“…The gravitational field of a cube was apparently first calculated in (MacMillan, 1958) and later extended to cuboid masses (Nagy, 1966;Mufti, 2006a), including varying density (Garcia-Abdeslem, 2005;Hansen, 1999) and also for general polyhedra (Paul, 1974;Coggon, 1976), as well as for a range of simpler planar objects such as straight line segments as well as disks and annular shapes (Riaguas et al, 1999;2001;Azevedo and Ontaneda, 2007;Azevedo et al, 2005;Fukushima, 2010;Alberti and Vidal, 2007;Blesa, 2005;Gutierrez-Romero et al, 2004;Palacian et al, 2006;Iorio, 2007;2012). These results were found to have application in the calculation of the gravitational anomalies on the Earth (Mufti, 2006b) and the slowdown of the Earth's rotation rate due to tidal drag (Celnikier, 1990).…”