The final section of the Earth might be compared to the yolk of the egg
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Moho
The Moho
The clitellum is a part of the earthworm's reproductive system. It is the part of the worm that makes the egg cocoon.
The discovery of the Mohorovičić discontinuity, or Moho, was primarily based on the observation that seismic waves travel at different speeds through the Earth's crust and mantle. When seismic waves generated by earthquakes were recorded, scientists noted a significant increase in velocity at a certain depth, indicating a transition from the less dense crust to the denser mantle. This abrupt change in wave speed suggested a distinct boundary, which was subsequently identified as the Moho. The depth of the Moho varies, typically located about 5 to 10 kilometers beneath the oceanic crust and around 30 kilometers beneath continental crust.
The part of an egg that is compared to the Moho is the yolk. The Mohorovičić discontinuity, or Moho, is the boundary between the Earth's crust and mantle. Similarly, the yolk is the inner portion of an egg surrounded by the egg white, just as the mantle surrounds the Earth's crust. Both the yolk and the Moho represent a distinct layer within their respective structures.
The Moho separates the crust and the mantle.
He compares him to a serpent's egg.
FeaR is MoHo
The boundary that separates the Earth's crust and the cooler part of the mantle is called the Mohorovičić discontinuity or Moho. It marks the transition between the Earth's crust and the uppermost part of the mantle.
The Moho, or Mohorovicic Discontinuity, is the boundary between the crust and the mantle.
A Part-to-part ratio
"moho" is the plate boundary between earth's crust and the mantle.
Mass
the lens
The chimney.
A fraction.