Extent of Pleistocene lakes in the western Great Basin
Extent of Pleistocene lakes in the western Great Basin
复制标题
大盆地西部更新世湖泊的范围
DOI：
10.3133/mf2323
复制
发表时间：
1999
期刊：
影响因子：
--
通讯作者：
M. Reheis
中科院分区：
文献类型：
--
作者：
M. Reheis
亨菲尔-黑利，M.A.，1987，第四纪地层学和沿俄勒冈州东南部斯廷斯山东部悬崖底部的晚全新世断层：洪堡州立大学阿尔卡塔硕士论文，第84页，D.N，以及亨菲尔-黑利，M.A.，1988，阿尔沃德盆地晚更新世洪水历史，哈尼公司，俄勒冈州哈尼公司[摘要]：西北科学，第62卷，第2期，第81页。米夫林，M.D.和麦特，M.M.，1979，《内华达州的雨水湖和估计的雨洪气候：内华达州矿产和地质局公报94，57页，雷海斯，密歇根州，和莫里森，R.B.，1997，内华达州西部的高地，旧雨水湖，在林克，P.K.，和科瓦利斯，B.J.，编辑，元古代到现代地层学，构造和火山学，犹他州，内华达州，爱达荷州南部，和墨西哥中部：普罗沃，杨百翰大学地质研究，第1卷，第459-492页。Reheis，M.C.，Sarna-Wojcicki，A.M.，Reynolds，R.L.，Repenning，C.和Mifflin，M.D.，出版社，《西部大盆地中上新世至中更新世湖泊：年龄和联系》，在Hershler，R.，Currey，D.和Madsen，D.编，《大盆地水系历史：华盛顿特区，史密森学会》。Reheis，M.C.，Slate，J.L.，Sarna-Wojcicki，A.M.和Meyer，C.E.，1993，《内华达州和加利福尼亚州鱼湖谷的晚上新世至中更新世洪水湖：美国地质学会公报》，第105卷，第959-967页。J·H·斯图尔特和多伦文德，1984，内华达州惠灵顿四合院地质图：美国地质调查局公开档案报告84-211，比例尺1：62,500。维德，D.L.，1975年，俄勒冈州华纳谷哈特山区的冰后地貌和环境：加州大学洛杉矶分校博士论文，293页。更新世湖泊概述大多数晚更新世海岸线高度和湖泊名称来自Mifflin和Mcand(1979)。韦德的华纳湖海岸线(1975)，来自海姆菲尔黑利的阿尔沃德湖海岸线和溢流(1987)，以及林德伯格和亨菲尔-海利湖的郊狼海岸线和溢洪线(1988)。从美国地质勘探局1：250,000比例尺DEM在Arc/Info中生成的阴影地貌基础。来自Reheis等人(1993)、Reheis和Morrison(1997)以及Reheis和其他人(印刷中)的晚更新世以前的海岸线，除了惠灵顿湖(Stewart和Dohrenwend，1984)。有关湖泊沉积地点的信息，请参阅Reheis和其他人(1993；正在出版中)。地图投影：兰伯特保角二次曲线。数字制图：迈克尔·奥唐奈和乔纳森·雷德迈克斯。晚更新世湖泊面积(未全部显示)。湖名下方以米为单位的海岸线高度
Hemphill-Haley, M. A., 1987, Quaternary stratigraphy and late Holocene faulting along the base of the eastern escarpment of Steens Mountain, southeastern Oregon: M.S. thesis, Arcata, Humboldt State University, 84 p. Lindberg, D.N., and Hemphill-Haley, M.A., 1988, Late-Pleistocene pluvial history of the Alvord basin, Harney Co., Oregon [abstract]: Northwest Science, v. 62, no. 2, p. 81. Mifflin, M. D., and Wheat, M. M., 1979, Pluvial lakes and estimated pluvial climates of Nevada: Nevada Bureau of Mines and Geology Bulletin 94, 57 p. Reheis, M. C., and Morrison, R. B., 1997, High, old pluvial lakes of western Nevada, in Link, P. K., and Kowallis, B. J., eds., Proterozoic to recent stratigraphy, tectonics, and volcanology, Utah, Nevada, southern Idaho, and central Mexico: Provo, Brigham Young University Geology Studies, v. 1, p. 459-492. Reheis, M. C., Sarna-Wojcicki, A. M., Reynolds, R. L., Repenning, C. A., and Mifflin, M.D., in press, Pliocene to middle Pleistocene lakes in the western Great Basin: Ages and connections, in Hershler, R., Currey, D., and Madsen, D., eds., Great Basin Aquatic Systems History: Washington D.C., Smithsonian Institution. Reheis, M.C., Slate, J.L., Sarna-Wojcicki, A.M., and Meyer, C.E., 1993, A late Pliocene to middle Pleistocene pluvial lake in Fish Lake Valley, Nevada and California: Geological Society of American Bulletin, v. 105, p. 959-967. Stewart, J. H., and Dohrenwend, J. C., 1984, Geologic map of the Wellington quadrangle, Nevada: U.S. Geological Survey Open-File Report 84-211, scale 1:62,500. Weide, D. L., 1975, Postglacial geomorphology and environments of the Warner Valley Hart Mountain area, Oregon: Ph.D. dissertation, Los Angeles, University of California, 293 p. PLEISTOCENE LAKES SUMMARY Most late Pleistocene shoreline altitudes and lake names are from Mifflin and Wheat (1979). Lake Warner shoreline from Weide (1975), Lake Alvord shoreline and overflow from HemphillHaley (1987), and Lake Coyote shoreline and overflow from Lindberg and Hemphill-Haley (1988). Shaded relief base generated in Arc/Info from USGS 1:250,000-scale DEMs. Pre-late Pleistocene shorelines from Reheis and others (1993), Reheis and Morrison (1997), and Reheis and others (in press), except for Lake Wellington (Stewart and Dohrenwend, 1984). See Reheis and others (1993; in press) for information on lake-deposit localities. Map projection: Lambert Conformal Conic. Digital cartography: Michael O'Donnell and Jonathon Rademaekers. Area of late Pleistocene lakes (not all are shown). Shoreline altitude in meters shown below lake name