Local topography and erosion rate control regolith thickness along a ridgeline in the Sierra Nevada, California

Emmanuel J. Gabet, Simon M. Mudd, David T. Milodowski, Kyungsoo Yoo, Martin D. Hurst, Anthony Dosseto

Research output: Contribution to journalArticle

9 Citations (Scopus)

Abstract

The ridgelines of mountain ranges are a source of geomorphic information unadulterated by the arrival of sediment from upslope. Studies along ridgecrests, therefore, can help identify and isolate the controls on important regolith properties such as thickness and texture. A 1.5km section of ridgeline in the Sierra Nevada (CA) with a tenfold decrease in erosion rate (inferred from ridgetop convexity) provided an opportunity to conduct a high-resolution survey of regolith properties and investigate their controls. We found that regolith along the most quickly eroding section of the ridge was the rockiest and had the lowest clay concentrations. Furthermore, a general increase in regolith thickness with a slowing of erosion rate was accompanied by an increase in biomass, changes in vegetation community, broader ridgeline profiles, and an apparent increase in total available moisture. The greatest source of variation in regolith thickness at the 10-100m scale, however, was the local topography along the ridgeline, with the deepest regolith in the saddles and the thinnest on the knobs. Because regolith in the saddles had higher surface soil moisture than the knobs, we conclude that the hydrological conditions primarily driven by local topography (i.e. rapid vs. slow drainage and water-storage potential) provide the fundamental controls on regolith thickness through feedbacks incorporating physical weathering by the biota and chemical weathering. Moreover, because the ridgeline saddles are the uppermost extensions of first-order valleys, we propose that the fluvial network affects regolith properties in the furthest reaches of the watershed.

Original languageEnglish (US)
Pages (from-to)1779-1790
Number of pages12
JournalEarth Surface Processes and Landforms
Volume40
Issue number13
DOIs
StatePublished - Oct 2015

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regolith
erosion rate
erosion
topography
geography
source of information
water
community
chemical weathering
water storage
biota
weathering
soil moisture
texture
moisture
watershed
drainage
valley
clay
vegetation

Keywords

  • Regolith production
  • Regolith thickness
  • Sierra Nevada
  • Weathering

Cite this

Local topography and erosion rate control regolith thickness along a ridgeline in the Sierra Nevada, California. / Gabet, Emmanuel J.; Mudd, Simon M.; Milodowski, David T.; Yoo, Kyungsoo; Hurst, Martin D.; Dosseto, Anthony.

In: Earth Surface Processes and Landforms, Vol. 40, No. 13, 10.2015, p. 1779-1790.

Research output: Contribution to journalArticle

Gabet, Emmanuel J. ; Mudd, Simon M. ; Milodowski, David T. ; Yoo, Kyungsoo ; Hurst, Martin D. ; Dosseto, Anthony. / Local topography and erosion rate control regolith thickness along a ridgeline in the Sierra Nevada, California. In: Earth Surface Processes and Landforms. 2015 ; Vol. 40, No. 13. pp. 1779-1790.
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