Search engine for discovering works of Art, research articles, and books related to Art and Culture
ShareThis
Javascript must be enabled to continue!

A Perspective on Arkansas Basin and Ozark Highland Prehistory

View through CrossRef
It is, from time to time, valuable to reassess and perhaps shed new light on long-held perspectives. In "The 'Northern Caddoan Area' was not Caddoan," Frank Schambach provides a provocative reinterpretation of the archaeology of the Arkansas Basin and Ozark Highland regions of Oklahoma, Arkansas, and Missouri. While certain comments in this paper have merit and deserve deeper consideration, the central theme and supporting arguments are severely flawed, both from conceptual and data points of view. Schambach's central argument is that there were no Caddoans in the Arkansas Basin and Ozark Highlands north of Spiro. To make this point he asserts that the only Caddoan site north of the Ouachita Mountains is the Brown Mound group at Spiro. All the other sites in the region, including the Craig Mound group at Spiro, are not Caddoan, but are instead a currently undefined Mississippian manifestation. Schambach's scenario goes. something like this: Mississippians moved up the Arkansas River valley in the early,Mississippian Period (presumably in the Harlan Phase, A.O. 850-1250), through western Arkansas to eastern Oklahoma where they displaced the Caddoans living at the Brown Mound group. The Caddoans moved back south to the Ouachita Mountains. The Mississippians, including "people of the Plum Bayou culture ... the Spiro phase [A.O. 1250-1450]" then built Craig Mound at Spiro while possibly operating a trade system "to supply buffalo meat arid hides to the rapidly growing and increasingly protein poor and clothing poor Mississippian populations. . .. " to the east. Later, the Mississippians, who were probably ancestral Tunica, retreated back down the Arkansas River "to south of Dardenelle, where De Soto encountered them in 1541." The Caddoans then returned to the Spiro area to become the people of the Fort Coffee Phase (A.O. 1450-1500s). This sequence of events is a fascinating reinterpretation of regional culture history, unfortunately it falls flat when confronted by either contemporary theory or the data.
Title: A Perspective on Arkansas Basin and Ozark Highland Prehistory
Description:
It is, from time to time, valuable to reassess and perhaps shed new light on long-held perspectives.
In "The 'Northern Caddoan Area' was not Caddoan," Frank Schambach provides a provocative reinterpretation of the archaeology of the Arkansas Basin and Ozark Highland regions of Oklahoma, Arkansas, and Missouri.
While certain comments in this paper have merit and deserve deeper consideration, the central theme and supporting arguments are severely flawed, both from conceptual and data points of view.
Schambach's central argument is that there were no Caddoans in the Arkansas Basin and Ozark Highlands north of Spiro.
To make this point he asserts that the only Caddoan site north of the Ouachita Mountains is the Brown Mound group at Spiro.
All the other sites in the region, including the Craig Mound group at Spiro, are not Caddoan, but are instead a currently undefined Mississippian manifestation.
Schambach's scenario goes.
something like this: Mississippians moved up the Arkansas River valley in the early,Mississippian Period (presumably in the Harlan Phase, A.
O.
850-1250), through western Arkansas to eastern Oklahoma where they displaced the Caddoans living at the Brown Mound group.
The Caddoans moved back south to the Ouachita Mountains.
The Mississippians, including "people of the Plum Bayou culture .
the Spiro phase [A.
O.
1250-1450]" then built Craig Mound at Spiro while possibly operating a trade system "to supply buffalo meat arid hides to the rapidly growing and increasingly protein poor and clothing poor Mississippian populations.
.
.
" to the east.
Later, the Mississippians, who were probably ancestral Tunica, retreated back down the Arkansas River "to south of Dardenelle, where De Soto encountered them in 1541.
" The Caddoans then returned to the Spiro area to become the people of the Fort Coffee Phase (A.
O.
1450-1500s).
This sequence of events is a fascinating reinterpretation of regional culture history, unfortunately it falls flat when confronted by either contemporary theory or the data.

Related Results

Geology and Ground-Water Resources of Hamilton and Kearny Counties, Kansas
Geology and Ground-Water Resources of Hamilton and Kearny Counties, Kansas
This report describes the geography, geology, and ground-water resources of Hamilton and Kearny counties in southwestern Kansas. The area embraces a total of 51.5 townships, or 1,8...
The Genetic Mechanism of the Sequence Stratigraphy of the Rift Lacustrine Basin in Jiyang Depression, East China
The Genetic Mechanism of the Sequence Stratigraphy of the Rift Lacustrine Basin in Jiyang Depression, East China
Abstract Through the studies of sequence stratigraphy of early Tertiary in the east part of Jiyang depression, the characteristics of sequence evolution in contin...
A method to quantify mouse coat-color proportions
A method to quantify mouse coat-color proportions
Coat-color proportions and patterns in mice are used as assays for many processes such as transgene expression, chimerism, and epigenetics. In many studies, coat-color readouts are...
Paddlefish Management, Propagation, and Conservation in the 21st Century
Paddlefish Management, Propagation, and Conservation in the 21st Century
<em>Abstract</em>.— Four special commercial fishing seasons (5–10 d) with mandatory check stations were used to closely monitor the harvest and exploitation of paddlefi...
Tectono-thermal evolution of the Junggar Basin, NW China: constraints from R o and apatite fission track modelling
Tectono-thermal evolution of the Junggar Basin, NW China: constraints from R o and apatite fission track modelling
The thermal evolution of the Junggar Basin, northwest China, was evaluated based on the thermal modelling results of 59 wells by using vitrinite reflectance (R o ...
Landscape Influences on Stream Habitats and Biological Assemblages
Landscape Influences on Stream Habitats and Biological Assemblages
<em>Abstract.</em>—We reviewed native fish zoogeography in 22 major tributary basins of the Missouri River basin in the Great Plains geomorphic province and used island...

Back to Top