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首页> 外文期刊>Journal of great lakes research >GIS-based geomorphologic study of Presque Isle Peninsula, a compound lacustrine barrier-spit system along the south-central Lake Erie margin
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GIS-based geomorphologic study of Presque Isle Peninsula, a compound lacustrine barrier-spit system along the south-central Lake Erie margin

机译:基于GIS的Presque Isle半岛地貌研究,Presque Isle半岛是伊利湖中南部边缘的一个复合湖相屏障-吐水系统

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The Presque Isle peninsula is a sandy barrier-spit system situated along the south-central Lake Erie coast. This investigation focuses on landform succession along its eastern terminus, where nautical charts and aerial images chronicle morphologic change over the last century. A conceptual framework of this recent terrain evolution provides a blueprint for understanding the process-landform interactions responsible for constructing the compound peninsula over the late Holocene. Presque Isle is compartmentalized into four distinct en echelon strandplains, each comprised of multiple beach ridges of similar orientations, heights and spacing. These strandplain segments are separated by topographically prominent ridgelines that extend across the width of the peninsula and obliquely truncate landward paleoshorelines. The processes responsible for this landform juxtaposition are exemplified by recent spit growth and decay along Presque Isle's eastern terminus, where net lateral accretion has extended the peninsula by similar to 0.8 km(2) since the early 1900s. Truncation of newly formed ridge morphologies here since the 1990s provides a reference frame for understanding broader peninsular evolution, as reflected in Presque Isle's morphological segmentation. Episodes of spit accretion and low elevation beach-ridge formation sequentially construct strandplains with little internal heterogeneity in way of beach-ridge spacing and height. Net-depositional episodes are subsequently punctuated by extensive erosion and the formation of high-elevation ridgelines at oblique angles to paleoshorelines. While this process is demonstrated over the recent similar to 100 years as a function of human-altered coastal hydrodynamics and sediment-supply reductions, potential linkages between older erosive landforms and major lake-level transgressions are inferred and could potentially be elucidated upon continued research. (C) 2016 International Association for Great Lakes Research. Published by Elsevier B.V. All rights reserved.
机译:Presque Isle半岛是位于伊利湖中南部海岸的沙质障碍吐水系统。这项研究的重点是东端的地貌演替,航海图和航拍图记录了上个世纪的形态变化。最近的地形演化的概念框架为了解导致全新世晚期构造复合半岛的过程-地形相互作用提供了一个蓝图。 Presque Isle被划分为四个不同的梯级平原,每个平原由取向,高度和间距相似的多个滩脊组成。这些链平原部分被地形突出的山脊线隔开,这些山脊线横跨半岛的整个宽度,并倾斜地截断了陆上的古海岸线。造成这种地形并列的过程以最近沿Presque Isle东端的唾液生长和腐烂为例,自1900年代初以来,净侧向吸积使半岛延伸了近0.8 km(2)。自1990年代以来,这里新形成的山脊形态的截断为理解更广泛的半岛演化提供了参考框架,正如Presque Isle的形态学分割所反映的那样。唾液的积聚和低海拔滩脊的形成顺序依次构造了滩滩间距和高度几乎没有内部异质性的链平原。随后,由于广泛的侵蚀和与古海岸线成斜角的高海拔山脊线的形成,使网状沉积物破裂。尽管在近100年的时间里证明了这一过程是人为改变的沿海水动力和沉积物供应减少的函数,但可以推断出较老的侵蚀性地貌与主要湖平面海侵之间的潜在联系,并有可能在继续研究中加以阐明。 (C)2016年国际大湖研究协会。由Elsevier B.V.发布。保留所有权利。

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