Blue pigments
Blue pigments are  natural or synthetic materials, usually made from minerals and  insoluble with water,  used to make the blue colors in painting and other arts. The raw material of the earliest blue pigment was lapis lazuli from mines in Afghanistan, that was refined into the pigment ultramarine. Since the late 18th and 19th century, blue pigments are largely synthetic, manufactured in laboratories and factories. Ultramarine 
Ultramarine was historically the most prestigious and expensive of blue pigments. It was produced from lapis lazuli, a mineral whose major source was the mines of Sar-e-Sang in what is now northeastern Afghanistan. It was transformed into a pigment by the Afghans beginning in about the 5th century, and exported by caravans to India. It was the most expensive blue used by Renaissance artists. It was often reserved for special purposes, such as painting the robes of the Virgin Mary. Johannes Vermeer used ultramarine only for the most important surfaces where he wanted to attract attention. Pietro Perugino, in his depiction of the Madonna and Child on the Certosa de Pavio Altarpiece, painted only the top level of the Virgin's robes in ultramarine, with azurite beneath. Ultramarine became more widely used after its successful synthesis in the 19th century, which reduced its price substantially. In 1814, a French chemist named Tassaert observed the spontaneous formation of a blue compound, very similar to ultramarine, in a lime kiln at St. Gobain. In 1824, the  offered  a prize for the artificial production of the precious color. Processes were devised independently by Jean Baptiste Guimet (1826) and Christian Gmelin (1828); while Guimet kept his process a secret, Gmelin published his, and thus became the originator of the French synthetic ultramarine industry. At the beginning of the 19th century, the price of a kilogram of lapis lazuli was between six and ten thousand francs. The price of artificial ultramarine was less than eight hundred francs per kilogram. Synthetic ultramarine was widely appreciated by the French impressionists, and Vincent van Gogh used both French ultramarine and cobalt blue for his painting The Starry Night (1889). Cobalt blue 
Cobalt blue is a synthetic blue pigment was invented in 1803 as a rival to ultramarine. It was made by the process of sintering, that is by compacting and forming a solid mass of material by heat or pressure without melting it to the point of liquefaction. It combined cobalt(II) oxide with aluminum(III) oxide (alumina) at 1200 °C. It was also used as colorant, particularly in blue glass and as the blue pigment used for centuries in Chinese blue and white porcelain, beginning in the late eighth or early ninth century. Cobalt glass, or Smalt, is a variation of cobalt blue. It is made of ground blue potassium glass containing cobalt blue. It was widely used in painting in the 16th and the 17th centuries. Smalt was popular because of its low cost; it was widely used by Dutch and Flemish painters, including Hans Holbein the Younger. Egyptian Blue 
Egyptian blue was the first synthetic blue pigment. It was made from a mixture of silica, lime, copper, and an alkali. It was widely used in The Fourth Dynasty of ancient Egypt (c. 2613 to 2494 BC). Egyptian blue is responsible for the blue colour seen very commonly in Egyptian faience. Cerulean blue 
Cerulean blue was created in 1789 by the Swiss chemist Albrecht Höpfner. Subsequently, there was a limited German production under the name of Cölinblau. The primary chemical constituent of the pigment is cobalt(II) stannate (). Han blue 
Han blue (also called Chinese blue) is a synthetic barium copper silicate pigment used in ancient and imperial China from the Western Zhou period (1045–771 BC) until the end of the Han dynasty (circa 220 AD). Han blue and the chemically related Han purple were used to decorate hu vessels during the Han dynasty, and were also used for mural paintings in tombs of the same period. Maya blue 
Maya blue is a synthetic turquoise-blue pigment made by infusing indigo dyes (particularly those derived from the anil shrub) into palygorskite, a clay that binds and stabilises the indigo such that it becomes resistant to weathering. Developed in Mesoamerica in the first millennium AD, it saw wide use in the region, most prominently in the art of the Maya civilisation. It is known on media from pottery to murals to codices, and also played an important role in ritual sacrifices of both objects and people: silt at the bottom of the Sacred Cenote at Chichén Itzá is heavily stained with Maya blue, washed off the hundreds of sacrificial offerings cast into the cenote during the city's occupation. Maya blue continued to be used into the Spanish colonial period; though falling out of widespread use in the Maya region during the 16th century, some areas apparently continued to produce it for export, as Cuban colonial paintings of the 18th and 19th century have been found to make use of Maya blue probably imported from Campeche. Prussian Blue 
Prussian blue is a dark blue pigment containing iron and cyanide produced by the oxidation of ferrous ferrocyanide salts. It was invented in Berlin between 1704 and 1710. It had an immediate impact on the pigment market, because its intense deep blue color approached the quality of ultramarine at a much lower price. It was widely adapted by major European artists, notably Thomas Gainsborough and Canaletto, who used it to paint the Venetian sky. It was also used by Japanese artists, including Hokusai, for the deeper blues of waves. Azurite 
Azurite pigment is derived from the soft, deep-blue copper mineral of the same name, which forms from the weathering of copper ore deposits. It was mentioned in Pliny the Elder's Natural History under the Greek name kuanos (κυανός: "deep blue," root of English cyan) and the Latin name caeruleum. The modern English name of the mineral reflects this association, since both azurite and azure are derived via Arabic from the Persian lazhward (لاژورد), an area known for its deposits of another deep-blue stone, lapis. Azurite was often used in the Renaissance and later as a less expensive substitute for ultramarine. Lower layers would be painted in azurite, with the most visible portions painted in ultramarine. The drawback of the pigment is that it degrades and darkens over time. List of inorganic blue pigments

This is a list of blue inorganic pigments, both natural and synthetic. :

Aluminium pigments

Ultramarine (PB29): a synthetic or naturally occurring sulfur-containing silicate mineral -  (generalized formula)
Persian blue: made by grinding up the mineral Lapis lazuli. The most important mineral component of lapis lazuli is lazurite (25% to 40%), a feldspathoid silicate mineral with the formula . Cobalt pigments

Cobalt blue (PB28): cobalt(II) aluminate. Cerulean blue (PB35): cobalt(II) stannate. Cerium uranium blue

Copper pigments

Egyptian blue: a synthetic pigment of calcium copper silicate (CaCuSi4O10). Thought to be the first synthetically produced pigment. Han blue: BaCuSi4O10. Azurite: cupric carbonate hydroxide (Cu3(CO3)2(OH)2). Basic copper carbonate: Cu2(OH)2CO3. Iron pigments

Prussian blue (PB27):  a synthetic inert pigment made of iron and cyanide: C18Fe7N18. Manganese pigments

YInMn Blue: a synthetic pigment discovered in 2009 (YIn1−xMnxO3). Manganese blue: barium manganate(VI) sulfate. Notes and citations

Bibliography 
 
 
 

Pigments