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Geologic Hazards Science Center

The Geologic Hazards Science Center (GHSC), on the Colorado School of Mines campus, is home to the National Earthquake Information Center (NEIC), many scientists in the Earthquake Hazards Program and Landslide Hazards Program, as well as the Geomagnetism Program staff.

News

New USGS map shows where landslides are most likely to occur in U.S.

New USGS map shows where landslides are most likely to occur in U.S.

Un nuevo mapa del USGS muestra dónde es más probable que ocurran deslizamientos de tierra en el país

Un nuevo mapa del USGS muestra dónde es más probable que ocurran deslizamientos de tierra en el país

The scoop on what USGS hopes to find in a Summit County trench

The scoop on what USGS hopes to find in a Summit County trench

Publications

Challenging ring-current models of the Carrington storm

A detailed analysis is made of horizontal-component geomagnetic-disturbance data acquired at the Colaba observatory in India recording the Carrington magnetic storm of September 1859. Prior to attaining its maximum absolute value, disturbance at Colaba increased with an e-folding timescale of 0.46 hr (28 min). Following its maximum, absolute disturbance at Colaba decreased as a trend having an e-f
Authors
Jeffrey J. Love, Kalevi Mursula

RegionGrow3D: A deterministic analysis for characterizing discrete three-dimensional landslide source areas on a regional scale

Regional-scale characterization of shallow landslide hazards is important for reducing their destructive impact on society. These hazards are commonly characterized by (a) their location and likelihood using susceptibility maps, (b) landslide size and frequency using geomorphic scaling laws, and (c) the magnitude of disturbance required to cause landslides using initiation thresholds. Typically, t
Authors
Nicolas Wahde Mathews, Ben Leshchinksy, Benjamin B. Mirus, Michael J. Olsen, Adam M. Booth

Postfire sediment mobilization and its downstream implications across California, 1984 – 2021

Fire facilitates erosion through changes in vegetation and soil, with major postfire erosion commonly occurring even with moderate rainfall. As climate warms, the western United States (U.S.) is experiencing an intensifying fire regime and increasing frequency of extreme rain. We evaluated whether these hydroclimatic changes are evident in patterns of postfire erosion by modeling hillslope erosion
Authors
Helen Willemien Dow, Amy E. East, Joel B. Sankey, Jonathan Warrick, Jaime Kostelnik, Donald N. Lindsay, Jason W. Kean
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