The Canadian Shield provides an unparalleled field laboratory for the study of secular changes in tectonic processes. Breaking up of continental crust that previously amalgamated during the Neoarchean produced new oceanic lithosphere, as well as thinned continental crust on which intracontinental and marginal basin formed, sequestring CO₂, Ca, Mg and P from the oceans in the process. Along the continental edges, tholeiitic magma provinces, including flood basalt, formed where mantle plumes impinged prior to breakup. After opening for about 170 Ma, which is within the time span of the modern Atlantic, the main (Manikewan) ocean closed producing arcs and back-arc basins that were later accreted to continental margins. In the Labrador Trough, Fe released in ca. 1.88 Ga continental back-arc vents precipitated in shallow, well-oxygenated near-shore waters, forming world-class iron-ore deposits of the Schefferville/ Labrador City areas. Fragments of the Manikewan paleo-ocean are now only preserved in the Watts Group of Cape Smith belt, where they are preserved in a klippe. Continental arc magmatism resulting from ocean lithosphere subducting beneath continental margins produced elongate batholiths and plutonic suites semi-continuous over distances of 2000 km or more, on scales comparable with Phanerozoic arcs. Accretion and collision following ocean closure resulted in the development of foreland and molasse basins, fed by modern-like fluvio-deltaic systems. In terms of collisional processes, many hallmarks observed in the Alpine-Himalayan orogenic system occurred, perhaps for the first time in Earth’s history, in the Superior-Churchill collision system (Trans-Hudson orogen). These processes include indenter tectonics, lower crustal flow, radial flow, formation of oroclines, and lateral extrusion. These observations suggest that thermal, petrological and mechanical parameters of the crust and mantle had attained states similar to those observed today by the Paleoproterozoic, roughly midway through Earth’s evolution.