New crust is forming at the Mid-Atlantic Ridge, causing the Atlantic ocean to grow wider at a rate of about 3 centimeters per year.
The Pacific Ocean generally has the thinnest oceanic crust compared to other oceans. This thinner crust is due to the presence of numerous trenches and subduction zones around the Pacific Ring of Fire, which causes crustal material to be recycled back into the mantle at a faster rate.
The rate of widening at divergent boundaries in the Atlantic Ocean is approximately 2.5 centimeters per year. This is caused by the seafloor spreading along mid-ocean ridges where tectonic plates move apart. Over time, this process leads to the formation of new oceanic crust.
The same rate as your fingernails are getting longer each year!
The Pacific seafloor formed at a faster spreading rate than the Atlantic seafloor.
The Atlantic Ocean widens at a rate of about 1 inch (2.5 cm) per year due to seafloor spreading along the Mid-Atlantic Ridge. This process involves the movement of tectonic plates, creating new oceanic crust and causing the ocean to gradually widen over time.
5 billion gallons per sec.
formation rate of the ocean crust
The magnetic bands in the eastern Pacific Ocean are more spread out because the spreading rate of the seafloor there is slower compared to the Mid Atlantic Ridge. Slower spreading rates lead to wider magnetic bands as less new crust is being formed over a longer period of time. Conversely, faster spreading rates at the Mid Atlantic Ridge result in narrower magnetic bands due to the more rapid formation of new crust.
Crust is neither formed nor destroyed when the rate of crust formation at mid-ocean ridges equals the rate of crust destruction at subduction zones. This balance is known as isostasy and helps maintain the overall thickness of the Earth's crust.
formation rate of the ocean crust
In a sense, yes. The oceans lay on top of the crust. As the crust moves on top of the mantle at a speed roughly equivalent to the rate of fingernail growth, the ocean gets out of the way.