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[[stamped]] 0595 [[/stamped]] 27 May 22. Spent all morning packing 8 kegs. In afternoon visited quarries in NE edge of Marion. Here 50' of Mosheim lies on [[margin]] 587 [[/margin]] the Knox and is overlain by 50' of Lenoir, nodular limestone which is shaley in the upper 5 - 10'. This shaley part contains brachiopods suggestive of the Upper Lenoir at Knoxville such as Bimuria and Isophragma. [[margin vertical]] Sowerbyites of lower OHosee must overlie this Lenoir. Note 10/17/43. [[/margin vertical]] Then we went 5 miles west of Marion to see Onondaga chest [[margin]]] 589 [[/margin]] overlying the Ordovician. May 23 Went from Marion northeastward to vicinity of Bland where we visited a small quarry in "Holston ls". This was a very pure crystalline limestone but fossils were not abundant. This quarry is said by Mr.Butts [[margin]] 590 [[/margin]] to be the McNutt Qy mentioned in Raymond and Willards' paper. After lunch in Bland we went down main road to SE and took first left turn to Grayson Farm. Here we [[margin]] 598-598a [[/margin]]