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Visualizing the geology of lake trout spawning sites; northern Lake Michigan

机译:可视化鳟鱼产卵站点的地质;北部密歇根湖

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摘要

Geologists and biologists are working together to understand the links between lake floor geology (composition and shape) and the distribution of lake trout throughout their life cycle. Lake floor geology is one of the main factors determining where lake trout spawn, feed, and hide. In support of ongoing research to study Lake Michigan trout habitats, the U.S. Geological Survey in cooperation with the U.S. Army Corps of Engineers mapped the morphology of principle lake trout spawning sites. Using the Army Corps of Engineeru27s SHOALS airborne lidar (Light Detection and Ranging) system we mapped six regions in Northern Lake Michigan in order to identify ideal spawning regions composed of shallow, clean, gravel/cobble substrate, adjacent to deeper water.Lidar mapping systems, which use laser pulses to measure water depths from an airplane, are now available to map the nearshore lake morphology at meter-scale detail. Maps generated from the bathymetric data are used to define regions with smooth homogeneous substrate, regions with higher relief, and mixed regions with both smooth and rough relief. This morphologic information combined with sediment samples and direct bottom observations enable geologists to map areas with rougher relief composed of rock outcrop, boulders, and cobbles, as well as smooth regions covered with sand or mud. This information helps biologists, fishery managers, and ecologists visualize the lake floor in significant detail which promotes better fishery management, species protection, and habitat identification.These maps present the maps and discuss the geology of the six lake trout spawning sites mapped by the lidar system. Where the mapping approached land, aerial photography of the land is combined with the bathymetric data to help visualize the scale of the offshore features. Map and perspective views of Boulder Reef, Hog Island Reef, and Little Traverse Bay are shown on sheet 1, whereas map and perspective views of Trout and High Island Shoal, Gull Island Reef, and Dahlia Shoal are shown on sheet 2. Additional information, bathymetric data, imagery, and metadata are available online athttp://geopubs.wr.usgs.gov/open-file/of03-120/.
机译:地质学家和生物学家正在共同努力,了解湖泊地质地质(组成和形状)之间的联系,以及整个生命周期的湖泊鳟鱼的分布。 Lake地板地质是确定湖鳟鱼产卵,饲料和隐藏的主要因素之一。为了支持持续研究,研究密歇根州克罗茨·栖息地,与美国工程师的地质调查合作,绘制了原则湖鳟鱼产卵网站的形态。使用工程师的陆军兵团 u27s浅滩空气传播激光雷达(光检测和测距)系统我们在北部密歇根州立六个地区映射了六个地区,以确定由浅,清洁,砾石/鹅卵石基底组成的理想产卵区,毗邻深水.Lidar使用激光脉冲来测量飞机的水深的映射系统现在可以在米级细节下映射近岸湖形态。从碱基数据产生的地图用于定义具有平滑均匀基板的区域,具有更高浮雕的区域,以及光滑和粗糙的浮雕的混合区域。这种形态学信息与沉积物样本相结合,直接底部观察使地质学家能够用岩石露头,巨石和鹅卵石组成的艰难浮雕的地区,以及覆盖着沙或泥浆的平滑区域。这些信息有助于生物学家,渔业经理和生态学家以重大细节可视化湖泊地板,促进更好的渔业管理,物种保护和栖息地识别。这些地图展示了地图,并讨论了六勒湖的地质地质绘制了激光器映射的六湖鳟鱼产卵网站的地质系统。在映射接近土地的情况下,该土地的航拍与碱基数据相结合,以帮助可视化海上特征的规模。博尔德礁,猪岛礁和小横向托架的地图和透视景观在纸张1上显示,而鳟鱼和高岛浅滩,鸥岛礁和大丽花浅滩的地图和透视景观在表2上显示2.附加信息,在线Athttp://geopubs.wl.usgs.gov/open-file/of03-120/可用浴约定数据,图像和元数据。

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