The Balfour Formation has a pronounced lithological variation that is characterized by alternating sandstone- and mudstone-dominated members.The sandstone-dominated Oudeberg and Barberskrans Members are composed of lithofacies that range from intraformational conglomerates to fine-grained sediments,whereas the mudstone-dominated members(Daggaboersnek,Elandsberg,and Palingkloof) are dominated by the facies Fm and Fl.Petrography,geochemistry,and a paleocurrent analysis indicated that the source rock of the Balfour Formation was to south east and the rocks had a transitional/dissected magmatic arc signature.The sandstones-rich members were deposited by seasonal and ephemeral high-energy,low-sinuous streams,and the fine-grained-rich members were formed by ephemeral meandering streams.The paleoclimates have been equated to present temperate climates;they were semiarid becoming arid towards the top of the Balfour Formation.This has been determined by reconstructing the paleolatitude of the Karoo Basin,geochemistry,paleontology, sedimentary structures,and other rock properties,like color. The Balfour Formation has a pronounced lithological variation that is characterized by alternating sandstone- and mudstone-dominated members. The sandstone-dominated Oudeberg and Barberskrans Members are composed of lithofacies that range from intraformational conglomerates to fine-grained sediments, but the mudstone-dominated members (Daggaboersnek, Elandsberg, and Palingkloof) are dominated by the facies Fm and Fl. Petrography, geochemistry, and a paleocurrent analysis indicated that the source rock of the Balfour Formation was to south east and the rocks had a transitional / dissected magmatic arc signature. The sandstones-rich members were deposited by seasonal and ephemeral high-energy, low-sinuous streams, and the fine-grained-rich members were formed by ephemeral meandering streams. The paleoclimates have been equated to present temperate climates; they were semiarid becoming arid towards the top of the Balfour Formation. This has been determined by reconstructing the paleolatitude of the K aroo Basin, geochemistry, paleontology, sedimentary structures, and other rock properties, like color.