We evaluated the feasibility of quantitative soil mapping in two catenas established on different lithologies (metavolcanic and granitic) in the Sierra Foothill Region of California. Indices of landform and microclimate were extracted from a 1-m elevation model. Variation in soil "character" (clay content, pH, color, cation-exchange capacity [CEC], and Fe o /Fe d ) was partitioned across variables associated with terrain shape and microclimate, lithologic variability, and sampling depth. The potential for using digital elevation models (DEM)-derived indices of terrain shape to predict spatial patterns in soil properties varied greatly between our two experimental catenas. Terrain shape accounted for 4% (metavolcanic site) to 30% (granitic site) of variance in soil properties, while lithology accounted for 14% (metavolcanic site) to 22% (granitic site) of variance in soil properties. Sample depth accounted for 3% (metavolcanic site) to 12% (granitic site) of variance in soil properties. At the metavolcanic site, variability in lithology contributed more to soil variation than terrain shape, which makes digital soil modeling efforts a challenge in these regions. Up to 66% of the variance in soil properties was explained at the granitic site when considering terrain, lithology, sample depth, and associated interactions of these variables. Variance proportions can provide insight into the relative importance of soil-forming factors and is a useful tool when evaluating the efficacy of digital soil mapping projects.Abbreviations: CEC, cation-exchange capacity; CS, conditional simulation; CTI, compound topographic index; DEM, digital elevation models; OK, ordinary kriging; pRDA, partial redundancy analysis; PCA, principal components analysis; QSM, quantitative soil mapping; RDA, redundancy analysis; RCS, restricted cubic splines; RST, regularized splines in tension; RTK, real-time kinematice; SFR, Sierra Nevada Foothill Region; SFREC, Sierra Foothill Research and Extension Center; SJER, San Joaquin Experimental Station; TCI, terrain characterization index; XRF, x-ray fluorescence.T he development and application of the soil-landscape paradigm has played a significant role in how soil scientists conduct research, interpret and communicate their findings, and apply the resulting knowledge to solve real-world problems (Hudson, 1992). Within this framework, repeating patterns in soil properties or classes are correlated with factors that drive redistribution of sediment (slope angle), effective precipitation (surface curvature), and microclimate (slope aspect); and are stratified according to differences in parent material, biota, and time. Traditionally, this approach has been implemented through qualitative evaluation (i.e., mental models) of Hans Jenny's ( Jenny, 1941) state-factor model of soil genesis. Modern extensions to this framework for mapping soils commonly termed digital soil mapping are based on a numerical integration of soil property or class data with quantitative proxies of soil-forming factors (Moore et ...