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Late Cenozoic stream incision and basin excavation have strongly influenced the modern Rocky Mountain landscape, but constraints on the timing and rates of erosion are limited. The geology of the Powder River basin provides an unusually good opportunity to address spatial and temporal patterns of stream incision. Numerous coal seams in the Paleocene Fort Union and Eocene Wasatch Formations within the basin have burned during late Cenozoic incision, as coal was exposed to dry and oxygen-rich near-surface conditions. The topography of this region is dominated by hills capped with clinker, sedimentary rocks metamorphosed by burning of underlying coal beds. We use (U-Th)/He ages of clinker to determine times of relatively rapid erosion, with the assumption that coal must be near Earth's surface to burn. Ages of 55 in situ samples range from 0.007 to 1.1 Ma. Clinker preferentially formed during times in which eccentricity of the Earth's orbit was high, times that typically but not always correlate with interglacial periods. Our data therefore suggest that rates of landscape evolution in this region are affected by climate fluctuations. Because the clinker ages correlate better with eccentricity time series than with an oxygen isotope record of global ice volume, we hypothesize that variations in solar insolation modulated by eccentricity have a larger impact on rates of landscape evolution in this region than do glacial-interglacial cycles. [ABSTRACT FROM AUTHOR]

Focuses on the laramide exhumation of the Bighorn Mountains in Wyoming. Preservation of a pre-Laramide partial retention zone; Temperature at the Cambrian unconformity; Sequences of sedimentary rocks.

View quality rating is an important component of land management that is still undergoing parameter definition and technical development.Methods enabling the efficient and accurate quantification of viewshed properties over large viewsheds using readily available data are particularly needed. This paper describes a procedure for measuring a suite of visual properties known to influence viewer preferences for hundreds of observation points in extensive Wyoming landscapes. Planimetric and panoramic simulations were used for quantifying appropriate viewshed parameters. These simulations were created in ArcInfo using USGS digital elevation data and satellite-derived landcover. The planimetric simulation was ideal for quantifying the dimensions of views (areal extent, depth, relief), but not adequate for quantifying thecomposition of views (landcover, diversity, and edge of landcover). Instead, a high correlation existed between panoramic estimates of landcover and equivalent images captured in the field (r2=0.97). The viewsheds examined in this study had large areal extents, large relief, extended depth, and naturalness, and may extend beyond the spatial scales for which view-quality concepts and preference relationships were developed. [ABSTRACT FROM AUTHOR]

Abstract: Redistribution of snow by wind is a defining feature of the physical environment in high-elevation upper treeline and alpine landscapes where most precipitation is snow and wind speeds are frequently high. In these landscapes, snow, wind, topography, and vegetation interact to produce a pattern of snow deposition where wind-driven snow is eroded from exposed areas and deposited on the lee sides of hills, trees, rocks, and other obstructions. During winters on Libby Flats, a broad, high-elevation ridge located in southeastern Wyoming, USA, snow is heterogeneously distributed with snow depths ranging from 0.1 to 7m over a lateral span of a few meters. Snow depth variations are principally controlled by the aerodynamic influence of trees on wind, with the deepest drifts forming on the lee sides of krummholz patches and ribbon forests. While precipitation varied from year to year, spatial patterns of snow scouring, drifting, and snowmelt were nearly identical. This characteristic and chronic pattern alters ecosystem structure (e.g., plant species distributions and soil characteristics) and function (e.g., decomposition, primary production, nutrient cycling, and water balance). To better comprehend and predict how ecosystem structure and function change with respect to snow distribution in treeline ecotones, an understanding of the snow transport process, ablation, and subsequent water distribution is required. Since snow accumulation and melt are difficult to observe spatially, we adapted and validated snow transport and land surface models to simulate the heterogeneous snow distributions produced during three consecutive water years (1998–2000). Comparisons of field measurements with model predictions indicate that the linked models generally mimicked the temporal and spatial characteristics of snow accumulation, redistribution, and ablation on Libby Flats. However, considerable modelled and observed discrepancies were associated with shallow or deep snow depths. Model agreement with observations could be improved with higher temporal resolution meteorological data, better resolved terrain and vegetation data, and model improvements. [Copyright &y& Elsevier]