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Alluvial fan depositional records from north and south-facing catchments in semi-arid montane terrain

Published online by Cambridge University Press:  13 December 2017

Michael J. Poulos  and
Jennifer L. Pierce
Michael J. Poulos*
Affiliation:
Department of Geosciences, Boise State University, 1910 University Drive, Boise, Idaho 83725, USA
Jennifer L. Pierce
Affiliation:
Department of Geosciences, Boise State University, 1910 University Drive, Boise, Idaho 83725, USA
*
*Corresponding author at: Department of Geosciences, Boise State University, 1910 University Drive, Boise, Idaho 83725, USA. E-mail address: [email protected]; [email protected] (M. Poulos).
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Abstract

Valley asymmetry reflects differences in landform evolution with aspect; however, few studies assess rates and timing of asymmetric erosion. In south-central Idaho, we combine alluvial fan volume reconstructions with radiocarbon deposit dating to compare the source-catchment normalized fan deposition rates of catchments incised into north (n=5) and south-facing (n=3) valleys, which differ during the late Holocene from 7.7 to 10.1 mm/ka, respectively, but are not significantly different. South-facing catchments produced 1.3× more fan sediment per unit source-area during the late Holocene, whereas over the last 10 Ma they have evolved to be 2.1× larger with 2.8× greater eroded volumes and 7.6° gentler slopes (24.5° versus 32.1°, average). Late Holocene differences in sediment yields with aspect cannot fully explain differences in landforms. Potential bias in sediment deposition and/or remobilization cannot fully explain the similarity of erosion rates during the late Holocene. Valley asymmetry appears to have developed primarily during different conditions. While valley asymmetry development may be quicker during glacial climates, development is likely accelerated early in a valley’s history, such as during initial valley incision, because asymmetric degradation serves as a negative feedback that reduces aspect-related differences in erosion and drives valleys towards steady state.

Keywords

AlluvialFanRadiocarbonLidarHoloceneAspectValleyAsymmetryClimateIdaho BatholithSemi-aridMontane
Type
Research Article
Information
Quaternary Research , Volume 89 , Issue 1: Tribute to Daniel Livingstone and Paul Colinvaux , January 2018 , pp. 237 - 253
Copyright
Copyright © University of Washington. Published by Cambridge University Press, 2017 

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References

Abrahams, A.D., 1968. Distinguishing between the concepts of steady state and dynamic equilibrium in geomorphology. Earth Science Journal 2, 160–166.Google Scholar
Aishlin, P., McNamara, J.P., 2011. Bedrock infiltration and mountain block recharge accounting using chloride mass balance. Hydrological Processes 25, 1934–1948.CrossRefGoogle Scholar
Anderson, B.T., McNamara, J.P., Marshall, H.P., Flores, A.N., 2014. Insights into the physical processes controlling correlations between snow distribution and terrain properties. Water Resources Research 50, 4545–4563.Google Scholar
Anderson, R.S., Anderson, S.P., Tucker, G.E., 2013. Rock damage and regolith transport by frost: An example of climate modulation of the geomorphology of the critical zone. Earth Surface Processes and Landforms 38, 299–316.Google Scholar
Armstrong, R.L., Taubeneck, W.H., Hales, P.O., 1977. Rb-Sr and K-Ar geochronometry of Mesozoic granitic rocks and their Sr isotopic composition, Oregon, Washington, and Idaho. Geological Society of America Bulletin 88, 397–411.Google Scholar
Baker, W.L., 2006. Fire and restoration of sagebrush ecosystems. Wildlife Society Bulletin 34, 177–185.Google Scholar
Blair, T.C., McPherson, J.G., 1994. Alluvial fans and their natural distinction from rivers based on morphology, hydraulic processes, sedimentary processes, and facies assemblages. Journal of Sedimentary Research 64. http://dx.doi.org/10.1306/D4267DDE-2B26-11D7-8648000102C1865D.Google Scholar
Brantley, S.L., Goldhaber, M.B., Ragnarsdottir, K.V., 2007. Crossing disciplines and scales to understand the critical zone. Elements 3, 307–314.Google Scholar
Bull, W.B., 1977. The alluvial-fan environment. Progress in Physical Geography 1, 222–270.Google Scholar
Bull, W.B., 1991. Geomorphic Responses to Climate Change. Oxford University Press, New York.Google Scholar
Burnett, B.N., Meyer, G.A., McFadden, L.D., 2008. Aspect‐related microclimatic influences on slope forms and processes, northeastern Arizona. Journal of Geophysical Research: Earth Surface 2003–2012, 113. http://dx.doi.org/10.1029/2007JF000789.Google Scholar
Cannon, S.H., 2001. Debris-flow generation from recently burned watersheds. Environmental and Engineering Geoscience 7, 321–341.CrossRefGoogle Scholar
Cannon, S.H., Gartner, J.E., Wilson, R.C., Bowers, J.C., Laber, J.L., 2008. Storm rainfall conditions for floods and debris flows from recently burned areas in southwestern Colorado and southern California. Geomorphology 96, 250–269.Google Scholar
Clayton, J.L., Megahan, W.F., 1986. Erosional and chemical denudation rates in the southwestern Idaho batholith. Earth Surface Processes and Landforms 11, 389–400.Google Scholar
Clayton, J.L., Megahan, W.F., Hampton, D., 1979. Soil and bedrock properties: weathering and alteration products and processes in the Idaho Batholith. USDA Forest Service Research Paper INT- 237. Intermountain Forest and Range Experiment Station, United States Department of Agriculture, Ogden, Utah.Google Scholar
Clemens, D.M., 1993. Tectonics and Silicic Volcanic Stratigraphy of the Western Snake River Plain, Southwestern Idaho. Master’s thesis, Arizona State University, Tempe.Google Scholar
Cook, E.R., Woodhouse, C.A., Eakin, C.M., Meko, D.M., Stahle, D.W., 2004. Long-term aridity changes in the western United States. Science 306, 1015–1018.Google Scholar
Criss, R.E., Lanphere, M.A., Taylor, H.P., 1982. Effects of regional uplift, deformation, and meteoric‐hydrothermal metamorphism on K‐Ar Ages of biotites in the southern half of the Idaho batholith. Journal of Geophysical Research: Solid Earth 87, 7029–7046.Google Scholar
Denny, C.S., 1967. Fans and pediments. American Journal of Science 265, 81–105.Google Scholar
Dohrenwend, J.C., 1978. Systematic valley asymmetry in the central California Coast Ranges. Geological Society of America Bulletin 89, 891–900.2.0.CO;2>CrossRefGoogle Scholar
Field, J., 2001. Channel avulsion on alluvial fans in southern Arizona. Geomorphology 37, 93–104.CrossRefGoogle Scholar
Fitch, E.P., Meyer, G.A., 2016. Temporal and spatial climatic controls on Holocene fire-related erosion and sedimentation, Jemez Mountains, New Mexico. Quaternary Research 85, 75–86.Google Scholar
Foster, M.A., Anderson, R.S., Wyshnytzky, C.E., Ouimet, W.B., Dethier, D.P., 2015. Hillslope lowering rates and mobile-regolith residence times from in situ and meteoric 10Be analysis, Boulder Creek Critical Zone Observatory, Colorado. Geological Society of America Bulletin 127, 862–878.Google Scholar
Garrote, J., Cox, R.T., Swann, C., Ellis, M., 2006. Tectonic geomorphology of the southeastern Mississippi Embayment in northern Mississippi, USA. Geological Society of America Bulletin 118, 1160–1170.Google Scholar
Gavin, D.G., 2001. Estimation of inbuilt age in radiocarbon ages of soil charcoal for fire history studies. Radiocarbon 43, 27–44.Google Scholar
Geroy, I.J., Gribb, M.M., Marshall, H.P., Chandler, D.G., Benner, S.G., McNamara, J.P., 2011. Aspect influences on soil water retention and storage. Hydrological Processes 25, 3836–3842.Google Scholar
Gilbert, G.K., 1904. Systematic asymmetry of crest lines in the High Sierra of California. The Journal of Geology 12, 579–588.Google Scholar
Gutiérrez‐Jurado, H.A., Vivoni, E.R., Istanbulluoglu, E., Bras, R.L., 2007. Ecohydrological response to a geomorphically significant flood event in a semiarid catchment with contrasting ecosystems. Geophysical Research Letters 34. http://dx.doi.org/ 10.1029/2007GL030994.Google Scholar
Hack, J.T., Goodlett, J.C., 1960. Geomorphology and forest ecology of a mountain region in the central Appalachians. Geological Survey Professional Paper 347. United States Government Printing Office, Washington, DC.Google Scholar
Heyerdahl, E.K., Morgan, P., Riser, J.P., 2008. Multi-season climate synchronized historical fires in dry forests (1650–1900), northern Rockies, USA. Ecology 89, 705–716.CrossRefGoogle Scholar
Istanbulluoglu, E., Yetemen, O., Vivoni, E.R., Gutiérrez‐Jurado, H.A., Bras, R.L., 2008. Eco‐geomorphic implications of hillslope aspect: Inferences from analysis of landscape morphology in central New Mexico. Geophysical Research Letters 35. http://dx.doi.org/ 10.1029/2008GL034477.Google Scholar
Kirchner, J.W., Finkel, R.C., Riebe, C.S., Granger, D.E., Clayton, J.L., King, J.G., Megahan, W.F., 2001. Mountain erosion over 10 yr, 10 ky, and 10 my time scales. Geology 29, 591–594.Google Scholar
Kormos, P.R., McNamara, J.P., Seyfried, M.S., Marshall, H.P., Marks, D., Flores, A.N., 2015. Bedrock infiltration estimates from a catchment water storage-based modeling approach in the rain snow transition zone. Journal of Hydrology 525, 231–248.Google Scholar
Kunkel, M.L., Flores, A.N., Smith, T.J., McNamara, J.P., Benner, S.G., 2011. A simplified approach for estimating soil carbon and nitrogen stocks in semi-arid complex terrain. Geoderma 165, 1–11.Google Scholar
Loughridge, R., 2014. Identifying Topographic Controls of Terrestrial Vegetation Using Remote Sensing Data in a Semiarid Mountain Watershed, Idaho, USA. Master’s thesis, Boise State University, Boise, Idaho.Google Scholar
Luckman, B.H., 2000. The little ice age in the Canadian Rockies. Geomorphology 32, 357–384.CrossRefGoogle Scholar
Matmon, A., Bierman, P.R., Larsen, J., Southworth, S., Pavich, M., Caffee, M., 2003. Temporally and spatially uniform rates of erosion in the southern Appalachian Great Smoky Mountains. Geology 31, 155–158.Google Scholar
McGuire, L.A., Pelletier, J.D., Roering, J.J., 2014. Development of topographic asymmetry: Insights from dated cinder cones in the western United States. Journal of Geophysical Research: Earth Surface 119, 1725–1750.Google Scholar
McNamara, J.P., Chandler, D., Seyfried, M., Achet, S., 2005. Soil moisture states, lateral flow, and streamflow generation in a semi‐arid, snowmelt‐driven catchment. Hydrological Processes 19, 4023–4038.Google Scholar
Melton, M.A., 1960. Intravalley variation in slope angles related to microclimate and erosional environment. Geological Society of America Bulletin 71, 133–144.Google Scholar
Meyer, G.A., Pierce, J.L., 2003. Climatic controls on fire-induced sediment pulses in Yellowstone National Park and central Idaho: a long-term perspective. Forest Ecology and Management 178, 89–104.Google Scholar
Meyer, G.A., Pierce, J.L., Wood, S.H., Jull, A.J.T., 2001. Fire, storms, and erosional events in the Idaho batholith. Hydrological Processes 15, 3025–3038.CrossRefGoogle Scholar
Meyer, G.A., Wells, S.G., Jull, A.T., 1995. Fire and alluvial chronology in Yellowstone National Park: climatic and intrinsic controls on Holocene geomorphic processes. Geological Society of America Bulletin 107, 1211–1230.Google Scholar
Meyer, G.A., Wells, S.G., 1997. Fire-related sedimentation events on alluvial fans, Yellowstone National Park, USA. Journal of Sedimentary Research 67(5.Google Scholar
Miller, R.F., Tausch, R.J., 2001. The role of fire in juniper and pinyon woodlands: A descriptive analysis. In: Galley, K.E.M., Wilson, T.P., (Eds.), Proceedings of the Invasive Species Workshop: The Role of Fire in the Control and Spread of Invasive Species. Fire Conference 2000: the First National Congress on Fire Ecology, Prevention, and Management. Miscellaneous Publication No. 11. Tall Timbers Research Station, Tallahassee, Florida, pp. 15–30.Google Scholar
Nelson, N.A., Pierce, J., 2010. Late-Holocene relationships among fire, climate and vegetation in a forest-sagebrush ecotone of southwestern Idaho, USA. The Holocene 20, 1179–1194.Google Scholar
Orem, C.A., Pelletier, J.D., 2016. The predominance of post‐wildfire erosion in the long‐term denudation of the Valles Caldera, New Mexico. Journal of Geophysical Research: Earth Surface 121, 843–864.Google Scholar
Othberg, K.L., 1994. Geology and geomorphology of the Boise Valley and adjoining areas, western Snake River Plain, Idaho. Idaho Geological Survey Bulletin 29, 54.Google Scholar
Parker, G., Paola, C., Whipple, K.X., Mohrig, D., 1998. Alluvial fans formed by channelized fluvial and sheet flow. I: Theory. Journal of Hydraulic Engineering 124, 985–995.Google Scholar
Pierce, J.L., Meyer, G.A., Jull, A.T., 2004. Fire-induced erosion and millennial-scale climate change in northern ponderosa pine forests. Nature 432, 87–90.Google Scholar
Pierce, K.L., Scott, W.E., 1982. Pleistocene episodes of alluvial-gravel deposition, southeastern Idaho. In: Bonnichsen, B., Breckenridge, R.M. (Eds.), Cenozoic Geology of Idaho. Idaho Bureau of Mines and Geology Bulletin 26, 685–702.Google Scholar
Poulos, M.J., 2016. Feedbacks Among Climate, Soils, Vegetation, and Erosion Drive Valley Asymmetry Development in the Mountains of Central Idaho. PhD dissertation, Boise State University, Boise, Idaho.Google Scholar
Poulos, M.J., Pierce, J.L., Flores, A.N., Benner, S.G., 2012. Hillslope asymmetry maps reveal widespread, multi‐scale organization. Geophysical Research Letters 39. http://dx.doi.org/ 10.1029/2012GL051283.Google Scholar
Powell, J.W., 1874. Remarks on the structural geology of the valley of the Colorado of the West. Washington Philosophical Society Bulletin 1, 48–51.Google Scholar
Ramsey, C.B., 2009. Bayesian analysis of radiocarbon dates. Radiocarbon 51, 337–360.Google Scholar
Riley, K.E., 2012. A 14,000-year Record of Wildfire and Alluvial Fan Deposition Reveals Relationships Among Fire, Climate, Vegetation, and Sediment Yields in the Middle Fork Salmon River, Idaho. Master’s thesis, Boise State University, Boise, Idaho.Google Scholar
Riley, K., Pierce, J., Meyer, G.A., 2015. Vegetative and climatic controls on Holocene wildfire and erosion recorded in alluvial fans of the Middle Fork Salmon River, Idaho. The Holocene 25. http://dx.doi.org/.10.1177/0959683615571423.Google Scholar
Ritter, J.B., Miller, J.R., Enzel, Y., Howes, S.D., Nadon, G., Grubb, M.D., Hoover, K.A., Olsen, T., Reneau, S.L., Sack, D., Summa, C.L., 1993. Quaternary evolution of Cedar Creek alluvial fan, Montana. Geomorphology 8, 287–304.Google Scholar
Smith, T.J., 2010. Using Soil Moisture Trends Across Topographic Gradients to Examine Controls on Semi-arid Ecosystem Dynamics. Master’s thesis, Boise State University, Boise, Idaho.Google Scholar
Smith, T.J., McNamara, J.P., Flores, A.N., Gribb, M.M., Aishlin, P.S., Benner, S.G., 2011. Small soil storage capacity limits benefit of winter snowpack to upland vegetation. Hydrological Processes 25, 3858–3865.Google Scholar
Stark, B.J., 2012. Assessing Eolian Dust Inputs to Soils in Dry Creek Experimental Watershed, SW Idaho. Master’s thesis, Boise State University, Boise, Idaho.Google Scholar
Stuiver, M., Reimer, P.J., 1993. Extended 14C database and revised CALIB radiocarbon calibration program. Radiocarbon 35, 215–230.Google Scholar
Straccia, F.G., Wilkinson, B.H., Smith, G.R., 1990. Miocene lacustrine algal reefs—southwestern Snake River Plain, Idaho. Sedimentary Geology 67, 7–23.Google Scholar
Sweetkind, D.S., Blackwell, D.D., 1989. Fission-track evidence of the Cenozoic thermal history of the Idaho batholith. Tectonophysics 157, 241–250.Google Scholar
Swirydczuk, K., Wilkinson, B.H., Smith, G.R., 1979. The Pliocene Glenns Ferry oolite: Lake-margin carbonate deposition in the southwestern Snake River plain. Journal of Sedimentary Research 49. http://dx.doi.org/ 10.1306/212F789C-2B24-11D7-8648000102C1865D.Google Scholar
Telford, R.J., Heegaard, E., Birks, H.J., 2004. The intercept is a poor estimate of a calibrated radiocarbon age. The Holocene 14, 296–298.Google Scholar
Tesfa, T.K., Tarboton, D.G., Chandler, D.G., McNamara, J.P., 2009. Modeling soil depth from topographic and land cover attributes. Water Resources Research 45. http://dx.doi.org/ 10.1029/2008WR007474.Google Scholar
Thomas, C.A., 1963. Cloudburst Floods at Boise, Idaho, August 20, September 22, 26, 1959. United States Geological Survey Open-file report. United States Geological Survey, Boise, Idaho.Google Scholar
Tuck, R., 1935. Asymmetrical topography in high latitudes resulting from alpine glacial erosion. The Journal of Geology 43, 530–538.CrossRefGoogle Scholar
Welcker, C., 2011. Bulking Debris Flow Initiation and Impacts. PhD dissertation, University of Idaho, Moscow.Google Scholar
Wende, R., 1995. Drainage and valley asymmetry in the Tertiary Hills of Lower Bavaria, Germany. Geomorphology 14, 255–265.Google Scholar
Weppner, K.N., Pierce, J.L., Betancourt, J.L., 2013. Holocene fire occurrence and alluvial responses at the leading edge of pinyon–juniper migration in the Northern Great Basin, USA. Quaternary Research 80, 143–157.Google Scholar
West, N., Kirby, E., Bierman, P., Clarke, B.A., 2014. Aspect-dependent variations in regolith creep revealed by meteoric 10Be. Geology 42, 507–510.Google Scholar
Wood, S.H., Burnham, W., Osterman, D., 1982. Field Trip Guide to the Boise Foothills, Idaho. Idaho Geological Survey, Moscow, Idaho.Google Scholar
Wood, S.H., Clemens, D.M., 2002. Geologic and tectonic history of the western Snake River Plain, Idaho and Oregon. Tectonic and Magmatic Evolution of the Snake River Plain Volcanic Province. Idaho Geological Survey Bulletin 30, 69–103.Google Scholar
Yetemen, O., Istanbulluoglu, E., Flores‐Cervantes, J.H., Vivoni, E.R., Bras, R.L., 2015. Ecohydrologic role of solar radiation on landscape evolution. Water Resources Research 51, 1127–1157.Google Scholar
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