Geology of Crystal Geyser and environmental implications of its effluent, Grand County, Utah

Utah Geology Pub Date : 1900-01-01 DOI:10.34191/ug-5-2-125
James L. Baer, J. Rigby
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引用次数: 15

Abstract

A geologic study was done in conjunction with an environmental impact investigation of the Crystal Geyser, 6.5 kilometers (4 miles) southeast of the community of Green River, Utah. Periodic eruptions of salt-laden waters from the geyser flow into the Green River and provide a source of salts into the Colorado River drainage system. Eruptions average 120 cubic meters (0.1 acre feet) of CO2 charged water with abundant Na, Ca, K. and Mg salts. The mineral laden waters form tufa deposits along a nearly 2 kilometer (1.3 miles) exposure that is situated along and controlled by the Little Grand Wash Fault. Three distinctive levels of tufa deposits indicate that the mineral-laden springs have been active along the fault for several hundred thousand years. Several methods considered to control the salt laden effluent were rejected as either impractical or too expensive.
水晶间歇泉的地质及其流出物的环境影响,格兰德县,犹他州
一项地质研究与对水晶间歇泉的环境影响调查一起完成,水晶间歇泉位于犹他州绿河社区东南6.5公里(4英里)处。间歇泉定期喷发的含盐水流入格林河,为科罗拉多河的排水系统提供了盐的来源。火山喷发平均120立方米(0.1英亩英尺)的含二氧化碳的水含有丰富的钠、钙、钾和镁盐。富含矿物质的水沿着一条近2公里(1.3英里)的暴露线形成凝灰岩沉积物,该暴露线位于小大冲刷断层并受其控制。三层不同层次的凝灰岩沉积物表明,富含矿物质的泉水已经沿着断层活跃了几十万年。考虑过的几种控制含盐废水的方法因不切实际或过于昂贵而被拒绝。
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