Winning the West for Christ: Sheldon Jackson and Presbyterianism on the Rocky Mountain Frontier, 1869-1880.

1998 ◽  
Vol 85 (1) ◽  
pp. 262
Author(s):  
James E. Fell Jr. ◽  
Norman J. Bender
Linguaculture ◽  
2019 ◽  
Vol 10 (1) ◽  
pp. 46-59
Author(s):  
Irina Chirica

This paper surveys the most significant ways in which the American West has been viewed as a place and region. Starting with Thomas Jefferson’s Louisiana Purchase of 1803, we follow the expansion of the West as a region throughout American history. Jefferson worked out a plan which involved the creation of territories which later became states, following a certain procedure. Inside the larger West, there are many Wests: the prairie states of the Midwest (also called the “Bread Basket” of America), the Rocky Mountain states, the Pacific Northwest, the Southwest and California. We analyze the myths and images associated with the west in American culture, and the influence of Frederick Jackson Turner’s essay dedicated to “the Frontier”. We discuss the New Historicism approach and the way in which it criticizes Tuner. Then we discuss the reflection of the West in the visual arts (the major landscape painters and in the work of the western movie director John Ford). We bring arguments to support the idea that the West is a construct of human experience and a cultural concept, more than a “place”.


Author(s):  
Amanda Rees

"Dude Ranch" is not an expression that carries a clear-cut meaning to everyone, for a dude ranch is neither a summer hotel nor a farm where dudes "ranch". . .. The most typical dude ranches of all the West are in this section of Wyoming. They range all the way from the most exclusive outfits that require references and advance reservations for not les than three weeks or a month at around $70 per week per person-including saddle horse and equipment, modern cabin, meals and other advantages-to the guest ranches or outfitters where accommodation may be had by the day, week or season. The person of moderate means can arrange his vacation in Jackson Hole to fit his purse. (Jackson Hole: Where to Go and What To See, published between 1929-1950) The American West is home to one of the most distinctive agricultural tourism activities in the world: dude ranching (Rees 2004). Dude ranching is the "single most unique contribution of the Rocky Mountain West to the ever-growing national vacation industry" (Roundy 1973), and it has been crucial in shaping the ways in which the West is perceived, working to effect continuing romantic notions of the American West (Rodnitzky, 1968). Though dude ranches can be found in the East (Zimmerman 1998), the South, the Southwest, California, Hawaii, and the Northwest, it is the Northern Rocky Mountain region, especially Montana and Wyoming, which forms the nucleus of dude ranch tourism (Rees 2005). However, unlike cattle ranching, agriculture, and mineral extraction, tourism has rarely received the attention it deserves in Wyoming, though it continues to be an important part of the Western image, as well as an important factor in the production and reproduction of that image. Just as dude ranching has failed to receive the attention it deserves in the state, it has also failed to receive that attention in one of the region's densest nexus or collection of dude ranching, Jackson Hole, and in particular, Grand Teton National Park (GTNP). Indeed, dude ranches have faired miserably in the first seventy-five years of the park's existence. As cultural landscapes dude ranches have been de­emphasized in favor of celebrating the natural environment. This project's research has revealed that a vast majority of the thirty-three dude ranches that once functioned in what is now GTNP have disappeared, been auctioned off, burned, pulled down, or allowed to rot in situ. In the last decade, critics of federal cultural resource management philosophy sought to reject this often-fragmented approach to cultural heritage protection, and looked to embrace environmental and cultural resources as an indivisible whole (Hufford 1994) and this research project falls within that effort to produce a narrative that embraces both environmental and cultural resources to tell a story of the ways in which humans and nature have interacted through tourism in GTNP.


1964 ◽  
Vol 1 (3) ◽  
pp. 184-205 ◽  
Author(s):  
C. H. Crickmay

The Rocky Mountain Trench is defined as the 1 000-mile valley which marks the west side of the Canadian Rocky Mountains. The background of the Trench as a problem is examined, and descriptions, geographical and geological, are given. Previous work on Trench origin is reviewed and note is taken of the seeming inapplicability of accepted erosion theories to the making of the erosion-made Trench. An hypothesis is offered in which the combined action of drainage hemmed in by bordering uplifts, guided headward erosion, lateral corrasion, and streams repeatedly reversed by continuing diastrophism is suggested as the excavator of the Trench, a valley characterized by the puzzling peculiarity of continuous depth without a consistent gradient.


1985 ◽  
Vol 22 (1) ◽  
pp. 108-125 ◽  
Author(s):  
Brian Wernicke

Geophysical studies suggest that the thin crust characteristic of the Basin and Range Province extends eastward beneath the west margin of the Colorado Plateau and Rocky Mountain regions. In Arizona and Utah, zones perhaps over 100 km wide may be defined, bounded on the west by the east limit of upper crustal normal faults that account for more that 10% extension and on the east by the east limit of thinning beneath the Colorado Plateau. A discrepancy exists within these zones between the negligible extension measurable in the upper crust and the substantial extension apparent from crustal thinning, assuming the "discrepant zone" crust was as thick as or thicker than the Colorado Plateau – Rocky Mountain crust prior to extensional tectonism.If various theories appealing to crustal erosion are dismissed, mass balance problems evident in the discrepant zones are most easily resolved by down-to-the-east normal simple shear of the crust, moving lower and middle crustal rocks that initially were within the zones up-and-to-the-west to where they now are locally exposed in the Basin and Range Province. West of the discrepant zones in both Arizona and Utah, east-directed extensional allochthons with large displacement are exposed. These geophysical and geological observations complement one another if it is accepted that the entire crust in both Arizona and Utah failed during extension on gently east-dipping, east-directed, low-angle normal faults and shear zones over a region several hundred kilometres wide.Large-scale, uniform-sense normal simple shear of the crust suggests the entire lithosphere may do the same. Such a hypothesis predicts major lithospheric thinning without crustal thinning will occur in plateau areas in the direction of crustal shear. In the case of the Arizona, Utah, and Red Sea extensional systems, and possibly the Death Valley extensional terrain, a broad topographic arch, typically 1500–2000 m higher than the extended terrain, is present, suggesting lithospheric thinning in areas predicted by the hypothesis.


1934 ◽  
Vol 66 (1) ◽  
pp. 1-6 ◽  
Author(s):  
Ferris Neave

The Purcell Range forms the easternmost portion of the Selkirk Mountains. It runs nearly north and south and is well marked off from other mountain ranges by the Rocky Mountain Trench on the east and the Purcell Trench on the west. The latter is occupied in part by Kootenay Lake. Even the broad geography of this range is imperfectly known as yet and its entomological resources are practically unknown.


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