Miranda “Randee” Allen Bruce Franklin Arkansas History 22 November 2015 Crater of Diamonds State Park: Murfreesboro, AR The Crater of Diamonds State Park is one of the “world’s only diamond-bearing sitse open to the public.” This famous state park is located in the southwestern corner of Arkansas near Lake Greeson, also known as Murfreesboro. There are many attractions such as: Diamonds Springs Aquatic playground, picnic sites, wildlife trails, a gift shop, and the exciting art of gem hunting. Hunters are given the chance to hunt for gems over thirty seven and a half acres of plowed land that has been eroded over the years. It is one of the eight largest volcanic centers in the world. The large area is plowed periodically to help access
Illinois State Geological Survey, 2005, Time Talks – The Geology of Starved Rock and Matthiessen State Parks
N. Scott Momaday wrote these lines in his 1991 book of poems, In the Presence of the Sun: “In the shine of photographs / are the slain, frozen and black / … In autumn there were songs, long / since muted in the blizzard.” In this poem called “Wounded Knee Creek”, Momaday depicts the aftermath of Federal and Native American conflict at the Battle of Wounded Knee. He reminds the reader of how the event and loss of native life are remembered solely through these photographs of the dead and lost. Momaday’s work represents the Western tradition of artists using their art to memorialize and remember the past peoples and places that have been transformed, built up, and destroyed through government institutions of the West. It is this remembrance of
The Bristol Caverns are open all year around, except for on holidays, and the time that you are able to visit is subject to change during different seasons. You can visit the Bristol Caverns from 9a.m.-5p.m. on Monday through Saturday and from 12:30p.m.-5p.m. on Sundays. It is suggested that you call before attempting to go to the Bristol Caverns because of the number of tourists. (http://www.bristolcaverns.com). The drive from the ETSU campus to the caverns takes about forty-two minutes. In order to get to the Bristol Caverns you can start on 11E, get off at the Bluff City exit, take it to 394, turn right onto 435, and you will then see the Bristol Caverns on the left. Upon arrival you will be expected to pay an admission fee of $9.00, which can change, according to age. The Bristol Caverns offers special rates and tours for groups interested in touring. One of these group opportunities, "Wild Tours" (http://www.bristolcaverns.com), gives groups the chance to explore parts of the cave normally not seen, provided a guide is present.
Harris, Ann G., Esther Tuttle, and Sherwood D. Tuttle. "Katmai National Park and Preserve." Geology of National Parks. 4th ed. Dubuque, IA: Kendall/Hunt Pub., 1990. 441-48. Print.
The tar creek mining site originally was owned by a Native American tribe, the Quapaw. The Quapaw wanted to keep these lands, but the Bureau of Indian Affairs deemed members opposing a transaction to mining companies “incompetent” (1). In such a case the business could continue and the Bureau of Indian Affairs sold the lands to mining companies. In essence these lands were stolen from the Quapaw because they were ripe for mining. These mines were then used from approximately 1891 to 1970. In the 79 years the mines were open 1.7 million metric tons (~3.75 billion pounds) of lead and 8.8 million metric tons (~19.4 billion pounds) of zinc were withdrawn from the mine (2). The entire area around Tar Creek is known as the tri-state mining area. This tri-state area was a massive source of metals. This area accounted for 35% of the all worldwide metal for a decade. It also provided the majority of metals the United States used in World wars I and II (3).
Stone Mountain is an igneous intrusion often referred to as a geological pluton. The granite pluton is part of the Piedmont Plateau region of the Appalachian Mountains and was formed along the same geological fault line that created the Blue Ridge Mountains but is not part of the Blue Ridge chain. Northern and Eastern Georgia have relatively frequent seismic activity with ten quakes recorded in 2013. These quakes occurred at an average depth of 9.6 km which make them less obvious and cause less property damage. This same seismic activity created Stone Mountain 300 million years ago during the last stages of the Alleghenian Orogeny when massive tectonic plate shifting allowed a large mass of magma from beneath the earth’s crust to well up . Flow structure markings on the mountain show the stone was formed underground after several eruption pulses failed to break through and then cooled to form, ultimately creating granite mass that rises 825 feet above ground, extends 9 miles underground and has a circumference of 5 miles at its base, making it the largest exposed dome in the world . Rising 1683 feet above sea level the summit of the dome is bare stone with rock pools and an unobstructed view that extends to Kennesaw Mountain, Amicacola Falls and Mt. Yonah state parks, including a breathtaking view of the Atlanta Skyline.
Yellowstone Park is the world’s first national park and the 8th largest national park in the United States. The park is primarily located in Wyoming and parts of Idaho and Nevada (56 Interesting Facts About . . . Var Addthis_config = ) It is a tourist attraction due it’s 5,000 to 15,000 years old geysers, over 45 waterfalls, canyons, rivers, hot springs, and its massive concentration of natural wildlife. Two of the most popular park attractions are the Old Faithful geyser and the Grand Prismatic springs. ("Fun Facts." - 32 Interesting Facts Yellowstone National Park.)
The Little Missouri River eroding the mountain range is the reason that the park is as it looks today. The park is believed to be <60 million years old. Over 60 million years ago volcanos all over the west were erupting and spitting out amounts of ash. The rivers near the volcanos were gathering. The rivers began to dry out, leveeing the ash behind. The ash was being dried in layers and turned into sandstone, siltstone and mudstone while the ash layers became bentonite clay. This Bentonite clay is dangerous because it gets people stuck, like quick sand it is located throughout the park. It can pull the car tires un...
Objectives • To evaluate the difficulty of mining and reclamation To calculate costs, expenses, income, and profit from a hands-on mining exercise. • To evaluate the effectiveness of reclamation and its added costs to mining. To describe the increasing rarity of some non-renewable mineral resources. Introduction Minerals play an important role in our day-to-day life, but we often do not contemplate how the minerals are obtained. Minerals are scattered all over the world, just like any other resource.
Out of the United States, Alabama was rated sixteenth among the states because of their industrial minerals produced. The industrial minerals that were produced were limestone, lime, dolomite, crushed stone, marble, building stone, sand, gravel, chalk, clay, shale, kaolin, bauxite, bentonite, fuller’s earth, fireclay, recovered sulfur, salt, and mica. In 2007, Alabama’s value of industrial minerals was about two percent of the national mineral production. In 1998, Alabama was ranked second in the nation because of their production of lime and clays. The state proceeded on to be third in bentonite, fourth in kaolin and masonry cement, and eighth in salt production in the United States. However, with the development of an operation in Micaville, Alabama was nationally ranked second in the production of mica. (Minerals in the Economy of Alabama, 1)
The Nevada Test Site is an area designated by the United States Government for Nuclear Weapons testing. It is located in rural southern Nevada and is about the size of the State of Rhode Island. This location was founded in 1952 as one of 5 on land sites designated for this task. Above ground nuclear or atmospheric testing was conducted at the Nevada Test Site until 1958. There was a break in testing until the United States decided to begin underground testing in 1962. There were a total of 828 nuclear tests performed underground during these years. In 1963 a limited Nuclear Test Ban Treaty was signed by the United States that limited above ground tests world wide. These underground tests were performed until 1992, and nuclear testing in the United States seized all together in 1994 when the Nuclear Test Ban Treaty was signed. The majority of the testing was conducted to further the efforts of the Cold War, as well as, to further general understanding of the effects and results of nuclear testing. This paper will discuss the history, geological aspects, and impacts of the Nevada Test Site on this and surrounding areas of Nevada.
around the gulch was called Diamond City, which is located 30 miles east of Helena in
At this National Park you may find miles and miles of hiking trails through volcanic craters, hot deserts and rainforests. They have Drive Chain of Craters Roads, Ranger Programs, A Walk Into The Past, and After Dark in the Park.
The Rock Cycle The Rock Cycle is a group of changes. Igneous rock can change into
One morning, a well-known gentleman went into a bank in London, and was received immediately by Mr. Alexander Holder, head of the bank. He asked for a loan of fifty thousand Pounds. Mr. Holder asked him to present collateral to cover that large sum of money; the man showed him a crown that belongs to the country. Knowing the risk, Mr. Holder agreed to lend the gentleman that large sum of money if he pays it back in a few days. After the gentleman left Mr. Holder decided to keep the crown all the time near by him, so he took the crown to his home in Streatham. There he lived with his only son Arthur and his niece Mary who was an orphan. He told them about his story with the crown of diamonds. When the father was going to sleep, Arthur asked for two hundred pounds. He refused to give him thinking his son was spoiled by his rich friends who had nothing to do except watch horses. Before going to sleep, he went to check that all windows and doors were locked. He saw Mary at a side window at the hall. She closed it quickly, and Holder noticed that she looked anxious. After he went to sleep, he heard some noise that woke him up; he waited until he heard it again coming from his sitting room. He jumped out of his bed and saw his son holding the crown broken from the side and three diamonds were missing. In grief, he accused Arthur of being a thief and a liar. Meanwhile Mary came in and seeing the crown fainted. Arthur asked if he could leave for five minutes but Holder refused and called the police to take his only beloved son to jail. The police searched the house but could not find anything and advised Holder to get the help of Mr. Holmes the famous detective.