How a New Cenozoic Geology and Glacial History Paradigm Explains Anomalous Monongahela River Drainage Basin Topographic Map Evidence, PA, WV and MD, USA

E. Clausen
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引用次数: 2

Abstract

A recently proposed and fundamentally different Cenozoic geology and glacial history paradigm (new paradigm) is used to explain previously reported and other anomalous Monongahela River drainage basin drainage system evidence (observable on detailed topographic maps in the form of barbed tributaries, asymmetric tributary drainage basins, large abandoned meander cutoffs, and poorly explained transverse drainages and abandoned transverse drainages). The north-oriented Monongahela River drainage system according to the accepted Cenozoic geology and glacial history paradigm (accepted paradigm) originated during preglacial times and was blocked by continental icesheets to form today’s Ohio River. Based on Missouri River drainage basin topographic map evidence the new paradigm predicts the Monongahela River drainage system developed during immense and prolonged south- and southwest-oriented continental icesheet melt water floods. The new paradigm also predicts icesheet caused regional uplift created a deep “hole” in which a thick icesheet was located and which forced south-oriented melt water floods to flow in southwest directions along the deep “hole’s” southeast rim (now the Ohio River-Atlantic Ocean drainage divide) until continued deep “hole” rim uplift and the deep valley headward erosion from space being opened up by icesheet melting reversed the flow direction to create the north-oriented Monongahela River drainage system. This new paradigm interpretation explains previously reported and other anomalous Monongahela River drainage system topographic map evidence and suggests the Monongahela River drainage system developed while a continental icesheet melted and not during preglacial time as has been commonly reported.
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一个新的新生代地质和冰川历史范式如何解释莫农加希拉河流域地形图证据,PA, WV和MD,美国
最近提出的一种根本不同的新生代地质和冰川历史范式(新范式)被用来解释以前报道的和其他异常的莫农加希拉河流域排水系统证据(在详细的地形图上以倒钩支流、不对称支流流域、大型废弃曲流断裂带、解释不清的横向流域和废弃横向流域的形式观察到)。根据公认的新生代地质和冰川史范式(公认范式),向北的莫农加希拉河(Monongahela)水系起源于前冰川期,被大陆冰原阻塞,形成了今天的俄亥俄河。基于密苏里河流域地形图证据,新范式预测了莫农加希拉河流域系统在大规模和长期的南部和西南方向的大陆冰原融化洪水期间发展。新的范式还预测,冰盖引起的区域性隆起造成了一个深“洞”,在这个深“洞”中有一个厚冰盖,这迫使南向的融水洪水沿着深“洞”的东南边缘(现在的俄亥俄河-大西洋排水分水岭)向西南方向流动,直到深“洞”边缘持续隆起,深山谷向上的侵蚀被冰盖融化打开,从而扭转了流动方向,形成了向北的莫农加希拉河排水系统。这种新的范式解释解释了先前报道的和其他异常的莫农加希拉河流域地形图证据,并表明莫农加希拉河流域系统是在大陆冰原融化时形成的,而不是像通常报道的那样在冰期前形成的。
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