An Introduction to General Geography
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In our eReader you can find the full English version of the book. Read An Introduction to General Geography Online - link to read the book on full screen. Our eReader also allows you to upload and read Pdf, Txt, ePub and fb2 books. In the Mini eReder on the page below you can quickly view all pages of the book - Read Book An Introduction to General Geography
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Vicksburg and many other river ports on the Lower Mississippi are on such bluffs.
As the water flows around the curve the stream has a greater velocity around the concave bank than around the convex bank. Thus the concave bank will be undercut and steep while a deposit on the opposite side of the stream will cause the convex bank to shelve gently to the HIGH UtSJ3£R-Cur B/\*K Fig. 76.
water (Fig. 76). And, in general, we find that materials worn from the undercut concave bank are deposited at t...he next convex part lower down on the same bank. The tendency is therefore for the course to become more wind- ing, until whole loops are cut off.
If the land is elevated, or if the rainfall is increased, the river may cut its bed deeper into the flood plain, and as it finds its new lower level, swinging from side to side, it cuts away the greater part of its old flood plain, and builds up a new one at a lower level. Often portions of the old flood plain are left high up on the sides of the valley.
What to read after An Introduction to General Geography?
You can find similar books in the "Read Also" column, or choose other free books by Alec a Golding to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
Vicksburg and many other river ports on the Lower Mississippi are on such bluffs.
As the water flows around the curve the stream has a greater velocity around the concave bank than around the convex bank. Thus the concave bank will be undercut and steep while a deposit on the opposite side of the stream will cause the convex bank to shelve gently to the HIGH UtSJ3£R-Cur B/\*K Fig. 76.
water (Fig. 76). And, in general, we find that materials worn from the undercut concave bank are deposited at t...he next convex part lower down on the same bank. The tendency is therefore for the course to become more wind- ing, until whole loops are cut off.
If the land is elevated, or if the rainfall is increased, the river may cut its bed deeper into the flood plain, and as it finds its new lower level, swinging from side to side, it cuts away the greater part of its old flood plain, and builds up a new one at a lower level. Often portions of the old flood plain are left high up on the sides of the valley.
What to read after An Introduction to General Geography?
You can find similar books in the "Read Also" column, or choose other free books by Alec a Golding to read onlineMoreLess
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