how do geologists think earths atmosphere is formed
the atmosphere is gas emission from when ground release toxic gases, hydrosphere is tsunamis, lithosphere is the shaking of the earth and avalanches.
The continents of the Earth are sliding through the asthenosphere. This is the viscous part of the mantle on which the plates of the lithosphere sit.
They are all formed when tectonic plate boundaries move against each other.
No, stereotyping is a transitive verb of the noun stereotype.It means to represent or categorize as a stereotype.Stereotype means an idea or opinion that is formed about someone or something.
Faults are formed at the outer solid layers of the Earth. They are developed within the earths crust or Lithosphere.
how do geologists think earths atmosphere is formed
The lithosphere consists of the Earth's crust and uppermost part of the mantle, and it is where tectonic plates are formed and move. It is also where geological processes like earthquakes and volcanic activity occur. The lithosphere plays a crucial role in shaping the Earth's surface and is essential for supporting life on our planet.
The lithosphere was formed over a vast expanse of time as the outer skin of the earth solidified from magma.
convergent
because stuff goes and hits some other stuff and.........BOOM..... oceanic lithosphere
the boundry formed by the collision of 2 lithosphere plates
The process of plate tectonics drives the creation and destruction of lithosphere. As new lithosphere is formed at mid-ocean ridges through seafloor spreading, older lithosphere is consumed at subduction zones, creating a balance between formation and destruction over time. This equilibrium maintains a relatively constant amount of lithosphere on Earth.
Diamonds are usually formed in the mantle.
New lithosphere is formed at divergent plate boundaries, where tectonic plates are moving away from each other. The process of seafloor spreading occurs in these areas, with magma rising up from the mantle to create new oceanic crust as it solidifies.
the mantle and the crust, in the lithosphere.
Obviously the older sedimentary rock is denser because it is much more compacted due to overburden.