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.
Activity 2 magnetic reversals and sea floor striping.
Plates i activity 2.
Magnetic striping magnetic minerals are found in rocks.
The figure below includes two images of the ocean floor.
300 km spreading rate.
This allows magma from under the surface to break up through the crust coming out and creating new sea floor.
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.
Each strip therefore represents an epoch of one or the other magnetic polarity and the symmetry is also explained.
The idea that this.
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.
These two things were the magnetic striping on the ocean floor and the age of seafloor rocks.
Magnetic reversals and sea floor striping f.
Distanoe my km.
Study maps of magnetic anomalies as measured over the oceanic ridges and look for the symmetrical patterns.
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.
Displaying top 8 worksheets found for activity seafloor spreading.
Following up the activity.
Magnetic reversals after molten lava emerges from a volcano it solidifies to a rock.
Midocean ridges and oceanic crust author.
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.
The earth s magnetic polarity reverses and so does the magnetization of the ocean floor.
Assuming the distance to the farthest isochron is 300 km the spreading rate of the ridge was.
Magnetic reversals and sea floor striping a key factor in establishing the theory of plate tectonics was recognition of past reversals in the earth s magnetic field and the mapping of normal and reverse magnetic striping on the ocean floor.
The plates move apart carrying the new sea floor with it.
The motion of the earth s molten outer core produces a magnetic field that is characterized by force lines emanating from near the.
It is as if the sea floor was a giant tape.
When the earth s magnetic field reverses a new stripe with the new polarity begins.
