The interactive animation below illustrates this concept.
Interactive sea floor spreading games.
Once the basalt cools completely into solid rock the.
The discovery of this phenomenon was an important bit of evidence that helped confirm the theory of plate tectonics.
As magma starts to harden into rock iron rich minerals solidify first.
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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Most basalt magmas contain abundant molten iron.
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.
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.
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Seafloor spreading is the movement of magma through a crack in a mid oceanic ridge.
Search for the seafloor.
Rocks on the seafloor on either side of a mid ocean spreading ridge preserve a record of the earth s magnetic field over time.
This can result in an ever widening seafloor at the.
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The process is continuous because forces cause opposite sides of the midocean ridge to constantly move apart making new room for the process to repeat.
The cycle of new seafloor forming and old seafloor subducting is extremely slow with the plates shifting just a few centimeters per year.
Play continental drift and seafloor spreading games in an arcade style format.
One intriguing thing about the rock that comes from seafloor spreading is that it shows the history of the earth.
South becomes north and north becomes south.
Their crystals are pulled into alignment by the earth s magnetic field just like a compass needle is pulled towards magnetic north.
The rocks on the seafloor show the history of the magnetic changes in the earth.