96 Notes on Geological Specimens from [Feb. 



Misrita-Nava-Dharm&mndydh. 



4. 2. I. 3. t. 



Pandara. Lochana. Vajradhatwiswari. Mamaki. Tara. 



S. 6. 7. f 9. 



Pratyangira. Vajrasatwatmika. Vasundhara. Guhyeswari. 



Manushlya-Nava-Buddhdmndydh. 



4. 2. 1. 3. 5. 



Sikhi Ratnagarbha. Dipankara. Vipasyi. Viswabhij. 



8. 6. 7. 9. 



Kasyapa. Kakutsanda. Kanakamuni. S5kyasinha. 



Mdnushlyd- Nava-Buddhdmndydh . 



1. 2. 3. 4. 5. 



Dipankara. Ratnagarbha. Vipasyi. Sikhi. Viswabhu. 



6. 7. 8. 9. 



Kakutsanda. Kanakamuni. Kasyapa. Sakyasinha. 



Mdnushiya- Nava-Prajndmndyi. 

 1. 2. 3. 4. 5. 



Jwalavati. Lakshanavati. Vipasyantf. Sikhamalinf. Viswadhara. 



6. 7. 8. 9. 



Kakudvati.. Kanthanamalini. Mahidhava. Yasodhara. 



Nava Bhikshu-Sanghdmndydh. 



1. 2. 3. 4. 5. 



Pradipeswara. Ratnaraja. Mahamati. Ratnadhara. A'kasaganja. 



6. 7. f 8. 9. 



Sakalamangala. Kanakaraja. Dharmodara. AnanJa. 



Iti Sri-Ekdmndyddi-Navdtnn&ya-Devatdh Samdptdh. 



N. B. The authority for these details is the Dharma Sangraha, or catalogue 



raisonne' of the terminology of Bauddha system of philosophy and religion. 



III. — Notes explanatory of a Collection of Geological Specimens from 

 the Country between Hyderabad and Ndgpur. By J. G. Malcolmson, 

 Assistant Surgeon, Madras Establishment. PI. V. 



I had the pleasure of forwarding from Madras, a selection of geolo- 

 gical specimens, collected in May, 1833, between the cities of Hyderabad 

 and Nagpur. I regret, that circumstances prevented my doing this 

 sooner, and that the notes in explanation of the localities whence they 

 were obtained, must now be short and imperfect ; I hope, however, 

 that the specimens themselves will be of use in illustrating the geology 

 of a tract of country hitherto undescribed, and which connects the 

 formations of the south-east of the Deccan, with those in the neigh- 

 bourhood of the valley of the Narbada. 



From my inability to identify, describe, and figure the numerous 

 fossils, discovered in the tract of country between the Godavery 

 and the town of Hinganghat, 47 miles south of Nagpur, and the 

 importance of these, in reference to the questions as to the relative 

 age of the great trap formation of the Deccan, and of the west of 

 India, and the clayslate formation of Voysey, with its associated sand- 

 stone*, and the periods of elevation of the granitic rocks, on which 



* See his account of the diamond mines of Banganapilly. — As. Res. xviii. 



