In the Conception Bay in Newfoundland, Southeastern coast of Canada, a series of Pre-Cambrian to Cambrian-linked volcanic rocks were silicified. The rocks mainly consist of rhyolitic and basaltic flows, with crystal tuffs and breccia interbedded. Regional silicification was taken place as a preliminary alteration process before other geochemical processes occurred. The source of silica near the area was from hot siliceous fluids from rhyolitic flow under a static condition. A significant portion of silica appeared in the form of white chalcedonic quartz, quartz veins as well as granular quartz crystal. Due to the difference in rock structures, silica replaces different materials in rocks of close locations. The following table shows the replacement of silica at different localities: