Mohorovicic

noun (proper noun; chiefly attributive, as in "Mohorovicic discontinuity")
/məʊhəˈɹɒvɪtʃɪtʃ/
The Mohorovicic discontinuity (commonly shortened to Moho) is the boundary between the Earth's crust and the mantle, occurring at an average depth of about 35 km beneath continents and about 10 km beneath the ocean floor, identified by an abrupt change in seismic wave velocities.

✍️ Usage in a UPSC answer

Just as the Mohorovicic discontinuity marks the hidden seismic boundary where the Earth's crust yields abruptly to a denser mantle, the transition from welfare populism to fiscal prudence in Indian budgeting is rarely visible on the surface yet decisively governs how shocks propagate through the wider economy.

Synonyms

MohoMohorovicic discontinuitycrust-mantle boundaryM-discontinuityseismic discontinuity

🌱 Word Family

Mohorovicic discontinuity (n phrase), Moho (n abbrev), No standard derived forms

🔡 Root

Proper noun: named after Croatian seismologist Andrija Mohorovičić (1857–1936); entered scientific literature 1930s

📜 Etymology

Named after Croatian seismologist Andrija Mohorovicic (1857-1936), who first identified this boundary in 1909 by studying seismic waves from a Zagreb earthquake; the term entered scientific literature in the 1930s.

🧠 Memory Hook

"MOHO" = the boundary where the crust says "no more" and the MOre-dense mantle begins; recall Mohorovicic as the man who heard the Earth's seismic waves "echo" (-vicic ~ "vich-itch") off this hidden floor.

Tip: press Alt+S to hear pronunciation

Ujiyari Ujiyari — Current Affairs