Background
Doell was born in Oakland, California in 1923 and grew up in Carpinteria, California.
Doell was born in Oakland, California in 1923 and grew up in Carpinteria, California.
University of California, Berkeley.
This work was a major step in the development of plate tectonics. After serving for 2 years as a combat infantryman during World World War II, he resumed his studies at University of California Berkeley, where he earned his doctorate in geophysics in 1955. Following graduation, Richard held teaching positions at the University of Toronto and Massachusetts Institute of Technology. Richard joined the Geological Survey Geophysics Branch in Menlo Park, California, in 1959 where he specialized in research on the Earth’s magnetic field and remanent magnetization in rocks.
Furthermore, isotopic dating of the rock samples provided the first time scale of polarity epochs for the last 3.2 million years.
The timed sequence of reversals, with subsequent refinements by this United States Geological Survey team and others, proved to be a major component of the plate tectonics revolution in the mid-to late 1960s. lieutenant not only provided the basis for confirming the hypothesis of sea floor spreading, but it also was a technique for quantifying rates and amounts of crustal plate movements on a global scale.
Richard served as President of the American Geophysical Union’s section on Geomagnetism and Paleomagnetism from 1968 to 1970 and as Chief of the Geological Survey’s Branch of Theoretical Geophysics from 1967 to 1971. In 1978, Richard retired from the United States Geological Survey to pursue his passions for the new field of environmental studies, sailing, exploration, and photography.
Having built a 38-foot sailboat, Muau, he began a series of long sailing cruises to Alaska, French Polynesia, and northern Europe.
Doell died in his sleep on March 6, 2008, at his home in Point Richmond, California, following a series of grave illnesses.
National Academy of Sciences]
He was an integral member of a team that presented convincing evidence of periodic polarity reversals of earth’s main magnetic field by analyzing magnetization of rock samples collected from widely separated, geologically young, volcanic sequences.