Latest Quake Info General Quake Info Hazards & Preparedness Earthquake Research You are here: Home Earthquake Research For teachers and students Slides Special Features Crustal Deformation Additional Resources Search Stress-Change Modeling Modeling Home page Online Publications Our work in the news Meet the team (our research, references,and vitae) The Northridge quake: 3 images to view and download a mm slides Wayne Thatcher Ross Stein G. Marshall and R. Stein, Serkan Bozkurt Bill Hammond A 3-slide set: maps of the Northridge, California, earthquak deformations, USGS Open File Report, 94-442, 1994. (revis Marleen Nyst Tom Parsons Fred Pollitz Chuck Wicks Visitors & Collaborators Aykut Barka Gerald Bawden Thomas Dewez Jian Lin Takuya Nishimura Shinji Toda Tim Wright earthquake struck on a 'blind thrust fault,' meaning that the fault is the earth's surface (see Stein and Yeats 1989 for examples). The fi aftershocks and ground cracking are shown. The surface faults act M=6.7 San Fernando earthquake are also shown. This event also s cutting faults thought to be active during the past 10,000 years are conceal blind thrust faults like the one that ruptured in the Northri The principal effects of the earthquake shaking are shown in the 'E distribution of 'red-tagged' buildings (damaged to the point where entry); bridge damage, landslides, ground cracking and surface fau sand and water shot to the surface), and the region in which the pe exceeded 0.4 g, the nominal design acceleration formerly used for The permannent ground movement is shown in the 'Deformation' Contours of predicted uplift are in blue and horizontal motions are deformation was measured by GPS receivers are red triangles.The uplifted 70 cm, or 2.3'. 3-Slides: Effects of the earthquake: [Preview 58kb] [High resolution 180kb] - Red tagged buildings - Landslides - Strong ground motion Tectonic and seismic setting of the quakes: [Preview 44kb] [High resolution 175kb] - main shock and aftershocks - known faults - previous surface ruptures The 35 mm slide set can also be mailed to you upon request free of The High resolution images can be used for PowerPoint presentatio images, for poster-size prints for instance, contact us. Technical details for the slides: Map Base: The digitally shaded relief was produced from the USGS 1: 100,000 (DEM). Roads are from the U.S. Tiger files. Active Faults are from Activity Map of California, California Division of Mines and Geolo Stein and R. S. Yeats, 1989, Hidden Earthquakes, Scientific Americ folds believed to be active during the past million years are depicted Effects of the 1994 M=6.7 Northridge, California, Earthquake S 1971 Surface Rupture corresponds to faulting associated wi San Fernando earthquake, from Charles W. Jennings (1975) Harp, E. L., and R. W. Jibson, Inventory of landslides trigge California earthquake, U.S. Geol. Surv. Open-File Rep., 95Holzer, T. L., M. J. Bennett, J. C. T. III, D. J. Ponti, and R. failure in alluvium during the Northridge, California, earthq U.S.-Japan Workshop on Earthquake Resistant Design of Li sures Against Soil Liquefaction, Tokyo: Nat. Cen. Earthqua Hecker, S., D. Ponti, C. Garvin, T. Powers, T. Fumal, J. Ham Prentice, and F. Cinti (1995). Ground deformation in Grana resulting from the January 17, 1994, Northridge, California, Open-File Rep. 95-62. Deformation of the 1994 M=6.7 Northridge, California, Earthq K.M. Hodgkinson, R.S. Stein, K.W. Hudnut, J. Satalich, and restoration of geodetic infrastructure caused by the 1994 No U.S. Geol. Surv. Open-File Report 96-517 [1996] (text, map internet at the site, http://www-socal.wr.usgs.gov/fema/. Hudnut, K. W., Z. Shen, M. Murray, S. McClusky, R. King, P. Fang, A. Donnellan, and Y. Bock ( 1996). Coseismic disp Northridge, California, earthquake, Bull. Seis. Soc. Amer., 8 Wald, D. J., T. H. Heaton, and K. W. Hudnut (1996). The sl California, earthquake determined from strong-motion, teles Bull. Seismol. Soc. Amer. , 86, S49-S70 , 1996. Damage associated with the Northridge, California, Earthquak Strong Shaking (peak horizontal acceleration > 0.4 g, or 40% contoured from roughly 50 strong ground motion stations by Borcherdt, Robert K. Mark, and David M. Boore (U.S.G.S., and in preparation. Strong motion recordings from Anthony Sacramento), Mihailo D. Trifunac (U.S.C.), and Ronald L. P Menlo Park and Pasadena). Severely Damaged Buildings are blocks or individual buildi by inspectors of the Federal Emergency Management Agenc Emergency Services, the City and County of Los Angeles, a Damaged (minor to major) and Collapsed bridges from Calt Transportation), Division of Structures, Post Earthquake Inv Buckle, I.G. (1994). The Northridge, California, earthquake Performance of Highway Bridges, Tech. Rep. NCEER-94-0 Res., Buffalo. Grant Marshall, now at SnapTrack, a QUALCOMM company, 675 Campbell CA, 95008, Homepage | Site Index | Contact Us | About Us | USGS E U.S. Geological Survey, Earthquake Hazards Program URL http://quake.wr.usgs.gov/research/deformation/modeling/ Page maintained by Serkan Bozkurt Contact: sbozkurt@usgs.gov Last modification: June 28, 2002