Tectonic controls of Holocene erosion in a glaciated orogen
<p>Recent work has highlighted a strong, worldwide, alpine glacial impact on orogen erosion rates over the last 2 Ma. While it may be assumed that glaciers increased erosion rates when active, the degree to which past glaciations influence Holocene erosion rates through the adjus...
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doaj-6a14917464104f6b8fcbff9d54683d962020-11-24T21:40:09ZengCopernicus PublicationsEarth Surface Dynamics2196-63112196-632X2018-07-01659561010.5194/esurf-6-595-2018Tectonic controls of Holocene erosion in a glaciated orogenB. A. Adams0B. A. Adams1T. A. Ehlers2Department of Geosciences, Universität Tübingen, 72074, Germanynow at: the School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, UKDepartment of Geosciences, Universität Tübingen, 72074, Germany<p>Recent work has highlighted a strong, worldwide, alpine glacial impact on orogen erosion rates over the last 2 Ma. While it may be assumed that glaciers increased erosion rates when active, the degree to which past glaciations influence Holocene erosion rates through the adjustment of topography is not known. In this study, we investigate the influence of long-term tectonic and post-glacial topographic controls on erosion in a glaciated orogen: the Olympic Mountains, USA. We present 14 new <sup>10</sup>Be and <sup>26</sup>Al analyses which constrain Holocene erosion rates across the Olympic Mountains. Basin-averaged erosion rates scale with basin-averaged values of 5 km local relief, channel steepness, and hillslope angle throughout the range, similar to observations from non-glaciated orogens. These erosion rates are not related to mean annual precipitation or the marked change in Pleistocene alpine glacier size across the range, implying that glacier modification of topography and modern precipitation parameters do not exert strong controls on these rates. Rather, we find that despite spatial variations in glacial modification of topography, patterns of recent erosion are similar to those from estimates of long-term tectonic rock uplift. This is consistent with a tectonic model where erosion and rock uplift patterns are controlled by the deformation of the Cascadia subduction zone.</p>https://www.earth-surf-dynam.net/6/595/2018/esurf-6-595-2018.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
B. A. Adams B. A. Adams T. A. Ehlers |
spellingShingle |
B. A. Adams B. A. Adams T. A. Ehlers Tectonic controls of Holocene erosion in a glaciated orogen Earth Surface Dynamics |
author_facet |
B. A. Adams B. A. Adams T. A. Ehlers |
author_sort |
B. A. Adams |
title |
Tectonic controls of Holocene erosion in a glaciated orogen |
title_short |
Tectonic controls of Holocene erosion in a glaciated orogen |
title_full |
Tectonic controls of Holocene erosion in a glaciated orogen |
title_fullStr |
Tectonic controls of Holocene erosion in a glaciated orogen |
title_full_unstemmed |
Tectonic controls of Holocene erosion in a glaciated orogen |
title_sort |
tectonic controls of holocene erosion in a glaciated orogen |
publisher |
Copernicus Publications |
series |
Earth Surface Dynamics |
issn |
2196-6311 2196-632X |
publishDate |
2018-07-01 |
description |
<p>Recent work has highlighted a strong, worldwide, alpine glacial impact on
orogen erosion rates over the last 2 Ma. While it may be assumed that
glaciers increased erosion rates when active, the degree to which past
glaciations influence Holocene erosion rates through the adjustment of
topography is not known. In this study, we investigate the influence of
long-term tectonic and post-glacial topographic controls on erosion in a
glaciated orogen: the Olympic Mountains, USA. We present 14 new <sup>10</sup>Be and
<sup>26</sup>Al analyses which constrain Holocene erosion rates across the Olympic
Mountains. Basin-averaged erosion rates scale with basin-averaged values of 5 km local relief, channel steepness, and hillslope angle throughout the range,
similar to observations from non-glaciated orogens. These erosion rates are
not related to mean annual precipitation or the marked change in Pleistocene
alpine glacier size across the range, implying that glacier modification of
topography and modern precipitation parameters do not exert strong controls
on these rates. Rather, we find that despite spatial variations in glacial
modification of topography, patterns of recent erosion are similar to those
from estimates of long-term tectonic rock uplift. This is consistent with a
tectonic model where erosion and rock uplift patterns are controlled by the
deformation of the Cascadia subduction zone.</p> |
url |
https://www.earth-surf-dynam.net/6/595/2018/esurf-6-595-2018.pdf |
work_keys_str_mv |
AT baadams tectoniccontrolsofholoceneerosioninaglaciatedorogen AT baadams tectoniccontrolsofholoceneerosioninaglaciatedorogen AT taehlers tectoniccontrolsofholoceneerosioninaglaciatedorogen |
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