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P.B. King - with Emphasis on the Iowa City Years
By Bill Raatz
Introduction
Philip Burke King (1903-1987; University of Iowa BS ‘24, MS ‘27) was one of the great geologic mappers of
the 20th century, spending most of his career with the USGS where he published works of such insight that
they remain the gold standard today. His West Texas publications covering the Marathon Basin, Glass
Mountains, Sierra Diablos, Hueco Mountains, and Guadalupe Mountains are venerated for their detailed
geologic interpretations, accuracy of mapping, and elegant hand-drawn illustrations. The Permian Basin
region is one of the most intensely studied areas on Earth, due to its economic importance as an oil and
gas province, and as an outdoor laboratory for examination of complex shelf to basin mixed carbonate
clastic depositional systems. King’s work created the foundation for our modern understanding of the
region. Despite the advent of satellite imagery, GPS, Lidar, Gigapans, drones and other modern tools, his
maps and observations stand the test of time.
Early Life Through Completion of Master’s Degree
King was born in Indiana but moved to Iowa City as a boy of five in 1908, following his father who was
Professor of Psychology and Education. He describes his life up until High School as “miserable” due to
bullying, as he had no aptitude for sports and was viewed as an introspective and bookish “stuck up
professor’s boy”. His father possessed an amateur interest in geology and was friends with Samuel Calvin,
whose fossil collection King envied. Unhappy with lack of promotion, King’s father left the university
during WWI to work a civilian job with the YMCA and was often away from home, creating a poor and
somewhat unsettled childhood.
King graduated from University High School (Iowa City) in 1920. Despite modern confusion, he received
his BS (1924) and MS (1927) from what is now the University of Iowa in Iowa City, at the time called State
P.B. King: Left from
University of Iowa
Hawkeye yearbook, 1924,
and Right circa 1965.
University of Iowa, leading some sources (e.g. Wikipedia) to incorrectly assign his alma mater as Iowa
State University (Ames, IA). He went on to receive his Ph.D. from Yale in 1929.
Upon entry to university life as a freshman, King described himself as “poor, shabby, and friendless” with
“few social graces”. One of his freshman courses was Geology in Old Science Hall (now Calvin Hall). The
Geology faculty all came from the University of Chicago, the leading Midwestern institution of the day,
and included George F. Kay (Head of Department, Dean, and State Geologist whom King described as “a
stuffed shirt” mainly interested in banning smoking from the building), Arthur Trowbridge (“a truly
dynamic guy”), Abram O. Thomas, Ralph C. Cheney (who left soon after for Berkeley where he attained
distinction), and Joseph J. Runner (“jolly and outgoing, quite a contrast with the rest of the department,
and something of a maverick; he shocked them all by talking seriously about continental drift”). C.K.
Wentworth was an Instructor, famous for publishing the Wentworth Scale for grain size classification in
1922. Wentworth invited sophomore King to attend his first field geology course at Baraboo, WI.
Wentworth “was a hard taskmaster” and “odd duck” who eventually gave King a ‘B’ grade, “which was
very generous of him”. As a junior, King learned plane-table surveying, also from Wentworth. In addition
to Geology, King took 3 years of art classes leading him to publish cartoons in a university humor magazine
and his senior year Hawkeye yearbook. His artistic skill is evident in his classic geology publications, which
are renowned for accurate field sketches. Socially the small group of art students became “the only real
attachments” he made at university.
Starting junior year, Prof. Runner took King under his wing and gave him an assistantship sorting out the
department’s mineral collection. That summer King worked as Runner’s assistant on a consulting job in
North Dakota, after which he visited Yellowstone Park, followed by Runner’s field geology course in the
Black Hills. This was his first taste of “the Great West” and the beauty of the country entranced him.
Returning “starry-eyed” to Iowa City he found it very dull by comparison. In his senior year, he took
Advanced General Geology from Prof. Trowbridge. Although in retrospect he felt some of the teachings
were “manifestly wrong”, the advanced study of topographic and geologic maps firmed up his interests,
and “Few young geologists in other schools ever got such rigorous map training.” Marshall Kay, son of
Dean George Kay, also took the class. Marshall went on to fame integrating tectonics and stratigraphy at
Columbia University, and is often associated with pre-plate tectonic Geosynclinal theory. King presented
his first scientific paper as a junior to the Iowa Academy of Sciences on the topic of physiography of
southwestern North Dakota.
King graduated in 1924 as a Phi Beta Kappa and With High Distinction. The Louden prize that year ($10)
was split between King and Marshall Kay. Socially, although he had friends in the Art Department, he
“…never dated anyone, and did not go to dances or other college affairs.” He took the Geological Survey
Civil Service exam and “…passed with a low grade of 73, but no Survey offers were made.” With no job
prospects presenting themselves, Prof. Runner again took interest in King by writing to an oil friend in
Dallas and getting him a position at Marland Oil Co. as Geological Assistant for $100 per month. Here he
purchased the Geologic Map of Texas and noticed that the peculiar area of the Marathon Basin and Glass
Mountains did not fit the well-ordered stratigraphic patterns found in the rest of the state. He transferred
to West Texas, where he would spend the next year surveying surface structures with alidade, plane table
and stadia – “the plane table had a wobble in it and was hard to keep level. We had a Model T Ford which
was always breaking down and getting many flat tires.” His social awkwardness continued, “The oil people
were a rough crowd, quite different from anything I had been exposed to in Iowa…a carousing, drinking,
whoring crowd. They made me the butt of their jokes, but other ‘nice boys’ were also picked on.”
In April 1925, King received a letter from his younger brother, Robert, who was graduating from Iowa with
a Bachelor in Geology and looking for a Master’s thesis topic focused on paleontology. P.B. decided to
quit the oil business and return to Iowa for graduate school, where he and Robert would work on the
geology of the Glass Mountains and Marathon country. The area had newly published topographic maps
but only reconnaissance level geology work, “…so the region was ready for geologic mapping”. The
brothers began the daunting task of mapping the exceedingly complex thrust-faulted terrane of the
Marathon region. While mapping, he met a group on their summer field course from the University of
Texas led by Prof. Whitney, and he shared his mapping results.
After a full summer of mapping, P.B. returned to Iowa City in the fall of 1925 to begin his Master’s work.
He took classes and had a graduate assistantship helping with the Geology 1 course. Although King
worked hard, he “…didn’t seem to accomplish much – later, I was to characterize it as ‘furious lost motion’.
I was much discouraged, but soon my fortunes were to take a dramatic turn for the better. Toward end
of October, I received an amazing letter from Prof. Whitney offering me a job as Instructor at University
of Texas at $1,800 per year.” The Iowa faculty permitted King to leave after Christmas, “They were much
surprised…because it was unheard of that anyone should get an Instructorship when he did not even have
a Master’s degree…”. In Austin, King spent much of his time at the Bureau of Economic Geology (also
housed on campus), and became friends with Bureau geologist John T. Lonsdale, a fellow University of
Iowa graduate. King “blossomed out” in Texas, leading many local field trips and working with the famous
paleontologist Charles Schuchert of Yale who was in Austin as visiting professor. Schuchert was interested
in the Glass Mountains region after his own visit there a number of years before determined it was a
critical section to understand the Permian of North America. Schuchert wanted Robert and P.B. to
continue their work and go to Yale for Ph.D.’s. He agreed to buy all of Robert’s Glass Mountains
paleontology collection for the Peabody Museum. “Up to then, I had no further plan than to get a Master’s
degree at Iowa; I had never conceived of the idea of getting a doctorate at one of the famous schools in
the East. So – Robert was to go to Yale the following fall, and I would follow next year, when I finished my
work at the University of Texas. Financing of further work in the Glass Mountains would come from a
subsidy from Professor Schuchert for the fossil collections, and from expenses that had been arranged by
Schuchert from the Bureau of Economic Geology.”
Robert E. King, P.B.’s younger brother and mapping
partner for the Marathon Basin, Glass Mountains,
Sierra Diablos, and Hueco Mountains of West Texas.
University of Iowa Hawkeye Yearbook, 1926.
For the 1926 field season P.B. and Robert based themselves in Alpine and Marathon, TX for further work
on the Glass Mountains/Marathon region. They took side trips to Carlsbad Caverns and the Guadalupe
Mountains, as well as the Sierra Diablos north of Van Horn – areas King would work in detail the following
years. Mapping went well, and “At the end of the season we drove back to Austin, and we both took the
train back to Iowa City, I for a short visit, Robert to go on to Yale, for his first year.” Returning to Austin
for his second semester as Instructor, King worked up the Geomorphology of the Glass Mountains and
Marathon Basin for his Master’s thesis at Iowa. “At Christmas, I went north by train to Iowa City, and
Robert came back from New Haven…I brought along my manuscript…and submitted [it] to the Geology
Department for a Master’s thesis. The Department gave me some written and oral examinations, and I
was given my M.S. degree…”
Excerpt from King’s landmark 1937 USGS publication Geology of the Marathon Region, Texas, illustrating
the complex thrusted and folded terrane of the area. Much of the basic fieldwork was completed with
his brother, Robert, while they were students at the University of Iowa.
Examples of King’s clear and fine artwork from King, 1937.
Ph.D. and Brief Synopsis of Later Life
Much of King’s work at Yale built upon the fieldwork he had begun as an Iowa student. The 1927 field
season included mapping the Sierra Madera hills which were “greatly confused, smashed, and jointed,
and hence hard to understand...”. The feature was later determined to be an impact structure, and
although not interpreted as such by King, it was correctly mapped. The Glass Mountains geologic mapping
was completed at the end of the 1927 field season, after which King headed east to New Haven to begin
at Yale.
P.B. and Robert moved their mapping area north in 1928 to the Hueco Mountains, where they “…found a
prominent angular unconformity at the base of the Permian…and to our surprise found that the Permian
beveled all the older formations southward…” It is now established this unconformity is part of the
Marathon-Ouachita tectonic event that formed the foreland Permian Basin, and is visible in outcrop and
seismic throughout the region. After finishing the Huecos, they set up doing fieldwork in the Sierra
Diablos. In 1929, P.B. finished his dissertation and went back to map the Marathon Basin area for the
USGS on a temporary assignment. Any future employment was uncertain, but in the fall of 1929, he was
offered a 1-year Instructor position at the University of Arizona teaching Introductory Geology. In June of
1930, he was back in the Marathon Basin working for the USGS, this time a permanent hire with an office
in Washington D.C. King married his wife, Helen, in 1932. His last major West Texas mapping project
(done without his brother Robert, who entered the oil industry) was the southern Guadalupe Mountains,
with most of the fieldwork completed over eight months in 1934-1935 and publication in 1948.
King had no great love for Iowa City and returned only sporadically through the 1930’s to visit family.
Some of this thoughts on Iowa include: “I have wondered how any one in Iowa City could have been
interested in the subject [of Geology], for it was a most uninspiring locale – a terrane of dissected Kansan
loess, without any distinguishing features of any kind…In spite of its uninspiring surroundings, the Iowa
department turned out many geologists, nevertheless, most of whom went into petroleum geology, and
many of whom distinguished themselves later…Possibly some of them, like me, found geology as a means
of getting away from the dull scenery and people of Iowa, into more exciting regions.”
In 1937, he returned to Iowa City for his father’s funeral, and during a 1938 visit saw his mother for the
last time. In 1939, he spent a month in Iowa City to deal with affairs and close up the family house. “While
there, I did what I could on the family estate…father’s affairs were somewhat tangled. Much of my time
was spent with Art Miller and Bill Furnish on the Permian, whose ammonoids they were working up into
a monograph. In the evening, Art and Bertha Miller took us sometimes to the Amana Colony about 12
miles west of Iowa City, where we ate lavish German dinners. We also spent a day…at Lake McBride, a
reservoir that had been built since my day…Finally, we packed up to go east, and I left Iowa City, never to
return.”
King would go on to look for strategic minerals during WWII in the Appalachia region, work that would
expand to extensive geologic mapping that would take up much of his later career. In addition, he
synthesized the Tectonic Map of North America (1969) and the Geologic Map of the United States (1974).
In 1965 he was awarded both the Penrose Medal by the Geological Society of America and the
Distinguished Service Medal by the U.S. Department of Interior, and in 1966 was elected to the American
Academy of Arts and Sciences. He held temporary teaching assignments at the University of Texas,
University of Arizona, UCLA, and the University of Moscow. He died in 1987 at the age of 83 in California,
having retired from the USGS at age 69.
After retiring, King wrote an autobiography from which most of the material in this article was
summerized, it is available through the USGS at:
https://pubs.usgs.gov/of/2000/of00-443/of00-443.pdf
Han
d dr
awn
sket
ches
of
the
Gua
dalu
pe M
ount
ains
fro
m K
ing
, 194
8: E
l Cap
itan
(a
bove
) an
d th
e W
est
Face
(be
low
).
King
bel
ieve
d, “
…th
at t
hese
dra
win
gs b
ring
out
man
y g
eolo
gica
l fea
ture
s m
ore
acc
urat
ely
tha
n p
hoto
gra
phs.
”
F. J
erry
Luc
ia, a
uth
or o
f th
e b
ook
Car
bona
te R
eser
voir
Cha
ract
eriz
atio
n (
1999
, 20
07),
sta
ted
“[K
ing
’s]
ske
tch
es
of
the
Gua
dalu
pe M
oun
tain
s a
re a
maz
ing
and
my
pho
togr
aph
s o
f th
e W
est
Face
onl
y a
dd s
ome
det
ails
an
d co
lor.
”
Excerpted detail of southern Guadalupe Mts, including El Capitan, Guadalupe Peak, and Schumard Peak,
from King, 1948. Prof. Lloyd C. Pray (University of Wisconsin-Madison), leader of Guadalupe Mts
research in the 1970’s and 1980’s, praised King by stating, “We are all just picking at the scraps and
bones” that King’s work left behind.
Selected major works:
King, Philip B., 1937, Geology of the Marathon Region, Texas, United States Geological Survey
Professional Paper 187, 148 pp.
King, Philip B., 1948, Geology of the Southern Guadalupe Mountains, Texas, United States Geological
Survey Professional Paper 215, 183 pp.
King, Philip B., 1959 revised edition 1977, The Evolution of North America, Princeton University Press
Tectonic Map of the United States (1944; 1962; 1989)
Tectonic Map of North America (1969)
Geologic Map of the United States (1974)