Counting marmots…
Lateral movement of river channels through erosion and deposition processes over time
Hillslope soil movement process modeled as diffusive flux proportional to topographic gradient
Physical principle balancing soil transport and production processes to predict soil thickness evolution
Lobate or tongue-shaped masses of rock and ice that form under cold climates in alpine regions and at high latitudes
Rate of bedrock weathering to mobile soil, typically decreasing exponentially with soil depth