Harmony Stone National Tiles, Industrial Tiles, Tiles, Travertine Tiles, Marble Tiles, French Pattern Tiles, Ledger Panels, Rumbles, Splitfaces, Stack Stones, Accessories, Wok, Mouldings

Pavers, Stone Pavers, Copings, Remodeling Copings, Copings, Remodeling Copings, Mosaic Collections, Vanilla Beige, Silver Shadow, Silver Mosaics,

1x1 Mystic Glass Collection, Shellstone Mosaics, Solto White Mosaics, Luna Sky, Patara Mosaics, Dolomite Mosaics, Mugla White Mosaics, Veneer Collections,

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All pavers are 1 and 1/4 (1.25″) inch thick.

French Pattern Pavers are a bundle set of the following sizes (1¼” thick): 8”x8”, 8”x16”, 16”x16”, 16”x24”.

French Pattern Tiles are a bundle set of the following sizes (0.5″ thick): 8”x8”, 8”x16”, 16”x16”, 16”x24”.

Yes, our hours are Monday to Friday 8:30am – 5pm. We are located at 3900 S. 50th Street, Tampa, FL 33619.

We sell natural stone products such as travertine tiles and pavers, marble tiles, mosaics, and pool copings.

Travertine colors range from warm- to medium-toned neutrals.
You’ll find travertine pavers, slabs, and tiles in soft and warm neutral hues, including ivory, gold, beige, brown, rust, and peach. Typically, the color swirls and waves throughout the stone, creating unique patterns that give travertine its timeless beauty.

Marble is formed by heat and pressure in the earth’s crust. The metamorphic process from sedimentary rocks causes a complete recrystallization of the calcium carbonate. The combined action of temperature and pressure, during the transformation of the sedimentary rock into marble, leads to the progressive obliteration of the structures and textures originally present in the rock. This process leads to the destruction of any fossil, stratification or other sedimentary structure present in the original rock.
Travertine is formed under additional high pressures and temperatures, in hot springs and limestone caves. The formation of travertine is related to the rise and release on the surface, in correspondence with the outlet of springs, of thermo-mineral waters very rich in calcium carbonate (which represents the main component of travertine). Its birth, due to a continuous and progressive accumulation of carbonate material from the areas of dissolution to those of deposition, led to a sedimentation of these rocks according to parallel horizontal stratifications, sometimes marked by variations in color and diffuse porosity.