Green Moss Agate tumbled

Aquamarine tumbled is a valuable gem of delicate beauty, distinguished by its pale blue to light green color. It is mined in many localities around the world, but the most important ones are Brazil and India. Cut into beads, cabochons, and brilliants, aquamarine tumbled is used for jewelry making, but larger specimens can be carved into figures.

Citrine Quartz tumbled is valued for its transparency and marvelous yellow color that can vary from light to golden yellow, and even to honey and amber shades. Its low price and durability also affect its popularity. It is mined in numerous localities around the world, but the most important are Mexico, Brazil, Argentina, Uruguay, Bolivia, Madagascar, Russia, and Spain. It is commonly cut into faceted gems and used for jewelry.

A well-known member of the feldspar group, white Moonstone is renowned for its shimmering white luster; in fact, the ancient Romans believed this stone to have been formed from solidified moonlight. Although it is the state gemstone of Florida (to honor the Apollo moon landings), it is not actually found in that state.

Tourmaline gemstone is a unique gemstone renowned for its wide range of colors, including red, green, pink, blue, and multi-colored specimens. The most prized color of Tourmaline gemstone is considered to be the "Paraíba" variety, which is a bright, neon blue or greenish-blue color due to traces of copper. Tourmaline gemstone is found in many locations around the world, including Brazil, Afghanistan, and the United States.

Tumbled smoky Quartz tumbled is produced from the abundant material found in many localities around the world. It is prized as an affordable and inexpensive gem whose color varies from light brown to almost black. It is commonly faceted or cut into beads and cabochons, and regularly used with jewelry, particularly necklaces, rings, and pendants. Darker varieties are a popular choice for men's jewelry.

Apatite is a group of phosphate minerals, usually referring to hydroxyapatite, fluorapatite and chlorapatite, with high concentrations of OH, F and Cl ions, respectively, in the crystal. The formula of the admixture of the three most common endmembers is written as Ca10(PO4)6(OH,F,Cl)2, and the crystal unit cell formulae of the individual minerals are written as Ca10(PO4)6(OH)2, Ca10(PO4)6F2 and Ca10(PO4)6Cl2. The mineral was named apatite by the German geologist Abraham Gottlob Werner in 1786, although the specific mineral he had described was reclassified as fluorapatite in 1860 by the German mineralogist Karl Friedrich August Rammelsberg. Apatite is often mistaken for other minerals. This tendency is reflected in the mineral's name, which is derived from the Greek word απατείν (apatein), which means to deceive or to be misleading.