T340 Heterogeneity in Landscape Evolution: Geomorphic Response to Spatially and Temporally Variable Forcings

Wednesday, 25 October 2017
1:30 PM - 5:30 PM
Chelan 2

TERRACES, KNICKPOINTS, AND SPATIALLY VARIABLE EROSION: INTERPRETING THE SIGNALS OF TRANSIENT TOPOGRAPHY

Paper number: T340-13
Program: Technical Sessions
Time: 4:40 PM – 4:55 PM

Authors

Abstract

Landscape heterogeneity impacts the fidelity of transient erosion signals. The South Fork Eel River (SFER) in the northern California Coast Ranges, USA exhibits characteristics suggestive of transient landscape adjustment: strath terraces, knickpoints, and headwater terrain eroding more slowly than downstream areas. A tectonically-induced uplift wave is commonly invoked as the driver of transience in this region. The wave is attributed to the northward migration of the Mendocino Triple Junction (MTJ). Nested basin-mean erosion rates calculated from 10Be detrital quartz sand increase down the mainstem of the SFER, roughly coinciding with the direction of MTJ migration. This erosion trend is attributed to the proportion of adjusted and unadjusted landscape portions upstream of the locations where the nested 10Be samples were collected. Adjusted and unadjusted landscape portions are separated by a broad knickzone that contains 28% of relief along the mainstem. Knickzone propagation and considerable stream incision is suggested by projection of the upper SFER above the knickzone through the highest flight of strath terraces.

Field observations and outcomes of numerical simulations using the Landlab modeling framework are incompatible with uplift modeled as a wave. Alternative uplift and variable sediment flux scenarios more reliably predict the pattern of terraces, knickpoints, and accelerated erosion. In the natural landscape, landforms and erosion rates follow the patterns expected for transient erosion along the mainstem, although a local base level lowering signal is not resolvable in many tributaries. Here we propose a framework in which rock properties are a key control upon preservation of a base level change in low order streams. This implies that transient erosion signals inferred using topography can be transformed or destroyed in certain lithologies, complicating efforts to infer climatic and tectonic history from topography.

Geological Society of America Abstracts with Programs. Vol. 49, No. 6

doi: 10.1130/abs/2017AM-306504

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