ON THE DISTRIBUTION AND HISTORY OF SOD TABLES IN THE EXPOSURE AREA OF THE WHITE RIVER GROUP, NORTHERN GREAT PLAINS, USA

2016 ◽  
Author(s):  
Patrick Burkhart ◽  
◽  
Paul Baldauf ◽  
Kaitlyn Marie Bouch ◽  
Maraina Miles ◽  
...  
2020 ◽  
Author(s):  
Paul Baldauf ◽  
◽  
Gregory Baker ◽  
Patrick Burkhart ◽  
Allen Gontz ◽  
...  

2019 ◽  
Vol 53 (1) ◽  
pp. 157-193
Author(s):  
Taylor Spence

Abstract This article reexamines a highly public dispute between a powerful and well-connected Episcopal bishop and his missionary priest, men both central to the government’s campaign of war and assimilation against Indigenous Peoples in the Northern Great Plains of the nineteenth-century United States. The bishop claimed that the priest had engaged in sexual intercourse with a Dakota woman named “Scarlet House,” and used this allegation to remove the priest from his post. No historian ever challenged this claim and asked who Scarlet House was. Employing Dakota-resourced evidence, government and church records, linguistics, and onomastics, this study reveals that in actuality there was no such person as Scarlet House. Furthermore, at the time of the incident, the person in question was not a woman but a child. The church created a fictional personage to cover up what was taking place at the agency: sexual violence against children. After “naming” this violence, this article makes four key historical contributions about the history of US settler colonialism: It documents Dakota Peoples’ agency, by demonstrating how they adapted their social structures to the harrowing conditions of the US mission and agency system. It situates the experiences of two Dakota families within the larger context of settler-colonial conquest in North America, revealing the generational quality of settler-colonial violence. It shows how US governmental policies actually enabled sexual predation against children and women. And, it argues that “naming violence” means both rendering a historical account of the sexual violence experienced by children and families in the care of the US government and its agents, as well as acknowledging how this violence has rippled out through communities and across generations.


The Holocene ◽  
2011 ◽  
Vol 21 (8) ◽  
pp. 1203-1216 ◽  
Author(s):  
William O. Hobbs ◽  
Sherilyn C. Fritz ◽  
Jeffery R. Stone ◽  
Joseph J. Donovan ◽  
Eric C. Grimm ◽  
...  

Sediment records from closed-basin lakes in the Northern Great Plains (NGP) of North America have contributed significantly to our understanding of regional paleoclimatology. A high-resolution (near decadal) fossil diatom record from Kettle Lake, ND, USA that spans the last 8500 cal. yr BP is interpreted in concert with percent abundance of aragonite in the sediment as an independent proxy of groundwater flow to the lake (and thus lake water level). Kettle Lake has been relatively fresh for the majority of the Holocene, likely because of the coarse substrata and a strong connection to the underlying aquifer. Interpretation of diatom assemblages in four groups indicative of low to high groundwater flow, based on the percent of aragonite in sediments, allow interpretations of arid periods (and probable meromictic lake conditions) that could not be detected based on diatom-based salinity reconstructions alone. At the centennial–millennial scale, the diatom record suggests humid/wet periods from 8351 to 8088, 4364 to 1406 and 872 to 620 cal. yr BP, with more arid periods intervening. During the last ~ 4500 years, decadal–centennial scale periods of drought have taken place, despite the generally wetter climate. These droughts appear to have had similar impacts on the Kettle Lake hydrology as the ‘Dust Bowl’ era droughts, but were longer in duration.


2019 ◽  
Vol 37 ◽  
pp. 14-24
Author(s):  
P.E. Baldauf ◽  
P.A. Burkhart ◽  
P.R. Hanson ◽  
M. Miles ◽  
A. Larsen

1993 ◽  
Vol 58 (4) ◽  
pp. 698-710 ◽  
Author(s):  
Robert J. Hoard ◽  
John R. Bozell ◽  
Steven R. Holen ◽  
Michael D. Glascock ◽  
Hector Neff ◽  
...  

High-quality cryptocrystalline silicates from the Oligocene-age White River Group of the central Great Plains (referred to here as White River Group Silicates [WRGS]) were widely used prehistorically for chipped-stone tools. There are three known source areas for WRGS: Flattop Butte in northeastern Colorado, Table Mountain in east central Wyoming, and the White River Badlands of South Dakota. Specimens from these sources are often visually indistinguishable, making it difficult to specify the source of WRGS from nonquarry archaeological sites. Using a quantitative method—neutron-activation analysis—these sources were differentiated. The sources of WRGS in two Central Plains archaeological sites also were determined using this technique. The results show that the technique has important implications for studies of prehistoric mobility and for the refinement of cultural-historical affiliation.


1996 ◽  
Vol 135 (1) ◽  
pp. 115 ◽  
Author(s):  
Charles Edward Umbanhowar

2017 ◽  
Author(s):  
Paul Baldauf ◽  
◽  
Patrick Burkhart ◽  
P.R. Hanson ◽  
Maraina Miles ◽  
...  

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