scholarly journals Survey of Precise Leveling Array Grand Teton National Park

Author(s):  
Arthur Sylvester ◽  
Robert Smith

Fifteen permanent bench marks were established east and south of the existing 22 km-long line of 50 bench marks across the Teton normal fault in Grand Teton National Park to compare height changes of Jackson Hole relative to the Teton Range on the west and Shadow Mountain on the east. The new bench marks, together with three other agency bench marks and three temporary bench marks, constitute a 7. 8 km-long extension to the existing line tied to the old line at bench mark GT01. The new bench marks were precisely leveled between 30 August and 5 September 1994. Misclosure of the double-run survey was 0.86 mm, thus the precision of the total survey is 1 part in 10 million. If the misclosure is simply spread equally among the (n-1) bench marks, then the probable error associated with the relative height of a single bench mark is effectively zero.

Author(s):  
David Harwood ◽  
Kyle Thompson

Eight in-service teachers, one pre-service education student, three observers from other universities, and two instructors from the University of Nebraska-Lincoln engaged in an inquiry-based geology field course from June 13 to 28, 2015 through Wyoming, South Dakota, and Nebraska. This commnity of learners spent three days working in the Grand Teton National Park area. Geological features and history present in Grand Teton National Park are an important part of the course curriculum. Large-scale extensional features of the Teton Range and Jackson Hole, and the glacial geomorphology and related climate changes of this area are some of the unique features examined here.


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.


Author(s):  
Arthur Sylvester ◽  
Robert Smith ◽  
Christopher Hitchcock ◽  
John Byrd

The 55 km-long Teton normal fault at the eastern base of the Teton Range, Wyoming, has one the highest rates of Holocene slip of any fault in the Basin-Range, but it is seismically dormant at the M2 + level and presently lies in the center of a 50 km-long seismic gap (Byrd et al, 1993). Analyses of trenching, fault scarp heights, and fault proftles indicate earthquakes on the Teton fault are non­Poissonian, with from 5 to 10 M >7 earthquakes occurring from 7,900 to 14,000 years ago, but only two such events between 5,000 and 7,900 years ago, and none in the last 5,000 years (Byrd et al., 1994).


Author(s):  
Kenneth Barrick

Harrison R. Crandall (or "Hank" as he preferred; Fig. 1) is best known for his paintings and photographs of the Teton Range, and ranch scenes of Jackson Hole, Wyoming. However, Hank 's multi-faceted life, which spanned the period from 1887-1970, was far more interesting and important than is generally recognized. He was the first artist and commercial photographer to operate a studio in the Jackson Hole area, but he was also a valley homesteader, an important supporter and patron in the establishment of the Grand Teton National Park, and a pioneer concessionaire of the National Park art and souvenirs before the advent of mass tourism. Hank's natural artistic talent was accompanied by a complex personality - a mixture of the spirited individualism required of a mountain adventureer and dry-land homesteader, a loving and dedicated family man who promoted shared labor and leisure, and an environmentally attuned visionary who helped many to interpret the meaning of the Grand Teton National Park experience.


Author(s):  
Robert Smith ◽  
John Byrd ◽  
Ronald Bruhn ◽  
David Susong ◽  
Arthur Sylvester ◽  
...  

The Teton fault is a major, range-front normal fault that bounds the east side of the ~70 km-long Teton Range, located in northwestern Wyoming. It is an integral component of the 1,300 km-long Intermountain Seismic Belt, an active zone of intraplate seismicity that extends from southern Utah, northward through western Wyoming, eastern Idaho and western Montana. Geologically the Teton fault has evolved in the last 7 to 9 million years accumulating 6 to 9 km of displacement, concomitant with the development of the Basin-Range extensional tectonics in western Wyoming. In the past 5 to 8 million years, the nearby Yellowstone hotspot has likely influenced the activity of the fault including the timing and amount of slip on the fault. Quaternary scarps of the Teton fault extend for ~55 km, north-south along the east side of the Teton Range and provide excellent exposures of the Teton fault. The Teton fault is the primary structure responsible for producing more than 2,100 m (7,000 ft) of vertical topographic relief of the range front and is the single most important factor contribution to the spectacular topography and scenery of the Teton Range - hence to the essence of the Grand Teton National Park.


Author(s):  
David Harwood ◽  
Kyle Thompson

Eight in-service teachers and two instructors engaged in an inquiry-based geology field course from June 14 to 29, 2014 through Wyoming, South Dakota, and Nebraska. This team of learners spent three days in mid-June working in the Grand Teton National Park area. The UW-NPS facilities provide an excellent opportunity for participants to discover the natural history of the Teton Range, as well as close-out a few projects while sitting in a real chair, at a real table, a welcome change from our usual campground setting.


Author(s):  
Matt McGee ◽  
Stan Anderson ◽  
Doug Wachob

A study of coyote (Canis latrans) habitat use and mortality in Grand Teton National Park and the suburban-agricultural land surrounding Jackson, WY was conducted between September 1999 and August 2000. This research focused on the influence of human development, habitat type, topography, and simulated wolf presence on coyote habitat use and on coyote mortality patterns in undeveloped and suburban-agricultural land. The overall goal of this project was to provide baseline information on the coyote population in Jackson Hole that can be used in the future to determine what, if any, impact wolves and human developments may have on coyotes. There were a total of fifteen radio-collared coyotes in the suburban-agricultural area and fourteen radio collared coyotes in Grand Teton National Park and adjacent areas in the National Elk Refuge and Bridger-Teton National Forest. Marked coyotes were tracked weekly using short interval telemetry relocations and triangulation to determine habitat use patterns. During the winter, track transects were skied weekly and coyote trails were backtracked and mapped using hand held GPS units to determine fine scale habitat use patterns. Coyote mortality was determined via telemetry and direct observation. Preliminary data analyses suggest that coyotes use mainly sagebrush-grasslands or forest-shrub-grass edge areas and avoid forest interior areas. Coyotes frequently use trails and roads in the undeveloped area when moving long distances. Preliminary analysis also indicates that roads and trails are used in a greater proportion than their abundance on the landscape. Coyotes were frequently observed using riparian corridors to move between open meadows in the suburban-agricultural area. There is some evidence that suggests coyotes selectively travel fences and irrigation ditches for long distances in agricultural areas. The movement data also suggests that coyotes avoid developed areas during the day and travel in these developed areas at night. The data on coyote locations suggests some avoidance of wolf urine scent grids in the undeveloped area, but not in the developed area. Coyote mortality was primarily human caused, and coyotes that were male, transient, and lived in the suburban-agricultural area were the most commonly killed animals.


Author(s):  
Michael Smith ◽  
Jerrold Dodd ◽  
Paul Meiman

The Snake River plains and foothill areas of Jackson Hole have been grazed by domestic livestock since settlement of the area. Wildlife populations, including elk, mule deer, and antelope have historically used and continue to use the area. Moose are currently relatively abundant and a small herd of bison have been introduced. Currently, livestock use part of the area contained in Grand Teton National Park either as a concession or due to authorization by Park enabling legislation. Park managers need information concerning the effects of grazing by large ungulates on vegetation resources to assist in effectively managing grazing to service forage needs and achieve desired plant community goals.


Author(s):  
Mary Humstone

During summer 2010, the University of Wyoming American Studies Program conducted an intensive cultural landscape survey and historical analysis of the Elk Ranch in Grand Teton National Park. Led by Research Scientist Mary Humstone, students documented the ranch landscape and remaining buildings. They conducted research in local archives to uncover the history of the ranch and determine its significance in the history of Jackson Hole and Grand Teton National Park. The team determined that the property is eligible for the National Register of Historic Places, with significance in agriculture and conservation.


Author(s):  
A. Barnosky

Under the auspices of the U. S. Geological Survey and the University of Washington, detailed investigations of Miocene vertebrates and sediments in Jackson Hole, Wyoming commenced in 1979. Principal objectives of this research include: 1. Documenting the occurrence of mid-Tertiary mammals from Jackson Hole. Although fossils have been reported from Miocene rocks in the region (Love, 1956; Sutton and Black, 1972), existing collections are small. 2. Biostratigraphic correlation of isolated vertebrate localities throughout the northern Rocky Mountains with the superimposed localities in and near Grand Teton National Park. Such correlation will help determine whether regional or local tectonic events caused downwarping of Jackson Hole and uplift of the Teton Range. 3. Clarifying geographic variation of some small mammals through long periods of geologic time by comparison of West Coast (Rensberger, 1971, 1973;· Martin, 1979), Great Plains (Macdonald, 1963, 1970; Galbreath, 1953; Wilson, 1960), and the newly collected Jackson Hole faunas. This report summarizes accomplishments of the 1980 field season. Approximately one more season of field work and an ensuing year of data analysis are required before a final report will be available.


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