Divergent Plate Boundaries
Divergent plate boundaries are locations where tensional forces are pulling things apart. In locations where lithospheric plates are diverging, the rates of divergent motion range from 2 to 17 cm/year.
Spreading Centers along Divergent Plate Boundaries
A spreading center is a linear area where new crust forms where two crustal plates are moving apart, such as along a mid-oceanic ridge. Spreading centers are typically seismically active regions in ocean basins and may be regions of active or frequent volcanism (Figure 4.7). Spreading centers are associated with divergent plate boundaries.
Seafloor spreading and formation of new ocean crust
Seafloor spreading features and processes include:
• Involves oceanic crust (OC) only.
• Tensional forces pull oceanic crust apart (forming faults that split deep into the newly forming ocean crust).
• This forms a mid-oceanic ridge (MOR).
• Volcanic activity along faults and fracture zones allows magma to rise cool on or near the seafloor surface.
• This volcanic activity generates new seafloor/oceanic crust,
• New oceanic crust moves away from spreading center as more is formed.
• Youngest oceanic crust is found near the ridge, oldest (and colder)crust is far away from ridge.
• Uplifts occurs as it is rifted, so MORs are the shallowest part of deep ocean basins.
• The MOR is symmetrical about the ridge.
• Magnetic reversals preserved in volcanic rocks are found along MORs worldwide.
• Sediments thicken away from the ridge (discussed in Marine Sediments chapter).• Hydrothermal vents (i.e.: vents of hot water
called "black smokers") are found in spreading centers.
Ocean Rises vs. Ridges
Spreading center are active at different rates, resulting in different physical characteristics.
A rise spreads faster and is less steep, a ridge is steeper and spreads slower.
• East Pacific Rise (see Figures 4-2, 4-3, 4-6, and 4-9)
• Mid-Atlantic Ridge (see Figures 4-2, 4-3, 4-6, and 4-7)
• On Iceland, the MOR rises to the land surface, its rate of spreading is about 15 cm/yr (Figure 4.8).
Figure 4.9. The East Pacific Rise is a rapidly forming spreading center (a mid-oceanic ridge that separates the Pacific Plate to the west from (north to south) the North American Plate, the Rivera Plate, the Cocos Plate, the Nazca Plate, and the Antarctic Plate. See Figure 4.6.
Continental Rifting occurs where divergent boundaries form within continental landmasses:
• Involves rifting (pulling apart) of continental crust (CC) only.
• Forms possibly from convection in the asthenosphere
• Large amounts of sediments are usually produced in continental rifting zones.
• Initially, when a continental rift forms it has continental processes such as the formation of large lakes, rivers, and beaches. Later, as it pulls farther apart it can become an oceanic rift when sea water floods in. It then becomes a MOR.
Present continental rifts include:
• Red Sea and East African Rift System (Figure 4.10 and 4-11).
* The breakup of Pangaea began with continental rifting starting about 200 million years ago with Africa pulling apart from North and South America. It eventually flooded with seawater and became the new Atlantic Ocean Basin.
Crustal Extension and Continental Rifting
Crustal extension occurs where a divergent plate boundary develops under a continental landmass on a large scale, associated with continental rifting (Figure 4.12).
Both crustal extension and continental rifting are occurring in northern Gulf of California and throughout North America's Great Basin region under Nevada, Arizona and eastward into the Rio Grand River rift valley in New Mexico (Figure 4.13). As the Atlantic Ocean opened, the North American continent was pushed over a spreading center that is now the entire region of Utah, Nevada, Arizona, and parts of New Mexico. Baja California and the Peninsular Ranges of San Diego and Orange counties have been rifted away from the Mexican coastline gradually over about 23 million years. Baja will continue moving northward, eventually crushing into southern Alaska in the distant future!