Susan E. Hough
Susan Hough is a scientist in the Earthquake Hazards Program.
Science and Products
Filter Total Items: 100
Shaking intensity from injection-induced versus tectonic earthquakes in the central-eastern United States
Although instrumental recordings of earthquakes in the central and eastern United States (CEUS) remain sparse, the U. S. Geological Survey's “Did you feel it?” (DYFI) system now provides excellent characterization of shaking intensities caused by induced and tectonic earthquakes. Seventeen CEUS events are considered between 2013 and 2015. It is shown that for 15 events, observed intensities at epi
Authors
Susan E. Hough
The petroleum geologist and the insurance policy
In a recent study, Hough and Page (2015) presented several lines of evidence suggesting that most of the significant earthquakes in Oklahoma during the twentieth century, including the Mw 5.7 El Reno earthquake of 9 April 1952, were likely induced by wastewater injection and possibly secondary oil recovery operations. We undertook an archival search for accounts of this event, which unearthed a ne
Authors
Susan E. Hough, Morgan T. Page
The 1868 Hayward fault, California, earthquake: Implications for earthquake scaling relations on partially creeping faults
The 21 October 1868 Hayward, California, earthquake is among the best-characterized historical earthquakes in California. In contrast to many other moderate-to-large historical events, the causative fault is clearly established. Published magnitude estimates have been fairly consistent, ranging from 6.8 to 7.2, with 95% confidence limits including values as low as 6.5. The magnitude is of particul
Authors
Susan E. Hough, Stacey Martin
Strong-motion observations of the M 7.8 Gorkha, Nepal, earthquake sequence and development of the N-shake strong-motion network
We present and describe strong-motion data observations from the 2015 M 7.8 Gorkha, Nepal, earthquake sequence collected using existing and new Quake-Catcher Network (QCN) and U.S. Geological Survey NetQuakes sensors located in the Kathmandu Valley. A comparison of QCN data with waveforms recorded by a conventional strong-motion (NetQuakes) instrument validates the QCN data. We present preliminary
Authors
Amod Dixit, Adam T. Ringler, Danielle F. Sumy, Elizabeth S. Cochran, Susan E. Hough, Stacey Martin, Steven Gibbons, James H. Luetgert, John Galetzka, Surya Shrestha, Sudhir Rajaure, Daniel E. McNamara
A century of induced earthquakes in Oklahoma?
Seismicity rates have increased sharply since 2009 in the central and eastern United States, with especially high rates of activity in the state of Oklahoma. Growing evidence indicates that many of these events are induced, primarily by injection of wastewater in deep disposal wells. The upsurge in activity has raised two questions: What is the background rate of tectonic earthquakes in Oklahoma?
Authors
Susan E. Hough, Morgan T. Page
Ground motions from the 2015Mw 7.8 Gorkha, Nepal, earthquake constrained by a detailed assessment of macroseismic data
To augment limited instrumental recordings of the Mw 7.8 Gorkha, Nepal, earthquake on 25 April 2015 (Nepali calendar: 12 Baisakh 2072, Bikram Samvat), we collected 3831 detailed media and first-person accounts of macroseismic effects that include sufficiently detailed information to assign intensities. The resulting intensity map reveals the distribution of shaking within and outside of Nepal, wit
Authors
Stacey Martin, Susan E. Hough, Charleen Hung
Introduction to the focus section on the 2015 Gorkha, Nepal, earthquake
It has long been recognized that Nepal faces high earthquake hazard, with the most recent large (Mw>7.5) events in 1833 and 1934. When the 25 April 2015Mw 7.8 Gorkha earthquake struck, it appeared initially to be a realization of worst fears. In spite of its large magnitude and proximity to the densely populated Kathmandu valley, however, the level of damage was lower than anticipated, with most v
Authors
Susan E. Hough
The 21 May 2014 Mw 5.9 Bay of Bengal earthquake: macroseismic data suggest a high‐stress‐drop event
A modest but noteworthy Mw 5.9 earthquake occurred in the Bay of Bengal beneath the central Bengal fan at 21:51 Indian Standard Time (16:21 UTC) on 21 May 2014. Centered over 300 km from the eastern coastline of India (Fig. 1), it caused modest damage by virtue of its location and magnitude. However, shaking was very widely felt in parts of eastern India where earthquakes are uncommon. Media outle
Authors
Stacey Martin, Susan E. Hough
Shaking from injection-induced earthquakes in the central and eastern United States
In this study I consider the ground motions generated by 11 moderate (Mw4.0-5.6) earthquakes in the central and eastern United States that are thought or suspected to be induced by fluid injection. Using spatially rich intensity data from the USGS “Did You Feel It?” system, I show that the distance decay of intensities for all events is consistent with that observed for tectonic earthquakes in th
Authors
Susan E. Hough
Intraplate seismic hazard: evidence for distributed strain and implications for seismic hazard
No abstract available.
Authors
Susan E. Hough
Earthquake intensity distributions: a new view
Pioneering work by Nicolas Ambraseys and many collaborators demonstrates
both the tremendous value of macroseismic data and the perils of its uncritical assessment. In
numerous publications he shows that neglect of original sources and/or failure to appreciate
the context of historical accounts, as well as use of unreliable indicators such as landslid-
ing to determine intensities, commonly leads
Authors
Susan E. Hough
Crustal structure and fault geometry of the 2010 Haiti earthquake from temporary seismometer deployments
Haiti has been the locus of a number of large and damaging historical earthquakes. The recent 12 January 2010 Mw 7.0 earthquake affected cities that were largely unprepared, which resulted in tremendous losses. It was initially assumed that the earthquake ruptured the Enriquillo Plantain Garden fault (EPGF), a major active structure in southern Haiti, known from geodetic measurements and its geomo
Authors
Roby Douilly, Jennifer S. Haase, William L. Ellsworth, Marie‐Paule Bouin, Eric Calais, Steeve J. Symithe, John G. Armbruster, Bernard Mercier de Lépinay, Anne Deschamps, Saint‐Louis Mildor, Mark E. Meremonte, Susan E. Hough
Science and Products
Filter Total Items: 100
Shaking intensity from injection-induced versus tectonic earthquakes in the central-eastern United States
Although instrumental recordings of earthquakes in the central and eastern United States (CEUS) remain sparse, the U. S. Geological Survey's “Did you feel it?” (DYFI) system now provides excellent characterization of shaking intensities caused by induced and tectonic earthquakes. Seventeen CEUS events are considered between 2013 and 2015. It is shown that for 15 events, observed intensities at epi
Authors
Susan E. Hough
The petroleum geologist and the insurance policy
In a recent study, Hough and Page (2015) presented several lines of evidence suggesting that most of the significant earthquakes in Oklahoma during the twentieth century, including the Mw 5.7 El Reno earthquake of 9 April 1952, were likely induced by wastewater injection and possibly secondary oil recovery operations. We undertook an archival search for accounts of this event, which unearthed a ne
Authors
Susan E. Hough, Morgan T. Page
The 1868 Hayward fault, California, earthquake: Implications for earthquake scaling relations on partially creeping faults
The 21 October 1868 Hayward, California, earthquake is among the best-characterized historical earthquakes in California. In contrast to many other moderate-to-large historical events, the causative fault is clearly established. Published magnitude estimates have been fairly consistent, ranging from 6.8 to 7.2, with 95% confidence limits including values as low as 6.5. The magnitude is of particul
Authors
Susan E. Hough, Stacey Martin
Strong-motion observations of the M 7.8 Gorkha, Nepal, earthquake sequence and development of the N-shake strong-motion network
We present and describe strong-motion data observations from the 2015 M 7.8 Gorkha, Nepal, earthquake sequence collected using existing and new Quake-Catcher Network (QCN) and U.S. Geological Survey NetQuakes sensors located in the Kathmandu Valley. A comparison of QCN data with waveforms recorded by a conventional strong-motion (NetQuakes) instrument validates the QCN data. We present preliminary
Authors
Amod Dixit, Adam T. Ringler, Danielle F. Sumy, Elizabeth S. Cochran, Susan E. Hough, Stacey Martin, Steven Gibbons, James H. Luetgert, John Galetzka, Surya Shrestha, Sudhir Rajaure, Daniel E. McNamara
A century of induced earthquakes in Oklahoma?
Seismicity rates have increased sharply since 2009 in the central and eastern United States, with especially high rates of activity in the state of Oklahoma. Growing evidence indicates that many of these events are induced, primarily by injection of wastewater in deep disposal wells. The upsurge in activity has raised two questions: What is the background rate of tectonic earthquakes in Oklahoma?
Authors
Susan E. Hough, Morgan T. Page
Ground motions from the 2015Mw 7.8 Gorkha, Nepal, earthquake constrained by a detailed assessment of macroseismic data
To augment limited instrumental recordings of the Mw 7.8 Gorkha, Nepal, earthquake on 25 April 2015 (Nepali calendar: 12 Baisakh 2072, Bikram Samvat), we collected 3831 detailed media and first-person accounts of macroseismic effects that include sufficiently detailed information to assign intensities. The resulting intensity map reveals the distribution of shaking within and outside of Nepal, wit
Authors
Stacey Martin, Susan E. Hough, Charleen Hung
Introduction to the focus section on the 2015 Gorkha, Nepal, earthquake
It has long been recognized that Nepal faces high earthquake hazard, with the most recent large (Mw>7.5) events in 1833 and 1934. When the 25 April 2015Mw 7.8 Gorkha earthquake struck, it appeared initially to be a realization of worst fears. In spite of its large magnitude and proximity to the densely populated Kathmandu valley, however, the level of damage was lower than anticipated, with most v
Authors
Susan E. Hough
The 21 May 2014 Mw 5.9 Bay of Bengal earthquake: macroseismic data suggest a high‐stress‐drop event
A modest but noteworthy Mw 5.9 earthquake occurred in the Bay of Bengal beneath the central Bengal fan at 21:51 Indian Standard Time (16:21 UTC) on 21 May 2014. Centered over 300 km from the eastern coastline of India (Fig. 1), it caused modest damage by virtue of its location and magnitude. However, shaking was very widely felt in parts of eastern India where earthquakes are uncommon. Media outle
Authors
Stacey Martin, Susan E. Hough
Shaking from injection-induced earthquakes in the central and eastern United States
In this study I consider the ground motions generated by 11 moderate (Mw4.0-5.6) earthquakes in the central and eastern United States that are thought or suspected to be induced by fluid injection. Using spatially rich intensity data from the USGS “Did You Feel It?” system, I show that the distance decay of intensities for all events is consistent with that observed for tectonic earthquakes in th
Authors
Susan E. Hough
Intraplate seismic hazard: evidence for distributed strain and implications for seismic hazard
No abstract available.
Authors
Susan E. Hough
Earthquake intensity distributions: a new view
Pioneering work by Nicolas Ambraseys and many collaborators demonstrates
both the tremendous value of macroseismic data and the perils of its uncritical assessment. In
numerous publications he shows that neglect of original sources and/or failure to appreciate
the context of historical accounts, as well as use of unreliable indicators such as landslid-
ing to determine intensities, commonly leads
Authors
Susan E. Hough
Crustal structure and fault geometry of the 2010 Haiti earthquake from temporary seismometer deployments
Haiti has been the locus of a number of large and damaging historical earthquakes. The recent 12 January 2010 Mw 7.0 earthquake affected cities that were largely unprepared, which resulted in tremendous losses. It was initially assumed that the earthquake ruptured the Enriquillo Plantain Garden fault (EPGF), a major active structure in southern Haiti, known from geodetic measurements and its geomo
Authors
Roby Douilly, Jennifer S. Haase, William L. Ellsworth, Marie‐Paule Bouin, Eric Calais, Steeve J. Symithe, John G. Armbruster, Bernard Mercier de Lépinay, Anne Deschamps, Saint‐Louis Mildor, Mark E. Meremonte, Susan E. Hough