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This document outlines a structured approach to log interpretation for analyzing geomorphic settings related to sedimentation, with a focus on earthquake evidence. Logs should record essential details such as the location and type of evidence, the quality assessment (poor, fair, good), the number of earthquakes, and their respective qualities. Additionally, it encourages speculation on paleoslip and magnitude. Notable evidence includes the North Frontal thrust fault identified in trenching through young alluvium, showcasing Holocene activity supported by radiocarbon dating.
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Logs for interpretation practice Things to record for each log: Interpretation of geomorphic setting of sedimentation overall Each piece of evidence for an earthquake: -location -type of evidence -quality (poor, fair, good) 3) Number of earthquakes and the quality of each 4) Speculation about paleoslip/magnitude
http://www.esp.geos.vt.edu/spotila/js-nfts.html Photo of the North Frontal thrust fault exposed in a trench through young alluvium. The 1.7 m dip-slip offset of a carbonate paleosol horizon is readily visible. This offset must postdate the age of detrital charcoal retreived from the hanging-wall one meter left of the tape measure, which we have dated with radiocarbon as 9.7 Ka. This demonstrates Holocene activity along the North Frontal thrust system.
http://www.geology.cwu.edu/facstaff/charlier/currentprojects/los_angeles_sum.htmlhttp://www.geology.cwu.edu/facstaff/charlier/currentprojects/los_angeles_sum.html
SW T4 NW Wall NE 0 1 m