Bathymetric trackline navigation collected by the U.S. Geological Survey within the St. Clair River between Michigan and Ontario, Canada, 2008 (ESRI VECTOR SHAPEFILE, 08016_SWATHPLUS_TRK.SHP)

In 2008, the U.S. Geological Survey (USGS), Woods Hole Coastal and Marine Science Center (WHCMSC), in cooperation with the U.S. Army Corps of Engineers conducted a geophysical and sampling survey of the riverbed of the Upper St. Clair River between Port Huron, MI, and Sarnia, Ontario, Canada. The objectives were to define the Quaternary geologic framework of the St. Clair River to evaluate the relationship between morphologic change of the riverbed and underlying stratigraphy. This report presents the geophysical and sample data collected from the St. Clair River, May 29-June 6, 2008 as part of the International Upper Great Lakes Study, a 5-year project funded by the International Joint Commission of the United States and Canada to examine whether physical changes in the St. Clair River are affecting water levels within the upper Great Lakes, to assess regulation plans for outflows from Lake Superior, and to examine the potential effect of climate change on the Great Lakes water levels ( http://www.iugls.org). This document makes available the data that were used in a separate report, U.S. Geological Survey Open-File Report 2009-1137, which detailed the interpretations of the Quaternary geologic framework of the region. This report includes a description of the suite of high-resolution acoustic and sediment-sampling systems that were used to map the morphology, surficial sediment distribution, and underlying geology of the Upper St. Clair River during USGS field activity 2008-016-FA . Video and photographs of the riverbed were also collected and are included in this data release. Future analyses will be focused on substrate erosion and its effects on river-channel morphology and geometry. Ultimately, the International Upper Great Lakes Study will attempt to determine where physical changes in the St. Clair River affect water flow and, subsequently, water levels in the Upper Great Lakes.

2008年，美国地质调查局（U.S. Geological Survey, USGS）联合伍兹霍尔海岸与海洋科学中心（Woods Hole Coastal and Marine Science Center, WHCMSC），协同美国陆军工程兵团，针对密歇根州休伦港至加拿大安大略省萨尼亚市之间的圣克莱尔河上游河床开展了地球物理与采样综合调查。本次调查的核心目标为明确圣克莱尔河的第四纪地质格架，以解析河床地貌演变与下伏地层之间的内在关联。
本报告收录了2008年5月29日至6月6日期间，作为“国际上五大湖上游研究项目”（International Upper Great Lakes Study）一部分所采集的圣克莱尔河地球物理与样本数据。该项目由美加国际联合委员会（International Joint Commission）资助，为期五年，旨在探究圣克莱尔河的物理变化是否对上五大湖水位产生影响、评估苏必利尔湖出水调控方案，并分析气候变化对五大湖水位的潜在作用（http://www.iugls.org）。
本数据集提供了美国地质调查局公开文件报告2009-1137（U.S. Geological Survey Open-File Report 2009-1137）中所使用的全部数据，该报告详细阐释了该区域的第四纪地质格架。
本报告详细介绍了美国地质调查局野外作业2008-016-FA期间，用于测绘圣克莱尔河上游河床地貌、表层沉积物分布与下伏地质特征的全套高分辨率声学与沉积物采样系统。本次调查同步采集了河床视频与照片资料，并将其纳入本次数据集发布范围。
后续研究将聚焦于河床基质侵蚀及其对河道地貌与形态的影响。最终，“国际上五大湖上游研究项目”将尝试明确圣克莱尔河的物理变化在哪些区域影响水流，并进而作用于上五大湖的水位。