Continental Drift and Plate Tectonics Flashcards
- (tekto = to build) are those that deform Earth’s crust to create major structural features, such as mountains, continents, and ocean basins.
Tectonic processes
Wegener suggested that a single supercontinent named * consists all Earth’s landmasses once
Pangaea (“all lands”)
According to the plate tectonics model, the crust and
the uppermost part of the mantle constitute Earth’s strong outer layer, the *
lithosphere (lithos = stone).
Oceanic crust is composed of * and rich in dense iron and magnesium, whereas continental crust is composed largely of less dense * rocks.
basalt, granitic (mafic)
The * is a hotter, weaker region in the mantle that lies below the lithosphere
asthenosphere (asthenos = weak)
Although these rocks in asthenosphere are solid, they are quite *and respond to forces acting on them by exhibiting a slow * . By contrast, the comparatively cool and strong lithosphere tends to respond to forces acting on it by * . These differences result in Earth’s rigid outer shell being effectively detached from the underlying asthenosphere, which allows it to move independently of the layers below
ductile, fluid-like flow
bending or breaking
where two plates move
apart, resulting in upwelling and partial melting of
hot material from the mantle to create new seafloor
Divergent plate boundaries
where two plates move together, resulting either in oceanic lithosphere descending beneath an overriding plate, eventually to be reabsorbed into the mantle, or possibly in the collision of two continental blocks to createa mountain belt
Convergent plate boundaries
where two plates grind past each other without the production or destruction of lithosphere
Transform plate boundaries
Most divergent plate boundaries (di = apart, vergere =
to move) are located along the crests of * and can be thought of as constructive plate margins because this is where new ocean floor is generated
Two adjacent plates move away from each other,
producing long, narrow fractures in the ocean crust. As
a result, hot molten rock from the mantle below migrates upward to fill the voids left as the crust is being ripped apart.
oceanic ridges
Divergent plate boundaries are also called *
spreading centers.
- are elevated areas of the seafloor characterized by high heat flow and volcanism.
The * is the longest
topographic feature on Earth’s surface, exceeding
70,000 kilometers (43,000 miles) in length.
Oceanic ridges, global oceanic ridge system
any of several vast submarine regions that collectively cover nearly three-quarters of Earth’s surface. This includes the continental shelf, abyssal plain, mid-ocean ridge, etc.
Ocean basin
Further, along the crest of some ridge segments is a deep Canyon-like structure called a *
rift valley
The mechanism that operates along the oceanic ridge system to create new seafloor is appropriately called *
seafloor spreading.