EXERCISES
Examination and evaluation of real-time oceanographic data on the internet
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TOPOGRAPHY OF THE OCEAN FLOOR
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Introduction to Terminology Describing the Topography
of the Ocean Floor:
- Definitions of terms and annotated images of features from lectures
- abyssal plain
- passive continental margin with shelf, slope and rise
- fracture zone
- mid-ocean ridge or spreading ridge
- lateral ridge
- deep sea trench
- island chains and seamounts
- triple point junction
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Definitions
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Images
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abyssal plain: flat ocean-basin floor extending seaward
from the base of the continental slope and rise, typically 4-6km deep
continental margin: zone separating continents
from the deep sea floor. passive, if seismically inactive.
continental shelf: zone bordering a continent
from shoreline to depth where a marked change in deoth occurs (shelf break).
continental slope: relatively steep downward
slope from shelf to depth.
continental rise: gentle slope at the
base of the continental slope.
fracture zone: linear zone of irregular
bathymetry associated with fault zones and offsetting mid-ocean ridges.
mid-ocean ridge (MOR): spreading ridge
at divergent plate boundary.
lateral ridges: volcanic ridges often
separating ocean basins that are not divergent plate boundaries
seamounts: isolate volcanic peaks that
rise >1km above the ocean floor, often in island chains formed
by 'hot spots.'
trenches: long, deep and narrow depressions
of the sea floor with relatively steep sides that are associated with subduction
zones.
triple point junction: a point where
three plates meet |
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Department of Geological Sciences,
1001 E. Tenth Street, Bloomington, IN 47405-1403
Phone: (812) 855-5582 Last updated: 6 October 2002
Comments: simon@indiana.edu
Copyright
2000, The Trustees of Indiana University
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