The delicate coloring and formations in this image are produced by chemical weathering. This form of weathering occurs wherever seeping ground water circulating through the sandstone dissolves the calcium-carbonate cement between the individual grains, causing the rock to crumble to sand. Cavities work their way back into the walls of the escarpment. Over time, the cavities deepen and roofs collapse. Columns are formed which, in turn, finally topple. Pink, white, yellow, and red formations are produced by oxidation (chemical weathering) of the iron-bearing minerals found in the rock.
Large tailings impoundment with ponded surface water in Colorado. Because tailings contain very small particles such as clays, portions of the tailings will have low permeabilities. Surface waters from drainings that flow into the tailings and rain or snowfall, will commonly lead to ponded surface waters as illustrated here. This can sustain water-saturated conditions within the tailings and continue to feed the discharge of metal-bearing waters in seeps.
The delicate coloring and formations are produced by chemical weathering. This form of weathering occurs wherever seeping ground water circulating through the sandstone dissolves the calcium-carbonate cement between the individual grains, causing the rock to crumble to sand. Cavities work their way back into the walls of the escarpment. Over time, the cavities deepen and roofs collapse. Columns are formed which, in turn, finally topple. Pink, white, yellow, and red formations are produced by oxidation (chemical weathering) of the iron-bearing minerals found in the rock.