TY - JOUR
T1 - Preliminary Observations of the 5 April 2024 Mw 4.8 New Jersey Earthquake
AU - Boyd, Oliver S.
AU - Barnhart, William D.
AU - Bourke, James
AU - Chapman, Martin
AU - Earle, Paul S.
AU - Huang, Guo Chin Dino
AU - Jobe, Jessica A.Thompson
AU - Kim, Won Young
AU - Link, Frederik
AU - Litherland, Mairi
AU - Lloyd, Andrew
AU - Long, Maureen D.
AU - McBride, Sara
AU - Michael, Andrew J.
AU - Mooney, Walter D.
AU - Mountain, Gregory S.
AU - Nikolaou, Sissy
AU - Savvaidis, Alexandros
AU - Waldhauser, Felix
AU - Wolfe, Cecily J.
AU - Yoon, Clara
N1 - Publisher Copyright:
© 2024. The Authors.
PY - 2024/10
Y1 - 2024/10
N2 - On 5 April 2024, 10:23 a.m. local time, a moment magnitude 4.8 earthquake struck Tewksbury Township, New Jersey, about 65 km west of New York City. Millions of people from Virginia to Maine and beyond felt the ground shaking, resulting in the largest number (>180,000) of U.S. Geological Survey (USGS) “Did You Feel It?” reports of any earthquake. A team deployed by the Geotechnical Extreme Events Reconnaissance Association and the National Institute of Standards and Technology documented structural and nonstructural damage, including substantial damage to a historic masonry building in Lebanon, New Jersey. The USGS National Earthquake Information Center reported a focal depth of about 5 km, consistent with a lack of signal in Interferometric Synthetic Aperture Radar data. The focal mechanism solution is strike slip with a substantial thrust component. Neither mechanism’s nodal plane is parallel to the primary northeast trend of geologic discontinuities and mapped faults in the region, including the Ramapo fault. However, many of the relocated aftershocks, for which locations were aug-mented by temporary seismic deployments, form a cluster that parallels the general northeast trend of the faults. The aftershocks lie near the Tewksbury fault, north of the Ramapo fault.
AB - On 5 April 2024, 10:23 a.m. local time, a moment magnitude 4.8 earthquake struck Tewksbury Township, New Jersey, about 65 km west of New York City. Millions of people from Virginia to Maine and beyond felt the ground shaking, resulting in the largest number (>180,000) of U.S. Geological Survey (USGS) “Did You Feel It?” reports of any earthquake. A team deployed by the Geotechnical Extreme Events Reconnaissance Association and the National Institute of Standards and Technology documented structural and nonstructural damage, including substantial damage to a historic masonry building in Lebanon, New Jersey. The USGS National Earthquake Information Center reported a focal depth of about 5 km, consistent with a lack of signal in Interferometric Synthetic Aperture Radar data. The focal mechanism solution is strike slip with a substantial thrust component. Neither mechanism’s nodal plane is parallel to the primary northeast trend of geologic discontinuities and mapped faults in the region, including the Ramapo fault. However, many of the relocated aftershocks, for which locations were aug-mented by temporary seismic deployments, form a cluster that parallels the general northeast trend of the faults. The aftershocks lie near the Tewksbury fault, north of the Ramapo fault.
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U2 - 10.1785/0320240024
DO - 10.1785/0320240024
M3 - Article
AN - SCOPUS:85206935154
SN - 2694-4006
VL - 4
SP - 240
EP - 250
JO - Seismic Record
JF - Seismic Record
IS - 4
ER -