Seafloor spreading is a geologic process in which tectonic plate s large slabs of earth s lithosphere split apart from each other.
The sea floor is part of the.
Like land terrain the ocean floor has ridges valleys plains and volcanoes.
In general the ocean floor can be divided into four major divisions.
Seafloor spreading and other tectonic activity processes are the result of mantle convection.
Below the ocean floor there are a few small deeper areas called ocean trenches.
By creating complex 3 d maps they re hoping to learn more about waves and achieve ambitious conservation goals.
It is actually a part of the continent sloping gently towards the sea floor.
Ocean b is very small and has volcanoes all along one side.
Plate tectonics and the ocean floor bathymetry the shape of the ocean floor is largely a result of a process called plate tectonics.
Wally is a planetologist in the future.
Charting the ocean floor.
When carbon dioxide from the atmosphere is absorbed.
The seabed also known as the seafloor sea floor or ocean floor is the bottom of the ocean no matter how deep.
All floors of the ocean are known as seabeds.
Using sound and laser technology researchers have begun to reveal the secrets of the ocean floor from the sonoma coast to monterey bay.
Features of the ocean include the continental shelf slope and rise.
Mantle convection is the slow churn ing motion of earth s mantle.
Tha san anreas fault is an example of this type of boundary.
Map showing the underwater topography bathymetry of the ocean floor.
Ocean a is very large and looks like it has baseball stitches down its center.
Sea levels during ice ages because much of the water that would otherwise be in the ocean is locked up in continental ice.
The ocean floor is called the abyssal plain.
He discovers a planet similar to earth that has two major oceans.
The outer rocky layer of the earth includes about a dozen large sections called tectonic plates that are arranged like a spherical jig saw puzzle floating on top of the earth s hot flowing mantle.
The part of the ocean floor immediately next to continents that has relatively shallow water above it.
Continental shelf is the shallow portion of the ocean which lies close to the continental margin.