Patio Paving Sandstone offers a durable and stylish solution for your outdoor space. With its natural sandstone composition, it provides a non-slip surface that is perfect for patios, walkways, and pool decks. Its high porosity allows for efficient drainage, ensuring a safer and long-lasting outdoor area. Impress your guests with the timeless beauty of Patio Paving Sandstone.
Slabs, tiles including walling tiles, and flooring tiles, kitchen countertops, vanity tops, work tops, window sills, skirting, steps & riser stairs.
Available Sizes
Tile size in 12“x12”(305x305mm), 18”x18”(457x457), 24”x24”(610x610mm), 36”x36”(914x914mm) etc.
Slab size in 2400upx1200up, 2400upx1600up etc.
Available Thickness
3/8”(10mm), 12mm, 15mm, 3/4”(20mm), 30mm or other thickness as customization.
Our advantages:
a) Owner of professional factories and quarries.
b) Experienced and have sophisticated craftsmanship.
c) With strict control of every process and quality-inspected.
d) Have big stock, prompt delivery and good fame in stone industry.
Patio paving sandstone is formed by quartz particles (sand) with stable structure, usually light brown or red, and mainly contains silicon, calcium, clay and iron oxide. patio paving sandstone is a kind of sedimentary rock, which is mainly formed by the cementation of sand, and the content of sand is more than half. Most sandstone is composed of quartz or feldspar. Let's introduce the main types of sandstone in detail below!
Quartz sandstone: The content of quartz and siliceous debris accounts for more than 95% of the total sand-grade debris, and it contains only a small amount or no feldspar, cuttings and heavy minerals. The detritus particles are often dominated by single crystal quartz, with good roundness and sortability, and the highest degree of maturity of composition and structure. Few hetero-bases and particle support. When the miscellaneous base> 15%, it is called quartz miscellaneous patio paving sandstone. Quartz sandstone is mainly formed in a stable geotectonic environment. The topography is quasi-plained. After long-term weathering of the parent rock, most of the products of denudation are formed in the ocean (such as beach) environment by strong selection of waves and currents and repeated erosion and slow deposition. . It often coexists with carbonate deposits, forming quartz sandstone-sea-forming carbonate structures, such as the Upper Precambrian in the Taipei half of North China.
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