mohorovicic discontinuity (Meaning)

Wordnet

mohorovicic discontinuity (n)

the boundary between the Earth's crust and the underlying mantle

No Synonyms and anytonyms found

The Mohorovičić discontinuity, commonly abbreviated as Moho, is the boundary between the Earth's crust and the mantle.
The Moho is characterized by a significant increase in seismic velocity, indicating a change in the composition and density of the Earth.
The depth of the Moho varies depending on the location and geological features of the region being studied.
In oceanic crust, the Moho is typically shallower, around 5-10 kilometers beneath the seafloor.
In continental crust, the Moho is generally deeper, ranging from 25 to 70 kilometers below the surface.
The Moho is not a sharp boundary but rather a transition zone that can span several kilometers in thickness.
The exact nature of the Moho is still not fully understood, but it is believed to be related to changes in mineral composition and crustal structure.
Studying the Moho helps scientists understand the composition and evolution of the Earth's interior.
The Moho is often used as a reference point for seismic imaging and other geophysical investigations.
The name "Mohorovičić discontinuity" comes from Andrija Mohorovičić, a Croatian seismologist who first identified the boundary in 1909.

the boundary between the Earth's crust and the underlying mantle

No synonyms found.

No antonyms found.

The Mohorovičić discontinuity, commonly abbreviated as Moho, is the boundary between the Earth's crust and the mantle.

The Moho is characterized by a significant increase in seismic velocity, indicating a change in the composition and density of the Earth.

The depth of the Moho varies depending on the location and geological features of the region being studied.

In oceanic crust, the Moho is typically shallower, around 5-10 kilometers beneath the seafloor.