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-31- <br />Mining activities which affect subsidence are: <br />- Size, shape, depth, location, and aerial extent of workings; <br />- Rate of development and extraction of resource; <br />- Mining methods; and <br />- Number of overlying and underlying coal seams mined. <br />The possible hydrologic impacts of subsidence include: <br />- Modification of surface water hydrology - channel and <br />watershed geometry and sediment erosion rates; <br />- Modification of ground water hydralogy - changes in spring <br />discharge, aquifer characteristics and recharge; <br />- Loss of water from surface impoundments due to disruption by <br />surface cracking; and <br />- Increase in surficial mass movement activity - landslides and <br />rock falls (affecting water quality and water movement). <br />Natural physical influences upon subsidence can be controlled to the <br />extent that mine plans can be designed to avoid obvious hazards (e.g., <br />shallow workings beneath perennial streams, landslide bodies, <br />impoundments, etc.), or to limit subsidence in accordance with the <br />current state-of-the-art of ground control (engineered control of roof <br />and pillar failures in mines). Subsidence prediction and ground control <br />engineering are not definitive sciences. Design engineering concepts <br />must be verified through continuous monitoring of surface topography, <br />ground water hydrology and surface water hydrology. <br />Evaluation of the impacts of subsidence upon hydrologic systems requires <br />the collection and analysis of extensive monitoring data consisting of <br />Surface water and ground water monitoring (quantity and quality), <br />precipitation gaging, geological mapping, topographic surveying and <br />monitoring of mine inflow, discharge, and consumption rates. The <br />monitoring data should be updated continuously as mining progresses to <br />improve engineering control design parameters or to mitigate any <br />unexpected hydrologic impacts of subsidence. Such procedures are <br />necessary at each mine within the Roaring Fork Drainage in order to <br />coordinate a comprehensive subsidence control plan. This monitoring is <br />now being required of operators through the Colorado Permanent Regulatory <br />Program permitting process. <br />The dimensions of surface cracks from subsidence appear to relate to the <br />type of rocks in which they occur, the thickness of coal removed, the <br />depth of the overburden, and the location of crack occurrence. Cracks'in <br />competent rocks tend to remain open and allow free movement of waters. <br />Cracks in incompetent rocks and soils are likely to fill and retard or <br />limit free movement of waters. <br />