Alan L. Mayo

TL;DR: In this article, ground water flow systems in the rugged central Wasatch Range, Utah, were investigated by solute and isotopic methods, and six types of ground water systems were identified on the basis of rock type and structure.

TL;DR: In this article, the formation and preservation of sandstone landforms such as pillars and arches is studied, and it is shown that load-bearing material weathers more slowly and thus the internal stress field can shape and stabilize the landforms.

TL;DR: In this article, the authors present a conceptual model of groundwater flow that describes active and inactive groundwater flow regimes, based on an analysis of interactions between surface water and shallow and deep groundwater in the 240 km-long Wasatch Range and Book Cliffs, Utah, USA.

TL;DR: Shoreline carbonate deposits of Pleistocene Lake Bonneville record the conditions and processes within the lake, including the evaporative balance as well as vertical and lateral chemical and isotopic gradients.

TL;DR: In this article, the authors used solute and isotopic compositions of non-evolved inflow groundwater and evolved mine discharge water to quantify the chemical evolution of mine discharge in a western underground coal mine.