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Europe (search for this): chapter 10
was perhaps the son of the celebrated professor of Neuchatel. The answer amazed him; he could hardly believe that the young man before him was the naturalist of European reputation. In connection with this journey occurs the first attempt at an English letter found among Agassiz's papers. It is addressed to Buckland, and contaiion of observation to remoter valleys on the northern and southern slopes of the Alps, where he followed the descent of the glacial phenomena to the plains of central Europe on the one side and to those of northern Italy on the other. We therefore seldom hear of him with the band of workers who finally settled on the glacier of t fastnesses of retreat became, as the Alps are now, centres of distribution for the broken debris and rocky fragments which are found scattered with a kind of regularity along certain lines, and over given areas in northern and central Europe. How he followed out this idea in his subsequent investigations will be seen hereafter.
Lausanne (Switzerland) (search for this): chapter 10
Chapter 9: 1837-1839: Aet. 30-32. Invitation to Professorships at Geneva and Lausanne.– death of his father. establishment of lithographic Press at Neuchatel. researches upon structure of Mollusks. internal casts of shells. glacial explorations. views of Buckland. relations with Arnold Guyot. their work together in the Alps. letter to Sir Philip Egerton concerning glacial work. summer of 1839. publication of Etudes sur les glaciers. Although Agassiz's daring treatment of. Promptitude and silence, then, are the two recommendations which I make to you while we await the Yes we so greatly desire. . . . More tempting still must have been the official invitation received a few months later to a professorship at Lausanne, strengthened as it was by the affectionate entreaties of relations and friends, urging him for the sake of family ties and patriotism to return to the canton where he had passed his earlier years. But he had cast in his lot with the Neuchatelo
Grindelwald (Switzerland) (search for this): chapter 10
ic blocks, transported far from their place of origin and disposed in an order and position unexplained by the agency of water. These excursions, though not without their dangers and fatigues, were full of charm for men who, however serious their aims, were still young enough to enter like boys into the spirit of adventure. Agassiz himself was but thirty-one; an ardent pedestrian, he delighted in feats of walking and climbing. His friend Dinkel relates that one day, while pausing at Grindelwald for refreshment, they met an elderly traveler who asked him, after listening awhile to their gay talk, in which appeals were constantly made to Agassiz, if that was perhaps the son of the celebrated professor of Neuchatel. The answer amazed him; he could hardly believe that the young man before him was the naturalist of European reputation. In connection with this journey occurs the first attempt at an English letter found among Agassiz's papers. It is addressed to Buckland, and contai
United States (United States) (search for this): chapter 10
ys they met to compare notes, at the session of the Geological Society of France, at Porrentruy, where Agassiz made a report upon the general results of his summer's work; while Guyot read a paper, the contents of which have never been fully published, upon the movement of glaciers and upon their internal features, including the laminated structure of the ice, the so-called blue bands, deep down in the mass of the glacier. See Memoir of Louis Agassiz, by Arnold Guyot, written for the United States National Academy of Sciences, p. 38. In the succeeding years of their glacial researches together, Guyot took for his share the more special geological problems, the distribution of erratic boulders and of the glacial drift, as connected with the ancient extension of the glaciers. This led him away from the central station of observation to remoter valleys on the northern and southern slopes of the Alps, where he followed the descent of the glacial phenomena to the plains of central Eur
Porrentruy (Switzerland) (search for this): chapter 10
ng there, and persuaded him to undertake a certain part of the investigation. During this very summer of 1838, therefore, while Agassiz was tracing the ancient limits of the ice in the Bernese Oberland and the Haut Valais, and later, in the valley of Chamounix, Guyot was studying the structure and movement of the ice during a six weeks tour in the central Alps. At the conclusion of their respective journeys they met to compare notes, at the session of the Geological Society of France, at Porrentruy, where Agassiz made a report upon the general results of his summer's work; while Guyot read a paper, the contents of which have never been fully published, upon the movement of glaciers and upon their internal features, including the laminated structure of the ice, the so-called blue bands, deep down in the mass of the glacier. See Memoir of Louis Agassiz, by Arnold Guyot, written for the United States National Academy of Sciences, p. 38. In the succeeding years of their glacial resea
Cambria (United Kingdom) (search for this): chapter 10
essed to Buckland, and contains this passage: Since I saw the glaciers I am quite of a snowy humor, and will have the whole surface of the earth covered with ice, and the whole prior creation dead by cold. In fact, I am quite satisfied that ice must be taken [included] in every complete explanation of the last changes which occurred at the surface of Europe. Considered in connection with their subsequent work together in the ancient ice-beds and moraines of England, Scotland, Ireland, and Wales, it is curious to find Buckland answering: I am sorry that I cannot entirely adopt the new theory you advocate to explain transported blocks by moraines; for supposing it adequate to explain the phenomena of Switzerland, it would not apply to the granite blocks and transported gravel of England, which I can only explain by referring to currents of water. During the same summer Mrs. Buckland writes from Interlaken, in the course of a journey in Switzerland with her husband. . . We have made
Scotia (search for this): chapter 10
. It is addressed to Buckland, and contains this passage: Since I saw the glaciers I am quite of a snowy humor, and will have the whole surface of the earth covered with ice, and the whole prior creation dead by cold. In fact, I am quite satisfied that ice must be taken [included] in every complete explanation of the last changes which occurred at the surface of Europe. Considered in connection with their subsequent work together in the ancient ice-beds and moraines of England, Scotland, Ireland, and Wales, it is curious to find Buckland answering: I am sorry that I cannot entirely adopt the new theory you advocate to explain transported blocks by moraines; for supposing it adequate to explain the phenomena of Switzerland, it would not apply to the granite blocks and transported gravel of England, which I can only explain by referring to currents of water. During the same summer Mrs. Buckland writes from Interlaken, in the course of a journey in Switzerland with her husband. . .
Department de Ville de Paris (France) (search for this): chapter 10
a, you would be the happiest, the most honored. Look at ——, who shone as a star of the first magnitude at Geneva, and who is but a star of second or third rank in Paris. This, to be sure, would not be your case; nevertheless, I am satisfied that at Geneva, where you would be a second de Saussure, your position would be still morels known hitherto only by the shell. I have made a plaster collection of them for the Geological Society. They have been packed some time, but my late journey to Paris has prevented me from forwarding them till now. As soon as I have a moment, I shall make out the catalogue and send it on. When you go to London, do not fail to exat he had given in his youth to his friend's scheme for establishing a permanent scientific summer station in the high Alps. In a short visit made by Agassiz to Paris in the spring of 1838 he unfolded his whole plan to Guyot, then residing there, and persuaded him to undertake a certain part of the investigation. During this ve
Scotland (United Kingdom) (search for this): chapter 10
z's papers. It is addressed to Buckland, and contains this passage: Since I saw the glaciers I am quite of a snowy humor, and will have the whole surface of the earth covered with ice, and the whole prior creation dead by cold. In fact, I am quite satisfied that ice must be taken [included] in every complete explanation of the last changes which occurred at the surface of Europe. Considered in connection with their subsequent work together in the ancient ice-beds and moraines of England, Scotland, Ireland, and Wales, it is curious to find Buckland answering: I am sorry that I cannot entirely adopt the new theory you advocate to explain transported blocks by moraines; for supposing it adequate to explain the phenomena of Switzerland, it would not apply to the granite blocks and transported gravel of England, which I can only explain by referring to currents of water. During the same summer Mrs. Buckland writes from Interlaken, in the course of a journey in Switzerland with her husb
Alpes (search for this): chapter 10
r station in the high Alps. In a short visit made by Agassiz to Paris in the spring of 1838 he unfolded his whole plan to Guyot, then residing there, and persuaded him to undertake a certain part of the investigation. During this very summer of 1838, therefore, while Agassiz was tracing the ancient limits of the ice in the Bernese Oberland and the Haut Valais, and later, in the valley of Chamounix, Guyot was studying the structure and movement of the ice during a six weeks tour in the central Alps. At the conclusion of their respective journeys they met to compare notes, at the session of the Geological Society of France, at Porrentruy, where Agassiz made a report upon the general results of his summer's work; while Guyot read a paper, the contents of which have never been fully published, upon the movement of glaciers and upon their internal features, including the laminated structure of the ice, the so-called blue bands, deep down in the mass of the glacier. See Memoir of Lo
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