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31	Development of an Interpretive Document for the Bear River Migratory Bird Refuge Burbridge, William R. 01 May 1972 (has links) Since its inception, the National Wildlife Refuge System has been administered for management and restoration of habitat essential to the propagation and welfare of resident and wintering wildlife species. Acquisition of additional System units has been primarily directed to the benefit of the migratory bird resource. As of July 1, 1968 about 250 of the 321 refuge units were managed for the waterfowl resource (U. S. Department of Interior, 1968a). However, this growth of the System has been accompanied by an increase in recreational use of the refuges. In 1962, Public Law 87-714, the Refuge Recreation Act, was passed to provide direction for recreational development. The Act recognized that recreation must be limited in type and scope to avoid conflict with the primary wildlife management objectives. Although the primary function of the Refuge System is to meet the needs of wildlife, the entire System is based on the philosophical precept that the wildlife on these refuges is for the enjoyment of the public. It thus follows that refuges should provide for some public use. In recent analyses of America's resource picture, the fastest rising curves and projection are those of travel and the recreational use of wildlands (Clawson, 1963). Attendance records at our wildlife Refuges have grown at a rate of 12 percent annually. Except for boating and fishing at reservoir sites, the fastest growth in outdoor recreation since World War II has been in the use of National Wildlife Refuges (Clement, 1964). Bear River Migratory Bird Refuge Interpretive Document National Wildlife Refuge System Life Sciences Other Life Sciences
32	Seasonal Utilization of Sago Pondweed by Waterfowl at Bear River Migratory Bird Refuge, Utah Sterling, Michael R. 01 May 1970 (has links) Seasonal utilization of sago pondweed (Potamogeton pectinatus L.) by waterfowl was studied at Bear River Miqratory Bird Refuge by comparing amounts of sago production on a series of plots on Unit Four. One plot was available to carp and waterfowl; one only to carp; and one available to neither. The cage used to eliminate carp and waterfowl use of a plot caused a significant increase in sago production. The increase was attributed to less turbidity and less wind and wave action within the cage. Carp distribution was limited to deep-water portions of Unit Four, a small area, and they had no significant effect on sago production. Therefore, sago production from carp and open plots was compared to determine utilization of sago by waterfowl. Waterfowl utilization of sago in summer and spring was not significant; however, 52 percent of the tuber crop was used by waterfowl in fall. The method of study did not allow detection of waterfowl use of windrowed or submersed seed. Water depths between 2 and 10 inches had little or no effect on waterfowl use of tubers in fall; however depths between 5 and 14 inches in spring and 4 and 13 inches in summer may have prevented full use of tubers. Tubers were most available to ducks in the first 6 inches of soil but were utili zed to 8 inch depths. A series of 50 foot-square pens (2,500 square feet) were stocked with semi-domestic mallards to determine the effect of certain levels of utilization on sago growth. Sago seemed to recover well after heavy spring utilization. Results concerning the effect of summer utilization on production were not conclusive. Sago recovered well in spring after waterfowl had consumed 52 percent of the tuber crop the previous fall. Sago Pondweed Waterfowl Bear River bird refuge Utah wildlife resources Other Life Sciences
33	Utah Boating and Fishing Survey: Applying Contingent Valuation and Travel Cost Methods to Estimate Recreational Values in Northern Utah for the Bear River Water Development Project Williams, Jeff T. 01 May 1994 (has links) The intent of this thesis is to compare contingent valuation methods (CVM) and travel cost methods (TCM) to estimate consumer surplus for boaters and anglers in northern Utah. TCM results are about three times that of CVM. Several limitations are noted, specifically that CVM solicits given willingness to pay (WTP for specific reservoir sites. TCM analyzes aggregated trips to reservoirs with a wide array of site characteristics. Utah boating fishing contingent valuation travel cost methods recreational values Northern Utah Bear River Water development project Economics
34	Growth-Form-Analysis and Paleoecology of the Corals of the Lower Mississippian Lodgepole Formation, Bear River Range, North-Central Utah Miller, Judith M. 01 May 1977 (has links) The Mississippian (Kinderhookian-Osagean) Lodgepole Formation contains a diverse fossil assemblage. Taxa present include brachiopods, crinoids, gastropods, cephalopods, trilobites and corals. Corals and associated fauna were collected from four localities within the Bear River Range. These are, from north to south, Beirdneau Hollow, Spring Hollow, Leatham Hollow and Porcupine Dam. The well-preserved tabulate and rugose (compound and solitary) corals exhibit a high degree of morphologic variability. The colonial corals of the Lodgepole Formation (particularly Lithostrotionella, Syringopora) exhibit a morphologic gradient from platy to hemispherical forms. The six morphologic categories of colonial corals discussed in this study are identified by mean corallus diameter/corallum height ratios, by the corallite growth direction, and by the shape of the base of the colony. Type I corals have an average mean diameter/height ratio of 3.4; corallites are directed laterally away from the flat base. Type I corals are interpreted to have been adapted to offshore, quiet-water conditions. Type II corals are flattened hemispheres; they have an average mean diameter/height ratio of 4.1. Corallites are directed radially (i.e., with vertical as well as a lateral component) away from the flat colony base. Type II corals are interpreted in this study to have been adapted to shallow, moderately-turbulent environments in which vertical growth was inhibited. Type III corals have an average mean diameter/height ratio of 3.9 and are similar to Type II corals in all respects but one, namely that there is an absence of corallites on the crown of the corallum. This feature is called balding and is interpreted in this study to have been the result of desiccation and subsequent death of coral polyps. Type III corals are thus interpreted to have inhabited very shallow water wherein subaerial exposure of the crown of the corallum occurred during periods of exceptionally low tides. Type IV corals are dome-shaped or slightly-flattened hemispheres; they have an average mean diameter/height ratio of 2.3. Corallites are directed radially away from the flat base. Type IV corals are interpreted to have inhabited a depth zone intermediate between that of Type II corals (within or barely below tidal range) and Type I corals (near or below wave base). The average mean diameter/height ratio of Type V corals is 1.7. Corallites are directed almost entirely vertically away from the rounded-to-conical colony base. Type V corals are interpreted to have inhabited areas where sedimentation rates were sufficiently high to encourage vertical growth to the virtual exclusion of lateral growth. Type VI corals are composite corals, consisting of combinations of hemispherical forms and platy forms. This morphologic type is characterized by a change in the direction of growth during the astogenetic development of colony. The combinations of varying growth forms presumably reflect fluctuations in sedimentation rate. growth form analysis paleoecology corals lower mississipian lodgepole fomration bear river range north Utah Central Utah Geology
35	Ghost Water Exhibition Sharp, Michael G. 01 March 2017 (has links) The Ghost Water exhibition of artworks by Michael Sharp was comprised of four main works titled: 30 x 60 Minute Grid Series, Suspension, History/Prehistory, and Lake Bonneville Remnants. The artwork was created as a reaction to the land that once held the prehistoric Lake Bonneville and to its current remnant Great Salt Lake. The work explores the dialogue between absence and presence. Great Salt Lake Lake Bonneville Red Rock Pass Stockton Bar Old River Bed Steep Mountain Long Divide The Threshold Utah the West Great Basin Bear River Weber River Jordan River desert salt asphalt water railroad glass book arts artist books installation archive collection kallitype collotype photography printmaking letterpress ghost climate change Geology time pigment Land Art Erdlebenbildkunst panorama ink identity place grid cartography Art Practice

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