From: Subject: Hubbert's Peak, About Ken Deffeyes Date: Tue, 13 Jun 2006 15:41:24 +0530 MIME-Version: 1.0 Content-Type: multipart/related; type="text/html"; boundary="----=_NextPart_000_010A_01C68EFF.D38066D0" X-MimeOLE: Produced By Microsoft MimeOLE V6.00.2900.2869 This is a multi-part message in MIME format. ------=_NextPart_000_010A_01C68EFF.D38066D0 Content-Type: text/html; charset="Windows-1252" Content-Transfer-Encoding: quoted-printable Content-Location: http://www.princeton.edu/hubbert/about-ken.html Hubbert's = Peak, About Ken Deffeyes

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Kenneth S. Deffeyes
B58A2 Guyot Hall=
Princeton University
Princeton NJ 08540

Phone: (609) 258-3597
Fax: (609) 258= -1274
Email: deffeyes@princeton.edu

Biography

Ken's grandfather, Elie Deffeyes, brought the family name over = from=20 Etrubles, a French-speaking village in what is now Italy. The=20 pronunciation "d-phase" occurs in the definition of frequency: =

Ken's other grandfather was a cowboy who drove cattle on the = Chisholm=20 Trail. Taking advantage of his Chickasaw ancestry, he settled on = one of=20 the best pieces of farmland along the trail, in what was then the=20 Chickasaw Nation.

Ken's parents, Hazel and J. A. "Dee" Deffeyes, grew up on farms = in=20 Oklahoma before the automobile transformed rural life. They were = in the=20 first generation of their families to go to college: both = graduated from=20 Oklahoma State University. Although they began careers in = teaching, Dee=20 soon found a job in the expanding oil industry. At that time, = petroleum=20 engineering was being invented from scratch. One family legend = holds that=20 Dee was nearly fired for inventing the acidizing process. He = remembered=20 that hydrochloric acid would dissolve limestone, which would = improve the=20 porosity around the well bore. His boss remembered that = hydrochloric acid=20 should also dissolve the steel pipe in the well. What we now call=20 "passivation" saved both the pipe and Dee's budding career.

Although Ken was born in the pit bottom of the Great = Depression, 1931,=20 his father was able to keep his job on through the Depression. One = of=20 Ken's earliest memories was being a temporary refugee from the = Dust Bowl.=20 In those days, oil company employees were moved to where the = action was:=20 Wichita, Hutchinson, Great Bend, Midland, Hobbs, Great Bend again. = In=20 1944, Dee joined the Getty group and was based in Casper, = Wyoming.

For a high-school kid, Casper was not a bad place to develop = interests.=20 Mineral collecting was fostered not only by the geologic diversity = on=20 nearby Casper Mountain but also by coaching from two distinguished = geologists: Paul Walton and Jack Fanshaw. (A few years later, as a = college=20 junior, Ken and his buddies from high school revisited one of the=20 pegmatite quarries on Casper Mountain. On the quarry face were = large flat=20 black crystals. Ken could hear his mineralogy instructor's voice = saying=20 that columbite-tantalite was the only mineral with a semi-metallic = luster,=20 high density, and high hardness. Ken announced that the black = crystals=20 were columbite-tantalite, an identification later confirmed by = X-ray=20 fluorescence.) In high school, Ken developed an interest in = skiing, won=20 first prize for lapidary work at the Wyoming State Fair, and = danced the=20 lead role in the Chippewa feather dance at the Wyoming State = Fair.

A career-interests test was part of the freshman orientation = program at=20 the Colorado School of Mines. Dean Burdick told Ken that he seemed = to be=20 in the appropriate profession, but teaching was a close second. = Although=20 Ken insisted at the time that he wanted to be an oilman, Burdick = replied,=20 "Teaching is a good racket." Those tests may actually work.

Although Ken was majoring in petroleum geology, geologists were = required to take a beginning course in petroleum engineering. In = the first=20 lecture, the professor said, "We date the birth of petroleum = engineering=20 from the invention of the bottom-hole-pressure gauge." Ken almost = fell out=20 of his chair because his father and three other guys cranked the = first=20 bottom-hole-pressure gauge by hand into a well in Oklahoma City. = Along the=20 way, Ken earned a varsity letter for ski racing and at graduation = won the=20 Coolbaugh Award for undergraduate work in chemistry.

As a senior, Ken was offered a job by Shell Oil. When he called = for=20 advice about accepting the job, his father's first words were, = "Don't go=20 to work for Texaco." Ken's career with Shell was interrupted by = being=20 drafted into the Army right at the end of the Korean War. After = earning an=20 expert-rifleman's badge during basic training, Ken was assigned to = a unit=20 in the Corps of Engineers that produced topographic maps-at the = Presido of=20 San Francisco. Ken learned the lithographer's trade and also = learned that=20 there were restaurants serving foods other than Middle Western=20 meat-and-potatoes. He ate his first pizza at age 22.

The Army had been shunting geologists, engineers, and = architects into=20 the topographic map unit at the Presidio. One of the architects, = as a=20 student, had known Eric Mendelsohn, an important founder of modern = architecture. Mendelsohn had recently died and his widow had = approached=20 the University of California Press about publishing a collection = of=20 Mendelsohn's architectural drawings. She was turned down because = the=20 drawings were smudged and would require an enormous amount of hand = work to=20 prepare copies for publication. A portfolio of Mendelsohn's = drawings was=20 published, unknowingly, by the Army Corps of Engineers. One = regret:=20 Einstein was a friend of the Mendelsohn family; Mendelsohn = designed the=20 Einstein Tower in Potsdam. Ken was scheduled to hand deliver = Einstein's=20 copy of the completed portfolio to Princeton in the fall, but = Einstein=20 died that summer.

As his revenge on his draft board, Ken wanted to go to graduate = school=20 in the most expensive place he could find. Ken got accepted into=20 Princeton's master's degree in geological engineering. The largest = gap in=20 his education at that point was sedimentology, so he began his = graduate=20 study with Prof. F. B. Van Houten. That gap turned into a career = in=20 sedimentology.

Drafting all the Depression babies into the Army at the end of = the=20 Korean War had an odd aftereffect. Two years later, graduate = schools,=20 Princeton included, could pick from a double set of applicants: = regular=20 college graduates and military veterans. Ken found himself = surrounded by a=20 wonderful collection of fellow students and a fabulous faculty. =

Ken's proposal for his Ph.D. thesis was examining volcanic ash = beds in=20 the Nevada basins to see whether some of them might be distinctive = markers. Like a good boy, Ken tried the idea out on half a dozen = very=20 distinguished geologists. Each of them said it wouldn't work, but = each=20 gave a different reason why it wouldn't work. Ken tried it anyway; = that's=20 what youth is for. It didn't work, but for a reason given by none = of the=20 six experts. Most of the volcanic ashfalls had been altered to = minerals in=20 the zeolite family. At Prof. Van Houten's suggestion, Ken = published a=20 review paper on zeolites in sedimentary rocks. Two surprises:

The review paper, and a memorable 1958 field trip with = geologists=20 from Union Carbide, founded the natural zeolite industry. (The = world's=20 finest specimen of mordenite, on display at the American Museum = of=20 Natural History, was collected by Ken on that field trip.)=20
The Journal of Sedimentary Petrology reprinted the zeolite = paper in=20 their 50th anniversary volume.

In the fall of 1958, Ken rejoined Shell at their research = laboratory in=20 Houston. It was an incredible postdoctoral education. = Top-of-the-line=20 physicists, mathematicians, and chemists were there, eager and = willing to=20 collaborate on geological problems. Progress was incredibly rapid. = The=20 biggest single thrill was discovering the first marine-related = modern=20 dolomite and finding the modern analog of the two types of = dolomite=20 described in 1916 by F. M. Van Tuyl. (Extra sweet, because Van = Tuyl taught=20 Ken freshman geology at the Colorado School of Mines.)

At the very top of the top-of-the-line staff at Shell was M. = King=20 Hubbert, curmudgeon. Hubbert was enormously productive and a = fearsome=20 opponent in a controversy. Harry Hess, who was the geology = chairman at=20 Princeton, asked Hubbert more than once whether he had met = Deffeyes yet;=20 Hubbert kept saying, "No." Hubbert finally rang Ken's phone and = asked him=20 to come downstairs for a chat. To Hubbert's great embarrassment, = he had=20 been occasionally sharing lunch tables with "Ken" for more than a = year,=20 but never got the "Deffeyes" part. From then on, Hubbert was a = good=20 friend.

Before there was FORTRAN, there was BELL. Ken started computer=20 programming in 1957 in a low-level language called BELL, and = learned=20 FORTRAN in 1959. Amongst programmers, 1959 was in the Late = Pleistocene.=20 Around 1980, he switched to BASIC on a personal computer, but he = still=20 makes an occasional lapse into FORTRAN.

Ken left Shell in 1962 for two reasons: 1) Reworking Hubbert's = 1956=20 prediction using 1962 data showed that U.S. oil production would = be down=20 to half of its peak size when Ken would retire in 1998. 2) Shell = was=20 planning to shift its primary research effort to the Netherlands. = Sputnik=20 had gone up and American graduate education was expanding. Ken = took off=20 for the University of Minnesota.

After being on the Minnesota faculty for all of three days, Ken = got a=20 phone call from the Minnesota Fish and Game Commission. In = Minnesota lakes=20 that precipitated calcium carbonate, fish would survive but would = not=20 grow. The lake would be populated with small elderly bass. The = Fish and=20 Game people had done traditional alkalinity titrations from the = ice=20 breakup through until late fall. To analyze their data, Ken = developed what=20 is known today as "Deffeyes' diagram"; rhymes with "phase = diagram." Around=20 1970, Ken generalized the concept. His next project after = "Hubbert's Peak"=20 is a book and software package for constructing Deffeyes' = diagrams.

Collaboration with Peter Weyl, which began at Shell, continued = by=20 correspondence after Weyl moved to Oregon State. After 1.5 = Minnesota=20 winters, Ken joined Weyl in the oceanography department at Oregon = State.=20 Ken made the unhappy discovery that he was a major seasicker. = (Charles=20 Darwin's great fieldwork on land during the voyage of the Beagle = was=20 motivated in part by his seasickness.)

Before the 1960s, American geologists largely rejected = arguments for=20 continental drift. As it happened, an interesting article by L. C. = King=20 advocating continental drift arrived in Ken's AAPG Bulletin while = he was=20 isolated in the Army. Ken's reaction was that King's arguments = seemed=20 convincing. At Princeton in 1956, the faculty was largely against=20 continental drift. (Not quite solidly against. A. F. Buddington, = the=20 beloved Dr. Budd, gave a lecture saying something was needed to = explain=20 the Permian glacial striations in South Africa. The = undergraduates,=20 mimicking McCarthy-era usage, announced that Buddington was "soft = on=20 continental drift.") In 1960, Harry Hess launched the scientific=20 revolution by writing about sea-floor spreading. Suddenly, = Princeton=20 largely lined up for continental drift. In October of 1965, Fred = Vine=20 published a paper showing a portion of the actively spreading = midocean=20 ridge just 100 miles off the Oregon coast. Ken had the shortest = commute of=20 any oceanographer to the midocean ridge. In November, Ken asked = for time=20 on the Oregon State ship to explore the Gorda Ridge. This was an = agenda=20 worth getting seasick for. In December, Ken dredged fresh, fresh = black=20 glassy basalt from the axial valley and hydrothermally altered = basalt=20 (greenstone) from the shoulder of the axial valley. Joyous side = effect:=20 Ken learned that he got over being seasick after the first three = days.

Dredging rock from the deep ocean was a new skill. Oregon State = sent=20 along a biology graduate student who had some experience getting = otter=20 trawls on the ocean floor. It was like the oil business of the = 1930s,=20 winging it. Ken wanted to use a pressure-time recorder to = establish the=20 depth of the rock dredge. Pressure-time recorders, = "bathykymographs",=20 existed but they were too fragile to survive a ride on a rock = dredge. It=20 dawned on Ken that "bathykymograph" was synonymous with = "bottom-hole=20 pressure gauge." Another call to his father located the = manufacturer of=20 the most rugged bottom-hole pressure gauges and Ken still has a = Kuster=20 AK-1 (an "Amerada bomb" to the old-timers) that survived many = dredge hauls=20 on the rocky sea floor.

A 1970 paper by Ken on the midocean ridge described the Oregon = State=20 work and contained what, to Ken, were two mathematical surprises. = Ken had=20 been a "B" student in calculus. However, a simple integral of a = cosine=20 allowed calculating the total amount of new sea floor appearing = each year:=20 exactly one square mile. (As you know, God doesn't use metric.) = The second=20 math surprise was subtle. In beginning calculus, L'Hopital's rule = stated=20 that if the numerator and denominator of an expression are both = zero, take=20 the derivative of the numerator and denominator and divide again. = Ken's=20 reaction as an undergraduate was that he would very likely reach=20 retirement age long before an instance of L'Hopital's rule turned = up. But=20 there it was, written on a scale of kilometers across the floor of = the=20 midocean ridge. At the exact center of the axial valley, the = spreading=20 velocity is zero and the cumulative basalt supply is zero. Divide = their=20 first derivatives and basalt two kilometers thick appears on the = floor of=20 the axial valley.

Ken took a substantial salary cut to join the Princeton faculty = in=20 1967. His early primary obligation was teaching the introductory = course:=20 Rocks for Jocks. In 1968, Ken's beginning geology course featured = Harry=20 Hess, Fred Vine, and Jason Morgan as visiting speakers on three=20 consecutive Fridays. It was like having Copernicus, Galileo, and = Newton=20 show up in freshman physics. One of the litmus tests for the = existence of=20 a scientific revolution is rewriting the textbook for the = beginning=20 course. In 1972, Ken joined Sheldon Judson and Rob Hargraves in = writing=20 the first introductory geology textbook organized around plate=20 tectonics.

For three years in the early 1980s, Ken served as master of = Stevenson=20 Hall, an undergraduate dining and social facility. (A recipe for = whitefish=20 pate is in the FRS Cookbook on this web site.) One of the = compensations=20 for the effort was a semester's leave after the three years. Ken's = aptitude for learning languages has always hovered near zero. Ken = chose=20 the University of Cambridge because they (sort of) spoke English. = The=20 department chairman at Cambridge was Ken's graduate school = classmate, Ron=20 Oxburgh (who is now a life peer, The Lord Oxburgh of Liverpool.) = After Ken=20 asked if there were anything he could do to help, Ron suggested = helping=20 teach the first-year students on an excursion to Scotland.

Each Cambridge natural-science student was required to take a = one-week=20 course on the Isle of Arran in Scotland. James Hutton, in 1785, = had=20 examined Arran as part of his foundations of modern geology. Ken's = role=20 was the outsider: how would an American oilman react to an area as = intensively studied as any in the world? One was to welcome the = Cambridge=20 students to former North America. Once they crossed the Iapetus = suture,=20 they were on the northeastern extension of the Appalacians. Ken = had=20 earlier had an out-of-body experience: he walked into the map room = of the=20 Princeton library and saw a geologic map unfolded on the first = table. From=20 a distance, the map looked like a spectacular display of what were = becoming known as "exotic terrains", strips of differing geology = that had=20 been pasted together along fault lines. Ken thought the map must = be of=20 Tierra del Fuego or someplace equally exotic. Turns out he was = looking at=20 the map upside down, it was Scotland, where geology was born! The = Isle of=20 Arran is Scotland in miniature. Specifically, is the Highland = Boundary=20 Fault an exotic terrain boundary? It has testable consequences on = Arran:=20 none of the older geologic units should be present on both sides = of the=20 fault.

When Ken started to learn about the geology of Arran, something = seemed=20 dimly familiar. After two weeks, he figured it out. Thirty years = earlier,=20 his undergraduate petrology textbook was written by G. W. Tyrrell = who also=20 wrote the 1928 book, "The Geology of Arran."

Meanwhile, back at the ranch, Jason Morgan had been bugging Ken = about=20 giving first-year students an opportunity to learn geology in the = field.=20 The Cambridge course on Arran was unlike an American field trip. = Americans=20 tend to barrel down the highway, hop out to examine a roadcut, and = pile=20 back in the vans. The Brits put their students out for the day, on = foot=20 with a map, a lunch, and a canteen. It felt like doing real = geology. The=20 opportunity was to steal the Cambridge agenda and to add = spectacular=20 American geology. Bob Phinney suggested Mammoth Lakes, California = with=20 active faulting, recent glaciation, and young volcanoes. After = three=20 sessions looking for suitable one-day study areas, the first = Mammoth Lakes=20 trip happened during the mid-semester fall break in 1988. After = Princeton=20 initiated a program in Freshman Seminars, the Mammoth field trip = became=20 the longest-running seminar in the FRS program. When Ken retired = from=20 teaching in 1998, he became the program's cook. See his FRS = Cookbook on=20 this web site.

Ken did geologic field work when the occasion called for it, = but he did=20 not deliberately search out field opportunities. He found lab work = equally=20 enjoyable. However, even without trying, he participated in field = trips=20 and field work in Turkey, Greece, Kenya, Tanzania, Nepal, = Krygyzstan,=20 Peru, Taiwan, Indonesia, and the Netherlands Antilles. He worked = in all=20 the states from the Rocky Mountains to the west coast.

Nevada remained a special interest. The Great Basin is so = complex that=20 one geologist's career is not long enough to decipher more than a = part of=20 the history. In his small way, Ken did contribute to keeping the = MX=20 missile out of the Great Basin. When it was first planned, the MX = was to=20 have 10 launch sites for every real missile and trucks would = continuously=20 be shuttling dummy missiles and real missiles from site to site = through a=20 large portion of the Great Basin. Further, each MX carried 10=20 independently targeted nuclear warheads. The MX was a "silo = buster", a=20 destabilizing weapon because it would be most effective if = launched in a=20 preemptive strike.

While working on his Ph.D. thesis, Ken found millions of tons = of=20 erionite, a mineral in the zeolite family, which had previously = been known=20 only from a single mineral specimen in the Harvard museum. Ken's = first=20 published paper was a redescription of erionite; it was his baby. = Around=20 1980, erionite was found to be associated with a high incidence of = cancer=20 in three villages in Turkey. When researchers at Mt. Sinai = Hospital=20 injected rats with the same dosage of erionite that they used for=20 asbestos, the rats didn't live long enough to get cancer. At a=20 much-reduced dose, the rats did get cancer. Erionite is probably = the most=20 toxic known mineral; a milligram of fibers in the lungs is lethal. = Ken's=20 reaction on learning that his baby was a mass murderer was like = all=20 parents of mass murderers: "I don't understand it, erionite was = such a=20 nice quiet mineral."

If the U.S. Air Force dug up half of the Great Basin to base = the MX=20 missile, they would inevitably dig up some erionite. Ken's first = reaction=20 was to make a buck: sell the Air Force some consulting time. He = went to=20 the Pentagon, whopped a one-kilogram chunk of erionite on a = colonel's desk=20 and announced that it was enough to kill a million people. The = colonel=20 phoned the group writing the environmental impact statement for = the MX and=20 asked about the zeolite problem. The reply was "zeolite?" After = many phone=20 calls, the Air Force contractor told Ken that they didn't want him = around=20 their environmental impact statement until they were "ready to = refute your=20 arguments." OK, you want an opponent; you got one. Ken called = Walter=20 Sullivan at The New York Times, told him where to find articles on = the=20 erionite hazard, and Sullivan took out after the problem. Ken = started a=20 search for additional erionite localities, a search financed out = of his=20 family's grocery budget. Nothing appeared in the Times. Ken = finally got a=20 senior Times editor on the phone, who said the story wasn't news. = Articles=20 about the Turkish villages were a year old. Ken was able to add = news: he=20 had found erionite in the only low mountain pass connecting two = big=20 sections of the proposed MX missile bases. The Times finally ran = the=20 story, but buried the article in between the obituaries at the end = of the=20 financial section. Thud. Nobody noticed. Well, one person noticed. = A=20 reporter for the Salt Lake Tribune called and asked for more = information.=20 Ken gave him the colonel's phone number at the Pentagon. The Salt = Lake=20 paper kept the "desert cancer mineral" story alive for several = days. And=20 later the Church of Jesus Christ of Latter Day Saints in America,=20 Incorporated came out against the MX. There is an old saying, = "Politics=20 makes strange bedfellows." Ken never expected to crawl into bed = with the=20 Mormons. The Reagan administration eventually abandoned the Great = Basin=20 basing mode for the MX.

Although officially retired, Ken wakes up every morning with = more work=20 than he can do. He taught geochemistry one semester at Bryn Mawr. = (All=20 male college professors have fantasies about teaching at a women's = college.) Writing and consulting more than fill up the time. His = only=20 nonprofessional hobby is curating a collection of desert purple = glass=20 inherited from his parents.

=A9 2001=972006 - K. Deffeyes All Rights = Reserved.
site by Deffeyes Design =

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