Cinza Alpendurada Granite

Cinza Alpendurada Granite, alternatively referred to as Alpendurada Grey Granite, emerges as a captivating natural stone sourced from the quarries of Alpendurada in the Favões region, within the municipality of Marco de Canavezes in Porto, Portugal. This granite variety boasts a unique blend of qualities that make it an exceptional choice for various design applications.

The defining characteristic of Cinza Alpendurada Granite lies in its captivating gray hue. This granite features a delightful mix of tones that range from light to medium gray, creating a palette that is versatile and adaptable to various design aesthetics. The granite's cool and composed color serves as an elegant canvas for both modern and traditional settings.

A distinctive aspect of this granite is the presence of two-mica minerals, which contribute to its intriguing texture. The granular medium and, at times, mega crystals of feldspar add depth and visual interest to the stone's surface. These mineral formations create a mesmerizing interplay of light and shadows, transforming the granite into a dynamic work of art.

Hailing from the quarries of Alpendurada in Porto, Cinza Alpendurada Granite embodies the geological heritage of the region. The history and character of this area are imprinted onto each slab, reflecting the intricate processes that have shaped it over time.

Cinza Alpendurada Granite, also known as Alpendurada Grey Granite, stands as a tribute to the natural beauty inherent in the Earth's formations. Its captivating gray tones, intricate mineral patterns, and textured surface celebrate the harmonious relationship between geological forces and human craftsmanship. Whether employed in flooring, countertops, or other design elements, this granite variety adds an element of timelessness and sophistication to any environment.

Open porosity :: 0.55%

Dilatación linear thermal coefficient maximum value :: 9.1 x 10-6 per ° C
Wear resistance :: 0.2 mm
Shock resistance :: 65 cm
not noticed any changes in color or in the structure of the specimens in the late 25 freeze-thaw cycles.