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THE TOPOGRAPHY OF THE OCEAN - Coggle Diagram
THE TOPOGRAPHY OF THE OCEAN
Guyot:
is an isolated underwater mountain with a flat top.
Canyon:
Submarine canyons are narrow valleys perpendicular to the coast that connect the continental shelf with the deep sea, characterized by steep slopes.
https://youtu.be/YATxHU3CXps?si=x6pIsbLlJFDEApDy
HYDROTERMAL VENT: fissure on the seabed that releases geothermally heated water.
Rift Valley:
is a lowland region that forms where Earth’s tectonic plates move apart, or rift.
https://youtu.be/6gf7FIqpCGc?si=WW8esvs9JYLY1iJV
Mid-ocean ridge:
is a continuous range of underwater volcanoes that wraps around the globe like seams on a baseball.
https://youtu.be/pHWceRySDb8?si=tfZqqgspPtVKZiJy
Conclusion:
https://youtu.be/K8blL9Ki2mQ?si=Umu9dxBr_-jVD85x
Continental shelf
UNDERWATER VOLCANO: vent or fissure on the ocean floor from which magma can erupt
ABYSSAL PLAIN: flat and featureless expanse of sediment-covered ocean floor
SEAMOUNT: large submarine volcanic mountains formed through volcanic activity and submerged under the ocean
TRENCH: long, narrow, and steep-sided depression in the ocean floor, typically 50 to 100 kilometers wide and can be thousands of kilometers in length
Everything about the formation of a Seamount
https://youtu.be/OPlNQBNGUTA?si=d_RRlVsbWBFLk5gr
What Is the Difference Between Oceanic Crust and Continental Crust?
