As so ci ate ed i tor: Tomis³aw Go³êbiowski The large neg a tive re sid ual Bouguer grav ity anom aly in north ern Po land called the Pomerania Grav ity Low (PGL) was an alysed us ing Parker's ideal body the ory. A re sid ual grav ity anom aly along the pro file was in verted to find bounds on the den sity con trast, depth, and min i mum thick ness of its sources. As the ideal body reaches the sur face, the great est max i mum neg ative den sity con trast is -0.038 g/cm 3 , while the body it self has a thick ness of 52 km. If 8 km is taken as a depth to the source body top, the den sity con trast must cor re spond to at least -0.092 g/cm 3 , with a max i mum al low able thick ness of 18 km. The ideal body in ver sions show that the depth to the body top can not ex ceed 15 km. As sum ing a geo log i cally rea son able max imum den sity con trast as small as -0.2 g/cm 3 , the source body top can be no deeper than 11.5 km, and its thick ness greater than or equal to 6 km, as sum ing it ex tends up to the Earth sur face, or greater than or equal to 7 km, when its top is be low 8 km depth. It can be hy poth e sized that the main source of the neg a tive grav ity anom aly is re lated to a pre dom i nance of fel sic rocks in the Paleoproterozoic Dobrzyñ Do main of the East Eu ro pean Plat form base ment.