First published in Germany in 1855 by the mineralogist Georg Landgrebe (1802–1872), this two-volume work presented the natural history of volcanoes for educated general readers. It reflects the lively
Sir John Frederick William Herschel (1792–1871) – astronomer, mathematician, chemist – was one of the most important British scientists of the nineteenth century. Son of the famous astronomer William Herschel, he was persuaded by his father to pursue the astronomical investigations William could no longer undertake; John's subsequent career resulted in a knighthood and a lifetime of accolades. This 1849 publication was commissioned by the Admiralty to encourage and assist naval officers to undertake scientific research while abroad. The work provides instructions in making and recording observations in a wide range of disciplines – astronomy; magnetism; hydrography; tides; geography; geology; earthquakes; mineralogy; meteorology; atmospheric waves; zoology; botany; ethnology; medicine; statistics – written by experts in these fields, including Whewell, Darwin, Hooker and Herschel himself. It was hoped that the instructions could also be used by other travellers to advance scientific kn
This Italian work, published in Naples in 1897, provides a comprehensive bibliography of works, published in Europe and the United States prior to the twentieth century, on the subject of Mount Vesuvius. Federigo Furchheim (b. 1844) begins with the famous eruption of 1631, on the ground that ancient accounts are sufficiently well known, and that reports and descriptions before the seventeenth century are not reliable. The bibliography is wide-ranging and includes works on other volcanos (such as Santorini), earthquakes and mineralogy. Nor is it confined to factual observations: travel writing, poetry, and even fiction, including Bulwer Lytton's The Last Days of Pompeii, appear alongside scientists such as Sir Humphry Davy and enthusiastic amateurs such as Sir William Hamilton. The book includes a chronological listing of published maps and illustrations, and an appendix, arranged chronologically and by topic, that briefly lists ancient and medieval accounts as well as more modern publi
This two-volume natural history of volcanoes and volcanic phenomena was first published in Germany in 1855 by the chemist and mineralogist Georg Landgrebe (1802–1872) and was intended for scientifically literate enthusiasts rather than for specialists. The book begins with a review of contemporary work on volcanoes, explaining the theories of Leopold von Buch and the lively international debates they had generated among scholars including Charles Lyell, George Poulett Scrope and Charles Daubeny (also reissued in this series). Volume 1 lists the world's volcanoes by region, giving details of their altitude, mineralogy, and recent eruptions (including Etna in 1832 and Mount St Helens in September 1842). Landgrebe makes frequent reference to published work, summarising eyewitness accounts of vegetation, terrain and volcanic activity. He gives particular attention to Vesuvius and to the volcanoes of Iceland and Java, but there is also thorough coverage of the Americas, the Caribbean and th
This two-volume natural history of volcanoes and volcanic phenomena was first published in Germany in 1855 by the chemist and mineralogist Georg Landgrebe (1802–1872), and was intended for scientifically literate enthusiasts rather than for specialists. The book begins with a review of contemporary work on volcanoes, explaining the theories of Leopold von Buch and the lively international debates they had generated among scholars including Charles Lyell, George Poulett Scrope and Charles Daubeny (also reissued in this series). Volume 1 lists the world's volcanoes by region. Volume 2 begins with chapters on earthquakes and other phenomena including hot springs, mud volcanoes and oil wells. It then focuses on the minerals found in volcanic regions, giving details of their composition and structure, references to scientific work about them, and information about locations where they occur. The volume ends with a section on basalts and other rocks associated with volcanoes.
Sir George Steuart Mackenzie (1780–1848) was a Scottish baronet whose interests included chemistry and geology. This work, first published in 1811, is his account of his voyage to Iceland in 1810 for the purposes of mineralogical research. Accompanied by physicians Henry Holland and Richard Bright, Mackenzie surveyed volcanoes, geysers and the other geological features of the island. In addition to reporting the results of the expedition's scientific exploration, this charming and evocative journal describes the history, culture, attire and cuisine of the islanders. Also included are Richard Bright's observations on the zoology and botany of Iceland and a survey of the health of the population by Henry Holland, who introduced smallpox inoculation during his visit. Written in an easy, accessible style, this account brings to life the sights, smells and tastes of the tour and the often rudimentary accommodation and travel conditions.
Alexander von Humboldt (1769–1859) was an intellectual giant: an explorer who helped lay the foundations of biogeography, a naturalist who influenced Charles Darwin, and a botanist who developed a model of the Earth's climate zones. He travelled extensively in Europe, carried out scientific explorations across the Russian Empire and in Latin America, and devoted much energy to seeking a unified view of the different branches of scientific knowledge. Ansichten der Natur, published in 1808 with a second edition in 1826, aimed to 'engage the imagination' as well as to communicate new ideas, and was translated into many European languages. This authorised translation of the third and final 1849 edition, dating from Humboldt's eightieth year, was published in 1850, though another English translation (by Mrs Sabine) had appeared the previous year. The wide coverage, including geology, geography and biology, is typical of Humboldt, as is the precise and engaging style.
The renowned geologist James D. Forbes (1809–68) presents an account of his systematic exploration of alpine mountain regions and glaciers in this important 1843 publication. Forbes' graphic descriptions of alpine scenery and his mountaineering feats are combined with detailed records of his scientific research and experiments. The study cemented Forbes' reputation in the field, which was later to be commemorated by the naming of the Aiguille Forbes in the Alps and of Mount Forbes in both Canada and New Zealand. The aim in writing the book, says Forbes, was to 'illustrate the physical geography of a particular district in one of the most frequented regions of the Alps'. In doing this, he draws upon the important work of the 'bold mountaineer' Horace Bénédict de Saussure, whose feats and achievements Forbes clearly admired. The book is still viewed today as one of the most influential and important publications on mountaineering.
Sir Andrew Crombie Ramsay (1814–91) was a British geologist with a particular interest in the effects of glaciation on the landscape. He travelled in Europe and America, and was a keen climber. His first work, Geology of the Island of Arran (1840), also published in this series, attracted the attention of Roderick Murchison, who found him employment with the Geological Survey, and Ramsay later succeeded Murchison as its director. He carried out important fieldwork in Wales, taught at University College London and the Royal School of Mines, and published a successful textbook. Another major contribution was his work on the origin of lakes: his controversial 1862 proposal that glaciers could hollow out lake basins even in the absence of earth movements was eventually accepted. Ramsay's younger colleague at the Geological Survey, Sir Archibald Geikie (1835–1924), who also wrote a biography of Murchison, published this memoir in 1895.
An industrial chemist by profession, Luke Howard (1772–1864) proposed the method of cloud classification that is still in use today. His life-long interest in meteorology led him to produce this landmark work in the history of the subject. General scientific opinion at the time was that clouds were too changeable to be classified, but, inspired by Linnaeus' work in biological classification, Howard proposed a method which used Latin terminology - cirrus, cumulus, stratus and nimbus - to provide a standard description for each of three groups of cloud types. His work was first published in the Philosophical Magazine in 1803; it was produced in book form in 1832 but went quickly out of print. This reissue is of the third printing (1865) of the edition brought out after his death in 1864 by two of his sons. Howard's other meteorological works are also reissued in this series.
John Tyndall (1820–93) was an Irish physicist who became fascinated by mountaineering after a scientific expedition to Switzerland in 1856. He traversed the summit of the Matterhorn in 1868 and climbed Mount Blanc three times. Alongside this love of mountains was a scientific interest in glaciers and ice formations. Tyndall was also well-regarded for his ability to communicate with the public about science. Many of his books, such as this one, published in 1872 as part of the International Scientific Series, are aimed at the general reader. Tyndall uses this work to explain many aspects of water, beginning with cloud formation and rain before moving on to ice, snow and glaciers. He also discusses the principles behind phenomena ranging from tropical rains to glacial movement. Illustrated and organised into 493 different points under themed headings, this book gives clear explanations of the complexity of the earth's water system.
Throughout the nineteenth century, Britain remained hungry for minerals to fuel her industrial and economic growth. Archibald Liversidge (1846–1927) found his knowledge and research to be in high demand. He had studied at the Royal College of Chemistry, and then obtained an exhibition to Cambridge, where he founded the Cambridge University Natural Sciences Club. At just twenty-seven years old Liversidge was appointed Reader in Geology at the University of Sydney, where he revolutionized the study of minerals and their potential applications. First published in 1876, and reprinted here from the enlarged, third edition of 1888, his chemical audit of the minerals of New South Wales became a key text for students of this field. Divided into two sections that address metallic and non-metallic minerals in turn, and incorporating a detailed map and substantial appendix, this work is of enduring interest and importance to geologists, chemists and historians of science.
In the nineteenth century, scientists were convinced that the North Pole was free of ice. This myth was fostered since the eighteenth century, when it was thought that ice came from rivers and mainly formed near coasts. Rivers supposedly carried into the north seas a prodigious amount of glaçons or 'ice cubes', which formed enormous masses of ice as they accumulated. This misconception led to an inaccurate climate theory that persisted until the beginning of the twentieth century: ice near a country's shores produces bitter cold in that country. This book, published in 1818, links the harsh winters of 1815–17 in England and Europe to the impressive amount of ice encountered at the same time in the Atlantic. The cold was thought to be caused by the break-up and southward drift of Arctic ice. It is attributed to the French meteorologist Antoine Aubriet, who was active in 1815–30.
Despite never graduating from university, Sir Archibald Geikie (1835–1924) forged an exceptionally successful scientific career. In 1855 he was appointed to the Scottish branch of the Geological Survey, and by 1882 was Director General of the Survey. In keeping with his Edinburgh beginnings, most of his career was spent studying igneous rocks. He was a prolific and gifted writer, producing textbooks, popular science books and biographical and historical works, including the influential Founders of Geology (1897), as well as numerous technical publications. The only geologist to hold the post of President of The Royal Society (1908–12), he also served as President of the Geological Society of London and the British Association, and received an array of honorary degrees and medals. This autobiography, published in the year of his death, provides a readable, personal account of the life of one of the great scientific figures of the nineteenth century.
Sir Henry Thomas De la Beche (1796–1855) was a talented and influential geologist. A friend of Mary Anning, he produced the famous lithograph Duria antiquior (1830), the first reconstruction of a scene from an ancient world, to support her work. He promoted government involvement in geology and became the founding Director of the British Geological Survey, which was officially recognised in 1835. Inspired by his work in Cornwall, he later founded the Royal School of Mines and the Museum of Practical Geology. Among his published works was a Manual of Geology (1831), which went through three English editions and was published in France, Germany and America. This 1824 collection of translations includes studies on sites across Europe and notes on the production of an early geological map of France. He also provides a table of equivalent formations and a translation of Brongniart's Classification of the Mixed Rocks.
Swiss-born zoologist, geologist and paleontologist Louis Agassiz (1807–73) was among the foremost scientists of his day. When he took up the study of glaciology and glacial geomorphology in Switzerland in 1836, he recorded evidence left by former glaciers, such as glacial erratics, drumlins and rock scouring and scratching. In this work, published in 1840, he proposed a revolutionary ice-age theory, according to which, glaciers are the remaining portions of sheets of ice which once covered the earth. His radical suggestion undermined the hypothesis that landscape features were the result of a great biblical flood. Although Agassiz's invaluable work led some to acclaim him as the 'father' of glacial theory, critics have cited the contributions of others, including Jean de Charpentier and Karl Schimper. The book also describes the features of active glaciers, including ice tables, ice pinnacles and moraines.
James Geikie (1839–1915) was born in Edinburgh, and his work from 1861 as a field geologist for the Geological Survey in Scotland provided the evidence for the theories he proposes in this work, first published in 1874 (revised editions appeared in 1877 and 1894). Geikie brought together his own research and the findings of other geologists in Scotland to support his main thesis of 'drift' being evidence of the action not of sea ice but of land ice. He was influenced by James Croll's theory that changes in the Earth's orbit led to epochs of cold climate in one hemisphere and warm in the other, and Geikie believed that the geological record provided evidence for inter-glacial periods. The book was hailed as a breakthrough at the time, and brought the author international recognition. With intricate scientific theories explained in clear uncluttered language, this remains a classic text.
Alexander von Humboldt (1769–1859), 'the greatest scientific traveller who ever lived' according to Darwin, made groundbreaking contributions to the fields of geography, oceanography, climatology and ecology. In 1804, he returned from a five-year exploration of Latin America with an incredible wealth of specimens and data which provided the foundations for his theories on the natural order. He expounds them in this book, which was printed in German in 1808 before being translated by the geographer Jean-Baptiste Benoît Eyriès (1767–1846) and published in French in 1828. Humboldt does more than provide descriptions of the great features and phenomena of the Earth, ranging from the geological character of immense plains and steppes to the structure and action of volcanoes. He combines a rigorous scientific approach with his emotional and aesthetic responses to the natural world, thereby constructing a true 'philosophy of nature'.
John Playfair (1748–1819) was a Scottish mathematician and geologist best known for his defence of James Hutton's geological theories. He attended the University of St Andrews, completing his theological studies in 1770. In 1785 he was appointed joint Professor of Mathematics at the University of Edinburgh, and in 1805 he was elected Professor of Natural Philosophy. This highly influential book, first published in 1802, contains Playfair's clarification and summary of Hutton's geological concepts. Playfair concisely explains Hutton's theories on erosion and geothermal heat in rock formation and the concept of uniformitarianism in geology, illustrating these theories with his own precise observations on different types of rock strata. The clarity of Playfair's explanations was instrumental in popularising Hutton's geological theories, many of which are now recognised as key principles of modern geology. Playfair's strident defence of Hutton's ideas formed part of a controversial debate
Leonard Horner (1785–1864) was a prominent geologist, educator and, later, a factory inspector. In 1833 he was appointed to the Royal Commission on the employment of children in factories, and he inspected sites around the north of England. His earlier scientific work saw him elected a fellow of the Royal Society in 1813, and he was twice president of the Geological Society. The two-volume Memoir of Leonard Horner, edited by his daughter, Katharine Lyell, and published in 1890, is a selection of letters to and from his family and friends. The correspondence gives vivid insights into the world of this influential reformer. Volume 1 focuses on Horner's life from his childhood until 1838, taking in many of the key events of his professional career, including his election to the Royal Society, his attempts at improving higher education in Edinburgh and his involvement with the inspection of factories.
