“…It is generally accepted that longwall mining causes changes in the properties of stream flows, springs, wells, and aquifers (e.g., flux, water levels, pore-water pressure, head, hydraulic gradients, drawdown, groundwater chemistry, porosity, storativity, permeability, transmissivity), stress alternation, fracture changes, and subsidence by observations in wells near the panel and by the use of borescope monitoring with the analysis of drill cores and surface fracture surveys in conjunction with microgravity measurements or other geophysical techniques, together with some computer modeling techniques [7,12,[35][36][37].…”