Mammoth Cave 1790s

To begin, the mouth of the canyon features a hilly landscape with scars from landslides created from the uplifting of land by the Wasatch Fault. The fault, responsible for the creation of the Wasatch Mountains 25 million years ago, is a normal fault (Eldredge, 2014). Unlike some faults, vertical movement of the terrain is limited and slippage only occurs every several hundred or thousand years. Signs of the fault at work can be seen through the mouth of the canyon with the orange Tintic Quartzite which is dated back to the Cambrian Age. Layered beneath the quartzite is tillite from the Precambrian Age. To the west and separate from the Quartzite and tillite by the Wasatch Vault are limestone sections from the Missippian Age. (Rigby, Hintze, 1968, pg 23).

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.

In class and watching this movie we find out that Chauvet Cave was discovered in December of 1994 when Christian Hillaire, Eliette Brunel-Deschamps and Jean-Marie accidently found it, because they had felt a draft. In the introduction to the movie we find out that the cave sits next to this beautiful river named Pont d’Arc. We later find out that it might be this river that feeds into the cave that brings some bones into it, such as golden eagle bones. I also find out that the entrance that these hikers had found was actually not the true entrance. We find out that the actual entrance was covered when the cave had collapsed in earlier times. I was really surprised that they were able to find the actual entrance. I thought since the cave had collapsed that it would have damaged or destroyed the original entrance.

Because the desolation and erosion depends the valley with time reducing the water table and allowing the water from the cave to diapate.

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

Explain how the type of rock can affect the formation of stalactites when impacted with rainfall in Princess Margaret Rose Cave?

This study is focus on the 11th Unnamed Cave in Tennessee. This cave was the first of its kind because this cave is the only one that was found to contain pictograph, petroglyph, and mud glyph all in one site. The article explain that the site is significant because there are evidence to showed that the site underwent a series of diverse but interrelated uses. The first out of all the cave sites to contain all three different form of rock art. Also, because the site was found in the eighteenth century which had some form of documentations on the uses of the cave. The authors believes that since the cave showed many different kind of activities, it is possible that the activities reflect a complex behaviors more elaborated and sacred than

Our hike will start here, at the north rim of the Grand Canyon. We will go all the way to the bottom of the canyon. But first, a description of this area. The Grand Canyon is one on the most visited and studies sites for geologists on Earth. There are almost forty major sedimentary rock layers exposed in the Grand Canyon. Some of these rocks layers are two hundred million years old or two billion years old. Most of the sediment that makes up the rocks was deposited by oceans and seas, which now, are long gone. We know this because there are many fossils and and other records on large bodies of water in the Grand Canyon. The Grand Canyon is found in the Colorado Plateau. The Colorado Plateau is lifted almost two miles, or four and a fifth kilometers. It started to lift up seventy-five million years ago. This started a mountain-building period of time called the Laramide orogeny. During this period, the Rocky Mountains were created. The main types of rocks found in the Grand Canyon are limestone, siltstone, shale, and sandstone. Many of the layers are made up of limestone. Some examples of these are the Kaibab Limestone, the Redwall Limestone the Temple Butte Limestone, and the Muav

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.

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 Naracoorte caves provides plenty of information about the history during the Pleistocene era. In terms of a scientific understanding, Palaeontologists have excavated and dated many of the fossils in Naracoorte Caves and have reconstructed the skeletons of a number of the megafauna that inhabited the area so many years ago. This gives them a better understanding of the evidence supporting Australia’s changing environment, climate and fauna and how each of these contributing factors have played a major role in the extinction of these megafauna's. With the reasons provided, the protection of the Naracoorte caves is essential as the caves holds many scientific evidence and fascinating values as well as Australia's record of

The only types of rocks found in Big Bend National park are Sedimentary (N.P). The specific names for these rocks are: limestones, shale and sandstones, clay, Lava Flow, Conglomerate, Marl, and Cherty Limestone are found in this park (N.P). These rocks were likely abundant throughout the park; when the area was covered by a salty sea during the Cretaceous period (N.P). The way how these rocks formed is by the results of pebbles being cemented together. Another way how the rocks can form is by how the earliest layer of rock was deposited in a relatively deep marine environment. After the next layer above the shale indicates that the rock is deposited in a very shallow way, that's when the ocean water starts

Mammoth Cave is found in Mammoth Cave National Park that was founded in 1941. Currently, it is the longest cave known in the world with approximately 350 miles of underground interconnected chambers and passages. Mapping and exploration continues and seems like it has no end. Mammoth Cave National Park is situated near Park City in south central Kentucky. It lies in forested and hilly areas of three counties; Hart, Edmonson, and Barren. It occupies about 50,000 acres. A landscape that is mainly covered by the solution features such as sinking streams, large springs, sinking holes, and caves is referred to as karst. For instance, as shown in figure 1.

The difference in the gameplay becomes much more apparent when looking at the two versions of the game as they were released. The original Colossal Cave Adventure was created by Will Crowther, and was heavily inspired by the work that he had done as a caver previously. He based the cave in the game off of Mammoth caves, which is a cave

A first group of caves was created in the 2nd century BC: the chaitya-grihas open into the rock wall by doorways surmounted by a horse-shoe shaped bay. The ground plan is a basilical one: piers separate the principal nave from the side aisles which join in the apsis to permit the ritual circumambulation behind the (commemorative monument). This rupestral architecture scrupulously reproduces the forms and elements visible in wooden constructions.