« « « 



XV ill 



NTENT 



diurnal motion, § 375, 376. 

 fion of Frifi, and of Maior'R 



Kh 



vvai 



mifa 



H 





mi 



§ 



§ 377» 378. 



and about 



§ 



Note xx. 



Inequalities of the Planetary Mo- 

 Page 437 



tions. 



§ 



cumljt 



§ 



AfH 



Dr Hutton 



with 



refpecl to the changes at the furface of the earth, § 581 



6 



Note xxi. 



Changes in the Apparent Level of 



th.e Sea. 



P- 441 



E.clative level of the fea and land fubject to change, 



Proofs that it has funk, on the ill ores of this 



^ 



on the coafts of P"rance and Flanders' 



§ 



§ 



-^ 



§ 



This 



r 



has not aiifen from the deprcfficn of the fea, but from 

 the elevation of the land, § .^9 , 393. 



Th 



e furface 



of tne Hadriatl 



« « 





hi2h(tr now 



§ 



S95. Alfo of the Mediterranean, S ^0 7. Irre mlari 



tiec in thef 



c 



§ 398? 399\ Hypothefis of Frifi, 



that towards the equator the fea is every v^here rifms^, 



D 



-Note xxii.-~FoffiI Bones. 



P-458 



'i^egexable and animal remains contained in the foITil 



§ 



I c 



Of thofe that aie enveloped or pe- 



netrated with calcareous earth, § 



bones buried in the loof 





§ 



05. Of the 

 Bones in Si- 



beria referred to the rhinoceros and tlie elephant, . 



§ 407. , 



i 



