* Your assessment is very important for improving the workof artificial intelligence, which forms the content of this project
Download Magnetic Anomalies Activity Name______ __
Van Allen radiation belt wikipedia , lookup
Maxwell's equations wikipedia , lookup
Magnetosphere of Jupiter wikipedia , lookup
Friction-plate electromagnetic couplings wikipedia , lookup
Electromagnetism wikipedia , lookup
Magnetosphere of Saturn wikipedia , lookup
Geomagnetic storm wikipedia , lookup
Mathematical descriptions of the electromagnetic field wikipedia , lookup
Superconducting magnet wikipedia , lookup
Lorentz force wikipedia , lookup
Edward Sabine wikipedia , lookup
Electromagnetic field wikipedia , lookup
Giant magnetoresistance wikipedia , lookup
Magnetometer wikipedia , lookup
Magnetic monopole wikipedia , lookup
Neutron magnetic moment wikipedia , lookup
Magnetic stripe card wikipedia , lookup
Magnetic nanoparticles wikipedia , lookup
Earth's magnetic field wikipedia , lookup
Electromagnet wikipedia , lookup
Magnetotactic bacteria wikipedia , lookup
Force between magnets wikipedia , lookup
Multiferroics wikipedia , lookup
Geomagnetic reversal wikipedia , lookup
Magnetotellurics wikipedia , lookup
Magnetoreception wikipedia , lookup
Magnetochemistry wikipedia , lookup
Magnetic Anomalies Activity Name________________________ Date_______________Hr_______ BACKGROUND: Before being widely accepted, a new hypothesis must be tested. One test for the seafloor-spreading hypothesis involved magnetic patterns on the sea floor. In the late 1950's, scientists mapped the present-day magnetic field generated by rocks on the floor of the Pacific Ocean. The volcanic rocks which make up the sea floor have magnetization because, as they cool, magnetic minerals within the rock align to the Earth's magnetic field. The intensity of the magnetic field they measured was very different from the intensity they had calculated. Thus, the scientists detected magnetic anomalies, or differences in the magnetic field from place to place. They found positive and negative magnetic anomalies. Positive magnetic anomalies are places where the magnetic field is stronger than expected. Positive magnetic anomalies are induced when the rock cools and solidifies with the Earth's north magnetic pole in the northern geographic hemisphere. The Earth's magnetic field is enhanced by the magnetic field of the rock. Negative magnetic anomalies are magnetic anomalies that are weaker than expected. Negative magnetic anomalies are induced when the rock cools and solidifies with the Earth's north magnetic pole in the southern geographic hemisphere. The resultant magnetic field is less than expected because the Earth's magnetic field is reduced by the magnetic field of the rock. From: http://volcano.und.nodak.edu/vwdocs/vwlessons/plate_tectonics/part9.html DIRECTIONS: 1. In the box below, create a magnetic stripe. 2. In the space below, create a magnetic anomaly wiggle that corresponds with your magnetic stripe above. 3. Tear along the dotted line and give your magnetic anomaly wiggles to a partner, and swap for theirs. Be sure that you don’t see each other’s magnetic stripes! 4. In the box below, create the magnetic stripe that matches your partner’s magnetic anomaly wiggle, while your partner does the same for yours. 5. Once both partners have successfully completed the magnetic stripes, compare your originals with your partner’s stripes. How did you do? 6. Are there any differences? What might account for that?