COAL FIRES: OPPORTUNITY FOR INNOVATIVE RESEARCH IN MINERALOGY, PETROLOGY, STRUCTURAL GEOLOGY, AND ENVIRONMENTAL SCIENCE
Mineral assemblages and coal-tar deposits that encrust gas vents form by complex thermochemical processes including gas-altered substrate (GAS), gas-liquid-altered substrate (GLAS), and reactions among select gas components (SGC). The minerals may include millosevichite, salammoniac, gypsum, alunogen, pickeringite, tschermigite, godovikovite, and mascagnite, to name a few. Their nucleation is controlled by the chemistry of gas exhaled from a vent or fissure, the mineralogy of the substrate encountered by the exhaled gas, and the stratigraphic association of the vents and fissures with geologic structures including faults and folds.
Toxic-gas components including methane, carbon monoxide, benzene, and toluene that are exhaled from coal-fire gas vents and ground fissures pollute the atmosphere, hydrosphere, and lithosphere while destroying floral and faunal habitats. The resonance time of such pollutants, e.g., in soil gas, is unknown as are the long-term effects associated with them.
In spite of their global occurrence both in the geologic past and at present, the study of underground- and surface-coal fires, coal-fires science, has not been at the forefront of geologic research. In fact, geoscience textbooks and courses devote little if any attention to the study of these fires. Consequently, coal-fires offer challenging opportunities for collaborative and innovative research in both environmental science and classical geology, with special emphasis in mineralogy, petrology, and structural geology.
Illustrations of rare mineral assemblages, explosion breccias, paralvas, gas vents juxtaposed along faults, differential weathering, and subsidence structures in addition to gas vent and soil-gas analyses all reveal the enormous potential for interdisciplinary-research awaiting the geoscientist.