The Center for Snow and Avalanche Studies serves the international mountain science community and regional water resource managers by hosting and conducting mountain system research and collecting integrative, real time, year-round mountain system observations. Mountain system research includes monitoring regional climate trends influential to snow melt, remote sensing of snowpack, snow and ice microstructure, and The Colorado Dust on Snow Program. Data includes information about weather, snowpack, radiation, soil, and hydrologic signals. By incorporating this research and information we are able to contribute to the understanding of water resource availability, from mountain snow, on a regional and global scale. CSAS does not forecast for avalanche hazard nor do we provide avalanche instruction. However, our resources and research do support avalanche science, forecasting, and education. Researching snow microstructure, and impacts of dust on snow, is valuable for the science of slab and weak layer formation.
Avalanche Launches API Partnership with Lead Wrench
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Investigated the remotely-triggered slide on the east face of Avalanche Peak. The slide released on a slope that faced from E to NE and broke 16 inches deep on a persistent weak layer of faceted snow that formed in mid-March. There is another persistent weak layer down nearly 3 feet that also looks concerning. Triggering a large persistent slab avalanche remains on the table on aspects facing E through N through NW. Enough cloud cover and cold temps to prevent snow surface from getting too wet, but solars still have a surface crust.
rock avalanche was radiocarbon dated to cal. Key words: Rock avalanche morphology, avalanche chronology, Schmidt-hammer estimate, dating of rock.
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What I Learned in Avalanche School
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In high mountainous areas worldwide, snow avalanches represent one of the main morphodynamic processes which influence the morphology.
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About this Archive
N2 – A tongue of very coarse rockslide debris that extends 1. Calculations based on frictional considerations imply that the feature is an excess-runout rock avalanche sturzstrom deposit. The morphological characteristics of the deposit appear consistent with movement by grainflow or fragmental flow.
For tree ring reduction dating we assumed that they produce reduced tree rings after the spruce trees were wounded, so that the age of the scar can be dated. A.
Comparative numerical surface exposure-age dating 10 Be and Schmidt hammer of an early-Holocene rock avalanche at Alstadfjellet, Valldalen, southern Norway. T1 – Comparative numerical surface exposure-age dating 10Be and Schmidt hammer of an early-Holocene rock avalanche at Alstadfjellet, Valldalen, southern Norway. N2 – Application of calibrated Schmidt-hammer surface-exposure dating SHD to the run-out debris of a rock avalanche at Alstadfjellet, Valldalen, southern Norway, has yielded ages that are consistent within uncertainties with terrestrial cosmogenic 10Be surface-exposure ages for the debris.
Three SHD calibration equations were generated based on different correction factors for the 10Be ages from the moraines. The SHD ages In addition, the former ages have a precision of 1. This work demonstrates that calibrated SHD can be of comparable accuracy to and may have improved precision over 10Be ages, and should be given greater consideration and prominence in Quaternary dating studies.
Colleagues pay tribute to mountaineer
The award celebrates well-known traditions, art forms and practices. Trained forecasters from all walks of life — from monks to housewives but increasingly the employees of ski areas and local communes – gather basic data on snow and weather conditions and the snowpack following traditional methods dating back over 70 years. Other countries have observer networks but the density of the Swiss network and level of training and expertise make it unique. The warning system is just one element.
36Cl surface-exposure dating of boulders of the avalanche mass indicates an event age of ± ka. A 14C age of ± cal yr BP of a palaeosoil within.