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Ohio State USBC WBA
86th Ohio USBC WBA Championship, Singles event only Sorted by Event, Division
Singles Handicap Place Team name Pollard, Vicky L Wiley, Denise E Van Huss, Cissy A Mann, Jeanne C Dickey, Tara A Broadus, Sherrie A Huff, Judith D Hallett, Sue A Casey, Stephanie L Kellett, Brittni R Brady, Danielle C Wilkins, Antoinette A Ridgeway, Octavia A Nape, Beth A Ramsey, Kimberly N Perrini, Lisa A Hall, Jody L Smith, Kelly G Cook, Jean M Mager, Linda S Harding, Rina C Cousino, Pamela S Duvall, Beth Krueger, Kris Buchanan, Sharon E Honerlaw, Ashley E Childs, Donna S Pacey, Helen M Pelfrey, Melinda C Pinski, Sue M Thornsberry, Vicki L Jolliff, Linda K Pollard, Erica L Brock, Frankie L Brickey, Diana C Marshall, Barbara A Enyeart, Peggy R Simmons, Karen S Nolte, Margie Seara, Christina L Bonnigson, Patricia A Fetherolf, Suzanna M Walder, Betty J Beair, Taylor Mitchell, Jacalyn A White, Amy B
Entry , 1, 775
From Gr Cincinnati USBC WBA Newark Lake-Geauga Coshocton Dayton Bryan ...
It may be conjectured that during the crystal growth of mica some impurities collect together and precipitate in the form of a group, producing imperfections in the crystal which is attacked during etching, leading to the curved bottomed pits and pits with halos.It may be assumedthat the point bottomed pit nucleateat the termination of a linear dislocation. That the ratio of the lengthsof the longer diagonalto the shorterdiagonal remains constant in all the samples irrespective of the sizes of the pits suggeststhat the pit shape on all the samplesremains the same. The density of imperfections will vary from crystal to crystal becauseit will depend upon the environments under which the crystal has grown. This explains the wide variation in the density of the pits observedin the present investigation.It may be conjecturedthat theseimperfectionsmight play an important role in the insulating propertiesof micas.
RnlennNcrs Dn r-.t Veur-r, R. (1944) Formation et symetrie des ...
VOL. 53, SEPTEMBER-OCTOBER, 1968
PERRIERITE, CHEVKINITE, AND ALLANITE IN UPPER CENOZOIC ASH BEDS IN THE WESTERN UNITED STATES1 Surwy, G. A. Iznrr ar.tn R. E. Wrr-cox, U. S. Geological Denaer,Colorailo.
Alstne.ct Small primary crystals of perrierite, chevkinite and allanite occur in Cenozoic airfall ash beds at several Iocalities in the western United States. The nometamict crystallinity of all three minerals gave definitive X-ray and optical data on unheated material.
INrnooucrroN Small primary crystals of perrierite, chevkinite, and allanite occur in trace amounts in glassy airfall volcanic ash beds interlayered with terrestrial sedimentary rocks of late Cenozoicage in the western United States. The three minerals are rare-earth silicates that strongly resemble each other under reflected or transmitted light, and distinction between them requires care. The minerals were found during study of a large number of samplesof volcanic ash beds to determine what petrographic ...