Rising from the Plains by John McPhee is about an influential geologist, John David Love, interpreting the geologic history of Wyoming. The surface area of Wyoming has been subjected to many geological formations from the rise of the Rocky Mountains through the Laramide Orogeny in late Cretaceous time to the deep structural basin known as the Jackson Hole with rock dating back to the Precambrian period. Throughout each time period of the Earth’s history, the surface of Wyoming has experienced significant changes that have affected the physical landscape, as well as living organisms, even to this day. In this story John David Love shares his knowledge of the geologic history of Wyoming with John McPhee as they travel across Wyoming taking in the vastness that the landscape of Wyoming presents. The main theme in Rising from the Plains is the formation of the Rocky Mountains. “Topography grows, shrinks, compresses, spreads, disintegrates, and disappears” (McPhee 27). The physical features of the Earth are temporary and are always changing. The …show more content…
As mountain ranges began to reappear, streams and rivers became more vibrant with rushing waters transferring boulders and gravels to different places on the surface of Earth. Water is known to be one of the most significant factors of the Exhumation of the Rockies; however wind is thought to have played an important role in the removal of the mountains from the depths of debris as well. As John David Love has said, “Wind erosion has tremendous significance in this part of the Rocky Mountain region” (McPhee 60). Consistent southwest winds, blowing in the same direction throughout each time period of the Earth’s history, picked up thousands of feet of debris from the surface of the Earth and carried it away into the Atlantic Ocean. The work of erosion through water and wind has given the landscape its
Turner, Frederick Jackson. "The Significance of the Frontier in American History," Learner: Primary Sources. Annenberg Learner, Web. 25 Mar. 2014.
The population of a community is vital to ensure that the needs of that community are met. A greater population allows for a larger vote in a democracy meaning a higher probability of attaining what that population wants. Indigenous communities were left hopeless when European settlers took over and slashed the numbers of their community making it impossible for them to ever overpower the Canadian government. The book “Clearing the Plains” by James Daschuk explains this critical period of time in which the population of Indigenous people dwindled based on the political, economic and ecological circumstances that were evident creating a society where Indigenous people lost their say, however Daschuk fails to mention the effects this population deflation has on society today and the racism that our society has perpetrated on Indigenous people.
(“Facts about mountains for kids) (“Mountains - geography games and videos for kids.” ) Mountains influence the weather and climate around them immensely. They break up wind flows, so the wind either has to go above or around the mountains. The air that is forced up becomes cooler, and condenses into rain, snow, fog, or mist. (Simon, Seymour pg. 21) The western sides of mountains are typically much wetter than the eastern side where very little rain falls at all. This is caused by the rain shadow effect. (Simon, Seymour pg. 21) Mountains also have the ability to create rain forests and deserts. They store water and then release the water in the form of rivers that help with growth of vegetation. The rivers can be used as drinking water or they can be harnessed to create electricity. (Simon, Seymour pg. 27) Some mountains are more prominent in the world’s geography than others. There is a mountain on Mars, Olympus Mons, that is the tallest mountain on any planet on this solar system. Olympus Mons is 14 miles tall. (Hartston, William) The longest mountains are the Andes and the highest mountains are the Himalayas. (“Facts about mountains for kids”) ( Morris, Neil pg. 28) The Mid-Ocean Ridge is an underwater mountain chain that stretches 47,000 miles long. Not all of these mountains were formed in the same
Mackey, Mike. "Nellie Tayloe Ross and Wyoming Politics." Journal of the West 42(2003): 25-31, 33.
West, Elliott, Contested Plains: Indians, Goldseekers and the Rush to Colorado, (University Press of Kansas,
Because of westward expansion, America gained a significant amount of fertile land which contributed to the nation 's’ agrarian identity. The wilderness and landscape
Hess, D., McKnight, T. L., & Tasa, D. (2011). McKnight's physical geography (Custom ed. for California State University, Northridge ; 2nd Calif. ed.). New York: Learning Solutions.
Glaciers are an integral part of the world’s climate. In fact, as Richard Armstrong of the University of Colorado says, “Glaciers are key indicators in monitoring and detecting climate change” (Univ. of Colorado, Boulder, 2003, p. 1). Not only are they an important part of monitoring current climate, they can hold many keys to the past. Glaciers are in fact, “a source of paleoclimate data…” (Meier and Dyurgerov, 1980, p. 37). This paleoclimate data can give geologists information on the conditions that were present at the time of the glaciers birth, as well as the approximate age. This has an important role in the geologic time scale of the Colorado Rocky Mountains. These Glaciers played a role in the carving of the present day Rocky Mountains in Colorado, which will be the primary focus of this paper. In addition, glacial formations will be discussed to give the reader background information and the future of the Glaciers in Colorado will close this paper.
...to Americans: if their prospects in the East were poor, then they could perhaps start over in the West as a farmer, rancher, or even miner. The frontier was also romanticized not only for its various opportunities but also for its greatly diverse landscape, seen in the work of different art schools, like the “Rocky Mountain School” and Hudson River School, and the literature of the Transcendentalists or those celebrating the cowboy. However, for all of this economic possibility and artistic growth, there was political turmoil that arose with the question of slavery in the West as seen with the Compromise of 1850 and Kansas-Nebraska Act. As Frederick Jackson Turner wrote in his paper “The Significance of the Frontier in American History” to the American Historical Association, “the frontier has gone, and with its going has closed the first period of American history.”
Robbins, Jim. Last Refuge: The Environmental Showdown in Yellowstone and the American West. New York: Morrow, 1993. Print.
During the Late Cretaceous a period of mountain building occurred along the west coast of North America. This is called the Laramide orogeny that started the Rocky Mountains growth about seventy-five million years ago. The Laramide orogeny was different from orogenies that had happened before hand. What caused the Laramide Orogeny is uncertain but there are many theories about what caused it. One big thing to better understand the Laramide orogeny is the theory of Uniformitarianism.
The canyon is a part of what is now the Yellowstone National Park in Wyoming, an area of land first acquired through the Louisiana Purchase. In this painting, the observer may notice many features which stand out. In the background, the image depicts a large, rocky ravine, occupied by a river and rows of trees. The river leads to a large orb of light, presumably stemming from a fire. In the foreground, two men are seen standing on a cliff above the ravine, presumably in awe at the wondrous land they have just discovered in the distance. Behind the men is an untraveled area of
The drive to cross the Kentucky border had taken hours and hours of strenuous patience to finally arrive in another state. The view was by far country like as hints of cow manure could be smelled far from a distance. We drive through small towns, half the size of our hometown of Glen Ellyn had been the biggest town we've seen if not smaller. The scenery had overwhelmed us, as lumps of Earth from a great distance turned to perfectly molded hills, but as we got closer and closer to our destination the hills no longer were hills anymore, instead the hills had transformed to massive mountains of various sizes. These mountains surrounded our every view as if we had sunken into a great big deep hole of green pastures. Our path of direction was seen, as the trails of our road that had followed for numerous hours ended up winding up the mountainous mountains in a corkscrew dizzy-like matter.
The average elevation in the Hudson Plains is 120m above sea level. It is a flat lowland area. The land is made up of mineral soils, with few outcrops of underlying sandstone and shale. This land was created when the weight of glaciers depressed the Hudson Bay region and the ocean waters flooded areas up to 300 km inland from the current coastline. Then, during the retreat of the huge continental ice sheets, drainage into the Hudson Bay was blocked and lakes (Agassiz and Ojibway for example) were formed along th...
This area of the world is so foreign to my Oklahoma life; it infuses me with awe, and with an eerie feeling of being strongly enclosed by huge mountains, and the mass of tall trees. However, when my foot first steps onto the dusty trail it feels crazily magical. The clean, crisp air, the new smell of evergreen trees and freshly fallen rain is mixed with fragrances I can only guess at. It is like the world has just taken a steroid of enchantment! I take it all in, and embrace this new place before it leaves like a dream and reality robs the moment. As I turn and look at my family, I was caught by my reflection in their impressions. The hair raising mischief in the car was forgotten and now it was time to be caught up in this newness of life. It was as if the whole world around us had changed and everyone was ready to engulf themselves in it. The trickling of water somewhere in the distance and the faint noise of animals all brought the mountains to