PDF-Earthquake Shaking Potential for California D

Branum S Harmsen E Kalkan M Petersen and C Wills This map shows the expected relative intensity of ground shaking and damage in California from anticipated future earthquakes The shaking potential is calculated as the level of ground mot. :. What You Need To Know. Tsunami Outreach Oregon. Oregon Department of . Geology . and Mineral Industries . Cascadia Earthquake: Key Messages. A local Cascadia earthquake will probably happen in most people’s lifetime or their children’s lifetime.. Acts . 16:22-34. Acts 16:22-34. 22. . The crowd joined in the attack against Paul and Silas, and the magistrates ordered them to be stripped and beaten. . 23. After they had been severely flogged, they were thrown into prison, and the jailer was commanded to guard . Operational Earthquake Forecasting (OEF) . Meeting. March . 16-17, 2015. Powell . Center. USGS Fort Collins Science Center. 2150 Centre Avenue, Building C. Fort Collins, CO. . OEF. – Real time, authoritative information on earthquake likelihoods. and Hazard. John N. Louie. , Nevada Seismological Lab.. with UNR undergraduate interns:. Will . Savran. , Brady . Flinchum. ,. Colton Dudley, Nick . Prina. and Geology B.S. graduate . Janice . Kukuk. Hazards are produced from the response of energy released. Amount and duration are related to the amount of energy released. Which hazards do you know?. Earthquake Hazards. Tsunami: displacement of a large volume of water. 2 . Department of Statistics and Institute for Policy Research, Northwestern University, Evanston, Illinois, USA. . Edward Brooks. 1. , Seth Stein. 1. , Bruce D. Spencer. 2. . Assessing the Long-Term Performance of Earthquake Hazard Maps. From Science to Real Implementation. . Jair TORRES. UNESCO. Earth Sciences and Geo-Hazards Risk Reduction Section. Natural Sciences Sector. E. ARTHQUAKE . E. ARLY . W. ARNING. . S. YSTEMS. ???????. Tectonic plates are huge rock pieces within the earth’s crust. The plates are usually marked by fractures or fault lines formed when the plates tear apart or slide or collide past each other. This results in a change of the earth’s interior masses which send out powerful shock waves with enough force to alter the surface of the earth. The shock waves can thrust up cliffs and open huge cracks on the ground leading to an earthquake event. Earthquake Risk. Earthquakes are likely wherever plate movement stores energy in the rock along faults.. Geologists can determine earthquake risk by locating where faults are active and where past earthquakes have occurred.. 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. . SYFTET. Göteborgs universitet ska skapa en modern, lättanvänd och . effektiv webbmiljö med fokus på användarnas förväntningar.. 1. ETT UNIVERSITET – EN GEMENSAM WEBB. Innehåll som är intressant för de prioriterade målgrupperna samlas på ett ställe till exempel:. . CEETEP. Sue Graves ~ August 2015. Local Cascadia Earthquake. 10,000-Year History of . Cascadia. 41 ruptures = average of 243 years. Damage to Homes. Damage to Schools. Structural Damage. Non-structural Damage. Amount and duration are related to the amount of energy released. Which hazards do you know?. Earthquake Hazards. Tsunami: displacement of a large volume of water. Shallow hypocenter, large volume of displaced crust, large earthquake. CERT Basic Training. Describe the functions of CERT, discuss your role as a CERT volunteer, and explain how CERT fits into your community’s emergency preparedness structure . Describe the types of hazards most likely to affect your communities and their potential impact on people, health, and infrastructure .