'Marine geology' involves
geophysical,
geochemical,
sedimentological and
paleontological investigations of the
ocean floor and coastal margins. Marine geology has strong ties to
physical oceanography and
plate tectonics.
Marine geological studies were of extreme importance in providing the critical evidence for
sea floor spreading and
plate tectonics in the years following World War II. The deep ocean floor is the last essentially unexplored frontier and detailed mapping in support of both military (submarine) objectives and economic (
petroleum and
metal mining) objectives drives the research.
The
Ring of Fire around the
Pacific Ocean with its attendant intense
volcanism and
seismic activity poses a major threat for disastrous
earthquakes,
tsunamis and volcanic eruptions. Any ''early warning'' systems for these disastrous events will require a more detailed understanding of marine geology of coastal and
island arc environments.
The study of
littoral and deep sea sedimentation and the precipitation and dissolution rates of
calcium carbonate in various marine environments has important implications for global
climate change.

A trench forms at the boundary where two tectonic plates meet
The discovery and continued study of
mid-ocean rift zone volcanism and
hydrothermal vents, first in the
Red Sea and later along the
East Pacific Rise and the
Mid-Atlantic Ridge systems were and continue to be important areas of marine geological research. The
extremophile organisms discovered living within and adjacent to those hydrothermal systems have had a pronounced impact on our understanding of life on Earth and potentially the
origin of life within such an environment.
Oceanic trenches are hemispheric-scale long but narrow topographic depressions of the sea floor. They also are the deepest parts of the ocean floor.
The
Mariana Trench (or Marianas Trench) is the deepest known submarine trench, and the deepest location in the Earth's crust itself. A
subduction zone where the
Pacific Plate is being subducted under the
Philippine Plate. The bottom of the trench is further below sea level than
Mount Everest is above sea level.
See also
★
List of geologists
★
Hawaiian-Emperor seamount chain
★
Pelagic sediments
References
★ Erickson, John, 1996, ''Marine Geology: Undersea Landforms and Life Forms'', Facts on File ISBN 0-8160-3354-4
★ Seibold, E. and W.H. Berger, 1994, ''The Sea Floor: An Introduction to Marine Geology'', Springer-Verlag ISBN 0-387-56884-0
External links
★
''Soundwaves'' Coastal Science & Research News from Across the USGS
★
Marine Geology and Geophysics - NOAA
★
Pacific Seafloor Mapping Project - USGS
★
Marine Geology and Geophysics at MIT
★
Ocean Drilling Program