20 Swiss Franc note

Banknotes of Switzerland 20 Swiss Franc note, Horace-Benedict de Saussure

Banknotes of Switzerland 20 Swiss Franc note
Swiss National Bank
Schweizerische Nationalbank - Banque Nationale Suisse - Banca Nazionale Svizzera - Banca Naziunala Svizra


Banknotes of Switzerland 20 Swiss Franc note, Alpinists in the Swiss Alps
Obverse: Portrait of geologist Horace-Bénédict de Saussure (1740-1799).
Reverse: Expedition in the Alps - de Saussure and his son arriving at the Tau Glacier Aiguille de Bellaval Peak (SW of Montblanc) & prehistoric conch (Ammonshorn). Horace-Bénédict de Saussure heads up Mont Blanc with his team of helpers in 1787. The last guide is carrying a charcoal stove. Contemporary engraving by Chrétien de Méchel.
Colors: blue.
Size 148 x 70 mm.
Watermark: portrait of Horace-Benedict de Saussure.
Artists: Ernst Hiestand und Ursula Hiestand.
Printer: Orell Füssli Arts Graphiques S.A.
In circulation from 04.04.1979 to 01.05.2000.
Cancelled from 01.05.2020.



























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Horace-Bénédict de Saussure
Horace-Bénédict de Saussure (17 February 1740 – 22 January 1799) was a Swiss aristocrat, physicist and Alpine traveller, often considered the founder of alpinism, and considered to be the first person to build a successful solar oven.

Horace Bénédict de Saussure - Life and work   
   Horace Bénédicte de Saussure was born the 17 February 1740 in Conches, near Geneva, and died the 22 January 1799 in his hometown.
   His early interest in botanical studies led him to undertake journeys among the Alps, and from 1773 onwards he directed his attention to the geology and physics of that region. This work did much to clear up the topography of the snowy portions of the Alps, and to attract the attention of tourists to spots like Chamonix and Zermatt.
   In 1760 he first visited Chamonix, and offered a reward to the first man to reach the summit of Mont Blanc, at the time unscaled. Since 1774 he tried to find a way to reach the summit on the Italian side, accompanied by the Courmayeur alpine guide Jean-Laurent Jordaney on the Miage glacier and on Mont Crammont. He made an unsuccessful attempt himself in 1785, by the Aiguille du Goûter route. Two Chamonix men, Michel Paccard and Jacques Balmat attained the summit in 1786, by way of the Grands Mulets, and in 1787 Saussure himself made the third ascent of the mountain.
   In 1788 he spent 17 days making observations on the crest of the Col du Géant (3,371 m). In 1774 he mounted the Crammont, and again in 1778, in which year he also explored the Valsorey glacier, near the Great St Bernard in 1776 he had ascended the Buet (3,096 m).
    In 1789 he climbed the Pizzo Bianco near Macugnaga, to observe the east wall of Monte Rosa, and crossed the Theodulpass (3,322 m) to Zermatt, which he was the first traveler to visit. On that occasion he climbed from the pass up the Klein Matterhorn (3,883 m), while in 1792 he spent three days making observations on the same pass without descending to Zermatt, and then visited the Theodulhorn (3,472 m).
   In 1780 he climbed the Roche Michel, above the Mont Cenis Pass. The descriptions of seven of his Alpine journeys, with his scientific observations gathered en route, were published by him in four quarto volumes, under the general title of Voyages dans les Alpes from 1779 to 1796. There was an octavo issue in eight volumes, issued from 1780 to 1796, while the non-scientific portions of the work were first published in 1834, and often since, under the title of Partie pittoresque des ouvrages de M. de Saussure.

Horace Bénédict de Saussure - Significance
   The Alps formed the centre of Saussure's investigations. He saw them as the grand key to the true theory of the earth, and they gave him the opportunity for studying geology in a manner never previously attempted. The inclination of the strata, the nature of the rocks, the fossils and the minerals received close attention.
   He acquired a thorough knowledge of the chemistry of the day; and he applied it to the study of minerals, water and air. Saussure's geological observations made him a firm believer in the Neptunian theory: he regarded all rocks and minerals as deposited from aqueous solution or suspension, and attached much importance to the study of meteorological conditions. His work with rocks, erosion, and fossils would also lead him to the idea that the earth was much older than generally thought and formed part of the basis of Darwin's Theory of Evolution.
   He carried barometers and boiling-point thermometers to the summits of the highest mountains, and estimated the relative humidity of the atmosphere at different heights, its temperature, the strength of solar radiation, the composition of air and its transparency. Then, following the precipitated moisture, he investigated the temperature of the earth at all depths to which he could drive his thermometer staves, the course, conditions and temperature of streams, rivers, glaciers and lakes, even of the sea.
   In the Essai sur l'hygrométrie, published in 1783, he records experiments made with various forms of hygrometer in all climates and at all temperatures, and supports the claims of his hair hygrometer against all others. He invented and improved many kinds of apparatus, including the magnetometer, the cyanometer for estimating the blueness of the sky, the diaphanometer for judging of the clearness of the atmosphere, the anemometer and the mountain eudiometer.
   His modifications of the thermometer adapted that instrument to many purposes: for ascertaining the temperature of the air he used one with a fine bulb hung in the shade or whirled by a string, the latter form being converted into an evaporimeter by inserting its bulb into a piece of wet sponge and making it revolve in a circle of known radius, at a known rate; for experiments on the earth and in deep water he employed large thermometers wrapped in non-conducting coatings so as to render them extremely sluggish, and capable of long retaining the temperature once they had attained it.
   With these instruments he showed that the bottom water of deep lakes is uniformly cold at all seasons, and that the annual heat wave takes six months to penetrate to a depth of 30 ft. in the earth. He recognized the immense advantages to meteorology of high-level observing stations, and whenever it was practicable he arranged for simultaneous observations being made at different altitudes for as long periods as possible.
   Saussure was particularly influential as a geologist, and although his ideas on the underlying principles were often erroneous, he was instrumental in greatly advancing that science. He was an early user of the term "geology"—see the "Discours préliminaire" to volume I of his Voyages, published in 1779—though by no means its inventor as some have claimed, the English word having been used in the 1680s and its Latin counterpart "geologia" during the previous several centuries.
   He constructed the first known Western solar oven in 1767, trying several designs before determining that a well-insulated box with three layers of glass to trap outgoing thermal radiation created the most heat. The highest temperature he reached was 230 °F, which he found did not vary significantly when the box was carried from the top of Mt. Cramont in the Swiss Alps down to the Plains of Cournier, 4,852 feet below in altitude and 34 °F above in temperature, thereby establishing that the external air temperature played no significant role in this solar heating effect.
   In 1784, he was elected a foreign member of the Royal Swedish Academy of Sciences.
   De Saussure died in Geneva in 1799.