A material becomes specifiable at the moment its dimensions stop being adjectives.
Volcanic stone is often described to architects in the language of character and origin, which is accurate but unusable at detail stage: an architect resolving a threshold, a substrate build-up or a cantilevered basin needs millimetres.
The technical parameters set out below sit behind the lava stone surfaces in the collection and govern how lava behaves as a construction element rather than as an image.
Three numbers do most of the work in a lava stone specification: the thickness range of the flat formats, the size of block available for monolithic pieces, and the dimensional tolerance of tooled surfaces. Each carries a design consequence, and each is published rather than estimated.
What follows is the documented set, together with an explicit statement of where the published data stops. That boundary is as useful to a specifier as the figures themselves.
Thickness: 10, 20 and 30 mm Across the Flat Formats
The flat formats are produced in three thicknesses: 10, 20 and 30 mm. This applies across both the square and the bar geometries. Squares are made at 50 x 50 mm and 100 x 100 mm, each available in all three thicknesses. Bars are made at 300 x 25 mm and 600 x 40 mm, again across all three.
This has a direct consequence for build-up. A 10 mm module allows lava to be introduced as a cladding layer where the substrate depth is constrained, for instance over an existing floor or against a lightweight partition. A 30 mm module reads as a solid stone element and behaves accordingly in terms of weight and edge profile. The same colour and finish can therefore be carried across conditions of very different depth, which is what makes continuity possible between a floor field and a vertical return.
An older figure of three to four centimetres circulated in earlier material about lava thicknesses. The published range is 10 to 30 mm for flat formats and 30 to 50 mm for three-dimensional profiles, and specifications should work from those numbers.