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The Mississippi Bubble is a 1902 novel by American author Emerson Hough. It was Hough's first bestseller, and the fourth-best selling novel in the United States in 1902. [2] The historical novel revolves around the story of John Law (1671-1729) and the "Mississippi Bubble", an economic bubble of speculative investment in the French colony of ...
It was also popularly referred to as the Compagnie du Mississippi (lit. ' Mississippi Company ' ), for which the related stock market boom-and-bust was known as the Mississippi Bubble . The company was at the center of the broader monetary and fiscal scheme known as Law's System ( French : le système de Law ).
Mississippi's highest point is Woodall Mountain at 807 feet (246 m) above sea level adjacent to the Cumberland Plateau; the lowest is the Gulf of Mexico. Mississippi has a humid subtropical climate classification. Mississippi is known for its deep religious roots, which play a central role in its residents' lives.
Mississippi Delta – green line marks boundary. The Mississippi Delta, also known as the Yazoo–Mississippi Delta, or simply the Delta, is the distinctive northwest section of the U.S. state of Mississippi (and portions of Arkansas and Louisiana) that lies between the Mississippi and Yazoo rivers.
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Money and trade considered, with a proposal for supplying the Nation with money, 1934 French translation of 1712 English edition. Law was born into a family of Lowland Scots bankers and goldsmiths from Fife; his father, William, had purchased Lauriston Castle, a landed estate at Cramond on the Firth of Forth and was known as Law of Lauriston.
The Mississippi embayment is a physiographic feature in the south-central United States, part of the Mississippi Alluvial Plain. It is essentially a northward continuation of the fluvial sediments of the Mississippi River Delta to its confluence with the Ohio River at Cairo, Illinois .
An example of a deltaic lobe is the bird's-foot delta of the Mississippi River, pictured at right with its sediment plumes. As the deltaic lobe advances, the slope of the river channel becomes lower, as the river channel is longer but has the same change in elevation. As the slope of the river channel decreases, it becomes unstable for two reasons.