Ahnert, F. (1970), Functional relationships between denudation, relief, and
uplift in large mid-latitude drainage basins, Am. J. Sci., 268(3), 243–263,
doi:10.2475/ajs.268.3.243.
Andrews, D. J., and R. C. Bucknam (1987), Fitting degradation of shoreline
scarps by a nonlinear diffusion model, J. Geophys. Res., 92(B12),
12,857–12,867, doi:10.1029/JB092iB12p12857.
Attal, M., P. A. Cowie, A. C. Whittaker, D. Hobley, G. E. Tucker, and G. P.
Roberts (2011), Testing fluvial erosion models using the transient
response of bedrock rivers to tectonic forcing in the Apennines, Italy,
J. Geophys. Res., 116, F02005, doi:10.1029/2010JF001875.
Balco, G., J. O. Stone, N. A. Lifton, and T. J. Dunai (2008), A complete
and easily accessible means of calculating surface exposure ages or
erosion rates from 10Be and 26Al measurements, Quat. Geochronol.,
3(3), 174–195, doi:10.1016/j.quageo.2007.12.001.
Bierman, P., and E. J. Steig (1996), Estimating rates of denudation using cosmogenic
isotope abundances in sediment, Earth Surf. Processes Landforms,
21(2), 125–139, doi:10.1002/(SICI)1096-9837(199602)21:2<125::
AID-ESP511>3.0.CO;2-8.
Bierman, P. R., M. C. Caffee, P. T. Davis, K. Marsella, M. Pavich,
P. Colgan, D. Mickelson, and J. Larsen (2002), Rates and timing of Earth
surface processes from in situ–produced cosmogenic 10Be, in Beryllium:
Mineralogy, Petrology, and Geochemistry, Rev. Mineral. Geochem.,
vol. 50, edited by E. Grew, pp. 147–205, doi:10.2138/rmg.2002.50.4,
Mineral. Soc. of Am., Washington, D. C.
Binnie, S. A., W. M. Phillips, M. A. Summerfield, and L. K. Fifield (2007),
Tectonic uplift, threshold hillslopes, and denudation rates in a developing
mountain range, Geology, 35(8), 743–746, doi:10.1130/G23641A.1.
Brown, E. T., R. F. Stallard, M. C. Larsen, G. M. Raisbeck, and F. Yiou
(1995), Denudation rates determined from the accumulation of in
situ–produced 10Be in the luquillo experimental forest, Puerto Rico,
Earth Planet. Sci. Lett., 129(1–4), 193–202, doi:10.1016/0012-821X
(94)00249-X.
Burbank, D. W., J. Leland, E. Fielding, R. S. Anderson, N. Brozovic, M. R.
Reid, and C. Duncan (1996), Bedrock incision, rock uplift and threshold
hillslopes in the northwestern Himalayas, Nature, 379(6565), 505–510,
doi:10.1038/379505a0.
Busby, C. J., and K. Putirka (2009), Miocene evolution of the western edge
of the Nevadaplano in the central and northern Sierra Nevada: Palaeocanyons,
magmatism, and structure, Int. Geol. Rev., 51(7–8), 670–701,
doi:10.1080/00206810902978265.
Cecil, M. R., M. N. Ducea, P. W. Reiners, and C. G. Chase (2006), Cenozoic
exhumation of the northern Sierra Nevada, California, from (U-Th)/
He thermochronology, Geol. Soc. Am. Bull., 118(11–12), 1481–1488,
doi:10.1130/B25876.1.
Clark, D. H. (1995), Extent, timing, and climatic significance of latest
Pleistocene and Holocene glaciation in the Sierra Nevada, California,
PhD thesis, 193 pp., Univ. of Wash., Seattle.
Clark, M. K., G. Maheo, J. Saleeby, and K. A. Farley (2005), The nonequilibrium
landscape of the southern Sierra Nevada, California, GSA
Today, 15(9), 4–10, doi:10.1130/1052-5173(2005)015[4:TNLOTS]2.0.
CO;2.
Codilean, A. T. (2006), Calculation of the cosmogenic nuclide production
topographic shielding scaling factor for large areas using DEMs, Earth
Surf. Processes Landforms, 31(6), 785–794, doi:10.1002/esp.1336.
Cowie, P. A., A. C. Whittaker, M. Attal, G. P. Roberts, G. E. Tucker,
and A. Ganas (2008), New constraints on sediment-flux-dependent
river incision: Implications for extracting tectonic signals from river
profiles, Geology, 36(7), 535–538, doi:10.1130/G24681A.1.
Crosby, B. T., K. X. Whipple, N. M. Gasparini, and C. W. Wobus (2007),
Formation of fluvial hanging valleys: Theory and simulation, J. Geophys.
Res., 112, F03S10, doi:10.1029/2006JF000566.
Culling, W. E. H. (1960), Analytical theory of erosion, J. Geol., 68(3),
336–344, doi:10.1086/626663.
Cyr, A. J., D. E. Granger, V. Olivetti, and P. Molin (2010), Quantifying
rock uplift rates using channel steepness and cosmogenic nuclidedetermined
erosion rates: Examples from northern and southern Italy,
Lithosphere, 2(3), 188–198, doi:10.1130/L96.1.
Daly, C., G. Taylor, and W. Gibson (1997), The PRISM approach to mapping
precipitation and temperature, paper presented at 10th Conference
on Applied Climatology, Am. Meteorol. Soc., Reno, Nev.
Davis, W. M. (1892), The convex profile of badland divides, Science, 20,
245, doi:10.1126/science.ns-20.508.245.
Day, H. W., and M. E. Bickford (2004), Tectonic setting of the Jurassic
Smartville and Slate Creek complexes, northern Sierra Nevada, California,
Geol. Soc. Am. Bull., 116(11–12), 1515–1528, doi:10.1130/B25416.1.
Densmore, A. L., M. A. Ellis, and R. S. Anderson (1998), Landsliding and
the evolution of normal-fault-bounded mountains, J. Geophys. Res.,
103(B7), 15,203–15,219, doi:10.1029/98JB00510.
DiBiase, R. A., and K. X. Whipple (2011), The influence of erosion thresholds
and runoff variability on the relationships among topography, climate,
and erosion rate, J. Geophys. Res., 116, F04036, doi:10.1029/
2011JF002095.
DiBiase, R. A., K. X. Whipple, A. M. Heimsath, and W. B. Ouimet (2010),
Landscape form and millennial erosion rates in the San Gabriel Mountains,
CA, Earth Planet. Sci. Lett., 289(1–2), 134–144, doi:10.1016/j.
epsl.2009.10.036.
DiBiase, R. A., A. M. Heimsath, and K. X. Whipple (2012), Hillslope
response to tectonic forcing in threshold landscapes, Earth Surf. Processes
Landforms, doi:10.1002/esp.3205, in press.
Dietrich, W. E., D. G. Bellugi, L. S. Sklar, and J. D. Stock (2003), Geomorphic
transport laws for predicting landscape form and dynamics, in Prediction
in Geomorphology, Geophys. Monogr. Ser, vol. 135, edited by
P. R. Wilcock and R. M. Iverson, pp. 103–132, AGU, Washington,
D. C., doi:10.1029/135GM09.
Dunai, T. J. (2000), Scaling factors for production rates of in situ produced
cosmogenic nuclides: A critical reevaluation, Earth Planet. Sci. Lett.,
176(1), 157–169, doi:10.1016/S0012-821X(99)00310-6.
Evans, I. S. (1980), An integrated system of terrain analysis and slope mapping,
Z. Geomorphol., 36, 274–295.
Fernandes, N. F., and W. E. Dietrich (1997), Hillslope evolution by diffusive
processes: The timescale for equilibrium adjustments, Water Resour.
Res., 33(6), 1307–1318, doi:10.1029/97WR00534.
Finnegan, N. J., G. Roe, D. R. Montgomery, and B. Hallet (2005), Controls
on the channel width of rivers: Implications for modeling fluvial incision
of bedrock, Geology, 33(3), 229–232, doi:10.1130/G21171.1.
Foufoula-Georgiou, E., V. Ganti, and W. Dietrich (2010), A nonlocal theory
of sediment transport on hillslopes, J. Geophys. Res., 115, F00A16,
doi:10.1029/2009JF001280.
Gabet, E. J. (2000), Gopher bioturbation: Field evidence for non-linear hillslope
diffusion, Earth Surf. Processes Landforms, 25(13), 1419–1428,
doi:10.1002/1096-9837(200012)25:13<1419::AID-ESP148>3.0.CO;2-1.
Gabet, E. J., and S. M. Mudd (2010), Bedrock erosion by root fracture and
tree throw: A coupled biogeomorphic model to explore the humped soil
production function and the persistence of hillslope soils, J. Geophys.
Res., 115, F04005, doi:10.1029/2009JF001526.
Gangodagamage, C., P. Belmont, and E. Foufoula-Georgiou (2011), Revisiting
scaling laws in river basins: New considerations across hillslope
and fluvial regimes, Water Resour. Res., 47, W07508, doi:10.1029/
2010WR009252.
Gilbert, G. K. (1877), Report on the Geology of the Henry Mountains,
160 pp., U.S. Gov. Print. Off., Washington, D. C.
Gilbert, G. K. (1909), The convexity of hilltops, J. Geol., 17(4), 344–350,
doi:10.1086/621620.
Gosse, J. C., and F. M. Phillips (2001), Terrestrial in situ cosmogenic
nuclides: Theory and application, Quat. Sci. Rev., 20(14), 1475–1560,
doi:10.1016/S0277-3791(00)00171-2.
Granger, D. E., J. W. Kirchner, and R. Finkel (1996), Spatially averaged
long-term erosion rates measured from in situ–produced cosmogenic
nuclides in alluvial sediment, J. Geol., 104(3), 249–257, doi:10.1086/
629823.
Heimsath, A. M., W. E. Dietrich, K. Nishiizumi, and R. C. Finkel (1997),
The soil production function and landscape equilibrium, Nature,
388(6640), 358–361, doi:10.1038/41056.
Heimsath, A. M., J. Chappell, W. E. Dietrich, K. Nishiizumi, and R. C.
Finkel (2001), Late Quaternary erosion in southeastern Australia: A field
example using cosmogenic nuclides, Quat. Int., 83–85, 169–185,
doi:10.1016/S1040-6182(01)00038-6.
Heimsath, A. M., R. A. DiBiase, and K. X. Whipple (2012), Soil production
limits and the transition to bedrock-dominated landscapes, Nat. Geosci.,
5, 210–214, doi:10.1038/NGEO1380.
Hobley, D. E. J., H. D. Sinclair, and P. A. Cowie (2010), Processes, rates,
and time scales of fluvial response in an ancient postglacial landscape
of the northwest Indian Himalaya, Geol. Soc. Am. Bull., 122(9–10),
1569–1584, doi:10.1130/B30048.1.
Howard, A. D. (1988), Equilibrium models in geomorphology, in Modelling
Geomorphological Systems, edited by M. G. Anderson, pp. 49–72,
John Wiley, New York.
Howard, A. D. (1994), A detachment-limited model of drainage-basin evolution,
Water Resour. Res., 30(7), 2261–2285, doi:10.1029/94WR00757.
Jones, C. H., G. L. Farmer, and J. Unruh (2004), Tectonics of Pliocene
removal of lithosphere of the Sierra Nevada, California, Geol. Soc. Am.
Bull., 116(11–12), 1408–1422, doi:10.1130/B25397.1.
Kirby, E., and W. Ouimet (2011), Tectonic geomorphology along the eastern
margin of Tibet: Insights into the pattern and processes of active
deformation adjacent to the Sichuan Basin, Spec. Publ. Geol. Soc., 353,
165–188, doi:10.1144/SP353.9.
Kirby, E., K. X. Whipple, W. Tang, and Z. Chen (2003), Distribution of
active rock uplift along the eastern margin of the Tibetan Plateau:
Inferences from bedrock channel longitudinal profiles, J. Geophys.
Res., 108(B4), 2217, doi:10.1029/2001JB000861.
Kirby, E., C. Johnson, K. Furlong, and A. Heimsath (2007), Transient channel
incision along Bolinas Ridge, California: Evidence for differential
rock uplift adjacent to the San Andreas fault, J. Geophys. Res., 112,
F03S07, doi:10.1029/2006JF000559.
Korup, O., and F. Schlunegger (2007), Bedrock landsliding, river incision,
and transience of geomorphic hillslope-channel coupling: Evidence from
inner gorges in the Swiss Alps, J. Geophys. Res., 112, F03027,
doi:10.1029/2006JF000710.
Lashermes, B., E. Foufoula-Georgiou, and W. E. Dietrich (2007), Channel
network extraction from high resolution topography using wavelets, Geophys.
Res. Lett., 34, L23S04, doi:10.1029/2007GL031140.
Lea, N. J. (1992), An aspect-driven kinematic routing algorithm, in Overland
Flow: Hydraulics and Erosion Mechanics, edited by A. J. Parsons
and A. D. Abrahams, pp. 393–407, U. C. L. Press, London.
Lifton, N. A., J. W. Bieber, J. M. Clem, M. L. Duldig, P. Evenson, J. E.
Humble, and R. Pyle (2005), Addressing solar modulation and longterm
uncertainties in scaling secondary cosmic rays for in situ cosmogenic
nuclide applications, Earth Planet. Sci. Lett., 239, 140–161,
doi:10.1016/j.epsl.2005.07.001.
Matsushi, Y., and H. Matsuzaki (2010), Denudation rates and threshold
slope in a granitic watershed, central Japan, Nucl. Instrum. Methods Phys.
Res., Sect. B, 268(7–8), 1201–1204, doi:10.1016/j.nimb.2009.10.133.
Montgomery, D. R. (2001), Slope distributions, threshold hillslopes, and
steady-state topography, Am. J. Sci., 301(4–5), 432–454, doi:10.2475/
ajs.301.4-5.432.
Montgomery, D. R., and M. T. Brandon (2002), Topographic controls on
erosion rates in tectonically active mountain ranges, Earth Planet. Sci.
Lett., 201(3–4), 481–489, doi:S0012821X02007252.
Moore, I. D., R. B. Grayson, and A. R. Ladson (1991), Digital terrain modeling:
A review of hydrological, geomorphological, and biological applications,
Hydrol. Processes, 5(1), 3–30, doi:10.1002/hyp.3360050103.
Mudd, S. M., and D. J. Furbish (2004), Influence of chemical denudation on
hillslope morphology, J. Geophys. Res., 109, F02001, doi:10.1029/
2003JF000087.
Mudd, S. M., and D. J. Furbish (2005), Lateral migration of hillcrests in
response to channel incision in soil-mantled landscapes, J. Geophys.
Res., 110, F04026, doi:10.1029/2005JF000313.
Mudd, S. M., and D. J. Furbish (2007), Responses of soil-mantled hillslopes
to transient channel incision rates, J. Geophys. Res., 112, F03S18,
doi:10.1029/2006JF000516.
National Operational Hydrologic Remote Sensing Center (2004), Snow
Data Assimilation System (SNODAS) data products at NSIDC, http://
nsidc.org/data/docs/noaa/g02158_snodas_snow_cover_model/index.
html, Natl. Snow and Ice Data Cent., Boulder, Colo., 3 March 2011.
Niemi, N. A., M. Oskin, D. W. Burbank, A. M. Heimsath, and E. J. Gabet
(2005), Effects of bedrock landslides on cosmogenically determined erosion
rates, Earth Planet. Sci. Lett., 237(3–4), 480–498, doi:10.1016/
j.epsl.2005.07.009.
Nishiizumi, K., M. Imamura, M. Caffee, J. Southon, R. Finkel, and J.
McAnich (2007), Absolute calibration of 10Be AMS standards, Nucl.
Instrum. Methods Phys. Res., Sect. B, 258, 403–413, doi:10.1016/
j.nimb.2007.01.297.
Norton, K. P., F. von Blanckenburg, F. Schlunegger, M. Schwab, and P. W.
Kubik (2008), Cosmogenic nuclide-based investigation of spatial erosion
and hillslope channel coupling in the transient foreland of the Swiss Alps,
Geomorphology, 95, 474–486, doi:10.1016/j.geomorph.2007.07.013.
Ouimet, W. B., K. X. Whipple, and D. E. Granger (2009), Beyond threshold
hillslopes: Channel adjustment to base-level fall in tectonically active
mountain ranges, Geology, 37(7), 579–582, doi:10.1130/G30013A.1.
Palumbo, L., R. Hetzel, M. Tao, and X. Li (2010), Topographic and
lithologic control on catchment-wide denudation rates derived from
cosmogenic 10Be in two mountain ranges at the margin of NE Tibet,
Geomorphology, 117(1–2), 130–142, doi:10.1016/j.geomorph.2009.
11.019.
Passalacqua, P., T. Do Trung, E. Foufoula-Georgiou, G. Sapiro, and W. E.
Dietrich (2010), A geometric framework for channel network extraction
from lidar: Nonlinear diffusion and geodesic paths, J. Geophys. Res.,
115, F01002, doi:10.1029/2009JF001254.
Pelletier, P. D., and M. L. Cline (2007), Nonlinear slope-dependent sediment
transport in cinder cone evolution, Geology, 35(12), 1067–1070,
doi:10.1130/G23992A.1.
Porder, S., P. M. Vitousek, O. A. Chadwick, C. P. Chamberlain, and G. E.
Hilley (2007), Uplift, erosion, and phosphorus limitation in terrestrial
ecosystems, Ecosystems, 10(1), 159–171, doi:10.1007/s10021-006-
9011-x.
Riebe, C. S., J. W. Kirchner, D. E. Granger, and R. C. Finkel (2000), Erosional
equilibrium and disequilibrium in the Sierra Nevada, inferred from
cosmogenic 26Al and 10Be in alluvial sediment, Geology, 28(9), 803–806,
doi:10.1130/0091-7613(2000)28<803:EEADIT>2.0.CO;2.
Riebe, C. S., J. W. Kirchner, D. E. Granger, and R. C. Finkel (2001a),
Strong tectonic and weak climatic control of long-term chemical weathering
rates, Geology, 29(6), 511–514, doi:10.1130/0091-7613(2001)029<0511:
STAWCC>2.0.CO;2.
Riebe, C. S., J. W. Kirchner,D. E.Granger, and R. C. Finkel (2001b),Minimal
climatic control on erosion rates in the Sierra Nevada, California, Geology,
29(5), 447–450, doi:10.1130/0091-7613(2001)029<0447:MCCOER>2.0.
CO;2.
Riggins, S. G., R. S. Anderson, S. P. Anderson, and A. M. Tye (2011),
Solving a conundrum of a steady-state hilltop with variable soil depths
and production rates, Bodmin Moor, UK, Geomorphology, 128(1–2),
73–84, doi:10.1016/j.geomorph.2010.12.023.
Roering, J. J. (2008), How well can hillslope evolution models
“explain” topography? Simulating soil transport and production with
high-resolution topographic data, Geol. Soc. Am. Bull., 120(9–10),
1248–1262, doi:10.1130/B26283.1.
Roering, J. J., J. W. Kirchner, and W. E. Dietrich (1999), Evidence for nonlinear,
diffusive sediment transport on hillslopes and implications for landscape
morphology, Water Resour. Res., 35(3), 853–870, doi:10.1029/
1998WR900090.
Roering, J. J., J. W. Kirchner, L. S. Sklar, and W. E. Dietrich (2001a),
Hillslope evolution by nonlinear creep and landsliding: An experimental
study, Geology, 29(2), 143–146, doi:10.1130/0091-7613(2001)029<
0143:HEBNCA>2.0.CO;2.
Roering, J. J., J. W. Kirchner, and W. E. Dietrich (2001b), Hillslope evolution
by nonlinear, slope-dependent transport: Steady state morphology
and equilibrium adjustment timescales, J. Geophys. Res., 106(B8),
16,499–16,513, doi:10.1029/2001JB000323.
Roering, J. J., J. T. Perron, and J. W. Kirchner (2007), Functional relationships
between denudation and hillslope form and relief, Earth Planet. Sci.
Lett., 264(1–2), 245–258, doi:10.1016/j.epsl.2007.09.035.
Roering, J. J., J. Marshall, A. M. Booth, M. Mort, and Q. S. Jin (2010), Evidence
for biotic controls on topography and soil production, Earth
Planet. Sci. Lett., 298(1–2), 183–190, doi:10.1016/j.epsl.2010.07.040.
Saleeby, J., and Z. Foster (2004), Topographic response to mantle lithosphere
removal in the southern Sierra Nevada region, Calif. Geol.,
32(3), 245–248, doi:10.1130/G19958.1.
Saleeby, J., Z. Saleeby, E. Nadin, and G. Maheo (2009), Step-over in the
structure controlling the regional west tilt of the Sierra Nevada microplate:
Eastern escarpment system to Kern Canyon system, Int. Geol.
Rev., 51(7–8), 634–669, doi:10.1080/00206810902867773.
Schmidt, J., I. S. Evans, and J. Brinkmann (2003), Comparison of polynomial
models for land surface curvature calculation, Int. J. Geogr. Inf.
Sci., 17(8), 797–814, doi:10.1080/13658810310001596058.
Schmidt, K. M., and D. R. Montgomery (1995), Limits to relief, Science,
270(5236), 617–620, doi:10.1126/science.270.5236.617.
Sklar, L., and W. E. Dietrich (1998), River longitudinal profiles and bedrock
incision models: Stream power and the influence of sediment supply,
in Rivers Over Rock: Fluvial Processes in Bedrock Channels,
Geophys. Monogr. Ser., vol. 107, edited by K. J. Tinkler and E. E. Wohl,
pp. 237–260, doi:10.1029/GM107p0237, AGU, Washington, D. C.
Small, E. E., and R. S. Anderson (1995), Geomorphically driven late Cenozoic
rock uplift in the Sierra Nevada, California, Science, 270(5234),
277–281, doi:10.1126/science.270.5234.277.
Small, E. E., R. S. Anderson, J. L. Repka, and R. Finkel (1997), Erosion
rates of alpine bedrock summit surfaces deduced from in situ 10Be and
26Al, Earth Planet. Sci. Lett., 150(3–4), 413–425, doi:10.1016/S0012-
821X(97)00092-7.
Snyder, N. P., K. X. Whipple, G. E. Tucker, and D. J. Merritts (2000),
Landscape response to tectonic forcing: Digital elevation model analysis
of stream profiles in the Mendocino triple junction region, northern California,
Geol. Soc. Am. Bull., 112(8), 1250–1263, doi:10.1130/0016-7606
(2000)112<1250:LRTTFD>2.0.CO;2.
Snyder, N. P., K. X. Whipple, G. E. Tucker, and D. J. Merritts (2003a),
Channel response to tectonic forcing: Field analysis of stream morphology
and hydrology in the Mendocino triple junction region, northern
California, Geomorphology, 53, 97–127, doi:10.1016/S0169-555X(02)
00349-5.
Snyder, N. P., K. X. Whipple, G. E. Tucker, and D. J. Merritts (2003b),
Importance of a stochastic distribution of floods and erosion thresholds
in the bedrock river incision problem, J. Geophys. Res., 108(B2), 2117,
doi:10.1029/2001JB001655.
Stock, G. M., R. S. Anderson, and R. C. Finkel (2004), Pace of landscape
evolution in the Sierra Nevada, California, revealed by cosmogenic dating
of cave sediments, Geology, 32(3), 193–196, doi:10.1130/G20197.1.
Stock, G. M., R. S. Anderson, and R. C. Finkel (2005), Rates of erosion and
topographic evolution of the Sierra Nevada, California, inferred from cosmogenic
26Al and 10Be concentrations, Earth Surf. Processes Landforms,
30(8), 985–1006, doi:10.1002/esp.1258.
Stock, J. D., and W. E. Dietrich (2006), Erosion of steepland valleys by
debris flows, Geol. Soc. Am. Bull., 118(9–10), 1125–1148, doi:10.1130/
B25902.1.
Stock, J. D., D. R. Montgomery, B. D. Collins, W. E. Dietrich, and L. Sklar
(2005), Field measurements of incision rates following bedrock exposure:
Implications for process controls on the long profiles of valleys cut by rivers
and debris flows, Geol. Soc. Am. Bull., 117(1–2), 174–194,
doi:10.1130/B25560.1.
Stone, J. O. (2000), Air pressure and cosmogenic isotope production,
J. Geophys. Res., 105(B10), 23,753–23,759, doi:10.1029/2000JB900181.
Strahler, A. N. (1950), Equilibrium theory of erosional slopes approached
by frequency distribution analysis, Part II, Am. J. Sci., 248, 800–814,
doi:10.2475/ajs.248.11.800.
Strahler, A. N. (1952), Hypsometric (area-altitude) analysis of erosional
topography, Geol. Soc. Am. Bull., 63(11), 1117–1142, doi:10.1130/
0016-7606(1952)63[1117:HAAOET]2.0.CO;2.
Tucker, G. E., and D. N. Bradley (2010), Trouble with diffusion: Reassessing
hillslope erosion laws with a particle-based model, J. Geophys. Res.,
115, F00A10, doi:10.1029/2009JF001264.
Tucker, G. E., and G. R. Hancock (2010), Modelling landscape evolution,
Earth Surf. Processes Landforms, 35, 28–50, doi:10.1002/esp.1952.
Tucker, G. E., S. W. McCoy, A. C. Whittaker, G. P. Roberts, S. T. Lancaster,
and R. Phillips (2011), Geomorphic significance of postglacial bedrock
scarps on normal-fault footwalls, J. Geophys. Res., 116, F01022,
doi:10.1029/2010JF001861.
Unruh, J. R. (1991), The uplift of the Sierra Nevada and implications for
late Cenozoic epeirogeny in the western Cordillera, Geol. Soc. Am.
Bull., 103(11), 1395–1404, doi:10.1130/0016-7606(1991)103<1395:
TUOTSN>2.3.CO;2.
Wakabayashi, J., and T. L. Sawyer (2001), Stream incision, tectonics,
uplift, and evolution of topography of the Sierra Nevada, California,
J. Geol., 109(5), 539–562, doi:10.1086/321962.
Warhaftig, C., and J. H. Birman (1965), The Quaternary of the Pacific
mountain system, in The Quaternary of the United States, edited by
H. E. J. Wright and D. G. Frey, pp. 299–340, Princeton Univ. Press,
Princeton, N. J.
Whipple, K. X. (2001), Fluvial landscape response time: How plausible is
steady-state denudation?, Am. J. Sci., 301(4–5), 313–325, doi:10.2475/
ajs.301.4-5.313.
Whipple, K. X., and G. E. Tucker (1999), Dynamics of the stream-power
river incision model: Implications for height limits of mountain ranges,
landscape response timescales, and research needs, J. Geophys. Res.,
104(8), 17,661–17,674, doi:10.1029/1999JB900120.
Whittaker, A. C., P. A. Cowie, M. Attal, G. E. Tucker, and G. P. Roberts
(2007a), Bedrock channel adjustment to tectonic forcing: Implications for
predicting river incision rates, Geology, 35(2), 103–106, doi:10.1130/
G23106A.1.
Whittaker, A. C., P. A. Cowie, M. Attal, G. E. Tucker, and G. P. Roberts
(2007b), Contrasting transient and steady-state rivers crossing active normal
faults: New field observations from the Central Apennines, Italy,
Basin Res., 19, 529–556, doi:10.1111/j.1365-2117.2007.00337.x.
Wilkinson, M. T., J. Chappell, G. S. Humphreys, K. Fifield, B. Smith, and
P. Hesse (2005), Soil production in heath and forest, Blue Mountains,
Australia: Influence of lithology and palaeoclimate, Earth Surf. Processes
Landforms, 30(13), 1683–1685, doi:10.1002/esp.1311.
Wobus, C., K. X. Whipple, E. Kirby, N. Snyder, J. Johnson, K. Spyropolou,
B. Crosby, and D. Sheehan (2006a), Tectonics from topography: Procedures,
promise, and pitfalls, Spec. Pap. Geol. Soc. Am., 398, 55–74,
doi:10.1130/2006.2398(04).
Wobus, C. W., B. T. Crosby, and K. X. Whipple (2006b), Hanging valleys
in fluvial systems: Controls on occurrence and implications for landscape
evolution, J. Geophys. Res., 111, F02017, doi:10.1029/2005JF000406.
Yoo, K., and S. M. Mudd (2008a), Discrepancy between mineral residence
time and soil age: Implications for the interpretation of chemical weathering
rates, Geology, 36(1), 35–38, doi:10.1130/G24285A.1.
Yoo, K., and S. M. Mudd (2008b), Toward process-based modeling of geochemical
soil formation across diverse landforms: A new mathematical
framework, Geoderma, 146(1–2), 248–260, doi:10.1016/j.geoderma.
2008.05.029.
Yoo, K., B. Weinman, S. M.Mudd,M. Hurst, M. Attal, and K. Maher (2011),
Evolution of hillslope soils: The geomorphic theater and the geochemical
play, Appl. Geochem., 26, S149–S153, doi:10.1016/j.apgeochem.2011.
03.054.
Zevenbergen, L. W., and C. R. Thorne (1987), Quantitative analysis of land
surface topography, Earth Surf. Processes Landforms, 12(1), 47–56,
doi:10.1002/esp.3290120107.