THE DEPTH AND MARINE DEPOSITS OF THE PACIFIC OCEAN. 125 
Kchinoid fragments and spines, Alcyonarian spicules, small Gasteropods and 
Lamellibranchs, otoliths, Ostracodes, pelagic and bottom-living Foraminifera, 
Pteropod fragments, Heteropod fragments, Polyzoa; small particles of 
obsidian were observed. 
Station 117, 18th October, 1899. 
Lat. 15° 54’ S.; long. 142° 16’ W.; depth, 563 fathoms. 
Only one or two small fragments of decomposed pumice, coated with 
manganese, were at hand, the largest being about 2 mm. in length, also some 
calcareous grains, which look like Coral fragments. 
Station 118, 18th October, 1899. 
Lat. 16° 12’ 8.; long. 142° 31’ W.; depth, 630 fathoms. 
CORAL SAND: gray, granular, quite incoherent; appears to have been 
washed ; consists of fragments of Corals, Polyzoa, small Lamellibranchs and 
Gasteropods, otoliths, Ostracodes, pelagic and bottom-living Foraminifera, 
Pteropods, Heteropods, Echinoid spines, Alcyonarian spicules, Tunicate 
spicules; small particles of obsidian and magnetite were observed. 
Station 119, 18th October, 1899. 
Lat. 16° 14’ S.; long. 142° 50’ W.; depth, 1516 fathoms. 
GLOBIGERINA OOZE: cream colored, granular, quite incoherent ; appears 
to have been washed; consists of pelagic and bottom-living Foraminifera, 
otoliths, Ostracodes, Tunicate spicules, coccoliths, rhabdoliths; minute par- 
ticles of obsidian and magnetite were observed. 
Station 120, 18th October, 1899. 
Lat. 16° 21’ S.; long. 143° 14’ W.; depth, 928 fathoms. 
CORAL SAND or PTEROPOD OOZE: very little material ; cream colored, 
granular, quite incoherent; appears to have been washed ; contains Coral 
fragments, Polyzoa, Pteropods, Heteropods, pelagic and bottom-living Fora- 
minifera, Ostracodes, otoliths, Tunicate spicules; small particles of obsidian 
and magnetite. 
Station 121, 19th October, 1899. 
Lat. 16° 25’ S.; long. 143° 33’ W.; depth, 1108 fathoms. 
PTEROPOD OOZE : very little material; granular, cream colored, inco- 
herent; has the appearance of having been washed ; consists of Pteropods, 
