- Andrija Mohorovichich or Mohorovičić (1857-1936), Croatian geologist and seismologist who discovered the Mohorovichich discontinuity or Moho
Generated definitions (experimental)
- Andrija Mohorovichich, a Croatian geologist and seismologist
- Mohorovichich discontinuity or Moho
Refers to a historical figure known for contributions to geology and seismology, particularly in the discovery of a significant geological boundary.
Andrija Mohorovichich was born in 1857.
He discovered the Mohorovichich discontinuity.
This term refers to the boundary between the Earth's crust and the underlying mantle, an important concept in geology and seismology.
dì qiú地球de的Mò huò luò wéi qí bù lián xù miàn莫霍洛维奇不连续面shì是dì qiào地壳hé和dì màn地幔zhī jiān之间de的jiè xiàn界限。
The Mohorovichich discontinuity of the Earth is the boundary between the crust and the mantle.
Scientists study the Mohorovichich discontinuity through seismic waves.
Generated collocations (experimental)
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