Applications of Ocean Acoustic Monitoring to Understanding Our Planet [electronic resource].
- Washington, D.C. : United States. Dept. of Energy. Office of Science, 2005. and Oak Ridge, Tenn. : Distributed by the Office of Scientific and Technical Information, U.S. Dept. of Energy.
- Additional Creators:
- Fermi National Accelerator Laboratory, United States. Department of Energy. Office of Science, and United States. Department of Energy. Office of Scientific and Technical Information
- Restrictions on Access:
- Free-to-read Unrestricted online access
- The ocean covers two-thirds of the surface of Earth, and hides long chains of seafloor volcanoes, bizarre and magnificent life forms, and many dynamic geological processes. Shrouded in darkness, much of what happens deep in the ocean is unknown to us. But sound can tell us a great deal about what is going on in the ocean. Changes in the physical properties of seawater with depth allow relatively quiet sounds to travel great distances without loosing much energy. In this way we are able to record many noises that occur within or on the boundary of the ocean, giving us insight into geological, biological and man-made activities in the ocean. One of the most interesting noises to a geophysicist is the sound of mid-ocean ridge volcanic eruptions. These eruptions are forming new surface for our planet and helping create an extraordinary seafloor ecosystem. Examples of sounds heard and some of their implications will be presented.
- Published through SciTech Connect., 10/26/2005., Fermilab Colloquia, Fermi National Accelerator Laboratory (FNAL), Batvia, Illinois (United States), presented on October 26, 2005., and Tolstoy, Maya.
- Funding Information:
View MARC record | catkey: 14378979