Sagavanirktok Formation

Unit symbol: Tsf
Age range Tertiary, Miocene to Paleocene (59.2 to 3.6 Ma)
Lithology: Sedimentary
Group name: Sagavanirktok Formation
Mostly nonmarine, poorly consolidated siltstone, sandstone, conglomerate and lignite of the North Slope of Alaska and present only east of the Colville River. Divided into four members, in descending stratigraphic order: Nuwok, Franklin Bluffs, White Hills, and Sagwon Members. Unit consists of northeasterly prograding, upward-fining sequences that have basal fluvial conglomerate and coarse sandstone grading to mudstone that is commonly bentonitic and contains lignite (Mull and others, 2003). Mull and others (2003) revised the original definition of the Sagwon Member to exclude the lower coal-bearing beds at Sagwon Bluffs (informal name for bluff located along Sagavanirktok River opposite the Sagwon airstrip in the central Sagavanirktok quadrangle), concluding that they more properly belong to the Prince Creek Formation; they defined the base of the Sagwon Member—and therefore the base of the Sagavanirktok Formation—as a white-weathering sandstone and conglomerate that caps ridges in the northern Brooks Range foothills. Conglomerate clasts are generally white quartz, black chert, and light-gray quartzitic sandstone and minor pale-green chert. Sagwon Member is late Paleocene in age (Mull and others, 2003). White Hills Member is lithologically similar, but the finer-grained upper part is poorly exposed. Conglomerate clasts are generally gray quartzitic sandstone, white quartz, black chert, and leached light-gray siliceous tuff and lesser gray to pale-green and maroon to red chert. Its age is considered late Paleocene to early Eocene. Franklin Bluffs Member definition was also revised by Mull and others (2003); its lower part consists of white- to pink-weathering, poorly consolidated sandstone and conglomerate; conglomerate clasts are predominantly black chert and lesser white and gray quartz. Its upper part, generally not exposed and primarily known from well data, consists of poorly consolidated thin-bedded mudstone and siltstone. Age is probably early Eocene to Miocene (Mull and others, 2003) and the fauna suggests a nearshore or estuarine environment. The Nuwok Member is only exposed in northeastern Alaska and consists of unconsolidated pebbly sandstone or conglomerate overlain by pebbly mudstone (Detterman and others, 1975). Its age is late Miocene to Pliocene and character of the sediments and fauna suggest a nearshore or beach environment. In the Harrison Bay quadrangle, Carter and Galloway (2005) report a Paleocene map unit (Tsg) assigned to the Sagavanirktok Formation where “* * * deposits consist of moderately to poorly consolidated conglomerate, sand, gravelly sand, and pebbly shale with thin coal beds and locally common lignitized logs”

Source map information

Source map Wartes, M.A., Wallace, W.K., Loveland, A.M., Gillis, R.J., Decker, P.L., Reifenstuhl, R.R., Delaney, P.R., LePain, D.L., and Carson, E.C., 2011, Geologic map of the Kavik River area, northeastern Brooks Range, Alaska: Alaska Division of Geological and Geophysical Surveys Report of Investigation 2011-3A, 14 p., 1 sheet, scale 1:63,360.
Symbol Tslm
Unit name Brookian Megasequence - LOWER SAGAVANIRKTOK FORMATION, MIDDLE PART
Description Light-gray- to tan-weathering, dominantly very-fine- to fine-grained, moderately sorted, salt-and-pepper sandstone. Tabular to wavy non-parallel beds range from 2 to 35 cm thick and include burrow-mottled massive to plane-parallel laminated facies and locally well developed low-angle and hummocky cross-stratification. A variable, but locally strong hydrocarbon odor is noted in many beds. Medium-gray-weathering, chippy siltstone commonly preserves load structures at the contact with overlying sandstone beds. Granule and pebble stringers are present, expanding locally into irregular conglomerate beds up to 35 cm thick. Carbonized wood fragments are abundant in some beds. Interval is interpreted as lower shoreface to delta front, possibly including small distributary channel deposits. Only occurrence is in the northeast corner of the map area along the west bank of the Canning River, where 120 m of section is exposed in the footwall of the Kavik fault. Assignment is based principally on projections from nearby Canning River Unit B-1 well and available seismic data; equivalent to an unnamed tongue illustrated in well log cross sections by Molenaar and others (1986) and Bird (1999); total thickness of 846 m is calculated for this tongue in the Beli 1 well (north-central part of map; Nelson and others, 1999)
Lithology Sedimentary

Correlated geologic units

Label Tswh
Description Sagavanirktok Formation, White Hills Member
Geologic age Late-Paleocene to Early-Eocene
Geologic setting Sedimentary, continental
Lithology Form Importance
Conglomerate < Clastic < Sedimentary Bed Major
Quartzose-sandstone < Sandstone < Clastic < Sedimentary Bed Indeterminate, major