Paul Heinrich Ritter von Groth, known as Paul Groth, was a German mineralogist and crystallographer born June 23, 1843, in Magdeburg, Germany, who died December 2, 1927, in Munich, Germany, and whose most important contribution was a systematic classification of minerals by their chemical composition and crystal structure; in 1888 he was among the first to propose that spherical atoms occupy equivalent positions within space lattices. He founded the journal Zeitschrift fuer Krystallographie und Mineralogie in 1877 and edited it until 1920, compiled the five-volume Chemische Kristallographie beginning in 1883, and published Tabellarische Uebersicht der einfachen Mineralien between 1874 and 1898 and Physikalische Krystallographie between 1876 and 1905. He held professorships of mineralogy at the University of Strasbourg from 1872 and at Munich, where he also curated minerals at the Deutsches Museum from 1883, was elected a Foreign Member of the Royal Society, was a member of multiple national academies, and received the Wollaston Medal in 1908.
Facts
Notable WorkSystematic classification of minerals by chemical composition and crystal structure 1 In the Other Atlases
- Also in Geography Atlas: Germany, nationality there.
Sources
1. Paul Heinrich von Groth, Wikipedia
Lead sentence, birth date
Paul Heinrich Ritter von Groth (23 June 1843 - 2 December 1927) was a German mineralogist.
Lead sentence, birth year
Paul Heinrich Ritter von Groth (23 June 1843 - 2 December 1927) was a German mineralogist.
Lead sentence, death date
Paul Heinrich Ritter von Groth (23 June 1843 - 2 December 1927) was a German mineralogist.
Lead sentence, death year
Paul Heinrich Ritter von Groth (23 June 1843 - 2 December 1927) was a German mineralogist.
Lead sentence, nationality
Paul Heinrich Ritter von Groth (23 June 1843 - 2 December 1927) was a German mineralogist.
Lead sentence, profession
Paul Heinrich Ritter von Groth (23 June 1843 - 2 December 1927) was a German mineralogist.
Lead paragraph, contribution
His most important contribution to science was his systematic classification of minerals based on their chemical compositions and crystal structures.
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