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== Biography ==
Arduino was born on 16 October 1714 at [[Caprino Veronese]], a small village in the [[Republic of Venice]], from a poor family of farmers. His brother was the [[botanist]] [[Pietro Arduino]]. He studied at Verona but did not take a degree. At eighteen he began an apprenticeship as a technician in the iron mines in [[Klausen, South Tyrol]], and [[Bolzano]], northern Italy. Arduino became quickly knowledgeable about mineralogy and [[metallurgy]] and developed an interest in [[paleontology]]. As a result of his practical experience he became recognized as a [[mining]] expert, in which capacity he served several Italian administrations.{{sfn|Rodolico|1970|p=233}} In 1769, Arduino was nominated agricultural superintendent of the Venetian Republic. He finally became professor of [[mineralogy]] at the [[University of Padua]] and a member of the [[Accademia nazionale delle scienze]]. Giovanni Arduino died in [[Venice]] in 1795. The [[Moon|lunar]] ridge [[Dorsum Arduino]] is named after him.
== Contributions ==
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* {{cite journal |last1=Arduino |first1=Giovanni |title=Lettera Segonda di Giovanni Arduino … sopra varie sue osservazioni fatte in diverse parti del territorio di Vicenza, ed altrove, apparenenti alla Teoria terrestre, ed alla Mineralogia |journal=Nuova Raccolta d'Opuscoli Scientifici e Filologici [New collection of scientific and philogical pamphlets] |date=1760 |volume=6 |pages=133 (cxxxiii)–180(clxxx) |trans-title=Second letter of Giovani Arduino … on his various observations made in different parts of the territory of Vincenza, and elsewhere, concerning the theory of the earth and mineralogy |language=it}} Available at: [https://bibdig.museogalileo.it/Teca/Viewer;jsessionid=3160EE486323866602B9590459D7111B?an=323812_6 Museo Galileo (Florence (Firenze), Italy)] From p. 158 (clviii): ''"Per quanto ho potuto sinora osservavare, la serie di questi strati, che compongono la corteccia visibile della terra, mi pare distinta in quattro ordini generali, e successivi, senza considerarvi il mare."'' (As far as I have been able to observe, the series of these layers that compose the visible crust of the earth seems to me distinct in four general orders, and successive, not considering the sea.)
* English translation: {{cite journal |last1=Ell |first1=Theodore |title=Two letters of Signor Giovanni Arduino, concerning his natural observations: first full English translation. Part 2. |journal=Earth Sciences History |date=2012 |volume=31 |issue=2 |pages=168–192|doi=10.17704/eshi.31.2.c2q4076006wn7751 |bibcode=2012ESHis..31..168E }}</ref> which was based on much study of rocks of the southern [[Alps]], grouped the rocks into four series. These were (in addition to the Volcanic or Quaternary) as follows: the Primary series, which consisted of [[schist]]s from the core of the mountains; the Secondary, which consisted of the hard [[sedimentary rock]]s on the mountain flanks; and the Tertiary, which consisted of the less hardened sedimentary rocks of the foothills. Because this arrangement did not always hold true for mountain ranges other than the Alps, the Primary and the Secondary were dropped in the general case. However, the term 'Tertiary' has persisted in geological literature until its recent replacement by the [[Palaeogene]] and [[Neogene]] periods. The last period of the [[Cenozoic]] Era is still known as the [[Quaternary]] period. The Cenozoic was studied and further determined by, among others, the English geologist (and mentor of [[Charles Darwin]]) [[Charles Lyell]].<ref name=Bates/>
==Further reading==
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