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Heezen
and Tharp Seafloor Map, 1977.
Courtesy of Marie Tharp.
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Acoustic and seismic research has contributed
more to understanding Earth’s physical history, natural hazard
potential, and climate systems than perhaps all other scientific
technology combined. It gives scientists the ability to map the
ocean floor, a tool that revolutionized earth sciences 50 years
ago with the discovery that continents break apart and tectonic
plates shift. It revealed the globe-encircling volcanic mid-ocean
ridge system, earthquake-producing boundaries of crustal plates,
drowned shorelines, and submarine landslide deposits.
The
deep interior of the oceans is as difficult for man to reach as
is deep space. The opaqueness of seawater to the passage of light
or radio waves makes it difficult to efficiently study the seafloor
or the deep interior of the oceans with either optical methods
(cameras, etc), or with radar or microwave radiation (such as used
in satellites). Sound, however, travels freely through the oceans
and can be used to measure topography and to map geology, ocean
temperatures, and currents.
Today,
marine acoustic surveys are fundamental tools guiding explorations
of this planet. Numerous scientific research vessels
from around the world are engaged in studying all of the Earth’s
oceans and the underlying seafloor. The data that is being collected
is critical to informed decision making regarding our future.
Press
Release, January 24, 2005: LDEO Marine Seismic Research Contributes to Global Tsunami Detection and Warning System
Press
Release, January 5, 2005: Chicxulub Crater Research off the Yucatan
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