18 MALONE JURASSIC FORMATION OF TEXAS. [bull. 26 
Locality No. 4. — About a mile a east of the railway station of Finlay; apparent* 
about the same horizon as the locality next below mentioned. 
Gryphsea mexicana. Trigonia proscabra?.» 
Lima interlineata. Astarte malonensis. 
Pecten insutus. Unicardium transversum. 
Modiola geniculata. Chemnitzia goodellii. 
Modiola maloniana. Nerinella stantoni. 
Trigonia calderoni. 
Locality No. 5. — Foothills near the railroad, at northwestern cud of Malou 
Mountain, a little over 2 miles east-southeast of Finlay station, not more tha 
200 feet above the gypsum bed; total exposure above gypsum bed here 54 
feet; fossils all from middle hundred feet. 
Cucullsea castilloi. Natica finlayensis. 
Lucina potosina, var. metrica. Natica inflecta. 
Lucina planiuscula. Nautilus naufragas. 
Unicardium semirotundum. Oppelia faliax?. 
Pholadomya paucicosta. Perisphinctes schucherti. 
Nerita finlayensis. 
Locality No. 6. — First high ridge west of Malone Mountain, about 2 miles ires 
of Malone station, in No. 1-1 of Doctor Stanton's Malone Mountain section. 
Gryphsea mexicana. Astarte malonensis. 
Pecten insutus. Pleuromya inconstans. 
Trigonia munita. 
Locality No. 7. — West of the north pari of Malone Mountain, about 2 mile 
SOUthwest Of Malone station, in \o. I.! of Doctor Sluiilou's Malone Mouulait 
section. 
Gryphsea mexicana. Martesia maloniana. 
Pecten insutus. Chemnitzia goodellii. 
Astarte malonensis. Nerinella stantoni. 
Unicardium semirotundum. Nautilus burkarti?. 
Pleuromya inconstans. Perisphinctes clarki. 
Locality No. s. At same locality as the preceding, but from a horizon ,1,1b fee, 
higher, viz, No. 25 of Doctor Stan ton's Malone Mountain section. 
Pygurus sp. Pinna quadrifrons. 
Gryphsea mexicana. Pleuromya inconstans. 
Locality No. 9. — West base of Malone Mountain, a short distance north of tin 
soul lie til ends 
Gryphsea mexicana. Pinna quadrifrons. 
Exogyra potosina (broadly triangular Pholadomya cf. marcoui. 
phase). Pleuromya inconstans. 
Gervillia Cinderella. Pleuromya inconstans. var. curta. 
Gervillia? riograndensis. Corbula? maloniana. 
" Something more than this distance, a litllo south of east. 
6 A cast ; it may possibly represent T. prwstriata. 
'On this collecting station, having previously referred in his field notes to a fresH 
watey limestone 7."i to 100 feet below a quartzitic conglomerate at top of Malone Moun- 
tain a short distance north of its southern end. Doctor Stanton comments as follows: 
"In the field this was believed to be between the fresh water horizon and the quartzitfl 
conglomerate above mentioned. It is certainly several hundred feet above a horizon of 
the Gryphw mexicana and Nerinea," 
