Blind-thrust mapping report by United States Geological Survey Created 2026-10-24 Updated 2026-11-05
Primary technical report hosted by the United States Geological Survey. Numbered mapping features 4 and 5, “Active fold scarp” and “Syncline axis corresponding to the base of a fold forelimb”, explain how exposed deformation relates to a buried thrust. Hosting does not imply that every author is employed by the agency.
Institutional record of the 2008 primary study “Dependence of displacement-length scaling relations for fractures and deformation bands on the volumetric changes across them”. Its abstract gives linear scaling for shearing discontinuities under constant driving stress.
The Pacific Coastal and Marine Science Center's primary instrument description lists configurable acoustic sources and hydrophone acquisition, including boomer plates, sparkers and complementary chirp sub-bottom profiler equipment. It explains why the equipment configuration is chosen for target materials and imaging depth.
The institutional Earthquake Hazards Program page explains how disrupted young layers and unbroken overlying cover identify event horizons, and how ages above and below the affected horizon bracket a past earthquake. It distinguishes primary fault displacement from secondary shaking evidence.
Reusable locator for Table 1, “Geomorphic features associated with active faults”, in the primary mapping report Late Quaternary Faulting, Death Valley–Furnace Creek Fault System, California-Nevada, USGS Bulletin 1991. The normal-slip column lists scarps, faceted spurs, oversteepened mountain-front bases and rejuvenated valley floors. The official publication record confirms the report identity and 1991 publication year: pubs.usgs.gov/publication/b1991 .
Cited passages: aircraft laser returns, point-cloud representation and filtering vegetation and structures to construct a bare-earth digital elevation model. No publication date is inferred from the crawl date.