Mohorovičić discontinuity - Wikipedia
The Mohorovičić discontinuity (/ ˌ m oʊ h ə ˈ r oʊ v ɪ tʃ ɪ tʃ / MOH-hə-ROH-vih-chitch; Croatian: [moxorôʋiːtʃitɕ]) [1] – usually called the Moho discontinuity, Moho boundary, or just Moho – is the boundary between the Earth's crust and the mantle.
Mohorovicic Discontinuity - The Moho - Geology.com
What is the Mohorovičić Discontinuity? The Mohorovicic Discontinuity, or "Moho," is the boundary between the crust and the mantle. The red line in the diagram shows its location. In geology the word "discontinuity" is used for a surface at which seismic waves change velocity.
Mohorovicic Discontinuity: The Crust-Mantle Boundary
2023年12月3日 · This discontinuity is also known as the Mohorovicic boundary. You can also colloquially call it the Moho or the Moho discontinuity. It is named after Andrija Mohorovičić, who discovered it. In geology, a discontinuity marks a surface with …
What Is the Mohorovicic Discontinuity and Can Humans Ever …
Mohorovicic discontinuity (pronounced moh-haw- roh - vuh -chich), more commonly known as the "Moho," is the geological term that describes the boundary zone between Earth's crust and the lower-lying mantle.
Moho | Crustal Discontinuity, Seismic Wave & Earth’s ... - Britannica
Moho, boundary between the Earth’s crust and its mantle. The Moho lies at a depth of about 22 mi (35 km) below continents and about 4.5 mi (7 km) beneath the oceanic crust. Modern instruments have determined that the velocity of seismic waves increases rapidly at this boundary.
What is the Mohorovicic Discontinuity? - WorldAtlas
2017年8月1日 · The Mohorovicic discontinuity layer marks the end of the earth’s crust and is estimated to be between 1 to 4 miles thick depending on the oceanic or continental crusts. It lies below the basalt rock system and above the dunites rock systems.
Moho Discontinuity - Explanation, Discovery, Role and FAQs
Moho discontinuity is defined as the boundary between Earth's crust and the mantle, observed by a sharp increase in the velocity of the seismic waves passing through the Earth. The name Mohorovicic discontinuity was received from Croatian geophysicist Andrija Mohorovičič, in 1909.
Mohorovičić Discontinuity (Moho) - SpringerLink
2014年11月19日 · The Mohorovičić seismic discontinuity, known today as the Moho, was discovered in 1909 by Andrija Mohorovičić. It is defined by a jump in seismic velocities from 5.6 to ~7.8 km/s. It represents the boundary between the more felsic crust and the mafic mantle.
The Mohorovičić discontinuity, also known as the Moho, is a discrete jump in seismic wave velocities – a seismic discontinuity – that has come to define the boundary between the crust and the mantle.
Discovery of Mohorovičić's (Moho) Discontinuity I Geotech …
Moho discontinuity On October 8, 1909, a strong earthquake hit the Pokuplje area. Its epicenter was about 40 km southeast of Zagreb near Pokupsko, where the intensity of the VIII ˚MCS scale was estimated.