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Countertops
Products >> Counter Tops

   

   

 

Granite

The composition of granite is primarily quartz, feldspars, micas, and other secondary materials. The distribution of these other minerals is what gives granite it’s many colors. Granite is extremely durable. It is one of the densest & hardest stones which makes it very scratch resistant. High gloss finishes are achieved by polishing with diamond pads. Lately, honed, brushed, & velvet finishes have become more popular for counter tops. Granites are quarried all over the world but most come from Brazil and India.

Marble

Marble is a metamorphic rock that forms first like a limestone but then undergoes a recrystalization. Many marbles have veins and softer lines that give it a more formal appearance. Marbles are most commonly finished to a high polish but can also be honed or tumbled. Many of the white marbles are quarried in Italy.

Limestone

Limestone is a sedimentary rock that result from millions of years of sediment being buried, compressed and cemented by precipitation from mineral rich waters. Limestones are most commonly finished with a honed surface but can also be polished or tumbled. Many times small fossils can be found imbedded into the stone.

Travertine

Travertine is a variety of limestone that is created when heated aquifer waters rise to the surface and leave layers of mineral granules. Over time, these deposits cool and crystallize into travertine. Many specimens maintain a linear appearance. Most travertine is imported from Turkey, Mexico, Italy, & Peru.

Onyx

Onyx is a translucent, semiprecious gem stone of a quartz variety with an extremely fine crystal formation. Colors range from whites to greens while displaying lots of fluid movement throughout the stone. For centuries the ancient Egyptians, Greeks, and Romans acknowledged Onyx for its mystical properties. In Greek, the name means “nail” or claw”. Many Onyx mines are found in Iran and Pakistan.

Slate

Slate - The metamorphic process of burial, compression, and heating creates first shale and then slate. Slate has a cleavage that allows it to be split into parallel sheets. This characteristic also gives slate its significant clefted appearance. Colors of slate vary from deep purples to grey green tones. Slate is adundant in Brazil and China but is also found in many areas of the United States.

Quartzite

Quartzite is composed of sandstone that has been metamorphosed. Quartzite is much harder than the parent rock, sandstone. It forms from sandstone that has come into contact with deeply buried magmas. Quartzite looks similar to it’s parent rock. The best way to tell quartzite from sandstone is to break the rocks. Sandstone will shatter into many individual grains of sand while quartzite will break across the grains. Colors range from greys to gold tones. Most quartzite quarrys are in India or China.
 

 
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