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〕 | lat_d = 37 | lat_m = 49 | lat_s = 20 | lat_NS = N | long_d = 114 | long_m = 25 | long_s = 0 | long_EW = W | area_unit = acre | area_imperial = 1608 | area_round = 0 | established = 1935 | management_body = Nevada Division of State Parks | map_locator = Nevada svg | map = USA Nevada location map.svg | map_caption = Location of Cathedral Gorge State Park in Nevada }} Cathedral Gorge State Park is a state park of Nevada, USA, featuring a gorge eroded through soft bentonite clay. The park covers . It is located in Central/Eastern Nevada along U.S. Route 93, north of the west end of State Route 319, near Panaca. Cathedral Gorge was established as one of the four original Nevada State Parks in 1935. The park sits at an elevation of above sea level, and is typically arid with semi-hot summers, and very cold winters. In the summer, temperatures usually range from in midday to roughly at night. Rainfall is variable, and thunderstorms are prevalent. At one time, Shakespearean plays were performed with the clay formations in the backdrop. The various naturally formed crevices were used as dressing rooms and as a backstage where actors and actresses would prepare, awaiting their cue. ==Natural history== 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「Cathedral Gorge State Park」の詳細全文を読む スポンサード リンク
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