1918.] The Fifth Indian Sctence Congress. elxxxvii 
erly a etn The specimens include several i ios 
nes, various bones of the feet (includin, g tw 
an Sealangos) he a a th. The limb bones are hollo ow and the Bri se ed 
generally is of lighter construction than that of 7. indicus. ptile 
was apparently a carnivorous dinosaur of the paboatne Theropoda. 
The Geotectonics of the Tertiary Irrawaddy Basin.—By G. 
DE P. CorTer. 
and in certain areas it is suggested wot t we ner St 
red earth facies of several beds which are "changing their facies. The 
boundary thus haat would appear bo fant pes 
nt Sipe ideneo neupheaval in the pia rstad 
Basin. The plate cee els are old sa giver gravels, an and the large 
size of their pebbles reg that the ised peace had steeper gradients. 
Gk Stscniie’ xs parts of Minbu are eutting through the recent 
alluvium : this G AGoies recent upheav io 
The (Gari top! of the Eocene of Burma.—By G. DE 
P. Corr 
The f is a meagre one, consisting of less than 20 species ae these, 
One is seuticnt with a form from the upper eocene of Java an sss 
one identical with a Khirthar species from India. The remain 
ie st 
pecies are given. The a wishes to than 
Vredenburg for kindly siaiatiog him with his advice in the prapasitibe of 
is pape 
oud Ganesa in the Mid Siwaliks of Jammu.—By D. N. 
Wap 
A fossilised tusk of an extinct elephant Poeneag’e! was discovered 
by the writer in the Mi i hi 
id Siwalik strata of the Jam a 
wer 2 description of the Siwaliks vet ‘ the positon of t 
: e characters of the skull, the r jaw 
iublanted in situ and ef olars Mesos ments and description, the 
oe a its oi 
incisor or tusk, its detailed measurements. Fossil ivory, its 
charac 
i ic 
es age on of the fo: a its stratigraphic position. Microscop 
ss 
Geology of Hyderabad (Deccan).—By K. A A. K. HaLLOwes. 
PP Nn eo aN oa inal 
Nes ee 
