Second kind of Earth’s layering ?
kiến thức chung
Rocks near surface are cool, strong, and brittle. This layer = lithosphere (= tectonic plate), includes crust and upper part of mantle (~100 km deep). With > depth (~100 - 300 km), it becomes hotter and rocks become weaker and deform plastically. This rock layer = asthenosphere, located entirely in mantle. Rock in asthenosphere is close to its melting temperature, consists of ~1% melt, 99% solid.
(based on mechanical properties - rock strength)
Rocks near surface are cool, strong, and brittle. This layer = lithosphere (= tectonic plate), includes crust and upper part of mantle (~100 km deep). With > depth (~100 - 300 km), it becomes hotter and rocks become weaker and deform plastically. This rock layer = asthenosphere, located entirely in mantle. Rock in asthenosphere is close to its melting temperature, consists of ~1% melt, 99% solid.
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Hồng Gia Vy