AIPG California Section Spring 2015 Newsletter AIPG California Section - UC Davis Student Section 2015 Meeting Schedule APRIL 2, 2015: DOT LOFSTROM, P.G. MAKING A DIFFERENCE WITH THE DTSC Dot Lofstrom, P.G., Division Chief of the Brownfields and Environmental Restoration Program, Department of Toxics Substances Control (DTSC) is one of the lead regulators in the state. As such, she will discuss her career, her decades of geology experience and her 13 years of experience with the DTSC in Sacramento. Dot Lofstrom is a Division Chief within DTSC’s Brownfields and Environmental Restoration Program at DTSC. She is a California Professional Geologist with both a B.S. and M.S. in geology (Missouri State and University of Missouri-Columbia). Ms. Lofstrom has over 25 years of experience in private consulting, community college instruction, and state, local and federal governments. Ms. Lofstrom is a co-author of DTSC’s Vapor Intrusion Mitigation Advisory, and a contributing author on DTSC’s Vapor Intrusion Guidance, Active Soil Gas Investigations Advisory, and Vapor Intrusion Public Participation Advisory. As the State Engagement Coordinator for the Interstate Technology and Regulatory Council (ITRC) she manages the State Points of Contact and serves on the ITRC Advisory Board. LOCATION: California Section AIPG - UC Davis Student Section Meeting at UC Davis, 7 pm – 9 pm on Thursday, April 2, 2015. Earth and Physical Sciences building Directions: From I-80, take the UC Davis exit, turn in the direction of campus on Old Davis Road and proceed past the Information Booth. Continue straight towards the Mondavi Center 1 where the road becomes New Davis Road. Visitor parking is available in Visitor Parking Lots everyday, and in Parking Lots on weekends except during special events. Evening from 7 pm – 9 pm, Pizza and soft drinks are provided. Meeting is free to the public, AIPG members and students. MAY 7, 2015: STEVE BAKER AIPG JOB HUNTING WORKSHOP, PART 2: THE INTERVIEW Steve will tackle the most challenging part of the job hunting process: the interview. For students, young professionals and senior geologists wanting to practice the art of the interview, this evening will be in a workshop format. Bring your resume and plan to be interviewed. Steve has worked in the environmental industry, interviewing dozens of possible employees for his company. For his radio programs, Steve is a seasoned interviewer and he has been interviewed by others on many occasions. He will tell participants some of his secrets in being interviewed. Plan to start off the evening with a decent and rousing self-introduction. Free pizza and soft drinks will be provided. The meeting is free and will be at UC Davis Earth and Planetary Sciences Building from 7 pm to 9 pm on Thursday, May 7th, 2015. ROCK GARDEN AT UC DAVIS IS A MUST SEE An identifying feature outside the Earth and Planetary Sciences Building are enormous rock samples: The California Rock Garden is open to the public every day. Located primarily along the eastern and southern sides of the Earth and Physical Sciences building, the garden features boulders and core samples representing various geologic features of California. For those not familiar with this rock garden, it has some of the best samples of California rocks found anywhere in the state, and is definitely worth coming to the UC Davis campus to study. Photo of UC Davis California Rock Garden – a must see for all California geologists. 2 FEATURED ARTICLE: MAPPING CALIFORNIA: PART 2: 1917 to 2015 The following public domain article is from the California Geological http://www.conservation.ca.gov/cgs/cgs_history/Pages/geologicmaps.aspx Survey: GEOLOGIC MAP OF CALIFORNIA - 1938 Twenty-two years later, another milestone in California geologic maps appeared in the form of a 1:500,000 scale map published in six sections by the California Division of Mines. This map was prepared by Olaf P. Jenkins, Chief Geologist of the Division of Mines, and represented nine years of careful geological research. 3 Much larger in scale than any preceding geologic maps of the state, the 1938 map shows much more detail than the earlier maps. The geologic boundaries of the 81 units depicted were drawn with greater precision than before. Care was taken to follow the source data faithfully. In areas where no geologic maps were available, or where previous maps were too general in nature or at a scale much smaller than the base map, the area was purposely left blank. This portrayal of the geology of the state showed that about 25 percent of the state was unmapped. The largest unmapped areas at that time were in the Klamath Mountains, the northern Coast Ranges, the southern Sierra Nevada, and the desert areas of southeastern California. For the first time, faults were shown on an official geologic map of California. GEOLOGIC ATLAS OF CALIFORNIA - 1958-1969 The ground work for the Geologic Atlas of California began in 1951, after the popular 1938 edition went out of print. Great demand prompted OIaf P. Jenkins to set up a program for preparing a new edition of the state map that would incorporate the large amount of new geologic data collected since the earlier map was compiled (Jahns, 1961). The first map to be completed, the Death Valley Sheet, was published in 1958. At the outset of the project, the difficulties associated with compiling a geologic map of the entire state, with all of its geologic diversity and complexity, were for the most part recognized, but it was hoped that the abundance of new data on hand would make overcoming these difficulties fairly simple. Actually, the inconsistent nature of these new data made the task more difficult. The source maps for some 4 areas of the state were excellent; in other areas they were very poor, incomplete, or simply nonexistent. Frequently, well-described areas were adjacent to poorly understood, incompletely mapped, or totally unmapped areas. Often, too, there was no continuity between maps for adjacent areas because of differences in geologic interpretation. Thus, the compilation could easily have resulted in a patchwork of data. Fortunately, perhaps, the scale of the atlas made it possible to ignore a multitude of discrepancies. Numerous problems, however, had to be resolved in the field, and almost all blank areas in the state were filled in by reconnaissance mapping by the California Division of Mines and Geology. Nevertheless, in a few areas of complex geology, or where particularly detailed work was surrounded by less detailed mapping, white areas were left around the more detailed area to preserve as much information as possible. Blank areas marked on the atlas sheets as "unmapped" or "incomplete" amount to a very small percentage of some map sheets and are absent entirely from others. FAULT MAP OF CALIFORNIA - 1975 and GEOLOGIC MAP OF CALIFORNIA - 1977 Even before the 1:250,000 scale Geologic Atlas of California was completed, it was recognized that a smaller-scale map of the state, one that would present an overview of the geology of the entire state, was highly desirable. It had become apparent that the individual atlas sheets, as useful as they were for field and office purposes, were not satisfactory for evaluation of statewide geologic and structural trends. Therefore, late in 1965, plans were made for a smaller scale map of California (Jennings, 1965). After consideration of various scales, 1:750,000 was chosen because this scale is sufficiently large to show a significant amount of geologic information and also is consistent with the first two official geologic maps of California published by the State in 1891 and 1916. At the beginning of the project, it was decided that a multipurpose map of the state would be most desirable. In addition to the geology, the map would emphasize recently active faults, recent volcanic rocks and volcanoes, thermal springs, offshore structures, and major fold axes. Therefore, all these data were plotted on the work sheets; but it became evident that, for publication purposes, it would be much more effective to separate some of this information and make two maps rather than one. Pursuing this concept, it was planned to present a series of maps at the same 1:750,000 scale illustrating various geologic and geophysical parameters that can conveniently be studied individually or in relation to one another. Thus, the first map in this series was the Fault Map of California with 5 Locations of Volcanoes, Thermal Springs and Thermal Wells, Geologic Data Map No. 1 (1975). This was followed by The Geologic Map of California, Geologic Data Map No. 2 (1977). FAULT ACTIVITY MAP OF CALIFORNIA AND ADJACENT AREAS - 1994 New data concerning the age and activity of California faults necessitated a revision to the 1975 Fault Map of California. In 1990 Charles W. Jennings began compilation of new data and classification of Quaternary faults into a five age subdivisions (historic, Holocene, late Quaternary, undivided Quaternary, pre-Quaternary. This map took advantage of the extensive mapping of active faults for the Alquist-Priolo Earthquake Fault Zoning act. Age designations were also enhanced by the extensive work for Alquist-Priolo zoning: faults must be shown to have Holocene surface displacement to be included in “A-P” zones. Any fault evaluated and included in such a zone can be shown on the Fault Activity Map as Historic or Holocene. In addition, a more extensive explanatory text was keyed to numbers for many faults to allow geologists to look up the source of the original fault mapping and reason for the age classification. GEOLOGIC MAP OF CALIFORNIA AND FAULT ACTIVITY MAP OF CALIFORNIA - 2010 New editions of the Geologic Map of California and the Fault Activity Map of California have been prepared in recognition of the California Geological Survey’s 150th Anniversary. Both are alldigital products built on the original compilations of C.W. Jennings published in 1977 and 1994. The digital version of the Jennings (1977) geologic map was released in 2000 (Saucedo and others, 2000) and serves as the base digital geologic data layer for the new geologic map with additions and modifications described below. The new editions remove, as much as possible, distortions in the previous digital versions that were inherited from the composite base map of the original printed versions. The 2010 Fault Activity Map of California presents a much more detailed depiction of faults in California than previous versions. Faults active in the Quaternary (2.6 Ma) were digitized from their original sources in order to preserve as much of the original detail as possible. Similar to the 1994 Fault Activity Map, the new map is accompanied by an extensive listing of the sources of fault maps and age determinations. 6 In the 2010 Fault Activity Map, the faults are depicted in as much detail as possible at the scale of the map. The 2010 Geologic Map of California includes modifications to the fault traces for consistency with the 2010 edition of the Fault Activity Map of California. Due to the complexity of the onshore geologic data depicted on the Geologic Map of California, it was not technically feasible to incorporate the detailed fault data in its entirety. A comparison of the datasets was made and numerous fault traces were replaced with simplified fault traces based on the new fault map. In addition, several faults that have been mapped since the compilation of the original geologic map were also identified and added, and traces no longer believed to be faults were removed. In general, the Quaternary faults shown in the onshore region of this map are intended to be a simplified representation of the faults depicted on the Fault Activity Map. Although the modification of faults in some areas necessitated the modification of bedrock geology adjacent to those faults, the distribution of bedrock geologic units compiled by Jennings (1977) has otherwise not been modified. Jennings (1977) simplified the depiction of Quaternary geologic units on the original map. As he put it: “various surficial deposits of Quaternary age are lumped into the unit ‘Q’.” Since Jennings’ work, subdivisions of these deposits have been found to have very different potential for liquefaction and for amplification of seismic shaking. Relative age of Quaternary alluvial fan deposits have also been found to correlate with potential for flooding. Since these units are important for evaluation of geologic hazards, the 2010 update of the geologic map includes a subdivision of Jennings “Q” into younger alluvium “Q” and older alluvium “Qoa”. In general, younger alluvium was deposited in Holocene time and represents the modern deposition in flood plains and on alluvial fans. Older alluvium is generally of Pleistocene age and represents depositional systems that are not currently active. References (for Part 1 and Part 2) Blake, W.P., 1857, Geological report, in Williamson, R.S., Report of explorations in California for railroad routes (from Mississippi River to the Pacific Ocean) 1853 [Senate Ex. Doc. no. 78], v. 5, pt. 2, 310p. Guillemin-Tarayre, Edmond, 1871, Description des anciennes possessions mexicaines du nord: Paris, France, Mission Sci. au Mexique et dans I'Amerique Centrale, Geologie, pt. 2, 216 p. Ireland, William, Jr., 1890, Report of the State Mineralogist: California State Mining Bureau tenth annual report, 983 p. 7 Jahns, R.H., 1961, Geologic Map of California, Olaf P. Jenkins edition: Economic Geology, v. 56, no. 6, p. 1154-1156. Jennings, C.W., 1965, 1:750,000 geologic map project: Memo to lan Campbell, Chief California Division Mines and Geology, December 30, 1965, 8 p. Jennings, C.W., 1975, Fault map of California with location of volcanoes, thermal springs, and thermal wells: California Division of Mines and Geology Geologic Data Map No. 1, scale 1:750,000. Jennings, C.W., 1977, Geologic Map of California: California Division of Mines and Geology Geologic Data Map No. 2, scale 1:750,000. 5 February 2015 California Section Newsletter Marcou, Jules, 1883, Note sur la geologie de la Californie: Soc. Geol. France Bull., 3d ser., v. 11, p. 407-435. Smith, J.P., 1916, The geologic formations of California with reconnaissance geologic map: California State Mining Bureau Bulletin No. 72, 47 p. ATTRACT-RETAIN-ENGAGE: Meetings to Inspire Presenter Steve Baker, an official California Section Mentor, works the crowd in a job searching skills workshop. 8 AIPG CALIFORNIA SECTION – UC DAVIS STUDENT SECTION MEETINGS March 2015 AIPG California Section – UC Davis Student Section Meeting featured Steve Baker, an official California Section Mentor providing a workshop on networking, job hunting skills, dressing for success at the interview and how to be better prepared for the challenges of the job search. He discussed jobs versus careers, and participants practiced getting up and introducing themselves to the crowd. Fortunately, the room was a friendly audience. Another meeting is planned in the future to discuss the subtle art of resume writing, posting and social media issues, improved networking for the young and experienced job hunter. UC DAVIS STUDENT SECTION PRESIDENT TIMOTHY NELSON Timothy Nelson, formerly manager of Ground Zero Skate and Snowboard of Davis, California, has been a Student Researcher and Geochemistry Student Lab Assistant while at UC Davis pursuing his undergraduate degree in geology. He is also the 2015 UC Davis Student Section President who with the team of the advisor, sponsor and student mentor, has had a successful string of monthly meetings since October 2014. Tim will graduate soon, and we wish him well with his career. 9 Tim, like the previous president, Richie Winn, has made a sizeable contribution to the UC Davis Student Section and we thank him for his efforts. Thanks again Tim! PROFESSOR ZIERENBERG- 2010-2015: 5 YEARS AS UC DAVIS STUDENT SECTION ADVISOR. Professor Robert A. Zierenberg has been the UC Davis Student Section Advisor since the founding in 2010. AIPG California Section appreciates his commitment to the UC Davis Student Section for the past five years. Professor Zierenberg, or “Z” as he likes to be called, is an expert in a variety of topics, including aqueous geochemistry; stable isotope geochemistry; economic geology. Research has focused on water/rock interaction in active and ancient hydrothermal systems, including the "black smokers" on the mid-ocean ridges. Research topics include the geology and geochemistry of sulfide deposits and hydrothermal alteration in seafloor hydrothermal systems and on-land analogs. Hydrothermal activity at sediment-covered portions of the northern Juan de Fuca Ridge and southern Gorda Ridge seafloor spreading centers have been a long term research interest, including participation in Legs 10 139 and169 of the Ocean Drilling Program. The Iceland Deep Drilling Project is providing new opportunities to investigate water/rock interaction in the deep, high-temperature roots of hydrothermal systems. Other interests include the environmental effects of mining, particularly the generation of acid mine drainage, mercury contamination in Clear Lake related to the abandoned Sulphur Bank Hg mine, the geochemical and biological cycling of sulfur, and sulfur isotope geochemistry. SUCCESSFUL SELF-INTRODUCTIONS It may be more art than science, but introducing oneself by standing up in a public dinner meeting is not all that easy. It takes practice and nerve to try to appear calm and intelligent. All participants in the recent March 2015 AIPG California Section – UC Davis Student Section meeting had the chance to get up and prepare an impromptu self-introduction. The trick is to give just enough information to be interesting and appealing, while not wearing out the welcome. ATTRACT-RETAIN-ENGAGE CAMPAIGN The AIPG California Section has an official mentor program to encourage regular and sustained involvement with the students, young professionals and senior members. This goes along with the concept of “attract-retain-engage” which is the focus of the California Section. Attraction occurs by getting students and young professionals interested in AIPG. We provide free meetings, free electronic versions of The Professional Geologist and free membership to students. We retain members by providing a simple value proposition: the cost and efforts associated with membership are far less than the benefits received. The value proposition is not a complicated equation. We engage our membership by having high-quality publications, meetings, training events, and professional activities. STEPHEN BAKER: OFFICIAL AIPG CALIFORNIA SECTION MENTOR Stephen J. Baker, MEM-2353, is an official California Student Section Mentor. There is a different level of commitment than just showing up to meeting occasionally. That means he helps plan student section meetings, goes to the meetings and related programs, and works with students and AIPG members on their career goals and job hunting challenges. Steve exemplifies the make-it-happen attitude of the professional geologist trying to give back to California geology students and the professional community. Steve has participated in more than half a dozen Annual Sacramento Drive-In legislative days with AIPG and other groups. He started attending the AIPG California Section meetings on a random basis several years ago. By 2013 he agreed to be an official AIPG California Section Student Mentor, and has consistently been in attendance at the California AIPG - UC 11 Davis Student Section meetings. In the past few years, there have been 8 monthly meetings and one or two field trips every year, and as an official AIPG Student Mentor, Steve has participated in almost all the meetings and a recent field trip. He gave two presentations at the AIPG California Section meetings, including a well-received workshop about job hunting skills and career development in March 2015 featuring resume writing, interviewing and networking skills. In helping the profession in California, Steve participated as an AIPG Student Mentor at the 2015 International Goldschmidt Conference in Sacramento where he spoke about career development to about 95 enthusiastic geology students. In 2014, Steve developed the “Meet Your Mentor” internet radio program to connect real mentors in the water industry with listeners who have interest in training and education in vocational and academic schools, finding a job, continuing education, ethics education and dealing with setbacks experienced in the industry. He has interviewed seasoned professionals and has piloted the project in California. Based on the initial success of the program, with appropriate funding, Steve plans to take the Meet Your Mentor Program nationally. Professionally, Steve not only started his own groundwater consulting company and ran it for over 29 years, but more recently, he has produced a short segment radio series that guides the listener in feeling and intellectually understanding the importance of water in their lives. “Water is a Many Splendid Thing” series of short-segment (3 to 8 minute) radio broadcasts that explore water’s relationship in the world. Two hundred forty seven segments have been produced to date. They are designed as public outreach pieces and to be easily understood. The radio show is popular and locally, Steve is known as “the Water Guy.” As a founding member of Operation Unite®, he has given workshops for communities, neighborhoods and private individuals interested in developing groundwater sustainability strategies and management programs. He also facilitates round table discussions of real situations in communities and public meetings. Some of these meetings are live or recorded radio broadcasts. Stephen J. Baker has given a lot of his time and energy to the California Section and mentoring activities and his efforts are appreciated! California from space (ESA) Have a good spring 2015! James A. Jacobs, C.P.G. #7760; California Section President Tel: 510-590-1098; [email protected] Website: www.jamesajacobs.net Clearwater Group, 229 Tewksbury Ave., Pt. Richmond, CA 94801; www.clearwatergroup.com 12
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