Early models for it used a constant velocity parametrization model. Those models only considered the regions of mafic and ultramafic rock that surrounded it. First hypothesized due to an event that occurred in the Kulpa valley, it is marked by a rapid increase in the velocity of compressional waves, and its depth ranges from five to fifty kilometers. Named for a Croatian seismologist, for 10 points, identify this region w
Early models for it used a constant velocity parametrization model. Those models only considered the regions of mafic and ultramafic rock that surrounded it. First hypothesized due to an event that occurred in the Kulpa valley, it is marked by a rapid increase in the velocity of compressional waves, and its depth ranges from five to fifty kilometers. Named for a Croatian seismologist, for 10 points, identify this region which forms the boundary between the crust and the mantle.
Early models for it used a constant velocity parametrization model.