Sea Floor Spreading And Subduction

This report describes how to build a model of the outer 300 km 180 miles of the earth that can be used to develop a better understanding of the principal features of plate tectonics including sea floor spreading the pattern of magnetic stripes frozen into the sea floor transform faulting thrust faulting subduction and volcanism.

Sea floor spreading and subduction.

These age data also allow the rate of seafloor spreading to be determined and they show that rates. For instance the atlantic ocean is believed to be expanding because of its few trenches. Scroll down for a preview of this learning objective s games and the concepts they drive home. The denser lithospheric material then melts back into the earth s mantle.

The seafloor spreading and subduction learning objective based on ngss and state standards delivers improved student engagement and academic performance in your classroom as demonstrated by research. The pattern of magnetic strips shows that the seafloor is expanding at mid ocean ridges. 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. Which statement accurately describes how magnetic stripes in ocean rock provide evidence of seafloor spreading.

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. Seafloor spreading theory that oceanic crust forms along submarine mountain zones and spreads out laterally away from them. Seafloor spreading is just one part of plate tectonics. At subduction zones the edge of the denser plate subducts or slides beneath the less dense one.

Subduction happens where tectonic plates crash into each other instead of spreading apart. Spreading rates determine if the ridge is fast intermediate or slow. Subduction and sea floor spreading are processes that could alter the size and form of the ocean. Subduction is one of the two major processes of plate tectonics the other being seafloor spreading.

Due to this continuous seafloor spreading occurs and makes atlantic ocean floor to be connected to other continental crust making the ocean gets wider over the time. As upwelling of magma continues the plates continue to diverge a process known as seafloor spreading samples collected from the ocean floor show that the age of oceanic crust increases with distance from the spreading centre important evidence in favour of this process. Spreading rate is the rate at which an ocean basin widens due to seafloor spreading.