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Happing of quarternary deposits on the South Mountain Batholitb (SMB) has resulted in a four-fold subdivision of tills, divided primarily on the basis of clast lithology, texture, stratigraphic position and morphology.  Three tills have clast lithologies characterized by granites eroded from the South Mountain Batholih. The oldest granite till is a compact till of restricted distribution, mianly observed In drumlin cores. Two younger granite tills dominate the surficial deposits of portions of the SMB and have textural properties ascribed to melt-out tills. The fourth till represents a farther-travelled till with a variable clast provenance typified by pebbles derived from both the SMB and regions to the north. Clast dispersal evidence suggests that all tills were transported in a general southward direction.  Detailed clast examinations allow reliable conclusions concerning direction of Ice flow and lithologic relationship between till and bedrock of the SMB. The SMB is an area of multiple glaciatlon where till prospecting cannot be successful unless the direction of till transport and source areas are established.   RESUME  Dn leve cartographique des depots quaternaires recouvrant le Batholite de South Mountain a permis de mettre en evidence quatre varletes de tills en fonctlon de la lithologie des clastes, la texture, la position stratlgraphlque et la morphologic  Dana trola tills, les clastes nontrent des lithologles caracterisees par des granites arraches au Batholite de South Mountain (BSM). Le plus vleux till de granite est un till tasse. de faible etendue, observe surtout dans les noyaux de drumlins. Dans certaines portions du BSM, les depots de surface sont domines par deux tills de granite plus recents qui possedent des caracteristlques texturales rapportees aux tills d'ablation. Le quatrieme till a parcouru une plus grande distance; la source de ses clastes est variable et comprend typiquement des galets provenant tant du BSM que des regions plus au nord. La dispersion des blocaux suggere un direction generale de transport des tills vers le sud.  Un exanen approfondi des clastes permet de tirer de solides conclusions a propos de la direction de l’ecouleroent glacialre et de la relation lithologique entre le till et le socle du BSM. Le BSM a subi de multiples glaciatlons et la prospection du till n'y est done guere profitable a molns de determiner la direction de transport et la source du till.  [Traduit par le journal]

The provenance of tills overlying the eastern part of the South Mountain Batholith, Nova Scotia