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Product Information -
4. 14 DELUXE WORKTOPS
DELUXE OAk SNACk TOP 80 MM THICk.
IMPERIAL OAk WORkTOP
Produced by gluing the typical parquet plank,
consisting of a 4/5 mm leaf of solid wood mounted on
multi-layered birch, onto a multilayered poplar panel.
The bottom is enclosed with an 18 mm thick particle
board panel with Opticall3D finish on two sides.
Varnishing components: acrylic clear top coat.
QUERCUS/VINTAGE OAk WORkTOP
Produced by gluing solid wood 3/5 mm thick onto a
multilayered poplar panel. The underside is enclosed
with an 18 mm thick particle board panel with
Opticall3D finish on two sides.
Varnishing components:
Quercus oak: Water-based stain, acrylic top coat.
Vintage oak: Antibacterial water-based stain and top
coat.
4. 15 STONE WORKTOPS
STONE TH. 20 MM – UNION WORkTOP TH. 20 MM.
Made with slabs 20 mm thick of Piasentina Stone,
which is a sedimentary limestone of secondary origin,
generated by gravitational processes triggered by
tectonic movements of the Earth’s crust.
Front and side edging with stone profiles 20 mm thick.
In the UNION version the worktop has an integral
upstand 24 mm thick; the total thickness of the top
and upstand is 80 mm.
STONE TH. 30 MM – UNION WORkTOP TH. 30 MM.
Made with slabs 20 mm thick of Piasentina Stone,
which is a sedimentary limestone of secondary origin,
generated by gravitational processes triggered by
tectonic movements of the Earth’s crust.
Front and side edging with stone profiles 30 mm thick.
In the UNION version the worktop has an integral
upstand 24 mm thick; the total height of the top and
upstand is 80 mm.
STONE TH. 40 MM – UNION WORkTOP TH. 40 MM.
Made with slabs 20 mm thick of Piasentina Stone,
which is a sedimentary limestone of secondary origin,
generated by gravitational processes triggered by
tectonic movements of the Earth’s crust.
Front and side edging with stone profiles 40 mm high.
In the UNION version the worktop has an integral
upstand 24 mm thick; the total height of the top and
upstand is 80 mm.
STONE WORkTOP 60 MM THICk
Made with slabs 20 mm thick of Piasentina Stone,
which is a sedimentary limestone of secondary origin,