OCEANOGRAPHY OF THE PACIFIC. 19 



erable size (up to (> millimeters), and a small proportion of foram- 

 inifera mostly broken and corroded. 



Station 362. — 1,937 fathoms. T^^pical globigerina ooze. Pinkish- 

 white. Very little tine washings. Sediment almost entirely foram- 

 inifera {Globigerina, Orbulma^ Pulmnulina., Lagena, CassiduUna, 

 Ehrenhergina^ VirguUna, Pvllenia). No radiolaria or diatoms 

 observed. \e.Yj few coccoliths. 



Station 369. — 966 fathoms. Globigerina ooze. Foraminif era of the 

 common pelagic species. 



Station 373. — 2,153 fathoms. Red clay. Fine yellowish-brown 

 mud. A few foraminifera, mostly in corroded fragments. Manga- 

 nese concertions, crystals and spherules of phillipsite, and minute 

 magnetic particles. 



Station 376. — 2,780 fathoms. Red clay. Yellowish-brown. Almost 

 entirely tine washings. No organic remains; very few mineral 

 fragments. 



Station 385. — 720 fathoms. Globigerina ooze. ( Glohigerina^ Orhu- 

 iina, Pulvinulina., Sphaeroidina^ Cristellaria.) An occasional radiola- 

 rian and bit of sand. 



Station 390. — 3,006 fathoms. Red claj^ Exceedingly tine brown 

 mud. Only separable residue a few minute manganese concretions, 

 crystals of phillipsite, and discoid radiolaria. 



Station JfiO. — 3,159 fathoms. Red clay. Light yellowish-brown, 

 very fine mud, containing no organic remains, ver}^ few mineral frag- 

 ments exceeding 0.08 millimeter in diameter, and many minute crj^stals 

 of phillijDsite. 



Station If-ll. — 3,188 fathoms. Red clay. Very fine brown mud. 

 A few radiolarians and diatoms, small crystals of phillipsite, and 

 minute glassy mineral fragments. 



Station Jf27. — 1,997 fathoms. Globigerina ooze. Grayish-white. 

 Foraminifera much broken. A few perfect specimens of Ehren- 

 hargina hydrix. Rather large manganese concretions, fragments of 

 pumice and spherules of phillipsite. Minute fragments of volcanic 

 glass. 



Station JiSl. — 3,150 fathoms. Red c\?iy. Yellowish-brown fine 

 mud, containing a few I'adiolaria. The washed sediment consists of 

 fine volcanic glass, and other mineral fragments varying in color from 

 dark red-brown to light brownish-yellow. Minute manganese par- 

 ticles and a few crystals of phillipsite. 



Station li.60. — 689 fathoms. Globigerina ooze. The usual pelagic 

 foraminifera, a ver}^ few coccoliths and rhabdoliths. Rarel}^ a mineral 

 fragment. 



Station Ji,63. — 1,913 fathoms. Globigerina ooze. Specimen con- 

 sists of a little globigerina ooze, and the fragments of a manganese 



