Activity 2 Magnetic Reversals And Sea Floor Striping Lab

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Activity 2 magnetic reversals and sea floor striping lab.

Distanoe my km. Displaying top 8 worksheets found for activity seafloor spreading. Show how dates in hundreds of thousands or millions of years may be assigned to the sea floor stripes by comparison to land based. The patterns reflect the creation and spreading of oceanic crust along the mid oceanic ridges.

Magnetic reversals and sea floor striping f. Magnetic reversals and sea floor striping created date. Demonstrate sea floor spreading. 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.

Basalt forming at the ridge crest picks up the existing magnetic polarity. The motion of the earth s molten outer core produces a magnetic field that is characterized by force lines emanating from near the. Assuming the distance to the farthest isochron is 300 km the spreading rate of the ridge was. These surveys revealed a series of invisible magnetic stripes of normal and reversed polarity in the sea floor like that shown in the figure below.

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. Plates i activity 2. Magnetic striping magnetic minerals are found in rocks. 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.

Midocean ridges and oceanic crust author. Study maps of magnetic anomalies as measured over the oceanic ridges and look for the symmetrical patterns.