Gradient Controlled Caves, Trapper-Medicine Lodge Area, Bighorn Basin, Wyoming
ABSTRACT Extensive caves have developed under canyons in the Trapper‐Medicine Lodge recharge area where ground‐water flow rates became maximized within the Madison carbonates during Cenozoic time. The large flow rates resulted directly from the superposition of steep local gradients on the ground‐wa...
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| Veröffentlicht in: | Ground water 1985-07, Vol.23 (4), p.443-448 |
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| Format: | Artikel |
| Sprache: | eng |
| Online-Zugang: | Volltext |
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