Banner
    The Posthumous Memoir Of Ignaz Venetz
    By Patrick Lockerby | July 31st 2011 08:29 AM | Print | E-mail | Track Comments
    About Patrick

    Retired engineer, 60+ years young. Computer builder and programmer. Linguist specialising in language acquisition and computational linguistics....

    View Patrick's Profile
    The Posthumous Memoir of Ignaz Venetz

    My  three part article on Venetz's prize-winning 1821 paper began with some facts tending to prove that he was the first person to discuss climate change scientifically.  Since beginning my researches concerning Venetz, I have discovered many more facts.


    The discovery of climate change.

    Spencer Weart's most excellent book and website on 'The Discovery of Global Warming' begins with the discovery that CO2 is a greenhouse gas.  I have for some time now taken that point in science history and worked backwards in my researches to determine the moment in history when the first major discoveries about climate change were made.

    The greatest and most widely known effect of climate change is probably glaciation.  Even the most ardent skeptics accept the fact of ice ages.  Indeed, many of them refer to ice ages in their attempts to discredit modern climate science.

    Ice ages constitute the most striking climate change evidence which is accepted by a vast majority of both scientists and the public at large.  My purpose in studying the topic was to determine just when the discoverers of ice ages figured out that an ice age was evidence of climate change.

    From my researches I found that most people credit Louis Agassiz with the theory of ice ages and with the the theory that they were triggered by climate change.

    In fact, until 1835, Agassiz was a supporter of the theory that most geological features had been caused by floods.  In 1835 he stayed with Jean de Charpentier and was introduced to glaciation theory.  Like de Charpentier before him, he at first rejected the theory, but later became an ardent supporter.  Jean de Charpentier, director of Bex salt mines, had been introduced to glaciation theory by Ignaz Venetz - and had at first rejected the theory.

    Louis Agassiz read, to the Swiss Natural Sciences Society, in 1837, a paper on glaciation.  A paper on the same topic was also read by Karl Friedrich Schimper, who had stayed with de Charpentier and Agassiz in 1836.  In his 1837 paper, Schimper used the term 'eiszeit' and thus coined the term 'ice age'.

    Thus we see that when Agassiz and Schimper read their papers to the society in 1837 they were building on foundations laid by Ignaz Venetz and published in 1821.  His researches showed that:

        there had been multiple glacier advances and retreats in Switzerland;

        these had been caused by multiple changes in climate;

        these changes in glaciation and climate were likely to be found in other countries.

    Jean de Charpentier died in 1855.  Ignaz Venetz died in 1859.  Louis Aggasiz, during his wide travels and lectures on glaciers seems to have quite forgotten on many occasions to mention the names of the two people who had first introduced him to the subject.

    Venetz gave evidence of multiple advances and retreats of glaciers.  By 1837 the evidence of multiple ice ages was quite strong.  However, it seems that much of the early research lay undiscovered in the archives, leading to a general belief in a single ice age, and a belief that Agassiz was its discoverer.  James Gieke's 'The Great Ice Age', 1873, discusses evidence of a single ice age.  These facts have led many science historians and writers of popular books to believe  that evidence of multiple ice ages was discovered only late in the 19th century.

    Only rarely has a writer or scientist correctly cited Venetz as having published in 1821, most giving instead the date of the reprint - 1833.

    The transport of erratic blocks in the Alps had long been attributed by mountain residents to earlier glacial advances. The first scientific discussion of the matter came from Venetz. In 1821 that excellent observer showed that the glaciers of Valais during the last centuries have been generally less extended than today, whereas these same, during an earlier period, must have been much more greatly advanced than now.
    Albrecht Fenck, 1881
    Die Vergletscherung Der Deutschen Alpen: Ihre Ursachen, Periodische Wiederkehr Und Ihr Einfluss Auf Die Bodengestaltung

    [my translation]

    An illustration of a perched block, from The Great Ice Age, James Gieke, 2nd. ed. 1877


    I hope to publish soon my transcriptions and translations of the 1837 papers of Agassiz and Schimper.  But first, I am pleased to publish Venetz's posthumous paper, here in part 2 of this current article.

    As before, I shall publish the translation when finished as part 3 and edit this part to place a link here.
    The translation is now published as - The Posthumous Memoir Of Ignaz Venetz #3