10 
Gen. Conchvliolithus. Fam. Anomit^. 
triangu- 
laris. 
stria tus. 
suiconicus. 
(uspidatus. 
Tab. 29. Tab. 36. - Fig . 1. 
Trigonal Anomite. 
Sedes : strata vetusta, calcaria. 
la most parts of the county where limestone occurs. 
12. Conch. Anomites trigonus longitudinaliter sulcatus, sinu angulato laevi. 
Tab. 36. Fig. 2. 
Triangular Anomite. 
Sedes : strata vetusta calcaria. 
Found with the foregoing, but less common. 
13. Conch. Anomites semiorbiculatus longitudinaliter undique striatus t 
striis approximatis elevatis subaequalibus, sinu rotundato parvo ad valvam 
perforatam subobsoleto. 
Tab. 23. Fig. I, 2. 
Striated Anomite. 
Sedes : strata vetusta, calcaria. 
Obs. This is the largest of out Derbyshire perforated frequently four or five inches 
in breadth, immediately at the hinge. 
14. Conch. Anomites longitudinaliter sulcatus, foramine magna, sinu angu- 
lato, valva imperforata semicircular! ; altera semiconica ; nate recta 
apiciformi. 
Tab. 47. Fig. 6, 7, 8. 
Subconical Anomite. 
Sedes: strata vetusta, calcaria. 
Found in the limestone of Middleton Dale. Rare. 
15. Conch. Anomites longitudinaliter sulcatus, foramine maxima, sinu 
rotundato, valva imperforata semicirculari j altera pyramidata : nate 
verticiformi subreflexa. 
