52 On. A. G. BUTLER ON LEPIDOPTEEA [Feb. 1, 



21. JUNONIA BOOPIS Trim. 



Nyakongoli, Makoto, August 21st ; Chiperoni, September 1896. 



22. PEOTOGONIOMOEPHA ANACAEDII Linn. 

 Eastern Transvaal and Portuguese East Africa. 



23. PEOTOGONIOMOEPHA AGLATONICE G-odt. 



Inure. 



The vars. aylatonice and nebulosa were both obtained. 



24. PTEAMEIS CAEDUI Linn. 

 Eastern Transvaal. 



25. EUEYPHTJEA ACHLTS Hopff. 



<3 . Chiperoni, Portuguese Central Africa, September 1896. 



26. EFETPHENE SENEGALENSIS Hiibn. 

 2 Chiperoni, October 1896. 



27. ATEEICA GALEKE Brown. 



Patawali, Portuguese East Africa, 27th August, 1897. 

 Only one much damaged male of this species was obtained. 



28. EUPHJEDEA NEOPHEON Hopff. 



Portuguese East Africa. 



No exact locality is given on the envelope. 



29. CEENZDOMIMAS CONCOEDIA Hopff. 



2 . Patawali district, Portuguese East Africa. 



The single example obtained corresponds exactly with Hopffer's 

 figure in the colouring of the upper surface, but the innermost 

 row of black spots on the secondaries is absent (as is sometimes the 

 case in the nearly allied C. crawshayi) : on the under surface the 

 colouring is a little deeper than in the figure : but, as I pointed 

 out when comparing C. crawshayi with Hopffer's figures, the blue 

 spots on the primaries (excepting at apex) are not connected with 

 the blue outer border ; on the other hand this border is not 

 continuous on the primaries as represented m Hopffer's description 

 and figure. In some of the characters which distinguish 0. craiv- 

 shayi from C. concordia the present specimen therefore seems to be 

 intermediate, though the more varied and blue- tinted upper 

 surface with the wider bifid whitish subapical bar give it a 

 different aspect from any of the females of the Nyasa type ; so 

 that, until the separation of the spots from the border on the 

 under surface has been proved to be variable, the two forms must 

 still be kept apart. 



30. CEEJQS BOISDFYALI "Wallgr. 



Eastern Transvaal. 



The example now received agrees most nearly with one which 



[4] 



