Loess Sheet in NW Michigan Essay

Published: 2020-02-17 09:51:55
355 words
2 pages
printer Print
essay essay

Category: Michigan

Type of paper: Essay

This essay has been submitted by a student. This is not an example of the work written by our professional essay writers.

Hey! We can write a custom essay for you.

All possible types of assignments. Written by academics

GET MY ESSAY
Soils of NW Michigan region have formed primarily in transported sediments such as glacial drift, loess, dune sand, and alluvium. Landforms associated with glacial melt water, such as outwash plains, eskers, and kames, are extremely commonplace in Michigan. Broad outwash plains, often containing abundant sand and gravel resources, dominate many Great Lakes landscapes, especially in the northern parts of the region. In the north, they are frequently covered by a blanket of loess, rendering the character of the soils on them silty rather than sandy (Garland 1955). Why is loess sheet located in NW Michigan?

Extensive loess sheet in NW Michigan illustrates river outwash processes. The main sources of loess sheet in NW Michigan are bare outwash deposits, till sheets, and floodplains along the windswept margins of advancing or retreating ice fronts, especially during the summer ablation season when outwash maximize and the landscape is neither frozen nor snow-covered. In many Michigan landscapes, the uppermost surficial deposit is a late Wisconsinan loess, the Peoria loess. In these areas, meltwaters ponded in front of the ice, allowing silts to settle out. Meltwater from the Outer Port Huron advance flowed into the Manistee River (Schaetzl 2007).

The Manistee River, therefore, is presumed loess source. Loess sheet in NW Michigan is wind-transported silt that is deposited as a poorly consolidated blanket whose thickness and grain size diminish downwind from source areas. As ice fronts retreated and vegetation invaded these source areas, loess deposition diminished and soil began forming. Loess accumulated through dry deposition of tropospheric dust (Garland 1955). Though readily observed on land, where it is trapped by plants and acquires cohesion from soil moisture and carbonate cementation, loess also settles through the water column of Lake Michigan.

Soils formed in the calcareous and nutrient-rich loess are typically highly fertile, though easily erodible by both wind and water. Bibliography Garland, John H. 1955. North American Midwest: A Regional Geography. Wiley: New York. Schaetzl, Randall J. 2007. The Buckley Loess Sheet in NW Lower Michigan: Evidence for a Manistee River Outwash Source. Geography, Michigan State University, [date last accessed 7 July 2008]. Available from World Wide Web: http://gsa. confex. com/gsa/2007AM/finalprogram/abstract_127735. htm

Warning! This essay is not original. Get 100% unique essay within 45 seconds!

GET UNIQUE ESSAY

We can write your paper just for 11.99$

i want to copy...

This essay has been submitted by a student and contain not unique content

People also read