How is everything going ? <| sep |> Same for me , joined one lobby in the past week and got kicked immediately . Kind of curious if it has to do with a lot of the community being overseas . <| sep |> The free money faucet has been turned off . <| sep |> and is there a way to clear some of the conversation ? <| sep |> Within the simple model I just include continents as an elevation block that adds to the final elevation so I cannot really distinguish between types of collisions . but sure that should be a way to include it nicely , I will think about it ! About the orogeny in the plates , I ' m doing it by a second layer of minor lines denser than the first one something like the results are cool ! If I include so many of them I don ' t even need Perlin noise as background . I also tried with two layers of particles at different temperatures to mimic continental platforms ' flouting ' over the magma . however I couldn ' t make it stable for too long and eventually everything melts and no continent remains . I ' m sure it ' s not impossible but indeed it requires an effort ! So I found a more stable algorithm by just a single layer of grid points interacting with their neighbors and moving along the group velocities . If they collide too heavily they can move under or if they move apart , the tissue can break . It ' s quite promising and I ' m in the process of checking if I can fully substitute the old method by this one . I still like the simple one because of that , simplicity , but as physicist I like one based on physical grounds indeed