区域尺度、高分辨率的山顶曲率测量结果揭示了构造、气候和岩性对山坡形态的控制作用

IF 4.8 1区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS
William T. Struble , Fiona J. Clubb , Joshua J. Roering
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引用次数: 0

摘要

气候、构造、岩性和生物都包含在地貌的形态中。山坡通过山顶弧度记录隆升和侵蚀速度,其中,更尖锐、更凸的山顶与更快的侵蚀速度相对应。然而,过去绘制隆升和侵蚀速率图的山顶曲率研究仅限于较小的空间尺度,这主要是由于曲率测量技术的速度相对较慢。由于缺乏区域尺度的观测数据,解构构造、气候和岩性对山坡形态的相对影响成为一项挑战。在这里,我们利用高性能计算和地形连续小波变换技术,快速绘制了俄勒冈州西部陡峭、多断面的俄勒冈海岸山脉(OCR)和邻近较平缓的卡斯卡迪亚弧前低地(CFL)的山顶曲率图,1 米激光雷达数据总面积达 43,000 平方公里。我们还将绘制的山顶曲率与根据宇宙成因 10Be 得出的侵蚀率进行了比较,其中包括 11 个新采样的流域。我们观察到,OCR 地区的山顶比 CFL 地区的山顶更尖锐,而且我们注意到流域平均侵蚀率与山顶曲率之间存在线性关系,这与之前的观察结果和理论是一致的,即在土壤覆盖的地貌中,侵蚀率与山顶曲率成线性比例关系。以山顶曲率划分的 OCR 和 CFL 之间的边界往往是突然的,并出现在分隔不同基底层但岩性和年平均降水量保持不变的测绘结构上。因此,虽然我们观察到山顶曲率的显著变化是由次要岩性和气候控制造成的,但我们的结果表明俄勒冈州西部的山坡形态主要是由构造控制的基底降低率所造成的隆起所决定的。这些区域性解释还凸显了小波变换在快速量化山顶曲率方面的计算优势。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Regional-scale, high-resolution measurements of hilltop curvature reveal tectonic, climatic, and lithologic controls on hillslope morphology
Climate, tectonics, lithology, and biology are encoded within the morphology of landforms. Hillslopes record uplift and erosion rate through hilltop curvature, in which sharper, more convex hilltops correspond with more rapid erosion rates. However, past hilltop curvature studies that map uplift and erosion rates have been limited to small spatial scales largely due to relatively slow speeds of curvature measurement techniques. This lack of regional-scale observations has made deconvolving the relative contributions of tectonics, climate, and lithology to hillslope morphology a challenge. Here, we used high performance computing and continuous wavelet transforms of topography to rapidly map hilltop curvature in the steep and dissected Oregon Coast Range (OCR) and the adjacent gentler Cascadia Forearc Lowland (CFL) in western Oregon, amounting to ∼43,000 km2 of 1 m lidar data. We additionally compared mapped hilltop curvature to published erosion rates derived from cosmogenic 10Be, including 11 newly sampled watersheds. We observed that hilltops are systematically sharper in the OCR than in the CFL, and we noted a linear relationship between catchment-averaged erosion rate and hilltop curvature, consistent with previous observations and theory that erosion rate scales linearly with hilltop curvature in soil-mantled landscapes. The boundary between the OCR and CFL, as demarcated by hilltop curvature, is often abrupt and occurs across mapped structures that separate disparate baselevels but where lithology and mean annual precipitation remain constant. Thus, while we observed significant variability in hilltop curvature that results from secondary lithologic and climatic controls, our results demonstrate that hillslope morphology in western Oregon is set primarily by uplift via tectonically-controlled baselevel lowering rates. These regional interpretations additionally highlight the computational advantages of the wavelet transform for rapidly quantifying hilltop curvature.
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来源期刊
Earth and Planetary Science Letters
Earth and Planetary Science Letters 地学-地球化学与地球物理
CiteScore
10.30
自引率
5.70%
发文量
475
审稿时长
2.8 months
期刊介绍: Earth and Planetary Science Letters (EPSL) is a leading journal for researchers across the entire Earth and planetary sciences community. It publishes concise, exciting, high-impact articles ("Letters") of broad interest. Its focus is on physical and chemical processes, the evolution and general properties of the Earth and planets - from their deep interiors to their atmospheres. EPSL also includes a Frontiers section, featuring invited high-profile synthesis articles by leading experts on timely topics to bring cutting-edge research to the wider community.
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