Section 10.2 The Oceans
From a meteorological perspective, oceans:
are the main source of atmospheric water vapor
exchange energy with the atmosphere
transfer heat poleward
71% of the Earth's surface area
Average depth of 3.8 km below sea level(average height of continents is 0.87 km above sea level)
per 100g, contains 3.5g total salt (mostly chlorides with some sulfates)
The lithosphere is the uppermost 100 km of the Earth that includes the crust and part of the upper mantle. The Earth is divided into numerous lithospheric plates that can move around relative to each other. In the context of plate tectonics, we find three main types of plate boundaries:
divergent: plates moving apart from each other. This type of boundary is constructive because new lithosphere must be added at the plate boundary. The best example of this type of boundary are the mid-ocean ridges found throughout the Earth's oceans, where new crust is added via volcanism.
convergent: plates moving toward each other. This type of boundary is referred to as destructive, because they require a decrease lithospheric plate area. Convergent boundaries can be further subdivided into
oceanic-continental: involving the subduction of oceanic lithosphere below continental lithosphere (example: Andes Mountains).
continental-continental: involving the collision of two continental plates. Neither will subduct, leading to mountain formation (example: Himalayas).
oceanic-oceanic: involving the collision of two oceanic plates. Typically, the older and cooler plate will subduct beneath the younger (example: Aleutian Islands)
transform: plates moving past each other. This type of boundary is referred to as conservative, because lithospheric plate area is neither created nor destroyed at the boundary. The best example of this type of boundary is the San Andreas fault in California.
ocean basins may be bounded by active margins (at lithospheric plate boundaries) or passive margines (embedded within a lithospheric plate)
the continental shelf is overlaid by sediment and slopes gradually out to shelf break and the continental slope. At the base of the continental slope is the continental rise.
the abyssal plains are relatively flat depositional surfaces (more common on older ocean floors) and may be dotted with submarine volcanoes.
the mid-ocean ridges are typically found near the centers of the ocean basins (classic example is the Atlantic Ocean) and form the world's largest mountain chains, typically rising 2.5 km above the abyssal plains.
trenches are found along active margins where subduction is occurring. Subduction also gives rise to volcanism on the overlying plate, forming a mountain chain such as the Andes Mountains or a volcanic island arc such as the Aleutian Islands.