Tanya Atwater

Tanya Atwater (born 1942) is an American geophysicist and marine geologist who specializes in plate tectonics. She is particularly renowned for her early research on the plate tectonic history of western North America.
Early life and education.
Atwater was born in Los Angeles, California in 1942. Her father was an engineer and her mother was a botanist. Atwater was one of the first women to research the ocean floor in terms of its Geology.
Atwater began her education in 1960 at the Massachusetts Institute of Technology, then received her B.A. in Geophysics from the University of California, Berkeley in 1965. She earned a Ph.D. (1972) in marine geophysics from Scripps Institution of Oceanography, University of California, San Diego. She is director of the University of California, Santa Barbara Educational Multimedia Visualization Center where she is an emerita professor of geological sciences. She was a professor at the Massachusetts Institute of Technology before joining the faculty at UCSB in 1980. Atwater retired from UCSB in 2007.
Career.
Atwater was a professor of tectonics, in the Department of Geological Sciences at the University of California, Santa Barbara before retiring. She authored and co-authored 50 articles in international journals, professional volumes, and major reports. Seven of these papers were published in the journals "Nature" or "Science". In 1975, she became a Fellow of the American Geophysical Union for her work in tectonophysics. From 1975 to 1977, Atwater was a Sloan Postdoctoral Fellowship Recipient in Physics. In 1984, she won the Encouragement Award from the Association for Women Geoscientists. Atwater is a member of the National Academy of Sciences elected for her contributions to marine geophysics and tectonics. In 2019 she received the highest award of the Geological Society of America, the Penrose Medal.
Scientific discoveries.
Atwater was involved in oceanographic expeditions using deep towed instruments to explore the ocean floor. To date, she has participated in 12 deep water dives in the deep-ocean submersible "Alvin". She researched the volcano-tectonic processes responsible for creating new oceanic crust at seafloor spreading centers. In 1968, she co-authored a research paper featuring groundbreaking work into the faulted nature of spreading centers. With Jack Corliss, Fred Spiess, and Kenneth Macdonald, she played key roles in expeditions that uncovered the distinct biology of ocean floor warm springs, which led to the discovery during the RISE project of the high temperature black smokers, undersea hydrothermal vents.
In Atwater's research on propagating rifts near the Galapagos Islands, she discovered that propagating rifts were created when spreading centers along the seafloor were disturbed by tectonic movement or magma and therefore had to change direction to realign. This helped to explain the complex pattern of the seafloor.
Atwater is perhaps best known for her work on the plate tectonic history of western North America. She wrote two major research papers outlining the history of plate tectonic evolution of North America and tectonic problems of the San Andreas Fault, which assisted in documenting the history of the San Andreas Fault Line.
She also studied geometric evolution, integrating and comparing the global plate motion records with the regional continental geologic records. She found emerging relationships that revealed the origins of many large-scale geologic features (e.g. Rocky Mountains, Yellowstone, Death Valley, Cascade volcanoes, California Coast Ranges).
Atwater's research paper, "Implications of Plate Tectonics for the Cenozoic Tectonic Evolution of Western North America", established the essential framework for the plate tectonics of western North America. In her work, she explains that approximately 40 million years ago, the Farallon Plate was subducting underneath the North American Plate and the Pacific Plate. The lower half of the Farallon plate was entirely subducted under Southern California and the upper half did not sink, which eventually became known as the Juan de Fuca Plate.Since the southern section of Farallon completely disappeared, the boundary of southern California was now between the Pacific Plate and the North American Plate. The San Andreas Fault is unique because it acts as a major fault line as well as a border between the Pacific Plate and the North American Plate. She updated this work in 1989.
Atwater is interested in communication and education at all levels. She has developed electronic multi-media (Educational Multimedia Visualization Center at UCSB) to enhance geologic visualization and understanding, particularly related to the histories of tectonic plates.