PPT-B ackground Information on First Motion Models for Earthquakes

Bruce Douglas Indiana UniversityBloomington Gareth Funning University of CaliforniaRiverside Version Dec 7 2015 We use a specific set of symbols to identify faulting geometry on maps The symbols are called earthquake focal mechanisms or sometimes . Motion and Sensing. Slide credits: Wolfram Burgard, Dieter Fox, Cyrill Stachniss, Giorgio Grisetti, Maren Bennewitz, Christian Plagemann, Dirk Haehnel, Mike Montemerlo, Nick Roy, Kai Arras, Patrick Pfaff and others. MODELS. Shuftan. Process. The image of a miniature model is reflected into the camera via a mirror.. Where the image of the miniature is not desired, that portion of the mirror silvering is scraped away, allowing the camera to see through the clear glass and photograph the primary scene, which is usually the foreground and live action.. and archiving . in Europe. Sinan Akkar. Earthquake Engineering Research Center. Middle East Technical University . Ankara, Turkey. Earthquake Engineering Research Institute . Middle East Technical University . By: Jennifer Marcial. A presentation on animation film-making, and how it works.. Definitions. *. Rigs. -Steadicam is a brand of camera stabilizer mount for motion picture cameras that mechanically isolates it from the operator's movement. It allows for a smooth shot, even when moving quickly over an uneven surface. The Steadicam was invented by cameraman Garrett Brown and was introduced in 1975.. Chapter 2 Section 3. Objectives. F.2.3.1. Explain how a seismograph works.. F.2.3.2. Describe how Geologists monitor faults.. F.2.3.3. . Explain how . seismograph data is used.. The Seismograph. Seismic waves cause the seismographs drum to vibrate but the suspended weight with the pen attached moves very little. Therefore the pen remains still and records the vibrations on the drum.. They Shape Our Landscape. As plates move, we may feel these movements as earthquakes. If there were no plate motions, our planet would not look like home. There would be no mountains, no valleys, no plateaus . . By : . Deavian. foster . Class : 5H. What is an earthquake?. A earthquake is a shaking of the earths crust and is a geological phenomenon . Earthquakes can cause intense vibration of the ground, soil liquefaction, and distortion of the ground. Earthquakes can happen almost anywhere but are most common along the boundaries of the tectonic plates. Earthquakes are primarily caused of movement of the tectonic plates. It lasts more than a few seconds.. Earth’s Dynamic Crust. Original Horizontality (law of superposition):. Assumption . that sedimentary/igneous rocks form in horizontal layers . Deformity. Folded: Layers are bent/curved. Deformity. Why you need to prepare for the next earthquake . Alaska has more earthquakes than any other region of the U.S. . And in fact is one of the most seismically active area of the world.. Great earthquakes (Earthquakes larger than magnitude 8) rock the state on average every 13 years since the 1900. . William Mackaness, Carol Blackwood, Charlotte Graves. Institute of Geography. School of GeoSciences. University of Edinburgh. Drummond St, Edinburgh EH8 9XP. william.mackaness@ed.ac.uk. Earthquakes. Measure on a Richter scale 1-7. By: Dan Arrington. EAS 4480. Spring 2012. Image obtained from: http://www.survival-goods.com/What_is_an_Earthquake_s/269.htm. Background Information. Richter Scale. Measures magnitude. Energy released. CAMPUT . Regulatory Key Topics Meeting. Montreal, . January 28-30, . 2018. JP Mousseau. AUC Counsel. Process is good, right? . Providing some form of process before deciding a motion is generally a good idea but it can sometimes add time and expense to a proceeding without material benefit. . JulyDebtorfiledhisVoluntaryPetitionunderChapterCaseNoECFNo1SeptembertheCourtenteredOrderGrantingtheChapterTrustee146sMotionforExtensionCertainCaseDeadlinesCaseNoECFNos12AprilPlaintiffsfiledtheirMotion : Western US. Authors: Ruth Powers (UNAVCO Master Teaching-in-Residence); . Becca Walker and Shelley Olds (UNAVCO). Activity Outcomes. Learners should be able to…. Describe how the locations of earthquakes, volcanoes, and velocity vectors from GPS stations in the Western United States inform us about plate boundary zones.