Product: South Natural Slate Color & Size: Black (1x1) Pasted on Net size 300x300mm
Lime 3D Pink, Green n Peacock Ledge
Lime Green Ledge
Lime pink hand Cutting 600x150mm
Lime Pink Ledge
Lime stone BUCHING 600x150mm chocolate
Lime stone BUCHING 600x150mm Pattern-3
Black Absoluto - Headstone with 3 sides Rock Pitch / Punched
Pebbles are sediments of rounded and smooth appearance in size of more than two millimeters Pebbles are composed of preexisting natural rocks and artificial materials Pebbles typically occur in a variety of different colors and textures Applications Construction Water treatment filtration media
Quartzite Bolls
Rever
40 mm
Quartzite Rubble
Quartzite 10mm
Quartzite 65mm
Quartzite 25mm
Quartzite 20MM
Quartzite is a naturally occurring metamorphic rock composed mainly of quartz, which is a mineral that belongs to the group of silicate minerals. It forms when sandstone is subjected to intense heat and pressure deep within the earth's crust. This process causes the sand grains in the sandstone to recrystallize and fuse together into a dense, hard rock. Quartzite is a very hard and durable rock that is resistant to both chemical and physical weathering. It is commonly used in construction and landscaping applications because of its durability and attractive appearance. Quartzite is often used as a building stone, flooring material, and as a decorative stone in gardens and landscapes.
Pegmatite is a type of igneous rock that is characterized by its unique texture and mineral composition. It is known for its exceptionally large crystals and often contains valuable minerals and gemstones. Here are some key features and information about pegmatite: Pegmatites are primarily composed of quartz, feldspar (especially potassium feldspar), and mica. These minerals are often found in exceptionally large crystals within pegmatite veins. The most distinguishing feature of pegmatite is its coarse-grained texture. It contains crystals that are much larger than those found in typical igneous rocks. Crystals can range from a few centimeters to several meters in size. Pegmatites are formed through the slow cooling of magma deep within the Earth's crust. The slow cooling allows for the growth of large crystals. Additionally, the composition of the magma and the presence of volatiles (such as water and gases) play a role in the formation of Pegmatites. Pegmatites are known for their mineral diversity. They can contain a wide variety of minerals, including not only quartz, feldspar, and mica but also rare and valuable minerals such as tourmaline, beryl, garnet, and spodumene. Because of their association with valuable minerals and gemstones, Pegmatites are often of interest to mineral collectors and gemstone enthusiasts. Some of the world's most famous gemstone deposits are associated with Pegmatites.
-M. Black Lanters, ( L 1800-2400) x ( W 900-1200) x (Thickness 150-200)
