The Earth's mantle can range from about 500 to 900 degrees Celsius at its upper boundary near the crust to over 4000 degrees Celsius at its lower boundary near the outer core.
The Mohorovičić discontinuity (Moho) is found between the Earth's crust and mantle, typically at a depth of 5-70 kilometers beneath the surface. It is named after Croatian seismologist Andrija Mohorovičić who first identified this boundary based on seismic wave studies.
Biosphere
The sphere that extends from Earth's core to Earth's crust is known as the mantle. It is a layer of solid rock that lies between the core and the crust, making up the majority of Earth's volume. The mantle is divided into the upper mantle and the lower mantle based on depth and composition.
The Earth's crust is composed of two layers: the continental crust, which makes up the landmasses, and the oceanic crust, which forms the seafloor. These two crustal layers differ in composition, thickness, and density.
Moho
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The lower boundary of the Earth's crust is called the Mohorovičić discontinuity, or Moho for short. It is typically located between 5 and 10 kilometers beneath the ocean floor and around 20 to 70 kilometers beneath the continents.
Oceanic crust is denser than continental crust, it floats lower in earths mantle.
There are almost no extrusive rocks on the earths surface because they are all under the earths surface. They are mainly lower than the earths surface.
lower core, upper core, mantle, and crust
The Earth's mantle extends from the base of the crust down to a depth of about 2,900 kilometers (1,800 miles) at the boundary with the outer core. This region is divided into the upper mantle and lower mantle based on differences in composition and behavior.
Gneiss is a part of the earths lower crust. No matter where you drill you will eventually uncover gneiss.
The Earth's mantle can range from about 500 to 900 degrees Celsius at its upper boundary near the crust to over 4000 degrees Celsius at its lower boundary near the outer core.
Oceanic crust is denser than continental crust. Oceanic crust has a density of about 3 g/cm^3, while continental crust has a lower density of about 2.7 g/cm^3.
The section of Earth's crust that moves during an earthquake is called a fault plane. This is where the two tectonic plates that are in contact with each other slip past one another, causing the ground to shake.
The Earth's outermost layer of hard brittle rock is called the crust. The crust is typically about 23 miles thick beneath continents, and about 6.5 miles thick beneath oceans. The crust is relatively light and brittle compared to other Earth layers. Most earthquakes occur within the crust.