specific rock located in the national park is the Moro Rock. Moro rock is a large granite rock that is shaped like a dome. It was made by the process of exfoliation that has to do with the layers of granite expanding over time (U.S. Department of the Interior | U.S. Geological Survey). The exfoliation process creates many of the rock features located in the park. This exfoliation process is the same one that creates many of

The karst terrain which creates the geomorphic conditions for sinkholes is a broad topic in the field of geology, and encompasses the study of groundwater, drainage, chemical processes, and many other considerations. Essentially, karst regions are located where the rock below the earth can be dissolved by the acidic groundwater which percolates through it (The Science of Sinkholes). These areas are underlain by soluble rocks such as gypsum, limestone, and dolomite which typically react with carbonic acid (H2CO3) from groundwater to dissolve the rock. Presence of limestone is

The Cherokee Caverns is located in 8524 Oak Ridge Highway Knoxville TN 37931 US. The cavern hold up events like music festival, Christmas, and the not so scary Halloween. Inside this wonderful caverns are inhabited by the nocturnal animals the bats. The history within the cavern began to form about 300 million years ago. There are shells and skeletons of ancient marine life would mix with sand, clay, and other material to form a rock known as copper ridge dolomite. Cherokee Caverns was discovered in 1854 by a Robert Crugdington. The cave was open to the public in 1929 under the previous name Gentry’s Cave. There were Indian artifacts that is located in the cave revealing how another entrance to the cave exist in the past. Within the cavern,

The Wyandotte caves are made out of limestone like any other cave in Indiana but the Wyandotte cave has a “cliff ”so when people go they have to be careful. There is a Mount Baldy in California but the one in indiana is special. Mount Baldy isn't a mountain, it’s a sand dune. Sand dunes are mountains hills and ridges with sand on them and they “Hide” behind beaches and are affected by tides. In other words Mount Baldy is a mountain with sand on it. Mount Baldy is also known as the “living” sand dune, because every year it is someplace new, South of the shore of Lake

Mesa Verde National Park on the Colorado Plateau contains many geological aspects of interest, including its sedimentary rock layers, its canyons, its alcoves utilized by ancient people and how these alcoves were formed. Mesa Verde National Park is located in the southwest corner of Colorado, close to the Four Corners area, on top of a high mesa overlooking the Mancos River (Harris et al. 2004). The park, covering 81 square miles, consists of several main sedimentary formations that are characteristic to the park (Encyclopedia Britannica 2015). Canyons are carved into the sedimentary rock, with the cave dwellings found high on their steep walls. These dwellings are an especially unique aspect to the Mesa Verde National Park, and are built out of large alcoves. The alcoves were produced by weathering and erosion of the sedimentary rock type. To better understand how these alcoves formed, we must understand the geology of Mesa Verde National Park and how it has developed over history.

In the movie Cave of the Forgotten Dreams, director Werner Herzog and a very small crew are given the opportunity to go to France and see Chauvet Cave. While watching the start of this movie, I was very surprised to see that they were limited with how many people they could bring into the cave. I have gone to a cave in South Dakota and they took hundreds of people in it at a time. So, seeing that I think they only had like five crew members was very shocking. I was surprised though how many experts they had working on mapping the map and doing other tests on the cave. I thought maybe, there would only be like two experts in at a time and not five or six. I also didn’t know there was that many different experts that all can work on the same thing at the same time. Also, while watching I was surprised to see the equipment that they had to use.I never really thought about how the lights can affect the cave walls and the paintings.I was impressed that they filmed the movie in the cave with a non professional movie camera, I did not know that there were other cameras that could work that well in the dark of a cave.

Kentucky has more than 850 miles of Kentucky caves at Mammoth Cave National Park, the longest cave system in the world. View exotic animals and hundreds of aquatic creatures at zoos and aquariums. Feel the rush of one of the top wooden roller coasters in the world. Visit the Kentucky Horse Park for an up close and personal experience with championship thoroughbreds. As well as soaking up all the amenities, nightlife, spas, theater and art of Kentucky’s major cities (Kentucky Unbridled

Up the ridge is a cave with a ladder leading to a glade. The large clearing is

Lechuguilla Cave, the fifth-longest cave in the world, exists in the park. It was discovered in 1984, when miners heard wind roaring from the cave. The cave contains antibiotic-resistance bacteria, which developed resistance over millions of years. However the bacteria cannot spread to humans, but is resistant to every type of antibiotic tested.