Geology Exam 3- Ch. 11 Notes        

StudyBlue printing of Geology Exam 3- Ch. 11 Notes         html, body, div, span, applet, object, iframe, h1, h2, h3, h4, h5, h6, p, blockquote, pre, a, abbr, acronym, address, big, cite, code, del, dfn, em, font, img, ins, kbd, q, s, samp, small, strike, strong, sub, sup, tt, var, b, u, i, center, fieldset, form, label, legend, table, caption, tbody, tfoot, thead, tr, th, td { margin: 0; padding: 0; border: 0; outline: 0; font-size: 100%; background: transparent; } body { line-height: 1; } blockquote, q { quotes: none; } blockquote:before, blockquote:after, q:before, q:after { content: ''; content: none; } /* remember to define focus styles! */ :focus { outline: 0; } /* remember to highlight inserts somehow! */ ins { text-decoration: none; } del { text-decoration: line-through; } /* tables still need 'cellspacing="0"' in the markup */ table { border-collapse: collapse; border-spacing: 0; } /* end RESET */ .header { min-width:800px; } .logo { padding:6px 20px 2px 20px; margin:0; font-size:25px; font-weight:bold; color:#808285; position:relative; border-bottom: 1px solid #c5c5c5; } .logo-blue { color:#70adc4; } .logo-desc { font-weight:normal; font-size:19px; color:#cccccc; margin-top:50px; position:absolute; display: none; } .back-button { position:absolute; top:20px; right:20px; font-size:13px; line-height:25px; color:rgb(0,175,225); font-weight:normal; } .back-button a { color:rgb(0,175,225); } .instructions { padding:0; margin:0; width:100%; position:relative; color:rgb(100,100,100); } .step-holder { border-left:1px solid #ededed; margin-left:20px; } .steps { padding:15px 0; float:left; width:24%; border-right:1px solid #ededed; text-align:center; } .steps-01 { } .steps-02 { } .steps-03 { } .steps-04 { } .label { padding:5px 10px; } .print-button { } .print-button a { background-color:rgb(0,175,225); color:white; line-height: 19px; padding:9px 8px 5px 30px; font-size:14px; text-decoration:none; background-image: url(images/printer.png); background-repeat: no-repeat; background-position: 7px 50%; -moz-border-radius: 5px; -webkit-border-radius: 5px; } .print-button a:hover { background-color:black; } .theNote .content { width: 8.0in !important; margin: 5px auto; padding:20px; background-color:white; } .theNote .header { border-bottom: 1px dashed #C8C8C8; font-size: 17px; padding: 0 0 10px; line-height: 19px; color: #00ADE1; min-width:500px; } .theNote .body { font-size: 14px; line-height: 19px; padding: 10px 0; } .theNote{ padding:6px 0; clear:both; background-color: rgb(200,200,200); } .theNote h3{ color: rgb(100,100,100); } .theNote h1, .theNote h3{ background-color:white; padding:2px 20px; width:8.0in !important; margin: 0 auto; font-size: 15px; } .theNote h1{ padding-top: 10px; font-size: 15px; } .theNote h1:first-child{ font-size: 20px; } .theNote h3 { font-size: 14px; font-weight: normal; } #options { border: 3px double #ccc; padding: 5px 12px; margin: 10px 50px 10px 20px; float: left; } #info { border-top: 1px solid #ccc; padding-top: 5px; font-style: italic; } li { margin: 5px 10px 5px 25px; } ul li { list-style: disc; } ol li { list-style: decimal; } img { border: 0; } table { clear: both; width: 100%; border: 1px solid #c5c5c5; border-width: 1px 0; margin: 0; page-break-after: always; } table#page { page-break-after: auto; } td { text-align: center; font-size: 12px; border-bottom: 1px dashed #c5c5c5; height: 1.75in; width: 50%; padding-left: 15px; } .leftside { border-right: 1px solid #cccccc; padding: 0 15px 0 0; } .bottom td { border-bottom: none; } .clearfix { clear:both; line-height:1px; height:1px; } img { max-width:80%; max-height:150px; margin:20px; } @media print {.header { display: none; } .content .header{ display:inherit; } table { border: 1px dashed #bbb; border-width: 1px 0; } .theNote{ background-color:white; } } Particle motions for P, S, surface waves P-waves Push or pull particles of matter in the direction of their path of travel S-waves push material at right angles (90 o ) to their path of travel Surface waves can either act as ocean waves OR can act much like S-waves Locating the Epicenter Step 1: Measure time interval between first arrivals of P- and S-waves at each station (differs for each station). Step 2: Determine the distance to the epicenter based on the time interval between the arrival of P- and S-waves (Figure 11.11) Step 3: Draw a circle around each station with a radius equal to the station’s distance from the epicenter (Figure 11.12) . The common intersection of all the circles defines the location of the epicenter. Building Damage from Earthquakes Destructiveness depends on many factors: – Size of the earthquake – Duration of the ground shaking – Strength of buildings – Distance from the epicenter – Nature of the soil and bedrock Types of Fault Movement Seismologists can also determine the type of fault movement (normal, reverse or strike-slip) that produced the earthquake. Determining Fault Mechanisms: • The first motion of P-waves arriving at seismograph stations is used to determine the orientation of the fault plane and the direction of slip – The first motion may be a push or pull • First motion for each seismic station plotted on graph coordinates as a push or pull – Quadrants are drawn separating regions of push from pull – The distribution and appearance of the quadrants define the type of fault movement The global distribution of earthquakes define plate boundaries (Figure 11.13) . Fault mechanism solutions of earthquakes that occur along the plate boundaries indicate the types of faulting, and hence the types of plate boundaries: • Normal faulting (divergent plate boundary) • Reverse and thrust faulting (convergent plate boundary ) • Strike-slip motion (transform plate boundary) Tsunamis Most form from vertical displacement along a fault located on the ocean floor OR From a large underwater landslide triggered by an earthquake - Not detectable in open sea, but as they get closer to shore, the waves pile up and can be huge