Mathematician Stamps

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  • Maderno Carlo (1556-1629)



Known as an architect who used his mathematical knowledge in the building of spectacular buildings such as the Petersdom. Born 1556, died 1629. Maderno came to Rome in 1588, and started working for his uncle, Domenico Fontana.In 1603, he completed the façade of Santa Susanna. His design broke with the Mannerist style, and announced the new Baroque style. The façade of Santa Susanna and the dome of Sant'Andrea della Valle are considered his masterpieces. He was appointed as architect of San Pietro in aticano in 1603. Maderno chSan Giovanni dei Fiorentinianged Michelangelo's plan by elongating the centralized plan. He completed the façade in 1612.He started building the Palazzo Barberini, which was completed after his death by Bernini.Maderno


  • Magnus Albertus (1193-1280)



Albertus Magnus, German scholastic scientist; the preeminent medieval man of science; teacher of Thomas Aquinas.


  • Majreeti Abu al-Qasem al- (950-1007)


MAJREETI, Abu al-Qasem al- (950-1007) Spanish-Arab mathematician, astronomer, author - Jordan 1278.




  • Malaspina Alejandro (1754-1809)


A Scientist from Spain who performed measurements of the Spain Pacific territory.


  • Maupertuis Pierre Louis de (1698-1759)



Maupertuis

A joint issue of France and Finland commemorates simultaneous 1736 French expeditions to the equator in South America and the polar regions of Lapland to determine the shape of the earth, generally acknowledged to be spherical. Charles LaCondamine (1701-1774) in Peru and Pierre Maupertuis (1698-1759) in Lapland surveyed the curvature of the meridians and found that the earth was somewhat flattened at the pole, and more curved at the equator, giving it the shape of an oblate spheroid. Maupertuis developed a theory of the evolution of species. He writes: “Chance one might say, turned out a vast number of individuals; a small proportion of these were organized in such a manner that the animals organs could satisfy their needs. A much greater number showed neither adaptation nor order; These last have all perished -- thus the species which we see today are but a small part of all those that a blind destiny has produced." Essaie de Cosmologie


Stamp: France 1986


  • Mercator Gerardus (1512-1594)



Biography


Latin name of Gerhard Kremer, was a Flemish cartographer, geographer and mathematician best known for his mapping work, especially the Mercator projection, which used straight lines to indicate latitude and longitude. He was born in Rupelmonde. In 1537 he produced his first map. Mercator studied in Leuven, Belgium, under Gemma Frisius, and in 1552 he became a mapmaker and lecturer at the University of Duisburg. His map of Europe (published in 1554) was the best of its kind for many decades. He produced a map of the British Isles in 1564 and in the same year was made court cosmographer to Duke William of Cleve. In 1568 he devised and produced a system of map projection, now called Mercator projection. This system represents meridians by parallel lines and parallels of latitude by straight lines intersecting the meridians at right angles. The projection's graphic distortions of the relative sizes of countries and continents affects global thinking for four hundreds years. He also invents the word atlas, to describe a book of maps. Only four copies of this map are known to exist. Mercator's great Atlas (begun in 1569), in which he sought to describe the creation and history of the world, was printed in its unfinished state by his son in 1595.



  • Milankovic Milutin (1879-1958)



Serbian mathematician and astronomer described the changes of climate due to the changing radiation that is received from the sun.
Stamp: Yugoslavia 1979. Milutin Milanković (a.k.a. Milankovitch) (May 28, 1879, Dalj near Osijek - December 12, 1958, Belgrade) was a Serbian geophysicist, best known for his theory of ice ages, relating variations of the earths orbit and long-term climate change, now known as Milankovitch cycles. Milankovic attended the Vienna Institute of Technology where he graduated in Civil Engineering in 1902 and earned a doctorate in technical sciences in 1904. Later he worked in then famous firm of Adolf Baron Pittel Betonbau-Unternehmung in Vienna. He built dams, bridges, viaducts, aqueducts and other structures in reinforced concrete throughout the Austria-Hungary of the time. Milankovic continued to practice civil engineering in Vienna until the autumn of 1909 when he was offered the chair of applied mathematics (rational mechanics, celestial mechanics, theoretical physics) in Belgrade. The year 1909 marked a turning point in his life. Though he continued to pursue his investigations of various problems pertaining to the application of reinforced concrete, he decided to concentrate on fundamental research.

Turbulent events took place as soon as he had settled down in Belgrade when the Balkan Wars were followed by World War I. When the war broke out in 1914 (he was just married), he was interned by Austro-Hungarian army in Nezsider and later in Budapest, where he was allowed to work in the library of the Hungarian Academy of Sciences. As early as 1912, his interests turned to solar climates and temperatures prevailing on the planets. Throughout his internment in Budapest he devoted his time to the work in this field and, by the end of the war, he had finished a monograph on the problem which was published in 1920, in the editions of the Yugoslav Academy of Sciences and Arts by Gauthiers-Villards in Paris, under the title Théorie mathématique des phénomènes thermiques produits par la radiation solaire (Mathematical theory of thermic phenomena caused by solar radiations).

The results set forth in this work won him a considerable reputation in the scientific world, notably for his curve of insolation at the Earth's surface. This solar curve was not really accepted until 1924 when the great meteorologist and climatologist Vladimir Koeppen with his son-in-law Alfred Wegener, introduced the curve in their work, entitled "Climates of the geological past". After these first tributes, Milankovic was invited, in 1927, to cooperate in two important publications: the first was a handbook on climatology (Handbuch der Klimatologie) and the second a handbook on geophysics (Guttenberg's Handbuch der Geophysik). For the former, he wrote the introduction Mathematische Klimalehre und astronomische Theorie der Klimaschwankungen (Mathematical science of climate and astronomical theory of the variations of the climate), published in 1930 in German and in 1939 translated into Russian. Here the theory of planetary climate is further developed with special reference to the Earth.

For the second textbook, Milankovic wrote four sections developing and formulating his theory of the secular motion of the Earth's poles and his theory of glacial periods (Milankovitch cycles), which was built on earlier work by James Croll. Milankovitch was able to advance on Croll's work partly by improved calculations of the earths orbit then recently published by Ludwig Pilgim in 1904. Fully aware that his theory of solar radiation had been successfully completed and that the papers dealing with this theory were dispersed in separate publications, he decided to collect and publish them under a single cover. Thus, in 1941, on the eve of war in his country, the printing of his great work Kanon der Erdbestrahlung und seine Anwendung auf das Eiszeitenproblem (Canon of Insolation of the Earth and Its Application to the Problem of the Ice Ages) was completed, 626 pages in quarto, in Cemian, published in the editions of the Royal Serbian Academy. This work was translated into English under the title Canon of Insolation of the Ice-Age Problem, in 1969 by the Israel Program for Scientific Translations and published for the U.S. Department of commerce and the National Science Foundation, Washington, D.C.

Objections were raised in the 1950s against the Milankovic theory of ice ages; these objections came mainly from meteorologists who claimed that the insolation changes due to the changes in the Earth's orbital elements were too small to significantly perturb the climate system. However, in the late 1960s and 1970s, investigation of the deep-sea sediments brought widespread acceptance of Milankovic's view, since the periodicity discovered (100,000 years) matched so closely with the longest orbital period - see Ice age for more discussion.


  • Monge Gaspard (1746-1818)


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