I 9 4 OF THE ASBESTINE EARTH. 



lamellated mafs only, and its confidence, which 

 is not fo firm. 



Cronitedt's Miner. $ 103. i. 



EXP. 29 and 30. It agrees perfeclly with the 

 former afbcfios in its apj>carance irvthe fire. 



EXP. 31. A centenary of it yielded by analy- 

 fis, of terra pondcrofa, o ; aerated chalk, 12.7; 

 aerated magnefia, 26.1 ; clay, 2; liliceous earth, 

 56.2 ; and calcined iron, 3. 



$ xi. Oftbcfafiiculatcd AJbeJlos of Grange. 



THIS fpccics is found in the parifh of Grange 

 in Dalecarlia, and confifls of grey parallel fibres, 

 rather ri^id, not very diftincl, and collecled in- 

 to little bundles, which are not parallel in rela- 

 tion to each other, but crofs in various direcli- 

 ons. 



Cronftedt's Mineralogy, 106. 



EXP. 32 and 33. In the fire it appears as ufual. 



EXP. 34, Analyfis difcovcrs in the centenary, 

 of terra ponderofa, o; aerated chalk, 12.8; aera- 

 ted magnefia, 16; clay, 1.1 ; filiceous cartli, 

 63.9; and calx of iron, 6. 



S xii. 



