Do you have more ideas to share? What project are you thinking of? Please leave a comment and help the GIS student community!
kω = dz/dt = k ρ g Q S / W
Substitution allows the rewriting the Stream Power equation. dz/dt is the vertical change in the elevation of the channel bed over time (advection or erosion and removal of bed material). The coefficient k accounts for erodibility of the channel bed influenced by rock strength, fracture density, and fissibility (and perhaps more).
See the calendar of upcoming exhibits and lectures at all of our library locations.
There will also be further costs for the following, not purchasable from the University: