(Note the lack of tributaries, dry or not, on the canyon walls, as well as the smooth surface of the cliff face. Also, look at the thin layer of soil that is both the same color as, and lies directly on, the bedrock! The plants at the bottom of the valley also tell us that there is a reliable water source.)

(Check out the highly triangular drainage basins! Strange how they are directly below the snow line don’t you think?)
These mountains however experience their significant mass wasting events during the warmer months. When the combination of melting snow and spring rain wash out much of the entisol in their drainage basins. All the way down into the tributaries and streams flowing far below.