Cyrus C. Adams and others

Summary

Cyrus C. Adams and others The New International Encyclopædia (1905)

From the Falls of Saint Anthony to the junction with the Missouri, near Saint Louis, the river flows through a valley of great beauty and uniform fertility. Cliffs and rocky bluffs, from 200 to 300 feet high, give a picturesque character to that part of the valley below Rock Island, where it strikes the Carboniferous strata, the geological formation of the valley, to about 100 miles below the Missouri.
Source: Wikisource

Cyrus C. Adams and others The New International Encyclopædia (1905)

The mouth of the Red River brought several vexed questions before the commission, and the practical result of their conclusions will not be known until the works now in progress are completed. It is feared that the bed of the Atchafalaya, the present main outlet of the Red River, will enlarge sufficiently to convert the entire country between it and the Mississippi into an arm of the sea. The only safeguard seems to be by a series of dikes and submerged dams to turn the low-water flow of the Red River all into the Mississippi.
Source: Wikisource

Cyrus C. Adams and others The New International Encyclopædia (1905)

On the west side is also a wide bottom land, which extends almost continuously to the Gulf of Mexico, widening southward. On the east side the river impinges against the bluffs for some distance south of Natchez, but below the boundary between Mississippi and Louisiana bottom land appears again on this side of the river and rapidly widens toward the Gulf. The entire valley of the lower section of the river is margined by bayous or arms, which leave the main stream to rejoin it farther down, and considerable parts of Louisiana, Mississippi, and Arkansas are intersected by them.
Source: Wikisource

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