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The plates move relative to each other in varying speeds. The Pacific plate moves against the North American plate at 5 cm/yr. The Arctic Ridge has the slowest rate at less than 2.5 cm/yr., while the East Pacific Rise has the fastest rate at more than 15 cm/yr.
rate of spreading for stripe = width of stripe / time duration If a magnetic strips is 60 km wide and formed over 2 million years, then the rate at which spreading formed the was 30 km/m.y. The rate is equivalent to 3 cm/year. Spreading added an equal width of oceanic crust to a plate on the other side of the mid-ocean ridge, so the total rate of spreading across the ridge was 60 km/m.y. (6 cm/year), a typical rate of seafloor spreading.
Typical rates of spreading average around 5 centimeter (2 inches) per year.
sea-floor spreading
The distance in kilometers of anomaly known (distance) divided by age of anomaly.
The Pacific seafloor formed at a faster spreading rate than the Atlantic seafloor.
The plates move relative to each other in varying speeds. The Pacific plate moves against the North American plate at 5 cm/yr. The Arctic Ridge has the slowest rate at less than 2.5 cm/yr., while the East Pacific Rise has the fastest rate at more than 15 cm/yr.
This depends at what point on Earth's surface you are interested in! For example the Mid Atlantic Ridge separating the North American and Eurasian plates is classified as a "slow" spreading centre with a spreading rate of around 25mm/yr (slow spreading centres generally have a rate of between 20-55 mm per year). This means that the North American plate is moving roughly to the west at a rate of 12.5 mm/yr. However a number of the spreading centres in the Pacific are considered to be "medium to fast" spreading centres with rates of between 80-120 mm/yr. Another example is the Indian plate which is moving north-east at a rate of approximately 50mm/yr causing it to collide with the more slowly moving Eurasian plate. This event started (and is continuing to cause) the Himalayan orogeny.
rate of spreading for stripe = width of stripe / time duration If a magnetic strips is 60 km wide and formed over 2 million years, then the rate at which spreading formed the was 30 km/m.y. The rate is equivalent to 3 cm/year. Spreading added an equal width of oceanic crust to a plate on the other side of the mid-ocean ridge, so the total rate of spreading across the ridge was 60 km/m.y. (6 cm/year), a typical rate of seafloor spreading.
The Pacific region spreads 80-120 mm/yr, while the north Atlantic Ocean is just ~ 25 mm/yr.
100-200 mm
Neither is spreading faster. They are both spreading at the same rate.
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If true, it would indicate that the divergent plates of the eastern Pacific are spreading at a faster rate than the plates of the Mid-Atlantic Ridge.
If true, it would indicate that the divergent plates of the eastern Pacific are spreading at a faster rate than the plates of the Mid-Atlantic Ridge.
An interest rate rise is when a person is late on a bill such as a credit card or insurance bill and the interest rate the person pays goes up.
Typical rates of spreading average around 5 centimeter (2 inches) per year.