SDAG Monthly Meeting
Wednesday - January 15 |
Location:
Catalina Room (south end of MVCC)
Marina Village Conference Center
1936 Quivira Way
San Diego, CA 92109
Directions:
FROM INTERSTATE 5: Take the SEA WORLD DRIVE exit. From SEA WORLD DRIVE,
take WEST MISSION BAY DRIVE on your right. When you see the large green sign that
says QUIVIRA ROAD, get in the farthest left of the two left turn lanes. Turn left, go one
very short block and turn left again. Drive about one half mile and MARINA VILLAGE will
be on your right.
FROM INTERSTATE 8:Exit at SPORTS ARENA BLVD., then take WEST MISSION BAY DRIVE exit to the right.
You will be on INGRAHAM STREET for a short distance from which you will take the next exit
marked WEST MISSION BAY DRIVE on your right. When you see the large green sign
that says QUIVIRA ROAD, get in the farthest left of the two left turn lanes. Turn left, go
one very short block and turn left again. Drive about 1/2 mile and MARINA VILLAGE will be on your right.
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6:00pm -
Social hour
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SDAG Monthly Meeting
6:00pm - Happy Hour
7:00pm - Dinner
8:00pm - Program
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7:00pm
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Menu: All American Buffet / Vegetarian
if pre-registered by the deadline, $5 extra if you did not make a reservation.
Click the SDAG member checkbox on the reservation form if you are a member.
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Cost: $ 60.00 Member; Non-Member $ 70.00; Student $ 30.00
Reservations:
Make/Pay your reservation online by clicking the button below
by Noon Monday, January 13
RESERVATIONS CANNOT BE ACCEPTED AFTER by Noon Monday, January 13
(Please note beginning January 2024 all meeting reservations will require on-line pre-payment due to venue costs,
venue contracts, and loss of money due to no shows.)
IF YOU DO NOT PRE-PAY YOUR FOOD RESERVATION, WE CANNOT GUARANTEE YOU A MEAL.
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8:00pm - Program
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"Factors Effecting the Interpretation of Faulting in Cone Penetrometer Test Sounding Investigations"
Speaker: Scott Rugg, RG CEG
Cone Penetrometer Test Soundings (CPTs) are an often-used method to characterize subsurface soil behavior properties
mostly in soft material conditions. The method has many geotechnical applications, some of which include liquefaction
analysis, mapping of alluvial deposits and fill, evaluation of soil density improvement and determination of seismic
S- and P-wave velocities. When a series of CPTs is advanced, the subsurface stratigraphy can be profiled. This was
recognized early on and soon CPTs were engaged to identify stratigraphic disruptions indicative of faulting. This method
is now widely used in the coastal province of Southern California, mostly in upper Quaternary materials. Oftentimes, only
several feet or less of vertical differential across unit horizons or thickness variations in strata are used to identify
potential faulting. This means it is imperative that depth recording of CPTs are as accurate as possible. Several factors
can cause errors in depth readings, leading to erroneous interpretations of faulting. These factors will be discussed in
this presentation as well as a quality control procedure to track actual depths and thus mitigate errors. In addition,
several examples will be presented where inaccurate depth readings resulted in misinterpretation of faulting. Finally,
both the advantages and limitations of the CPT method will be discussed.
Mr. Rugg has 38 years of experience in the fields of engineering geology and geotechnical engineering, having worked on
thousands of sites throughout California and the Southwest. He has focused his vocation on fault and seismic hazard
assessment, having worked extensively on all types of projects including high-rise buildings, hospitals, water and
wastewater treatment plants, airports, dams, transportation, education facilities, and residential sites. Early in his
career he evaluated hundreds of sites damaged during the 1986 Palm Springs, 1987 Whittier Narrows, 1989 Loma Prieta,
and 1994 Northridge earthquakes. A sampling of fault hazard projects he has led are the Master-plan Investigation of
San Diego International Airport, San Diego, CA, - Mid-Coast Trolley Extension, San Diego, CA, - Airfield Expansion,
Naval Weapons Station, China Lake, CA, - Biosolids and Clarifiers Replacement, Orange County Sanitation District,
Huntington Beach, CA - Exxon Mobil Carbon Capture Facility, Baytown, Tx - Camp Blaz Satellite Facility, US Territory
Guam, and the Automated People Mover, Inglewood, CA. He has proficiency in all methods of fault investigation with
extensive experience in the use of Cone Penetrometer Test Soundings for fault hazard analysis.
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Upcoming SDAG meetings - 2025
February 19 - Karl Mueller will give his talk on new work on active faulting in San Diego
March 19 - Don Barrie on New Zealand Geology
April 16 - Student research presentations by student scholarship recipients
May 21 - TBA
June 18 - SDAG / SCGS Joint Meeting
July 16 - TBA
August 20 - TBA
September 26-28 - SDAG Annual Field Trip, San Andreas Fault in the Wrightwood area, Transverse Ranges (no meeting this month)
October 15 - TBA
November 19 - Joint Meeting with AEG Inland Empire Section
December 17 - Traditional Holiday Celebration at the San Diego Natural History Museum with Tom Deméré
Recordings of past meetings
Note: If the video or sound does not play, try using another web browser. Firefox and Chrome may work on some of the videos. MS Edge and Safari are most likely to work.
8/21/2024 Upper Cretaceous through lower Eocene strata in San Diego: Messages for the end-Cretaceous impact, extinctions, and paleoclimates - Dr. Pat Abbott
5/15/2024 Exploring Iceland's Geological Wonders: From a Regional Perspective to a Hiking Expedition - Don Barrie & William Buckley
3/19/2024 Mighty Bad Land: A Perilous Expedition to Antarctica Reveals Clues to an Eighth Continent - Bruce Luyendyk
Meetings are usually scheduled for the 3rd Wednesday evening of the month.
Meeting information on this website is normally updated the second week of the month.
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2024 SDAG Secretary.
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The submittal deadline for the next SDAG newsletter is the last Friday of the month.
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