Earth's mantle has part(s) Upper mantle
Structure
Rheology
Earth's mantle is divided into two major rheological layers: the rigid lithosphere comprising the uppermost mantle, and the more ductile asthenosphere, separated by the lithosphere-asthenosphere boundary. Lithosphere underlying ocean crust has a thickness of around 100 km, whereas lithosphere underlying continental crust generally has a thickness of 150–200 km. The lithosphere and overlying crust make up tectonic plates, which move over the asthenosphere.
The Earth's mantle is divided into three major layers defined by sudden changes in seismic velocity:
the upper mantle (starting at the Moho, or base of the crust around 7 to 35 km (4.3 to 21.7 mi) downward to 410 km (250 mi))
the transition zone (approximately 410–660 km or 250–410 mi), in which wadsleyite (≈ 410–520 km or 250–320 mi) and ringwoodite (≈ 525–660 km or 326–410 mi) are stable
the lower mantle (approximately 660–2,891 km or 410–1,796 mi), in which bridgmanite (≈ 660–2,685 km or 410–1,668 mi) and post-perovskite (≈ 2,685–2,891 km or 1,668–1,796 mi) are stableThe lower ~200 km of the lower mantle constitutes the D" (D-double-prime) layer, a region with anomalous seismic properties. This region also contains large low-shear-velocity provinces and ultra low velocity zones.
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