Cutoff Floodplain W Cutbank Point bar Neck
Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
Problem 1LR
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A. The modern floodplain of the Souris River near latitude , longitude can be identified by the flat area on both sides of the active stream channel. What other meandering stream features named in Fig. 12.13 do you recognize in this image?
![The 7.5-minute quadrangle map of Voltaire, North Dakota, includes part of the course of the
Souris River (Fig. A12.4.1). Part of a large continental ice sheet extended south and west from the
Hudson Bay area of eastern Canada during the Pleistocene Ice Age, covering this area. As the ice
sheet melted and became smaller, meltwater streams flowed where the ice had been, transporting
and depositing vast amounts of sediment. Streams have been forming and modifying this
landscape since the ice retreated, about 11,000-12,000 years ago.
Figure A12.4.1
48TH ST M
D Waley Cen
X
River
oo
Profile bax; 10x vertical exaggeration
RIVER AD M
47TH PAYN
457M TH
Visdo
Westgaard
North
vo
1:33,333
Contour interval 10 Feet
Y
-1650 ft
1600
+1550
-1500
RIVE H
5000.ft
1.km
IN ANY HAS](/v2/_next/image?url=https%3A%2F%2Fcontent.bartleby.com%2Fqna-images%2Fquestion%2Fee710977-90c8-4f84-9cb1-1102aa3efb9b%2F6acdb5ac-179e-4c01-be4d-896b6a424922%2Fshbxvt_processed.png&w=3840&q=75)
Transcribed Image Text:The 7.5-minute quadrangle map of Voltaire, North Dakota, includes part of the course of the
Souris River (Fig. A12.4.1). Part of a large continental ice sheet extended south and west from the
Hudson Bay area of eastern Canada during the Pleistocene Ice Age, covering this area. As the ice
sheet melted and became smaller, meltwater streams flowed where the ice had been, transporting
and depositing vast amounts of sediment. Streams have been forming and modifying this
landscape since the ice retreated, about 11,000-12,000 years ago.
Figure A12.4.1
48TH ST M
D Waley Cen
X
River
oo
Profile bax; 10x vertical exaggeration
RIVER AD M
47TH PAYN
457M TH
Visdo
Westgaard
North
vo
1:33,333
Contour interval 10 Feet
Y
-1650 ft
1600
+1550
-1500
RIVE H
5000.ft
1.km
IN ANY HAS
![Figure 12.13 A meandering river and its floodplain features.
Oxbow
-50 m
Cutoff
Floodplain
Floodplain
Abandoned channel
Cutbank
Point bar
Neck
The meandering channel of a small stream near Elko, Nevada, is typical of streams across a very broad range of
sizes, including the Mississippi River.](/v2/_next/image?url=https%3A%2F%2Fcontent.bartleby.com%2Fqna-images%2Fquestion%2Fee710977-90c8-4f84-9cb1-1102aa3efb9b%2F6acdb5ac-179e-4c01-be4d-896b6a424922%2Ftd70e0l_processed.png&w=3840&q=75)
Transcribed Image Text:Figure 12.13 A meandering river and its floodplain features.
Oxbow
-50 m
Cutoff
Floodplain
Floodplain
Abandoned channel
Cutbank
Point bar
Neck
The meandering channel of a small stream near Elko, Nevada, is typical of streams across a very broad range of
sizes, including the Mississippi River.
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