Preview

Chapter 15 Test: Glaciers And Erosion Answers

Satisfactory Essays
Open Document
Open Document
378 Words
Grammar
Grammar
Plagiarism
Plagiarism
Writing
Writing
Score
Score
Chapter 15 Test: Glaciers And Erosion Answers
Chapter 15 Test: Glaciers and Erosion
Matching:
1. ________ pyramid-like peak made of arêtes A. snowfield
2. ________the unsorted material left beneath B. snowline the glacier when the ice melts
3. ________depressions where most outwash plains are pitted C. cirque
4. ________theory that most scientists now accept D. kettles
5. ________large cracks E. horn
6. ________masses of ice that occupy millions of square kilometers F. Milanokovitch Theory
7. ________an almost motionless mass of permanent snow and ice G.ground moraine
8. ________elevation above which ice and snow remain throughout H. crevasses the year
9. ________grainy ice I. continental ice sheets
10. ________bowl-shaped depression J. firn
…show more content…

The Great Lakes of North America are the result of a combination of erosion and deposition by continental ice sheets. ¬¬¬¬¬_______
12. When continental ice sheets recede, long ridges of gravel and course sand are absorbed on the way. ________
13. Snow accumulates year after year in polar regions and in the United States. _______
14. A snowline is an almost motionless mass of permanent snow and ice. ________
15. Glacial erosion may produce a bowl-shaped depression know as an esker. ________
16. A kettle is a mound. ______
17. A long period of climatic cooling during which continental sheets cover large areas of the earth’s surface is known as an ice age. ________
18. The composition of the water in a salt lake depends on the solved materials it contains.


You May Also Find These Documents Helpful

  • Good Essays

    Ap Chem Chapter 17 Outline

    • 4585 Words
    • 19 Pages

    • However, the initial concentration of the common ion (from the salt) must be considered.…

    • 4585 Words
    • 19 Pages
    Good Essays
  • Good Essays

    1. Calculate the temperature of the parcel at the following elevations as it rises up the wind-ward side of the mountain:…

    • 978 Words
    • 4 Pages
    Good Essays
  • Satisfactory Essays

    Deserts Lab Worksheet

    • 348 Words
    • 2 Pages

    Questions are from Geoscience Laboratory, 5th ed. (p. 268–278), by T. Freeman, 2009, New York, NY: John Wiley & Sons. Reprinted with permission.…

    • 348 Words
    • 2 Pages
    Satisfactory 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
  • Good Essays

    The glaciers that covered Michigan over one million years ago scraped the top layer of the landscape as they moved, carving landscapes throughout the land. As the glaciers melted, rivers streamed through the channels created by the glacier. The streams that formed from the glaciers spread the materials caught in the glacier throughout the land down south. The glaciers aimed to travel the least resistant path and thus the great lakes provided a great path, as they were riverbeds…

    • 937 Words
    • 4 Pages
    Good Essays
  • Satisfactory Essays

    Exam 2 Geology

    • 2092 Words
    • 9 Pages

    | Please read each question carefully before answering, Remember to submit the exam when you finish.…

    • 2092 Words
    • 9 Pages
    Satisfactory Essays
  • Good Essays

    Env Sci Help

    • 5433 Words
    • 22 Pages

    A) There are already hundreds of lakes in the northeastern United States and eastern Canada which are lifeless.…

    • 5433 Words
    • 22 Pages
    Good Essays
  • Good Essays

    One way to manage erosion is to eradicate the process of tilling. Tilling removes the soil from the top and exposes subsoil while burying the top soil. Presenting farmers with different methods that do not include the use of tilling would lower soil erosion. Surface cover and runoff are great ways to manage soil erosion. Surface cover prevents heavy showers from deteriorating the soil while runoff focuses on managing the flow of water at a down slope (Preventing and Managing Erosion,…

    • 724 Words
    • 3 Pages
    Good Essays
  • Satisfactory Essays

    2. Melted snow and Ice mixed with ash and rock created lahars a destructive mudflow on the slopes of a volcano…

    • 395 Words
    • 2 Pages
    Satisfactory Essays
  • Good Essays

    The individual area was also formed by the erosion and was filled by glacial melt water. Before the glacial erosion to the Ice Age, the Great Lakes were a plateau of ancient bedrock that had been eroding away for millions of years after an uplift of basin containing ancient seas. The Great Lakes Basin consists of ancient consolidated material. The bedrock is mainly covered in the Great Lakes Basin. The geological time scale and the geological map of the Great Lakes region can help understand the history of life in the Great Lakes region. The Great Lakes region has fossils located in different units of the geological time scale. The Precambrian Era depicts all of the time between the origin of the earth and the Cambrian period, when life first became abundant. Precambrian rocks haven’t been able to be depicted in the Great Lakes region because much of the original structure of the rocks has been changed by metamorphic processes and because billion of years erosion has removed a huge amount of materials. The Precambrian rocks almost enclosed the area around Lake Superior and extended over a large part of Lake Huron and Lake…

    • 851 Words
    • 4 Pages
    Good Essays
  • Better Essays

    About two million years ago we entered into the Pleistocene Epoch, an ice age that lasted until about 12,000 years ago and covered all of North America in over 6,000 feet of snow and ice. During this time, the temperatures went up and down causing the glaciers to melt or to expand, often times causing them to move. This carved the landscape of Michigan (Why). Glacial erosion can happen in two primary ways, the first is called plucking, and this happens when rocks and debris stick to the underside of a glacier and then are carried off with it. The second is called abrasion, this is more of what we might think on when we think of erosion, it’s what happens when two pieces of hard material scrape against each other. It is described almost as sanding the earth with a very large piece of sandpaper. When glaciers pick up a boulders or other debris and move it to another place, this is called glacial transportation. Often this transported debris has a different make up than the bedrock on which it has been distributed (Glacial erosion). These accumulations of glacial debris are called a moraines. Moraines are fairly common in Michigan and they are formed when a glacier either pauses for a good amount of time or begins to retreat. One remarkable moraine in Michigan is the Port Huron Moraine that is pictured below. Of course moraines are not the only landform in Michigan that has been shaped by glaciers (Moraines). There are many more landforms that are formed by glaciers. One in particular are drumlins. Drumlins are long features that can be up to 5 kilometers long and 50 meters high. One end usually has a very steep incline while the other end tapers off in an easy incline .The main theory on exactly how drumlins are formed is essentially that when a glacier becomes too overloaded with sediment and debris, that is deposits it in the form of a…

    • 1652 Words
    • 7 Pages
    Better Essays
  • Good Essays

    The Little Ice Age (LIA)

    • 1482 Words
    • 6 Pages

    The Little Ice Age (LIA) was a period of cooling where the world had all round colder temperatures than are experienced now in the 20th century, with Europe being, on average, 1.8℃ colder.…

    • 1482 Words
    • 6 Pages
    Good Essays
  • Good Essays

    Frost heave is the initial cause of patterned ground, and this process is a result of the summer months melting the top one metre of ice, called the active layer. This layer contains both water and mud, which both have different viscosities and therefore different specific heat capacities. During the three months of summer, when the active layer is visible, rocks will embed themselves into it. These rocks have a fairly high specific heat capacity in relation to ice, so the ice around it will be melted, and the process of percolation will cause a pool of water will form below the rock. As the temperature drops and the angle of incidence is further from the sun, the water will begin to freeze. Due to the chemistry of the water, it can freeze and expand when it drops below a certain temperature, around 0 degrees Celsius. Frozen water will take up a certain amount of space, and when it melts, 9% of the space it previously occupied will be disused. The melted water beneath the rock will expand when it freezes and fill up the extra 9% of space, however due to the fact there is a rock above it, the ice will force the rock upwards. As the stone ascends it pushes the finer sediment above it upwards too, creating a more compacted dome of finer material at the surface. This process is called frost heave. Consequently, the ground above the rock will be pushed upwards; creating a contour, but the ground around the land will stay the same. Inside the active layer the water is not equally spread throughout. In addition to this, there will be many rocks that are affected by frost heave, and all of…

    • 686 Words
    • 3 Pages
    Good Essays
  • Good Essays

    A Regelation Slip is another technique by which Glaciers can move; in this system the glacial ice moves towards a piece of outlying hard rock upon the bed rock, which results in friction being created. Subsequently, the increased friction increases the heat to a point at which it overcomes the Pressure Melting Point, ultimately melting the ice. The melt water created travels over the rocky outcrop to the lee, where the friction is at a much lower level, consequently causing the ice to re-freeze as the temperature of the melt water has dropped.…

    • 291 Words
    • 1 Page
    Good Essays
  • Better Essays

    Geography Landforms

    • 1071 Words
    • 5 Pages

    The Rock Lip is a feature of a corrie, and is formed during glaciation, where the ice was thinner, therefore less erosion took place. The rock lip dams the tarn.…

    • 1071 Words
    • 5 Pages
    Better Essays

Related Topics