he little town 
Monastery 
IS. 
  
iis figure 
he route of 
from different 
id the result of 
s query is 
earch records 
he key word 
a” (investiture) 
tery of 
All data have 
1 in the source 
f Rifreddo, that 
SQL 
The result is in 
umn: the 
has been 
'a court, a 
of, a vineyard 
l, grown to 
ial for 
se. 
    
  
Aile 
shit aise 
eitis 
  
  
al 
às. 
  
cam ou 
2 40m 
de 
  
  
  
  
  
   
it pe 
edes we 
  
  
Fig. 8 — The short sequence allow to realize where 
next geological and historical recognitions will be 
adressed. Cima di Crosa and Rocce dei Rastelli 
are reported by literature as possible sites of 
extraction of metals. We certainty know istead that 
lower in the valley there were metallurgical 
villages. (Documentary sources tell us about 
working sites but we still don't know where mines 
were located in the valley). 
x wenpeerdones 
QOSETGUMOSE CON DEBOLE STRATO 93 ALTER 
ALELIIONALT 
ATTOUORE 
GHIA EC LOSE, TALOR 
MON ALTERATI 
ALTERATI TALOSJA IN 
E aecnar sn Tose CALAZIONI SABE AR 
Ld sanete, z LY GREASE ED 
Egenanikg APGHLOSE GES QHVENTI DI 
Ds 
e NABNE DOSRENACEE (PIETRA DA CANTOHITE CALCAE 
POL EGENT a EL SRENARIE 
DICALCART, CALCARE MAR CALARTS M 
f AR 
  
  
    
  
Ea. 
Erwan 
  
MARMOSE, CALCARE 
OCT G STRATIFICATI 2M EN 
CALCSREI 
  
Bl cuss 
  
    
  
—313— 
Fig. 9 — The last picture is 
about a spatial analysis 
regarding the comparison 
between quarries tipology 
(points) and lithological layer 
(aeas)