Red Sandstone Floor Tiles

Expertly crafted from elegant red sandstone, these floor tiles add a touch of natural warmth to any space. With a timeless appeal and durable composition, they are perfect for both indoor and outdoor use. Durable, beautiful, and versatile - elevate your home or office with these stunning red sandstone floor tiles.

Feature	Details
Material	Natural Sandstone
Surface Finished	Honed, Flamed, Bush-hammered, Nature, Mushroom, Swan etc
Finished Products	Floor tiles, Wall cladding, Countertops, Windowsills, Special-shaped tiles,  Small slabs, Swimming pool, Steps, Wall panel, Flooring, Veneers, Slabs, Coping tiles, etc
Color	Yellow, Black, White, Red,Purple Wood, green,Grey,Rainbow etc
Finished	Honed, Split, Sandblasted, Sawn, Antiqued, Pineapple, etc.
Quality details	Polished degree: 95 degree or up. Thickness tolerance: +/-0.5mm. Diagonal tolerance: +/-1mm. Surface flatness tolerance: +/-0.3mm. Adjacent edge verticality tolerance: +/-0.5mm, Precise Cutting by infrared-ray-cut machine
Usage	For internal & external decoration and construction, Walling or flooring tile.
Edgeing	Full Bullnose, Half bullnose, Flat eased (eased edge), Bevel top, Radius Top, Laminated Countertop, Ogee Edge, DuPont, Edge, Beveled or others.
Size	Standard (But if you have special requirements, you can consult our CSA.)
Surface Finish	Polished, Flamed,Honed, Bush Hammered-sandblast, Chisselled.
Package	Fumigation wooden crates;Slab:fumigation wooden bundles
Payment	T/T 30% Deposite

 

Volcanic Tuff

1. Red Sandstone Floor Tiles Composition:

① Glass Debris (≈ 35%)

• Red, mostly arc-shaped, pumice-shaped, and irregularly shaped.
• Particle size: 0.7mm.
• Completely extinct under orthogonal light, indicating vitreous nature.
• Some glass chips are zeolized, containing lath-shaped zeolite crystals, making them colorless and transparent.

② Crystal Chips (≈ 25%)

• Plagioclase: Bright feldspar crystals with weak secondary changes and step-like broken edges. Some appear as single crystals, while others are polycrystalline and covered with darkened minerals. Twin crystals, including Kana composite twins, are visible.
• Quartz: Present in small amounts, cracked, and eroded.
• Biotite: Mostly darkened, but cleavage and pleochroism remain visible.

③ Cuttings (≈ 5%)

• Andesite: Shows a porphyritic structure, with plagioclase phenocrysts and a fine lath plagioclase matrix rich in iron minerals. Some exhibit an interwoven structure of glass crystals.
• Matrix: Contains chlorite.
• Tuff: Glassy crystalline tuff composed of plagioclase and biotite.

④ Pulp Chips (≈ 15%)

• Irregularly shaped, large in size.
• Interior has a twisted texture and vitreous nature.
• Some individuals show devitrification with visible chlorite.

⑤ Volcanic Dust (5%–35%)

• Glassy with no microstructure.
• Appears colorless and transparent under monolithic light.

2. Comprehensive Naming:

Purple-red magma-bearing crystalline debris tuff