Pop Quiz 3 Review.

Slides:



Advertisements
Similar presentations
 Depth Into the earth Surface of the earth Distance along the fault plane 100 km (60 miles) Slip on an earthquake fault START.
Advertisements

$100 $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $300.
Liquefaction, Landslides, and Fault Rupture Tom Holzer Research Engineering Geologist 1.
San Francisco Geological Study By Emily Williams Victoria Hogg.
Earthquakes Seismic Waves in the Earth’s Crust. Earthquakes ► An earthquake is a series of seismic waves or tremors in the earth’s crust. ► They are caused.
Earthquakes in the San Francisco Bay Area Sheryl Braile, Happy Hollow School West Lafayette, IN Larry Braile, Purdue University
Long and short term deformation along the San Andreas Fault Examples of issues of spatial and temporal scale of interest. Also indicates rate of deformation.
Procedure Wax Paper Tray. Faults Type of Faults and Their Formations.
Using Geodetic Rates in Seismic Hazard Mapping March 30, Geodetic and Geologic slip rate estimates for earthquake hazard assessment in Southern California.
Geology of Australia and New Zealand, HWS/UC NZ Seismicity and Seismic Hazards.
Map scale.
Earthquakes recorded in the landscape: Using digital topography to investigate earthquake faulting Christopher Crosby GEON / Arizona State University SDSC.
Map Scales CGC1D.
Map Scale Looking at the maps on the screen ask the students which one has the largest scale? This will remind the students of what they have already learnt.
The San Francisco Earthquake of 1906 Learning from the Past to Advance the Future By Mrs. Cheney.
Segments of the San Andreas Fault Historically, the San Andreas has been divided up into individual fault segments that range from tens to hundreds of.
Outline: Lecture 4 Risk Assessment I.The concepts of risk and hazard II.Shaking hazard of Afghanistan III.Seismic zone maps IV.Construction practice What.
By: Bradley Z.. These are some pictures of the destruction.
Paleoseismic and Geologic Data for Earthquake Simulations Lisa B. Grant and Miryha M. Gould.
EARTHQUAKES Practice for 6 th grade quiz Ms. Cooper’s class Korematsu Elementary School.
The Land Around Us An Introduction to Maps By: Mrs. Miles.
Seismic Hazard Assessment for the Kingdom of Saudi Arabia
$100 $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $300.
Lisa Wald USGS Pasadena U.S. Department of the Interior U.S. Geological Survey USGS Earthquake Hazards Program Earthquakes 101 (EQ101)
Finding Faults in California The Great California ShakeOut.
National Seismic Hazard Maps and Uniform California Earthquake Rupture Forecast 1.0 National Seismic Hazard Mapping Project (Golden, CO) California Geological.
Chapter 5 Study Guide Friday, February 26, Section 1 Understand what a fault is. Be able to describe the different types of faults. Be able to discuss.
LiDAR and the San Andreas Fault exercise Sarah Robinson ASU.
Quiz/Review Get out a small piece of paper and put your name on it. When the bell rings, the quiz will begin.
OPENQUAKE Mission and Vision It is GEM’s mission to engage a global community in the design, development and deployment of state-of-the-art models and.
Quantifying and characterizing crustal deformation The geometric moment Brittle strain The usefulness of the scaling laws.
FAULT TYPES By Ashlyn Boswell. Strike Slip Strike Slip Fault NormalNormal Fault ReverseReverse Fault ThrustThrust Fault.
Seismographs Are instruments located at or near the surface of the Earth that record seismic waves.
The repetition of large earthquakes, with similar coseismic offsets along the Carrizo segment of San Andreas fault has been documented using geomorphic.
Earthquakes 101 (EQ101) Lisa Wald USGS Earthquake Hazards Program
I. What is an earthquake? Earthquake defined Fractures and faults
1 Wallace Creek, USGS aerial view, about 1990 USGS Photo.
Understanding Earth Sixth Edition Chapter 13: EARTHQUAKES © 2011 by W. H. Freeman and Company Grotzinger Jordan.
Mapping Earthquakes Scripps Classroom Connection USGS real time earthquake map Question of the day: where do most earthquakes occur?
Earthquakes! Richter scale.  Developed in California at Cal Tech by Charles Richter in 1935  Based on the specific rocks found there  Only measures.
EARTHQUAKES Information from the USGS Locations of Earthquakes Dots are earthquakes.
GEOL 308 Quiz: Focal Mechanisms
Sandy Creek Nature Center
Eg San Andreas Fault California
Uplift: Faults and Earthquakes
Friday, October 28, 2016 CW: Earthquake Quiz Study Guide
Section 6.5: Studying Earthquakes
Map scales A scale drawing is a drawing in which all dimensions have been reduced in exactly the same proportion. For example, if a model boat is made.
Referencing Data to Real Locations
Hire Toyota Innova in Delhi for Outstation Tour
Make Your Own Quiz.
Understanding Earth Chapter 13: EARTHQUAKES Grotzinger • Jordan
Tip Meckel Ph.D. Candidate Geological Sciences
We first consider plate motions at a point on Earth’s surface, or within a small region. In this case we can neglect the curvature of the planet and treat.
هل يمكن أن نكون جيل الأرض الأخير؟
Map Scales CGC1D.
Inside Earth 1.2 & 1.5.
Using Distances to known Earthquake epicenters, create
What everyone should Know about map Contents!
Seismic Waves.
VII. Earthquake Mitigation
Earthquakes and Fault Types
Earthquakes! OBJECTIVES Differentiate between Focus & Epicenter
Seismology Introduction.
Why do they happen? Where do they happen? How do they happen?
Earthquakes.
Seismology – Summary.
Fig. 1 Map of the trifurcation area of the SJFZ.
What is a scale? Scale is the ratio of the size of objects on a map compared to their size in the real world. 4 cm:1 km For example on a map with the scale.
San Andreas Fault Images
Presentation transcript:

Pop Quiz 3 Review

http://conservation.ca.gov/cgs/rghm/psha/Pages/Index.aspx

San Andreas fault at Wallace Creek. Because earthquake fault slip rates feed into Seismic Hazard, I will calculate the fault slip rate (i.e. source characterization). The following are the steps I would take: Rate = Distance / Time. The stream is 10,000 years old, so the time span is 10,000 years. The stream channel has been offset. I will measure the distance in Map Units. I will determine the scale of the map (conversion factor). I will convert the Map Units to Real World Distance with the conversion factor. I will divide the Real World Distance by the time to get the fault slip rate. I will convert the slip rate units to mm/yr so it can be used by the design engineer, she will appreciate this. http://arrowsmith410-598.asu.edu/Lectures/Lecture4/GLG410_598--Excel_Warmup3.html