Question:  Katrina Jane Edwards heading the Fe-Oxidizing Microbial Observatory Project on a seamount the top of which is?

full_context: Document 1: Keiana Cavé: Keiana Cavé is an American Entrepreneur. She is also a student at the University of Michigan studying chemical engineering. She was honored in the Forbes 30 Under 30 Class of 2017 in the "Energy and Cleantech" Category. Keiana is one of the youngest changemakers to be featured on the list. She is originally from New Orleans, Louisiana. Keiana began her own independent research on the BP Deepwater Horizon Oil Spill with a focus on nanotechnology at the University of New Orleans at 15. Now, she has two published scientific research papers and two patents. After placing second at Intel ISEF in the Earth and Environmental Sciences category for her project, “A Method for Identifying the Photoproducts, Mechanisms, and Toxicity of Petroleum from the Deepwater Horizon by High-Performance Liquid Chromatography and DNPHi Derivatization,” Keiana became a member of Tulane University's Van Bael Lab where she continued her oil spill research with a focus on bacterial and fungal endophytes.
Document 2: Meiji Seamount: Meiji Seamount, named after Emperor Meiji, the 122nd Emperor of Japan, is the oldest seamount in the Hawaiian-Emperor seamount chain, with an estimated age of 82 million years. It lies at the northernmost end of the chain, and is perched at the outer slope of the Kuril-Kamchatka Trench. Like the rest of the Emperor seamounts, it was formed by the Hawaii hotspot volcanism, grew to become an island, and has since subsided to below sea level, all while being carried first north and now northwest by the motion of the Pacific Plate. Meiji Seamount is thus an example of a particular type of seamount known as a guyot, and some publications refer to it as Meiji Guyot.
Document 3: Mark Zoback: Mark D. Zoback is an American geophysicist and the Benjamin M. Page Professor of Geophysics at Stanford University. He is also a Senior Fellow at the Precourt Institute for Energy at Stanford University, an Elected Fellow of the American Association for the Advancement of Science and the National Academy of Engineering, and he directs or co-directs the Stanford Center for Induced and Triggered Seismicity (SCITS), the Stanford Natural Gas Initiative (NGI), and the Stanford Rock Physics and Borehole Geophysics program (SRB). Dr. Zoback is the author of the textbook "Reservoir Geomechanics", and he teaches a free online course by the same name that is taken annually by thousands of students. Dr. Zoback is the author of over 300 peer-reviewed publications and he holds seven patents. He is married to the American geophysicist Mary Lou Zoback.
Document 4: Katrina Edwards: Katrina Jane Edwards (15 March 1968 - 26 October 2014) was a pioneering geomicrobiologist known for her studies of organisms living below the ocean floor, specifically exploring the interactions between the microbes and their geological surroundings, and how global processes were influenced by these interactions. She spearheaded the Center for Dark Energy Biosphere Investigation (C-DEBI) project at the University of Southern California, which is ongoing. Edwards also helped organize the deep biosphere research community by heading the Fe-Oxidizing Microbial Observatory Project on Loihi Seamount, and serving on several program steering committees involving ocean drilling. Edwards taught at the Woods Hole Oceanographic Institute (WHOI) and later became a professor at the University of Southern California.
Document 5: Lindsay Collins: Lindsay Boyd Collins (19 February 1944 – 2 September 2015) was an Australian marine geologist and sedimentologist, a faculty member in the department of applied geology at Curtin University in Western Australia. He was interested in studying the continental shelf of Western Australia and coral reefs. Collins was a prominent scholar, he has completed projects on continental shelf mapping of Australian shelves, microbialites and seagrass banks at Shark Bay, and coral reef studies at the Abrolhos, Ningaloo, Scott Reef, the Rowley Shoals and the Kimberley.
Document 6: James E. Atwater: James E. Atwater (born 1946) is a retired North American multidisciplinary physical scientist with training in geophysics, chemistry and biological science. He was awarded the Wright Brothers Medal for his work on microwave powered methods for microbial stabilization and water recovery from solid waste. Atwater served in the United States Marine Corps [1963-1967] prior to attending the University of Utah [1968-1975]. In his early career [1977-1980] Atwater concentrated on methods and instrumentation for identification and quantification of radionuclides associated with uranium exploration and recovery by gamma ray and alpha particle energy spectrometry. Subsequently [1980-1987] he applied radiometric geophysical well logging techniques to the characterization of sandstone, limestone, dolomite and shale core samples. At this time he also refined methods for the determination of porosity and permeability of unconsolidated bitumen and heavy oil bearing sands. Later Atwater’s attention turned to problems of long-term human presence in space, working on regenerable systems for water and air purification, and means for decomposition and stabilization of solid waste materials and recovery of useful resources therefrom. During these years Atwater and colleagues also developed novel sensors and analytical instrumentation for monitoring and control of life support systems. In addition to instrumentation and methods, much of this work entailed the development of novel materials and the characterization of material properties, particularly with respect to magnetic and broadband microwave dielectric phenomena. Recent research includes the study of multiphase immiscible fluid flow in porous media, and the recovery of hydrogen from methane (natural gas) using magnetically stabilized fluidized bed and microwave plasma reactors. Though in retirement, Atwater continues his association with former colleagues, providing theoretical analysis of experimental data, and preparation of materials for publication.
Document 7: Axial Seamount: Axial Seamount (also Coaxial Seamount or Axial Volcano) is a seamount and submarine volcano located on the Juan de Fuca Ridge, approximately 480 km west of Cannon Beach, Oregon. Standing 1100 m high, Axial Seamount is the youngest volcano and current eruptive center of the Cobb-Eickelberg Seamount chain. Located at the center of both a geological hotspot and a mid-ocean ridge, the seamount is geologically complex, and its origins are still poorly understood. Axial Seamount is set on a long, low-lying plateau, with two large rift zones trending 50 km to the northeast and southwest of its center. The volcano features an unusual rectangular caldera, and its flanks are pockmarked by fissures, vents, sheet flows, and pit craters up to 100 m deep; its geology is further complicated by its intersection with several smaller seamounts surrounding it.
Document 8: Evolution of Hawaiian volcanoes: The fifteen volcanoes that make up the eight principal islands of Hawaiʻ i are the youngest in a chain of more than 129 volcanoes that stretch 5800 km across the North Pacific Ocean, called the Hawaiian-Emperor seamount chain. Hawaiʻ i's volcanoes rise an average of 4572 m to reach sea level from their base. The largest and most famous, Mauna Loa, has built itself up to a height of 4169 m . As shield volcanoes, they are built by accumulated lava flows, growing no more than 3 m at a time to form a broad and gently sloping shape.
Document 9: Sally Ride Science: Sally Ride Science at UC San Diego is a nonprofit run by the University of California, San Diego. It was founded as a company in 2001 by Sally Ride, America's first woman in space, along with Tam O'Shaughnessy, Karen Flammer, Terry McEntee, and Alann Lopes to inspire young people in science, technology, engineering, and math (STEM) and to promote STEM literacy. Sally Ride Science was relaunched at UC San Diego on October 1, 2015. It is based at UC San Diego Extension, and its programs are coordinated jointly by UC San Diego Extension, Scripps Institution of Oceanography, and San Diego Supercomputer Center. O'Shaughnessy is executive director and Flammer is director of education for Sally Ride Science at UC San Diego.
Document 10: Hawaiian–Emperor seamount chain: The Hawaiian–Emperor seamount chain is a mostly undersea mountain range in the Pacific Ocean that reaches above sea level in Hawaii. It is composed of the Hawaiian ridge, consisting of the islands of the Hawaiian chain northwest to Kure Atoll, and the Emperor Seamounts: together they form a vast underwater mountain region of islands and intervening seamounts, atolls, shallows, banks and reefs along a line trending southeast to northwest beneath the northern Pacific Ocean. The seamount chain, containing over 80 identified undersea volcanoes, stretches over 5800 km from the Aleutian Trench in the far northwest Pacific to the Loʻihi seamount, the youngest volcano in the chain, which lies about 35 km southeast of the Island of Hawaiʻi.
Document 11: Susan Avery: Susan K. Avery (born 1950) is an American atmospheric physicist and President Emerita of the Woods Hole Oceanographic Institution (WHOI) in Massachusetts, where she led the marine science and engineering research organization from 2008-2015. She was the ninth president and director and the first woman to hold the leadership role at WHOI. She is Professor Emerita at the University of Colorado, Boulder (UCB), where she served on the faculty from 1982-2008. While at UCB she also served in various administrative positions, including director of the Cooperative Institute for Research in Environmental Sciences (CIRES), a 550-member collaborative institute between UCB and the National Oceanic and Atmospheric Administration (NOAA) (1994-2004); and interim positions (2004-2007) as vice chancellor for research and dean of the graduate school, and provost and executive vice chancellor for academic affairs. Currently she is a senior fellow at the Consortium for Ocean Leadership in Washington, D.C.
Document 12: Lōʻihi Seamount: Lōʻihi Seamount (also known as Loihi) is an active submarine volcano about 35 km off the southeast coast of the island of Hawaiʻi. The top of the seamount is about 975 m below sea level. This seamount is on the flank of Mauna Loa, the largest shield volcano on Earth. Lōʻihi, meaning "long" in Hawaiian, is the newest volcano in the Hawaiian-Emperor seamount chain, a string of volcanoes that stretches over 5800 km northwest of Lōʻihi. Unlike most active volcanoes in the Pacific Ocean that make up the active plate margins on the Pacific Ring of Fire, Lōʻihi and the other volcanoes of the Hawaiian-Emperor seamount chain are hotspot volcanoes and formed well away from the nearest plate boundary. Volcanoes in the Hawaiian Islands arise from the Hawaiʻi hotspot, and as the youngest volcano in the chain, Lōʻihi is the only Hawaiian volcano in the deep submarine preshield stage of development.
Document 13: Māhukona: Māhukona is a submerged shield volcano on the northwestern flank of the Island of Hawaiʻ i. A drowned coral reef at about 3,770 feet (-1,150 m) below sea level and a major break in slope at about 4,400 feet (-1,340 m) below sea level represent old shorelines. The summit of the shield volcano was once 800 feet (250 m) above sea level. It has now subsided below sea level. A roughly circular caldera marks the summit of Māhukona. A prominent rift zone extends to the west. A second rift zone probably extended to the east but has been buried by younger volcanoes. The main shield-building stage of volcanism ended about 470,000 years ago. The summit of the shield volcano subsided below sea level between 435,000 and 365,000 years ago.
Document 14: Kīlauea: Kīlauea ( , ; ] ) is a currently active shield volcano in the Hawaiian Islands, and the most active of the five volcanoes that together form the island of Hawaiʻ i. Located along the southern shore of the island, the volcano is between 300,000 and 600,000 years old and emerged above sea level about 100,000 years ago. It is the second youngest product of the Hawaiian hotspot and the current eruptive center of the Hawaiian–Emperor seamount chain. Because it lacks topographic prominence and its activities historically coincided with those of Mauna Loa, Kīlauea was once thought to be a satellite of its much larger neighbor. Structurally, Kīlauea has a large, fairly recently formed caldera at its summit and two active rift zones, one extending 125 km east and the other 35 km west, as an active fault of unknown depth moving vertically an average of 2 to per year.
Document 15: Mauna Loa: Mauna Loa ( or ; Hawaiian: ] ; English: Long Mountain ) is one of five volcanoes that form the Island of Hawaii in the U.S. state of Hawaiʻi in the Pacific Ocean. The largest subaerial volcano in both mass and volume, Mauna Loa has historically been considered the largest volcano on Earth. It is an active shield volcano with relatively gentle slopes, with a volume estimated at approximately 18000 mi3 , although its peak is about 120 ft lower than that of its neighbor, Mauna Kea. Lava eruptions from Mauna Loa are silica-poor and very fluid, and they tend to be non-explosive.
ground_truth: about 975 m below sea level