Interpreting erosion frequency and magnitude from luminescence profiles in boulders
<p>Exposed bedrock is ubiquitous on terrestrial and planetary landscapes, yet little is known<br>about the rate of bedrock erosion at a granular scale on timescales longer than the<br>instrumental record. As recently suggested, using the bleaching depth of luminescence<br>signals as a measure of bedrock erosion may fit these scales. Yet this approach assumes<br>constant erosion through time, a condition likely violated by the stochastic nature of erosional<br>events. Here we simulate bleaching in response to power-law distributions of removal<br>lengths and hiatus durations. We compare simulation results with previously measured<br>luminescence profiles from boulder surfaces to illustrate that prolonged hiatuses are unlikely<br>and that typical erosion scales are sub-granular with occasional loss at mm scales,<br>consistent with ideas about microflaws governing bedrock detachment. For a wide range of<br>erosion rates, measurements are integrated over many removal events, producing<br>reasonably accurate estimates despite the stochastic nature of the simulated process. We<br>hypothesize that the greater or equal erosion rates atop large boulders compared to rates at<br>ground level suggest that subcritical cracking may be more influential than aeolian abrasion<br>for boulder degradation in the Eastern Pamirs, China.</p>