Cumberland River Resource Stewardship and Protection: Managing the Cumberland River and the Land Between the Lakes Landscapes

Kenneth Ray Olson
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Abstract

Cumberland River formed on Cumberland Plateau by confluence of the Poor and Clover forks in Harlan county, Kentucky and loops south through northern Tennessee. It joints the Ohio River at Smithland, Kentucky. The Cumberland River is 1107 km long and has a drainage area of 46,830 km2. The Cumberland crosses a highland bench in Cumberland Plateau and flows in a gorge between 90 - 120 m cliffs. The Cumberland Falls is 20.7 m high. The river enters the central limestone basin of Tennessee, turning north, crosses the plain of western Kentucky to Ohio River at Smithland, Kentucky and at one point it is less than 3 km from Tennessee River. The Cumberland River had a long history of transporting furs, canoes, guns, armies, settlers, coal products and manufactured goods in the 1700s and 1800s. Three separate forks (Martin’s Fork, Clover Fork, and Poor Fork) flow out of the Appalachian Mountains in southeast Kentucky near the Virginia border to form the headwaters of the Cumberland River near Harlan, Kentucky. Steamboat traffic on the Cumberland River increased substantially in the 1800s as expanding coal fields, stone quarries and Tennessee produce began to be shipped throughout the region. The Cumberland River was surveyed during this period and between 1832 and 1838 Congress appropriated $155,000 for improving commercial navigation. With this infusion of money the United States Army Corps of Engineers (USACE) could clear the river of snags and build wing dams to deepen the channel. A 1060 km Cumberland River regional trail system, similar to the Tennessee River regional trail system under development, is needed to promote recreational tourism and increase use of the Cumberland River and basin. The primary objectives are: 1) to document how the landscape and geological resources of the Cumberland River have contributed to the successful water resource and economic development of a historic region in North America, 2) to identify future risks to the natural and environmental resources, 3) create a regional trail system with community access points and 4) create generations of people who care about the environmental stewardship and protection of the river and landscape resources.
坎伯兰河资源的管理和保护:管理坎伯兰河和湖间土地景观
坎伯兰河形成于坎伯兰高原,由肯塔基州哈兰县的普尔和克拉弗分叉汇合而成,向南流经田纳西州北部。它在肯塔基州的史密斯兰与俄亥俄河汇合。坎伯兰河长1107公里,流域面积46,830平方公里。坎伯兰河穿过坎伯兰高原的一个高地,在90 - 120米高的悬崖之间的峡谷中流淌。坎伯兰瀑布高20.7米。这条河进入田纳西州中部的石灰岩盆地,向北转,穿过肯塔基州西部的平原,在肯塔基州的史密斯兰到达俄亥俄河,一度距离田纳西河不到3公里。在18世纪和19世纪,坎伯兰河在运送毛皮、独木舟、枪支、军队、定居者、煤炭产品和制成品方面有着悠久的历史。三个独立的分叉(马丁的叉,三叶草叉,和穷人叉)流出阿巴拉契亚山脉在肯塔基州东南部靠近弗吉尼亚边境,形成坎伯兰河的源头,靠近肯塔基州的哈兰。19世纪,随着煤田、采石场和田纳西农产品的扩张,坎伯兰河上的汽船交通大幅增加。在此期间,对坎伯兰河进行了调查,在1832年至1838年期间,国会拨款155,000美元用于改善商业航运。有了这笔资金,美国陆军工程兵团(USACE)就可以清除河流上的障碍,建造翼形水坝来加深河道。需要一个1060公里的坎伯兰河区域步道系统,类似于正在开发的田纳西河区域步道系统,以促进休闲旅游和增加对坎伯兰河和流域的利用。主要目标是:1)记录坎伯兰河的景观和地质资源如何为北美历史地区成功的水资源和经济发展做出贡献;2)确定自然和环境资源的未来风险;3)创建一个带有社区入口的区域步道系统;4)培养一代又一代关心河流和景观资源环境管理和保护的人。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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