Between the thin rocky crust and inner core, in order from upper to lower, are the upper mantle, mantle, and outer core.
The mantle.
The mantle lies between the crust, which is the outermost layer of the Earth, and the core, which is the innermost layer of the Earth. The mantle is a region of hot, flowing rock that lies beneath the Earth's crust and above the core.
The boundary between the crust and the mantle was discovered by Croatian seismologist Andrija Mohoroviฤiฤ in 1909. This boundary is known as the Mohoroviฤiฤ discontinuity or "Moho" and marks the change in seismic wave velocities between the Earth's crust and mantle.
The upper mantle is located beneath the Earth's crust, extending from about 30 to 400 kilometers deep. It is part of the Earth's mantle layer, which lies between the crust and the core.
It is between the Crust and the upper mantle
moho
moho
It is between the Crust and the upper mantle
The Moho Barrier is characterized by a seismic velocity discontinuity that separates the Earth's crust from the underlying mantle. It is located at an average depth of about 25-35 kilometers beneath continental crust and 5-10 kilometers beneath oceanic crust.
Moho barrier: Top of mantleOceanic crust: Thinnest layerUpper mantle: Moves the crustLower mantle: Borders liquid core
15 kilo meters is the distance between the crust and the mantle
The Mohorovicic Discontinuity (also known as the Moho) separates the Earth's crust from the underlying mantle. It is the boundary where seismic waves change speed, indicating a change in composition and density between the two layers.
a mantle is something between the crust
The boundary between the crust and upper mantle is known as the Mohoroviฤiฤ discontinuity or Moho. It represents the change in seismic wave velocity and composition between the rigid outer layer (crust) and the more ductile layer beneath (mantle).
The mantle.
The mantle.