A short history of ideas on the origin of the Grand Canyon

W. Ranney
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Abstract

—For as well known and highly regarded as the Grand Canyon is, its precise age and the specific processes involved in its formation remain somewhat elusive to the geologist. This is not due to a lack of trying, for the great gorge has been the subject of passionate inquiry since John Strong Newberry first laid eyes on it over 155 years ago. Research into the canyon’s origin has accelerated greatly since the turn of the millennium and a survey of the ever evolving ideas related to its development can serve to frame the foundations of many modern proposals. Historic ideas on the canyon’s origin gener- ally sought to relate the deeply dissected modern landscape (that continues to captivate practically anyone who encounters it), with the possible evolution of the Colorado River. The earliest geologists however, could not perceive of the dynamism that can be involved in a rivers’ history, nor could they benefit from a larger understanding of the tectonic evolution of the American Cordillera. It took nearly seventy years of research before definitive evidence was found that showed that the modern Colorado River, one that begins in the Rocky Mountains and drains across the elevated Colorado Plateau to the foundered Basin and Range and the Gulf of California, might actually be one of the younger geologic features found upon the southwestern landscape. Since this relative youthfulness of the river has been detected, myriad searches for prior ancestors, cut-off chan-nels, past configurations, or flow reversals have been postulated, presented, debated upon and accepted or rejected. Ideas that the river and canyon might be as old as the Laramide Orogeny have never gone away but consensus points to younger dates. A familiarity with historic theories for how the Grand Canyon and Colorado River evolved is presented below to help to frame modern debate.
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关于大峡谷起源的简短历史
尽管大峡谷广为人知,受到高度重视,但它的确切年龄和形成过程对地质学家来说仍然有些难以捉摸。这并不是因为缺乏尝试,因为自从155年前约翰·斯特朗·纽伯里第一次看到大峡谷以来,它就一直是人们热情探索的主题。自世纪之交以来,对峡谷起源的研究大大加快,对与其发展有关的不断发展的观点的调查可以为许多现代建议提供框架基础。关于峡谷起源的历史观点,一般都试图将深入剖析的现代景观(它继续吸引着几乎所有遇到它的人)与科罗拉多河可能的演变联系起来。然而,最早的地质学家既不能认识到河流历史中蕴含的活力,也不能从对美洲科迪勒拉山脉构造演化的更深入了解中获益。经过近七十年的研究,才发现确凿的证据,表明现代科罗拉多河可能是西南地区较年轻的地质特征之一。这条河发源于落基山脉,流经科罗拉多高原,流经盆地、山脉和加利福尼亚湾。自从这条河的相对年轻性被发现以来,无数关于先祖、切断的河道、过去的构造或水流逆转的研究被假设、提出、辩论、接受或拒绝。这条河和峡谷可能与拉腊米造山运动一样古老的观点从未消失,但共识指向更年轻的年代。以下是对大峡谷和科罗拉多河如何演变的历史理论的熟悉,以帮助构建现代辩论。
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