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.
Incrase - http://geology.about.com/library/bl/maps/blseafloorage.htm
The further from the ridge, the older the rock. This is measures/observed by using Paleomagnetism.
the ocean floor gets older as distance gets larger
decreases with increasing altitude. as altitude increases so does the distance between the air molecules. increasing distance between air molecules leads to increased resistance to flow.
The measure of change in elevation in a certain distance is called gradient.
As the altitude increases, the temperature in the troposphere will decrease. The troposphere is the lowest portion of planet's atmosphere.
The temperature increases with increasing depth within Earth's crust.
true
as distance increases gravity's force decreases as mass increases gravity's force increases
The force of attraction that decreases as distance increases will change inversely to the square of the distance. This is true for any two objects.
Age of seafloor rock and sediment increases with distance from the oceanic ridges.
The slope increases.
The intensity increases by a factor of 4-APEX
The distance of the object
age increases
not change
The gravitational force then increases by a factor of 4 .
the focal length of the eye lens is adjusted so that the image distance does not change.
The force of gravity between two objects will decrease in proportion to the square of the change of distance between them.
the planet would have its year shorter