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[[stamped]] 0601 [[/stamped]]

October 21. Went over to Eidson in morning. zone of abundant D. atavoides is about 5' vertical above the zone of abundant Sowerbyites. The latter genus also occurs in the zone of D. atavoides.

About 100' below the Dinorthis zone in field to east of highway fossils are fairly common & include a multiplicate Cameralla like C. elliptica, Hesperorthis, Mimella and Murina. This horizon may be close to the murina zone on yellow Branch. Several marbles occur in the Ottosee here. They are reefs without a doubt.

Hotel at Kingsport                                      [[checkmark]] 3.00
Breakfast                                               [[checkmark]] 0.80
Lunch                                                                      
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Supper (Morristown)                                     [[checkmark]] 1.20

In the Thorn Hill section Fascifera underlies Pionodema (as it appears in Crytophagmus). This is indicated by position and we saw Fascifera but not Pionodema. Zygospira indicates Witten.

Oct. 22
Hotel (Morristown)                                     [[checkmark]]  2.00
Breakfast                                              [[checkmark]]  0.50
Lunch                                                  [[checkmark]]  0.38

At bend 1/4 mile - 1/2 mi. East of Red Hill big development Sowerbyites]beds, with [[Din]] willandi. H13
1/4 mi. E, Beech Grove Ch. occurs Oligophynaliva beds which are above the Sowerbyites H12A

The Sowerbyites bed is above S triseptatus bed & this zone may tie close to Echnosphantos zone farther north.

Supper Bristol                                                         1.40

[[margin]] Hiskell = Wardell [[/margin]]