Activity 2 Magnetic Reversals And Sea Floor Striping

When the earth s magnetic field reverses a new stripe with the new polarity begins.

Activity 2 magnetic reversals and sea floor striping.

Each strip therefore represents an epoch of one or the other magnetic polarity and the symmetry is also explained. Label the age of each isochron solid line at the bottom of the right hand side of the map using the information recorded on your ocean floor map. This allows magma from under the surface to break up through the crust coming out and creating new sea floor. Assuming the distance to the farthest isochron is 300 km the spreading rate of the ridge was.

Magnetic striping magnetic minerals are found in rocks. These two things were the magnetic striping on the ocean floor and the age of seafloor rocks. It is as if the sea floor was a giant tape. Plates i activity 2.

300 km spreading rate. Following up the activity. Magnetic reversals and sea floor striping created date. The plates move apart carrying the new sea floor with it.

Magnetic striping of the sea floor after mid ocean ridges and trenches were discovered more evidence was discovered that helped to support the theory that the continents had moved around. Distanoe my km. The motion of the earth s molten outer core produces a magnetic field that is characterized by force lines emanating from near the. The idea that this.

Displaying top 8 worksheets found for activity seafloor spreading. Periodic reversals of the earth s magnetic field are shown by the remanent magnetisation of rocks of the sea bed which have been used to demonstrate sea floor spreading. Magnetic reversals after molten lava emerges from a volcano it solidifies to a rock. Midocean ridges and oceanic crust author.

Such magnetic patterns led to recognition of the occurrence of sea floor spreading and they remain some of the strongest evidence for the theory of plate tectonics. Some of the worksheets for this concept are sea floor spreading work sea floor spreading a model of seafloor spreading inside earth work magnetic reversals activity name date sea floor spreading l 1 2 3 5 4 ovr l lesson 3 seafloor profiling seafloor spreading and subduction. Magnetic striping in the pacific northwest 70 k as more and more of the seafloor was mapped during the 1950s the magnetic variations turned out not to be random or isolated occurrences but instead revealed recognizable patterns. The earth s magnetic polarity reverses and so does the magnetization of the ocean floor.

The figure below includes two images of the ocean floor. Study maps of magnetic anomalies as measured over the oceanic ridges and look for the symmetrical patterns.