Herbert Smith CBE | |
---|---|
Born | Edgbaston, England | 26 May 1872
Died | 20 April 1953 80) | (aged
Education | Winchester College |
Alma mater | New College, Oxford |
Known for | Gemstones (1912) |
Scientific career | |
Fields | Mineralogy, gemmology |
Institutions | British Museum (Natural History), London |
George Frederick Herbert Smith CBE (26 May 1872 – 20 April 1953) was a British mineralogist who worked for the British Museum (Natural History). [1] He discovered the mineral paratacamite in 1906, and developed a jeweller's refractometer for the rapid identification of gems. [2] The minerals smithite and herbertsmithite are named after him, [1] as is Herbert's rock-wallaby. [3]
Smith was born in 1872, went to school at Winchester College and then to New College, Oxford. In Oxford, he studied mathematics from 1891 to 1895, gaining first class marks, and then graduated in physics in 1896. [4] Smith was appointed as an assistant in the British Museum (Natural History) in December 1896. [5] He worked in the mineralogy department of the museum until 1921, when he became assistant secretary of the museum, succeeding Charles E. Fagan. [6]
In his mineralogical career, Smith worked on topics including the determination of mineral structures and compositions. He wrote papers on the structure of the gold telluride mineral calaverite (AuTe2); [7] and he described the new copper-zinc oxychloride mineral paratacamite. [8] Smith also developed new instruments for the practical measurement of the crystallographic and optical features of minerals and gems (goniometers and a refractometer), [4] and wrote a text book on gemstones and gemmology that was first published in 1912, [9] [10] and went through many editions, with the thirteenth edition published in 1958. [11]
In his role as secretary of the museum, he oversaw the expansion of the museum and the creation of new buildings for the department of entomology; and he was in charge of the celebrations of the 50th anniversary of the Natural History museum in 1931. He also started the practice of selling postcards of museum items, and established a sports club for the staff of the museum. [6] He served as secretary of the museum until 1935, [12] before returning to the mineralogical department for two years before retirement. [4] He retired in 1937. [13]
In 1927, in conjunction with the Society of Civil Servants, Smith arranged for a special train to take civil servants to Richmond, Yorkshire, to view the solar eclipse. [14] [6] Smith provided pieces of smoked glass for viewing, and wrote a guide to the eclipse. Richmond was in the line of totality, and many thousands of visitors attended on fleets of special excursion trains that day, including Virginia Woolf, who described the events in her diary and in a 1928 essay The Sun and the Fish. [15] [16] At totality, the Sun was obscured by clouds. [6]
In 1918, Smith helped to establish the Society of Civil Servants 'to cover the middle and upper grades of the service'. [17] He was honorary secretary of this society from 1918 to 1925, vice-president from 1925 to 1928, and president for the period 1928 to 1932. [13]
Smith played a major role in the professional work of gemmologists in the United Kingdom. He set and marked the first diploma in gemmology (from 1912), [6] and was later an examiner for the Gemmological Association of Great Britain (Gem-A) from 1931 to 1951. He was elected president of the association from 1942 to 1953, and was awarded the title of honorary fellow in 1946. [18]
Smith served on the council of the Royal Albert Hall from 1930 to 1953, and worked for many years for the society for the promotion of nature reserves, which eventually became the UK government agency, Nature Conservancy in 1948 and the National Parks Commission in 1949. [6] [19]
In 1905, mineralogist R H Solly named a silver arsenic sulphide mineral (AgAsS2) smithite after Smith. This mineral was from the Lengenbach Quarry in the Binn valley, Switzerland. At that time, Smith was working on other minerals from the same location. [20] [6] In 2004, a copper zinc oxychloride mineral (ZnCu3(OH)6Cl2) herbertsmithite was named after Smith, since it was found to share chemical and structural features with paratacamite, which Smith had discovered in 1906. [21]
In 1926, Herbert's rock-wallaby, Petrogale herberti was named in Smith's honour, to reflect the assistance he had provided to Hubert Wilkins, on whose expedition the wallaby had been discovered. [3]
In June 1949, Smith was awarded the CBE for 'services to the flora and fauna of the British Isles'. [22]
Smith married Rosalie Ellerton (d. 1936), and they had a daughter. Smith died on 20 April 1953, after a short illness. [6]
Thortveitite is a rare mineral consisting of scandium yttrium silicate (Sc,Y)2Si2O7. It is the primary source of scandium. Occurrence is in granitic pegmatites. It was named after Olaus Thortveit, a Norwegian engineer. It is grayish-green, black or gray in color.
Painite is a very rare borate mineral. It was first found in Myanmar by British mineralogist and gem dealer Arthur C.D. Pain who misidentified it as ruby, until it was discovered as a new gemstone in the 1950s. When it was confirmed as a new mineral species, the mineral was named after him.
Hutchinsonite is a sulfosalt mineral of thallium, arsenic and lead with formula (Tl,Pb)2As5S9. Hutchinsonite is a rare hydrothermal mineral.
Herbert's rock-wallaby is a member of a group of seven very closely related rock-wallabies found in northeastern Queensland, Australia. Herbert's is the most southerly and most widespread of the group.
Herbertsmithite is a rhombohedral green-coloured mineral with chemical formula ZnCu3(OH)6Cl2. It is named after the mineralogist Herbert Smith (1872–1953) and was first found in 1972 in Chile. It is polymorphous with kapellasite and closely related to paratacamite. Herbertsmithite has also been found near Anarak, Iran, hence its other name, anarakite.
Tobermorite is a calcium silicate hydrate mineral with chemical formula: Ca5Si6O16(OH)2·4H2O or Ca5Si6(O,OH)18·5H2O.
Boleite is a complex halide mineral with formula: KPb26Ag9Cu24(OH)48Cl62. It was first described in 1891 as an oxychloride mineral. It is an isometric mineral which forms in deep-blue cubes. There are numerous minerals related to boleite, such as pseudoboleite, cumengite, and diaboleite, and these all have the same complex crystal structure. They all contain bright-blue cubic forms and are formed in altered zones of lead and copper deposits, produced during the reaction of chloride bearing solutions with primary sulfide minerals.
George Thurland Prior FRS was a British mineralogist. He made great contributions to mineralogical chemistry, petrology and meteoritics.
Vesselina Vassileva Breskovska was a 20th-century Bulgarian geologist, mineralogist and crystallographer.
Ivan Kostov Nikolov Hon HonFMinSoc, Aka Ivan Kostov, was a Bulgarian geologist, mineralogist and crystallographer.
Kostovite (IMA symbol: Ktv) is a rare orthorhombic-pyramidal gray white telluride mineral containing copper and gold with chemical formula AuCuTe4.
Bultfonteinite, originally dutoitspanite, is a pink, light-brown or colorless mineral with chemical formula Ca2SiO2(OH,F)4. It was discovered in 1903 or 1904 in the Bultfontein mine in South Africa, for which the mineral is named, and described in 1932.
Diaboleite is a blue-colored mineral with formula Pb2CuCl2(OH)4. It was discovered in England in 1923 and named diaboleite, from the Greek word διά and boleite, meaning "distinct from boleite". The mineral has since been found in a number of countries.
Paratacamite is a mineral in the halide minerals category. Its chemical formula is Cu3(Cu,Zn)(OH)6Cl2. Its name is derived from its association with atacamite. Paratacamite was first described by Herbert Smith in 1906. The zincian endmember Cu3(Zn)(OH)6Cl2 is called herbertsmithite, and paratacamite is polymorphous with botallackite and atacamite.
Fumarole minerals are minerals which are deposited by fumarole exhalations. They form when gases and compounds desublimate or precipitate out of condensates, forming mineral deposits. They are mostly associated with volcanoes following deposition from volcanic gas during an eruption or discharge from a volcanic vent or fumarole, but have been encountered on burning coal deposits as well. They can be black or multicoloured and are often unstable upon exposure to the atmosphere.
Lizardite is a mineral from the serpentine subgroup with formula Mg3(Si2O5)(OH)4, and the most common type of mineral in the subgroup. It is also a member of the kaolinite-serpentine group.
George William Brindley was a British-American crystallographer and mineralogist. He was known for his study of clay minerals including the structure of kaolinites.
Matteo Tondi was an Italian physician, mineralogist, and natural scientist. He contributed to studies in chemistry, mineralogy, ideas in geology, mining and metal refining. The mineral Tondiite is named after him.
Marie Louise Lindberg was a mineralogist. She was affiliated with the U.S. Geological Survey and noted for her studies of mineralogy in Brazil. Multiple species of mineral were first described by her, including frondelite, faheyite, moraesite, barbosalite, and tavorite. These 5 minerals were all described by her and various collaborators in the 1940s and 1950s, and sourced from a quarry in Galileia, Minas Gerais. As of March 1950, Lindberg held both Bachelor of Arts and Master of Arts degrees.
Smithite is a sulfosalt mineral with the chemical formula AgAsS2. It was first described by mineralogist R H Solly in 1905, in samples from the Lengenbach quarry near Binn, Switzerland, and was named for Herbert Smith, who was an assistant in the department of mineralogy of the British Museum. Smithite is a dimorph of trechmannite.