USGS Pasadena Earthquake Response Coordinator surveys displaced rocks near the southern end of the surface rupture of the 5 July 2019 M7.1 Ridgecrest earthquake. USGS photograph. Photo credit: Sue Hough, USGS
Susan E. Hough
Susan Hough is a scientist in the Earthquake Hazards Program.
Science and Products
The 1886 Charleston, South Carolina, Earthquake: Relic railroad offset reveals rupture
A study on the effect of site response on California seismic hazard map assessment
The 8 April 1860 Jour de Pâques earthquake sequence in southern Haiti
Contributed reports of widely felt earthquakes in California, United States: If they felt it, did they report it?
The 6 May 1947 Milwaukee, Wisconsin, earthquake
Which earthquake accounts matter?
The normal faulting 2020 Mw5.8 Lone Pine, Eastern California earthquake sequence
Revisiting California’s past great earthquakes and long-term earthquake rate
EERI earthquake reconnaissance report: 2019 Ridgecrest earthquake sequence
The 1933 Long Beach Earthquake (California, USA): Ground motions and rupture scenario
Where was the 31 October 1895, Charleston, Missouri Earthquake?
Poroelastic stress changes associated with primary oil production in the Los Angeles Basin, California
USGS Pasadena Earthquake Response Coordinator surveys displaced rocks near the southern end of the surface rupture of the 5 July 2019 M7.1 Ridgecrest earthquake. USGS photograph. Photo credit: Sue Hough, USGS
USGS Pasadena Earthquake Response Coordinator Sue Hough, surveys displaced rocks near the southern end of the surface rupture of the 5 July 2019 M7.1 Ridgecrest earthquake. Photo credit: Sue Hough, USGS
USGS Pasadena Earthquake Response Coordinator Sue Hough, surveys displaced rocks near the southern end of the surface rupture of the 5 July 2019 M7.1 Ridgecrest earthquake. Photo credit: Sue Hough, USGS
Following the devastating 2010 Haiti earthquake, the USGS has been helping with earthquake awareness and monitoring in the country, with continued support from the U.S. Agency for International Development (USAID).
Following the devastating 2010 Haiti earthquake, the USGS has been helping with earthquake awareness and monitoring in the country, with continued support from the U.S. Agency for International Development (USAID).
Following the devastating 2010 Haiti earthquake, the USGS has been helping with earthquake awareness and monitoring in the country, with continued support from the U.S. Agency for International Development (USAID).
Following the devastating 2010 Haiti earthquake, the USGS has been helping with earthquake awareness and monitoring in the country, with continued support from the U.S. Agency for International Development (USAID).
Following the devastating 2010 Haiti earthquake, the USGS has been helping with earthquake awareness and monitoring in the country, with continued support from the U.S. Agency for International Development (USAID).
Following the devastating 2010 Haiti earthquake, the USGS has been helping with earthquake awareness and monitoring in the country, with continued support from the U.S. Agency for International Development (USAID).
Following the devastating 2010 Haiti earthquake, the USGS has been helping with earthquake awareness and monitoring in the country, with continued support from the U.S. Agency for International Development (USAID).
Following the devastating 2010 Haiti earthquake, the USGS has been helping with earthquake awareness and monitoring in the country, with continued support from the U.S. Agency for International Development (USAID).
Traditional construction throughout Burma utilizes bamboo and other lightweight building materials, resulting in structures that are not generally durable but are quite earthquake-safe. As traditional structures such as this house give way to more modern masonry buildings, seismic risk will increase.
Traditional construction throughout Burma utilizes bamboo and other lightweight building materials, resulting in structures that are not generally durable but are quite earthquake-safe. As traditional structures such as this house give way to more modern masonry buildings, seismic risk will increase.
The Schwedagon pagoda, Burma's most revered shrine, has been damaged multiple times by earthquakes throughout its long history.
The Schwedagon pagoda, Burma's most revered shrine, has been damaged multiple times by earthquakes throughout its long history.
The historic record documents many instances of damage to pagodas throughout Burma's cities and the countryside. These ancient and beautiful structures bear witness to a significant level of seismic hazard.
The historic record documents many instances of damage to pagodas throughout Burma's cities and the countryside. These ancient and beautiful structures bear witness to a significant level of seismic hazard.
Burma's most populous city, Rangoon, is underlain by a thick blanket of soft sediments that will significantly amplify earthquake shaking. With a period of economic expansion on the horizon, new construction such as these buildings in the capital city will be potentially vulnerable to earthquake damage unless appropriate seismic provisions are adopted in the bu
Burma's most populous city, Rangoon, is underlain by a thick blanket of soft sediments that will significantly amplify earthquake shaking. With a period of economic expansion on the horizon, new construction such as these buildings in the capital city will be potentially vulnerable to earthquake damage unless appropriate seismic provisions are adopted in the bu
This photo was taken by USGS seismologist Susan Hough two months after the magnitude-7 earthquake struck Port-au-Prince on Jan. 12, 2010. Dr. Hough traveled to Haiti with USGS colleagues Doug Given, Mark Meremonte, and J. Zebulon Maharrey to install seismometers, which monitor the earth's movement and can detect and measure aftershocks.
This photo was taken by USGS seismologist Susan Hough two months after the magnitude-7 earthquake struck Port-au-Prince on Jan. 12, 2010. Dr. Hough traveled to Haiti with USGS colleagues Doug Given, Mark Meremonte, and J. Zebulon Maharrey to install seismometers, which monitor the earth's movement and can detect and measure aftershocks.
USGS seimologist Doug Given works with colleagues from the Bureau des Mines et de l'Energie to install a seismometer. Seismometers monitor the earth's movement and can detect and measure aftershocks. Given traveled to Haiti with USGS colleagues Susan Hough, Mark Meremonte, and J. Zebulon Maharrey shortly after a magnitude-7 earthquake struck on Jan. 12, 2010.
USGS seimologist Doug Given works with colleagues from the Bureau des Mines et de l'Energie to install a seismometer. Seismometers monitor the earth's movement and can detect and measure aftershocks. Given traveled to Haiti with USGS colleagues Susan Hough, Mark Meremonte, and J. Zebulon Maharrey shortly after a magnitude-7 earthquake struck on Jan. 12, 2010.
The Hotel Montana, shown here, is a portable seismometer site. USGS Seismologists Doug Given, Susan Hough, Mark Meremonte, and J. Zebulon Maharrey traveled to Haiti shortly after the magnitude-7 earthquake struck Port-au-Prince on Jan. 12, 2010 to install seismometers. Seismometers monitor the earth's movement and can detect and measure aftershocks.
The Hotel Montana, shown here, is a portable seismometer site. USGS Seismologists Doug Given, Susan Hough, Mark Meremonte, and J. Zebulon Maharrey traveled to Haiti shortly after the magnitude-7 earthquake struck Port-au-Prince on Jan. 12, 2010 to install seismometers. Seismometers monitor the earth's movement and can detect and measure aftershocks.
USGS seismologist Doug Given worked with colleagues from the Bureau des Mines et de l'Energie to install a seismometer. Seismometers monitor the earth's movement and can detect and measure aftershocks. Given traveled to Haiti with USGS colleagues Susan Hough, Mark Meremonte, and J.
USGS seismologist Doug Given worked with colleagues from the Bureau des Mines et de l'Energie to install a seismometer. Seismometers monitor the earth's movement and can detect and measure aftershocks. Given traveled to Haiti with USGS colleagues Susan Hough, Mark Meremonte, and J.
Science and Products
The 1886 Charleston, South Carolina, Earthquake: Relic railroad offset reveals rupture
A study on the effect of site response on California seismic hazard map assessment
The 8 April 1860 Jour de Pâques earthquake sequence in southern Haiti
Contributed reports of widely felt earthquakes in California, United States: If they felt it, did they report it?
The 6 May 1947 Milwaukee, Wisconsin, earthquake
Which earthquake accounts matter?
The normal faulting 2020 Mw5.8 Lone Pine, Eastern California earthquake sequence
Revisiting California’s past great earthquakes and long-term earthquake rate
EERI earthquake reconnaissance report: 2019 Ridgecrest earthquake sequence
The 1933 Long Beach Earthquake (California, USA): Ground motions and rupture scenario
Where was the 31 October 1895, Charleston, Missouri Earthquake?
Poroelastic stress changes associated with primary oil production in the Los Angeles Basin, California
USGS Pasadena Earthquake Response Coordinator surveys displaced rocks near the southern end of the surface rupture of the 5 July 2019 M7.1 Ridgecrest earthquake. USGS photograph. Photo credit: Sue Hough, USGS
USGS Pasadena Earthquake Response Coordinator surveys displaced rocks near the southern end of the surface rupture of the 5 July 2019 M7.1 Ridgecrest earthquake. USGS photograph. Photo credit: Sue Hough, USGS
USGS Pasadena Earthquake Response Coordinator Sue Hough, surveys displaced rocks near the southern end of the surface rupture of the 5 July 2019 M7.1 Ridgecrest earthquake. Photo credit: Sue Hough, USGS
USGS Pasadena Earthquake Response Coordinator Sue Hough, surveys displaced rocks near the southern end of the surface rupture of the 5 July 2019 M7.1 Ridgecrest earthquake. Photo credit: Sue Hough, USGS
Following the devastating 2010 Haiti earthquake, the USGS has been helping with earthquake awareness and monitoring in the country, with continued support from the U.S. Agency for International Development (USAID).
Following the devastating 2010 Haiti earthquake, the USGS has been helping with earthquake awareness and monitoring in the country, with continued support from the U.S. Agency for International Development (USAID).
Following the devastating 2010 Haiti earthquake, the USGS has been helping with earthquake awareness and monitoring in the country, with continued support from the U.S. Agency for International Development (USAID).
Following the devastating 2010 Haiti earthquake, the USGS has been helping with earthquake awareness and monitoring in the country, with continued support from the U.S. Agency for International Development (USAID).
Following the devastating 2010 Haiti earthquake, the USGS has been helping with earthquake awareness and monitoring in the country, with continued support from the U.S. Agency for International Development (USAID).
Following the devastating 2010 Haiti earthquake, the USGS has been helping with earthquake awareness and monitoring in the country, with continued support from the U.S. Agency for International Development (USAID).
Following the devastating 2010 Haiti earthquake, the USGS has been helping with earthquake awareness and monitoring in the country, with continued support from the U.S. Agency for International Development (USAID).
Following the devastating 2010 Haiti earthquake, the USGS has been helping with earthquake awareness and monitoring in the country, with continued support from the U.S. Agency for International Development (USAID).
Traditional construction throughout Burma utilizes bamboo and other lightweight building materials, resulting in structures that are not generally durable but are quite earthquake-safe. As traditional structures such as this house give way to more modern masonry buildings, seismic risk will increase.
Traditional construction throughout Burma utilizes bamboo and other lightweight building materials, resulting in structures that are not generally durable but are quite earthquake-safe. As traditional structures such as this house give way to more modern masonry buildings, seismic risk will increase.
The Schwedagon pagoda, Burma's most revered shrine, has been damaged multiple times by earthquakes throughout its long history.
The Schwedagon pagoda, Burma's most revered shrine, has been damaged multiple times by earthquakes throughout its long history.
The historic record documents many instances of damage to pagodas throughout Burma's cities and the countryside. These ancient and beautiful structures bear witness to a significant level of seismic hazard.
The historic record documents many instances of damage to pagodas throughout Burma's cities and the countryside. These ancient and beautiful structures bear witness to a significant level of seismic hazard.
Burma's most populous city, Rangoon, is underlain by a thick blanket of soft sediments that will significantly amplify earthquake shaking. With a period of economic expansion on the horizon, new construction such as these buildings in the capital city will be potentially vulnerable to earthquake damage unless appropriate seismic provisions are adopted in the bu
Burma's most populous city, Rangoon, is underlain by a thick blanket of soft sediments that will significantly amplify earthquake shaking. With a period of economic expansion on the horizon, new construction such as these buildings in the capital city will be potentially vulnerable to earthquake damage unless appropriate seismic provisions are adopted in the bu
This photo was taken by USGS seismologist Susan Hough two months after the magnitude-7 earthquake struck Port-au-Prince on Jan. 12, 2010. Dr. Hough traveled to Haiti with USGS colleagues Doug Given, Mark Meremonte, and J. Zebulon Maharrey to install seismometers, which monitor the earth's movement and can detect and measure aftershocks.
This photo was taken by USGS seismologist Susan Hough two months after the magnitude-7 earthquake struck Port-au-Prince on Jan. 12, 2010. Dr. Hough traveled to Haiti with USGS colleagues Doug Given, Mark Meremonte, and J. Zebulon Maharrey to install seismometers, which monitor the earth's movement and can detect and measure aftershocks.
USGS seimologist Doug Given works with colleagues from the Bureau des Mines et de l'Energie to install a seismometer. Seismometers monitor the earth's movement and can detect and measure aftershocks. Given traveled to Haiti with USGS colleagues Susan Hough, Mark Meremonte, and J. Zebulon Maharrey shortly after a magnitude-7 earthquake struck on Jan. 12, 2010.
USGS seimologist Doug Given works with colleagues from the Bureau des Mines et de l'Energie to install a seismometer. Seismometers monitor the earth's movement and can detect and measure aftershocks. Given traveled to Haiti with USGS colleagues Susan Hough, Mark Meremonte, and J. Zebulon Maharrey shortly after a magnitude-7 earthquake struck on Jan. 12, 2010.
The Hotel Montana, shown here, is a portable seismometer site. USGS Seismologists Doug Given, Susan Hough, Mark Meremonte, and J. Zebulon Maharrey traveled to Haiti shortly after the magnitude-7 earthquake struck Port-au-Prince on Jan. 12, 2010 to install seismometers. Seismometers monitor the earth's movement and can detect and measure aftershocks.
The Hotel Montana, shown here, is a portable seismometer site. USGS Seismologists Doug Given, Susan Hough, Mark Meremonte, and J. Zebulon Maharrey traveled to Haiti shortly after the magnitude-7 earthquake struck Port-au-Prince on Jan. 12, 2010 to install seismometers. Seismometers monitor the earth's movement and can detect and measure aftershocks.
USGS seismologist Doug Given worked with colleagues from the Bureau des Mines et de l'Energie to install a seismometer. Seismometers monitor the earth's movement and can detect and measure aftershocks. Given traveled to Haiti with USGS colleagues Susan Hough, Mark Meremonte, and J.
USGS seismologist Doug Given worked with colleagues from the Bureau des Mines et de l'Energie to install a seismometer. Seismometers monitor the earth's movement and can detect and measure aftershocks. Given traveled to Haiti with USGS colleagues Susan Hough, Mark Meremonte, and J.