Seafloor spreading labeled diagram.
Sea floor spreading labeled.
This graphic shows several ocean floor features on a scale from 0 35 000 feet below sea level.
A model of sea floor spreading teacher s guide ellen p.
The following features are shown at example depths to scale though each feature has a considerable range at which it may occur.
1 use a shoe box with approximate dimensions 6 5 x 13 by 5 deep.
Seafloor spreading plate divergence label the growth of new oceanic crust as two plates diverge.
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Labeled diagram of seafloor spreading.
Subduction plate divergence label the subduction of an oceanic plate under a continental plate plate convergence.
Glue these two pages together to form the cross section through the earth.
Soil layers diagram label the layers of soil.
Here magma rises up from below as the sea floor spreads out to either side as shown in figure 1.
Tornado quiz label tornado alley printout.
Students will make a paper model illustrating the concept of sea floor spreading and the development of symmetrical magnetic stripes on either side of a mid ocean spreading center.
Label seafloor spreading plate divergence printout.
Over time new.
This spreading occurs at about the same rate as your fingernails grow.
Seafloor spreading occurs along mid ocean ridges large mountain ranges rising from the ocean floor.
Sea floor spreading occurs at the mid ocean ridge where two plates are moving away from each other.
2 trim as indicated the pages labeled left portion of side of shoe box and right.
A transform fault may occur in the portion of a fracture zone that exists between different offset spreading centres or that connects spreading centres to deep sea trenches in.
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The mid atlantic ridge for instance separates the north american plate from the eurasian plate and the south american plate from the african plate the east pacific rise is a mid ocean ridge that runs through the eastern pacific ocean and separates the pacific plate from the north american.
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Transform fault in geology and oceanography a type of fault in which two tectonic plates slide past one another.
Students work as individuals.