1996/02/01 by Edwin L. Harp, Randall W. Jibson · 368 citations
Earth and Planetary Sciences · Environmental Science · #Aerial photography #Archaeology #Block (permutation group theory) #Cryospheric studies and observations #Fire effects on ecosystems #Geography #Geology #Geomorphology #Landslide #Landslide classification #Landslides and related hazards #Remote sensing #Seismology #Slump
paper · doi:10.1785/bssa08601bs319
published in Bulletin of the Seismological Society of America 86(1B), S319-S332 (Seismological Society of America)
openalex publication_date 1996/02/01 · openalex created_date 2025/10/10 · openalex updated_date 2026/07/29
Abstract The 17 January 1994 Northridge, California, earthquake (Mw = 6.7) triggered more than 11,000 landslides over an area of about 10,000 km2. Most of the landslides were concentrated in a 1000-km2 area that included the Santa Susana Mountains and the mountains north of the Santa Clara River valley. We mapped landslides triggered by the earthquake in the field and from 1:60,000-nominal-scale aerial photography provided by the U.S. Air Force and taken the morning of the earthquake; these mapped landslides were subsequently digitized and plotted in a GIS-based format. Most of the triggered landslides were shallow (1- to 5-m thick), highly disrupted falls and slides within weakly cemented Tertiary to Pleistocene clastic sediment. Average volumes of these types of landslides were less than 1000 m3, but many had volumes exceeding 100,000 m3. The larger disrupted slides commonly had runout paths of more than 50 m, and a few traveled as far as 200 m from the bases of steep parent slopes. Deeper (>5-m thick) rotational slumps and block slides numbered in the tens to perhaps hundreds, a few of which exceeded 100,000 m3 in volume. Most of these were reactivations of previously existing landslides. The largest single landslide triggered by the earthquake was a rotational slump/block slide having a volume of 8 × 106 m3. Analysis of the mapped landslide distribution with respect to variations in (1) landslide susceptibility and (2) strong shaking recorded by hundreds of instruments will form the basis of a seismic landslide hazard analysis of the Los Angeles area.