Annual report . hale 14 Tichenor limestone. 14 Moscow shale 15 PAGE Pyrite layer in horizon of Ttdly limestone 15 Genesee black 16 Genundewa limestone 17 West River dark shale 17 Middlesex black shale 18 Cashaqua shale 19 Rhinestreet black shale 19 Hatch shale and 20 Grimes sandstone 21 and shales. ... 22 Nunda sandstone 22 Wiscoy beds 23 Chemung sandstone and shale 24 24 Index 27 New York State Education Department Science Division, December 2, ipio Hon. Andrew S. Draper Commissioner of EducationSir : I have the honor to transmit to you
Annual report . hale 14 Tichenor limestone. 14 Moscow shale 15 PAGE Pyrite layer in horizon of Ttdly limestone 15 Genesee black 16 Genundewa limestone 17 West River dark shale 17 Middlesex black shale 18 Cashaqua shale 19 Rhinestreet black shale 19 Hatch shale and 20 Grimes sandstone 21 and shales. ... 22 Nunda sandstone 22 Wiscoy beds 23 Chemung sandstone and shale 24 24 Index 27 New York State Education Department Science Division, December 2, ipio Hon. Andrew S. Draper Commissioner of EducationSir : I have the honor to transmit to you herewith and to recom-mend for publication as a bulletin of the State Museum a manu-script report and map covering the geology of the Honeoye andWayland quadrangles of the geological map of the State, which havebeen prepared by Mr D. Dana Luther, of this staff. Very respectfully John M. Clarke Director STATE OF NEW YORK EDUCATION DEPARTMENT commissioners ROOM Approved for publication this 2d day of December 1910. Commissioner of Education Education Department Bulletin Published fortnightly by the University of the State of New York Entered as second-class matter June 24, 1908, at the Post Office at Albany, N. Y., underthe act of Congress of July 16, 1894 No. 504 ALBANY, N. Y. October i, 19n New York State Museum John M. Clarke, DirectorMuseum Bulletin 152 GEOLOGY OF THE HONEOYE-WAYLAND QUAD-RANGLES By D. Dana Luther The Honeoye-Wayland quadrangles are included between thelines of latitude 42° 30 and 43° north, and of longitude JJ° 30and yy° 45 west and contain one-eighth of a. degree, or about 441square miles of territory. The rocks of these quadrangles have an estimated aggregatethickness of about 2660 feet, of which 1510 feet are surface rocksbecause of the difference in altitude between the lowest outcrop,which is on Honeoye creek near Sibleyville at 590 feet A. T., andthe highest, at the top of Sand hill near the south line of the Waylandquadrangle at 2100 feet A. T. El
Size: 3061px × 816px
Photo credit: © The Reading Room / Alamy / Afripics
License: Licensed
Model Released: No
Keywords: ., bookcentury1900, bookdecade1900, booksubjectscience, bookyear1902
