[meteorite-list] Carolina Bays, etc. meteor
From: Keith <littlejo_at_meteoritecentral.com>
Date: Thu Apr 22 10:08:31 2004 Message-ID: <Pine.SOL.4.33.0209251555420.19941-100000_at_katie.vnet.net> On Wed, 25 Sep 2002 14:04:50 -0400, Rothery Melvin ann.melvin_at_sympatico.ca wrote: >Most of the authorities with which I am familiar >discount the possibility of an impact along the >Carolinas and Virginia coast, excepting Chesapeake >Bay; however, there are those who prefer otherwise >and one such is Rufus Johnson who has written a small >speculative pamphlet, The comet of doom, (Roanoke >Rapids, NC: Kerr Books; 2001), which does not >convince me. There are a number of recently published studies that have looked at the internal structure using cores and ground-penetrating radar and dated the age of the Carolina Bays. This is research, which is ongoing, has found nothing in the way of evidence that supports the impact hypotheses for their origin and provides a lot evidence for them being oriented lakes whose current morphology is the results of 100,000 to 80,000 years modification by erosion and accretion along the shorelines of these landforms. If nothing else, the morphology of these bays have been so altered over the Pleistocene that their current morphology cannot be used to argue for an impact origin. For example, Optically Stimulated Luminescence (OSL) dating of the sand composing the rims of the Carolina Bays showed that they formed at various times between 80,000 to 100,000 years ago. For a summary this recent research go read "Age and Climatic Correlates of Carolina Bays and Inland Dunes of the South Atlantic Coastal Plain: New Data" at http://www.cla.sc.edu/sciaa/srs.html On that web page it is stated: "On the U.S. Department of Energy's Savannah River Site (SRS), adjacent to the Savannah River in the Upper Coastal Plain, two OSL dates from the rim of Flamingo Bay indicate that the bay formed initially at 108.7 1 10.9 ka B.P. and was rejuvenated at 40.3 1 4.0 ka B.P. A single date from Bay 40 indicates that it formed at 77.9 1 7.6 ka B.P." The Carolina Bays are also older than surficial dunes that have been dated using OSL dating at "29.9 1 2.8 ka B.P., 31.4 1 2.5 ka B.P., 35.8 1 4.8 ka B.P., 36.7 1 6.0 ka B.P., and 39.0 1 4.5 ka B.P." This is discussed in detail at: http://www.cla.sc.edu/sciaa/srs.html The idea that the Carolina Bays "must be quite young-- either late Wisconsinan or early Holocene" is soundly refuted by the above recent research by Brooks and Taylor (2001). The above web pages discusses what Brooks and Taylor have to say about the Carolina Bays. In addition, Grant et al. (1998), using ground-penetrating radar to study the internal structure of the rims of some Carolina Bays, show that they are **not** "essentially unaltered", but rather the evolution of these bays is characterized by multiple periods of bay-rim accretion with intervening intervals erosion. The more recent research, e.g. Brooks and Taylor (2001) and Grant (1998) refutes an Early Holocene to Late Wisconsinan age for the Carolina Bays and greatly disputes an extraterrestrial origin for them. For on-line details, a person can go to http://www.cla.sc.edu/sciaa/srs.html Another URL: NEBRASKA'S CAROLINA BAYS by ZANNER, C. William http://gsa.confex.com/gsa/2001AM/finalprogram/abstract_22324.htm References Cited: Brooks, M. J., B. E. Taylor, P. A. Stone, and L. B. Gardner (2001) Pleistocene encroachment of the Wateree River Sand Sheet into Big Bay on the middle coastal plain of South Carolina. Southeastern Geology. vol. 40, no. 4., pp, 241-257. Grant, J. A., M. J. Brooks, and B. E. Taylor (1998) New constraints on the evolution of Carolina bays from ground- penetrating radar. Geomorphology vol. 22, pp. 325-345. http://www.uga.edu/srel/Reprint/2276.htm Another Important Recent Reference: Brooks, M. J., B. E. Taylor, and J. A. Grant (1996) Carolina bays and Holocene landscape evolution on the Upper Coastal Plain of South Carolina. Geoarchaeology. vol. 11, pp. 481-504 Yours. Keith New Orleans, LA Received on Wed 25 Sep 2002 04:00:40 PM PDT |
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