Trade Networks and the Development of Local Status and Rank in Dallas Society
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Cherokee Ethnogenesis in Southwestern North Carolina
The following chapter is from: The Archaeology of North Carolina: Three Archaeological Symposia Charles R. Ewen – Co-Editor Thomas R. Whyte – Co-Editor R. P. Stephen Davis, Jr. – Co-Editor North Carolina Archaeological Council Publication Number 30 2011 Available online at: http://www.rla.unc.edu/NCAC/Publications/NCAC30/index.html CHEROKEE ETHNOGENESIS IN SOUTHWESTERN NORTH CAROLINA Christopher B. Rodning Dozens of Cherokee towns dotted the river valleys of the Appalachian Summit province in southwestern North Carolina during the eighteenth century (Figure 16-1; Dickens 1967, 1978, 1979; Perdue 1998; Persico 1979; Shumate et al. 2005; Smith 1979). What developments led to the formation of these Cherokee towns? Of course, native people had been living in the Appalachian Summit for thousands of years, through the Paleoindian, Archaic, Woodland, and Mississippi periods (Dickens 1976; Keel 1976; Purrington 1983; Ward and Davis 1999). What are the archaeological correlates of Cherokee culture, when are they visible archaeologically, and what can archaeology contribute to knowledge of the origins and development of Cherokee culture in southwestern North Carolina? Archaeologists, myself included, have often focused on the characteristics of pottery and other artifacts as clues about the development of Cherokee culture, which is a valid approach, but not the only approach (Dickens 1978, 1979, 1986; Hally 1986; Riggs and Rodning 2002; Rodning 2008; Schroedl 1986a; Wilson and Rodning 2002). In this paper (see also Rodning 2009a, 2010a, 2011b), I focus on the development of Cherokee towns and townhouses. Given the significance of towns and town affiliations to Cherokee identity and landscape during the 1700s (Boulware 2011; Chambers 2010; Smith 1979), I suggest that tracing the development of towns and townhouses helps us understand Cherokee ethnogenesis, more generally. -
CTT Economic Impact Study
THE POTENTIAL ECONOMIC IMPACTS OF THE PROPOSED CAROLINA THREAD TRAIL FINAL REPORT MARCH 2007 Submitted to: Catawba Lands Conservancy 105 West Morehead Street, Suite B Charlotte, NC 28202 Submitted by: Econsult Corporation th 6 Floor 3600 Market Street Philadelphia, PA 19104 and Greenways Incorporated 5850 Fayetteville Road, Suite 211 Durham, NC 27713 MarchTABLE 2007 OF CONTENTS A REGIONAL ECONOMIC IMPACT STUDY OF THE CAROLINA THREAD TRAIL Executive Summary i 1.0 Introduction 1 2.0 Potential Economic Benefits of the Carolina Thread Trail 4 2.1 Enhanced Property Values and Local Property Tax Revenues 5 2.2 Increased Tourism 7 2.3 Construction Investment Impacts 8 2.4 Business Expansion / Economic Development 10 2.5 Air and Water Quality 15 2.6 Increased Aggregate Recreation Value 21 2.7 Return on Investment 26 3.0 Summary and Conclusion 30 Appendix A. Enhanced Property Values 34 B. Economic And Fiscal Impact Model Methodology 46 C. Improved Water and Air Quality 49 March 2007 A REGIONAL ECONOMIC IMPACT STUDY OF THE CAROLINA THREAD TRAIL i EXECUTIVE SUMMARY The proposed Carolina Thread Trail (“the Trail”) will span approximately 500 miles across a 15- county region, including parts of both North and South Carolina. In addition to providing open space and enhanced recreational opportunities to residents and visitors, the Trail will be designed to “thread” communities together along routes designed by the communities themselves. The Trail is expected to help the region continue to compete aggressively with other rapidly growing and quickly developing metro areas of the country by providing local amenities for area residents, visitors, and businesses. -
THE MISSISSIPPIAN OCCUPATION of the SAVANNAH RIVER VALLEY Author(S): David G
THE MISSISSIPPIAN OCCUPATION OF THE SAVANNAH RIVER VALLEY Author(s): David G. Anderson, David J. Hally and James L. Rudolph Source: Southeastern Archaeology, Vol. 5, No. 1 (Summer 1986), pp. 32-51 Published by: Allen Press on behalf of the Southeastern Archaeological Conference Stable URL: http://www.jstor.org/stable/40713472 . Accessed: 02/10/2013 09:25 Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at . http://www.jstor.org/page/info/about/policies/terms.jsp . JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact [email protected]. Allen Press and Southeastern Archaeological Conference are collaborating with JSTOR to digitize, preserve and extend access to Southeastern Archaeology. http://www.jstor.org This content downloaded from 160.36.64.162 on Wed, 2 Oct 2013 09:25:14 AM All use subject to JSTOR Terms and Conditions THE MISSISSIPPIAN OCCUPATION OF THE SAVANNAH RIVER VALLEY David G. Anderson chronologicaland culturalsequence forthe period David J.Hally along much of the drainage;(b) the publicationof and major surveyand excavationreports from several areas of the workat several L. basin, including major James Rudolph moundand village sites; (c) the linkageof ethnoh- istoricand archaeologicalsite records;and (d) the initiationof diachronicanalyses encompassing both drainage-specificand regional political evolution, 1970, in the Before knowledgeof Mississippian occupations subsistencetrends, mortuary practices, and settle- SavannahRiver came isolated, re- Valley from oftenbrief mentpatterning. -
Plant Remains from the Smokemont Site in the Appalachian Mountains of North Carolina
University of Tennessee, Knoxville TRACE: Tennessee Research and Creative Exchange Masters Theses Graduate School 8-2013 Plant Remains from the Smokemont Site in the Appalachian Mountains of North Carolina Gabrielle Casio Purcell [email protected] Follow this and additional works at: https://trace.tennessee.edu/utk_gradthes Part of the Archaeological Anthropology Commons Recommended Citation Purcell, Gabrielle Casio, "Plant Remains from the Smokemont Site in the Appalachian Mountains of North Carolina. " Master's Thesis, University of Tennessee, 2013. https://trace.tennessee.edu/utk_gradthes/2447 This Thesis is brought to you for free and open access by the Graduate School at TRACE: Tennessee Research and Creative Exchange. It has been accepted for inclusion in Masters Theses by an authorized administrator of TRACE: Tennessee Research and Creative Exchange. For more information, please contact [email protected]. To the Graduate Council: I am submitting herewith a thesis written by Gabrielle Casio Purcell entitled "Plant Remains from the Smokemont Site in the Appalachian Mountains of North Carolina." I have examined the final electronic copy of this thesis for form and content and recommend that it be accepted in partial fulfillment of the equirr ements for the degree of Master of Arts, with a major in Anthropology. Kandace D. Hollenbach, Major Professor We have read this thesis and recommend its acceptance: Gerald Schroedl, Michael Logan Accepted for the Council: Carolyn R. Hodges Vice Provost and Dean of the Graduate School (Original signatures are on file with official studentecor r ds.) i Plant Remains from the Smokemont Site in the Appalachian Mountains of North Carolina A Thesis Presented for the Master of Arts Degree The University of Tennessee, Knoxville Gabrielle Casio Purcell August 2013 ii Copyright © 2013 by Gabrielle Casio Purcell All rights reserved. -
2016 Athens, Georgia
SOUTHEASTERN ARCHAEOLOGICAL CONFERENCE PROCEEDINGS & ABSTRACTS OF THE 73RD ANNUAL MEETING OCTOBER 26-29, 2016 ATHENS, GEORGIA BULLETIN 59 2016 BULLETIN 59 2016 PROCEEDINGS & ABSTRACTS OF THE 73RD ANNUAL MEETING OCTOBER 26-29, 2016 THE CLASSIC CENTER ATHENS, GEORGIA Meeting Organizer: Edited by: Hosted by: Cover: © Southeastern Archaeological Conference 2016 TABLE OF CONTENTS THE CLASSIC CENTER FLOOR PLAN……………………………………………………...……………………..…... PREFACE AND ACKNOWLEDGEMENTS…………………………………………………………………….…..……. LIST OF DONORS……………………………………………………………………………………………….…..……. SPECIAL THANKS………………………………………………………………………………………….….....……….. SEAC AT A GLANCE……………………………………………………………………………………….……….....…. GENERAL INFORMATION & SPECIAL EVENTS SCHEDULE…………………….……………………..…………... PROGRAM WEDNESDAY, OCTOBER 26…………………………………………………………………………..……. THURSDAY, OCTOBER 27……………………………………………………………………………...…...13 FRIDAY, OCTOBER 28TH……………………………………………………………….……………....…..21 SATURDAY, OCTOBER 29TH…………………………………………………………….…………....…...28 STUDENT PAPER COMPETITION ENTRIES…………………………………………………………………..………. ABSTRACTS OF SYMPOSIA AND PANELS……………………………………………………………..…………….. ABSTRACTS OF WORKSHOPS…………………………………………………………………………...…………….. ABSTRACTS OF SEAC STUDENT AFFAIRS LUNCHEON……………………………………………..…..……….. SEAC LIFETIME ACHIEVEMENT AWARDS FOR 2016…………………….……………….…….…………………. Southeastern Archaeological Conference Bulletin 59, 2016 ConferenceRooms CLASSIC CENTERFLOOR PLAN 6 73rd Annual Meeting, Athens, Georgia EVENT LOCATIONS Baldwin Hall Baldwin Hall 7 Southeastern Archaeological Conference Bulletin -
Dot 16550 DS1.Pdf
DRAFT NOTES ON THE SEMINOLE TRAIL (U.S . 29) Ill VIRGIBU Howard Newloa, Jr. October 28, 1976 According to McCary the indians that inhabited Virginia prior to English settlement were linguistically Algonquian, 'Iroquoian and Siouan- The general areas are indicated on his map attached as Figure 1.") Harrison in his extensive work on Old Prince William which extended as far west as Fauquier County likewise describes the indians as Algonquian and Iroquois. Specific tribes associated with Piedmont Virginia are largeiy Sapoai, Hanahuac, Tutelo, and Occaneechi. No mention is made in any county or state histories consulted of habitation or travel in the Virginia area by Seminoles. Despite this, U.S. 29 between Warrenton and the Horth Carolina line in 1928 was designated "TIie Seminole Trail". This designation was apprwed as Senate Bill 64 on February 16, 1928, which stated 1. Be it enacted by the general assembly of Virginia that that part of the Virginia State highway system, beginning at the Borth Carolina line and leading through Danville , Chatham, Alta Vista, Lynchburg, Amherst, Lovingston, Charlottesville, Ruckersville, Nadison and Culpeper to Warrenton, be, and is hereby designated and shall. be, here- after , known as the "Seminole Trail.". No supporting arguments were found in the Senate Journal or other public documents in the University of Virginia Library. Like- wise no documentation or descriptions were found in tourist oriented publications. Thus a question remains as to the origin and validity of the designation. Attempts to find supporting evidence in published sources on American Indians were likewise unsuccessful. The mo8t extensive -1- documentation of Southeastern indian trails was published by Myer in 1928!3) His map is attached as Figure 2. -
Upper Mon River Trail
Upper Monongahela River Water Trail Map and Guide Water trails are recreational waterways on a lake, river, or ocean between specific locations, containing access points and day-use and/or camping sites for the boating public. Water trails emphasize low-impact use and promote stewardship of the resources. Explore this unique West Virginia and Pennsylvania water trail. For your safety and enjoyment: Always wear a life jacket. Obtain proper instruction in boating skills. Know fishing and boating regulations. Be prepared for river hazards. Carry proper equipment. THE MONONGAHELA RIVER The Monongahela River, locally know as “the Mon,” forms at the confluence of the Tygart and West Fork Rivers in Fairmont West Virginia. It flows north 129 miles to Pittsburgh, Pennsylvania, where it joins the Allegheny River to form the Ohio River. The upper section, which is described in this brochure, extends 68 miles from Fairmont to Maxwell Lock and Dam in Pennsylvania. The Monongahela River formed some 20 million years ago. When pioneers first saw the Mon, there were many places where they could walk across it. The Native American named the river “Monongahela,” which is said to mean “river with crumbling or falling banks.” The Mon is a hard-working river. It moves a large amount of water, sediment, and freight. The average flow at Point Marion is 4,300 cubic feet per second. The elevation on the Upper Mon ranges from 891 feet in Fairmont to 763 feet in the Maxwell Pool. PLANNING A TRIP Trips on the Mon may be solitary and silent, or they may provide encounters with motor boats and water skiers or towboats moving barges of coal or limestone. -
The Common Field Mississippian Site(23SG100), As Uncovered by the 1979 Mississippi River Flood Richard E
The Common Field Mississippian Site(23SG100), as Uncovered by the 1979 Mississippi River Flood Richard E. Martens Two of the pictures I took during an early visit to the he Common Field site occurs near the bluffs in the site are shown in Figure 1. The first shows Mound A, the TMississippi River floodplain 3 km south of St. Gen- largest of the six then-existing mounds. The nose of my evieve and approximately 90 km south of St. Louis. It is brand-new 1980 Volkswagen parked on the farm road is a large Mississippian-period site that once had as many as in the lower right corner of the picture. The second photo eight mounds (Bushnell 1914:666). It was long considered shows the outline of a burned house structure typical of to be an unoccupied civic-ceremonial center because very many evident across the site. Although it has been noted few surface artifacts were found. This all changed due that many people visited the site shortly after the flood, I to a flood in December 1979, when the Mississippi River did not meet anyone during several visits in 1980 and 1981. swept across the Common Field site. The resulting erosion I subsequently learned that Dr. Michael O’Brien led removed up to 40 cm of topsoil, exposing: a group of University of Missouri (MU) personnel in a [a] tremendous quantity of archaeological material limited survey and fieldwork activity in the spring of 1980. including ceramic plates, pots and other vessels, articu- The first phase entailed aerial photography (black-and- lated human burials, well defined structural remains white and false-color infrared) of the site. -
A Spatial and Elemental Analyses of the Ceramic Assemblage at Mialoquo (40Mr3), an Overhill Cherokee Town in Monroe County, Tennessee
University of Tennessee, Knoxville TRACE: Tennessee Research and Creative Exchange Masters Theses Graduate School 12-2019 COALESCED CHEROKEE COMMUNITIES IN THE EIGHTEENTH CENTURY: A SPATIAL AND ELEMENTAL ANALYSES OF THE CERAMIC ASSEMBLAGE AT MIALOQUO (40MR3), AN OVERHILL CHEROKEE TOWN IN MONROE COUNTY, TENNESSEE Christian Allen University of Tennessee, [email protected] Follow this and additional works at: https://trace.tennessee.edu/utk_gradthes Recommended Citation Allen, Christian, "COALESCED CHEROKEE COMMUNITIES IN THE EIGHTEENTH CENTURY: A SPATIAL AND ELEMENTAL ANALYSES OF THE CERAMIC ASSEMBLAGE AT MIALOQUO (40MR3), AN OVERHILL CHEROKEE TOWN IN MONROE COUNTY, TENNESSEE. " Master's Thesis, University of Tennessee, 2019. https://trace.tennessee.edu/utk_gradthes/5572 This Thesis is brought to you for free and open access by the Graduate School at TRACE: Tennessee Research and Creative Exchange. It has been accepted for inclusion in Masters Theses by an authorized administrator of TRACE: Tennessee Research and Creative Exchange. For more information, please contact [email protected]. To the Graduate Council: I am submitting herewith a thesis written by Christian Allen entitled "COALESCED CHEROKEE COMMUNITIES IN THE EIGHTEENTH CENTURY: A SPATIAL AND ELEMENTAL ANALYSES OF THE CERAMIC ASSEMBLAGE AT MIALOQUO (40MR3), AN OVERHILL CHEROKEE TOWN IN MONROE COUNTY, TENNESSEE." I have examined the final electronic copy of this thesis for form and content and recommend that it be accepted in partial fulfillment of the equirr ements for the degree of Master of Arts, with a major in Anthropology. Kandace Hollenbach, Major Professor We have read this thesis and recommend its acceptance: Gerald Schroedl, Julie Reed Accepted for the Council: Dixie L. -
Hclassification
Form No. 10-300 (Rev. 10-74) UNITED STAThSDhPARTMHNT OF THE INTERIOR NATIONAL PARK SERVICE NATIONAL REGISTER OF HISTORIC PLACES INVENTORY -- NOMINATION FORM SEE INSTRUCTIONS IN HOW TO COMPLETE NATIONAL REGISTER FORMS ____________TYPE ALL ENTRIES - COMPLETE APPLICABLE SECTIONS______ I NAME HISTORIC Long Island of the Holston AND/OR COMMON Long Island of the Holston LOCATION STREET& NUMBER South Fork of the Holston Elver _NOT FOR PUBLICATION CITY, TOWN CONGRESSIONAL DISTRICT Kingsport __. VICINITY OF 1st STATE CODE COUNTY CODE Tennessee 047 Sullivan 16^ HCLASSIFICATION CATEGORY OWNERSHIP STATUS PRESENT USE ^DISTRICT —PUBLIC -^OCCUPIED X.AGRICULTURE —MUSEUM _ BUILDING(S) ^.PRIVATE —UNOCCUPIED X-COMMERCIAL —PARK —STRUCTURE —BOTH _ WORK IN PROGRESS —EDUCATIONAL ^r^RIVATE RESIDENCE —SITE PUBLIC ACQUISITION ACCESSIBLE —ENTERTAINMENT —RELIGIOUS —OBJECT _IN PROCESS •^TYES: RESTRICTED —GOVERNMENT —SCIENTIFIC _ BEING CONSIDERED _ YES: UNRESTRICTED X-INDUSTRIAL —TRANSPORTATION X?NO _ MILITARY —OTHER: [OWNER OF PROPERTY NAME SEE CONTINUATION SHEET STREETS. NUMBER CITY, TOWN STATE __ VICINITY OF LOCATION OF LEGAL DESCRIPTION COURTHOUSE, REGISTRY OF DEEDS,ETC. Registry of Deeds STREET& NUMBER Sullivan County Court House CITY, TOWN STATE Blountville Tennessee I REPRESENTATION IN EXISTING SURVEYS TITLE Inventory of Historic Assets DATE in progress — FEDERAL ?_STATE —COUNTY —LOCAL DEPOSITORY FOR SURVEY RECORDS Tennessee Historical Commission CITY, TOWN STATE Nashville Tennessee DESCRIPTION CONDITION CHECK ONE CHECK ONE -EXCELLENT X&ETERIORATED east _UNALTERED X.QRIGINALSITE west -RUINS XALTERED _MOVED DATE. _FA)R _UNEXPOSED DESCRIBETHE PRESENT AND ORIGINAL (IF KNOWN) PHYSICAL APPEARANCE Long Island of the Holston is located along the South Fork of the Holston River just east of the junction of the North and South Forks and immediately south of the city of Kingsport, Tennessee. -
Paddler's Guide to Civil War Sites on the Water
Southeast Tennessee Paddler’s Guide to Civil War Sites on the Water If Rivers Could Speak... Chattanooga: Gateway to the Deep South nion and Confederate troops moved into Southeast Tennessee and North Georgia in the fall of 1863 after the Uinconclusive Battle of Stones River in Murfreesboro, Tenn. Both armies sought to capture Chattanooga, a city known as “The Gateway to the Deep South” due to its location along the he Tennessee River – one of North America’s great rivers – Tennessee River and its railroad access. President Abraham winds for miles through Southeast Tennessee, its volume Lincoln compared the importance of a Union victory in Tfortified by gushing creeks that tumble down the mountains Chattanooga to Richmond, Virginia - the capital of the into the Tennessee Valley. Throughout time, this river has Confederacy - because of its strategic location on the banks of witnessed humanity at its best and worst. the river. The name “Tennessee” comes from the Native American word There was a serious drought taking place in Southeast Tennessee “Tanasi,” and native people paddled the Tennessee River and in 1863, so water was a precious resource for soldiers. As troops its tributaries in dugout canoes for thousands of years. They strategized and moved through the region, the Tennessee River fished, bathed, drank and traveled these waters, which held and its tributaries served critical roles as both protective barriers dangers like whirlpools, rapids and eddies. Later, the river was and transportation routes for attacks. a thrilling danger for early settlers who launched out for a fresh The two most notorious battles that took place in the region start in flatboats. -
The Late Mississippian Period (AD 1350-1500) - Draft
SECTION IV: The Mississippian Period in Tennessee Chapter 12: The Late Mississippian Period (AD 1350-1500) - Draft By Michaelyn Harle, Shannon D. Koerner, and Bobby R. Braly 1 Introduction Throughout the Mississippian world this time period appears to be a time of great social change. In eastern Tennessee, Dallas Phase sites further elaborated on the Mississippian lifeway, becoming highly organized and home to political leaders. Settlements were sometimes quite extensive (i.e., the Dallas, Toqua, and Ledford Island sites with deep middens, often a palisade wall, sometimes with bastions, densely packed domestic structures, and human interments throughout the village area and also in mounds. Elsewhere in the region, there is evidence that much of West Tennessee and parts of the Cumberland-Tennessee valley were either abandoned by Mississippian societies or so fundamentally reorganized that they were rendered archaeologically invisible. This abandonment appears to be part of a larger regional trend of large portions of the Central Mississippi Valley, often referred to as the vacant quarter. A number of motives for this abandonment have been provided including the dissolution of Cahokia, increased intra- regional warfare, and environmental shifts associated with the onslaught of the Little Ice Age (Meeks 2006; Cobb and Butler 2002; Williams 1983, 1990). This two sides of the continium is important since it gives us a more microscopic glimpse of what was being played out in the larger pan-Mississippian stage. Regional and temporal refinements that are currently in progress gives us a unique perspective into the similarities and differences in which Tennessee Mississippian societies reacted to this unstable period.