An improved method of in situ combustion of carbonaceous material in a subterranean earth formation for effecting the recovery of hydrocarbons, comprising the steps of penetrating the earth formation with a pair of boreholes projecting into the earth formation along a substantially horizontal plane with respect to the earth surface and along a plane substantially perpendicular to the plane of maximum permeability in the earth formation with said boreholes being parallel to and separated from one another along the plane of maximum permeability, penetrating the earth formation with a plurality of vertically extending boreholes with these vertical boreholes being spaced apart from one another along a plane substantially parallel to and intermediate said pair of boreholes, providing an induced fracture in said earth formation at each of the plurality of vertical boreholes along a plane substantially parallel to the plane of maximum permeability and intersecting with each of said pair of boreholes for establishing a plurality of fluid flow paths projecting between said pair of boreholes and said plurality of boreholes, introducing a combustion-supporting medium into said earth formation through at least one of said pair of boreholes, initiating combustion of the carbonaceous material adjacent to at least one of said pair of boreholes to form a combustion zone, withdrawing hydrocarbon-containing fluid resulting from or displaced by said combustion primarily via said fluid flow paths through said plurality of boreholes, and controlling the rate of flow of said fluid through each of said plurality of boreholes for selectively controlling the configuration and rate of propagation of said combustion zone.