As the lithosphere cools, asthenosphere's hot rocks freeze onto their undersides. So lithosphere becomes thicker. As time goes on or within the time period of 10 million years, it even becomes thicker than asthenosphere.
the density increases
The density of the substance becomes higher because of the particles slow down and move closer together when the substance cools.
At mid-ocean ridges, tectonic plates move apart, allowing magma from the mantle to rise and create new crust. This process is known as seafloor spreading. As the magma cools and solidifies, it forms new oceanic crust, which pushes the older crust away from the ridge.
-- The average density of the entire contents of the container decreases,because the density of the shaved ice is less than the density of the waterto which it was added.-- The density of the water alone increases steadily as it cools to 4°C (39°F),then decreases as the water cools further to a lower temperature.
No, water's density decreases as it cools. Water reaches its maximum density at around 4 degrees Celsius, and as it cools further, the water molecules form a crystalline structure, causing the density to decrease.
the density increases
As the oceanic lithosphere moves away from a mid-ocean ridge, it cools and thickens. This process causes the ocean floor to become older and denser, resulting in its gradual subsidence. The farther it gets from the ridge, the deeper the ocean floor becomes due to the increased thickness and weight of the lithosphere.
as air cools, the space it occupies becomes less. this result in an increas density
As air cools, the space it occupies becomes less. This results in an increase in density.
As rock cools, its density increases. This is because cooling causes the atoms and molecules to arrange themselves in a more compact and ordered manner, leading to an increase in the density of the rock.
Nothing they stay the same - their density changes.
The density of the substance becomes higher because of the particles slow down and move closer together when the substance cools.
This process is called seafloor spreading. As magma rises from the mantle to the surface at mid-ocean ridges, it cools and solidifies to form new oceanic lithosphere. This continuous process helps in the expansion of the ocean basins and the movement of tectonic plates.
At mid-ocean ridges, tectonic plates move apart, allowing magma from the mantle to rise and create new crust. This process is known as seafloor spreading. As the magma cools and solidifies, it forms new oceanic crust, which pushes the older crust away from the ridge.
it becomes part of the oceanic crust
New oceanic crust is created at the mid-ocean ridges where rift volcanoes feed solidifying magma from the asthenosphere to both sides of the divergent plate boundaries. The mid-ocean ridge marks the line where heat from the Earth's interior is being carried to the surface by convection currents in the mantle. At the opposite end of the convection currents, colder, denser, and older oceanic crust is being drawn down into the asthenosphere, the birth to death of oceanic crust occurring in roughly 150 million year cycles.
-- The average density of the entire contents of the container decreases,because the density of the shaved ice is less than the density of the waterto which it was added.-- The density of the water alone increases steadily as it cools to 4°C (39°F),then decreases as the water cools further to a lower temperature.