GSW: 1990 MEETING MINUTES

 

MINUTES OF THE GEOLOGICAL SOCIETY OF WASHINGTON

1194th Meeting,  January 10, 1990

     President Simkin called the meeting to order promptly at 8:00 PM.   69 attendees were present at the beginning of the meeting and these numbers swelled to 71 with the late arrival of Dick Fisks and his entourage.   The minutes of the 1193rd slightly irregular meeting were submitted by Brooks Hanson, read by Bruce Wardlaw, and, nevertheless approved as read.   10 guests were introduced,  including visitors Chris Vinyl from University of Tennessee and Tim Johns from the University of Arkansas, one from the Smithsonian,  3 from NRC,  2 from JTM, and Chip Parrott by self-introduction.   No new members were announced.   The President pointed out that membership forms are available.   There were no other announcements,  informal communications, or old or new business,  causing the slow-writing secretary to misspeak.

     Of special interest this meeting would be the behavior of our recently retired luminaries E-an Zen and Gene Robertson.   Gene seemed to be overly full of vim and vigor, hounding every speaker that he could.   But E-an was sadly quiet for questions for the first speaker, leaving us worried about the affects of retirement; BUT rose to his old form for questions to the second speaker.   I'm sure both Gene and E-an would have asked questions of the film had they been given the opportunity.

     The first speaker was Laurel Woodruff from the U.S. Geological Survey.   She presented "Stable isotope investigation of Mesozoic diabases".   Laurel reviewed ongoing work on magmatic intrusions (diabases)  of the East Coast Triassic basins, particularly the Culpepper basin.   chill margins are enriched in δ18O and there appears to be no oxygen exchange with the internal fluid.   A δ18O shift along veins appears to represent oxygen rich aqueous fluids.   Diabases are undersaturated with respect to sulfur and this is probably due to degassing with a major loss of volatile H2S from the residual melt.   The talk was a speedy 18 minutes, and provoked at least 5 real questions.

     The second speaker, Selwyn Saks, from the Department of Terrestrial Magnetism, Carnegie Institute, enlightened us on "Strain diffusion in the earth's crust:  Mantle viscosity and triggered earthquakes".   Unfortunately this stirring talk was presented with overhead transparencies.   Apparently,  structural seismically active troughs some 200 km from the subduction zone of the Japan Trench release stress (as earthquakes)  that moves the continental plate away from the subducting plate which allows it to slide some 36 years latter.   This is due to the viscosity of the asthenosphere and strain/pulse propagation.  The talk was an even speedier 17 minutes. 11 questions were asked; Robin Brett missed a golden chance at a zinging analogy with "Is it flea bites elephant or flea falling off elephant?"  (probably better "or elephant stomps flea")  but he got to the heart of the matter of which event is really the driver.

     The third presentation was a film by Fiske, Duffield,  and Swanson, of the Smithsonian and U.S. Geological Survey, on "Inside Hawaiian volcanoes".   This slick production was offered for sale in the back of the room and has an accompanying teachers guide.   The film introduction and running time was 27 minutes.   No formal questions were allowed, and adjournment was called at 9:37 PM (obviously for a need of a beer).

     [signed Bruce R. Wardlaw]

 

MINUTES OF THE GEOLOGICAL SOCIETY OF WASHINGTON

1195th Meeting,  January 24,  1990

     President Simkin called the meeting to order at 8:00:57, barely making the 8 o'clock starting time.   I didn't realize that being minutes secretary really meant being a minute time keeper.   60 people were in attendance.   The minutes of the 1194th meeting were surprisingly approved as read.   4 guests were introduced, Jim Quick, Denver USGS, a-son-of-speaker, Jon Cross and his girlfriend Sara,  and some Jacques in the back.   Simkin called for volunteers for GSW administration; Simon groveled for pledges to the endowment as announcements to the meeting.   Four new members were announced: Robert Stamm, Chip Parrott, Peter Heaney, and Rodney Koozmin.   No informal communications or old or new business was introduced.

     The first speaker was Whitman Cross II, Red Mountain Museum, speaking on C.  (Charles) Whitman Cross:   from rocks to roses. Whitman Cross liked igneous rocks and roses but he didn't like Charles.   The speaker,  rather than being called after his namesake or as "half wit" became known as "Pete".   His Grandfather was one of the "four horseman",  a founder of GSW as  its  first secretary,  and a devotee of the University of Virginia.   He had a distinguished career with the Survey lasting 45 years.   This fascinating talk was cut in the quick at 21 minutes by an aggressive secretary and president.  There were 7 questions including ones by Rankin, Robertson, Toulmin, Simkin,  Zen, and Milton.

     The second speaker was Sandra H. B. Clark, U.S. Geological Survey, Reston.   She presented "Classification of barite deposits".   Her barite work is aided by two Barneys, Barite Barney Poole and Barite Barney Gallagher.   There are three basic types of Barite deposits: bedded, vein and cavity fill,  and residual.   The talk went 16 minutes and there were two questions; one each by Toulmin and Towe.

     The third speaker was Charles Prewitt (I don't know if this means he is from a family that precedes Whitman's and liked the name Charles or what?).   He (Charles)  is from the Geophysical Laboratory and he presented "Hydrous magnesian silicates:   water in the mantle?"   This work is a large collaborative effort by the Geophysical Lab and SUNY by 8 people.   Charles apologized for presenting his talk with overheads, especially after the secretary rammed a previous speaker for doing the same.   Charles, however, approached the audience rather than falling to that dread habit of addressing the overhead.   We learned that Phase B has a crystal structure of two different kinds of layers one similar to brucite and one with the characteristics of humite and forsterite and occurs in hydrous and anhydrous phases.   We don't know much about Phase E-and Phase C may not exist.   Water could be in a lot of phases and there is much more work to be done for the Mantle phase.   There 7 questions,  including 2 by Milton, and one each by Appleman, Toulmin, Zen,  Robertson,  and  Sorensen.

     The President quickly recognized the Current Program Chair, Sorena Sorensen, announced the next program and adjourned the meeting at 9:30 bringing this phase of GSW to an end.

     [signed Bruce R. Wardlaw]

 

MINUTES OF THE GEOLOGICAL SOCIETY OF WASHINGTON

1196th Meeting,  February 14,  1990

     President Simkin called the meeting to order at 7:59:28 to a crowd of 80 attendees.   The minutes were read, amended to delete all superfluous Charles'****, and approved as amended.   President Simkin announced there were AAPG membership forms available at the back of the room.   Treasurer Simon announced he had taken Draconian measures and there were no pretzels, chips, and half as much beer at the back of the room.   Reduction of the beer had been discussed at council meeting because of reduce audiences and a too heavy keg at the end of the evening; but the missing chips solely rest on Simon's shoulders. Jerry Barton of the Potomac Geophysical Society of Washington invited members to their next meeting featuring Grossling on climatic warming.   Dr. Sergei Khmelevtsov of the Institute of Experimental Meteorology, Obninsk, USSR was introduced.   A new member was elected to the Society in the back of the room prior to the meeting, Kenneth (mumbled last named, not recorded).   There was no other business and no informal communications.

     The first speaker, Brian Huber of the Smithsonian Institution talked about "Foraminifera:   Indicators of Late Cretaceous Climate and Paleo-oceanography.   Benthic foraminifers are good paleoecologic indicators and planktic foraminifers are good indicators of depth and latitudinal gradients, and surface patterns.   With detailed paleomagnetic stratigraphy can determine latitudinal and vertical gradients and the source of bottom waters in the Late Cretaceous.   We learned that keeled ornamented planktics mean stratified surface waters (they occur at depth).   High latitude waters cooled through the Maastrichtian,  show converging water masses, and bottom waters had a probably Antarctic source.   The talk was 21 minutes,  included overhead transparencies and 4 questions were asked by Burke (2), Segovia, and Stifel.

     The second speaker,  Peter Heaney of the Smithsonian Institution, presented "The many faces of Quartz: a TEM study of Agates".   Agates are concentrically banded nodules of layers of chalcedony (cryptocrystalline)  and quartz  (coarse crystalline)  SiO2.   Chalcedony differs from Quartz in that it has 1-2% H20,  it is elongate in an axis normal to that of quartz  (C),  it is twisted about its elongate axis,  it has a planar disorder, has structural superperiodicities and intergrowths.   This can all be analogized to quartz being layers of Wonder Bread and Chalcedony being a series of PB&J sandwiches with OH and H2O being the PB and J.   The slides to this talk showed some disorder in going in reverse several times (NO operator error).   The talk was 21 1/2 minutes, questions by Dennis, Milton, Toulmin and Simkin.

     The Third speaker, Kevin Burke, National Research Council, presented "Catastrophes:   The State of the Art", presented on overhead transparencies and based essentially on the Snowbird I and II Catastrophes (ah, catastrophic conferences).   This exciting series of anecdotes stressed that the less exciting things  (like solid research and documentation) are not being done and need to be so that the likes of Kevin can get up and give a new exciting series of anecdotes of personal and global catastrophes  The talk was 21 minutes.   Huber asked 2 questions about shocked quartz, Michael 2 about soot, Appleman 2 about impact structure size and timing being off; Zen and Robertson were not present but would have asked questions at this time; and additional questions by Milton, Cross, Jeffries, and Hanson.  Simkin quickly announced the next meeting and adjourned at 9:39:50.

     [signed Bruce R. Wardlaw]

 

MINUTES OF THE GEOLOGICAL SOCIETY OF WASHINGTON

1197th Meeting,  February 28,  1990

     Though President Simkin made a call to order promptly at 8:00, the unruly crowd of 83 attendees could not be fully brought to order and the meeting was begun at 8:01:43.   The crowd included several visitors and at least 8 of them were introduced:  Anne O'Donnell, State Dept., a Tamera from OSM, two Russians who'll have to forgive me for not getting their names, Jim Straw, and three USGS luminaries, John Barron, Charlie Bacon, and a person better known for her Pick and Hammer pseudonym, Christine Turnip-Potato Head.

     Gene Robertson announced,  in an irregular manner, that he spoke for Nick Van Driel in announcing a consultant seller of computer graphics.   The GSW field trip on Saturday, April 28, on Metapelitic rocks of the Baltimore Gneiss Terrane was announced, and mapping jobs appear to be available with Coastal Engineering.

     We finally had our first informal communication of the year.  Dick Fisk introduced us to ongoing activity at the Hawaiian Volcano Observatory which included pictures of a lava fall, the "fire hose", and a lava artist.

     Gray Bebout, Geophysical Laboratory, presented the first formal talk,  "Volatile recycling by devolatilizaton of subducted sedimentary and mafic rocks--field geochemical evidence."   This talk showed us that in subduction zones there is a slab-derived volatile component given to the mantle wedge.   A series of supporting isotopic trends, especially the homogenization of oxygen isotopes convinced us?. The case study was the Santa Catalina Schist Complex and somehow throughout the talk I was reminded of the old refrain,  "26 miles across the sea, Santa Catalina is a'waiting for me,  Santa Catalina the island of romance,  romance,  romance,  romance".   21 minutes and questions by Wright, who thought it was the other way, higher to lower, Rumble, who agreed with low to high flow, Hanson,  Zen one for Bruce,  and Towe.

     The second speaker was Russell Blong, Macquarie University,  "AD 1700 eruption in Papua New Guinea: evidence from thick ash and Huli legends".   Through solid detective work, we learned that the time of darkness was probably the time of deposition of the Tibito Tephra when sand fell from the sky,  from eruption of Long Island 300 years ago.   Running time 21:44, questions by Bacon, Robertson, Stifel,  Zen and van Oss.

     The last speaker was George Wetherill, Department of Terrestrial Magnetism,  "The earliest history of the Earth" who enjoyed sharing the platform with the author of Genesis.  Molecular cloud contracts, planetesimals form, planetesimals accumulate, runaway accretion gives embryos and most stuff is impacted, so what's new?  Things go bump in the night, the earth forms,  is partially melted, has 300 deg. K surface temperatures, an a heck of a high initial heat flow. 20 minutes, questions by Toulmin, Robertson, van Oss, Galvin, Towe, Zen.

     The next meeting was quickly announced by President Simkin and the meeting was adjourned at a late 9:46:16.

     [signed Bruce R. Wardlaw]

 

MINUTES OF THE GEOLOGICAL SOCIETY OF WASHINGTON

1198th Meeting, March 14,  1990

     President Simkin managed to get three calls to order on the order of two minutes, and the meeting began at 8:00:55.   Continuing on our ever increasing attendance, no doubt due to the superlative efforts of Sorena Sorensen to capture imaginative speakers,  91 people were present.   7 visitors were introduced including Mike Brown, the new chairman of Geology at Maryland, new members of the Smithsonian staff, Judy Kulum and Tom Gordon, Dave Rohr of Sul Ross State University in Alpine Texas, the gateway to Big Bend Country, and a Doug, Dick and Julie.   8 new members were announced, including the elusive Timothy Moore, who all council members couldn't remember a few meetings ago (group amnesia, but we did take his money).   Other new members include:   Diane Bellis, Terauki Ishii, Michael Brown, Marty Power, Wayne Mandell, Anne O'Donnell, and Brian Huber, who after we invited him to speak thought we were a worthwhile enough organization to join.   We were beleaguered with announcements,  7: Potomac Geophysical society Meeting, Science Fair help see Fred Wilson, the GSW field trip, Pittsburgh Geological Society Meeting on Carbonates, AAPG Heritage of English Geologists, and Help E-an's kids at McLean High School, Virginia Junior Academy,  and Piedmont Environmental Council.

     Tom Dutro presented our second informal communication of the year, spectacular slides of Millford Sound, New Zealand, for the benefit of Brian Mason, a New Zealandite, who has never seen the sound unshrouded.   The talk showed that even a paleontologist can appreciate a granulite if put in proper perspective (6:32).

     The first formal speaker was Raymond Jeanloz, U.C.  Berkeley, presenting "Deep mantle corrosion:   The ultimate metasomatism?"  Studying the largest magma chamber,  looking at the core/mantle boundary between liquid iron alloy core and solid mantle oxides, highlighting the "zone of dregs",  the diffusion zone.   Unable to visit his field area he uses a diamond anvil cell to simulate high temperature/pressure conditions of the mantle/core boundary.   Put Perovskite next to iron and we get physical penetration of oxygen into iron, forming metallic melts.  Mixing yields metal alloys and alloy rich regions create magnetic anomalies  (or something like that).   Approximately 3 questions by Moto Sato, One each by Stewart, Milton, Shirey, Robertson, and Robin Brett wanting to know what happened to "Ma Bell" experiment.  (20 minutes).

     The second speaker was Bryan Isacks,  Cornell University,  speaking on "Tectonic (we're not talking climatic tonight)  interactions and the evolution of the Central Andes".   Armed with spiffy imagery, Bryan explained why the Altoplano is so alto y plano.   It has to do with shifting your slopes of your Benioff zone like so.  (18:30, scared to a stop by the secretary's first alarm).   Questions by Zen and Hanson.

     Our last speaker, Hatten S. Yoder, Jr., Geophysical Laboratory, spoke on "Geophysical Laboratory:   Scientific contribution 1905-1990 and the U.S.G.S. heritage".   It appears that the successful Geophysical Laboratory amassing 2166 publications since 1903, was largely initiated and staffed by Survey employees and has periodically been reinvigorated by the Survey.   Prompting Dave Stewart to moan why can't the Carnegie Institute and Geophysical Lab invigorate the Survey.  Other questions and points of interest, like Becker left an endowment to the Smithsonian which now pays for Fiske's research, by Fiske and Robertson.  The Geophysical lab will be moving to the DTM campus and there is a Geophysical yearbook out with the history of the organization.  The talk ran 23:36.

     The next meeting was quickly announced and President Simkin adjourned the meeting at 9:43:44.

     [signed Bruce R. Wardlaw]

 

MINUTES OF THE GEOLOGICAL SOCIETY OF WASHINGTON

1199th Meeting, March 28,  1990

     An unruly and massive crowd of 118 attendees kept President Simkin from the podium, so he was unable to call the meeting to order until 8:01:26.   The meeting began noisily at 8:01:55.   Had the beer guzzlers sat down, nearly every seat would have been filled.   Seven visitors were introduced including Bill Davis from National Parks, Maggie Dillie, William Keffner, Daly and Alice Dennington, Herb Black, and an Egyptian.   New member Tom Jorstad was elected at,  oddly enough, a regular council meeting today and was so announced.   The passing of Izzy Adler was announced and a moment of silence observed.   GSW participation in local science fairs, earlier believed dormant, may be surviving in rural parts of Virginia.   Ann Wylie discussed details of the upcoming GSW field trip on April 28; interested trippers are to meet in the parking lot of the Adult Education Center at U.M.   There was no new business nor were there any informal communications.

     The first speaker was Mary Jo Baedecker, U.S. Geological Survey, presenting "geochemical alterations of ground water by crude oil".  Mary Jo conducted a detailed study of an oil lens at subsurface water table,  its plume, and the anoxic and restricted oxygen lenses below the oil lens created in the oxygenated ground water in glacial outwash in northern Minnesota (an available field area, because no one cared).   The talk ran 18:40 and there were five questions by French, Towe, Milton, 2 by Rye, and a point of information by Wardlaw.

     The second speaker, Chris Fiedler, FBI,  spoke of "Applied forensic geology at the F.B.I.:   Some 'case' studies".  Chris awarded Sorena Sorensen a coveted FBI hat for duties rendered in the past.   Forensic geology deals with the 3 "C's", crap,  crud, and corrosion and can be dumped into those with class or individual characteristics.   Just as our speaker was getting warmed up and about to present some case examples, his time was waning, so he tripped quickly through some cases, and abruptly ended at 23:45.   3 questions all by French and we learned to use our computers, not old typewriters,  if we're thinking of doing anything sinister to Robin Bret.

     The final speaker was Mark Meier, University of Colorado, presenting "Global warming,  ice, and rising sea level:   Run, the glacier is melting!".   Through 20 minutes of ocean warming, alpine glacier-retreating (except recently), big ice-sheet thickening, iceberg-counting, and meltwater-watching, we learned that not much is changing, but a small rise will have a major impact (Bruce is glad to know that).   At least 9 questions were asked by Towe, Robertson, Hanson, French (2), Tracey,  Zen, and anonymous in a red sweater.  Meyer Rubin, from Isotope Branch (or what's left of it), got up, noted that isotope geologists are slow to respond, and proceeded to ask the first speaker a question, and then surprised everyone by also asking the last speaker a question.

     President Simkin quickly announced the next meeting and adjourned at 9:46:38.   At 10:15 the keg was floating.

     Absent-mindedly submitted, Bruce R. Wardlaw (read by J. Thomas Dutro, Jr.)

 

MINUTES OF THE GEOLOGICAL SOCIETY OF WASHINGTON

1200th Meeting, April 11,  1990

     President Simkin called the meeting to order at approximately 8 o'clock.   Several guest were introduced, but their names were not recorded by the acting secretary.   Tom Dutro, surrogate secretary for Bruce Wardlaw, read the minutes of the 1199th meeting and they were approved as edited by Dutro.  An informal communication by Cyrus Galvin was related to sea-level rise and beach erosion predictions.  He pointed out that the most recent USGS map on rising and falling sea levels along the U.S. coastline bears little resemblance to reality when checked against available data for specific stretches of coast.   The map lacked a defender in the audience.

     The first speaker, Chris Kincaid of the Department of Terrestrial Magnetism, presented results of laboratory modeling of plate tectonics mechanisms.   His sugar-coated technique involved emplacing a slab of treacle onto a liquid surface so that by gravity alone the slab would penetrate the liquid, dependant only on the dip angle and density difference between the slab and the liquid.   Velocity was scaled at approximately 1/2 cm/yr.   Kincaid talked for about 19 1/2 minutes and then spent more than 5 minutes answering questions by Galvin,  Druid, Barton, Hanson, Taylor, Toulmin, Nancy Milton,  and Ryan.

     The second speaker, Mike Wise of the Smithsonian, discussed color variation of accessory minerals as indicators for evolution of pegmatites.   Rare elements are significant in zoned pegmatites,  where accessory minerals tend to occur in swarms; they increase and occur as coarser crystals away from granite contacts.   color change is most sensitive in tourmalines, but apparently they don't behave very well.   Garnets are ubiquitous.   Properly evaluated, mineral color can be a useful field criterion.   After 20 1/2 minutes, Mike answered questions by van Oss, Toulmin, and Robertson.

     The last speaker, Bob Hamilton, quondam chief geologist of the U.S.G.S., told us all we wanted to know about the mid-continent New Madrid seismic zone.   Although it's the most active zone east of the Rockies, there is not much chance if a major quake in the near future.   Hamilton stated that there is no evidence of compression; he apparently favors a diapirism mechanism.   After his 20 minute talk, Bob spent more than 15 minutes answering questions by Dave Stewart (3), Kevin Burke  (2), Robertson, Ryan, Druid, Kincaid, Toulmin, and Simkin.

     Attendance was 68.   President Simkin, after announcing the program for the next meeting, adjourned the meeting about 10 minutes shy of 10 o'clock.

     Respectfully submitted, Tom Dutro

 

MINUTES OF THE GEOLOGICAL SOCIETY OF WASHINGTON

1201st Meeting, April 25,  1990

     Tom Simkin called the meeting to order late, because the acting secretary from the meeting before insisted on the unprecedented reading of his own minutes and he was late to the meeting.   The meeting began at 8:04.   123 were in attendance.   Tom Dutro (van Oss) read the minutes (Hendrik van Oss) and they were approved as (Hendrik G. van Oss)  corrected.   Hendrik G. van Oss's name was corrected in the minutes.   Three visitors were introduced, a student from N.C. State, an aerospace-head, and Mike Nelson.   The usurper lost the names of new members, which were finally announced from the floor by Kathleen Kozey Krohn and include:   Judith Calem, Sue Cox, G. William Davis, William G. Miller, and John Osweiler.   A death was announced and a moment of silence observed.   The Spring field trip was announced.   Leann Milton announced something about volcano workers.  There were no informal communications.

     Continuing on an irregular vein, an irregular meeting (unnumbered)  of the Geological Society of Washington in a special joint meeting with the Potomac Geophysical Society was held on September 27 at the Fort Meyer Officers' Club and featured Walter Alvarez as speaker.   The minutes of this meeting were taken dutifully by the GSW meeting secretary and will be incorporated in the annual report.   It was learned that the PGS has no meetings secretary and records no minutes.

     The first speaker, Gautam Sen from Florida International University, spoke on "the mantle under Hawaii: a xenolith story."  Xenoliths incorporated in posterosional volcanism represent mantle or magma/wall rock cumulate samples.   Sen differentiated these and showed Us the lithosphere is substantially heated up. Sen tried to convince us he was at the cutting edge of science by using a knife as a pointer.  He rushed through his transparencies, ending his talk in 15:45.   Questions were asked by Peck, Robertson (sort of two), unidentified, and Ross (sort of three).   The secretary uncharacteristically bolted for a beer.

     The second speaker, Dallas Peck, Director of the U.S. Geological Survey presented "U.S. Geological Survey:   Outlook for the 21st century."   This surly veteran of 13 years at the stewardship of the USGS talked of the Survey past,  present,  and future.   There were no slides, so I have to assume the picture is bleak.   We can depend on a big earthquake in Southern California, an extended drought, and climate deterioration or change to aid future funding.   The talked lasted 20:30 and evoked 8 questions, mostly pleas from employees, including Sato (2), Ross (2), Jingle-Ruppert, Justice, van Oss, and Mac Ross.

     The third speaker,  Tom Casadevall, U.S.G.S.,  regaled us with "Jet aircraft and volcanic ash clouds--or,  'This is your captain speaking...is there a geologist on board?'  "   There have been 5 near fatal aircraft encounters with ash clouds in the last 10 years.   The geologist,  specifically the USGS, needs to monitor active volcanism, assist research of material properties of ash clouds, and educate the public and air transportation industry on the hazards of flying a big jet through an ash cloud.  We need to know and distribute information on the time eruption starts, the altitude of the top of the eruption cloud and whether the cloud contains ash.   Areas that should be keenly monitored are Indonesia, Japan, and the U.S.A.  The talk ran 25:20.  There were six questions by Peck, Toulmin (2), Gluskoter, Sato, and Krohn.

     The meeting was adjourned at 9:50:45.

     [signed Bruce R. Wardlaw]

 

Minutes of the Geological Society of Washington in a special joint meeting with the Potomac Geophysical Society (unnumbered)

Thursday,  September 27,  1990

     The Social Hour (cash bar)  started at a 6:30 p.m.,  Dinner at 7:30 p.m.   The formal meeting was supposed to start at 8:30 p.m. but due to the dinner crowd of 88 and the extensive drinking, the meeting did not start until after 9:00.   Total attendance was 132.   Karl Veith called the meeting to order and announced that the PGS generally meets on the third not fourth Thursday during the speaking season and something about the SEG in San Francisco.   Tom Simkin called for nominations for an AGU medal, announced the next GSW field trip and the next GSW meeting.

     Tom Simkin than introduced the speaker, Walter Alvarez, better known to Tom for his piano-playing and parties,  from the University of California,  Berkeley.   His talk was titled "The terminal Cretaceous event:   the impact after 10 years."   The speaker started at 9:06:30.   We revisited the Gubbio section in Umbria,  Italy; a nice place to get grant money to visit.   We saw a bunch of unreadable stratigraphic sections  (even if we were sober)  to show more detailed work is going on.   (I guess you have to take a lot of this on faith).   We also saw big forams go to small ones in an instant, Iridium,  spheroids, and the "white layer".   The impact site may be in the Caribbean or may be subducted.   This rather fascinating update on impact extinctions generated 7 rather in-depth questions.   Being on foreign turf, the secretary was unable to identify most of the questioners, except for Kevin Burke.   Zen and Robertson asked none.

     [signed Bruce R. Wardlaw]

 

MINUTES OF THE GEOLOGICAL SOCIETY OF WASHINGTON

1202nd Meeting,  October 10,  1990

     In the absence of Bruce Wardlaw, who is in West Texas, the minutes will be mercifully brief.   Tom Simkin called the meeting to order at 8:01 pm.   70 people were in attendance.   Two visitors were introduced (Patti Swain and a distinguished Russian, Andre Tsvetkov).   The following 11 new members were announced:  Mary E. Turner, David Lescinsky, Patti Swain, Candace Martin, Richard J. Walker, S. Richard O'Day, Robert L. Lamons, Robert J. Tworkowski, Michael R. Nelson, Heather L. Collins, and J. Michael Palin.   The passing of Bill Davies and Charlie Milton was announced and a moment of silence was observed.   The fall field trip was announced.   E-an Zen reported that the Education Committee, Geoscience Division will meet at the G.S.A.   Brooks Hansen presented an informal communication.   The secretary, noting that there was gunk all over the table, thus smearing the notes, missed most of what was said of fluid flow at depth.   The communication lasted 9 minutes.

     The first speaker, Mike Brown, University of Maryland, presented "The late Archaean Qorqut granite complex of southern West Greenland:   a colorful story of black and white rocks".   We learned the history of some very old contorted rocks and their three zones.  3 questions were asked.

     The second speaker, Jim Hibbard, North Carolina State University, presented "Ridge prints in the muds of time:   Miocene spreading ridge subduction in southwest Japan".   We saw just what happens when a ridge indentor subducts contorting the countryside.   5 questions were asked.

     The third speaker,  Ian MacGregor, National Science Foundation, presented "Subduction eclogites and kimberlites!"   Kimberlites are our sampler of mantle eclogites, some of which represent ancient subducted oceanic crust.   3 questions, with a very long two by Sato were asked.

     All in all,  it was a very subdued evening.   The meeting was adjourned at 9:58 pm.

     Respectfully submitted, Bruce R. Wardlaw (read by Robert G. Stamm)

 

MINUTES OF THE GEOLOGICAL SOCIETY OF WASHINGTON

1203rd Meeting, October 24,  1990

     I apologize for my technician delivering the minutes at the last meeting.   The one primary and one backup alternate secretary did not show leaving my shy technician the horror of standing before you and the further horror of reading my minutes.   The only saving humor he could find that night was not letting President Simkin know the minutes were in hand until the final minute.   I'll try to reconstruct the meeting from the varied notes and scribbles left me.   The meeting began innocently enough at 8:04 pm.   81 people were in attendance.   5 visitors were calmly introduced.   These included Jonathan Kishen, Kevin Malone, George Plumel, a suspicious Women named only Susan,  and Guy Hovis.   The slate of council nominees for next year was discussed and is listed on this meetings announcement.   Tom Nesser presented an informal communication on Wagners continental drift theory in picture form,  1 minute.   Then it happened  ....  The lights went out.    How can you write anything in this darkness  ....  And how do you start this stupid egg timer.   The first speaker, Ken Towe of the Smithsonian, speaking on "Aerobic carbon cycling on the early Archean Earth"   was half way through the Archean, when the timer was finally subdued and abandoned,  left on the floor for the evening.   Facing now the crisis of the darkness, why did the speaker keep talking about Fe203, the burial of organic carbon, and the freedom of Oxygen.   Suspicious speaking for a government employee.   The lights came on and the dead egg timer was quietly placed out of sight. Three questions were asked.

     The second speaker, Jim Hays of the National Science Foundation, began speaking on "Earth sciences at NSF", the lights dimmed before I had a chance to recover my notes...Ah, the darkness again.   The history of NSF earth sciences was barred on the screen,  28 grants to 400 in 38 years, with a happy inflation-beating projection for 1993. The-the egg timer,  its not dead, but ringing.   Stifle it,  Stifle it, where is Peter Stifel when you need him.   8 questions were asked, including one from Robin Brett.

     Joe Boyd, Geophysical Laboratory, gave us "Mining diamonds from A to Z:   Argyle to Zarnitsa, the dope on diamonds from Australia, Africa, and Russia.   Better edified on the "rocks" we confidently buried the egg timer beneath the carpet.   Six questions were asked, Brett again chirping in.   The evening was suspiciously quiet from Zen and Robertson,  leading me to suspect, they were missing or asleep! The meeting was adjourned at 9:44 pm.

     Edited and rewritten from bleary handwritten notes and presented by Bruce R. Wardlaw

 

MINUTES OF THE GEOLOGICAL SOCIETY OF WASHINGTON

1204th Meeting,  November 14,  1990

     The meeting was promptly brought to order by President Simkin at 8:00 pm.   83 somewhat alert people were in attendance.   The minutes were surprisingly approved with the minor change of Havans to Hovis. 5 guests were introduced: Marti Turdito, NHM, Chip, AGI, Janet Johnson, and Gary Epsen and Bob Johnson of MMS.   There were three announcements:   The AAPG Pittsburgh '91 Meeting, a self-serving announcement by the president of openings in global volcanism at the Museum, prompting Mark McBride to announce that Dames and Moore are looking for six good men/women.   Jane Hammarstrom,  in order to warm up for her future role as secretary, presented an informal communication attempting to inform us of the International Archive of Economic Geology in Laramie, Wyoming, as a significant resource.

     The official egg timer, shot at the previous meeting, was still recuperating, and unavailable to time and aggravate speakers.

     The first speaker, Steve Leatherman, University of Maryland, spoke on "The day Hurricane Hugo came knocking at my beach house door".   This 100 year event came ashore with 125 mph winds,  a 20 ft surge at Bulls Bay, and did tremendous damage to beach houses.   All in all, the speaker convinced us that the rapidly decaying Foley Island should be renamed Folley Island.  The talk ran a short 16:48.  Questions by Gohn, Simkin, anonymous, French, Sy and Zen.

     The second speaker, Margo Kingston, USGS, delivered "A bird's eye view of two North American carbonatites with airborne imaging spectroscopy".   We saw Mountain Pass, California and Iron Hill, Colorado, carbonatites and learned that igneous carbonates display a unique combination of spectra (carbonate,  iron, and multiple neodymium bands)  and dense foliation causes problems and needs a flat field correction.   The talk ran a short 17:40.   3 questions by Hammarstrom, Robertson, and Zen.

     The final speaker, Chris Newhall, USGS, showed us "Unrest at Iwo Jima--precursor of a caldera-forming eruption?"   Iwo Jima (Sulfur Island) shows marked uplift, a conservative 20 cm/yr, on the NE side and surrounding rocky shoals and probably represents an actively resurgent dome with magma 2-4 km below.   Yeah,  it's gonna blow.   It represents an unique opportunity to study a large scale caldera eruption because it is isolated and lacks population.   Why do I feel this was a funding request?  The talk ran a lengthy 23:26 and there were 11 questions by Sato, Shirey, Sy, Herron, Zen, Keith, Robertson, McClelland, anonymous, Milton, and Tracey.

     The last regular meeting was announced and President Simkin adjourned the meeting at 9:39:23.

     [signed Bruce R. Wardlaw]

 

MINUTES OF THE GEOLOGICAL SOCIETY OF WASHINGTON

1205th Meeting,  November 28,  1990

     Soon-to-be past president Simkin attempted to bring the meeting to order at 8:00:55.   72 people were in attendance.   The minutes were approved as read.   7 guests were introduced, Caroline Edwards and Mike Hamilton of DTM, Peter Stifel introduced two University of Maryland students (who were also induced to become members in the back of the room), and David Palmer, Barry Bone, and Pat Okito.   5 new members were elected at council and 4 new members were elected in a huddle in the back.   These include:   Guy Hovis, NSF, Joseph B. Jurinski, NuChem, Ned Mamula, Terradynamics, Jennifer A. Smith, Earth Technology, Allan E. Dewall, Army Corp of Engineers, Margaret Chauncey and Teresa Messina introduced as guests, and John Nay, all from the University of Maryland, and Laurel A. Muehlhausen, NACLS.   It was announced that the Carnegie Institution of Washington  also has talks, call 202-234-6869.   There were no informal communications.

     The first speaker,  Klaus Schulz, USGS,  spoke on "An early Proterozoic ophiolite in the Penokean orogen, northeastern Wisconsin".   He told us what we should expect in an ophiolite complex in the Proterozoic and Archean and proceeded to document one,  and by all things, mostly by field observations.   What a refreshing new ideal   Sheeted dikes are of utmost importance and the Niagara fault zone appears to be a forearc/craton suture.   The talk was exactly 20 minutes.   Questions by Brooks Hanson and Zen.

     Susse Wright, Geophysical Laboratory, then spoke on Paleozoic epiric seas:   oxygen isotope perspectives from shells and seawater." Both brachiopod shells (calcite)  and conodont skeletal elements (apatite)  indicate too high temperatures in the Paleozoic and perhaps this is related to the fact that epeiric seas were much more extensive then and were partly decoupled isotopically from the open oceans.   The talk ran 16 minutes.   Three questions were asked, two by anonymous and one by Zen.

     Guy Hovis, NSF, gave the final presentation,  "Calorimetric research:   memories of Dave Waldbaum, and recent results on nepheline-kalsilite."  Guy, quickly overcoming the problems of the slide advance which plagued speakers all evening, showed us that quality research can be carried out at a small university (Lafayette College) with proper NSF support.   In the thermodynamic mixing properties (heat of solution) of nepheline, tetrakalsilite and kalsilite,  silicon is a major player.   Gene Robertson joined Guy in honoring the exacting Dave Waldbaum.   The talk lasted just 10 seconds short of 20 minutes.

     President Simkin quickly announced the atypical regular/annual meeting/presidential address and the new slate of officers and adjourned the meeting at 9:20:02.

     [signed Bruce R. Wardlaw]

 

MINUTES OF THE GEOLOGICAL SOCIETY OF WASHINGTON

1206th Meeting, December 12,  1990

     President Simkin brought the restless and boisterous crowd of approximately 123 moving attendees to order at 8:01:00.   The minutes were approved as corrected, replacing girls with students.   9 guests were introduced including the Hanshaw clan (both of Peggys folks), a Miller, Marty Giaramita, John Dean,  Sergei Meshinko, the Bridas, and a Duke.   There was a brief announcement of AAPG anniversary charter members.   There were no informal communications.

     Paul Barton then took the podium to introduce "the president of global volcanism since 1894" and the retiring president of the GSW, Tom Simkin, who presented the presidential address,  "The caldera of Volcan Fernandina, Galapagos:   its ups and downs in the last few decades".   Tom quickly disclaimed that the observations were not entirely his own, but those of a succession of travelers, who took time to observe something other than the thin skin of biota on the rocks.   Fernandina is a summit caldera with concentric fissure vents and eruptions generally 3-5 km from the center of the caldera and is characterized by central caldera collapse.   Tom dramatically documented several spectacular collapse and landslide events in the central caldera.   Tom closed remarking on his Galapagos calderas and "Their drudging impulse for horizontality", missing a golden opportunity to notice the same thing of the general GSW audiences.  The talk ran 56 minutes and 55 seconds, no questions were allowed at the discretion of the President, and the meeting was adjourned for 15 minutes of beer guzzling before the 98th Annual Meeting would commence.    

     Respectfully submitted,

     [signed Bruce R. Wardlaw]

 

MINUTES OF THE GEOLOGICAL SOCIETY OF WASHINGTON

98th Annual Meeting, December 12, 1990

     President Tom Simkin resumed the festivities of the combined regular and annual meetings at 9:31:10. The minutes of the previous year's bacchanal were approved as corrected. Then proceeded a series of boring reports, the meetings secretary, Bruce Wardlaw's annual report questioning Robertson, approved as commented, the council secretary, Brooks Hansen's annual report, approved as read, the treasurer, Fred Simon's report, fund, fund, fund, the audit committee report, Dick Tollo approving so both reports were approved, the membership committee report by Kathy Krohn which needed no approval, the public service committee report, science fairs by Frank Ireton and field trips by Ann Wylie and read by Mike Brown, and finally the Centennial Committee report by Gene Robertson.

     The came the real meat of the evening - the Bradley and Great Dane committee report. The Great Dane was awarded to Cy Galvin for his informal communication on beach erosion.  The Bradley Award for best paper seemed to have every speaker from the year receiving honorable mention, but the runner-up, second best paper of the year, was awarded to Mark Meier, for his paper on global warming, Run the glacier is melting! The best paper, cup, and check were awarded to Bob Hamilton for his report on the New Madrid seismic zone.

     The Sleeping Bear Award was presented by Dick Fiske. Several worthy members of the society, Schulz, Stewart (a perennial favorite), and Simkin were considered. The award was clearly won by Tom Dutro for his remarkable eying of the petrologists section of the auditorium during his comment "gneiss view".

The new slate of officers was approved by acclamation and everybody in the room was honored, including the standing members of the council, the projectionist, and Sorena Sorenson as program chair. She was awarded the first and last "bringing them out on a cold winter's night award" by President Simkin for her excellent program selection that increased attendance.

     Finally, the gavel and Robert's Book of Rules were turned over to Paul Barton, the next meeting announced, and the meeting was adjourned at 10:42:10.