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Grande Ronde Aquifer : ウィキペディア英語版 | Grande Ronde Aquifer The Grande Ronde Aquifer is part of the regional Columbia Basin basalt aquifer system and is one of three aquifer systems that make up the Water Resource Inventory Area (WRIA) 32 along with the Wanapum and Saddle Mountain aquifers. The Grand Ronde Aquifer is the main source of drinking water for Pullman, Washington and Moscow, Idaho. For several decades the water levels in the Grande Ronde Aquifer have been in decline – up to 3 feet per year – due to pumping by the cities and universities.〔(Columbia Institute for Water Policy )〕 ==References==
抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)』 ■ウィキペディアで「Grande Ronde Aquifer」の詳細全文を読む
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