quote: Original post by CrankDude
How about considering the fact that seperated land masses that sit by each other have "interlocking" features? Like when the earth''s plate moved and such and the continents divided, and the land ripped apart, you can still see how many pieces fit together. I had an idea about generating land by considering how the continents divide, which would form oceans and such, also considering erosion and other factors. Just let the program start with a big blob of land and let it calculate what it would be in x thousands of years.
Dude, I was trying to simulate tectonic uplift, which is essentially two plates crunching together. In the ''island'' picture, all the terrain is eroded equally and considered the same age. What I wanted to add was the uplift part, so that certain ridges, etc. continue to rise and impart their ''youngish'' features. As for the plates shifting and moving apart, I hadn''t looked into that.