258 THE 600SOO 0V M. DE BORDA. 



tremely compressed, whilst that of this fossile is 

 broader than it is high. The teeth also are quite of 

 another form. Neither the level above the sea, nor 

 the relation of the specimen to the neighbouring 

 country, are rprorded in the source* whence we 

 have extracted tms truly interesting notice. 



