50 MEMOIK OF WERNER 



riod iron appears under different forms, and we can 

 assign the age of its different mines. 



The necessity of abridgment obliges me thus to 

 bring together, under one view, results which, as 

 may easily be conceived, could not be obtained but 

 by many thousand observations. All Werner's ob- 

 servations, however, were made with so much care, 

 and so scrupulously combined, that their accuracy 

 has been confirmed by all subsequent investigation ; 

 and if we except his opinions regarding volcanic 

 countries, none of his views met with any opposition 

 which did not soon pass away. 



Such, then, is the nature of Geognosy, or of the 

 position of minerals, viewed as lying above one an- 

 other, or in a vertical direction. But in their hori- 

 zontal positionthat is, as they are placed by the 

 sides of each other there are likewise differences, 

 of which it is important to take notice. These dif- 

 ferences form the fourth point of view under which 

 Werner regards minerals, and which he designates 

 by the name of Geographical Mineralogy. 



Indeed, the rocks of most recent formation, and 

 which lie above the others, are the least elevated ; 

 the oldest penetrate through them, and form high 

 mountains. From this we infer, that the fluid sunk 

 in its level, in proportion as the solid substances in- 

 creased. It divided itself into basins, the produc- 

 tions of which became of a diversified character. 

 The surface of different countries is therefore dissi- 



