NOTES 173 



termination of Pacific Chalk Ooze by Radiocarbon and 

 Titanium Content," Telliis, 5 (1951), 222. 



Chapter 9. The Bottom Waters of the 

 Ocean and Their Movements 



1. L. Bruneau, N. G. Jerlov, and F. Koczy, "Physical and 

 Chemical Data," in Fascicle II of Physics and Chemistry, 

 Reports, 3, Pt. IV (1953). 



2. N. G. Jerlov, "Particle Distribution in the Ocean," op. cit., 

 3, Pt. III. 



3. K. Kalle, "Die Erscheinung eines leuchtenden 'Strahlen- 

 kranzes' an der Meeresoberflache," Annalen der Hydro- 

 grciphie iind maritimen Meteorologie, 67 (1939), 22—3. 



4. R. A. Daly, "Origin of Submarine 'Canyons,' " Am. Journ. 

 Sc.,31 (1936), 401-20. 



5. Ph. H. Kuenen, "Experiments in Connection with Daly's 

 Hypothesis on the Formation of Submarine Canyons," 

 Leidsche gcologische Mededeelingen, 8 (1937), 327-51. 



6. Ph. H. Kuenen and C. I. Migliorini, "Turbidity Currents 

 as a Cause of Graded Bedding," Journal of Geology, 58 

 (1950), 91-127; Kuenen, "Properties of Turbidity Cur- 

 rents of High Density," Society of Economic Paleontolo- 

 gists and Mineralogists, Special Publication, No. 2 (1951), 

 p. 14; Kuenen and H. W. Menard, "Turbidity Currents, 

 Graded and Non-Graded Deposits," Journal of Sedimen- 

 tary Petrology, 22 (1952), 83-96; Kuenen, "Estimated 

 Size of the Grand Banks Turbidity Current," Am. Journ. 

 Sc, 250 ( 1952), 874-84; Kuenen, "Significant Features of 

 Graded Bedding," Bulletin of the American Association of 

 Petroleum Geologists, 37 (1953), 1044-66. 



7. R. S. Dietz, "Possible Deep-Sea Turbidity-Current Chan- 



