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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
Surface Ruptures of the M w 6.8 March 2011 Tarlay Earthquake, Eastern Myanmar
Twin‐Surface Ruptures of the March 2007 M >6 Earthquake Doublet on the Sumatran Fault
Interseismic Deformation and Earthquake Hazard along the Southernmost Longitudinal Valley Fault, Eastern Taiwan
Robert E. Wallace
Introduction to the Special Issue on the 2004 Sumatra–Andaman Earthquake and the Indian Ocean Tsunami
Rupture Kinematics of the 2005 M w 8.6 Nias–Simeulue Earthquake from the Joint Inversion of Seismic and Geodetic Data
Coseismic Slip and Afterslip of the Great M w 9.15 Sumatra–Andaman Earthquake of 2004
Geomorphic analysis of the Central Range fault, the second major active structure of the Longitudinal Valley suture, eastern Taiwan
Six similar sequential ruptures of the San Andreas fault, Carrizo Plain, California
A Structural Interpretation of the Aftershock “Cloud” of the 1992 M w 7.3 Landers Earthquake
A Structural Interpretation of the Aftershock “Cloud” of the 1992 M w 7.3 Landers Earthquake
Reply to “Comment on `A Vertical Exposure of the 1999 Surface Rupture of the Chelungpu Fault at Wufeng, Western Taiwan: Structural and Paleoseismic Implications for an Active Thrust Fault,' by Jian-Cheng Lee, Yue-Gau Chen, Kerry Sieh, Karl Mueller, Wen-Shan Chen, Hao-Tsu Chu, Yu-Chang Chan, Charles Rubin, and Robert Yeats,” by Yuan-Hsi Lee, Shih-Ting Lu, Tung-Sheng Shih, and Wei-Yu Wu
A Comparative Study of the Sumatran Subduction-Zone Earthquakes of 1935 and 1984
A Vertical Exposure of the 1999 Surface Rupture of the Chelungpu Fault at Wufeng, Western Taiwan: Structural and Paleoseismic Implications for an Active Thrust Fault
Late Quaternary activity and seismic potential of the Santa Monica fault system, Los Angeles, California
Modern Vertical Deformation above the Sumatran Subduction Zone: Paleogeodetic Insights from Coral Microatolls
Active parasitic folds on the Elysian Park anticline: Implications for seismic hazard in central Los Angeles, California
Active tectonics, paleoseismology, and seismic hazards of the Hollywood fault, northern Los Angeles basin, California
Stratigraphic evidence for seven meters of dextral slip on the San Andreas fault during the 1857 earthquake in the Carrizo Plain
Abstract From either the coast or the interior, Wallace Creek is most easily reached by way of California 58 (Fig.1). Precisely at the southwestern base of the Temblor Range, leave California 58 and drive southwest onan unmarked paved road about 0.2 mi (0.3 km) to a junction with an unpaved road (Fig.2). Turn left (south) on this road and follow the San Andreas fault to Wallace Creek.The unpaved road leading to Wallace Creekis impassable to all vehicles during and immediately following major storms.At all other times, two-wheel- or four-wheel-drive vehicles can be easily driven to within 1,300 ft (400 m) of the site. To avoid the gradual destruction of fragile tectonic landforms, park vehicles along the road near the section 33/34 boundary fence and walk theshort distance north to the fault. During the dry season, be careful not to park on dry, flammable vegetation.