Who discovered gutenberg discontinuity On 8 October an earthquake occurred with its epicenter in the Pokuplje region, 39 km southeast of Zagreb. A number of seismographs, installed beforehand, provided invaluable data, which led Mohorovičić to new discoveries.
Mohorovicic pronunciation Croatian seismologist Andrija Mohorovičić is credited with discovering and defining the Moho. [11] In , he was examining data from a local earthquake in Zagreb when he observed two distinct sets of P-waves and S-waves propagating out from the focus of the earthquake. [12].
Andrija mohorovicic pronunciation To one of Mohorovičić’s biggest contributions to science belogs the famous Mohorovičić Discontinuity, which was discovered around and it can be described as the boundary between the Earth’s crust and the mantle.
Beno gutenberg contribution The Mohorovicic Discontinuity was discovered in by Andrija Mohorovicic, a Croatian seismologist. Mohorovicic realized that the velocity of a seismic wave is related to the density of the material that it is moving through.
Andrija mohorovicic contribution One of the first to make a major contribution was Andrija Mohorovicic, a prominent Croatian meteorologist and seismologist. The boundary between the Earth's crust and the underlying upper mantle is now recognised by a significant increase in the velocity of seismic P-waves at depths between 15 and 50 km depth.
Gutenberg discontinuity
Mohorovičić, Andrija (–) A Croatian seismologist, Mohorovičić discovered a seismic discontinuity (since named after him, see MOHOROVIČIĆ DISCONTINUITY) at the crust–mantle boundary, when analysing the results of an earthquake in Mohorovicic discontinuity Andrija Mohorovicic Croatian geologist who discovered Earth's crust-mantle boundary—the Mohorovicic discontinuity. Mohorovicic's study of seismic records from a earthquake revealed two distinct sets of waves.
Who discovered the crust Andrija Mohorovicic discovered the boundary between the crust and the mantle. Mohorovicic's major contribution for which he is famous is the discovery of the discontinuity between the mantle and the crust. In a major earthquake in Croatia provided Mohorovicic with empirical evidence that he used to discover the division between the crust and the mantle, as well as the mantel and the core.