A mechanistic model and experiments on bedrock incision and channelization by rockfall

Beer, Alexander R.; Fischer, Jade N.; Ulizio, T. P.; Ma, Zewei; Sun, Zhongguang; Lamb, Michael P.

doi:10.22541/essoar.167898500.01983170/v1

Cited by 1 publication

(1 citation statement)

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“…The experimental data and the dry gravel abrasion model DGAM code (in R language) is publicly available at https://fdat.uni-tuebingen.de/records/98546-hfv72 (Beer et al, 2024). We are thankful to Joel Scheingross for help with PU foam selection, Roman DiBiase for providing his model code, and Kim Miller for measuring grain friction angles.…”

Section: Data Availability Statementmentioning

confidence: 99%

A Mechanistic Model and Experiments on Bedrock Incision and Channelization by Rockfall

Beer,

Fischer,

Ulizio

et al. 2024

JGR Earth Surface

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Rockfall and rock avalanches are common in steep terrain on Earth and potentially on other planetary bodies such as the Moon and Mars. Since impacting rocks can damage exposed bedrock as they roll and bounce downhill, rockfall might be an important erosive agent in steep landscapes, even in the absence of water. We developed a new theory for rockfall‐driven bedrock abrasion using the ballistic trajectories of rocks transported under gravity. We calibrated this theory using laboratory experiments of rockfall over an inclined bedrock simulant. Both the experiments and the model demonstrate that bedrock hillslopes can be abraded by dry rockfall, even at gradients below the angle of repose, depending on the bedrock roughness. Feedback between abrasion and topographic steering of rockfall can produce channel‐like forms, such as bedrock chutes, in the absence of water. Particle size has a dominant influence on abrasion rates and runout distances, while the hillslope angle has a comparatively minor influence. Rockfall transport is sensitive to bedrock roughness; terrain with high friction angles can trap rocks creating patches of rock cover that affect subsequent rockfall pathways. Our results suggest that dry rockfall can play an important role in eroding and channelizing steep, rocky terrain on Earth and other planets, such as crater degradation on the Moon and Mars.

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Section: Data Availability Statementmentioning

confidence: 99%

A Mechanistic Model and Experiments on Bedrock Incision and Channelization by Rockfall

Beer,

Fischer,

Ulizio

et al. 2024

JGR Earth Surface

View full text Add to dashboard Cite

show abstract

A mechanistic model and experiments on bedrock incision and channelization by rockfall

Abstract: Rockfall can erode rocky hillslopes even below the angle of repose • Grainsize has a dominant effect on impact abrasion; slope is of minor importance • Topographic steering of grains results in self-formed bedrock channels

Cited by 1 publication

References 73 publications

A Mechanistic Model and Experiments on Bedrock Incision and Channelization by Rockfall

A Mechanistic Model and Experiments on Bedrock Incision and Channelization by Rockfall

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