SSSAJ Grow Your Career with SSSA
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published in Soil Sci Soc Am J 43:558-564 (1979)
© 1979 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
This Article
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Bliley, D. J.
Right arrow Articles by Pettry, D. E.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Bliley, D. J.
Right arrow Articles by Pettry, D. E.
Agricola
Right arrow Articles by Bliley, D. J.
Right arrow Articles by Pettry, D. E.

Carolina Bays on the Eastern Shore of Virginia1

D. J. Bliley and D. E. Pettry2

ABSTRACT

Carolina bays were analyzed on the Eastern Shore of Virginia utilizing infrared imagery and pedologic techniques. Over 160 bays were delineated thus indicating they are major landforms in the area. Bays differed from those reported in other regions by being less elliptical, more westerly oriented, and lacking well-developed rims in any specific quadrant. Bay location and size are apparently controlled by landscape and sandy parent materials as evidenced by association with less distinct natural depressions with similar orientation as the related geomorphic urface. Soils on bays of recent surfaces have weaker profile development compared to Pleistocene upland bays. More than one period of bay formation is suggested by differential pedogenic development and geomorphic positions. Data indicate Carolina bays were formed by the alteration of poorly drained areas on undissected Coastal Plain interfluves. Wind and waves are suggested as factors in bay formation based on well-sorted sands of elevated rims, "dune-like" character, and silt content of possible aeolian origin.


NOTES

1 Research was conducted at the Department of Agronomy, Virginia Polytechnic Institute and State University, Blacksburg, VA 24061. Supported in part by National Aeronautics and Space Administration-Wallops Flight Center, VA. (NASA Contract NAS 6-1863). Presented before Div. S-5, Soil Sci. Soc. of Am., Chicago, Ill., 11 Nov. 1974.

2 Soil Scientist, Soil Conservation Service, Smithfield, N. C., and Professor Soil Science, Department of Agronomy, Mississippi State Univ., Mississippi State, MS. 39762, respectively.

Received for publication June 19, 1978. Accepted for publication December 22, 1978.







HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Vadose Zone Journal Journal of Plant Registrations
Journal of Natural Resources
and Life Sciences Education
Journal of
Environmental Quality
Copyright © 1979 by the Soil Science Society of America.