Numerical modeling of the late Cenozoic geomorphic evolution of Grand Canyon, Arizona
Jon D. Pelletier (v. 122, no. 3/4, p. 595–608, doi: 10.1130/B26403.1)
The sentence beginning “The values,” on line 4, column 3, p. 601, should instead read “The value of K′ was assumed to be everywhere equal to the value of K for the strong rocks, hence the value of K′τ reduces to a critical value for τ = SA0.5.
Sediment yield from the tectonically active semiarid Western Transverse Ranges of California
Jonathan A. Warrick and Leal A.K. Mertes (v. 121, no. 7/8, p. 1054–1070,...