Verde san francisco granite countertops

Every slab of natural stone is completely unique. Verde Bamboo is a truly unique granite that has a light moss green color with diagonal veining throughout. It makes an artistic statement when used as a kitchen countertop, bathroom vanity top, backsplash, fireplace surround, bar top or an outdoor surface. Wherever you install it, Verde Bamboo granite is truly one of the most beautiful natural stones that you can find.

Beyond the visual improvement your home will see, Verde Bamboo granite is also a very durable material. It will be able to stand up to the wear and tear that it will face in various areas of the home.

Between the beauty, durability and the many other positive qualities this stone has, Verde Bamboo granite is truly one of the best materials you can choose to complete your home remodeling project.

Installing it can very well end up being one of the best decisions that you ever make for your home. Costa Esmeralda Italy. Costa Esmeralda Extra. Giallo Arctic Leather. Call now for assistance: Visit our Virtual Yard. Toggle navigation. My account Favorites Sign in. Home Countertops Granite. Get Your Countertop Estimate Today! You must be logged in before you can vote.

Verde Bamboo. Your review. Review guidelines. When writing a review, leave a title and write a concise and detailed summary of what you thought of our products. Block Sizes: This is a quarry yielding selectable, grades of granite with blocks suitable for gangsaw size down to economical tile-sized blocks.

For commercial projects it is important to ensure that blocks are selected from the same quarry face. Rough blocks are usually exported by Break Bulk however intermodal containerisation is available at extra cost. Finished products are packed into sea-worthy wooden crates and loaded into containers.

Francisco, Verde S. Gneiss: A high grade metamorphic rock. Gneiss is medium to coarse-grained and may contain abundant quartz and feldspar, which some petrographers regard as essential components. The banding is usually due to the presence of differing proportions of minerals in the various bands; dark and light bands may alternate because of the separation of mafic dark and felsic light minerals. Banding can also be caused by differing grain sizes of the same minerals. The mineralogy of a particular gneiss is a result of the complex interaction of original rock composition, pressure and temperature of metamorphism, and the addition or loss of components.

Metatexite: Migmatites are sometimes sub-divided into metatexites, that have experienced low degrees of partial melting, or diatexites, that have experienced high degrees.