Bailey Willis

At 91 years old, Bailey Willis physical status not available right now. We will update Bailey Willis's height, weight, eye color, hair color, build, and measurements.

After receiving degrees in mining engineering and civil engineering, Willis worked from 1881 to 1884 as a survey geologist for Northern Pacific Railroad looking for sources of coal. Called the "boy boss" by work crews during his work looking for coal, he began studying the geology of Mount Rainier, the Cascade Range, and the Rocky Mountains. From 1884 to 1915, he worked for the USGS, being named director of the Appalachian division in 1889. In 1893 he published "The Mechanics of Appalachian Structure" in the Report of the United States Geological Survey. From 1895 to 1902 he lectured on geology at Johns Hopkins University. In 1900 he was appointed head of the Division of Areal Geology of the USGS. In 1903 he received a grant of $12,000 from the newly established Carnegie Institution of Washington to lead an expedition to northern China, an experience which was later described in his book Friendly China. From 1910 until 1914 he consulted for the government of Argentina an experience later recorded in his book A Yanqui in Patagonia. When he returned to the United States in 1915 he was named Head of the Stanford University Geology Department. He led a vigorous public campaign in the 1920s to raise awareness of earthquake hazards and safe building practices. It is claimed that many of California's early building codes were inspired by experiments performed by Willis on an "earthquake table" at Stanford University. Willis, concerned about the dangers of earthquakes convinced engineers to dig the foundation of the southern tower of the Golden Gate Bridge deeper. After finishing his work with the USGS, he was appointed as a professor and chairman of the geology department at Stanford University, where he served until 1922. In 1920, he was elected to the National Academy of the Sciences. He was president of the Seismological Society of America from 1921 to 1926, during which time he published his Geologic Structures. He was president of the Geological Society of America in 1928. On July 11 1927, while in Cairo, Egypt, he heard that a destructive earthquake struck the Holy Land. The day after, he took a private flight from Cairo to Palestine, Made observations of the impacted sites, and stayed there for several days to further investigate. A year later, he published his findings in the Bulitin of Seismological Society of America. In 1928, he published "Continental Drift" in the SP 2: Theory of Continental Drift, by the American Association of Petroleum Geologists, where he rejects the theory. Stating "After considering the theory of continental drift with avowed impartiality, the author concludes by means of geophysical, geological and paleontologic reasoning that it should be rejected, because the original suggestion of the idea sprang from a similarity of form (coast lines of Africa and South America) which in itself constitutes no demonstration, because such a drift would have destroyed the similarity by faulting, and because other contradictions destroy the necessary consequences of the hypothesis." In 1932, he published "Isthmian Links" in the Bulletin of the Geological Society of America.

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