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.
Activity 2 magnetic reversals and sea floor striping.
Magnetic reversals and sea floor striping created date.
Displaying top 8 worksheets found for activity seafloor spreading.
The plates move apart carrying the new sea floor with it.
Following up the activity.
Assuming the distance to the farthest isochron is 300 km the spreading rate of the ridge was.
The figure below includes two images of the ocean floor.
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.
Study maps of magnetic anomalies as measured over the oceanic ridges and look for the symmetrical patterns.
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.
These two things were the magnetic striping on the ocean floor and the age of seafloor rocks.
Magnetic reversals after molten lava emerges from a volcano it solidifies to a rock.
Each strip therefore represents an epoch of one or the other magnetic polarity and the symmetry is also explained.
The idea that this.
When these magnetic patterns were mapped over a wide region the ocean floor showed a zebra like pattern.
When the earth s magnetic field reverses a new stripe with the new polarity begins.
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.
Plates i activity 2.
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.
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.
Magnetic striping magnetic minerals are found in rocks.
Magnetic reversals and sea floor striping f.
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.
The earth s magnetic polarity reverses and so does the magnetization of the ocean floor.
300 km spreading rate.
It is as if the sea floor was a giant tape.
