PPT-150 th Anniversary of the 1868 Hayward fault earthquake

Earthquake Country Alliance Cisco San Jose March 1 2018 SAFRR Science Application for Risk Reduction SAFRR Science Application for Risk Reduction NATURAL HAZARDS MISSION AREA Earthquake Hazards Program. (1) . Geometrically. : . angles or vectors . describe . the fault orientation and slip . direction. .. (2) . Graphically. : . focal mechanisms . describe two possible fault orientations and slip directions.. ed. ) Spin on Renewal Models . Karen Felzer. USGS Pasadena. The time-predictable renewal model. Two key predictions:. 1) There is a minimum wait time before a fault patch is eligible for re-rupture.. Luis Gomez. Alicia Sellsted. Elena Pierce. Paulo Dos Santos. Francisco Raygoza. Team 3:. Faults of Los Angeles . . SCEC UseIT. Los Angeles: The City of Faults. Ernest Scapini. Faults . in Los Angeles . By. VAMSI. &. VINAY. . Hazard . Prediction Based on Seismicity . Simulation. . Shiyong. Zhou Russell Robinson . Xiaofei. Chen . M. Jiang . X. . Jin. . B. Gao . Luis Gomez. Alicia Sellsted. Elena Pierce. Paulo Dos Santos. Francisco Raygoza. Team 3:. Faults of Los Angeles . . SCEC UseIT. Los Angeles: The City of Faults. Ernest Scapini. Faults . in Los Angeles . EARTHQUAKES AND FAULTS. Why do earthquakes occur? . What is the relationship between earthquakes and faults? . A shallow MAGNITUDE 7.2 earthquake struck Central . Visayas. Tuesday, October 15. The quake struck at 8:12 am, with EPICENTER 2 kilometers southeast of Carmen, Bohol. The quake's depth of FOCUS was 33 kilometers. According to scientists, the earthquake was caused by movement along the North Bohol Fault. . Bill . Menke. Seismologist. Public Lecture. American Canoe Association. Hilltop Facility. 4PM Saturday May 21 2011. Another Small Earthquake Rattles Central N.J. . WCBS-TV . | Feb 15, 2009 . MORRISTOWN, N.J. (CBS) -- For the second time in two weeks, a small earthquake has rattled an area of central New Jersey. . Karen Felzer. USGS Pasadena. Preliminary Work!!. Subject to change!. The ETAS simulations assign aftershock density with distance, . r. ,. from the . mainshock. as:. Aftershock density = 1/(r . dmin). earthquake. (also known as a . quake. , . tremor. or . temblor. ) is the result of a sudden release of energy in the . Earth's. . crust. that creates . seismic waves. . . The . seismicity. , . seismism. . What Is an Earthquake?. An . earthquake. is the vibration of Earth produced by the rapid release of energy. Energy released radiates in all directions from its source, the . focus. . Energy is in the form of waves. Created By:-. Ghanva Krishna. Department:-. computer. Year:-. 3. rd. year(5. th. . sem. ). Gides. :. Ankita. . Parmar. Sapan. . parekh. SCET(. Surat. ). Introduction. Earthquakes. constitute one of the worst natural hazards which often turn into disaster causing widespread destruction and loss to human life.. Pick up materials for the model. Assemble your model. Explore the behavior of the model and consider the following… “How this might this model represent the earthquake process?”. Earthquake Machine. 36. Cl cosmogenic exposure dating and decadal GPS strain-rate.. Francesco Iezzi. (francesco.iezzi.15@ucl.ac.uk). ,. G. Roberts, J. Faure Walker, I. Papanikolaou, A. . Ganas. , G. . Deligiannakis. , J. Beck, S. Wolfers, D. .