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Haroldson Lafayette Hunt Jr. (February 17, 1889 – November 29, 1974) was an American oil tycoon. [1] By trading poker winnings for oil rights according to legend, but more likely through money he gained from successful speculation in oil leases, he ultimately secured title to much of the East Texas Oil Field, one of the world's largest oil deposits.
Haroldson Lafayette Hunt Jr. was born on February 17, 1889, near Ramsey, Illinois. [3] During the 1930s, he bought the title for the East Texas Oil Field for $1,000,000, and became one of the eight richest Americans until his death on November 29, 1974, with a net worth between $300–700 million.
Hunt was born in El Dorado, Arkansas, but lived most of his life in Dallas, Texas. [4] He was the son of Lyda Bunker and oil tycoon H. L. Hunt, who set up Placid Oil, once one of the biggest independent oil companies, [5] He had six siblings: Margaret Hunt Hill (1915–2007), H. L. Hunt III (1917–2005), Caroline Rose Hunt (1923–2018), Lyda Bunker Hunt (born and died in 1925), William ...
The East Texas Oil Field is a large oil and gas field in east Texas. Covering 140,000 acres (57,000 ha) and parts of five counties, and having 30,340 historic and active oil wells, it is the second-largest oil field in the United States outside Alaska, and first in total volume of oil recovered since its discovery in 1930. [ 1 ]
The program, which issues permits for drawn hunts on both public and private lands throughout Texas, is now accepting applications for a shot at nearly 9,400 permits in more than 60 high-quality ...
East Texas is a broadly defined cultural, geographic, and ecological region in the eastern part of the U.S. state of Texas that comprises most of 41 counties. It is primarily divided into Northeast and Southeast Texas. Most of the region consists of the Piney Woods ecoregion. East Texas can sometimes be defined only as the Piney Woods. [1]
The East Texas iron ore belt spans several counties, including Cherokee, Upshur, Camp, Gregg, Harrison, and others. The geology of the region is dominated by the Weches greensand, which consists of glauconitic sand and clay. This greensand is underlain by various sedimentary formations, including the Queen City sand member and the Sparta sand.
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