Replying to:<BR/><DIV CLASS='Discussion_PostQuote'>I don't think density really has anything to do with the phenomena being described. Certainly, it plays a role in determining the mass of an object and the density gradient between the core and the surface, but the phenomena is probably best described with:g = [G(M1*m)/r^2] - [G(M2*m)/r^2] Where the M1 is the mass below you and M2 is the mass above you. This should give you a net gravitaional force felt on m (you). Once you determine the mass, you can assume the density is uniform. Obviously, you have to recalculate the mass as you bore down because the earth is not of uniform density, but once you determine the mass, the density is a non-factor.I think what I am trying to say is that density gradient within a sphere will affect the location where the graviational forces can start decreasing, but even if the desnity was uniform throughout, the phenomena would still exist. <br />Posted by derekmcd</DIV><br /><br />Yes, you said it very well. <div class="Discussion_UserSignature"> <p><font color="#000080"><em><font color="#000000">But the Krell forgot one thing John. Monsters. Monsters from the Id.</font></em> </font></p><p><font color="#000080">I really, really, really, really miss the "first unread post" function</font><font color="#000080"> </font></p> </div>