Preview

Glacier And Desert Research Paper

Good Essays
Open Document
Open Document
815 Words
Grammar
Grammar
Plagiarism
Plagiarism
Writing
Writing
Score
Score
Glacier And Desert Research Paper
Deserts, Glaciers, and Climate
September 19, 2010
SCI/245

Deserts and Glaciers Deserts cover about one-third of the earth’s surface and have unique geologic features that cannot be found in more humid environments. The features found in deserts are mostly formed by wind and water erosion. Desserts are usually created because they are located in a dry region downwind of a mountain range caused by air losing its moisture as it passes over mountains, also known as a rain shadow. Rocks of different hardness and strength weather at different rates producing many of the unique shaped structures in found in the desert. There are many geological forms found in the desert, but here are a few of the unique ones. Arroyo is a dry gully, usually a small, narrow canyon with steep walls and flat, gravel floor. A butte is a narrow flat topped hill of resistant rock with very steep sides, which may have previously been a mesa.
…show more content…
A glacier is a large body of ice that is formed on land from the compaction and recrystallization of snow. Glaciers move slowly downhill due to gravity. The erosion features of a glacier can be extremely large or extremely small. As a glacier moves, its scours away material underneath it pulling up rocks, this is the material that is embedded in the ice at the base of a glacier. Though there are many landforms caused by glaciers but here are a few, cirque, crevasse, erratic, a kettle. A cirque is a bowl shaped depression carved out of a mountain by an alpine glacier. A crevasse is a deep, vertical crack that develops in the upper portion of glacier ice. Erratic is a large boulder that a glacier deposits on a surface made of different rock. And a kettle is a shallow, bowl shaped depression formed when a large block of glacial ice breaks away from the main glacier and is buried beneath glacial till, then melts. If the depression fills with water then it is called a kettle lake.

You May Also Find These Documents Helpful

  • Good Essays

    Soil and Glaciers

    • 630 Words
    • 3 Pages

    From Visualizing Earth Science, by Merali, Z., and Skinner, B. J, 2009, Hoboken, NJ: Wiley. Copyright 2009 by Wiley. Adapted with permission.…

    • 630 Words
    • 3 Pages
    Good Essays
  • Powerful Essays

    - Glaciers: large masses of ice on land that show evidence of being in motion or of once…

    • 3535 Words
    • 15 Pages
    Powerful Essays
  • Good Essays

    Geology 105 Study Guide

    • 1186 Words
    • 5 Pages

    9. a moving body of ice and snow, lying mostly on land. glaciers form where more snow accumulates in winter than melts in the summer.…

    • 1186 Words
    • 5 Pages
    Good Essays
  • Good Essays

    Striations are gouges on the bedrock. Bedrock is loose deposits of soil overlying rocks. Striations are made when a glacier moves over layers in which bedrock is contained. The glacier might have incorporated rocks and pebbles over time, so when the glacier moves through the bedrock the pebbles on the bottom of the glacier scratch the rock, and create…

    • 60 Words
    • 1 Page
    Good Essays
  • Satisfactory Essays

    This most influential glacier also created extremely steep valley walls and hanging valleys. When this glacier retreated, it most likely left waterfalls and a large lake that provided the sediments that cover up the U-shaped valley. After that glacier there were about two more but they were not as large. The last glaciation of Yosemite occurred only about 20,000 years ago and was not very big. When this last glacier retreated, it left moraines, Lake Yosemite, and waterfalls such as Yosemite Falls, Bridalveil Fall, Vernal Fall, and Nevada Fall. All of these landforms remain except for Lake Yosemite which was filled with sediment to cover the U-shaped valley even more. Currently, the Merced River runs through the valley. During all of this glacial…

    • 150 Words
    • 1 Page
    Satisfactory Essays
  • Satisfactory Essays

    -Attributes of deserts: low percipitation, high in mineral content, located leeward side of rain shadow…

    • 349 Words
    • 2 Pages
    Satisfactory Essays
  • Good Essays

    What if I told you that there was a place so harsh that only a handful of plants and animals can survive there? Well, there is and this place is called the tundra biome. This place is too harsh for most trees, too cold for large animals, and too isolated for most humans.…

    • 471 Words
    • 2 Pages
    Good Essays
  • Powerful Essays

    Mountaintop removal is currently the most commonly used form of mining throughout Appalachia and it has a significant impact on life there. These different effects are environmental, physical, mental, emotional, and economical. While mountaintop removal may be safer for the miners themselves, the big question is how mountaintop removal is affecting the very way of life of the people of Appalachia…

    • 1959 Words
    • 8 Pages
    Powerful Essays
  • Satisfactory Essays

    Approach to the subject of my paper: I will first introduce my paper with an explanation of what mountaintop removal is. Then, I will use my knowledge from working on the strip mining job. I will also discuss how mountaintop removal is not as bad as most people make it out to be.…

    • 434 Words
    • 2 Pages
    Satisfactory Essays
  • Better Essays

    Climate Change In Michigan

    • 1057 Words
    • 5 Pages

    Glaciers did have a large impact on the surface of Michigan over thousands of years by eroding land from one area and transporting it somewhere else to deposit. There are many examples within Michigan alone of glacial movement. Drumlins, formed by receding and then advancing glaciers, scrape and pushed elongated hills together on the surface of the earth. This erosion/deposit can be seen in Iron Mountain, Michigan (Wilson, p.6). Other landforms created by glaciers are moraines, eskers, and kames. Moraines occur when the ice is melting at an equal rate of the glacier advancing, and so dumping rocks, soil, debris taken from other areas the glacier has moved over, and even ice chunks fall off and can become buried under the other materials (Wilson, p. 6). So moraines are characterized by a rugged terrain often with high reliefs. When the ice melts, this creates depressions and makes for even more rugged area. In Michigan, this land form is…

    • 1057 Words
    • 5 Pages
    Better Essays
  • Good Essays

    Humans are evolving to interpret the world as a giant playground that they are inventing to make life more livable. Ski resorts are adapting to human desires for escapism. Skiers view the mountain as a journey, not so much as a destination. Virtually anywhere in the world, snow is generated due to scientific advances in machinery. Even though snow can be created through the means of science, does not mean it should. Despite the fact that fake snow is becoming a popular business market for the US and other foreign countries, real snow provides the skier with a more breath-taking experience.…

    • 536 Words
    • 3 Pages
    Good Essays
  • Satisfactory Essays

    bans on pitbulls

    • 476 Words
    • 2 Pages

    Ice land is a product of volcanic action along the north American and Eurasian tectonic plate…

    • 476 Words
    • 2 Pages
    Satisfactory Essays
  • Good Essays

    Mars has many of the kinds of surface features that are common on Earth. These include plains, canyons, and volcanoes. Overall, craters occur throughout the surface of Mars, while…

    • 572 Words
    • 2 Pages
    Good Essays
  • Better Essays

    Drumlins

    • 1981 Words
    • 8 Pages

    Drumlins are undoubtedly among the most intensively studied of all glacial landforms and have bee particularly widely used as ice-directional indicators. They frequently occur in ‘fields’ or ‘swarms’ in lowland areas where there was little obstruction to the passage of ice, or in piedmont zones where flow was radiative or dispersive. They are also occasionally found on the floors of glacial troughs. Many are ellipsoidal in form, some kilometres in length have been observed (Lemke 1958). Most possess a prominent stoss end with a trailing distal slope. It is generally agreed with the direction of the drumlin long axis reflects local direction of ice movement with the stoss end usually pointing up-glacier. The ice moulded or streamlined form appears to be produced by variations in stress levels at the base of the ice, although the precise mode of formation of the features is far from clear. The Kingscourt drumlins mentioned below gives a detailed account of the spatial characteristics and it’s internal components. ‘In addition to the regional ice flow trends displayed by their long axes, the overall shape of drumlins can provide information on former glacial dynamics, such as indications of basal ice pressure and rate and type of ice flow (Doornkamp and King 1971)’[1].…

    • 1981 Words
    • 8 Pages
    Better Essays
  • Good Essays

    Geology Notes

    • 1392 Words
    • 6 Pages

    The table below gives an idea how complex the Pleistocene really was. Ice advances and retreats in different areas are given different names because it is not always certain that they began at the same time everywhere.…

    • 1392 Words
    • 6 Pages
    Good Essays