Abstract Although modern geotourism, as a form of sustainable geoheritage tourism, was only recognized as such in the 1990s, its roots lie in the seventeenth century and the Grand Tour with its domestic equivalents. At that time, a few elite travellers recorded their experiences of landscapes, natural wonders, quarries and mines. Such travellers’ observations were supplemented by those of the antiquarians for much of the eighteenth century; at that century’s close, the first modern geologists were recording their observations. The nineteenth century witnessed an explosion in public interest and engagement with geology, and field excursions were provided by the burgeoning natural history and geology societies. By the close of the nineteenth century, the Romantic movement had successfully promoted wild landscapes to a newly expanding urban population. The development of the Grand Tour and the landscape aesthetic movements, the various influential institutions, key personalities and locations are considered insofar as they provide an overview of the background to historical geotourism. All are underpinned by a theoretical consideration of the geotourism paradigm and how geotourism historical studies can contextualize modern geotourism.

Abstract The first evidence of tourism on the Dutch coast can be found in drawings and etchings from the end of the sixteenth century. In this period Holland developed into one of the most urbanized regions of Europe. The interest in landscape originated in the towns. The first scenes depicted are those of mass tourism on the beach: sensation-mongers drawn to the beach by whales, sailing cars and departing kings and queens. Somewhat later the dune landscape became a main recreational focus, in which the physical aspects of the landscape were also appreciated. Around the town of Haarlem, individuals and small groups of people started exploring the dune landscape. In the wake of this new interest, landscape painting developed as an artistic genre. It became the most popular genre in the first half of the seventeenth century, and Haarlem developed as a centre for landscape painters. This paper discusses geomorphological features and geotourism engagement as depicted in several of the early etchings and landscape paintings.

Abstract This paper outlines some significant visits made to north Norway by geologists and mountaineers from Britain and Ireland from the early to late nineteenth century. These visitors wrote up their travels and climbing experiences in a region in north Norway that was difficult to get to other than by sea: Øksfjordjøkelen and Lyngen. Early travellers revealed the sights of the fjord areas and thereby promoted the region for subsequent travellers. Leopold von Buch’s Travels though Norway and Lapland during the Years 1806, 1807, and 1808 probably prompted J. D. Forbes to visit and produce Norway and Its Glaciers and Archibald Geikie’s Geological Sketches at Home and Abroad as part of the contemporary discussions about the ‘glacial theory’. In the latter years of the nineteenth century the British climbers William Cecil Slingsby and George Hastings, with local climber Josef Caspari, explored the Lyngen Peninsula. Elizabeth Main (Mrs Aubrey Le Blond) also climbed in Lyngen. As well as providing written summaries of their exploits, the early explorers included photographs in their books. Some of these images are helpful in the reconstruction of the glacierized landscapes at the end of the Little Ice Age. It is suggested that present-day travellers might leave their observations available, in digital media, for future investigators.

Abstract Local voluntary natural science societies played an important role in the development of early modern geotourism. This chapter explores the development of field, especially geological, excursions and their popularity in two local natural science societies – The Chester Society of Natural Science and the Woolhope Naturalists’ Field Club – from the 1850s to the 1950s. Both societies were established in the borderlands between England and Wales and had a strong emphasis on local and regional scientific studies. They exemplify broader trends in public engagement in the natural sciences and associated fieldwork consequent upon the British socio-political environment. Further, they draw out comparisons between the attitudes of society to excursions and scientific fieldwork, as well as involvement by social status and gender.

Abstract From its earliest days in London in 1858, the Geologists’ Association (GA) brought together people from all backgrounds – amateur and professional geologists, men, women and children – to share their enthusiasm for geology and their desire to seek out and explore the geological world around them. The travels of the Geologists’ Association, in search of geological enlightenment, are documented in the Proceedings of the Geologists’ Association . These include accounts of organized excursions, detailing the geology seen and describing the discussion had, the refreshments taken and the transport used. Bringing these accounts to life is the Geologists’ Association’s Carreck Archive, which provides a rare insight into the world of the early geotourist documenting both familiar and lost places. Much is owed to the skill of the photographers such as T. W. Reader, whose albums document the field meetings between 1907 and 1919, while the spirit of the early travelling Geologists’ Association is captured in the albums of Miss M. S. Johnston. This paper explores the early travels of the Geologists’ Association through the literal views of the Carreck Archive and accounts in its literature, and the establishment of the GA as an inadvertent geotourism agent.

Abstract The limestone caves of Stoney Middleton Dale are a Site of Special Scientific Interest (SSSI) for features of geological interest, but have been open access since at least the eighteenth century and have a documented history of geotourism. Using the examples of Carlswark Cavern and Merlin Cavern, this chapter sets out evidence that 300 years of open access has resulted in significant disturbance to the features of geological interest. In particular, the integrity of the overall site for scientific research was affected by historical removal of speleothem formations long before it became a SSSI, with damage still occurring today. As most cave SSSIs in Derbyshire have historically had similar open-access arrangements, the examples presented highlight that there is potential for the integrity of less well historically documented caves elsewhere to have been disturbed. This article highlights the importance of establishing a baseline of historical disturbance to recognize whether the integrity of cave SSSIs have been affected and help monitor if disturbance is still occurring. For cave SSSIs to be useful for geological research, it is suggested that there is a need for the historical legacy of open access to individual caves elsewhere to be better understood.

Abstract Carclaze tin mine was an open pit operation which exploited a massive cassiterite-bearing greisen-bordered quartz-tourmaline vein stockwork, straddling the granite margin near St Austell. It became a ‘must-see’ location for visitors to Cornwall from all over Europe in the late eighteenth and early nineteenth centuries, particularly those interested in the then-fashionable pursuits of geology and mineralogy. Intellectually, the early scientific interest in Carclaze can be seen as part of the Enlightenment, but in the nineteenth century the influence of Romanticism can also be detected. Much of the attraction was due to the openness and accessibility of Carclaze pit, which allowed the geology to be easily appreciated. This resulted in the development of the mine being particularly well documented by a large number of contemporary accounts and illustrations, which has also enabled an early, partly underground, canal to be rediscovered. The earliest account was by the Frenchman M. Jars who visited the pit in 1765; this was followed by accounts by other French geotourists from the early to mid-nineteenth century. The Germans Von Oeynhausen and Von Dechen provided the first geological map and cross-section of the pit in 1829. Accounts by local Cornish authors emphasize that Carclaze was a significant ‘sight’ for visitors. The earliest account of the pit by an English geologist was by Adam Sedgwick in 1822 ; in later publications he speculated on the formation of parallel vein swarms and schorl rock, partly based on his observations in Carclaze Old Tin Pit. De la Beche provided a pen-and-ink sketch of the south face of the pit in 1839. There are also many accounts by non-scientific visitors throughout the nineteenth century and, together with published lithographs, these are particularly helpful in describing and showing the methods of mining. Tin extraction from the Old Tin Pit had practically ceased by the mid-nineteenth century as production switched to china clay from new pits to the north. The historic south face of the Old Tin Pit, as illustrated by De La Beche, has survived into the twenty-first century and has been designated a County Geology Site by the Cornwall Geoconservation Group, although it is now threatened by housing and industrial development proposals.

Abstract This paper traces the touristic trajectories of three spectacular gorges located in the Alpine foreland and the southern Jura: the gorges of the upper Rhône (Ain/Haute-Savoie), the Sierroz (Savoie) and the Fier (Haute-Savoie). All three are located within a distance of 50 km from each other. The upper Rhône gorge, already famous at the end of the eighteenth century, was drowned under the floodwaters of the Génissiat dam in 1948; only a significant iconography remains of two centuries of (geo)tourism. The Sierroz gorge, close to the spa resort of Aix-les-Bains, became famous after the dramatic and tragic death in 1810 of a young noblewoman. Following that event many tourists staying on the shore of the lake Bourget visited the gorge until 1970 when it was closed to the public. Since then, the gorge has gradually become a touristic wasteland. The Fier gorge near Annecy became a tourist attraction in 1869 with the opening of the nearby railway station of Lovagny; since then, visitors have been attracted to it in increasing numbers. The history of these three gorges illustrates how tourism and heritage are in constant interaction; however, the development of the one will not always ensure the protection of the other. Today, geoheritage assessment is based upon criteria that are as objective as is possible. The intrinsic geological and geomorphological characteristics are the initial geoheritage values, to which can be added the cultural value elements. Associated with the development of geotourism and geoparks, this new approach should ensure a better and sustainable use of these sites in the long term.

Abstract The Sudetes is a mountain range in Central Europe and an area of remarkable geodiversity. In recent years, the area has been promoted as a geotourist destination and various initiatives aimed at better understanding geoheritage have been implemented. An interest in scenic landscapes is not new however, and dates back to the end of the eighteenth century. Two areas within the Sudetes are cradles of local nature-based tourism. These are the granite massif of the Karkonosze in the west and the sandstone stepped plateau of Broumov Highland and Stołowe Mountains in the central part of the Sudetes. In both, physical access to the key geosites was provided as early as in the nineteenth century, while an interpretation component was added in the early twentieth century. A side-effect of political change following the end of World War II was the neglect and dilapidation of many sites, as well as the disappearance of geoheritage appreciation from the collective social memory. In the last decade many of those early achievements were rediscovered and provided the foundations for contemporary activities. An educational component based on modern science is now included in the features which were discovered as tourist attractions long ago.

Abstract Loess is wind-blown sediment that covers extensive areas in the middle latitudes. Much of the loess in Eastern and Central–Eastern Europe has been redeposited by the River Danube and its tributaries. The case study area (Vojvodina region) encompasses the confluence area of the Danube, Sava and Tisa rivers. This region includes the most complete and the thickest loess–palaeosol sequences found in Europe, a valuable record of palaeo-climates over the past two million years only recognized in the closing decades of the twentieth century. Long before then however, several enthusiasts, engineers and travellers recognized and appreciated loess as a significant natural phenomenon. Among them was Luigi Ferdinando Marsigli (1658–1730) who gave the first scientific description of European loess in his outstanding multivolume work Danubius Pannonico Mysicus where he drew and explained notable loess–palaeosol exposures along the Danube River. Many other loess observations were also recorded by a number of international travellers, whose illustrated travelogues (mainly published in the nineteenth century) mentioned and illustrated loess observations along the Danube and its major tributaries. This chapter explores the interplay of scientific loess research and its geo-historical literary aspects as the foundations of modern loess geotourism.