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.
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.
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.
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.
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.
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 2 covers the period 1839–1864, and includes letters about Horner's activities at the Geological Society, his travels in Italy in 1861, his political concerns, and key moments in his personal life, such as the birth of his grandson in 1850.
Mount Etna in Sicily is one of a small number of active volcanoes in the Mediterranean area, where written history survives from more than two millennia: its eruptions are therefore among the best documented in the world. This account of the eruption of 1819 was written by the chemist and vulcanologist Carmelo Maravigna, a professor at the University of Catania, who was commissioned by his colleagues to make scientific observations of the phenomena and to publish them in a clear and methodical format. Maravigna's book opens with the diary of his own observations from 27 May to 5 August 1819; it then describes the physical consequences of the eruption, including the spread and depth of lava flows, and discusses various theories of volcanic activity. The sixth chapter analyses the mineral deposits in the lava, and the last describes the volcano returned to its dormant state.
Jean François Aubuisson de Voisins (1769–1841) was a French geologist and engineer who studied under Abraham Gottlob Werner at Freiberg together with Humboldt, von Buch and Jameson. Werner had coined the term geognosy to define a science based on the recognition of the order, position and relation of the layers forming the earth. His theory of the marine origins of the Earth's crust (Neptunism) was widely accepted at the time. Aubuisson however showed that igneous rocks such as basalt were similar to surface lava flows, and were not chemical precipitates of the ocean. His two-volume Traité de Géognosie, published in 1819, was one of the earliest geology books in French. It was highly successful, and gained him wide professional recognition. Volume 2 describes different categories of rocks and minerals, and formations including basalt dykes, ore deposits, and intruded veins. It also puts forward arguments challenging some of Werner's theories.
Jean François Aubuisson de Voisins (1769–1841) was a French geologist and engineer who studied under Abraham Gottlob Werner at Freiberg together with Humboldt, von Buch and Jameson. Werner had coined the term geognosy to define a science based on the recognition of the order, position and relation of the layers forming the earth. His theory of the marine origins of the Earth's crust (Neptunism) was widely accepted at the time. Aubuisson however showed that igneous rocks such as basalt were similar to surface lava flows, and were not chemical precipitates of the ocean. His two-volume Traité de Géognosie, published in 1819, was one of the earliest geology books in French. It was highly successful, and gained him wide professional recognition. Volume 1 examines the earth, its size, atmosphere and oceans. Aubuisson describes the various processes that affect the surface of the earth, and how mineral deposits are laid down.
Robert Jameson (1774–1854) was a renowned geologist who held the chair of natural history at Edinburgh from 1804 until his death. A pupil of Gottlob Werner at Freiberg, he was in turn one of Charles Darwin's teachers. Originally a follower of Werner's influential theory of Neptunism to explain the formation of the earth's crust, and an opponent of Hutton and Playfair, he was later won over by the idea that the earth was formed by natural processes over geological time. He was a controversial writer, accused of bias towards those who shared his Wernerian sympathies such as Cuvier, while attacking Playfair, Hutton and Lyell. He built up an enormous collection of geological specimens, which provided the evidence for his System of Mineralogy, first published in 1808 and here reprinted from the second edition of 1816. Jameson's position in the academic world helped prolong the acceptance of Werner's theory.
Robert Jameson (1774–1854) was a renowned geologist who held the chair of natural history at Edinburgh from 1804 until his death. A pupil of Gottlob Werner at Freiberg, he was in turn one of Charles Darwin's teachers. Originally a follower of Werner's influential theory of Neptunism to explain the formation of the earth's crust, and an opponent of Hutton and Playfair, he was later won over by the idea that the earth was formed by natural processes over geological time. He was a controversial writer, accused of bias towards those who shared his Wernerian sympathies such as Cuvier, while attacking Playfair, Hutton and Lyell. He built up an enormous collection of geological specimens, which provided the evidence for his System of Mineralogy, first published in 1808 and here reprinted from the second edition of 1816. Volume 3 deals with metal ores such as gold, iron and lead.
Robert Jameson (1774–1854) was a renowned geologist who held the chair of natural history at Edinburgh from 1804 until his death. A pupil of Gottlob Werner at Freiberg, he was in turn one of Charles Darwin's teachers. Originally a follower of Werner's influential theory of Neptunism to explain the formation of the earth's crust, and an opponent of Hutton and Playfair, he was later won over by the idea that the earth was formed by natural processes over geological time. He was a controversial writer, accused of bias towards those who shared his Wernerian sympathies such as Cuvier, while attacking Playfair, Hutton and Lyell. He built up an enormous collection of geological specimens, which provided the evidence for his System of Mineralogy, first published in 1808 and here reprinted from the second edition of 1816. Volume 2 continues 'earthy minerals' and covers saline and inflammable minerals, including coals.
Robert Jameson (1774–1854) was a renowned geologist who held the chair of natural history at Edinburgh from 1804 until his death. A pupil of Gottlob Werner at Freiberg, he was in turn one of Charles Darwin's teachers. Originally a follower of Werner's influential theory of Neptunism to explain the formation of the earth's crust, and an opponent of Hutton and Playfair, he was later won over by the idea that the earth was formed by natural processes over geological time. He was a controversial writer, accused of bias towards those who shared his Wernerian sympathies such as Cuvier, while attacking Playfair, Hutton and Lyell. He built up an enormous collection of geological specimens, which provided the evidence for his System of Mineralogy, first published in 1808 and here reprinted from the second edition of 1816. Volume 1 deals with what Jameson terms 'earthy minerals', including diamonds, rubies and feldspar.
The geologist Joseph Beete Jukes (1811–1869) studied at Cambridge under Adam Sedgwick (1785–1873). Between 1839 and 1846, he participated in expeditions to the coasts of Newfoundland, Australia and New Guinea. This posthumous book, edited by Jukes' sister and published in 1871, contains selected highlights from Jukes' professional and personal writings. After a short biographical sketch, the material is arranged chronologically, beginning with Newfoundland and Australia and then focusing on Britain and Ireland, where Jukes was involved with national geological surveys. Linking passages by the editor explain the contexts of the pieces, and the book includes a list of Jukes' publications. Jukes lived during an exciting period that saw far-reaching discoveries and advances in his field, and his energy and enthusiasm permeates even his technical communications. Modern readers, like the original audience, will form a vivid impression of Jukes' lively personality, his 'penetrating glance
The geologist Joseph Beete Jukes (1811–1869) studied at Cambridge under Adam Sedgwick (1785–1873). In 1841, having already gained field experience in England and Newfoundland, he joined the H.M.S. Fly as a naturalist for an upcoming four-year expedition to chart the coasts of Australia and New Guinea. In 1847, he published a two-volume Narrative of the Surveying Voyage of H.M.S. Fly (also reissued in this series). That was followed in 1850 by this pioneering study of the geology of Australia, which drew on Jukes' own observations as well as on some earlier work. It describes features including the mountains along the East coast, raised beaches, alluvial plains and the Great Barrier Reef, and rock types from limestone and sandstone to granite and lava. The book made an important contribution to the scientific literature on Australia at a time when that continent was still largely unknown to European scholars.
James Bryce (1806–77) was a Scottish schoolteacher and geologist. His numerous articles on geology earned him a place in the Geological Society of London (1834) and in the Royal Society of Edinburgh (1875). He also campaigned to reform the Scottish universities and for Scottish education to be independent of the English system. In 1855 Bryce conducted a geological survey of Clydesdale and the Isle of Arran for the British Association for the Advancement of Science (BAAS). His findings were published the same year, in this book. Bryce's study records the natural history of the two regions, with descriptions of the geological features encountered on various expeditions in Arran. Bryce also describes the Arran flora, marine fauna, and rare insect life. This book remained the geological authority on Arran and Clydesdale for a long time; the third edition, reissued here, was published in 1865.
Luke Howard (1772–1864) was a pharmacist and businessman, but is most famous for his contributions to meteorology. He classified clouds by their appearance and gave them their modern names of cumulus, cirrus, nimbus and stratus. He was educated at a Quaker school in Oxfordshire, then trained as a pharmacist, but was fascinated by weather throughout his life, and developed into a keen amateur meteorologist. He wrote several important texts on the subject including The Climate of London, an early study in urban climatology, and On the Modification of Clouds (both also reissued in this series). Published in 1837, Seven Lectures on Meteorology covers the components of the atmosphere, seasonal variation in winds and temperature, the use of barometers, cloud structure, and visual phenomena such as rainbows and the Aurora Borealis. This reissue also includes Howard's short 1842 book which details selected British weather data from 1824 to 1841.
William Phillips (1773–1828) was a printer and geologist who became a Fellow of the Royal Society in 1827. A founder of the London Askesian Society, he was also an active member of the British Mineralogical Society. In 1807 he and twelve others founded the Geological Society of London, and he was described by the Society's historian as 'the most distinguished, as a geologist, of the original founders'. His pioneering 1818 digest of British geology, Outlines of the Geology of England and Wales, was the most ambitious and influential work of its kind. Phillips gave free lectures to young people in his village in 1814, and these were published the following year. This work followed in 1816, and both went on to become standard textbooks. Aimed at students, it collects observations of a wide range of minerals' characteristics and occurrence, incorporating crystallographic work using the new reflecting goniometer.
Prussian explorer and naturalist Alexander von Humboldt (1769–1859) was described by Darwin as 'the greatest scientific traveller who ever lived'. His boundless curiosity as well as his scientific and cultural knowledge helped lay the foundations of physical geography, climatology, ecology and oceanography. In 1799, Humboldt embarked on a five-year trip to explore Central and South America. He devoted a large amount of time to the study of géognosie, the science of the origin and distribution of minerals and rocks forming the earth, later known as geology. In 1805, Humboldt published his first impressions of volcanoes and earthquakes in the Americas in his Personal Narrative. In this 1826 work, he makes the first systematic attempt to compare the rocks of the Old and New Worlds. This groundbreaking analysis became one of the most important geological works of its time.
Prussian explorer Alexander von Humboldt (1769–1859) was one of the most respected scientists of his day, influencing the work of Darwin. He is considered the founder of physical geography, climatology, ecology and oceanography. In 1829, the Russian government invited Humboldt to visit the gold and platinum mines in the Urals. As he studied the mountains' mineral wealth, he was the first to predict the presence of diamonds. During six months, his epic 10,000-mile expedition took him as far as the Altai Mountains and the Chinese frontier. Humboldt's observations on the geography, volcanic geology and meteorology of Central Asia, being then a largely unexplored territory, were acknowledged as pioneering contributions. The results of his journey also provided much of the data used in part of his great work Kosmos. The second volume of this book, published in 1831, deals with the hydrology and climatology of Central Asia.
