X-Received: by 2002:a05:620a:3184:b0:67d:cce9:bab4 with SMTP id bi4-20020a05620a318400b0067dcce9bab4mr9441020qkb.685.1649341972714; Thu, 07 Apr 2022 07:32:52 -0700 (PDT) X-Received: by 2002:a05:6214:e64:b0:441:76a5:22ed with SMTP id jz4-20020a0562140e6400b0044176a522edmr11872605qvb.27.1649341972451; Thu, 07 Apr 2022 07:32:52 -0700 (PDT) Path: csiph.com!weretis.net!feeder6.news.weretis.net!news.misty.com!border2.nntp.dca1.giganews.com!nntp.giganews.com!news-out.google.com!nntp.google.com!postnews.google.com!google-groups.googlegroups.com!not-for-mail Newsgroups: sci.physics.relativity Date: Thu, 7 Apr 2022 07:32:52 -0700 (PDT) Injection-Info: google-groups.googlegroups.com; posting-host=75.172.97.72; posting-account=_-PQygoAAAAciOn_89sZIlnxfb74FzXU NNTP-Posting-Host: 75.172.97.72 User-Agent: G2/1.0 MIME-Version: 1.0 Message-ID: <399dc474-eefb-4bb0-97df-e603c60f293an@googlegroups.com> Subject: Geodesy From: "Ross A. Finlayson" Injection-Date: Thu, 07 Apr 2022 14:32:52 +0000 Content-Type: text/plain; charset="UTF-8" Lines: 18 Xref: csiph.com sci.physics.relativity:582128 Basically looking at world lines in collision, basically for the world lines through the center of the collision, or the layers. In one case, from collision the pressure, moves out all the world lines from meeting in parallel, to diverging in parallel. In the other, the collision makes the world lines as meeting in parallel, to meet or to meet in parallel. Then, it seems the geodesy is between, when collisions are poles and when collisions are not poles, where poles are points or particles, in the space-frame. That the geodesy is between the impulse moments and around the impulse moments, is then that the impulse moments in the geodesy, result in terms between those bounds, what makes for the region, its statistical content, in momentae, or statistics in time, this is what I am looking at to model super-gravity in space-contraction. Which is all very usual .... So, "space-time and geometry", are lifted as the effective, over the effective field equations, left back in the effective field equations, as a tendency to equilibrium. Then for "geodesy", world-line, it's still sum-of-histories and all, it's a "unified theory".