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Geological history of Mammoth Cave
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Mammoth Cave National Park is home to the world’s largest known cave system. Millions of years ago this region was originally located 10° south of the equator (GORP.com, 2002) in an area was covered by shallow seas. Over the years plate tectonics have caused this area to move to 37.1833° north of the equator. Also, causing the shallow sea waters to dissipate and upheaval of the earth’s crust, known as the Cincinnati Arch (Livesay,1953). Over the years the Cincinnati Arch and surrounding areas have been subjected to erosion, weathering and more upheavals causing the rivers to once again flow. The, weathering, erosion and area hydrology created the karst topography seen in the area and consequently the cavern systems with in Mammoth Cave. …show more content…
In the Mississippian Era this area was located 10° south of the equator (GORP.com, 2002) and was covered by shallow seas, the Mississippian Seas (NPS.com). During this time deposition of sediment consisting largely of sand, silt, clay and the calcium carbonate shells from the inhabitants of the seas began forming layers of sandstone, limestone and shale. (Livesay and McGrain, 1962-1953) Between the Pennsylvania and Permian Era crustal movements, known as plate tectonics, shifted this area to 37.1833° north of the equator, causing the seas to dissipate, and the land to start to warp upward. The rivers now flowing over this land deposited additional sediment forming new layers. Continued warping of the crust created an upheaval of the crust known as the Cincinnati Arch (Fig 1) during the Paleozoic Era. (Livesay and McGrain, …show more content…
Uplifting combined with the intricate water network, known as hydrology, and the resulting weathering and erosion processes of the area formed the karst topography visible on the surface, the caverns and geologic formations below the surface. The cave system below the surface consists of around 390 miles of explored caverns and is believed to have at least another 1000 miles of caves yet to be explored.( http://www.nps.gov/maca/naturescience/cave.htm) Over the years many studies have been conducted to determine exactly how and why the caves formed. Research found both the composition of the land (rock types), the area hydrology and the geologic processes occurring are the
This is a report based on three days of observations and testing in the region known as the Peterborough drumlin field. It will address a variety of regional elements, such as climate, soil, vegetation, hydrology, geomorphology, and geology. A variety of sites located on the Canadian Shield, the zone of thick glacial deposits to the south, and the transition between them will be the focus of the report. It is supplemented with previous research on the region. September 8, 1999, day one of the field study involved an area of largely granite bedrock that is part of the Canadian Shield and is the most northern point of study (see Map 2). September 9, 1999, day two, involved three main areas of study: the Bridgenorth esker (Map 3), Mark S. Burnham Park (Map 4), and the Rice Lake drumlin (Map 6). These sites are in areas of thick glacial deposits. September 10, 1999, day three, involved studying the Warsaw Caves (see Map 5) as a transition zone between Precambrian Shield rock to the north and Paleozoic rock to the south. A general map of the entire study region is provided by Map 1.
The entire tour requires a lot of walking, so wearing tennis shoes is recommended. Dress prepared for a cool environment because while inside the cave you will experience temperatures from 50-60 degrees. As you walk along the tour of the Bristol Caverns, a tour guide will inform you about the history of the cave: such as the original entrance place to the caverns used by the Cherokee Indians and how an early pioneer would store his fruit in the cave for extended freshness (tour guide). While the guide leads you through the cave of the caverns, you can view many formations and scenes. The formations are called stalagmites and stalagtites, which are created by the moisture and minerals in the cave hardening. One inch of these formations lengths can take from 150-300 years to form (tour guide). During the tour you will venture through different levels of the cave.
Earthquakes are a natural part of the Earth’s evolution. Scientific evidence leads many geologists to believe that all of the land on Earth was at one point in time connected. Because of plate tectonic movements or earthquakes, continental drift occurred separating the one massive piece of land in to the seven major continents today. Further evidence supports this theory, starting with the Mid-Atlantic ridge, a large mass of plate tectonics, which are increasing the size of the Atlantic Ocean while shrinking the Pacific. Some scientists believe that the major plate moveme...
The sharp differences in elevation between the Badwater Basin and the surrounding mountains that include the highest point in the continental US (Mt. Whitney at 14,494 feet) stand as a representation of the regions violent tectonic past. The mountains themselves are considered fault block mountain ranges meaning that they were formed when blocks of rocks were squeezed through the Earth's crust along parallel faults or were loosened from the crust when it separated at a fault. In the valley, both of these methods not only were the cause of the current mountains formation less than four million years ago, but also are causing the mountains to be uplifted while the valley floor drops even further. This phenomenon is one of the reasons why the lowest and highest points in the continental...
After the Laramide orogeny things were still happening, just as always with Earth. Something is always changing even if it is not detectable day by day. Due to the Farallon Plate subducting there was a suction like effect going on because of the water that was being taken in with it (Humphreys). This would cause the North American plate to become weak and unstable, because it was being hydrated. This eventually would result in large plateaus and large amounts of uplift (Humphreys). There are many things that have been going on through out this time period but it all turns around and creates and shapes the earth into what it is today as well as what it will be in the future.
This seemingly boring process came to fruition in one of the most beloved National Parks in the United States of America. The Grand Canyon National Park is located in the state of Arizona. It is over 270 miles long and, at some points, is up to 18 miles wide and deep (History.com Staff). Its deep walls help provide a geologic history of the earth, because the many layers contain artifacts and information about the climate at the time (History.com Staff).
The geological processes that formed and continue to influence Mono Lake began approximately 215 million years ago when the Farallon sea floor plate began subducting, or pushing, under the North American plate. The North American plate was pushed over the sea floor plate by the force of the African and South American plates rifting apart. The friction from the North American plate rubbing against the Farallon plate melted some of the continental rocks, which then erupted in a long volcano chain, the Sierran Arc, stretching from Alaska to Mexico inland from the coast. Over time, the unerupted magma chambers from the Sierran Arc cooled into the granitic batholith that is the Sierra Nevadas (Tierney, 26-27).
The team of scientists consisted of a biogeologist, geochemist, and tectonic geologist with the common goal of understanding the coevolution of life and environ...
The Grand Canyon has a lot of different features and is an exciting place that holds a lot of secretes and mysteries that scientists have been trying to figure out since the Grand Canyon was formed. It is millions of years old, over 277 miles wide, 18 miles wide, and defies many normal Geography features that are true in every other situation. Many theories have been presented that seek to explain the formation of the Grand Canyon. The first theory is that the Grand Canyon has a lot of Erosional Scarp Face’s, that have come together over the years, which is one theory that has been presented. Scientists have also tried to see if the Colorado River cutting into the canyon caused the Grand Canyon.
Nature had sculpted the basic geological shape of North America as recently as 10 million
Krajick, Kevin. "Tracking Myth to Geological Reality." American Association for the Advancement of Science. 310.5749 (2005): 762. Print. .
When John Wesley Powell conducted his first expedition through the Grand Canyon in 1869, he and his team barely survived the arid desert conditions. Despite their beleaguered situation, Powell recognized the “great antiquity of the earth” in the landscape of the Grand Canyon, and determined to return under more opportune conditions. While the names Powell gave to geologic formations did not always accurately
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The foundation of the Great Lakes began around three billion years ago, which is known as the Precambrian Era. The Precambrian Era contains numerous ecological events, which consists of volcanic activity to erosion to the mountains and hills seen today being formed. Then during the Pleistocene Epoch or known as the “Ice Age, occurred between 1.6 million and 10,000 years ago. At least four times during the Pleistocene Epoch, large masses of ice advanced and retreated over the surface of what is now North America. As the glaciers advanced, giant sheets of ice flowed across the land, leveling mountains and carving out massive ...
also films that could have been seen for a small price, but if one has the time