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The Continents

The Continents
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Description: Continents
Flat features that average 0.8 km (0.5 mi) in elevation
Granitic rocks

Ocean basins
Average 3.8 km (2.8 mi) below sea level
Basalitic rocks

Mountain Belts
Principally the circum-Pacific belt and the Alps/Himalayas

Stable Interior
Shields – expansive, flat regions of deformed crystalline rock
Stable platforms – deformed rocks covered by sedimentary rocks.

Continental Margins

Portions of seafloor adjacent to major landmasses
Includes:
Continental shelf – gently sloping platform extending seaward from shore
Continental slope – steep drop off at edge of continental shelf
Continental rise – more gradual incline; continental slope merges with thick accumulation of sediments

Deep-Ocean Basins
Between continental margins and oceanic ridges
Abyssal plains – flat features of deep-ocean basins
Deep-ocean trenches – deep depressions in ocean floor
Seamounts – submerged volcanic structures

Oceanic Ridge
Also called mid-ocean ridge
Includes Mid-Atlantic Ridge and East Pacific Rise
Continuous mountain belt that winds around globe
Many layers of igneous rock

Earth is a dynamic body with many separate but highly interacting parts or spheres
Earth system science studies Earth as a system composed of numerous parts, or subsystems
System – any size group of interacting parts that form a complex whole

System
Closed systems are self-contained (e.g., an automobile cooling system)
Open systems – both energy and matter flow into and out of the system (e.g., a river system)

Earth as a system
Consists of a nearly endless array of subsystems (e.g., hydrologic cycle, rock cycle)

Earth as a system
Sources of energy
Sun – drives external processes such as weather, ocean circulation, and erosional processes
Earth’s interior – drives internal processes including volcanoes, earthquakes, and mountain building
Humans are part of the Earth system




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