| North-Central Section–40th Annual Meeting (20–21 April 2006) | |
| Paper No. 6-6 | |
| Presentation Time: 9:40 AM-10:00 AM | ||
THE CORRELATION BETWEEN THE GEOPHYSICAL QUALITIES AND SOIL DISTURBANCES AT THE MUD LAKE SITE IN NORTHERN INDIANA | ||
|
BOUVRON, Christel M., University of Notre Dame, 211 Farley Hall, Notre Dame, IN 46556, cbouvron@nd.edu The Mud Lake site (12 Le 14), located in Northern Indiana is the site of two Middle Woodland mounds of the Goodall Tradition, and was excavated in 1999, 2003 and 2005 by a few groups of students from the University of Notre Dame. Two different methods of geophysical surveys were utilized: soil resistivity to locate certain parts of the site that contained unusual features, and gradiometry to test the amount of magnetivity in the ground. The results from resistivity and magnetic surveys performed at the east mound indicate a looted mound, while those from the west mound, which was excavated in 2003 and 2005, produced similar signals. However, the latter also displayed a higher amount of resistivity, which could be caused by a different type of soil, or instead indicate a natural topographic elevation, which is relatively unlikely due to the amount and nature of artifacts found from excavation works. Resistivity and magnetic survey results correlate with field results obtained from excavation work that includes artifact cataloging and the detailing of floor and wall profiles from E 99-100 N 98-104. Higher resistivity was detected just towards the west of around E 99-100 N 102 and pieces of bone were discovered here that may indicate part of a burial. | ||
|
North-Central Section–40th Annual Meeting (20–21 April 2006)
General Information for this Meeting | ||
| Session No. 6 Teaching and Practicing Geophysical Prospecting in Archaeology Student Center, University of Akron: Room 310 8:00 AM-11:00 AM, Thursday, 20 April 2006 Geological Society of America Abstracts with Programs, Vol. 38, No. 4, p. 10 | ||
© Copyright 2006 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions. | ||