78 



CHAPTER V 



The Mackay soils are of an acidic tj'pe formed from the decay of mixed 

 siliceous rocks, and are in sharp distinction to those of the Bundaberg district. 



The average analysis of the soils from the Mackay and Cairns district is 

 thus found by Maxwell : — 



REFERENCES IN CHAPTER V. 



1. A Treatise on Rocks, Rock Weathering and Soils. 



2. H.S.P.A. Ex. Sta., Agric. Series, Bull. 45. 



3. Principles and Practice of Agricultural Analysis. 



4. Soils, New York, 1906. 



5. Jour. Chem. Soc, 1894, 65, 115. 



6. Ensayo sobre el Cultivo de la Cana de Azucar. 



7. La Canne k Sucre. 



8. Culture de la Canne a Sucre a Guadeloupe. 



9. Hawaiian Agricultural Ex. Sta., Bull. 40. 



10. Int. Sug. Jour., 1905, 7, 572. 



11. Porto Rico Ex. Sta., Bull. 11 



12. Bevista de Agricola y Industria de Tiicuman, 1912, 3, 306. 



13. Report of the Government Laboratory, British Guiana, 1908. 



14. Agricultural Ledger (Agricultural Series), 1898, 53. 



15. Estacion Central Agronomica, Cuba, Boletin 2. 



16. Estacion Central Agionomica, Cuba, Boletin 28. 



17. Bull. Assoc. Chim. Sue, 24, 1691. 



18. Jour, of the Khedivial Agric. Soc, 180S. 



19. Lavas and Soils of the Hawaiian Islands. 



20. Soils, New York, 1906. 



21. Soils, New York, 1906. 



22. Java Arch., 1912, 20, 1251. 



23. Stubbs' " Sugar Cane." 



24. On the Sugar Industry of Peru. 



25. Philippine Journal of Science, Section A„ 1914, i, i. 



26. Report, Bureau of Experiment Stations, Queensland, 1904-5. 



