William Buckland nasceu há duzentos e quarenta anos

     

William Buckland (Axminster, Devon, 12 de março de 1784 - 24 de agosto de 1856) foi um teólogo britânico que se tornou Deão de Westminster, geólogo e paleontólogo que fez a primeira recolha e descrição completa de um dinossauro nomeado megalossauro, no seu trabalho na caverna de Kirkdale comprovando um covil pré-histórico de hiena, e pelo qual foi premiado com a Medalha Copley, foi amplamente elogiado como um exemplo de como a análise científica detalhada pode ser usada para entender a história geológica pela reconstrução de eventos de tempo profundo. Foi um pioneiro no uso de fezes, restos fossilizados, pelo qual ele inseriu o termo coprólito, para reconstruir antigos eco-sistemas. Buckland foi o proponente da Teoria do Hiato, que interpretava o acontecimento Bíblico de Génesis se referindo a dois episódios da Criação separados por um período de duração, que surgiu no final do século XVIII e começo do século XIX com uma maneira de reconciliar os acontecimentos das escrituras com as descobertas geológicas que sugeria a terra muito antiga. No começo de sua carreira ele acreditou que tivesse encontrado evidência geológica do Dilúvio Bíblico, porém mais tarde convenceu-se que a Era do Gelo de Louis Agassiz era uma melhor explicação e desempenhou um importante papel na promoção da teoria na Grã Bretanha.

Foi laureado com a Medalha Copley, em 1822, e com a medalha Wollaston, concedida pela Sociedade Geológica de Londres, em 1848.

   

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O zoólogo e geólogo Louis Agassiz morreu há cento e cinquenta anos...

Jean Louis Rodolphe Agassiz (Môtier, 18 de maio de 1807 - Cambridge, 14 de dezembro de 1873) foi um zoólogo e geólogo suíço, famoso pela sua Expedição Thayer.

Louis Agassiz nasceu em Môtier (Vully), no Cantão de Friburgo, Suíça. O início da sua educação começou em casa, seguido de quatro anos numa escola secundária em Bienne (alemão Biel), completou os seus estudos elementares na academia de Lausanne. Selecionando a medicina como a sua profissão, estudou nas universidades de Zurique, Heidelberg e Munique. Em seguida aumentou o seu conhecimento nos processos biológicos, especialmente na Botânica. Em 1829, doutorou-se em Erlangen e em 1830 doutorou-se em Medicina em Munique.

Mudou-se para Paris e ficou sobre a tutela de Alexander von Humboldt e de Georges Cuvier, que o lançaram nas suas carreiras da Geologia e do Zoologia respetivamente. Até esta altura não prestou nenhuma atenção especial ao estudo da Ictiologia, a qual se transformou na grande ocupação de sua vida, ou pelo menos na área em que atualmente é mais recordado.

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In 1832 he was appointed professor of natural history in the University of Neuchâtel. The fossil fish there soon attracted his attention. The fossil-rich stones furnished by the slates of Glarus and the limestones of Monte Bolca were known at the time, but very little had been accomplished in the way of scientific study of them. Agassiz, as early as 1829, planned the publication of the work which, more than any other, laid the foundation of his worldwide fame. Five volumes of his Recherches sur les poissons fossiles ("Research on Fossil Fish") appeared at intervals from 1833 to 1843. They were magnificently illustrated, chiefly by Joseph Dinkel. In gathering materials for this work Agassiz visited the principal museums in Europe, and meeting Cuvier in Paris, he received much encouragement and assistance from him. They had known him for seven years at the time.

Agassiz found that his palaeontological labours made necessary a new basis of ichthyological classification. The fossils rarely exhibited any traces of the soft tissues of fish. They consisted chiefly of the teeth, scales and fins, even the bones being perfectly preserved in comparatively few instances. He therefore adopted a classification which divided fish into four groups: Ganoids, Placoids, Cycloids and Ctenoids, based on the nature of the scales and other dermal appendages. While Agassiz did much to place the subject on a scientific basis, this classification has been superseded by later work.

As Agassiz's descriptive work proceeded, it became obvious that it would over-tax his resources unless financial assistance could be found. The British Association came to his aid, and the Earl of Ellesmere — then Lord Francis Egerton — gave him yet more efficient help. The 1,290 original drawings made for the work were purchased by the Earl, and presented by him to the Geological Society of London. In 1836 the Wollaston Medal was awarded to Agassiz by the council of that society for his work on fossil ichthyology; and in 1838 he was elected a foreign member of the Royal Society. Meanwhile invertebrate animals engaged his attention. In 1837 he issued the "Prodrome" of a monograph on the recent and fossil Echinodermata, the first part of which appeared in 1838; in 1839–40 he published two quarto volumes on the fossil Echinoderms of Switzerland; and in 1840–45 he issued his Etudes critiques sur les mollusques fossiles ("Critical Studies on Fossil Mollusks").

Before his first visit to England in 1834, the labours of Hugh Miller and other geologists brought to light the remarkable fish of the Old Red Sandstone of the northeast of Scotland. The strange forms of the Pterichthys, the Coccosteus and other genera were then made known to geologists for the first time. They were of intense interest to Agassiz, and formed the subject of a special monograph by him published in 1844–45: Monographie des poissons fossiles du Vieux Gres Rouge, ou Systeme Devonien (Old Red Sandstone) des Iles Britanniques et de Russie ("Monograph on Fossil Fish of the Old Red Sandstone, or Devonian System of the British Isles and of Russia"). In the early stages of his career in Neuchatel, Agassiz also made a name for himself as a man who could run a scientific department well. Under his care, the University of Neuchâtel soon became a leading institution for scientific inquiry.

In 1837 Agassiz was the first to scientifically propose that the Earth had been subject to a past ice age. In the same year, he was elected a foreign member of the Royal Swedish Academy of Sciences. Prior to this proposal, Goethe, de Saussure, Venetz, Jean de Charpentier, Karl Friedrich Schimper and others had made the glaciers of the Alps the subjects of special study, and Goethe, Charpentier as well as Schimper had even arrived at the conclusion that the erratic blocks of alpine rocks scattered over the slopes and summits of the Jura Mountains had been moved there by glaciers. The question having attracted the attention of Agassiz, he not only discussed it with Charpentier and Schimper and made successive journeys to the alpine regions in company with them, but he had a hut constructed upon one of the Aar Glaciers, which for a time he made his home, in order to investigate the structure and movements of the ice.

These labours resulted, in 1840, in the publication of his work in two volumes entitled Etudes sur les glaciers ("Study on Glaciers"). In it he discussed the movements of the glaciers, their moraines, their influence in grooving and rounding the rocks over which they travelled, and in producing the striations and roches moutonnees seen in Alpine-style landscapes. He not only accepted Charpentier's and Schimper's idea that some of the alpine glaciers had extended across the wide plains and valleys drained by the Aar and the Rhône, but he went still farther. He concluded that, in the relatively recent past, Switzerland had been another Greenland; that instead of a few glaciers stretching across the areas referred to, one vast sheet of ice, originating in the higher Alps, had extended over the entire valley of northwestern Switzerland until it reached the southern slopes of the Jura, which, though they checked and deflected its further extension, did not prevent the ice from reaching in many places the summit of the range. The publication of this work gave a fresh impetus to the study of glacial phenomena in all parts of the world.

Thus familiarized with the phenomena associated with the movements of recent glaciers, Agassiz was prepared for a discovery which he made in 1840, in conjunction with William Buckland. The two visited the mountains of Scotland together, and found in different locations clear evidence of ancient glacial action. The discovery was announced to the Geological Society of London in successive communications. The mountainous districts of England, Wales, and Ireland were also considered to constitute centres for the dispersion of glacial debris; and Agassiz remarked "that great sheets of ice, resembling those now existing in Greenland, once covered all the countries in which unstratified gravel (boulder drift) is found; that this gravel was in general produced by the trituration of the sheets of ice upon the subjacent surface, etc."

In 1842–1846 he issued his Nomenclator Zoologicus, a classified list, with references, of all names employed in zoology for genera and groups — a work of great labour and research. With the aid of a grant of money from the King of Prussia, Agassiz crossed the Atlantic in the autumn of 1846 with the twin purposes of investigating the natural history and geology of North America and delivering a course of 12 lectures on “The Plan of Creation as shown in the Animal Kingdom,” by invitation from J. A. Lowell, at the Lowell Institute in Boston, Massachusetts. The financial and scientific advantages presented to him in the United States induced him to settle there, where he remained to the end of his life. He was elected a Foreign Honorary Member of the American Academy of Arts and Sciences in 1846.

His engagement for the Lowell Institute lectures precipitated the establishment of the Lawrence Scientific School at Harvard University in 1847 with him as its head. Harvard appointed him professor of zoology and geology, and he founded the Museum of Comparative Zoology there in 1859 serving as the museum's first director until his death in 1873. During his tenure at Harvard, he was, among many other things, an early student of the effect of the last Ice Age on North America.

He continued his lectures for the Lowell Institute. In succeeding years, he gave series of lectures on “Ichthyology” (1847–48 season), “Comparative Embryology” (1848–49), “Functions of Life in Lower Animals” (1850–51), “Natural History” (1853–54), “Methods of Study in Natural History” (1861–62), “Glaciers and the Ice Period” (1864–65), “Brazil” (1866–67) and “Deep Sea Dredging” (1869–70). In 1850 he married an American college teacher, Elizabeth Cabot Cary Agassiz, who later wrote introductory books about natural history and, after his death, a lengthy biography of her husband.

Agassiz served as a non-resident lecturer at Cornell while also being on faculty at Harvard. In 1852 he accepted a medical professorship of comparative anatomy at Charlestown, Massachusetts, but he resigned in two years. From this time his scientific studies dropped off, but he was a profound influence on the American branches of his two fields, teaching decades worth of future prominent scientists, including Alpheus Hyatt, David Starr Jordan, Joel Asaph Allen, Joseph Le Conte, Ernest Ingersoll, William James, Nathaniel Shaler, Samuel Hubbard Scudder, Alpheus Packard, and his son Alexander Agassiz, among others. He had a profound impact on the paleontologist Charles Doolittle Walcott. In return his name appears attached to several species, as well as here and there throughout the American landscape, notably Lake Agassiz, the Pleistocene precursor to Lake Winnipeg and the Red River.

During this time he grew in fame even in the public consciousness, becoming one of the best-known scientists in the world. By 1857 he was so well-loved that his friend Henry Wadsworth Longfellow wrote "The fiftieth birthday of Agassiz" in his honor. His own writing continued with four (of a planned ten) volumes of Natural History of the United States which were published from 1857 to 1862. During this time he also published a catalog of papers in his field, Bibliographia Zoologiae et Geologiae, in four volumes between 1848 and 1854.

Stricken by ill health in the 1860s, he resolved to return to the field for relaxation and to resume his studies of Brazilian fish. In April 1865 he led a party to Brazil. Returning home in August 1866, an account of this expedition, entitled A Journey in Brazil, was published in 1868. In December 1871 he made a second eight month excursion, known as the Hassler expedition under the command of Commander Philip Carrigan Johnson (brother of Eastman Johnson), visiting South America on its southern Atlantic and Pacific seaboards. The ship explored the Magellan Strait, which drew the praise of Charles Darwin.

Elizabeth Aggasiz wrote, at the Strait: '…the Hassler pursued her course, past a seemingly endless panorama of mountains and forests rising into the pale regions of snow and ice, where lay glaciers in which every rift and crevasse, as well as the many cascades flowing down to join the waters beneath, could be counted as she steamed by them.... These were weeks of exquisite delight to Agassiz. The vessel often skirted the shore so closely that its geology could be studied from the deck.'

   

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William Buckland nasceu há 239 anos

     

William Buckland (Axminster, Devon, 12 de março de 1784 - 24 de agosto de 1856) foi um teólogo britânico que se tornou Deão de Westminster, geólogo e paleontólogo que fez a primeira recolha e descrição completa de um dinossauro nomeado megalossauro, no seu trabalho na caverna de Kirkdale comprovando um covil pré-histórico de hiena, e pelo qual foi premiado com a Medalha Copley, foi amplamente elogiado como um exemplo de como a análise científica detalhada pode ser usada para entender a história geológica pela reconstrução de eventos de tempo profundo. Foi um pioneiro no uso de fezes, restos fossilizados, pelo qual ele inseriu o termo coprólito, para reconstruir antigos eco-sistemas. Buckland foi o proponente da Teoria do Hiato, que interpretava o acontecimento Bíblico de Génesis se referindo a dois episódios da Criação separados por um período de duração, que surgiu no final do século XVIII e começo do século XIX com uma maneira de reconciliar os acontecimentos das escrituras com as descobertas geológicas que sugeria a terra muito antiga. No começo de sua carreira ele acreditou que tivesse encontrado evidência geológica do Dilúvio Bíblico, porém mais tarde convenceu-se que a Era do Gelo de Louis Agassiz era uma melhor explicação e desempenhou um importante papel na promoção da teoria na Grã Bretanha.

Foi laureado com a Medalha Copley, em 1822, e com a medalha Wollaston, concedida pela Sociedade Geológica de Londres, em 1848.

   

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Louis Agassiz morreu há 149 anos

   

Jean Louis Rodolphe Agassiz (Môtier, 18 de maio de 1807 - Cambridge, 14 de dezembro de 1873) foi um zoólogo e geólogo suíço, famoso pela sua Expedição Thayer.

Louis Agassiz nasceu em Môtier (Vully), no Cantão de Friburgo, Suíça. O início da sua educação começou em casa, seguido de quatro anos numa escola secundária em Bienne (alemão Biel), completou os seus estudos elementares na academia de Lausanne. Selecionando a medicina como a sua profissão, estudou nas universidades de Zurique, Heidelberg e Munique. Em seguida aumentou o seu conhecimento nos processos biológicos, especialmente na Botânica. Em 1829, doutorou-se em Erlangen e em 1830 doutorou-se em Medicina em Munique.

Mudou-se para Paris e ficou sobre a tutela de Alexander von Humboldt e de Georges Cuvier, que o lançaram nas suas carreiras da Geologia e do Zoologia respetivamente. Até esta altura não prestou nenhuma atenção especial ao estudo da Ictiologia, a qual se transformou na grande ocupação de sua vida, ou pelo menos na área em que atualmente é mais recordado.

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In 1832 he was appointed professor of natural history in the University of Neuchâtel. The fossil fish there soon attracted his attention. The fossil-rich stones furnished by the slates of Glarus and the limestones of Monte Bolca were known at the time, but very little had been accomplished in the way of scientific study of them. Agassiz, as early as 1829, planned the publication of the work which, more than any other, laid the foundation of his worldwide fame. Five volumes of his Recherches sur les poissons fossiles ("Research on Fossil Fish") appeared at intervals from 1833 to 1843. They were magnificently illustrated, chiefly by Joseph Dinkel. In gathering materials for this work Agassiz visited the principal museums in Europe, and meeting Cuvier in Paris, he received much encouragement and assistance from him. They had known him for seven years at the time.

Agassiz found that his palaeontological labours made necessary a new basis of ichthyological classification. The fossils rarely exhibited any traces of the soft tissues of fish. They consisted chiefly of the teeth, scales and fins, even the bones being perfectly preserved in comparatively few instances. He therefore adopted a classification which divided fish into four groups: Ganoids, Placoids, Cycloids and Ctenoids, based on the nature of the scales and other dermal appendages. While Agassiz did much to place the subject on a scientific basis, this classification has been superseded by later work.

As Agassiz's descriptive work proceeded, it became obvious that it would over-tax his resources unless financial assistance could be found. The British Association came to his aid, and the Earl of Ellesmere — then Lord Francis Egerton — gave him yet more efficient help. The 1,290 original drawings made for the work were purchased by the Earl, and presented by him to the Geological Society of London. In 1836 the Wollaston Medal was awarded to Agassiz by the council of that society for his work on fossil ichthyology; and in 1838 he was elected a foreign member of the Royal Society. Meanwhile invertebrate animals engaged his attention. In 1837 he issued the "Prodrome" of a monograph on the recent and fossil Echinodermata, the first part of which appeared in 1838; in 1839–40 he published two quarto volumes on the fossil Echinoderms of Switzerland; and in 1840–45 he issued his Etudes critiques sur les mollusques fossiles ("Critical Studies on Fossil Mollusks").

Before his first visit to England in 1834, the labours of Hugh Miller and other geologists brought to light the remarkable fish of the Old Red Sandstone of the northeast of Scotland. The strange forms of the Pterichthys, the Coccosteus and other genera were then made known to geologists for the first time. They were of intense interest to Agassiz, and formed the subject of a special monograph by him published in 1844–45: Monographie des poissons fossiles du Vieux Gres Rouge, ou Systeme Devonien (Old Red Sandstone) des Iles Britanniques et de Russie ("Monograph on Fossil Fish of the Old Red Sandstone, or Devonian System of the British Isles and of Russia"). In the early stages of his career in Neuchatel, Agassiz also made a name for himself as a man who could run a scientific department well. Under his care, the University of Neuchâtel soon became a leading institution for scientific inquiry.

In 1837 Agassiz was the first to scientifically propose that the Earth had been subject to a past ice age. In the same year, he was elected a foreign member of the Royal Swedish Academy of Sciences. Prior to this proposal, Goethe, de Saussure, Venetz, Jean de Charpentier, Karl Friedrich Schimper and others had made the glaciers of the Alps the subjects of special study, and Goethe, Charpentier as well as Schimper had even arrived at the conclusion that the erratic blocks of alpine rocks scattered over the slopes and summits of the Jura Mountains had been moved there by glaciers. The question having attracted the attention of Agassiz, he not only discussed it with Charpentier and Schimper and made successive journeys to the alpine regions in company with them, but he had a hut constructed upon one of the Aar Glaciers, which for a time he made his home, in order to investigate the structure and movements of the ice.

These labours resulted, in 1840, in the publication of his work in two volumes entitled Etudes sur les glaciers ("Study on Glaciers"). In it he discussed the movements of the glaciers, their moraines, their influence in grooving and rounding the rocks over which they travelled, and in producing the striations and roches moutonnees seen in Alpine-style landscapes. He not only accepted Charpentier's and Schimper's idea that some of the alpine glaciers had extended across the wide plains and valleys drained by the Aar and the Rhône, but he went still farther. He concluded that, in the relatively recent past, Switzerland had been another Greenland; that instead of a few glaciers stretching across the areas referred to, one vast sheet of ice, originating in the higher Alps, had extended over the entire valley of northwestern Switzerland until it reached the southern slopes of the Jura, which, though they checked and deflected its further extension, did not prevent the ice from reaching in many places the summit of the range. The publication of this work gave a fresh impetus to the study of glacial phenomena in all parts of the world.

Thus familiarized with the phenomena associated with the movements of recent glaciers, Agassiz was prepared for a discovery which he made in 1840, in conjunction with William Buckland. The two visited the mountains of Scotland together, and found in different locations clear evidence of ancient glacial action. The discovery was announced to the Geological Society of London in successive communications. The mountainous districts of England, Wales, and Ireland were also considered to constitute centres for the dispersion of glacial debris; and Agassiz remarked "that great sheets of ice, resembling those now existing in Greenland, once covered all the countries in which unstratified gravel (boulder drift) is found; that this gravel was in general produced by the trituration of the sheets of ice upon the subjacent surface, etc."

In 1842–1846 he issued his Nomenclator Zoologicus, a classified list, with references, of all names employed in zoology for genera and groups — a work of great labour and research. With the aid of a grant of money from the King of Prussia, Agassiz crossed the Atlantic in the autumn of 1846 with the twin purposes of investigating the natural history and geology of North America and delivering a course of 12 lectures on “The Plan of Creation as shown in the Animal Kingdom,” by invitation from J. A. Lowell, at the Lowell Institute in Boston, Massachusetts. The financial and scientific advantages presented to him in the United States induced him to settle there, where he remained to the end of his life. He was elected a Foreign Honorary Member of the American Academy of Arts and Sciences in 1846.

His engagement for the Lowell Institute lectures precipitated the establishment of the Lawrence Scientific School at Harvard University in 1847 with him as its head. Harvard appointed him professor of zoology and geology, and he founded the Museum of Comparative Zoology there in 1859 serving as the museum's first director until his death in 1873. During his tenure at Harvard, he was, among many other things, an early student of the effect of the last Ice Age on North America.

He continued his lectures for the Lowell Institute. In succeeding years, he gave series of lectures on “Ichthyology” (1847–48 season), “Comparative Embryology” (1848–49), “Functions of Life in Lower Animals” (1850–51), “Natural History” (1853–54), “Methods of Study in Natural History” (1861–62), “Glaciers and the Ice Period” (1864–65), “Brazil” (1866–67) and “Deep Sea Dredging” (1869–70). In 1850 he married an American college teacher, Elizabeth Cabot Cary Agassiz, who later wrote introductory books about natural history and, after his death, a lengthy biography of her husband.

Agassiz served as a non-resident lecturer at Cornell while also being on faculty at Harvard. In 1852 he accepted a medical professorship of comparative anatomy at Charlestown, Massachusetts, but he resigned in two years. From this time his scientific studies dropped off, but he was a profound influence on the American branches of his two fields, teaching decades worth of future prominent scientists, including Alpheus Hyatt, David Starr Jordan, Joel Asaph Allen, Joseph Le Conte, Ernest Ingersoll, William James, Nathaniel Shaler, Samuel Hubbard Scudder, Alpheus Packard, and his son Alexander Agassiz, among others. He had a profound impact on the paleontologist Charles Doolittle Walcott. In return his name appears attached to several species, as well as here and there throughout the American landscape, notably Lake Agassiz, the Pleistocene precursor to Lake Winnipeg and the Red River.

During this time he grew in fame even in the public consciousness, becoming one of the best-known scientists in the world. By 1857 he was so well-loved that his friend Henry Wadsworth Longfellow wrote "The fiftieth birthday of Agassiz" in his honor. His own writing continued with four (of a planned ten) volumes of Natural History of the United States which were published from 1857 to 1862. During this time he also published a catalog of papers in his field, Bibliographia Zoologiae et Geologiae, in four volumes between 1848 and 1854.

Stricken by ill health in the 1860s, he resolved to return to the field for relaxation and to resume his studies of Brazilian fish. In April 1865 he led a party to Brazil. Returning home in August 1866, an account of this expedition, entitled A Journey in Brazil, was published in 1868. In December 1871 he made a second eight month excursion, known as the Hassler expedition under the command of Commander Philip Carrigan Johnson (brother of Eastman Johnson), visiting South America on its southern Atlantic and Pacific seaboards. The ship explored the Magellan Strait, which drew the praise of Charles Darwin.

Elizabeth Aggasiz wrote, at the Strait: '…the Hassler pursued her course, past a seemingly endless panorama of mountains and forests rising into the pale regions of snow and ice, where lay glaciers in which every rift and crevasse, as well as the many cascades flowing down to join the waters beneath, could be counted as she steamed by them.... These were weeks of exquisite delight to Agassiz. The vessel often skirted the shore so closely that its geology could be studied from the deck.'

   

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William Buckland nasceu há 238 anos

     

William Buckland (Axminster, Devon, 12 de março de 1784 - 24 de agosto de 1856) foi um teólogo britânico que se tornou Deão de Westminster, geólogo e paleontólogo que fez a primeira recolha e descrição completa de um dinossauro nomeado megalossauro, no seu trabalho na caverna de Kirkdale comprovando um covil pré-histórico de hiena, e pelo qual foi premiado com a Medalha Copley, foi amplamente elogiado como um exemplo de como a análise científica detalhada pode ser usada para entender a história geológica pela reconstrução de eventos de tempo profundo. Foi um pioneiro no uso de fezes, restos fossilizados, pelo qual ele inseriu o termo coprólito, para reconstruir antigos eco-sistemas. Buckland foi o proponente da Teoria do Hiato, que interpretava o acontecimento Bíblico de Génesis se referindo a dois episódios da Criação separados por um período de duração, que surgiu no final do século XVIII e começo do século XIX com uma maneira de reconciliar os acontecimentos das escrituras com as descobertas geológicas que sugeria a terra muito antiga. No começo de sua carreira ele acreditou que tivesse encontrado evidência geológica do Dilúvio Bíblico, porém mais tarde convenceu-se que a Era do Gelo de Louis Agassiz era uma melhor explicação e desempenhou um importante papel na promoção da teoria na Grã Bretanha.

Foi laureado com a Medalha Copley, em 1822, e com a medalha Wollaston, concedida pela Sociedade Geológica de Londres, em 1848.

   

in Wikipédia

Louis Agassiz morreu há 148 anos

   

Jean Louis Rodolphe Agassiz (Môtier, 18 de maio de 1807 - Cambridge, 14 de dezembro de 1873) foi um zoólogo e geólogo suíço, notório por sua Expedição Thayer.

Louis Agassiz nasceu em Môtier (Vully), no Cantão de Friburgo, Suíça. O início da sua educação começou em casa, seguido de quatro anos numa escola secundária em Bienne (alemão Biel), completou os seus estudos elementares na academia de Lausanne. Seleccionando a medicina como a sua profissão, estudou nas universidades de Zurique, Heidelberg e Munique. Em seguida aumentou o seu conhecimento nos processos biológicos, especialmente na Botânica. Em 1829, doutorou-se em Erlangen e em 1830 doutorou-se em medicina em Munique.

Mudou-se para Paris e ficou sobre a tutela de Alexander von Humboldt e de Georges Cuvier, que o lançaram nas suas carreiras da Geologia e do Zoologia respectivamente. Até esta altura não prestou nenhuma atenção especial ao estudo da Ictiologia, a qual se transformou na grande ocupação de sua vida, ou pelo menos na área em que actualmente é mais recordado.

in Wikipédia

   

In 1832 he was appointed professor of natural history in the University of Neuchâtel. The fossil fish there soon attracted his attention. The fossil-rich stones furnished by the slates of Glarus and the limestones of Monte Bolca were known at the time, but very little had been accomplished in the way of scientific study of them. Agassiz, as early as 1829, planned the publication of the work which, more than any other, laid the foundation of his worldwide fame. Five volumes of his Recherches sur les poissons fossiles ("Research on Fossil Fish") appeared at intervals from 1833 to 1843. They were magnificently illustrated, chiefly by Joseph Dinkel. In gathering materials for this work Agassiz visited the principal museums in Europe, and meeting Cuvier in Paris, he received much encouragement and assistance from him. They had known him for seven years at the time.

Agassiz found that his palaeontological labours made necessary a new basis of ichthyological classification. The fossils rarely exhibited any traces of the soft tissues of fish. They consisted chiefly of the teeth, scales and fins, even the bones being perfectly preserved in comparatively few instances. He therefore adopted a classification which divided fish into four groups: Ganoids, Placoids, Cycloids and Ctenoids, based on the nature of the scales and other dermal appendages. While Agassiz did much to place the subject on a scientific basis, this classification has been superseded by later work.

As Agassiz's descriptive work proceeded, it became obvious that it would over-tax his resources unless financial assistance could be found. The British Association came to his aid, and the Earl of Ellesmere — then Lord Francis Egerton — gave him yet more efficient help. The 1,290 original drawings made for the work were purchased by the Earl, and presented by him to the Geological Society of London. In 1836 the Wollaston Medal was awarded to Agassiz by the council of that society for his work on fossil ichthyology; and in 1838 he was elected a foreign member of the Royal Society. Meanwhile invertebrate animals engaged his attention. In 1837 he issued the "Prodrome" of a monograph on the recent and fossil Echinodermata, the first part of which appeared in 1838; in 1839–40 he published two quarto volumes on the fossil Echinoderms of Switzerland; and in 1840–45 he issued his Etudes critiques sur les mollusques fossiles ("Critical Studies on Fossil Mollusks").

Before his first visit to England in 1834, the labours of Hugh Miller and other geologists brought to light the remarkable fish of the Old Red Sandstone of the northeast of Scotland. The strange forms of the Pterichthys, the Coccosteus and other genera were then made known to geologists for the first time. They were of intense interest to Agassiz, and formed the subject of a special monograph by him published in 1844–45: Monographie des poissons fossiles du Vieux Gres Rouge, ou Systeme Devonien (Old Red Sandstone) des Iles Britanniques et de Russie ("Monograph on Fossil Fish of the Old Red Sandstone, or Devonian System of the British Isles and of Russia"). In the early stages of his career in Neuchatel, Agassiz also made a name for himself as a man who could run a scientific department well. Under his care, the University of Neuchâtel soon became a leading institution for scientific inquiry.

In 1837 Agassiz was the first to scientifically propose that the Earth had been subject to a past ice age. In the same year, he was elected a foreign member of the Royal Swedish Academy of Sciences. Prior to this proposal, Goethe, de Saussure, Venetz, Jean de Charpentier, Karl Friedrich Schimper and others had made the glaciers of the Alps the subjects of special study, and Goethe, Charpentier as well as Schimper had even arrived at the conclusion that the erratic blocks of alpine rocks scattered over the slopes and summits of the Jura Mountains had been moved there by glaciers. The question having attracted the attention of Agassiz, he not only discussed it with Charpentier and Schimper and made successive journeys to the alpine regions in company with them, but he had a hut constructed upon one of the Aar Glaciers, which for a time he made his home, in order to investigate the structure and movements of the ice.

These labours resulted, in 1840, in the publication of his work in two volumes entitled Etudes sur les glaciers ("Study on Glaciers"). In it he discussed the movements of the glaciers, their moraines, their influence in grooving and rounding the rocks over which they travelled, and in producing the striations and roches moutonnees seen in Alpine-style landscapes. He not only accepted Charpentier's and Schimper's idea that some of the alpine glaciers had extended across the wide plains and valleys drained by the Aar and the Rhône, but he went still farther. He concluded that, in the relatively recent past, Switzerland had been another Greenland; that instead of a few glaciers stretching across the areas referred to, one vast sheet of ice, originating in the higher Alps, had extended over the entire valley of northwestern Switzerland until it reached the southern slopes of the Jura, which, though they checked and deflected its further extension, did not prevent the ice from reaching in many places the summit of the range. The publication of this work gave a fresh impetus to the study of glacial phenomena in all parts of the world.

Thus familiarized with the phenomena associated with the movements of recent glaciers, Agassiz was prepared for a discovery which he made in 1840, in conjunction with William Buckland. The two visited the mountains of Scotland together, and found in different locations clear evidence of ancient glacial action. The discovery was announced to the Geological Society of London in successive communications. The mountainous districts of England, Wales, and Ireland were also considered to constitute centres for the dispersion of glacial debris; and Agassiz remarked "that great sheets of ice, resembling those now existing in Greenland, once covered all the countries in which unstratified gravel (boulder drift) is found; that this gravel was in general produced by the trituration of the sheets of ice upon the subjacent surface, etc."

In 1842–1846 he issued his Nomenclator Zoologicus, a classified list, with references, of all names employed in zoology for genera and groups — a work of great labour and research. With the aid of a grant of money from the King of Prussia, Agassiz crossed the Atlantic in the autumn of 1846 with the twin purposes of investigating the natural history and geology of North America and delivering a course of 12 lectures on “The Plan of Creation as shown in the Animal Kingdom,” by invitation from J. A. Lowell, at the Lowell Institute in Boston, Massachusetts. The financial and scientific advantages presented to him in the United States induced him to settle there, where he remained to the end of his life. He was elected a Foreign Honorary Member of the American Academy of Arts and Sciences in 1846.

His engagement for the Lowell Institute lectures precipitated the establishment of the Lawrence Scientific School at Harvard University in 1847 with him as its head. Harvard appointed him professor of zoology and geology, and he founded the Museum of Comparative Zoology there in 1859 serving as the museum's first director until his death in 1873. During his tenure at Harvard, he was, among many other things, an early student of the effect of the last Ice Age on North America.

He continued his lectures for the Lowell Institute. In succeeding years, he gave series of lectures on “Ichthyology” (1847–48 season), “Comparative Embryology” (1848–49), “Functions of Life in Lower Animals” (1850–51), “Natural History” (1853–54), “Methods of Study in Natural History” (1861–62), “Glaciers and the Ice Period” (1864–65), “Brazil” (1866–67) and “Deep Sea Dredging” (1869–70). In 1850 he married an American college teacher, Elizabeth Cabot Cary Agassiz, who later wrote introductory books about natural history and, after his death, a lengthy biography of her husband.

Agassiz served as a non-resident lecturer at Cornell while also being on faculty at Harvard. In 1852 he accepted a medical professorship of comparative anatomy at Charlestown, Massachusetts, but he resigned in two years. From this time his scientific studies dropped off, but he was a profound influence on the American branches of his two fields, teaching decades worth of future prominent scientists, including Alpheus Hyatt, David Starr Jordan, Joel Asaph Allen, Joseph Le Conte, Ernest Ingersoll, William James, Nathaniel Shaler, Samuel Hubbard Scudder, Alpheus Packard, and his son Alexander Agassiz, among others. He had a profound impact on the paleontologist Charles Doolittle Walcott. In return his name appears attached to several species, as well as here and there throughout the American landscape, notably Lake Agassiz, the Pleistocene precursor to Lake Winnipeg and the Red River.

During this time he grew in fame even in the public consciousness, becoming one of the best-known scientists in the world. By 1857 he was so well-loved that his friend Henry Wadsworth Longfellow wrote "The fiftieth birthday of Agassiz" in his honor. His own writing continued with four (of a planned ten) volumes of Natural History of the United States which were published from 1857 to 1862. During this time he also published a catalog of papers in his field, Bibliographia Zoologiae et Geologiae, in four volumes between 1848 and 1854.

Stricken by ill health in the 1860s, he resolved to return to the field for relaxation and to resume his studies of Brazilian fish. In April 1865 he led a party to Brazil. Returning home in August 1866, an account of this expedition, entitled A Journey in Brazil, was published in 1868. In December 1871 he made a second eight month excursion, known as the Hassler expedition under the command of Commander Philip Carrigan Johnson (brother of Eastman Johnson), visiting South America on its southern Atlantic and Pacific seaboards. The ship explored the Magellan Strait, which drew the praise of Charles Darwin.

Elizabeth Aggasiz wrote, at the Strait: '…the Hassler pursued her course, past a seemingly endless panorama of mountains and forests rising into the pale regions of snow and ice, where lay glaciers in which every rift and crevasse, as well as the many cascades flowing down to join the waters beneath, could be counted as she steamed by them.... These were weeks of exquisite delight to Agassiz. The vessel often skirted the shore so closely that its geology could be studied from the deck.'

   

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William Buckland nasceu há 237 anos

  

William Buckland (Axminster, Devon, 12 de março de 1784 - 24 de agosto de 1856) foi um teólogo britânico que se tornou Deão de Westminster, geólogo e paleontólogo que fez a primeira coleta e descrição completa de um dinossauro nomeado megalossauro, seu trabalho na caverna de Kirkdale comprovando um covil pré-histórico de hiena, e pelo qual foi premiado com a Medalha Copley, foi amplamente elogiado como um exemplo de como a análise científica detalhada pode ser usada para entender a história geológica pela reconstrução de eventos do conceito Tempo Profundo. Foi um pioneiro no uso de fezes, restos fossilizados, pelo qual ele inseriu o termo coprólito, para reconstruir antigos eco-sistemas. Buckland foi o proponente da Teoria do Hiato, que interpretava o acontecimento Bíblico de Génesis se referindo a dois episódios da Criação separados por um período de duração, que surgiu no final do século XVIII e começo do século XIX com uma maneira de reconciliar os acontecimentos das escrituras com as descobertas geológicas que sugeria a terra muito antiga. No começo de sua carreira ele acreditou que tivesse encontrado evidência geológica do Diluvio Bíblico, porém mais tarde convenceu-se que a Era do Gelo de Louis Agassiz era uma melhor explicação, e, ele desempenhou um importante papel na promoção da teoria na Grã Bretanha.

Foi laureado com a Medalha Copley, em 1822, e com a medalha Wollaston, concedida pela Sociedade Geológica de Londres, em 1848.

   

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O geólogo William Buckland nasceu há 235 anos

William Buckland (Axminster, Devon, 12 de março de 1784 - 24 de agosto de 1856) foi um teólogo britânico que se tornou Deão de Westminster, geólogo e paleontólogo que fez a primeira coleta e descrição completa de um dinossauro nomeado megalossauro, seu trabalho na caverna de Kirkdale comprovando um covil pré-histórico de hiena, e pelo qual foi premiado com a Medalha Copley, foi amplamente elogiado como um exemplo de como a análise científica detalhada pode ser usada para entender a história geológica pela reconstrução de eventos do conceito Tempo Profundo. Foi um pioneiro no uso de fezes, restos fossilizados, pelo qual ele inseriu o termo coprólito, para reconstruir antigos eco-sistemas. Buckland foi o proponente da Teoria do Hiato, que interpretava o acontecimento Bíblico de Génesis se referindo a dois episódios da Criação separados por um período de duração, que surgiu no final do século XVIII e começo do século XIX com uma maneira de reconciliar os acontecimentos das escrituras com as descobertas geológicas que sugeria a terra muito antiga. No começo de sua carreira ele acreditou que tivesse encontrado evidência geológica do Diluvio Bíblico, porém mais tarde convenceu-se que a Era do Gelo de Louis Agassiz era uma melhor explicação, e, ele desempenhou um importante papel na promoção da teoria na Grã Bretanha.

Foi laureado com a Medalha Copley, em 1822, e com a medalha Wollaston, concedida pela Sociedade Geológica de Londres, em 1848.

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O geólogo William Buckland nasceu há 230 anos

William Buckland (Axminster, Devon, 12 de março de 1784 - 24 de agosto de 1856) foi um teólogo britânico que se tornou Deão de Westminster, geólogo e paleontólogo que fez a primeira coleta e descrição completa de um dinossauro nomeado megalossauro, seu trabalho na caverna de Kirkdale comprovando um covil pré-histórico de hiena, e pelo qual foi premiado com a Medalha Copley, foi amplamente elogiado como um exemplo de como a análise científica detalhada pode ser usada para entender a história geológica pela reconstrução de eventos do conceito Tempo Profundo. Foi um pioneiro no uso de fezes, restos fossilizados, pelo qual ele inseriu o termo coprólito, para reconstruir antigos eco-sistemas. Buckland foi o proponente da Teoria do Hiato, que interpretava o acontecimento Bíblico de Génesis se referindo a dois episódios da Criação separados por um período de duração; Que surgiu no final do século XVIII e começo do século XIX com uma maneira de reconciliar os acontecimentos das escrituras com as descobertas geológicas que sugeria a terra muito antiga. No começo de sua carreira ele acreditou que tivesse encontrado evidência geológica do Diluvio Bíblico, porém mais tarde se convenceu que a Era do Gelo de Louis Agassiz proveu melhor explicação, e, ele desempenhou um importante papel em promoção da teoria na Grã Bretanha.

Foi laureado com a Medalha Copley, em 1822, e com a medalha Wollaston, concedida pela Sociedade Geológica de Londres, em 1848.

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Louis Agassiz morreu há 138 anos

Jean Louis Rodolphe Agassiz (Môtier, 18 de maio de 1807 - Cambridge, 14 de dezembro de 1873) foi um zoólogo e geólogo suíço, notório por sua Expedição Thayer.

Louis Agassiz nasceu em Môtier (Vully), no Cantão de Friburgo, Suíça. O início da sua educação começou em casa, seguido de quatro anos numa escola secundária em Bienne (alemão Biel), completou os seus estudos elementares na academia de Lausanne. Seleccionando a medicina como a sua profissão, estudou nas universidades de Zurique, Heidelberg e Munique. Em seguida aumentou o seu conhecimento nos processos biológicos, especialmente na Botânica. Em 1829, doutorou-se em Erlangen e em 1830 doutorou-se em medicina em Munique.

Mudou-se para Paris e ficou sobre a tutela de Alexander von Humboldt e de Georges Cuvier, que o lançaram nas suas carreiras da Geologia e do Zoologia respectivamente. Até esta altura não prestou nenhuma atenção especial ao estudo da Ictiologia, a qual se transformou na grande ocupação de sua vida, ou pelo menos na área em que actualmente é mais recordado.

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In 1832 he was appointed professor of natural history in the University of Neuchâtel. The fossil fish there soon attracted his attention. The fossil-rich stones furnished by the slates of Glarus and the limestones of Monte Bolca were known at the time, but very little had been accomplished in the way of scientific study of them. Agassiz, as early as 1829, planned the publication of the work which, more than any other, laid the foundation of his worldwide fame. Five volumes of his Recherches sur les poissons fossiles ("Research on Fossil Fish") appeared at intervals from 1833 to 1843. They were magnificently illustrated, chiefly by Joseph Dinkel. In gathering materials for this work Agassiz visited the principal museums in Europe, and meeting Cuvier in Paris, he received much encouragement and assistance from him. They had known him for seven years at the time.

Agassiz found that his palaeontological labours made necessary a new basis of ichthyological classification. The fossils rarely exhibited any traces of the soft tissues of fish. They consisted chiefly of the teeth, scales and fins, even the bones being perfectly preserved in comparatively few instances. He therefore adopted a classification which divided fish into four groups: Ganoids, Placoids, Cycloids and Ctenoids, based on the nature of the scales and other dermal appendages. While Agassiz did much to place the subject on a scientific basis, this classification has been superseded by later work.

As Agassiz's descriptive work proceeded, it became obvious that it would over-tax his resources unless financial assistance could be found. The British Association came to his aid, and the Earl of Ellesmere — then Lord Francis Egerton — gave him yet more efficient help. The 1,290 original drawings made for the work were purchased by the Earl, and presented by him to the Geological Society of London. In 1836 the Wollaston Medal was awarded to Agassiz by the council of that society for his work on fossil ichthyology; and in 1838 he was elected a foreign member of the Royal Society. Meanwhile invertebrate animals engaged his attention. In 1837 he issued the "Prodrome" of a monograph on the recent and fossil Echinodermata, the first part of which appeared in 1838; in 1839–40 he published two quarto volumes on the fossil Echinoderms of Switzerland; and in 1840–45 he issued his Etudes critiques sur les mollusques fossiles ("Critical Studies on Fossil Mollusks").

Before his first visit to England in 1834, the labours of Hugh Miller and other geologists brought to light the remarkable fish of the Old Red Sandstone of the northeast of Scotland. The strange forms of the Pterichthys, the Coccosteus and other genera were then made known to geologists for the first time. They were of intense interest to Agassiz, and formed the subject of a special monograph by him published in 1844–45: Monographie des poissons fossiles du Vieux Gres Rouge, ou Systeme Devonien (Old Red Sandstone) des Iles Britanniques et de Russie ("Monograph on Fossil Fish of the Old Red Sandstone, or Devonian System of the British Isles and of Russia"). In the early stages of his career in Neuchatel, Agassiz also made a name for himself as a man who could run a scientific department well. Under his care, the University of Neuchâtel soon became a leading institution for scientific inquiry.

In 1837 Agassiz was the first to scientifically propose that the Earth had been subject to a past ice age. In the same year, he was elected a foreign member of the Royal Swedish Academy of Sciences. Prior to this proposal, Goethe, de Saussure, Venetz, Jean de Charpentier, Karl Friedrich Schimper and others had made the glaciers of the Alps the subjects of special study, and Goethe, Charpentier as well as Schimper had even arrived at the conclusion that the erratic blocks of alpine rocks scattered over the slopes and summits of the Jura Mountains had been moved there by glaciers. The question having attracted the attention of Agassiz, he not only discussed it with Charpentier and Schimper and made successive journeys to the alpine regions in company with them, but he had a hut constructed upon one of the Aar Glaciers, which for a time he made his home, in order to investigate the structure and movements of the ice.

These labours resulted, in 1840, in the publication of his work in two volumes entitled Etudes sur les glaciers ("Study on Glaciers"). In it he discussed the movements of the glaciers, their moraines, their influence in grooving and rounding the rocks over which they travelled, and in producing the striations and roches moutonnees seen in Alpine-style landscapes. He not only accepted Charpentier's and Schimper's idea that some of the alpine glaciers had extended across the wide plains and valleys drained by the Aar and the Rhône, but he went still farther. He concluded that, in the relatively recent past, Switzerland had been another Greenland; that instead of a few glaciers stretching across the areas referred to, one vast sheet of ice, originating in the higher Alps, had extended over the entire valley of northwestern Switzerland until it reached the southern slopes of the Jura, which, though they checked and deflected its further extension, did not prevent the ice from reaching in many places the summit of the range. The publication of this work gave a fresh impetus to the study of glacial phenomena in all parts of the world.

Thus familiarized with the phenomena associated with the movements of recent glaciers, Agassiz was prepared for a discovery which he made in 1840, in conjunction with William Buckland. The two visited the mountains of Scotland together, and found in different locations clear evidence of ancient glacial action. The discovery was announced to the Geological Society of London in successive communications. The mountainous districts of England, Wales, and Ireland were also considered to constitute centres for the dispersion of glacial debris; and Agassiz remarked "that great sheets of ice, resembling those now existing in Greenland, once covered all the countries in which unstratified gravel (boulder drift) is found; that this gravel was in general produced by the trituration of the sheets of ice upon the subjacent surface, etc."

In 1842–1846 he issued his Nomenclator Zoologicus, a classified list, with references, of all names employed in zoology for genera and groups — a work of great labour and research. With the aid of a grant of money from the King of Prussia, Agassiz crossed the Atlantic in the autumn of 1846 with the twin purposes of investigating the natural history and geology of North America and delivering a course of 12 lectures on “The Plan of Creation as shown in the Animal Kingdom,” by invitation from J. A. Lowell, at the Lowell Institute in Boston, Massachusetts. The financial and scientific advantages presented to him in the United States induced him to settle there, where he remained to the end of his life. He was elected a Foreign Honorary Member of the American Academy of Arts and Sciences in 1846.

His engagement for the Lowell Institute lectures precipitated the establishment of the Lawrence Scientific School at Harvard University in 1847 with him as its head. Harvard appointed him professor of zoology and geology, and he founded the Museum of Comparative Zoology there in 1859 serving as the museum's first director until his death in 1873. During his tenure at Harvard, he was, among many other things, an early student of the effect of the last Ice Age on North America.

He continued his lectures for the Lowell Institute. In succeeding years, he gave series of lectures on “Ichthyology” (1847–48 season), “Comparative Embryology” (1848–49), “Functions of Life in Lower Animals” (1850–51), “Natural History” (1853–54), “Methods of Study in Natural History” (1861–62), “Glaciers and the Ice Period” (1864–65), “Brazil” (1866–67) and “Deep Sea Dredging” (1869–70). In 1850 he married an American college teacher, Elizabeth Cabot Cary Agassiz, who later wrote introductory books about natural history and, after his death, a lengthy biography of her husband.

Agassiz served as a non-resident lecturer at Cornell while also being on faculty at Harvard. In 1852 he accepted a medical professorship of comparative anatomy at Charlestown, Massachusetts, but he resigned in two years. From this time his scientific studies dropped off, but he was a profound influence on the American branches of his two fields, teaching decades worth of future prominent scientists, including Alpheus Hyatt, David Starr Jordan, Joel Asaph Allen, Joseph Le Conte, Ernest Ingersoll, William James, Nathaniel Shaler, Samuel Hubbard Scudder, Alpheus Packard, and his son Alexander Agassiz, among others. He had a profound impact on the paleontologist Charles Doolittle Walcott. In return his name appears attached to several species, as well as here and there throughout the American landscape, notably Lake Agassiz, the Pleistocene precursor to Lake Winnipeg and the Red River.

During this time he grew in fame even in the public consciousness, becoming one of the best-known scientists in the world. By 1857 he was so well-loved that his friend Henry Wadsworth Longfellow wrote "The fiftieth birthday of Agassiz" in his honor. His own writing continued with four (of a planned ten) volumes of Natural History of the United States which were published from 1857 to 1862. During this time he also published a catalog of papers in his field, Bibliographia Zoologiae et Geologiae, in four volumes between 1848 and 1854.

Stricken by ill health in the 1860s, he resolved to return to the field for relaxation and to resume his studies of Brazilian fish. In April 1865 he led a party to Brazil. Returning home in August 1866, an account of this expedition, entitled A Journey in Brazil, was published in 1868. In December 1871 he made a second eight month excursion, known as the Hassler expedition under the command of Commander Philip Carrigan Johnson (brother of Eastman Johnson), visiting South America on its southern Atlantic and Pacific seaboards. The ship explored the Magellan Strait, which drew the praise of Charles Darwin.

Elizabeth Aggasiz wrote, at the Strait: '…the Hassler pursued her course, past a seemingly endless panorama of mountains and forests rising into the pale regions of snow and ice, where lay glaciers in which every rift and crevasse, as well as the many cascades flowing down to join the waters beneath, could be counted as she steamed by them.... These were weeks of exquisite delight to Agassiz. The vessel often skirted the shore so closely that its geology could be studied from the deck.'

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