The boundaries between Earth's layers are the crust-mantle boundary (Moho), the mantle-core boundary (Gutenberg discontinuity), and the outer core-inner core boundary.
Gutenburg Discontinuity
The boundary that separates the Earth's core from the mantle is known as the core-mantle boundary (CMB). It lies approximately 2,900 kilometers beneath the Earth's surface and marks the transition between the solid inner core and the molten outer core.
It is the upper and lower mantle. It has the consistency of warm asphalt.
by the plate tectonics
the boundary between mantel and crust is mohorovisic the boundary between mantel and core is guttenberg
"mantel"
"mantel"
The boundary of mantle and core are called Gutenberg Discontinuity
The boundary between the mantle and core of the Earth is called the core-mantle boundary. It is located approximately 2,900 kilometers (1,800 miles) beneath the Earth's surface. This boundary separates the liquid outer core from the solid inner core and is marked by a significant change in density and composition.
The boundary between the mantle and core is called the core-mantle boundary. This region is marked by a significant change in density and composition, representing the transition from the solid mantle to the liquid outer core of the Earth.
The boundary separating the Earth's mantle and core is known as the core-mantle boundary. This boundary is characterized by a sharp decrease in seismic wave velocities, indicating a difference in composition and properties between the outer core and the lower mantle.
The boundary between the inner core and outer core is located approximately 2,900 kilometers beneath the Earth's surface. This boundary is defined by the transition from liquid iron in the outer core to solid iron in the inner core.
The boundaries between Earth's layers are the crust-mantle boundary (Moho), the mantle-core boundary (Gutenberg discontinuity), and the outer core-inner core boundary.
Gutenburg Discontinuity
Yes, the boundary between the liquid outer core and the solid mantle is known as the Gutenberg discontinuity. The Mohorovičić discontinuity, or Moho, is the boundary between the Earth's crust and the mantle.
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