废地案

Utah Geology Pub Date : 1900-01-01 DOI:10.34191/ug-1-1_1
D. McMillian
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引用次数: 0

摘要

1974年2月,高级巡回法官查尔斯·法希(Charles Fahy)裁定,对于1896年1月4日(当时大盐湖位于海拔4201英尺)至1967年6月15日(当时湖面已降至海拔4195英尺)之间暴露的大盐湖周围的32.5万英亩土地,美利坚合众国不能对犹他州提出任何索赔。在最初的特别法官J. Cullen Ganey去世后,Fahy法官被美国最高法院任命为犹他州诉美国一案(406 US 484)的特别法官。巧合的是,在法伊做出决定后的几周内,这个湖的水位就上升到了4201英尺。有争议的海岸的重要性在20世纪60年代变得明显。由于无法获得建设蒸发池和炼化厂所需的明确土地所有权,对湖盐水中所含矿产资源的开发受到阻碍。结果,国会于1966年6月3日通过了一项法案,要求内政部长放弃对大盐湖弯曲线以下土地的所有美国权益的要求,除了熊河候鸟保护区和韦伯盆地联邦填海工程。为此,国会指示部长在六个月内完成“犹他州大盐湖周围的公共土地调查,关闭该湖的曲线,尽可能准确地遵循大盐湖的平均高水位,用于在未测量区域的两侧固定曲线”。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The Relicted Lands Case
In February, 1974, Charles Fahy, a Senior Circuit Judge, concluded that the United States of America could not assert any claim against the state of Utah to the 325,000 acres of land surrounding the Great Salt Lake exposed between January 4, 1896, when the lake stood at 4,201 feet above sea level and June 15, 1967, when the lake level had receded to 4,195 feet above sea level. Judge Fahy, was appointed Special Master by the United States Supreme Court in the case of Utah vs United States (406 US 484) after the original Special Master, Judge J. Cullen Ganey, died. By coincidence, within a few weeks after Fahy's decision, the lake had risen to the 4,201 foot level. Importance of the contested shorelands became obvious during the 1960's. Development of mineral resources contained in the lake brines was held up because clear title to land needed for construction of evaporation ponds and refining plants could not be obtained. As a result, Congress passed an act on June 3, 1966, requiring the Secretary of the Interior to quitclaim to the state of Utah all United States interest in lands lying below the meander line of the Great Salt Lake excepting the Bear River Migratory Bird Refuge and the Weber Basin federal reclamation project. To effect this, Congress directed the Secretary to complete, within six months, "the public land survey around the Great Salt Lake in the state of Utah by closing the meander line of that lake, following as accurately as possible the mean high water mark of the Great Salt Lake used in fixing the meander line on either side of the unsurveyed area".
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