tt 



-^it 





) 



Us 



en 



c 



I 



a 



i^oiii; 



^k is 



I 



Y I 



I' 



'. ■ fluid - ' 



■ ^'^ h that 

 "^ « force 



h 







Pr 



. ^-itli 



1^ 



m '. 



P^oportioiMji 



'''I ftones ffF 



'" into mpi 



' J q iiiet d i 



• t 



remain m 



'"!i. 



•<» move the wt 



r^in tlie 



•Jpr; of a 



iCE. 



I 



i' 



• • -pther'^" 



110 



theni' 



^ 



icefl 



tliefl 



J 



ii 



-d tl>^'' fl 



HUTTONIAN THEORY. 



395: 



hich a 



few hours before were 



d 



verd 



now buried under heaps of (Ion 



th 



or 



helmed by ma 



f 



the fides of the mountains cut 

 where the track of the fmaileft 

 before to be difcovered *. 



iquid 

 : by c 



d 



I 



not 



It is b 



ly, ho 



even 





like thefe, that fuch 



aft 



afles of rock can be 



feen adtually in motion, as are 



ften found 



the furface, apparently removed to a great d 



llance from their native pi 



The magnitude 



of thefe is fo great, in many inftances, that their 

 tranfportation cannot be explained without fup- 

 pofmg, that the furface was very different when 

 thefe tranfportations took place from what it is 



prefe 



that the elevation of the mou 



greater, and the ground fmoother and 



fo 



at leaft in fo 



dired 



If thefo 



fuppofitions are admitted, and they 



d 

 phenomenon 



have already feen, by almoil every 



^ ip.>ui«. j phenomenon m geoK 



^ty, fays 3D £5?^ prefent themfelves h 



eology, th 



difficultie 



hich 



will 



appear infur 



able 



3 



One of the largeii blocks of granite that 



on the eaft fide of the lake of 



know of. is 



BbA 



G 



* See an 



account of a thunder llorm Hear Bareges, in 



Effai fur la M 



P-'34 



