PPT-Week 2 Faults and waves Before: What are faults?

During Fault notes After Exit slip 4 questions Day 1 Faults Fault a breaks in the earths surface along which rocks can move Three kinds of faults determined by how the rocks move against each . Dr. . Chuck . Neufeld. Lander University. Phonation Faults. Hypofunctional (Breathy) Phonation. Forced Breathiness. Hyperfunctional Phonation. Phonation Faults. Hypofunctional. (Breathy) Phonation. Failure to demand enough appropriate activity from the vocal mechanism. Regional Strain. Types of Fault and the Principal Stresses. Fault Rocks. Gouge: non-cohesive, fine grained. Breccia: coarse angular fragments. Cataclasite: cohesive fragments. Fault Melt (pseudotachylite):. and Folds. The illustration shows an east-west cross section between the Allegheny Structural Front and North Fork Mountain. The topographic feature called Germany Valley sits atop the geologic structure called the Wills Mountain Anticline. Westward directed compressive forces associated with the . Layali Rashid. Errors that occur in bursts, at the same location, when the fault is activated . [WDSN07]. .. Faults which occur frequently and irregularly for a period of time . [ASPLOS08]. .. A persistent defect that causes zero or more failures, such as a speck of conductive dust partially bridging two traces . Faults of the Los Angels Field trip. How were the San Gabriel Mountains uplifted? –Kim . Gloersen. . How the Raymond, Hollywood, and Santa Monica faults are related? –Diego Furtado. How are we “blind” to some of our faults? – Hannah . Lecture 29. Gly. 326. Compression and deformation. In areas of compression, we have several options for deformation. Dependent on lithology, rock strength, confinement, fluid occurrence, etc.. Reverse/Thrust faults. 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.. ITET G. . MAGGIOLINI . & . “The green . school. network. ” . present. . What. . is. an . earthquake. ?. An earthquake (also known as a quake, . tremor) . is the . shaking of the surface. of the Earth, resulting from the sudden release of energy in the Earth's lithosphere that creates seismic waves. . An . earthquake. is a shaking of the ground caused by the sudden movement of large blocks of rock along a fault. Earthquakes occur along faults.. A . fault. is a fracture, or break, in Earth’s lithosphere, along which blocks of rock move past each other.. Faults are classified by how rocks move.. The blocks of rock along different types of faults move in different directions, depending on the kinds of stress they are under.. There are three types of faults:. lithosphere,. where movement occurs.. Stress. A force that presses on, pulls on, or pushes against another object.. Earthquake. The ground shaking caused by the sudden movement of large blocks of rock around a fault.. Craig . Hyslop. Robert Stewart. Outline. Purpose. Process. Synthetics. Field . d. ata. Conclusions. 2. Purpose. 3. (. Engelkemeir. , 2006). Identification of blind faults. Depth: . 0-50m. Exploration. These terms must be included in your foldable for home work. Seismology. Deformation. Elastic rebound. Seismic waves. P waves. S waves. What are Earthquakes?. The shaking or trembling caused by the sudden release of energy. This topic will shake you up. Stress. Stress-. a force (energy) that acts on rock to change its shape or volume. Types of Stress. Tension-. pulls or stretches rock so that it becomes thinner in the middle. This happens at divergent plate boundaries..