Diagram Of The Sea Floor Spreading

Seafloor spreading occurs along mid ocean ridges large mountain ranges rising from the ocean floor.

Diagram of the sea floor spreading. If the spreading rate relative velocity is high magma must be rising rapidly and the lithosphere is relatively hot beneath the ridge. Read the definitions below then label the seafloor spreading plate divergence diagram. Spreading rate is the rate at which an ocean basin widens due to seafloor spreading. In seafloor spreading.

Spreading rates determine if the ridge is fast intermediate or slow. Lower mantle semi rigid the deepest parts of the mantle just above the core. The rate at which new oceanic lithosphere is added to each tectonic plate on either side of a mid ocean ridge is the spreading half rate and is equal to half of the spreading rate. Thus for fast spreading centers the ridge stands at higher elevations than for slow spreading centers.

Start studying sea floor spreading 3 2. Most of the mountains in the mid ocean ridge lie hidden under hundreds of meters of. The mid ocean ridge curves like the seams of a baseball along the sea floor extending into all of earth s oceans. Lithosphere the crust plus the rigid upper mantle.

Enjoy the videos and music you love upload original content and share it all with friends family and the world on youtube. This can result in an ever widening seafloor at the. This idea played a pivotal role in the development of the theory of plate tectonics which revolutionized geologic thought during the last quarter of the 20th century. Seafloor spreading theory that oceanic crust forms along submarine mountain zones and spreads out laterally away from them.

Learn vocabulary terms and more with flashcards games and other study tools. The red colors are the youngest parts of the seafloor where fresh new crust is formed as lava seeps up from the deep interior of the earth at spreading ridges as new crust forms at these spreading ridges older crust colored green in the diagram moves away from. Seafloor spreading is the continuous process of forming new igneous rock at midocean ridges by injection of magma that forms new seafloor. The process is continuous because forces cause opposite sides of the midocean ridge to constantly move apart making new room for the process to repeat.

Sea floor topography is controlled by the age of the oceanic lithosphere and the rate of spreading. Sea floor spreading powerpoint 1. This diagram provides evidence of seafloor spreading by showing the ages of ocean floor in the atlantic and eastern pacific oceans.