I ' m Mexican that dates lost white women . You have nothing to worry about . Hispanics are really welcoming . Only issue would be if your boyfriend was one momma ' boy . <| sep |> Man marble brewery looks pretty different even since this pic was first done <| sep |> Everyone talking about Florida lol . A bunch of stupid pussies that got nothin on Philly . <| sep |> Part of me loves the simplicity of this , but when compared with actual orogeny , I think you ' d get better results if you were taking more geologic principles into account . I would say you ' d need to simulate at the minimum both oceanic and continental crust , and simulate the differences between their collisions . Oceanic crust running into continental crust tends to create subduction zones , with associated low altitude forearc coastal mountains and high altitude volcanic mountains on the continental side , and a trench on the oceanic side . Continental crust running into continental crust creates extreme ranges like the Himalayas . You ' d also have to extend your orogeny to include regions further from the plate boundaries themselves . Perhaps an easy way to do that would be to create ripples of subranges that extend away from your convergent boundaries . Or , why not go all the way down the rabbit hole and start modeling lithosphere riding on top of a molten , plastic mantle ? Treat the material of the plates like semipliable , semibrittle lithosphere , that gets fractured and folded by the stress of the plates interacting . Go all the way to simulating physics . That sounds like a pain . but it might be worth it