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1. Divergent plate boundaries. The uplift of magma at the mid-ocean ridge is pushing the two plates apart.

2. The sea floor is older the further away from the mid-ocean ridge. (i.e. New crust is being formed at the mid -ocean ridge and pushing the older crust away.

3. 1 km = 100,000 cm / 3 per yr. = 33,333 years

4. rift zones, pillow basalts, black smokers, etc.

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12y ago
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15y ago

Incrase - http://geology.about.com/library/bl/maps/blseafloorage.htm

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12y ago

The further from the ridge, the older the rock. This is measures/observed by using Paleomagnetism.

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12y ago

the ocean floor gets older as distance gets larger

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Q: As distance from the mid atlantic ridge increases what change in the age of the sea floor is observed?
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