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Research about northern Alaska

Source-linked reports with geographic coverage including northern Alaska.

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Habitat characteristics of polar bear terrestrial maternal den sites in northern Alaska

Polar bears ( Ursus maritimus ) give birth to and nurture their young in dens of ice and snow. During 1999-2001, we measured the structure of 22 dens on the coastal plain of northern Alaska after polar bear families had evacuated their dens in the spring. During the summers of 2001 and 2002, we revisited the sites of 42 maternal and autumn exploratory dens and recorded characteristics of the under-snow habitat. The structure of polar bear snow dens was highly variable. Most were simple chambers with a single entrance/egress tunnel. Others had multiple chambers and additional tunnels. Thickness of snow above and below dens was highly variable, but most dens were overlain by less than 1 m of snow. Dens were located on, or associated with, pronounced landscape features (primarily coastal and river banks, but also a lake shore and an abandoned oil field gravel pad) that are readily distinguished from the surrounding terrain in summer and catch snow in early winter. Although easily identified, den landforms in northern Alaska were more subtle than den habitats in many other parts of the Arctic. The structure of polar bear dens in Alaska was strikingly similar to that of dens elsewhere and has remained largely unchanged in northern Alaska for more than 25 years. Knowledge of den structure and site characteristics will allow resource managers to identify habitats with the greatest probability of holding dens. This information may assist resource managers in preventing negative impacts of mineral exploration and extraction on polar bears.

Alaska↗

The Kingak shale of northern Alaska—regional variations in organic geochemical properties and petroleum source rock quality

The Kingak Shale, a thick widespread rock unit in northern Alaska that ranges in age from Early Jurassic through Early Cretaceous, has adequate to good oil source rock potential. This lenticular-shaped rock unit is as much as 1200 m thick near the Jurassic shelf edge, where its present-day burial depth is about 5000 m. Kingak sediment, transported in a southerly direction, was deposited on the then marine continental shelf. The rock unit is predominantly dark gray Shale with some interbeds of thick sandstone and siltstone. The thermal maturity of organic matter in the Kingak Shale ranges from immature (<0.6% R 0 ) on the Barrow arch to postmature (>2.0% R 0 ) in the Colville basin toward the south. Its organic carbon and hydrogen contents are highest in the eastern part of northern Alaska south of and around the Kuparuk and Prudhoe Bay oil fields. Carbon isotope data of oils and rock extracts indicate that the Kingak Shale is a source of some North Slope oil, but is probably not the major source.

Alaska↗

Map showing paleocurrent and clast-size data from the Devonian-Mississippian Endicott Group, northern Alaska

The Devonian-Mississippian Endicott Group (Tailleur and others, 1967) is an important geologic unit in the Brooks Range of northern Alaska. It reflects a major tectonic event in the middle and late Paleozoic history of the North American Cordillera. Tailleur and Brosge (1970) interpreted the Endicott as a clastic wedge derived from land to the north during the Late Devonian and from land to the northeast during Early Mississippian, when a shallow sea transgressed the area. In the north-central and eastern parts of the range, the Endicott is composed of three formations, in ascending order, the Upper Devonian Hunt Fork Shale and Kanayut Conglomerate and the Lower Mississippian Kayak Shale; in the western part of the range, the stratigraphic relations of these formations with formations in the Endicott is uncertain. Donovan systematically collected paleocurrent and clast-size data from the Endicott Group along the Brooks Range for Mobil Oil Corporation in 1967 and 1968. In recognition of the general interest in the information, Mobil has permitted its release. I.L Tailleur summarized the regional geologic information.

Alaska↗

Phosphate deposits in northern Alaska

Deposits of low and medium grade phosphate rock were found recently at seven localities on the Arctic slope of Alaska. They were reported by field parties of the U.S. Geological Survey during the mapping of Naval Petroleum Reserve No. 4 and adjacent areas. The deposits are sedimentary in origin and are confined to a thin zone in the Lisburne group of Mississippian age. Six of the localities are in a narrow belt along the north front of the Brooks gang between the Anaktuvuk and Okokmilaga rivers. The seventh is near the Ipnavik River about 100 miles northwest of the Okokmilaga River. At all but two of these localities the zone of soft phosphatic rocks does not crop out extensively and samples of phosphate rock were collected chiefly from float or talus. Little or nothing is known about the thickness and extent of the deposits. Near Chandler Lake on the upper Kiruktagiak River and 11 miles west of at the head of Tiglukpuk Creek, the phosphatic zone is well-exposed. This paper is a preliminary report on the results of a detailed examination of the phosphatic zone in these two areas during the summer of 1953.

Alaska↗