Seismic, magnetic and gravity data indicate that the Chukchi and Beaufort epicontinental seas off northern Alaska overlie three sedimentary basins, or provinces, separated by structural highs of regional extent. The basins trend west to northwest and their enclosed sediments become increasingly marine from south to north. The Chukchi-Beaufort continental margin is similar to those of Atlantic type. Hope Basin, in the southern Chukchi Sea, overlies strongly deformed Paleozoic to mid-Cretaceous rocks of the Brooks Range orogen. The basin is inferred to contain nonmarine and marine clastic sedimentary rocks in a one km-thick Upper Cretaceous (?), a 1.5 km-thick Paleogene (?), and a 1.5/0.75 km-thick Neogene(?) sequence. A large anticline and many faults and smaller folds disrupt mainly the older sequences. The Hope Basin sedimentary units onlap Herald Arch, which trends northwestward from Cape Lisburne in the central Chukchi Sea. At the Herald fault zone Brooks Range rocks in the arch are thrust eastward or northeastward over Mississippian to Jurassic shelf carbonate and clastic rocks of the Arctic Alaska (Ellesmerian) basin and overlying Cretaceous flysch and molasse of the Colville Geosyncline. These Mississippian to Cretaceous rocks underlie the northeast Chukchi Sea and reportedly are about 10 km thick near the Herald fault zone on the Lisburne Peninsula. The great Chukchi syntaxis in western Brooks Range rocks and structures is thought to result from intersection of the west-trending Brooks Range orogen with the northwest-trending Herald fault zone. The Mississippian to Jurassic shelf sequence thins northward, and onlaps the Barrow Arch, which trends northwest from Point Barrow to 161° W. Long., thence west-southwest to the Herald fault zone. The Colville Geosyncline sequence oversteps both the pre-Cretaceous rocks and the Barrow Arch to form the North Chukchi Basin west of 161° W. Long, and the progradational Beaufort continental terrace to the east. The North Chukchi Basin may contain about 6 km of probable Cretaceous and Tertiary section, which may be deltaic in origin. Diapirs (of Cretaceous shale?) pierce the gently northward-dipping strata of this basin, in places reaching the sea floor. Thick Tertiary marine and nonmarine clastic rocks of the Camden Basin overlie the Cretaceous rocks of the North Slope and inner Beaufort continental terrace east of the Colville River delta. These rocks dip gently seaward west of 146° W. Long, but are deformed into long, high-amplitude, east-northeast-striking folds to the east.