This paper reports the results of a finite element study of the geothe
rmal heatflow into dry mine airways. For isotropic and unsteady state
conditions the heatflow into mine airways is studied for a range of su
rface heat transfer coefficients between rock and air, and age of the
airway. Dimensionless temperature gradient values are presented in tab
les for different values Of Boit and Fourier numbers and the results a
re compared with Starfield tables and Gibson algorithm. It is found th
at Starfield tables have consistently over-predicted the G values with
errors ranging from 2% to 10%. The differences between results obtain
ed from the finite element study and the G values calculated from Gibs
on's approximation method are mapped. The small error values over a la
rge range of Fourier and Biot numbers confirm the suitability of Gibso
n's algorithm to rapidly calculate G values for estimating the heat tr
ansfer from surrounding rock to mine air.