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
Ocean lithosphere forms at mid-ocean ridges, where tectonic plates diverge and magma rises from the mantle to create new oceanic crust. As the magma cools and solidifies, it forms basaltic rock, which composes the ocean floor. This process is part of seafloor spreading, where the newly formed lithosphere gradually moves away from the ridge, allowing for the continuous renewal of the oceanic crust. Over time, this lithosphere can be subducted back into the mantle at convergent plate boundaries.
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.
New oceanic crust and lithosphere are formed at mid-ocean ridges through the process of seafloor spreading. As tectonic plates diverge, magma from the mantle rises to fill the gap, cools, and solidifies, creating new basaltic crust. This newly formed crust is part of the lithosphere, which includes the rigid outer layer of the Earth. Over time, the new crust moves away from the ridge, contributing to the dynamic nature of plate tectonics.
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 results in an increase in density.
as air cools, the space it occupies becomes less. this result in an increas 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.
Ocean lithosphere forms at mid-ocean ridges, where tectonic plates diverge and magma rises from the mantle to create new oceanic crust. As the magma cools and solidifies, it forms basaltic rock, which composes the ocean floor. This process is part of seafloor spreading, where the newly formed lithosphere gradually moves away from the ridge, allowing for the continuous renewal of the oceanic crust. Over time, this lithosphere can be subducted back into the mantle at convergent plate boundaries.
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.
New oceanic crust and lithosphere are formed at mid-ocean ridges through the process of seafloor spreading. As tectonic plates diverge, magma from the mantle rises to fill the gap, cools, and solidifies, creating new basaltic crust. This newly formed crust is part of the lithosphere, which includes the rigid outer layer of the Earth. Over time, the new crust moves away from the ridge, contributing to the dynamic nature of plate tectonics.
it becomes part of the oceanic crust