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American Cyclone
When Theodore Roosevelt entered national politics as the Republicans' nominee for the vice presidency in 1900, he was only forty-one years old. However, he had caught the public's attention with the popular version of his life story. Child of East Coast privilege. Sickly, bespectacled youth. Naturalist and author. Harvard graduate. New York assemblyman. Young widower. Badlands cowboy. Civil Service reformer. Urban police commissioner. Assistant Secretary of the Navy. Rough Rider and war hero. Enemy of political bosses as governor of the nation's most important state. Attentive husband to his second wife, Edith, and the father of six children. Few candidates for the presidency or vice preside...
Campaigns and Hurricanes
When William McKinley traveled to Mississippi in 1901, he became the first US president to visit the state while in office. Though twenty-four men served as president prior to McKinley, none of them included Mississippi in their travel plans. Presidents in the twentieth and twenty-first centuries have a better record of visiting Mississippi. There were forty-five presidential trips to the state between 1901 and 2016. Thirty-three communities hosted one or more of the sixty-nine stops the presidents made during those visits. George W. Bush is the unrivaled champion when it comes to the number and frequency of presidential visits. During eight years in office, he visited Mississippi nineteen t...
Geological Survey Bulletin
Nine uranium deposits occur in a small area west of Clancey, Jefferson County, Mont. These deposits are all in or near silicified fracture zones in quartz monzonite and related rocks of the Boulder batholith. The deposits contain pockets of uranium minerals in cavities in brecciated silicified rock. The primary uranium mineral pitchblende has been found in one pod. Secondary uranium minerals occur as fracture linings and in pore spaces in and adjacent to silicified zones. Uranium in the Clancey district was deposited probably during one of the later of at least four periods of silicification. The quartz monzonite, rather than the younger alaskitic dike rocks, is the host rock of the deposits.
