Rocks on the seafloor on either side of a mid ocean spreading ridge preserve a record of the earth s magnetic field over time.
Interactive sea floor spreading games.
This interactive activity is simple to prepare and to execute and allows the students to understand seafloor spreading and the position of newer rock and older rock in relation to the mid oceanic ridge.
Because it takes a long time for the crust to move the crust at the trenches is about 200 million years old.
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Play continental drift and seafloor spreading games in an arcade style format.
As magma starts to harden into rock iron rich minerals solidify first.
Most basalt magmas contain abundant molten iron.
In total there are nine games in this learning objective including.
Search for the seafloor.
The cycle of new seafloor forming and old seafloor subducting is extremely slow with the plates shifting just a few centimeters per year.
Seafloor spreading is the movement of magma through a crack in a mid oceanic ridge.
This can result in an ever widening seafloor at the.
The discovery of this phenomenon was an important bit of evidence that helped confirm the theory of plate tectonics.
The interactive animation below illustrates this concept.
Plate tectonics and sea floor spreading for science interactive notebooks teaching the concept of sea floor spreading can be easily modeled using my simple yet powerful interactive resource for science interactive notebooks.
One intriguing thing about the rock that comes from seafloor spreading is that it shows the history of the earth.
The rocks on the seafloor show the history of the magnetic changes in the earth.
Seafloor spreading is the continuous process of forming new igneous rock at midocean ridges by injection of magma that forms new seafloor.
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Their crystals are pulled into alignment by the earth s magnetic field just like a compass needle is pulled towards magnetic north.
For example every million years the earth s magnetic poles tend to reverse 4 or 5 times.
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South becomes north and north becomes south.