BIROn - Birkbeck Institutional Research Online

    One million years of climate-driven rock uplift rate variation on the Wasatch Fault revealed by fluvial topography

    Smith, Adam G.G. and Fox, M. and Moore, J.R. and Miller, S.R. and Goren, L. and Morriss, M. and Carter, Andrew (2024) One million years of climate-driven rock uplift rate variation on the Wasatch Fault revealed by fluvial topography. American Journal of Science 324 (1), ISSN 0002-9599.

    [img]
    Preview
    Text
    Wasatch.pdf - Published Version of Record
    Available under License Creative Commons Attribution.

    Download (3MB) | Preview

    Abstract

    Displacement along the Wasatch Fault, Utah, has created the Wasatch Range. Owing to its topographic prominence, location on the eastern boundary of the Basin and Range, presently active fault slip, and proximity to Utah’s largest cities, the range and fault have garnered much attention. On the 102–103 year timescale, the behavior, displacement and seismic history of the Wasatch Fault has been well categorized in order to assess seismic hazard. On the 107 year timescale, the rock uplift rate history of the Wasatch range has also been resolved using thermochronometric data, owing to its importance in inferring the history of extension in the western US. However, little data exists that bridges the gap between these two timescales. Here, we infer an approximately 1 Ma rock uplift rate history from analysis of three river networks located in the center of the range. Our recovered rock uplift rate histories evidence periodic changes to rock uplift on the Wasatch Fault, that coincide with climate driven filling and unfilling of lakes in the Bonnneville Basin. To ensure our rock uplift rate histories are robust, we use field data and previously published cosmogenic 10Be erosion rate data to tightly constrain the erodibility parameter, and investigate an appropriate value for the slope exponent of the stream power model, n. We use our river network inversion to reconcile estimates of erodibility from a number of methodologies and show that the contrast between bedrock and bedload strength is an important factor that determines erodibility.

    Metadata

    Item Type: Article
    School: Birkbeck Faculties and Schools > Faculty of Science > School of Natural Sciences
    Depositing User: Adam Smith
    Date Deposited: 31 Jan 2024 14:47
    Last Modified: 31 Jan 2024 15:33
    URI: https://eprints.bbk.ac.uk/id/eprint/52911

    Statistics

    Activity Overview
    6 month trend
    136Downloads
    6 month trend
    290Hits

    Additional statistics are available via IRStats2.

    Archive Staff Only (login required)

    Edit/View Item
    Edit/View Item