Temporary movable plank houses for the students.
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Walter Mooney is a geophysicist in the Earthquake Hazards Program.
Walter Mooney is a research seismologist and geophysicist at the U.S. Geological Survey, Menlo Park, California (See video presentation). He is also a AGU member since 1974 (and Fellow since 1996). His major interest is global Earth crustal structure and tectonics, particularly of the continental lithosphere. Mooney was the branch Chief of Seismology from 1994 to 1997. He has led field work throughout North and South America and participated in extensive research affiliations with colleagues in Mexico, Europe, Russia, China and Taiwan, Japan, India, Australia, New Zealand, East Africa.
Mooney is a consulting Professor of Geophysics, Stanford University, and a visiting faculty at the following institutions: University of Karlsruhe and Kiel University, Germany, University of Paris and University of Strasbourg, France, Rice University, and the California Institute of Technology. Finally, he is the Program Leader for the USGS contribution to the Indian Ocean Tsunami Warning System and has extensive experience at leading training.
Sample of Videos Produced
San Francisco, California Bay Area Earthquake Hazards and Preparedness
Indian Ocean Tsunami Warning System (IOTWS)
The Wenchuan China Earthquake May 12, 2008, filmed by Sarah Bahan
Mauritius Training Program in Seismology and Tsunami Warning
The Earthquake of September 30, 2009 Padang, Indonesia
Tsunami Preparedness along the West Coast, USA
Temporary movable plank houses for the students.
Temporary movable plank houses for the students.
Damage to a village house.
Damage to a village house.
Damage to a village house.
Damage to a village house.
Damage to a local school building. Guozhang Middle School.
Damage to a local school building. Guozhang Middle School.
Damage to a local school building. Guozhang Middle School.
Damage to a local school building. Guozhang Middle School.
Total collapse of a reinforced building with masonry infill walls. Rubble has been disturbed by heavy equipment.
Total collapse of a reinforced building with masonry infill walls. Rubble has been disturbed by heavy equipment.
Landslide in the earthquake.
Landslide in the earthquake.
Students having class in temporary movable plank houses.
Students having class in temporary movable plank houses.
Timberwork house with "soft connection" has little damage during earthquake.
Timberwork house with "soft connection" has little damage during earthquake.
Timberwork house with wood embedded in cement wall has little damage during earthquake.
Timberwork house with wood embedded in cement wall has little damage during earthquake.
Emergency shelter camp for thirty families erected at the site of a former village.
Emergency shelter camp for thirty families erected at the site of a former village.
People next to the ruins.
People next to the ruins.
People next to the ruins.
People next to the ruins.
People next to the ruins.
People next to the ruins.
Damage to a village house.
Damage to a village house.
Damage to a village house. Gaojiabian, Lushan.
Damage to a village house. Gaojiabian, Lushan.
A real view of Port-au-Prince, Haiti, looking southeast with the port in the foreground and main city residences and other buildings showing as white in the center. Many of the neighborhoods with the heaviest destruction from the magnitude-7 earthquake that struck Haiti on Jan. 12, 2010 are included in this view.
A real view of Port-au-Prince, Haiti, looking southeast with the port in the foreground and main city residences and other buildings showing as white in the center. Many of the neighborhoods with the heaviest destruction from the magnitude-7 earthquake that struck Haiti on Jan. 12, 2010 are included in this view.
USGS seismoogists Dr. Walter Mooney completes the installation of a sensitive temporary seismograph to record earthquake aftershocks. The seismograph is installed in a small storage room in a small village. The cable leads to an outdoor antenna that provides accurate time via a GPS signal.
USGS seismoogists Dr. Walter Mooney completes the installation of a sensitive temporary seismograph to record earthquake aftershocks. The seismograph is installed in a small storage room in a small village. The cable leads to an outdoor antenna that provides accurate time via a GPS signal.
This young girl stands in front of a massive crack in the road on highway Nationale 2 near Petit Gaove, Haiti. The highway collapse was caused by lateral spreading of the underlying soil during the magnitude-7 earthquake that struck Haiti on Jan. 12, 2010.
This young girl stands in front of a massive crack in the road on highway Nationale 2 near Petit Gaove, Haiti. The highway collapse was caused by lateral spreading of the underlying soil during the magnitude-7 earthquake that struck Haiti on Jan. 12, 2010.
The epicenter of the magnitude-7 earthquake that struck Haiti on Jan. 12, 2010 is shown in this photo below the highest peak in the center of the view. The mapped Enriquillo fault zone comes towards the viewer in the low-lying hills and passes north (left) of the deforested clearing in the foreground.
The epicenter of the magnitude-7 earthquake that struck Haiti on Jan. 12, 2010 is shown in this photo below the highest peak in the center of the view. The mapped Enriquillo fault zone comes towards the viewer in the low-lying hills and passes north (left) of the deforested clearing in the foreground.
Massive rock slides were caused by strong ground shaking during the main shock of the magnitude-7 earthquake that struck Haiti on Jan. 12, 2010 and several of the stronger aftershocks. This mountain road leads north to the city of Dufort, located near the larger city of Leogane.
Massive rock slides were caused by strong ground shaking during the main shock of the magnitude-7 earthquake that struck Haiti on Jan. 12, 2010 and several of the stronger aftershocks. This mountain road leads north to the city of Dufort, located near the larger city of Leogane.
Temporary movable plank houses for the students.
Temporary movable plank houses for the students.
Damage to a village house.
Damage to a village house.
Damage to a village house.
Damage to a village house.
Damage to a local school building. Guozhang Middle School.
Damage to a local school building. Guozhang Middle School.
Damage to a local school building. Guozhang Middle School.
Damage to a local school building. Guozhang Middle School.
Total collapse of a reinforced building with masonry infill walls. Rubble has been disturbed by heavy equipment.
Total collapse of a reinforced building with masonry infill walls. Rubble has been disturbed by heavy equipment.
Landslide in the earthquake.
Landslide in the earthquake.
Students having class in temporary movable plank houses.
Students having class in temporary movable plank houses.
Timberwork house with "soft connection" has little damage during earthquake.
Timberwork house with "soft connection" has little damage during earthquake.
Timberwork house with wood embedded in cement wall has little damage during earthquake.
Timberwork house with wood embedded in cement wall has little damage during earthquake.
Emergency shelter camp for thirty families erected at the site of a former village.
Emergency shelter camp for thirty families erected at the site of a former village.
People next to the ruins.
People next to the ruins.
People next to the ruins.
People next to the ruins.
People next to the ruins.
People next to the ruins.
Damage to a village house.
Damage to a village house.
Damage to a village house. Gaojiabian, Lushan.
Damage to a village house. Gaojiabian, Lushan.
A real view of Port-au-Prince, Haiti, looking southeast with the port in the foreground and main city residences and other buildings showing as white in the center. Many of the neighborhoods with the heaviest destruction from the magnitude-7 earthquake that struck Haiti on Jan. 12, 2010 are included in this view.
A real view of Port-au-Prince, Haiti, looking southeast with the port in the foreground and main city residences and other buildings showing as white in the center. Many of the neighborhoods with the heaviest destruction from the magnitude-7 earthquake that struck Haiti on Jan. 12, 2010 are included in this view.
USGS seismoogists Dr. Walter Mooney completes the installation of a sensitive temporary seismograph to record earthquake aftershocks. The seismograph is installed in a small storage room in a small village. The cable leads to an outdoor antenna that provides accurate time via a GPS signal.
USGS seismoogists Dr. Walter Mooney completes the installation of a sensitive temporary seismograph to record earthquake aftershocks. The seismograph is installed in a small storage room in a small village. The cable leads to an outdoor antenna that provides accurate time via a GPS signal.
This young girl stands in front of a massive crack in the road on highway Nationale 2 near Petit Gaove, Haiti. The highway collapse was caused by lateral spreading of the underlying soil during the magnitude-7 earthquake that struck Haiti on Jan. 12, 2010.
This young girl stands in front of a massive crack in the road on highway Nationale 2 near Petit Gaove, Haiti. The highway collapse was caused by lateral spreading of the underlying soil during the magnitude-7 earthquake that struck Haiti on Jan. 12, 2010.
The epicenter of the magnitude-7 earthquake that struck Haiti on Jan. 12, 2010 is shown in this photo below the highest peak in the center of the view. The mapped Enriquillo fault zone comes towards the viewer in the low-lying hills and passes north (left) of the deforested clearing in the foreground.
The epicenter of the magnitude-7 earthquake that struck Haiti on Jan. 12, 2010 is shown in this photo below the highest peak in the center of the view. The mapped Enriquillo fault zone comes towards the viewer in the low-lying hills and passes north (left) of the deforested clearing in the foreground.
Massive rock slides were caused by strong ground shaking during the main shock of the magnitude-7 earthquake that struck Haiti on Jan. 12, 2010 and several of the stronger aftershocks. This mountain road leads north to the city of Dufort, located near the larger city of Leogane.
Massive rock slides were caused by strong ground shaking during the main shock of the magnitude-7 earthquake that struck Haiti on Jan. 12, 2010 and several of the stronger aftershocks. This mountain road leads north to the city of Dufort, located near the larger city of Leogane.