Certain criticisms regarding the modern mathematical model of this phenomenon launched by so-called Gilbertians assume at least some partial rigidity.
Certain criticisms regarding the modern mathematical model of this phenomenon launched by so-called Gilbertians assume at least some partial rigidity. Despite these criticisms, the Hayford-Bowie model accurately predicts gravitational anomalies that are directly related to topographical features. A precursor explanation of this concept was given by the Finnish scientist Aleksanteri Heiskanen, which represented a compromise between two other earlier hypotheses. According to calculations, the imaginary mathematical line central to this prinicple, called the "depth of compensation" occurs about 70 miles below the surface of the earth. The two earlier hypotheses originally developed in the mid-19th century, differed on whether the central structure had uniform density, the Pratt and Airy hypotheses. Coined by Clarence Dutton, for 10 points, name this tendency of the earth's crust to seek equilibrium
Certain criticisms regarding the modern mathematical model of this phenomenon launched by so-called Gilbertians assume at least some partial rigidity.
Isostasy