OLD OUTDATED VERSION!
An improved one is here: http://youtu.be/-gQHZM5v9lc
Steady state topography development. Calculated assuming constant uplift rate at the center (x=-50 to +50 km) and a 2D model of stream power law erosion. River erosion is proportional to slope and water discharge. Constant precipitation rate over the entire profile. Calculated under Linux with the program tAo by Garcia-Castellanos.
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