The Mw 6.7, 1994 Northridge earthquake (NE) produced water-pipeline failures (WPF) in California's highly urbanized San Fernando Valley (SFV) and Sylmar Basin (SB). The causative fault was a south-dipping blind thrust, one of several that underlie the SFV in the Los Angeles Basin with little, if any, obvious geomorphic expression. Prior NE studies indicated WPF are a proxy for tectonic permanent ground deformations (PGD) and secondary shaking hazards including liquefaction, differential settlement, and slope failure (Johnson and Shlemon, 2013, 2015). To determine the specific causes for WPF, we employed the count-circle method (CCM). The CCM is a novel analysis used to calculate WPF densities with known x, y locations and z values that are equal to one. The CCM analysis involves constructing a study area grid of square cells. A circle is then placed over the center of four adjacent cells and WPF within the circle are counted. This is followed by shifting the circle west to east and south to north until all WPF are counted. Adjacent circles exceed the recommended minimum 50% overlap. The resulting CCM data are then machine contoured to construct the WPF isopleths. These isopleths also enclose several faults associated with ground rupture stemming from the nearby 1971 San Fernando, California earthquake and as well as from others that have no evidence of Holocene slip. The isopleth analysis shows that many regional pipeline failures were associated with PGD caused by multi-fault, hanging-wall triggered slip and epicentral area fracture zones unrelated to known geologic structures. From our WPF documentation in southern California, we suggest that CCM analysis of WPF is a useful tool to forecast potential infrastructure damage and lifeline failures stemming from future blind thrusts and associated hanging-wall deformation.
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