1 8 Bur,ivETiN 14 284 



C I. Heavy bedded layers, largely made up of 

 sand grains cemented by lime. Exposed in a ridge 

 running N. E. and S. W. 8 ft. 2 in. 8 ft. 2 in.. 



r Maclurea magna. c Asaphus canalis. 



rr Oiihis hippolite. c Leperditia. canaden- 



rr Rhynchonella (?) acutiros- sis var. nana. 



tris. r Leperditia amygda- 



XX Camarella varians. li?ia. 



2. Covered across a nearly level field. 82 ft. 90 ft. 2 in. 



3. Bottom foot a very hard, dark gray, fine 

 grained, rather pure limestone containing no fossils. 

 Above this, 6 ft. 2 in. of impure, very fossiliferous, 



shaly limestone. 7 ft. 2 in. 97 ft. 4 in. 



Q. Macbirea magna. x Rajinisqitinafasciata. 



XX Ecailioniphalus fredericits . rr Camarella longiros- 



c Dinorthis defle^a (?). tris. 



X Rafinisquina champlainen- c Asaphus canalis. 



sis. X Leperditia amygda- 



lina. 



4. Thin, impure, evenly bedded layers on west 



side of a small ridge parallel to C i. 7 ft. 3 in. 104 ft. 7 in. 



c Maclurea mag7ia. rr Illcenus ovatiis. 



XX Camarella longirostris. rr Asaphus canalis. 



c Dinorthis dejlefia (?). rr Lepei^ditia amygda- 



lina. 



5. One layer of hard, fine grained, dark gray 

 limestone with no recognizable fossils beyond Lep- 

 erditia canadensis var. nana and a few fragments of 

 a trilobite. The dip on the surface of this layer is 



7° 20' N. 59° W. 2 ft. 3 in. 106 ft. 10 in. 



6. Impure, shaly, somewhat nodular and irreg- 

 ularly bedded layers with fucoid markings, forming 

 the top layers of the ridge a few yards southeast of 

 the pavilion. One of the best collecfting places for 

 trilobites and gastropods. 5 ft, 3 in. 112 ft. i in. 



