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The Silurian sedimentary rocks are predominantly terrigenous. The basal strata of the Silurian vary in composition from place to place. The lowermost formation, the Cabano, is characterized by lithic wackes interbedded with lithic conglomerates or lutites. The Cabano Formation grades upward into lutites and arkosic wackes of the Lac Raymond Formation (new name, LESPfiRANCE and GREINER, in press). A coarse terrigenous facies, comprising the Pointe-AuxTrembles Formation (new name, LESPfiRANCE and GREINER, in press), inte tongues with the Lac Raymond, and extends to the southwest. The Pointe-Aux-Trembles Formation consists mainly of lithic pyroclastic sandstones and conglomerates. Further east the Cabano Formation is overlain by lutites making up the Awantjish Formation.

Silurian Stratigraphy and Paleogeography of the Matapedia - Temiscouata Region. Quebec