PPT-Direct observations of a dynamic earthquake rupture in the lower crust

Arianne PetleyRagan 1 BenZion Y 2 Austrheim H 1 Ildefonse B 3 Renard F 14 and Jamtveit B 1 1 Physics of Geological Processes The Njord Centre University of Oslo Oslo Norway. Isostasy. When . gravitational and buoyant forces are equal, a state of . isostasy. exists. . As . erosion wears away the crust, the lithosphere becomes lighter and rises. .. As . erosion continues, the . The Earths crust . The earths crust is in constant motion.. Volcanoes and earthquakes arise as sections of crust push . toghether. or pulled apart. Volcanoes and earthquakes are more common in certain parts of the world. By monitoring ground vibrations scientists can sometimes. Nathalie . Degenaar. . University of Michigan. X-ray observations. Interior properties. Thermal evolution. Neutron stars . in transient X-ray binaries. Quiescence. :. No/little accretion. Faint X-ray emission. and . the contribution of array seismology. J.-P. . Ampuero. Caltech . Seismolab. Acknowledgements. : . Lingsen. . Meng. (now at UC Berkeley). Overview. Earthquake physics: how earthquakes start, propagate and stop? + broader impact. Active Fault. Earthquakes Create Seismic Waves. (also hypocenter). 3 Types of Seismic Waves. P wave: Primary. S wave: Secondary. Surface waves. Fastest. Slowest. Depiction of Seismic Waves. Types of Earthquake Waves. tial of a fault commonly is evaluated from estimates of fault rupture parameters that are, in turn, related to earthquake magnitude. It has been known for some time that earthquake magnitude may be co pg. . 115. http://www.indiana.edu/~g103/G103/week9/wk9.html. . http://www.uwgb.edu/DutchS/EarthSC202Notes/quakes.htm. . Folding. : . When . Rock Layers. . Bend. . because of STRESS. What are anticlines?. Stage 1.. Magma rises to the crust within the mantle. This creates friction and causes the plates to move.. What are the 3 main ways plates move. 1.. 2.. 3. . Stage 2. Pressure builds between plates and sometimes small earthquakes are felt. . 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. HLF . 1089526 1/10# . Jake’s Code: VFSH18. SELLING FEATURES. Top crusted for perfect experience. Flaky and flavor packed, crunchy crust.. Authentic Ingredients, handmade appearance!. …). Describe how models of the inside of Earth developed over time. Success Criteria: (Can you . …). Complete a time line. LISTEN and RECORD carefully.. How to organize lesson . 045. The lessons Agenda was:. La gamme de thé MORPHEE vise toute générations recherchant le sommeil paisible tant désiré et non procuré par tout types de médicaments. Essentiellement composé de feuille de morphine, ce thé vous assurera d’un rétablissement digne d’un voyage sur . ABSTRACT KEYWORDS: seismic design, retrofit, fault rupture, isolation bearings INTRODUCTION At the Duzce station near the epicenter, a Peak recorded before the ground motion d due to its limitatio 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.