The lithosphere was formed over a vast expanse of time as the outer skin of the earth solidified from magma.
New oceanic lithosphere forms as a result of seafloor spreading at mid-ocean ridges. Magma rises from the mantle, solidifies at the mid-ocean ridge, and creates new oceanic crust. This process leads to the continuous expansion of the ocean floor.
The lithosphere consists of the crust and upper mantle.
The crust is the outer layer of the lithosphere.
The lithosphere is composed of the brittle rock that forms the outer layer of the planet. The lithosphere is divided into plates which move independently from each other.
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.
False. It forms in the Athenosphere!!
it forms
New oceanic lithosphere forms as a result of seafloor spreading at mid-ocean ridges. Magma rises from the mantle, solidifies at the mid-ocean ridge, and creates new oceanic crust. This process leads to the continuous expansion of the ocean floor.
it forms the lithosphere
The lithosphere consists of the crust and upper mantle.
ocean,sea,ponds,rivers and swamps.
The crust is the outer layer of the lithosphere.
forms when two {crustal} lithosphere plates move apart.
The lithosphere is composed of the brittle rock that forms the outer layer of the planet. The lithosphere is divided into plates which move independently from each other.
The lithosphere.
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.
depends on what you belive creation or evalution