L4. STRUCTURE AND EVOLUTION OF OCEAN BASINS AND THE PLATE TECTONIC THEORY Flashcards
This caused the formation of different topographic features.
Seafloor Spreading
TOPOGRAPHIC FEATURES OF THE SEAFLOOR
An area with shallow water that surrounds the land(continent).
Continental Shelf
TOPOGRAPHIC FEATURES OF THE SEAFLOOR
It is the border of the continental shelf. It is the submerged outer edge of the continent where continental crust transitions into oceanic crust.
Continental Margin
TOPOGRAPHIC FEATURES OF THE SEAFLOOR
It is sometimes referred to as the seafloor. An extremely vast flat surface underwater, that is sometimes interrupted by hills, seamount and valleys.
Abyssal Plain
TOPOGRAPHIC FEATURES OF THE SEAFLOOR
These are elongated hills, typically 50-300m high and common on the slopes of mid oceanic ridge
Abyssal Hill
TOPOGRAPHIC FEATURES OF THE SEAFLOOR
It is a submarine mountain chain that winds for more than 65,000 km around the globe. It has a central rift valley and rugged topography on its flanks.
Mid-ocean Ridges
TOPOGRAPHIC FEATURES OF THE SEAFLOOR
These are narrow, elongated depressions on the seafloor many of which are adjacent to arcs of island with active volcanoes; deepest features of the seafloor
Deep-ocean Trenches
TOPOGRAPHIC FEATURES OF THE SEAFLOOR
Submerged volcanoes are called ____________ while those that rise above the ocean surface are called ___________ __________. These features may be isolated or found in clusters or chains.
Seamounts; Volcanic Islands
Any of several vast submarine regions that collectively cover nearly three-quarters of Earth’s surface.
Ocean Basin
EVOLUTION OF THE OCEAN BASIN
The formation of the ocean basin starts with a rifting of a continental crust. A continent may split and forms a rift valley.
Embroyonic Stage
EVOLUTION OF THE OCEAN BASIN
In this stage, basalt which comes from the molten material oozing from the rift will start to form the seafloor.
Juvenile Stage
EVOLUTION OF THE OCEAN BASIN
In this stage, the ocean basin continues to widen. At some point its boundary, will meet with continental crust that will start its subduction on the other side.
Mature Stage
EVOLUTION OF THE OCEAN BASIN
As the movement of the plates may change, ocean basins may start to narrow. The origin, which are diverging plates may end up to be converging with other plates that will permit the narrowing of the ocean floor.
Terminal
EVOLUTION OF THE OCEAN BASIN
The last stage of ocean basin evolution ends with the complete collision of two continental plates. The last seafloor will be eliminated and a previously formed ocean basin will no longer be seen as mountain chains replaces it
Continental Collision