Lecture 23 Paleoseismology San Andreas fault II Not given in 2008.

Slides:

Advertisements

Similar presentations

Earthquake recurrence models Are earthquakes random in space and time? We know where the faults are based on the geology and geomorphology Segmentation.

Advertisements

New paleoseismic data from the northern San Jacinto Fault Zone, southern California Nate Onderdonk (CSULB) Tom Rockwell (SDSU) Sally McGill (CSUSB) Gayatri.

Forces in Earth’s Crust Chapter 6 Section 1. Earthquakes Elasticity is the ability for an object to return to or keep its original shape Which is more.

Recurrence Intervals Frequency – Average time between past seismic events – aka “recurrence interval” Recurrence Interval = Average slip per major rupture.

Assimilating Data into Earthquake Simulations Michael Sachs, J.B. Rundle, D.L. Turcotte University of California, Davis Andrea Donnellan Jet Propulsion.

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.

A New Approach To Paleoseismic Event Correlation Glenn Biasi and Ray Weldon University of Nevada Reno Acknowledgments: Tom Fumal, Kate Scharer, SCEC and.

1 Integrating Wind into the Transmission Grid Michael C Brower, PhD AWS Truewind LLC Albany, New York

Tracing Evolutionary History. Macroevolution Dating Prehistoric Material Radioactive Isotopes Carbon 14 Potassium 40.

Pleistocene Terrace Deposits in Estero San Antonio Two interpretations of 1 valley by Robert Davies.

Map of magnetic anomaly numbers Deep Sea Drilling sites.

Last lecture Historical behavior of San Andreas fault.

A Look Inside the San Andreas fault at Parkfield Through Vertical Seismic Profiling Chavarria, Malin, Catchings, and Shalev Science, 302, pp ,

Tsunami Great Sumatra Earthquake Tsunami Death Toll ~ 250,000 Tsunami Death Toll ~ 250,000.

Transforming California Landforms of the San Andreas Fault Images & text by Thomas McGuire, Cave Creek Digital, Cave Creek, AZ

Plate boundary project. Instructions Today you will be making plans to make a power point project over tectonic plate boundaries. You will need to include.

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.

NA-Pa Plate Boundary Wilson [1960] USGS Prof. Paper 1515.

Southern California Earthquake Center Mini Grand Challenge Lindsay Arvin Daniel Philo Ryan Meier Jing Yuan Kelvin Vasquez Ngoc Kiem.

2007 NSTA: St. Louis, Missouri Earthquake Prediction and Forecasting: A Case Study of the San Andreas and New Madrid Faults Sponsored by: IRIS (Incorporated.

San Andreas Big Bend A geometric feature Restraining the relative plate motion Nature’s solution Impacts include:  patterns of faults, seismicity  Rupture.

Paleoseismic and Geologic Data for Earthquake Simulations Lisa B. Grant and Miryha M. Gould.

Thailand Training Program in Seismology and Tsunami Warnings, May 2006 Forecasting Earthquakes.

1857 Rupture 300 km Ray Weldon (with material from colleagues and students) How to do Paleoseismology for SOSAFE.

National Seismic Hazard Maps and Uniform California Earthquake Rupture Forecast 1.0 National Seismic Hazard Mapping Project (Golden, CO) California Geological.

Национальная процедура одобрения и регистрации проектов (программ) международной технической помощи (исключая представление информации об организации и.

Largest discontinuity along the San Andreas fault San Andreas fault slip decreases to a minimum of 5–10 mm/yr at the SGP, from 24 ± 3.5 mm/yr at Cajon.

PREDICTION Paleoseismology: Documenting and evaluating past events. 1.) Usually done with looking at offset layers in sediments in trenches 2.) Calculate.

Pearblossom Geodetic Networks EDM Network 1980 – 2001 Early 1980s; Frequent Mid 1980s to mid 1990s quarterly measurement Late 1990s to the end annual GPS.

Strike-Slip Faulting. Outline Tectonic setting –Transform plate boundaries –Escape structures in the hinterland of plate collision zones –Transfer zones.

San Andreas MW 7.9 Earthquake: Slip at Critical Lifeline Crossings ShakeOut scenario for southern California Dr. Ken Hudnut U.S. Geological Survey,

An absolute chronology for early Egypt using radiocarbon dating and Bayesian statistical modelling by Michael Dee, David Wengrow, Andrew Shortland, Alice.

Forecasting Earthquakes

Double click here to add event title Double click here to add event date Double click here to add event time Double click here to add event location.

Using this approach we have integrated all of the tidal and leveling records from coastal Oregon to determine the 3d uplift pattern along the coast. Topography.

Forecasting Earthquakes ・ Difference between Predictions and Forecasts ・ Earlier Efforts in Earthquake Prediction ・ Long-term Probability Estimates.

SCEC Annual Meeting Sept , 2006 Southern San Andreas Fault Evaluation SoSAFE A New SCEC Special Project Ken Hudnut Thanks to Terry Tullis, Tom Jordan.

The Time-Predictable Recurrence Model The original models (Shimazaki & Nakata 1980) Complications and pitfalls (Thatcher 1984) Modern examples Relevance.

基督再來（一）. 經文： 1 你們心裡不要憂愁；你們信神，也當信我。 2 在我父的家裡有許多住處；若是沒有，我就早已告訴你們了。我去原是為你們預備地去。 3 我若去為你們預備了地方，就必再來接你們到我那裡去，我在那裡，叫你們也在那裡， ] ( 約 14 ： 1-3)

Lecture 9: Geomorphology

Relative Dating.

“Road” To Revolution Project

Tips Need to Consider When Organizing a College Event

Checklist for Site Reconnaissance (Sabatini et al_2002)

San Clemente Fault Zone Catalina Fault Zone San Diego Trough

Five Year Construction Plan

ماجستير إدارة المعارض من بريطانيا

Systems Development Life Cycle II Lecture 4: Method Specifications

Слайд-дәріс Қарағанды мемлекеттік техникалық университеті

.. -"""--..J '. / /I/I =---=-- -, _ --, _ = :;:.

Aseismic Slip and Repeating Earthquakes on the San Andreas Fault

Strawperson Design II TA-type array 45 $75K Intermediate band

Date, location, department

II //II // \ Others Q.

Фейлетоните на Алеко Константинов

I1I1 a 1·1,.,.,,I.,,I · I 1··n I J,-·

Date, location, department

Name of Event Name of Event

Department | Website | Phone Number

Name of Event Name of Event Date, location, department

Patient Disposition James A. de Lemos et al. JAMA 2004; 292:

Thing / Person:____________________ Dates:_________________

Faults and Folding 9/24.

NAME OF EVENT Name of Speaker Date, location, department

. '. '. I;.,, - - "!' - -·-·,Ii '.....,,......, -,

Fig. 1 Map of the trifurcation area of the SJFZ.

Similarities between the studies: Differences between the studies:

Title: Date: Cause: Event: Effect: Title: Title: Title: Date: Cause:

by Julian C. Lozos Science Volume 2(3):e March 11, 2016

Presentation transcript:

Lecture 23 Paleoseismology San Andreas fault II Not given in 2008

8 m >5.4

What is the effect of the San Gorgonio Pass restraining bend ?

Event dates at the Burro Flat site

800 An attempt at a Chronology

950

1050

1100

1200

1350

1500

1550

1600

1680

1812

1857

Weldon et al., 2002 and 2004

The Wrightwood site allows a test of the time- and slip-predictable models periodictime-predictableslip-predictable