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Tanya Marie Atwater
Tanya Atwater Galapagos Rift Expedition, 1982.jpg
Tanya Atwater on the Galapagos Propagating Rift expedition, 1982.
Born 1942
Los Angeles, California
Nationality American
Education Scripps Institution of Oceanography
Scientific career
Fields Tectonics

Marine geology

Marine geophysics
Institutions University of California, Santa Barbara
Thesis Implications of Plate Tectonics for the Cenozoic Tectonic Evolution of Western North America (1972)

Tanya Atwater (born 1942) is an American geophysicist and marine geologist. She is famous for her work on plate tectonics, which is the study of how Earth's large land plates move. She is especially known for her early research about the history of plate movements in western North America.

Early Life and Learning

Tanya Atwater was born in Los Angeles, California in 1942. Her father was an engineer, and her mother was a botanist. Tanya Atwater was one of the first women to study the ocean floor and its geology.

She started her college education in 1960. She earned her first degree in geophysics from the University of California, Berkeley in 1965. Later, she received her Ph.D. in marine geophysics in 1972. This degree was from Scripps Institution of Oceanography, which is part of the University of California, San Diego.

Tanya Atwater became a professor at the Massachusetts Institute of Technology. In 1980, she joined the faculty at the University of California, Santa Barbara (UCSB). She retired from UCSB in 2007. Today, she is an emerita professor of geological sciences. She also directs the Educational Multimedia Visualization Center at UCSB.

Her Work and Discoveries

Tanya Atwater was a professor of tectonics at the University of California, Santa Barbara. She wrote or helped write many articles in science journals and reports. Her important work led to her becoming a Fellow of the American Geophysical Union in 1975. This honor recognized her contributions to tectonophysics, which is the study of forces that shape Earth's crust.

In 1984, she won an award from the Association for Women Geoscientists. She is also a member of the U.S. National Academy of Sciences. This means she is one of the top scientists in the country. In 2019, she received the Penrose Medal, the highest award from the Geological Society of America. In 2022, she received the Wollaston Medal from the Geological Society of London, which is also a very high honor.

Exploring the Ocean Floor

Tanya Atwater took part in many ocean trips to explore the ocean floor. She used special tools that could be towed deep underwater. She even made 12 dives herself in a deep-ocean submarine called Alvin.

She studied how new ocean crust is made at places called seafloor spreading centers. These are like underwater mountain ranges where Earth's plates pull apart. In 1968, she helped write a paper about how these spreading centers are often broken by faults.

She also played a key role in expeditions that found unique living things near warm springs on the ocean floor. These discoveries led to finding very hot "black smokers." These are undersea hydrothermal vents that shoot out hot, mineral-rich water.

Understanding Plate Movements

Tanya Atwater studied "propagating rifts" near the Galápagos Islands. She found that these rifts form when spreading centers on the seafloor are disturbed. This can happen because of plate movement or magma (melted rock). When disturbed, the spreading centers have to change direction. This discovery helped explain the complicated patterns found on the ocean floor.

She is perhaps most famous for her work on the plate tectonic history of western North America. She wrote important papers that explained how the plates moved in this region. Her work helped us understand the history of the San Andreas Fault.

She also studied how global plate movements connect with regional geology. She found links that explained how many large features on Earth were formed. These include the Rocky Mountains, Yellowstone, Death Valley, Cascade volcanoes, and the California Coast Ranges.

Her research paper, "Implications of Plate Tectonics for the Cenozoic Tectonic Evolution of Western North America," created the main framework for understanding plate tectonics in this area. In her work, she explained that about 40 million years ago, a plate called the Farallon plate was sliding under the North American plate and the Pacific plate. The lower part of the Farallon plate completely slid under Southern California. The upper part did not sink and is now known as the Juan de Fuca plate. Because the southern Farallon plate disappeared, the boundary in Southern California became directly between the Pacific plate and the North American plate. The San Andreas Fault is special because it is a major fault line and also the border between these two large plates. She updated this important work in 1989.

Atwater and Luyendyk
Chief Scientist Tanya Atwater and Bruce P. Luyendyk, ALVIN expedition to Mid-Atlantic Ridge, 1978

Tanya Atwater is also very interested in sharing knowledge and teaching. She has created electronic multimedia tools. These tools help people visualize and understand the history of tectonic plates better.

Awards and Honors

See also

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