No. used in this report USGS Cenozoic No. 2683 2685 No. USGS used in Cenozoic Field this Na. No. report 41b 18839 209 Field No. 127 Description of locality GRAYWACKE GRIT MEMBER OF BOHIO FORMATION QUEBRANCHA SYNCLINE, PANAMA South bank of eastward-flowing tributary of Rio Quebrancha, 375 oneters west-northwest of Transisthmian Highway bridge across Rio Quebrancha. Sandy siltstone in basal part of graywacke grit member of Bohio formation. T. F. Thompson and W. P. Woodring, 1949. Smaller Foraminifera. MARINE MEMBER OF BOHIO(?) FORMATION GATUN LAKE AREA, CANAL ZONE Vamos Vamos station, Panama Canal, in a cut about 2 meters above level of canal. Collected by F. Sensa, received from Alexander AgassiZ, 1891. [A submerged locality off Palenquilla Point west of Barro Colorado Island, originally on south bank of French Canal.] Location approximate. Vamos Vamos, lot 1. R. T. Hill, 1895. [The six collections frosn Vamos Vamos are presumably from the same locality.] Not plotted. Panama Canal at Vamos Vamos and 10.5 kilometers from Colon. R. T. Hill, 1895. [The designation "and 10.5 kilometers from Colon" should be deleted. Vamos Vamos was about 20 kilometers from Col6n.] Not plotted. Vamos Vamos, lot 2. R. T. Hill, 1895. Not plotted. Vamos Vamos, lower bed. D. F. MacDonald and T. W. Vaughan, 1911 (MacDonald, 1919, p. 542, pl. 154). Not plotted. Vamos Vamos, tpper sandstone. D. F. MacDonald and T. W. Vaughas, 1911 (MacDonald, 1919, p. 542). Poorly preserved molds in weathered sandstone. Not plotted. East side of promontory 375 meters southeast of Palenquilla Point, west of Barro Colorado Island. Loose calcareous concretions at water's edge. T. F. Thompson and W. P. Woodring, 1949. East side of Palenquilla Point, wide cove east of triangulation station. Approximately same as locality 41a, but from soft weathered mediumgrained sandstone. W. P. Woodring, 1954. Not plotted. 149 42a 17693 1 149a 42b 42c 42d 42e 149b 17965 1 149c 18837 18835 207 205 42f 18836 206 The trails on Barro Colora tervals of I hectometer, starting end of the trail heading toward 115 Description of locality MARINE MEMBER OF BOHIO(?) FORMATION GATUN LAKE AREA, CANAL ZONE-cOntinued East side of Palenquilla Point, head of cove north of triangulation station and southwest of Corozo Island. Calcareous concretion in soft sandstone. W. P. Woodring, 1954. Not plotted. Northeast coast of Trinidad Island. Sandy siltstone, basal 3 meters of exposed section. T. F. Thompson and W. P. Woodring, 1949. Also larger Foraininifera (Cole, 1952 [1953]). Same locality and same part of section, but from thin calcareous layer. T. F. Thompson and W. P. Woodring, 1949. Not plotted. Same locality, about 3 meters higher stratigraphically. One-meter ledgeforming silty medium-grained calcareous sandstone containing few small pebbles, few worn small heads of calcareous algae, and worn shell tips of Turritella. T. F. Thompson and W. P. Woodring, 1949. Larger Foraminifera (Cole, 1952 [1953]). Not plotted. Same locality, sandy siltstone about 4.5 meters stratigraphically above locality 42b. T. F. Thompson and W. P. Woodring, 1949. Not plotted. B301IO FORMATION, GATUN LAKE AREA, CANAL ZONE Barro Colorado Island, northern part of island, stream heading west of Miller Trail near Miller 17,4 about 100 meters above mouth. Somewhat calcareous medium-grained subgraywacke. W. P. Woodring, 1954. Barro Colorado Island, northern part of island, stream southeast of Fuertes House, about 275 meters above mouth. Conglomerate. W. P. Woodring, 1954. Not plotted. Barro Colorado Island, same stream as that for locality 42e, but about 60 meters upstream and from slide on west side of stream. Poorly sorted subgraywacke. W. P. Woodring, 1954. Not plotted. do Island have consecutively numbered signs at ing from the laboratory at the launch landing or at the the laboratory. GASTROPODS: TROCHIDAE TO TURRITELLIDAE 40 40a 40b 42 40c 2687 40d 6028a 40e 6028b 17692 18 19 26 17716 148 18838 208