Arenisca Uncastillo

Gold-shaded sandstone, which main characteristics are its beauty and its durability. This material is used for coatings as well as paving, even though its specifications and its workability make it highly suitable for restoring and decorating applications.

 

Aserrado
Sawn
Abujardado fino
Fine Hammered
Abujardado Rústico
Rustic Hammered

 

Apomazado
Honed
Puntero
Pointer
Tallante
Carving

 

Technical caracteristics:

Absorption. UNE-EN 13755:2002
7,1%
Open porosity. UNE-EN 13755: 2002
15,4%
Determination of the bulk density. UNE-EN 1936:2007
2158,2 Kg/m3
Determination of the water absorption coefficient through capilarity UNE-EN
1925:1999
C1
255,56 gr/m2s0,5
C2
224,84 gr/m2s0,5
Resistant to bending. UNE-EN 12372:2007
5 MPa
Resistant to bending after freezing. UNE-EN 12372- 12371
4,7 MPa
Resistant to compression. UNE-EN 1926:2007
46,7 MPa
Resistant to compression after freezing. UNE-EN 1926-12371
44,6 MPa
Resistant to slippage without polishing. UNE-EN 14231: 2004
70
Resistant to erosion provoked by abrasion. UNE-EN 14157: 2005
28,5mm
Determination of the breaking load for anchors UNE-EN 13364: 2002
500N
Determination of the resistance during the aging process provoked by thermal shock UNE-EN 14066:2003 after 20 cycles volume loss
0,11%
Determination of the resistance during the aging process provoked by thermal shock UNE-EN 14066:2003 after 20 cycles reduction of an elastic module
6,4%
Petrography study UNE-EN 12407:2001
Litoarenita

Reference works with "Arenisca Uncastillo"

Petrography:

 

Nicoles cruzados Nicoles paralelos
Crossed Parallel

Through the microscope, it is a sandstone, of fine grain (particles’ average diameter: 150 microns), in which the cement and part of its components are of calcitic composition. The texture is grain-supported and the stone lacks of matrix.

The detrital particles correspond to a mainly angular (32.1%) quartz and stone fragments (50.6%; silexitic, quartzitic/limolitic, calcitic and dolomitic stones). The cement (8.2%) is calcitic and increases the carbonated particles in a epitaxial way (in crystalline continuity). The opaque and ferruginous particles, of doubtful detrital form (they could be diagenetic) constitute 7.9% of the stone. The muscovite, tourmaline and rutile act as mineral accessories.

 

Geology:

 

Cantera Arenisca Uncastillo
   Quarry Arenisca Uncastillo
Cantera Arenisca Uncastillo
  Quarry Anisca Uncastillo
Cantera Arenisca Uncastillo Cantera Arenisca Uncastillo
Quarry Arenisca Uncastillo
Quarry Arenisca Uncastillo  
 
Geographically, the Uncastillo rock quarry is located in the Uncastillo’s municipality, in the province of Saragossa. 
 
Geologically, this material belongs to the Uncastillo formation which is the time of: Miocene inferior (Aquitaniense-Burdigaliense), (Puigdefábregas, 1975) equivalent to the Sariñena formation (Quirantes, 1978), located in the north of the Ebro’s Depression and in contact with the Outer Mountain ranges. The Uncastillo’s sanstone is a detrital sedimentary rock formed by the accumulation of fluvial currents’ depositions. This form of accumulation of the sediment allows layers that can be parallel or intercrossed, with certain variability in the grain size and the composition based on the river energy, to form. Thanks to the compaction’s process of these sediments and cementation’s process by chemical precipitation in the interstices, the stone acquires its characteristics of hardness and cohesion. 
 
The subhorizontal disposition of the Uncastillo’s sanstones layers allows OLNASA to do simple mechanical extraction, without the need of realizing great material's dismantling, which implies a low environmental and visual impact of the quarries.

 

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