FREE BOOKS

Author's List




PREV.   NEXT  
|<   41   42   43   44   45   46   47   48   49   50   51   52   53   54   55   56   57   58   59   60   61   62   63   64   65  
66   67   68   69   70   71   72   73   74   75   76   77   78   79   80   81   82   83   84   85   86   87   88   89   90   >>   >|  
ge of nothing but light and heat. Within these cavities, we find, _1st_, The coat of crystals with which this cavity is always lined; and this is general to all substances concreting, in similar circumstances, from a state of fusion; for when thus at liberty they naturally crystallise. _2dly_, We have frequently a subsequent crystallization, resting on the first, and more or less immersed in it. _3dly_, There is also sometimes a third crystallization, superincumbent on the second, in like manner as the second was on the first. I shall mention some particulars. I have one specimen, in which the primary crystals are siliceous, the secondary thin foliaceous crystals of deep red but transparent iron-ore, forming elegant figures, that have the form of roses. The tertiary crystallization is a frosting of small siliceous crystals upon the edges of the foliaceous crystals. In other specimens, there is first a lining of colourless siliceous crystals, then another lining of amethystine crystals, and sometimes within that, fuliginous crystals. Upon these fuliginous and amethystine crystals are many sphericles or hemispheres of red compact iron-ore, like haematites. In others, again, the primary crystals are siliceous, and the secondary calcareous. Of this kind, I have one which has, upon the calcareous crystals, beautiful transparent siliceous crystals, and iron sphericles both upon all these crystals, and within them. _Lastly_, I have an agate formed of various red and white coats, and beautifully figured. The cavity within the coated part of the pebble is filled up without vacuity, first, with colourless siliceous crystals; secondly, with fuliginous crystals; and, lastly, with white or colourless calcareous spar. But between the spar and crystals there are many sphericles, seemingly of iron, half sunk into each of these two different substances. From these facts, I may now be allowed to draw the following conclusions: 1_st_, That concretion had proceeded from the surface of the agate body inwards. This necessarily follows from the nature of those figured bodies, the figures of the external coats always determining the shape of those within, and never, contrarily, those within affecting those without. 2_dly_, That when the agate was formed, the cavity then contained every thing which now is found within it, and nothing more. 3_dly_, That the contained substances must have been in a fluid state, in order to t
PREV.   NEXT  
|<   41   42   43   44   45   46   47   48   49   50   51   52   53   54   55   56   57   58   59   60   61   62   63   64   65  
66   67   68   69   70   71   72   73   74   75   76   77   78   79   80   81   82   83   84   85   86   87   88   89   90   >>   >|  



Top keywords:

crystals

 

siliceous

 
crystallization
 

substances

 

cavity

 

colourless

 

calcareous

 

fuliginous

 

sphericles

 

secondary


primary
 
amethystine
 
figured
 

formed

 

lining

 

transparent

 
figures
 

foliaceous

 

contained

 

affecting


contrarily
 

lastly

 

coated

 

beautifully

 

pebble

 

seemingly

 

vacuity

 

filled

 

allowed

 

inwards


surface
 

conclusions

 

proceeded

 

necessarily

 

concretion

 

determining

 

external

 

nature

 

bodies

 

crystallise


naturally
 

liberty

 

frequently

 

subsequent

 

immersed

 
resting
 

cavities

 

Within

 

circumstances

 

fusion