Earth's mantle is a rocky shell about 2,890 km (1,800 mi) thick that constitutes about 84 percent of Earth's volume. Two main zones are distinguished in the upper mantle: the inner asthenosphere composed of flowing rock in the state of plasticity, about 200 km thick, and the lowermost part of the lithosphere, composed of rigid rock, about 50 to 120 km thick. A thin crust, the upper part of the lithosphere, surrounds the mantle and is about 5 to 75 km thick. The mantle is divided into sections which are based upon results from seismology. These layers (and their depths) are the following: the upper mantle (starting at the Moho, or base of the crust around 7 to 35 km, downward to 410 km), the transition zone (410-660 km), the lower mantle (660-2891 km), and in the bottom of the latter region there is the anomalous D" layer with a variable thickness (on average ~200 km thick)
The metosphere is the name of the mantle
a moving portion of earths crust and upper mantle is called a ridge that's when the ocean floor has underwater volcano that erupts
The upper mantle is in between the lower mantle and the earths crust Crust- the outer most solid shell of the earth. The Uppermost mantle and the earth's crust form the lithosphere.
Upper Mantle. This is also called the Asthenosphere
The crust and uppermost hard rocky mantle, together, is known as the lithosphere, which is above the plastic-like upper mantle area known as the asthenosphere.
The metosphere is the name of the mantle
Continents drift on top of the upper mantle. The core is much further down.
410km
hard rock
about 20 inches
a moving portion of earths crust and upper mantle is called a ridge that's when the ocean floor has underwater volcano that erupts
The lithosphere.
it is the lithosphere
convection currents in the upper mantle
2900 km
there are two parts to the mantle. there is th upper and lower mantle. to the earths interior
It is called the lithosphere.