Abstract
Detailed topographic maps provide much of the information needed to understand how drainage divides like the southeast Wyoming Medicine Bow River-Laramie River drainage divide originated. Topographic map evidence for each Medicine Bow-Laramie River drainage divide segment is here described and analyzed first using a commonly published interpretation (accepted paradigm) in which drainage routes developed on a surface of now mostly absent Oligocene and Miocene sediments that previous investigators have hypothesized to have once filled the Laramie Basin and to have also buried (or partially buried) the surrounding Laramie and Medicine Bow Mountains. Second, the same map evidence is analyzed using a recently proposed interpretation (new paradigm) in which massive and prolonged floods flowed across Wyoming as the Laramie and Medicine Bow Mountains began to be uplifted and as the southeast-oriented North Platte River valley eroded headward along the rising Laramie Mountains northeast flank. Low points along the drainage divide (referred to as divide crossings) are interpreted to be places where water once flowed across the drainage divide with the drainage divide being formed when capture events diverted the water in other directions. Valleys leading away from divide crossings are used to determine the nature of observed capture events, many of which are difficult or impossible to explain from the accepted paradigm perspective, but which are consistent with the mountain uplift, headward erosion of deeper valleys, and/or draining of floodwaters trapped in the Laramie Basin as the new paradigm predicts. However, the new paradigm requires a North American continental ice sheet heavy enough to raise entire regions and mountain ranges as massive and prolonged meltwater floods flowed across them, something the accepted paradigm does not recognize.
Highlights
IntroductionIn natural settings drainage divides often cross precipitation and hydrologic regimes and can begin in high mountain ranges and cross mountain-enclosed basins before entering and ending in other mountain ranges
Low points along the drainage divide are interpreted to be places where water once flowed across the drainage divide with the drainage divide being formed when capture events diverted the water in other directions
Valleys leading away from divide crossings are used to determine the nature of observed capture events, many of which are difficult or impossible to explain from the accepted paradigm perspective, but which are consistent with the mountain uplift, headward erosion of deeper valleys, and/or draining of floodwaters trapped in the Laramie Basin as the new paradigm predicts
Summary
In natural settings drainage divides often cross precipitation and hydrologic regimes and can begin in high mountain ranges and cross mountain-enclosed basins before entering and ending in other mountain ranges. Such drainage divides do not delineate precipitation and hydrologic regimes differences or influence erosional processes. One such drainage divide is the southeast Wyoming Medicine Bow-Laramie River drainage divide shown, which at its southwest end begins at Medicine Bow Peak (southeast Wyoming’s highest point) as a triple drainage divide with the north-oriented North Platte River drainage basin (to the southwest). As the drainage divide progresses northeastward it crosses abandoned valleys as it descends approximately 1500 meters to cross the Laramie Basin floor before rising more than 500 meters into the Laramie Mountains where it meets the southeast-oriented North Platte River drainage basin (note in Figure 1 how the North Platte River in central Wyoming turns from flowing in a north direction to flow in a southeast direction)
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