This slab

The recorded size of a slab in this lot is 107″ × 68″, about 51 square feet. Thickness is 2 cm. The color on record is cream with beige. Natural stone still varies inside that description, so the slab itself is the reference for movement and shade. Saint Beauzire is also known as Zola Beige. Searching either name should lead to this same material. This material is recorded as quarried in Morocco.

The leather finish is lightly textured, with a softer look than a full polish. Two centimeters is a standard slab thickness for counters, vanities, and wall cladding.

In the slab gallery

The slabs can be seen in person at our Los Angeles slab gallery before anything is cut.

Where it works

For this kind of stone, the usual applications are floors, wall cladding, and vanities. The right use still depends on the finish, the thickness, and how the slab will be cared for after it is installed. Inspiration photos show this stone in a Floor.

The material

Limestone is a sedimentary stone, usually calmer in pattern than marble, with a soft mineral color. It is more porous than granite and is a frequent choice for floors, cladding, and vanities. Honed and brushed finishes suit its matte character. Acidic products can etch it, and a sealer is often part of the care plan. Slabs from the same lot are the right set to compare for shade before they are cut.

About Saint Beauzire

Saint Beauzire, also known as Zola Beige, is an exquisite limestone primarily quarried in Morocco. Distinguished by its warm, creamy ivory background and remarkably consistent texture, it offers a serene aesthetic that captures and reflects natural light. This sedimentary stone is prized for its fine grain and dense structure, making it a durable choice for interior flooring, wall cladding, and bathroom surfaces. A fascinating characteristic of Moroccan limestone is its origin in ancient seabed deposits; the stone often contains subtle, calcified remnants of prehistoric marine life, serving as a silent, million-year-old record of the earth’s geological evolution.