DESCRIPTION OF PLATES. 123 



Fis;s. 6, 6 a, and 6 b. — Proximal end of tibia, with articular surface. 

 — B.M. No. 18452. 



Length of fragment, 9'5 in. Breadth of upper extremity, 6 - 8 in. Antero- 

 posterior diameter of ditto, 3*8 in. 



Fia"?. 7, 7 a, and 7 b. — Proximal end of tibia, with articular surface. 

 —B.M. No. 16,611. 



Breadth of upper extremity, 7'1 in. Antero-posterior diameter of ditto, 4 - in. 



Fi°;s. 8, 8 a, and 8 b. — Distal half of tibia, with lower articular sur- 

 face.— B.M. No. 39,548. 



Length of fragment, 9 - 5 in. Breadth of inferior extremity, 5 - in. Antero- 

 posterior diameter of ditto, 3" in. 



Fisrs. 9, 9 a, and 9 b. — Distal end of tibia, with lower articular sur- 

 face.— B.M. No. 39,549. 



Length of fragment, 7' in. Breadth of inferior extremity, 5* in. Antero- 

 posterior diameter of ditto, 2 - 6 in. 



Fig. 10. — Calcaneum and astragalus, in situ, restored. 



Figs. 11, 11 a, and 11 b.— Astragalus.— B.M. No. 16,998. 

 Length of astragalus, extreme, 4 - 9 in. Breadth of ditto, 3"4 in. Height of ditto, 

 2 4 in/" 



Figs. 12, 12 a, and 12 b.— Calcaneum, imperfect.— B.M. No. 39,543. 

 Length of fragment, 8 - 2 in. Projection of heel, 6 - 2 in. Breadth of calcaneal 

 tuberosity, 2 - 9 in. Height of calcaneal tuberosity, 2 - 8in. 



Fi?s. 13, 13 «, 13 b, 13 c, and 13 cl— Scapho-cuboid bone. — B.M. 

 No. 39,5441 



Breadth of scapho-cuboid bone, 4 - 9 in. Greatest antero-posterior diameter, 

 5- in. Greatest height, 3'4 in. Breadth of astragalar surface, 3 - 6 in. Breadth of 

 calcaneal ditto, 1'3 in. Breadth of cuneiform ditto, 1*5 in. Breadth of metatarsal 

 ditto, 1-8 in. 



Plate E. 

 Camelopardalis Sivalensis (Falc. and Caut.). 



Fijrs. 1, 1 a, 1 b, 1 c, and 1 d. — Third cervical vertebra of fossil giraffe, 

 from the Sewalik hills. The elongated character of the vertebra shows 

 that the animal had a columnar neck, and the fact that the transverse 

 processes are provided with foramina for the vertebral arteries shows 

 that it was not a camel. The complete synostosis of the upper and 

 lower articulating surfaces, the strong relief of the ridges, and the depth 

 of the muscular depressions, indicate that the animal was an adult, 

 which had long attained its full size. 



A note of this specimen, by Captain (now Sir Proby T.) Cautley, 

 appeared in the Journ. As. Soc. for July 1838, vol vii. p. 658, and a 

 detailed account was afterwards communicated to the Geological So- 

 ciety of London by Dr. Falconer and Captain Cautley, an abstract of 

 which appeared in the ' Proceedings,' No. 98. In the latter com- 

 munication the measurements and drawings of the specimen are given. 

 —B.M. No. 39,747. 



Figs. 2 and 2 a. — Fragment of second cervical vertebra of Camelo- 

 pardalis Sivalensis, from Perim Island. The right margin of the drawing 

 shows the mesial longitudinal ridge under the side of the body, and the 

 left margin is the ridge of the spinous process. The process pointing 



