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?
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.
"The History of Wyoming" explains detailed information of territorial and state developments. This second edition also includes the post-World War II chapters containing discussion about the economy, society, culture and politics not included on the previous edition.
Wyoming attorney John W. Davis retells the story of the West’s most notorious range war. Having delved more deeply than previous writers into land and census records, newspapers, and trial transcripts, Davis has produced an all-new interpretation. He looks at the conflict from the perspective of Johnson County residents—those whose home territory was invaded and many of whom the invaders targeted for murder—and finds that, contrary to the received explanation, these people were not thieves and rustlers but legitimate citizens. The broad outlines of the conflict are familiar: some of Wyoming’s biggest cattlemen, under the guise of eliminating livestock rustling on the open range, hire two-dozen Texas cowboys and, with range detectives and prominent members of the Wyoming Stock Growers Association, “invade” north-central Wyoming to clean out rustlers and other undesirables. While the invaders kill two suspected rustlers, citizens mobilize and eventually turn the tables, surrounding the intruders at a ranch where they intend to capture them by force. An appeal for help convinces President Benjamin Harrison to call out the army from nearby Fort McKinley, and after an all-night ride the soldiers arrive just in time to stave off the invaders’ annihilation. Though taken prisoner, they later avoid prosecution. The cattle barons’ powers of persuasion in justifying their deeds have colored accounts of the war for more than a century. Wyoming Range War tells a compelling story that redraws the lines between heroes and villains.
People of the Wind River, the first book-length history of the Eastern Shoshones, tells the tribe's story through eight tumultuous decades -- from 1825, when they reached mutual accommodation with the first permanent white settlers in Wind River country, to 1900, when the death of Chief Washakie marked a final break with their traditional lives as nineteenth-century Plains Indians. Henry E. Stamm, IV, draws on extensive research in primary documents, including Indian agency records, letters, newspapers, church archives, and tax accounts, and on interviews with descendants of early Shoshone leaders. He describes the creation of the Eastern political division of the tribe and its migration from the Great Basin to the High Plains of present-day Wyoming, the gift of the Sun Dance and its place in Shoshone life, and the coming of the Arapahoes. Without losing the Shoshone perspective, Stamm also considers the development and implementation of the federal Peace Policy. Generally friendly to whites, the Shoshones accepted the arrival of Mormons, miners, trappers, traders, and settlers and tried for years to maintain a buffalo-hunting culture while living on the Wind River Reservation. Stamm shows how the tribe endured poor reservation management and describes whites' attempts to "civilize" them. After 1885, with the buffalo gone and cattle herds growing, the Eastern Shoshone struggled with starvation, disease, and governmental neglect, entering the twentieth century with only a shadow of the economic power they once possessed, but still secure in their spiritual traditions.
