| 单词 | Mohorovicic discontinuity |
| 释义 | Mohorovicic discontinuity /moh'haw roh"veuh chich, -hoh-/, Geol. the discontinuity between the crust and the mantle of the earth, occurring at depths that average about 22 mi. (35 km) beneath the continents and about 6 mi. (10 km) beneath the ocean floor. Also, Moho. [1935-40; named after Andrija Mohorovicic (1857-1936), Croatian geophysicist, who discovered it] |
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