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Sponsored by a grant from the National Science Foundation to the Denver Museum of Natural History. Ever wondered what the ground below you was like millions of years ago? Merging paleontology, geology, and artistry, Ancient Wyoming illustrates scenes from the distant past and provides fascinating details on the flora and fauna of the past 300 million years. The book provides a unique look at Wyoming, both as it is today and as it was throughout ancient history—at times a vast ocean, a lush rain forest, and a mountain prairie.
Big Horn City was the first town established in 1881 in what later became Sheridan County, Wyoming. Nestled in the foothills of the Big Horn Mountains, it is no wonder the Crow and Sioux Indian tribes coveted the Little Goose Valley for its abundance of wild game. Sheridan County's first white resident and founder of the town of Big Horn City was Oliver Perry Hanna. Numerous immigrants soon found their way to Big Horn City along the Bozeman Trail to begin a new life. The Bozeman Trail Museum, which serves as a place for local families to share their collectibles, was a blacksmith shop on the Bozeman Trail.
The riveting untold story of the fight for the Hudson River Valley, the decisive campaign of the Revolutionary War. No part of the country was more contested during the American Revolution than New York City and its surroundings. Military leaders of the time—and generations of scholars since—believed that the Hudson River Valley was America’s geographic jugular, which, if cut, would quickly bleed the rebellion to death. In Revolution on the Hudson, prize-winning historian George C. Daughan makes the daring new argument that this strategy would never have worked, and that dogged pursuit of dominance over the Hudson ultimately cost Britain the war. This groundbreaking naval history offers a thrilling response to one of our most vexing historical questions: How could a fledgling nation have defeated the most powerful war machine of the era?
An account of the birds of the Bighorn area of Montana, including descriptions of vegetation zones and bird distributions; notes on regional birding loops, birding locations, and site descriptions; species accounts; and a discussion of the zoogeographic significance and other ecological aspects of the bird life of the Bighorn Mountains.
Custer's defeat at the Battle of the Little Big Horn did its part to win fame for the Big Horn Basin, and much has been written about the famous characters of Wyoming. But until now the region which is Wyoming's last frontier has not received comprehensive treatment. This new study examines the Big Horn Basin during its frontier period. Isolated by Indian lands and impassable natural barriers, the Big Horn Basin remained a frontier for years after the frontier faded from other Western regions. The Indian Treaties of 1868 had left the Basin effectively encircled by Crow, Sioux, and Shoshoni Indians. The Yellowstone cordillera, Big Horn River and Wind River cut off travel on the west, east and south. Secluded and remote, the Big Horn Basin attracted only the most rugged and foolhardy, giving it a history distinct in the American saga. Trail breakers, fur traders and gold seekers, the first to open the Basin to settlement, are each highlighted. The efforts of Jedediah Smith, Charles Kemble, William Gordon, Robert Campbell, William Ashley and others were the first to blaze routes into the Basin for fur trade. There is much information on military expeditions and Indian encounters led by the likes of Lt. John Mullins, Lt. Henry E. Maynadier and Capt. William F. Reynolds, and Col. Nelson A. Miles. James Bridger, Edward Shelly, and the Expedition of 1870 figure prominently. The adventures of various prospectors are included. Stock growing entrepreneurs and alliances receive prime attention in this study. The disastrous winter of 1886-1887 and the Johnson County Invasion are described at length. Cattlemen Mason and Lovell, Torrey, and a great many others are discussed in a sweeping roster of who's who. Horse and cattle thieves, robbers and outlaws are discussed, including Hank Gorman, Charles and Ed Anderson, and Albert Nard. The lawmen who brought justice to Wyoming are also heralded here: Thomas R. Adams, Ed Lloyd, and Walter W. Peay among others. The railroad through the Big Horn Basin and its impact on a once impenetrable frontier are spotlighted. The importance of the Hill Line, Toluca Line, Lower Hanover Canal Project, and Wind River Canyon Dam are all brought to light. Water appropriation, the Carey Act, and other development, immigration and settlement projects-including Mormon settlements-are all addressed by Woods. Governor William Alford Richards, W. S. Collins, and W.D. Pickett's contributions are chronicled.
This comprehensive study of the geology and water resources of the Bighorn Basin in Wyoming is an essential resource for scientists, researchers, and policymakers. Drawing on decades of research and fieldwork, the author provides a detailed analysis of the basin's hydrology, geology, and mineral resources. Geology and Water Resources of the Bighorn Basin, Wyoming is a must-read for anyone interested in the science of hydrology and its practical applications. This work has been selected by scholars as being culturally important, and is part of the knowledge base of civilization as we know it. This work is in the "public domain in the United States of America, and possibly other nations. Within the United States, you may freely copy and distribute this work, as no entity (individual or corporate) has a copyright on the body of the work. Scholars believe, and we concur, that this work is important enough to be preserved, reproduced, and made generally available to the public. We appreciate your support of the preservation process, and thank you for being an important part of keeping this knowledge alive and relevant.
Fluvial and lacustrine-dominated clastic sedimentary rocks as thick as 1,800 m (6,000 ft) comprise the Paleocene Fort Union Formation and the Eocene Wasatch Formation of the western Powder River Basin in northeastern Wyoming and southeastern Montana. The systematic mineralogy of 45 samples of channel-fill sandstone from this sequence reflects the uplift and erosion of the Bighorn Mountains. Samples were collected to study vertical changes in the mineralogy of lower Tertiary sandstones adjacent to the Bighorn Mountains, lateral variations in the composition of the upper Paleocene Tongue River Member of the Fort Union Formation along the eastern front of the mountains, and variations in the composition of equivalent upper Paleocene sandstones of the central and western parts of the basin. Vertical changes in the mineralogy of a succession of Paleocene and Eocene sandstone units adjacent to the Bighorn Mountains most likely were produced by uplift and sequential erosion of the rocks that formerly overlaid the mountains. Uplift probably began in the middle Paleocene, during deposition of the Lebo Member of the Fort Union Formation, and continued into the Eocene. Differences in the mineralogy of the sandstone units along the western edge of the Powder River Basin that correspond to differences in the rock types now exposed along the crest of the Bighorn Mountains suggest that much of the erosional degradation of the Bighorn Mountains occurred during an early Tertiary tectonic episode. Lateral changes in the suite of unstable detrital grains within the Tongue River Member are compatible with facies and paleotransport studies that indicate a substantial eastward flux of detritus of early Tertiary age from the Bighorn Mountains into the central Powder River Basin.