The Federal Emergency Management Agency (FEMA) developed a free software package (HAZUS) with the primary purpose to simulate the effects of earthquakes and other natural disasters in order to estimate potential regional damages and loss. Environmental Geology, fault, Denver, Colorado 80225. The full set of individual county- and fault-based HAZUS reports are also available as a single ZIP-file download. Imagine an earthquake centered near your city or town. The largest historical earthquake known in Colorado occurred on 7 November 1882. These estimates may be used by local, state and regional officials to 1) plan and stimulate risk-reduction efforts and 2) to prepare emergency response and recovery action plans. Open File Report. The New York Times Archives. Engineering Geology, pdf, 1801 Moly Road 967. We estimate that, had there been a more evenly distributed population, the 1882 earthquake would have been felt over an area of about 850,000 km2, with a corresponding moment magnitude (Mw) of 6.6 ?? This series of simulations are based on our current knowledge of historical earthquakes, their locations, and estimated magnitudes. This signup is not the same as your CGS Publications login.
From the USGS's Earthquake Hazards web site By studying the 1984 earthquake… publication,

Earthquake magnitude is estimated at 6.2 0.3 ML, based on felt area size. United States.

Therefore, there may be significant differences between the modeled results contained in this report and the actual social and economic losses following a specific earthquake. Monetary values are in either 2006 or 2013 dollars, depending on the date of the simulation (which appears on the report cover sheet). 1801 Moly Road Bulletin of the Seismological Society of America.

Share sensitive information only on official, secure websites. Earthquakes in Colorado. These will include notices for new blog entries, new publications, and the occasional geoscience event or news item of note. The possibility of there having been two earthquakes closely spaced in time at different locations was specifically addressed and no data supporting this theory was found. It was felt over 470,000 km, with a maximum reported Modified Mercalli intensity of VII. hazards, 0.6, at depths from shallow to mid-crustal, are possible throughout the Laramie Mountains and the Front Range, approximately from Casper, Wyoming, to Pueblo, Colorado. Fill out and submit this form so that we can send you information updates. Golden, Colorado 80401, e/ cgs_pubs@mines.edu “HA-70 HAZUS 2006: 1882 Fault Earthquake Event Report.” Earthquake Simulation. The primary aftershock of the 1882 earthquake was felt most strongly in the northern Front Range, leading Kirkham and Rogers (1985) to locate the epicenters of the aftershock and mainshock there. LockA locked padlock Hazards, earthquake, The simulations are based on either the Western US (WUS) or Central and Eastern US (CEUS) attenuation functions (see the USGS, A global summary report that tabulates losses based on the stated scenario conditions. Golden, Colorado 80401, e/ cgs_pubs@mines.edu Earthquake, Search for other works by this author on: GSW. OF-86-08D. Google Scholar. fema, Golden, CO: Colorado Geological Survey, 2006. Amy Zimmer, December 1, 2015. A microearthquake survey shows aftershocks to be just above the mainshock's rupture, mostly in a volume measuring 3 to 4 km across. this time. Interpretation of these reports also might be affected by ground-motion amplification from fluvial deposits and possible significant focal depth for the mainshock. Heerschap, Lauren, and Matthew L. Morgan. The dashed lines indicate zones of different levels of shaking. There are uncertainties inherent in any loss estimation technique. It was felt over 470,000 km, with a maximum reported Modified Mercalli intensity of VII. Each HAZUS historical-earthquake-based ZIP file includes a number of PDF files of individual reports that may or may not include: The PDF files may be navigated using the built-in bookmarks feature that may be seen to the left of an Adobe Acrobat (Reader) window. Knowledge of its size, location, and specific tectonic environment is important for the design of critical structures in the rapidly growing region of the Southern Rocky Mountains.

On November 7, 1882 an earthquake rocked parts of Colorado, Wyoming, Utah, and Kansas. t/ (+1) 303-384-2655, A set of worst-case scenarios replicating events of maximum intensity based on particular known historical earthquakes or faults. This high stress drop may explain why the earthquake was felt over an area about 3.5 times that expected for a shallow earthquake of the same magnitude in this region. The shaded oval on the map is is the felt area of the largest after-shock. ?2.7 km updip, with a corresponding average displacement of about 48 cm and average stress drop of about 180 bars.

Explore recent publications by USGS authors, Browse all of Pubs Warehouse by publication type and year, Descriptions of US Geological Survey Report Series, Rare, large earthquakes at the laramide deformation front - Colorado (1882) and Wyoming (1984), The Publications Warehouse does not have links to digital versions of this publication at mitigation, Golden, CO: Colorado Geological Survey, 2006. https://coloradogeologicalsurvey.org/publications/hazus-report-1882. Yes, earthquakes are certainly possible in Colorado, and on November 7, 1882,…. The Front Range is a geomorphic extension of the Laramie Mountains. pdf, More than one century later, on 18 October 1984, an mb 5.3 earthquake occurred in the Laramie Mountains, Wyoming. In the general earthquake model, the probabilistic ground motion and earthquake faults are developed from data supplied by the U.S. Geological Survey in Golden, Colorado.

1.0 km and to have ruptured ?? A .gov website belongs to an official government organization in the t/ (+1) 303-384-2655. Secure .gov websites use HTTPS This signup is not the same as your CGS Publications login. statewide. A set of worst-case scenarios replicating events of maximum intensity based on particular known historical earthquakes or faults. 63, No. Intensity map and felt area for the 1882 earthquake. Staff at the CGS assembled an Earthquake Reference Collection that brings together in one place more than 500 references that pertain broadly to seismicity, structural geology, faulting, and tectonics across the state of Colorado. earthquake, Knowledge of its size, location, and specific tectonic environment is important for the design of critical structures in the rapidly growing region of the Southern Rocky Mountains.
The only data for the 1882 earthquake were intensity reports from a heterogeneously distributed population. On November 7, 1882 an earthquake rocked parts of Colorado, Wyoming, Utah, and Kansas. zip. AN EARTHQUAKE IN COLORADO.

OF, These will include notices for new blog entries, new publications, and the occasional geoscience event or news item of note. hazus, Digital PDF download. Where would the most damage occur?

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