Two coal samples (810 Panel and Area 900) collected from Clarence Colliery have been tested under a controlled heating procedure to evaluate the gas evolution trends corresponding to increasing temperature. Gas evolution data are normally used to identify key gas indicators and validate the trigger action response plan settings for the mine as part of the Principal Hazard Management Plan for Spontaneous Combustion. The samples were located some 6 km apart and there is a significant coal-type difference between them. At low temperatures (<100c), the graham's ratio (gr) values for the two samples are almost identical. however, at elevated temperatures, there is a significant difference, with the 810 panel coal having higher gr values than the area 900 coal. this is most likely due to a difference in the coal reactivity. the 810 panel coal does not evolve ethylene until temperatures in excess of 140c are reached, whereas area 900 coal evolves ethylene once temperatures in excess of 120c are reached. the 810 panel coal also produces significant ethane evolution (200 ppm) at low temperatures (50c) due to the presence of retained ethane seam gas, which decreases as the temperature increases due to desorption from the coal. once the coal temperature exceeds 130c, the ethane evolution increases again due to coal oxidation reactions, reaching levels of 50 ppm. in contrast, the area 900 coal has no significant low-temperature ethane evolution, and ethane evolution only increases once the coal temperature exceeds 120c. there are also noticeable differences in the trends of other gases evolved from the coal. these findings have implications for the interpretation of gas monitoring results from the two different areas of the mine. they also illustrate the need for obtaining results from each new area of a mine as it develops so that changing gas evolution trends can be identified in advance of mining.citation:beamish, b, sargeant, j, levi, t and theiler, j, 2015. gas evolution trends for coal from two different areas at clarence colliery, in proceedings the australian mine ventilation conference, pp 273-278 (the australasian institute of mining and metallurgy: melbourne).>