The mesoamerican people known as the Olmec are belived to have used loadstones as early as 1000 BC.
provide evidence for sea-floor spreading
Periodically, the magnetic field of the earth reverses polarity. The direction of the magnetic field is recorded in the magnetic properties of rocks when they are erupted. Rocks are being continuously added at sea floor spreading regions, and thus the magnetic reversals are recorded as pairs of parallel 'stripes' alongside the mid ocean spreading ridge.
The earths magnetic polarity at the time of rock formation.
magnetic rocks on the ocean floor show that the Earths magnetic field has been frequently reversed forming new sea floor.
Magnetic alignment of rocks, in alternating strips that run parallel to ridges, indicates reversals in Earth's magnetic field and provides further evidence of seafloor spreading.
As the sea floor spreads the magnetic orientation in the rocks as they cooled is preserved. As the earth's magnetic field changes then a distinct pattern is imprinted in the rocks. If sea floor spreading is true then this unique pattern should be the same on both sides from the spreading point. Measurements of sea bottom rocks verify this symmetry is true. :)
The polarity of the Earth's magnetic field is recorded in igneous rocks, and reversals.
The polarity of the Earth's magnetic field is recorded in igneous rocks, and reversals.
Scientists date sea-floor rocks by looking at patterns in the rocks, including magnetic patterns, and by looking at the geomagnetic reversal time scale.
The seafloor spreads apart, creating new rocks that record magnetic orientation. Small grains of magnetite on the volcanic basalt (ocean floor) have magnetic properties.
provide evidence for sea-floor spreading
provide evidence for sea-floor spreading
provide evidence for sea-floor spreading
Periodically, the magnetic field of the earth reverses polarity. The direction of the magnetic field is recorded in the magnetic properties of rocks when they are erupted. Rocks are being continuously added at sea floor spreading regions, and thus the magnetic reversals are recorded as pairs of parallel 'stripes' alongside the mid ocean spreading ridge.
Rocks have a north and south pole. The sea floor was discovered to have different magnetic poles on cracks in the ocean floor.
The earths magnetic polarity at the time of rock formation.
magnetic rocks on the ocean floor show that the Earths magnetic field has been frequently reversed forming new sea floor.