Montana Little Belt Mountains

Rock Canyon is an excellent site for geologic research and has been investigated by geologists from around Utah and neighboring states. With outstanding extrusions of quartzite, tillite and limestone, it’s a favored destination for hikers, rock climbers and scientists. The quartzite is considered the most unique feature of Rock Canyon as it’s one of the few clear and distinct examples of the sedimentary processes involved with a shallow marine setting. The tillite beneath the quartzite draws attention to the ancient glaciers to the past. In conjunction with the active Wasatch Fault found at its doorstep, Rock Canyon is an important place in Utah for geologists.

The Rocky Mountains, also known as the Rockies, extends for some 3,000 miles (4,800 km), that covers land in two North American countries! With a distance of 3,000 miles, the Rockies must have a variety of physical features and landscapes that makes it an attractive area to tour and explore. However, all of the human interest in this mountain range could come at a devastating cost. Disturbances such as resource extraction, tourism/settlement, and farming in the Rocky Mountain region must cease because they are causing major, irreversible environmental degradation.

The Appalachian region is one of the most valuable areas of the United States. It is rich in many natural aspects and is home to some of the hardest working citizens in this country. Unfortunately, Appalachia is also home to a variety of harsh social problems including severe drug abuse and a gripping poverty facing a large portion of Appalachian citizens. The two of these issues seem to go hand in hand in many cases, so the solution of one could also lead to the solution of the other. Appalachians have always had a history of handling their own problems, these drastic social problems are no different.

The Ozark Mountains are characterized by eroded plateaus caused by the collision of the super continent of Gondwana, which compressed the present continents of South America, Africa, Antarctica and other land masses. These forces uplifted Arkansas with limestone and calcareous rocks such as sandstone and chert. Erosion lowered the surface creating a level plateaus which included: The Boston Plateau, the Springfield Plateau, and the Salem Plateaus. Rivers, over time, cut valleys into the plateaus. Present day Fayetteville-Springdale-Rodgers, Harrison, Mountain Home, Batesville, and Clinton are all cities which are within the Ozark Mountains boundaries.

estled between the Blue Ridge Mountains and Allegheny Mountains, Rockingham County is located within the Shenandoah Valley of Virginia. Originally founded in 1778, Rockingham County has become a historical community committed to implementing an economic strategy of attracting new business and industry that are compatible with the way of life in the Shenandoah Valley and assisting in the retention and expansion of existing companies (Rockingham County). Most commonly known for its beauty, Rockingham County is comprised of six metropolitan cities, of which Harrisonburg holds the county seat (Rockingham County).

The Washoe and Paiute tribe’s lives changed with the influx of settlers that came with the Comstock mining rush. Nevada being a desert had limited resources and the settlers came in and started using them without care. The whites cut down pine trees that were a food source to the tribes, they dug big holes while mining for minerals, and they hunted the game of the area. The use of these limited resources caused tension between the whites and the Indians and settlers.

There are so much geographic treasures to see in Montana. The eastern part of Montana is considered the plains country where the sky is just never-ending. The central part is surrounded by mountain ranges while the western part is a combination of mountain ranges and valleys. The Yellowstone National Park is on the southern central portion of Montana. It has the massive area of geyser

The book RISING FROM THE PLAINS (1986) talks about how the Rocky Mountains had developed in Wyoming, McPhee was accompanied by David Love during this book. It was the first of the books “Annals of the Formal World” that talked about the effects of human beings, and how it complicates science. The book concentrates on how different parts of geology directly affects

The painting by Albert Bierstadt “Rocky Mountain, Lander’s Peak” is truly magnificent. Its high horizon line portrays a wide, vast piece of land containing a Native American village besides a lake, sitting below the mountains in the background. The atmospheric perspective is present here with the mountains being painted lighter, and not as detailed, than the rest of the painting. There is a pretty prominent presence of a one point perspective, with the vanishing point being the light, oasis-looking, waterfall in the distance. The colors vibrancy are dependent on the clouds in the sky, being it is clearly not a bright and sunny day, giving a more realistic feel to the whole composition. The focus point, the waterfall, is painted with bright

Daugneaux, Christine B. Appalachia: A Separate Place, A Unique People. Parsons: McLain Printing Company, 1981. Print.

Biggers referred to the Appalachia as, “the burning ground of industrial America; the region’s coal.” Coal was a vast reason why immigrants began to inhabit the area to work and families settled to make a living on the natural resources offered. It was not until the late 1800s, after the Civil War when cotton mills became established and “outside corporations and entrepreneurs, tied their hopes for prosperity to the whirling of spindles and the beating of looms.” Jacquelyn Hall, Luke a Family: The Making of the Southern Cotton Mill World.

Traditionally the Western Shoshone Nation’s ancestral land covers an area spanning from southern California, clear through Nevada, and barely touching southern Idaho. Within this scope of land is the previously mentioned Yucca Mountain, but also Mount Tenabo, a mountain in the Cortez Range of Northern Nevada, which is currently subject to mining. This large area of land is know as the Great Basin, where the habitat is dependent on the rain and snow melt water which comes off the high mountains, feeding the creeks which keep the living, living. Mount Tenabo is one such mountain; however it also holds a place in Shoshone creation stories, and is the site of ancient burials causing it to be of great importance to the entire nation of the Western Shoshone. The people of the Western Shoshone Nation still use the mountain to gather medical plants from these sacred places of their ancestors, and hold ceremonies.

On June 6, 1861 in a mountain, North of the Grand River a man and his crew were digging for gold. It was common for people to be look for gold because of the Gold Rush. The land they were in was a plan field near a mountain where there once used to be a field of buffalo . There was no buffalo because of the of the recent railroad construction. What also lead to the destruction of the land was the new people that started to moving into the indians territory. They started building new towns where rows of field used to be. This caused tension between the indians and the newly established people.

The partnership of Jacob and Sylvester Harpenau, officially named the Harpenau Brothers, began coal mining in St. Marks, Indiana. Due to the loss in production of coal in St. Marks, the Harpenau Brothers looked west toward St. Meinrad. The options for the partnership included the Abbey Mine; this mine provided coal as fuel to help piece together the enormous sandstone buildings at the Abbey in St. Meinrad. (Luecke 1) When the brothers went to see The Christmas Mine, located very close to the Abbey Mine, it was filled with water. They thought that if they could empty the mine by pumping out the water, they would potentially coal mine it. (Harpenau 2) Around the year of 1944, Jacob and Sylvester reopened the ironically named mine一 The Christmas

The area north of the Nantac Rim is typical of the Colorado Plateaus province (Broomfield & Shride, 1956). It is generally characterized by high elevation (average about 6,000 feet), and by the approximate horizontal position of its rocks. The drainage of this area is generally northward to the Salt and Black Rivers. The rivers and their principal tributaries have cut steep canyons into the plateau surface, making parts of the area almost inaccessible. Much of the area is