Morgan. — Records of Unconformities in New Zealand. 17 



28. Hutton, F. W. " On some Railway Cuttings in tlie Weka Pass." 



Trans. N.Z. Inst., vol. 20, 1888, pp.'257-63. 



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35. McKay, Alex. " Report on Supposed Coal-seams in Kaiata Range, 



Greymouth." Pari. Paper C.-IO (in Mines Report), 1901, pp. 2, 7-8. 

 See also New Zealand Mines Record, vol. 4, 1900-1, pp. 203^. 



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East Cape Districts." Pari. Paper C.-IO (in Mines Report), 1901, 

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37. Mulgan, E. K. " On the Volcanic Grits and Ash-beds in the Waitemata 



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38. Fox, C. E. " The Volcanic Beds of the Waitemata Series." Ihid., 



pp. 452-93. 



39. Park, James. " On the Age and Relations of the New Zealand Coal- 



fields." Trans. N.Z. Inst., vol. 36, 1904, pp. 405-18. 



40. Clarke, E. de C. " The Fossils of the Waitemata and Papakura Series." 



Trans. N.Z. Inst., vol. 37, 1905, pp. 413-21. 



41. Park, James. " On the Marine Tertiaries of Otago and Canterbury, 



with Special Reference to the Relations existing between the Pareora 

 and Oamaru Series." Ihid., pp. 489-551. 



42. Bell, J. M., and Clarke, E. de C. " The Geology of the Whangaroa 



Subdivision, Hokianga Division." N.Z. Geol. Surv. Bull. No. 8 (n.s.), 

 1909. 



43. Morgan, P. G. " Field-work in the Grevmouth Subdivision." Third 



Ann. Rep. (n.s.) of N.Z. Geol. Surv., 1909, pp. 11-17. 



43a. " Petroleum and other Minerals in Eastern Wairarapa District." 



Pari. Paper C.-16, 1910. 



44. Adams, J. H. " The Geology of the Whatatutu Subdivision, Rau- 



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 1910. 



45. Park, James. " The Geology of New Zealand," 1910. 



46. Morgan, P. G. " The Geology of the Greymouth Subdivision, North 



Westland." N.Z. Geol. Surv. Bull. No. 13 (n.s.), 1911. 



47. Marshall, P. ; Speight, R. ; and Cotton, C. A. " The Younger Rock- 



series of New Zealand." Trans. N.Z. Inst., vol. 43, 1911, pp. 378^07. 



48. Park, James. " The Unconformable Relationship of the Lower Ter- 



tiaries and Upper Cretaceous of New Zealand." Geol. Mag. (n.s.), 

 dec. V, vol. 8, Dec, 1911, pp. 539-49. 



