a 
Son: all 
THE DEPTH AND MARINE DEPOSITS OF THE PACIFIC OCEAN. III 
Station 29, 17th September, 1899. 
Lat. 9° 16’ S.; long. 140° 25’ W.; depth, 1932 fathoms. 
GLOBIGERINA OOZE: appears to have been washed, is granular, and 
slightly coherent; pelagic, bottom-living, and arenaceous Foraminifera, 
coccoliths, rhabdoliths, Sponge spicules. 
Minerals (mean diameter 0.07 mm.), augite, olivine (?), plagioclase, mag- 
netite. 
Station 30, 18th September, 1899, 
Lat. 10° 29'S.; long. 141° 52’ W.; depth, 2456 fathoms. 
GLOBIGERINA OOZE: has the appearance of having been washed, is 
granular and incoherent, dirty brown in color, consisting of broken pelagic 
Foraminifera, bottom-living Foraminifera, arenaceous Foraminifera, cocco- 
liths, rhabdoliths ; Sponge spicules; with volcanic mineral particles, angular, 
mean diameter 0.1 mm., felspar, obsidian, much magnetite, and plagioclase. 
Station 34, 20th September, 1899. 
Lat. 14° 26’ S.; long. 146° 25’ W.; depth, 1208 fathoms. 
GLOBIGERINA OOZE: very little material, which has the appearance of 
having been washed, cream colored, quite incoherent, consisting of pelagic 
and bottom-living Foraminifera, Pteropods, Polyzoa, Echinoid spines, frag- 
ments of Mollusc shells, including one or two small Gasteropod shells 
(like Pleurotoma), coccoliths, rhabdoliths; arenaceous Foraminifera, Sponge 
spicules; plagioclase, volcanic glass, and small phillipsite crystals, one or 
two cosmic spherules. 
Station 37, 24th September, 1899. 
Avatoru Pass, Paumotu Islands; depth, 112 fathoms. 
CORAL SAND: very little material, made up of small fragments of Coral, 
pelagic Foraminifera, Echinoid spines, small Gasteropods (Pleurotoma), Tuni- 
cate spicules; volcanic glass, felspar, magnetite, and grains of manganese. 
Station 38, 24th September, 1899. 
Avatoru Pass, Paumotu Islands; depth, 604 fathoms. 
CORAL SAND: incoherent, white, made up of broken Corals, pelagic 
Foraminifera, coccoliths, Pteropods, Heteropods, Hchinoid spines, small 
Gasteropods (like Plewrotoma), Ostracodes; small mineral fragments, the 
largest about 2 nm. in diameter, containing felspar. 
