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The disaster resilience value of shared rooftop solar systems in residential communities
Near-surface characterization using a roadside distributed acoustic sensing array
San Andreas Fault Exploration Using Refraction Tomography and S ‐Wave‐Type and F ϕ ‐Mode Guided Waves
Analysis of Landslide Kinematics Using Multi-temporal Unmanned Aerial Vehicle Imagery, La Honda, California
Evaluation of the Scaling Factor Bias Influence on the Probability of Collapse Using S a ( T 1 ) as the Intensity Measure
Seismic monitoring leveraging existing telecom infrastructure at the SDASA: Active, passive, and ambient-noise analysis
The 1868 Hayward Fault, California, Earthquake: Implications for Earthquake Scaling Relations on Partially Creeping Faults
A lithologic control on active meandering in bedrock channels
Retreat of a Coastal Bluff in Pacifica, California
Devil's Slide: An Evolving Feature of California's Coastal Landscape
Reassessment of the 1906 San Andreas Fault Rupture in Portola Valley, California, from Synthesis of Lidar and Historical Data
Determining the Diagenetic Conditions of Concretion Formation: Assessing Temperatures and Pore Waters Using Clumped Isotopes
Zircon U-Pb age of the Pescadero felsite: A Late Cretaceous igneous event in the forearc, west-central California Coast Ranges
Determining Soil–Tree–Grass Relationships in a California Oak Savanna Using Eco-Geophysics All rights reserved. No part of this periodical may be reproduced or transmitted in any form or by any means, electronic or mechanical, including photocopying, recording, or any information storage and retrieval system, without permission in writing from the publisher.
Design and Application of an Electromagnetic Vibrator Seismic Source
Abstract This field trip consists of two stops at locations where it is possible to see damage from the 1906 earthquake and to gauge the intensity of the ground shaking that caused the damage. The first stop is at a cemetery in Colma, where the damage to monuments and headstones was photographed and roughly quantified in the Report of the State Earthquake Investigation Commission , Lawson (1908), commonly referred to as the “Lawson Report.” The Lawson Report represents the formal study of the earthquake and consists of a compilation of the reports of many investigators who gathered information about faulting, ground failure, and damage due to the 1906 earthquake. The second stop is at a brick office building at the southern limit of San Francisco that was damaged by the earthquake but repaired in such a fashion that the damage is still clearly evident.