Sonar (stands for Sound Navigation and Ranging)
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Transcript Sonar (stands for Sound Navigation and Ranging)
Ocean Landforms
Revealing the Ocean Floor
• If you could travel to the bottom
of the ocean, you would see the
world’s largest mountain chain
and canyons much deeper than
the Grand Canyon.
• How can the ocean floor be
mapped?
Revealing the Ocean Floor
Sonar (stands for Sound
Navigation and Ranging)
Invented in the 1920s
Primary instrument for
measuring depth
Reflects sound from ocean
floor
Revealing the Ocean Floor
Use of satellites for mapping
Employs satellites equipped with radar
altimeters
Scientists are able to measure the
direction and speed of ocean currents.
Measure the different heights of the
ocean surface to make maps of ocean
floor.
Can cover more territory using
satellites rather than ship sonar.
Practice Problems:
1. A ship transmits a signal that takes 6
seconds to return. How deep is the
water at this point?
2. The ship transmits the next signal and it
takes 10 seconds to return. How deep is
the water at this point? What conclusion
might be made?
Take out notebook and turn to DRW 10-2.
We will do the problems at the bottom of
page.
Continental Shelf
• Begins at the shoreline
• Continues until it begins to slope
more steeply downward
• Depth can reach 200 meters
• This is what you walk on at the
beach.
Continental Slope
•Begins at the edge of shelf
and continues to flattest part
of ocean floor
•Depth ranges from 200
meters to 4000 meters
•Continent ends at bottom of
continental slope
Abyssal Plain
• Broad, flat portion of the deep-
ocean floor.
• Covered with mud and remains of
marine organisms.
• Average depth is 4,000 meters
Mid-Ocean Ridges
• Mountain chains formed where
tectonic plates pull apart.
• Pulling motion creates cracks in
the crust called rift zones.
• Rift Valley forms between
mountains in the mid-ocean ridge.
Seamounts
• Individual mountain of volcanic
material.
• If a seamount builds up above
sea level, it becomes an island.
• A guyot is a flat-topped
seamount.
Ocean Trench
• Seemingly bottomless
cracks in the ocean basin.
• Formed where one oceanic
plate is forced underneath
another plate.
• Most famous: Mariana
Trench