Mineralogy, 
^41 
bf thefe fubftances have been fofr at th^ 
inftant of their union, 
2. Conglutinated Hones, Sax a mnglutmata^ 
Are fuch Hones whofe particles have been 
united by fome cementitious fubHance, which^ 
however^ is feldom perceivable, and which 
often has not been fufficient to fill every fpace 
between the particles : In this cafe the parti- 
cles feem to have been hard, worn off, and in 
ioofe, fmgle, unfigured pieces, before they 
were united. 
SECT. CCLXr, 
i. Compound Saxa, Saxa compcftta, 
A. Ophites. Scaly limeHone with kernels 
or bits of ferpentine Hone in it, Saxunt 
compofitum particulis calcar eis et argillaceis. 
1 . KolmorcTs marble. It is white and green* 
2. Serpentino antico^ is white, with round 
pieces of black Heatites in it. This 
muH not be confounded with the Ser‘^ 
pentino verde antlco. Sed. cclxvi. 
3. The Haraldjlo marble^ White, with 
quadrangular pieces of a black Heatites. 
4. "Y\izM.aTmor Pozzevera dl Genoua. Dark 
green marble, with white veins. 
This kind receives its fine polifli and 
appearance from the ferpentine Hone. 
SECT. CCLXIL 
B. Stellften or Gefiellftein^ Saxum compofitum paf^, 
ticiilis quartzofs & mkaceis, 
t. Of diHind particles, Particulis difthidfis. 
This is found at Garpenberg in the 
province of Dalarne. It is likewife met 
R 2 with 
