The principle has been known for centuries and has proven its worth many times over – still, with „RATIO“, we managed to create a double depression interlocking pantile that is twice as good. We have taken over only the best characteristics of the proven classics „RATIO KLASSIK“ and „TECTA“ and developed them further to create a new tile. Thus, „RATIO“ combines the advantages of „TECTA“ and „RATIO KLASSIK“ – a sensible idea – and its proportions correspond to those of the original tile Z1. This is how the extremely harmonious „double depression roof geometry“, created by Ludowici in 1879, is combined with technical and economical advantages.
|Size:||approx. 265 x 445 mm|
| ||min. approx.||on av. approx.||max. approx.|
|Covering width:||221 mm||223 mm||225 mm|
|Covering length:||357 mm||368 mm||380 mm|
| ||max. approx.||on av. approx.||min. approx.|
|Tile requirement:||12,7 Pcs./m²||12,2 Pcs./m²||11,7 Pcs./m²|
|Weight||approx. 3,5 kg/pcs.||approx. 42,7 kg/m²|
|Small pack: 6 Piece||Pallet: 288 Piece|
|LAF = distance between laths and ridge intersection , FLA = distance between ridge laths|
Measurements apply to 30/50-laths.
In case of 40/60-laths, CREATON will supply the LAF-measurements on demand.
|Verge tiles, double bead, half-length||Ridge connection ventilation tile, shed tile|
|approx. 2.7 pcs./m||ca. 4,5 Stk./lfm.|
Extensive fluidic tests have confirmed the superior protection against the intrusion of rain of our model „RATIO NEU“. The sophisticated interlockings
allow for the protection against the intrusion fo rain in case of roof pitches of 20° by means of a trussing sheet (CREATON „UNO“), of 18° using a heat-sealed or bonded sub-coverage sheet (CREATON „DUO“), of 16° with a rainproof sub-roof (CREATON „TRIO“) necessary according to our conditions of warranty. We would be pleased to advise you with regard to the execution of the sub-roof area. In case of lath distances in the minimum/maximum limit range, it is absolutely necessary to indicate the lath distances in your order!
Mionor colour and size deviations are possible due to the natural variations of the raw clay.