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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 ...
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 .
View of the camp of John Law at Biloxi, December 1720. The Mississippi Company (French: Compagnie du Mississippi; founded 1684, named the Company of the West from 1717, and the Company of the Indies from 1719 [1]) was a corporation holding a business monopoly in French colonies in North America and the West Indies.
Mississippi River-Gulf Outlet Canal The Mississippi River Alluvial Plain is an alluvial plain created by the Mississippi River on which lie parts of seven U.S. states , from southern Louisiana to southern Illinois (Illinois, Missouri, Kentucky, Tennessee, Arkansas, Mississippi, Louisiana).
The Mississippi bubble coincided with the South Sea bubble in England, which allegedly took ideas from it. Law was a gambler who would win card games by mentally calculating odds . He propounded ideas such as the scarcity theory of value [ 5 ] and the real bills doctrine . [ 6 ]
Mississippi is entirely composed of lowlands, the highest point being Woodall Mountain, at 807 ft (246 m) above sea level, in the northeastern part of the state. The lowest point is sea level at the Gulf Coast. The state's mean elevation is 300 ft (91 m) above sea level. Most of Mississippi is part of the east Gulf Coastal Plain.
Yale professor Robert Shiller correctly predicted the bubble in tech stocks at the turn of the millennium and the housing bubble in the middle part of the last decade, so he knows a little ...
The Mississippian is so named because rocks with this age are exposed in the Mississippi Valley. The Mississippian was a period of marine transgression in the Northern Hemisphere: the sea level was so high that only the Fennoscandian Shield and the Laurentian Shield were dry land.