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Gjeoidi

Nga Wikipedia, enciklopedia e lirë

Gjeoidi (greqisht : ge - tokë dhe eidos - pamje). Eshte siperfaqe ekuipotenciale e cila perputhet perafersisht me nivelin mesatar te detit (Perparim Ameti). Kjo siperfaqe perdoret per referencimin e lartesive orthometrike (mbidetare). Ne cdo pike te gjeoidit forca e rendeses eshte ne kendin 90°, ndersa potenciali i rendeses konstant.

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