Bahama Blue Granite Tombstone

Crafted from stunning Bahama Blue Granite, this tombstone is a timeless and durable tribute to your loved one. Known for its unique blue and white swirls, this granite is not only visually striking but also resistant to natural elements. Honor your loved one with this elegant and lasting memorial.

This problem is often mentioned by consumers, but compared to marble, bahama blue granite tombstone can be said to "never fade". But in the long run, granite will fade, it's just time.

The minerals in bahama blue granite tombstone are mainly composed of feldspar, quartz, mica, pyroxene, hornblende and so on. In the main silicate mineral structure, each silicon ion is surrounded by four oxygen ions to form a silicon-oxygen tetrahedron. This basic structural unit has very stable properties, strong acid and alkali resistance, hard to dissolve, weathering resistance, and good discoloration.

The fading of bahama blue granite tombstone is also different due to different types of stone. Generally speaking, darker and lighter granite is easy to fade, because the mineral composition of darker (such as black, dark green) bahama blue granite tombstone is mainly pyroxene, amphibole, basic plagioclase, and magnetite Wait. The light-colored bahama blue granite tombstone is mainly acid plagioclase, potash feldspar, biotite, quartz and so on. Minerals are generally formed underground, some minerals are formed first, and some are formed later. The first ones are often those with heavier atomic weight, deeper positions, less oxygen supply, and greater pressure; the latter ones are the opposite. Therefore, different minerals generally have different formation periods, and the order is roughly: dark minerals: olivine-pyroxene-hornblende-biotite; light-colored minerals: basic plagioclase-acid plagioclase-potash Stone-quartz. After the first minerals are exposed to the earth's surface, due to major changes in the environment, secondary changes are prone to occur, while the later minerals have less changes, and the most stable is quartz. Another situation is that secondary minerals are easier to fade than primary minerals. For example, green and grass-green veneer plates with epidote and chlorite as the main component have faded in color after 5 to 10 years, but they are similar to marble. In comparison, this change is still very weak. The color change (fading) is also related to the environment. The high acid-base content in the air in the industrial zone is easy to change and fade. In addition, the degree of maintenance is also very important.