( 5 °9 ) 
their Repofitory. From the Surface of the Ground 
down to the Place where thefe Bones were found, 
the Difpofition of the Strata , or Layers, was as 
follows : A black Soil four Foot deep, Gravel two 
Foot and a Half, the Middle whereof was made up 
of Ofteocolla and Stones to the Depth of two Foot, 
Ofteocolla and Stones half a Foot, a fandy Clay fix 
Foot, with about two Inches of Ofteocolla in the 
Middle, Ofteocolla and Pebbles one Foot, Gravel 
fix Foot, a white and fine Sand, the Depth whereof 
was unknown, and in this the Bones were found. 
In the Second Volume of Count Mar fill's c Danu - 
biusy where he treats of the Antiquities he obferved 
along this River, there is Mention made of feveral 
Bones and Teeth of Elephants, which that inquifitive 
Nobleman met with in Hungary and Tranjylvanlay 
and which are now in his valuable Colledion of 
natural and artificial Curiofities at Bologna. Accord- 
ing to the beft Information, the People of whom he 
had them could give him, they were found in Rivers, 
Lakes and Pools. One of the Vertebra?, a Grinder, 
and a confiderable Part of the dens exert us, or Tusk, 
were found in the Lake, or Pool of Hiulca. Two 
Fragments of the Os Tibia, a little corroded on the 
Infide, were taken out of a Pool near Fogheras in 
Tranfylvanla, once the Seat of the Princes of that 
Country ; and the whole lower Jaw, with two 
Grinders as yet flicking in it, he had from fome 
Fifhermen, who found it in the Handing Waters by 
the River Tlblfcus, a little above die Romerskantz, 
or the Roman Fort. All thefe the Author caufed to 
be figured as big as the Life. I have above related 
the Opinion of Goroplus about the Antiquity of thofe 
two 
