monday march 21, 2011
DESCRIPTION
Monday March 21, 2011. (Landforms Created by Glacial Erosion; Glacial Deposits). The Launch Pad Monday, 3/21/11. Why are most glaciers in the world today receding?. The Launch Pad Monday, 3/21/11. - PowerPoint PPT PresentationTRANSCRIPT
![Page 1: Monday March 21, 2011](https://reader036.vdocuments.mx/reader036/viewer/2022062302/56816449550346895dd61236/html5/thumbnails/1.jpg)
MondayMarch 21, 2011
(Landforms Created by Glacial Erosion; Glacial Deposits)
![Page 2: Monday March 21, 2011](https://reader036.vdocuments.mx/reader036/viewer/2022062302/56816449550346895dd61236/html5/thumbnails/2.jpg)
The Launch PadMonday, 3/21/11
Why are most glaciers in the world today
receding?
![Page 3: Monday March 21, 2011](https://reader036.vdocuments.mx/reader036/viewer/2022062302/56816449550346895dd61236/html5/thumbnails/3.jpg)
The Launch PadMonday, 3/21/11
More ice is melting every summer than can be replaced by
snowfall the next winter. This could be caused by a gradual
increase in world temperatures (global warming.)
![Page 4: Monday March 21, 2011](https://reader036.vdocuments.mx/reader036/viewer/2022062302/56816449550346895dd61236/html5/thumbnails/4.jpg)
Announcements??
![Page 5: Monday March 21, 2011](https://reader036.vdocuments.mx/reader036/viewer/2022062302/56816449550346895dd61236/html5/thumbnails/5.jpg)
Assignments For This Six-Weeks Date Issued Date DueVideo Quiz - Lakes, Rivers, and Other
Water Sources 2/27 2/27
WS - Running Water and Groundwater (Part 1) 2/25 3/4
PowerPoint Project – Rivers (P5 only) 2/28 3/3
WS - Running Water and Groundwater (Part 2) 3/2 3/9
Video Quiz - Groundwater 3/3 3/3
Cornell Notes - Ice 3/8 3/9
WS - Ice 3/9 ??
![Page 6: Monday March 21, 2011](https://reader036.vdocuments.mx/reader036/viewer/2022062302/56816449550346895dd61236/html5/thumbnails/6.jpg)
Continue Worksheet
Ice
![Page 7: Monday March 21, 2011](https://reader036.vdocuments.mx/reader036/viewer/2022062302/56816449550346895dd61236/html5/thumbnails/7.jpg)
Landforms Created by Glacial ErosionCertain types of special landforms can be created by glacial erosion. These include:
glacial troughs – As a glacier widens, deepens, and straightens a valley, it transforms a v-
shaped valley into a u-shaped glacial trough.hanging valleys – After a glacier has receded,
the valleys of tributary glaciers are left standing above the main glacial trough and are termed
hanging valleys.
![Page 8: Monday March 21, 2011](https://reader036.vdocuments.mx/reader036/viewer/2022062302/56816449550346895dd61236/html5/thumbnails/8.jpg)
Landforms Created by Glacial Erosion
cirques – a bowl-shaped depression at the head of a glacier that was a depression
where snow could accumulate, thus starting the formation of the glacier.arêtes – sharp-edged ridges that are
formed when cirques grow and the divide separating them becomes very narrow.
![Page 9: Monday March 21, 2011](https://reader036.vdocuments.mx/reader036/viewer/2022062302/56816449550346895dd61236/html5/thumbnails/9.jpg)
Landforms Created by Glacial Erosion
horns – several cirques surrounding a single mountain create the spires of rock
called horns.fiords - glacial troughs that became
submerged as the ice left the valley and sea levels rose following the Ice Age
![Page 10: Monday March 21, 2011](https://reader036.vdocuments.mx/reader036/viewer/2022062302/56816449550346895dd61236/html5/thumbnails/10.jpg)
Erosional Landforms Created by Alpine Glaciers
Figure 6.10 C
![Page 11: Monday March 21, 2011](https://reader036.vdocuments.mx/reader036/viewer/2022062302/56816449550346895dd61236/html5/thumbnails/11.jpg)
The Matterhorn in the Swiss Alps
Figure 6.12
![Page 12: Monday March 21, 2011](https://reader036.vdocuments.mx/reader036/viewer/2022062302/56816449550346895dd61236/html5/thumbnails/12.jpg)
Figure 6.10 (top right)
![Page 13: Monday March 21, 2011](https://reader036.vdocuments.mx/reader036/viewer/2022062302/56816449550346895dd61236/html5/thumbnails/13.jpg)
Figure 6.10 (middle right)
![Page 14: Monday March 21, 2011](https://reader036.vdocuments.mx/reader036/viewer/2022062302/56816449550346895dd61236/html5/thumbnails/14.jpg)
Figure 6.10 (bottom right)
![Page 15: Monday March 21, 2011](https://reader036.vdocuments.mx/reader036/viewer/2022062302/56816449550346895dd61236/html5/thumbnails/15.jpg)
Figure 6.11A
![Page 16: Monday March 21, 2011](https://reader036.vdocuments.mx/reader036/viewer/2022062302/56816449550346895dd61236/html5/thumbnails/16.jpg)
Figure 6.11B
![Page 17: Monday March 21, 2011](https://reader036.vdocuments.mx/reader036/viewer/2022062302/56816449550346895dd61236/html5/thumbnails/17.jpg)
Glacial DepositsGlaciers pick up and transport a huge load of debris as they slowly
advance across the land.Ultimately, these materials are deposited when the ice melts.
In regions where glacial sediment is deposited, it can play a significant role in forming the physical landscape.
Long before the theory of an extensive Ice Age was proposed, much of the soil and rock debris covering portions of Europe was recognized as
coming from elsewhere.At the time, these foreign materials were believed to have been
“drifted” into their present positions by floating ice during an ancient flood.
Therefore, the term drift was applied to this sediment.Today, glacial drift is a term for sediments of glacial origin, no matter
how, where, or in what form they were deposited.
![Page 18: Monday March 21, 2011](https://reader036.vdocuments.mx/reader036/viewer/2022062302/56816449550346895dd61236/html5/thumbnails/18.jpg)
Glacial DepositsTypes of Glacial Drift
Till refers to material that is deposited directly by ice.
![Page 19: Monday March 21, 2011](https://reader036.vdocuments.mx/reader036/viewer/2022062302/56816449550346895dd61236/html5/thumbnails/19.jpg)
Glacial DepositsTypes of Glacial Drift
Stratified drift is a sorted sediment deposited by meltwater.
![Page 20: Monday March 21, 2011](https://reader036.vdocuments.mx/reader036/viewer/2022062302/56816449550346895dd61236/html5/thumbnails/20.jpg)
Glacial DepositsTypes of Glacial Drift
Boulders found in till or lying free on the surface are called
glacial erratics if they are different from the bedrock
below.Erratics must have been
derived from a source outside the area where they are
found.