scholarly journals Depositional framework and regional correlation of pre-Carboniferous metacarbonate rocks of the Snowden Mountain area, central Brooks Range, Northern Alaska

1994 ◽  
Author(s):  
Julie A. Dumoulin ◽  
A.G. Harris
1986 ◽  
Vol 81 (7) ◽  
pp. 1728-1752 ◽  
Author(s):  
R. J. Newberry ◽  
J. T. Dillon ◽  
D. D. Adams
Keyword(s):  

1994 ◽  
Vol 68 (6) ◽  
pp. 1235-1240 ◽  
Author(s):  
Mary E. Baxter ◽  
Robert B. Blodgett

A new species of the genus Droharhynchia Sartenaer is established from lower Eifelian strata of west-central Alaska and the northwestern Brooks Range of Alaska. Droharhynchia rzhonsnitskayae n. sp. occurs in the Cheeneetnuk Limestone of the McGrath A-5 quadrangle, west-central Alaska, and the Baird Group of the Howard Pass B-5 quadrangle, northwestern Alaska. These occurrences extend the lower biostratigraphic range of both the genus and the subfamily Hadrorhynchiinae into the Eifelian. They also suggest close geographic proximity of the Farewell terrane of southwestern and west-central Alaska and the Arctic Alaska superterrane of northern Alaska during Devonian time.


2021 ◽  
pp. 120568
Author(s):  
John F. Slack ◽  
Ryan J. McAleer ◽  
Wayne C. Shanks ◽  
Julie A. Dumoulin
Keyword(s):  

2017 ◽  
Vol 88 (2) ◽  
pp. 169-178 ◽  
Author(s):  
Alistair J. Monteath ◽  
Maarten van Hardenbroek ◽  
Lauren J. Davies ◽  
Duane G. Froese ◽  
Peter G. Langdon ◽  
...  

AbstractHolocene tephrostratigraphy in Alaska provides independent chronology and stratigraphic correlation in a region where reworked old (Holocene) organic carbon can significantly distort radiocarbon chronologies. Here, we present new glass chemistry and chronology for Holocene tephras preserved in three Alaskan lakes: one in the eastern interior and two in the southern Brooks Range. Tephra beds in the eastern interior lake-sediment core are correlated with the White River Ash and the Hayes tephra set H (~4200–3700 cal yr BP), and an additional discrete tephra bed is likely from the Aleutian arc/Alaska Peninsula. Cryptotephras (nonvisible tephras) found in the Brooks Range include the informally named “Ruppert tephra” (~2700–2300 cal yr BP) and the Aniakchak caldera-forming event II (CFE II) tephra (~3600 cal yr BP). A third underlying Brooks Range cryptotephra is chemically indistinguishable from the Aniakchak CFE II tephra (4070–3760 cal yr BP) and is likely to be from an earlier eruption of the Aniakchak volcano.


1959 ◽  
Vol 25 (1) ◽  
pp. 94-105 ◽  
Author(s):  
John M. Campbell

AbstractApproximately 2400 stone and 77 bone and antler artifacts were obtained by extensive trenching of the Kayuk site, a large area on the banks of Kayuk Creek in Anaktuvuk Pass, Brooks Range, northern Alaska, where several Nunamiut Eskimo families now camp. No stratigraphy was noted and no structural features were encountered, but four fire areas were excavated. The most diagnostic artifact is the Kayuk point, a lanceolate form with finely executed parallel oblique flaking, which resembles most closely the Angostura point of the Great Plains. Other stone artifacts, some of which also exhibit the parallel oblique flaking, include blades, scrapers, angle burins, microblades, drills, and adz blades. Implements of bone and antler, mostly caribou, include harpoons, leister and fish spear prongs and barbs, and other forms common in recent and prehistoric Arctic sites. The Kayuk site is believed to have been a hunting camp used during caribou migrations through Anaktuvuk Pass by a prehistoric Eskimo group which probably wintered on the northern coast as do the modern Nunamiut. The Kayuk complex probably belongs somewhere in time between the Denbigh Flint complex and Ipiutak.


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