Abstract Radon ( 222 Rn) has been highlighted by a number of authors as a significant public health concern. For example, it is the second most significant cause of lung cancer after tobacco smoking ( c. 1000–2000 and 21 000 deaths per year in the UK and USA, respectively), yet a very high proportion of the general public appears to be unaware of the risk. This chapter deals with topical radon issues, such as: radon in the workplace; radon in homes; exposure to radon during leisure activities; radon and water; measurement and monitoring; seasonal correction; remediation; cancer risks; cost–benefit analysis and cost-effectiveness; mapping; future policies; and further research. This assessment of the state of radon research is focused on the UK as an example of a country where radon has been on the governmental agenda since the late 1970s, but also highlights radon issues throughout the world in, for example, the USA, Europe and Asia.

Abstract Up until the late 1980s geology contributed very little to the study of tsunamis because most were generated by earthquakes which were mainly the domain of seismologists. In 1987–88 however, sediments deposited as tsunamis flooded land were discovered. Subsequently they began to be widely used to identify prehistorical tsunami events, providing a longer-term record than previously available from historical accounts. The sediments offered an opportunity to better define tsunami frequency that could underpin improved risk assessment. When over 2200 people died from a catastrophic tsunami in Papua New Guinea (PNG) in 1998, and a submarine landslide was controversially proven to be the mechanism, marine geologists provided the leadership that led to the identification of this previously unrecognized danger. The catastrophic tsunami in the Indian Ocean in 2004 confirmed the critical importance of sedimentological research in understanding tsunamis. In 2011, the Japan earthquake and tsunami further confirmed the importance of both sediments in tsunami hazard mitigation and the dangers from seabed sediment failures in tsunami generation. Here we recount the history of geological involvement in tsunami science and its importance in advancing understanding of the extent, magnitude and nature of the hazard from tsunamis.

Abstract In January 2013, the US WISSARD programme measured and sampled Lake Whillans, a subglacial water body at the edge of West Antarctica, in a clean and environmentally sensitive manner, proving the existence of microbial life beneath this part of the ice sheet. The success of WISSARD represented a benchmark in the exploration of Antarctica, made possible by a rich and diverse history of events, discoveries and discussions over the past 60 years, ranging from geophysical measurement of subglacial lakes to the development of scientific hypotheses concerning these environments and the engineering solutions required to test them. In this article, I provide a personal account of this history, from the published literature and my own involvement in subglacial lake exploration over the last 20 years. I show that our ability to directly measure and sample subglacial water bodies in Antarctica has been made possible by a strong theme of international collaboration, at odds with the media representation of a scientific ‘race’ between nations. I also consider plans for subglacial lake exploration and discuss how such collaboration is likely to be key to success of future research in this field.

Abstract The 2011 Tohoku earthquake, tsunami and resulting damage is often referred to as 3.11 after the date on which it took place. Leading to almost 20 000 people dead or missing, a major nuclear disaster and severe economic damage, 3.11 represents the biggest challenge faced by Japan since the end of World War II. Before 3.11, the possibility of a Mw 9 earthquake in this area was not generally recognized, highlighting the need to reassess seismic risk in NE Japan. The large amount of new quantitative data covering a range of disciplines and from onshore and offshore studies makes 3.11 an important case study that can contribute to improving our understanding of tsunamis, including their formation, their effects on coastal regions and the effectiveness of defensive measures old and new. Geological studies have a key role to play in this new phase of tsunami studies and this is the only method available for determining recurrence intervals over timescales of thousands of years. Data from 3.11 have improved our ability to identify sedimentary records of tsunami events and to estimate tsunami size from geological data. More complete databases will provide invaluable information for long-term planning of coastal regions in convergent plate margins.

The Mesozoic and Paleogene pelagic carbonate rocks of the Northern Apennines have proved to be a fertile source for paleomagnetic research. Investigations of the magnetic properties of the Scaglia limestones illuminated the processes by which they were magnetized. Their directions of remanent magnetization contributed to an understanding of the geodynamic history of Adria as a promontory of the African plate and have been used to refine the Mesozoic part of the African polar wander path. Magnetic stratigraphy in the Umbrian sequence and in similar facies in the southern Alps has established an independent record of geomagnetic polarity history since the Middle Jurassic. Correlation with the record derived from interpretation of oceanic magnetic anomalies mutually confirmed the global nature of the polarity history. This enabled the dating of plate motions and the development of a geomagnetic polarity time scale for the late Mesozoic and Cenozoic.

The Great Lakes Geologic Mapping Coalition (GLGMC), consisting of state geological surveys from all eight Great Lakes states, the Ontario Geological Survey, and the U.S. Geological Survey, was conceived out of a societal need for unbiased and scientifically defensible geologic information on the shallow subsurface, particularly the delineation, interpretation, and viability of groundwater resources. Only a small percentage (<10%) of the region had been mapped in the subsurface, and there was recognition that no single agency had the financial, intellectual, or physical resources to conduct such a massive geologic mapping effort at a detailed scale over a wide jurisdiction. The GLGMC provides a strategy for generating financial and stakeholder support for three-dimensional (3-D) geologic mapping, pooling of physical and personnel resources, and sharing of mapping and technological expertise to characterize the thick cover of glacial sediments. Since its inception in 1997, the GLGMC partners have conducted detailed surficial and 3-D geologic mapping within all jurisdictions, and concurrent significant scientific advancements have been made to increase understanding of the history and framework of geologic processes. More importantly, scientific information has been provided to public policymakers in understandable formats, emphasis has been placed on training early-career scientists in new mapping techniques and emerging technologies, and a successful model has been developed of state/provincial and federal collaboration focused on geologic mapping, as evidenced by this program’s unprecedented and long-term successful experiment of 10 geological surveys working together to address common issues.

African geological surveys are playing an important role in local and global development. Core functions are mapping, mineral exploration, geophysics, geochemistry, research, and geoengineering. Regulatory functions, geohazards, training, environment, water resources, and land-use planning are also addressed by some. Most African geological surveys were founded to assist in the search for mineral resources, but they have had to adapt to a much wider field of responsibilities in more recent times. Examples from the Geological Survey of Namibia are given. Faced with challenges of funding and skills shortage, African geological surveys have united under the auspices of the Organization of African Geological Surveys in order to jointly resolve the difficulties experienced.

The western Pacific region contains 22 independent island countries and territories spread over an area of 27.8 million km 2 . Pacific peoples have lived here for as long as 50,000 yr, developing isolated cultures with close relationships to the environment. Although food security is adequate, the region suffers from persistent poverty that places many in a precarious position. Beginning in the 1920s, geological surveys conducted pioneering studies geared toward development. Beginning in the mid-1990s, many aid donors shifted their focus away from science, leading to a depletion of geo-science capacity. Lately, regional organizations have made considerable headway in expanding scientific capacity. The Geoscience Division of the Secretariat of the Pacific Community plays a significant role in helping the region attract geoscience-related aid funding and stitching the dispersed geoscience communities together. Universities in the region, assisted by geoscientists abroad and private employers, are also playing a role. This paper describes three examples of how geoscience can contribute to inclusive sustainable development. One example explores deep-sea minerals as a new source of wealth generation and the challenges the region faces in developing capacity and addressing the environmental concerns of this new revenue stream. A second project in Kiribati has moved aggregate extraction from beaches only 3 m above sea level to sediment-rich lagoons, providing new options for the future. Lastly, the promises and benefits of sustainable geothermal and ocean thermal technology are described.

Many geoscientists apply their expertise to international community development through projects that involve direct interaction with host country agencies, community groups, and individuals. As someone with expertise or financial resources, one often has power to frame the definition of success around one’s own perceived reality regarding human development. Both local counterparts and international geoscientists themselves are often in a position to shape project goals toward their own needs and interests, rather than those of intended beneficiaries. We argue that one-sided engagement is often ineffective and even harmful for target beneficiaries. Awareness of such power dynamics minimizes the waste of resources and unintentional perpetuation of harmful social dynamics. Guidelines are presented in this editorial to help geoscientists partner equitably with groups or communities they intend to serve. The guidelines in this editorial may assist geoscientists to identify the felt needs of their target beneficiaries, define their own role in meeting those needs, define project goals of mutual interest, and make progress toward meeting felt needs. These guidelines include: (1) form relationships and build trust; (2) understand the local context; (3) be observant of internal power relations; (4) examine your motivations and expertise; (5) utilize local expertise in project implementation; and (6) recognize change takes time and investment in monitoring and evaluation. Although equitable engagement is rarely straightforward, especially in an unfamiliar cultural or socioeconomic context, it is crucial if geoscientists are to contribute effectively to global development.

To better understand regional variations in radon occurrences, the Kentucky Geological Survey (KGS) is working in partnership with the University of Kentucky College of Nursing’s Clean Indoor Air Partnership to examine spatial and statistical associations between residential radon measurements and near-surface geologic rock formations that may serve as a radon source or pathway. A primary goal is to understand potential risk for population-level radon exposure. The Clean Indoor Air Partnership has been investigating the associations among radon prevalence, secondhand smoke, and lung cancer risk reduction. KGS and faculty in the College of Nursing formed a partnership to better understand the spatial variability of radon incidence by using a geologically referenced radon data set. Two studies have taken place, and one is currently under way. To facilitate the collaboration, a pilot study by KGS compared radon values to geologic formations in Boyle County, Kentucky. This study helped to communicate radon occurrence less in terms of political boundaries and more in terms of physical phenomena. The next phase of collaboration is a statistical analysis of the radon data in higher-population areas (central and northern Kentucky) to define those geologic units spatially associated with the high radon values. This will enable College of Nursing researchers to systematically target areas with the most potential for high radon exposure levels. The latest collaboration will create five county maps using residential radon testing values (supplied by the College of Nursing) to advance radon education and awareness and reduce lung cancer risk in Kentucky.

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 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.

Abstract The Late Cretaceous (Cenomanian–Maastrichtian) Chalk Group and Eocene (Ypresian) London Clay Formation are two British marine deposits that yield globally significant assemblages of fossil actinopterygian (ray-finned) fishes. Materials from these units, especially the Chalk, featured prominently in the work of Arthur Smith Woodward. Here we summarize the history of study of actinopterygian fossils from the Chalk and London Clay, review their geological and palaeoenvironmental context and provide updated faunal lists. The Chalk and London Clay are remarkable for preserving fossil fishes in three dimensions rather than as the flattened individuals familiar from many other famous Lagerstätten , as well as capturing detailed ‘snapshots’ of marine fish faunas that bracket the major taxonomic shift that took place near the Cretaceous–Palaeogene boundary.

Abstract Although primarily a pre-eminent palaeoichthyologist, Arthur Smith Woodward’s research and publications ranged across all major tetrapod groups: nevertheless, his contributions in this area have generally been overshadowed by involvement in the ‘Piltdown Man’ affair. Smith Woodward published on fossil amphibians, every major group of reptiles and on mammals. Most of the new taxa he named remain valid, a testament to his wide knowledge and understanding of fossil vertebrates beyond his principal speciality, although some of these have now been extensively revised. He travelled widely in Europe and the Americas, resulting in some of the earliest work on Gondwanan Cretaceous reptiles. Several of his taxa revealed the existence of previously unknown groups (e.g. notosuchian crocodiles) or provided important character data that have fuelled various phylogenetic debates (e.g. snake and tyrannosauroid origins). His influence extended beyond his own scientific efforts to incorporate his role as a senior administrator, supporting the acquisition of significant reptile specimens for the collection, and as an educator, producing articles for museum visitors and the general public.

Abstract In 1908, Carl Wiman of Uppsala University, Sweden, discovered rich horizons with Triassic vertebrate remains in Spitsbergen on Svalbard, Norway. This marked the beginning of vertebrate palaeontology as a science in Sweden, subsequently developed mainly through the collection and study of non-Swedish fossil remains. Wiman’s accomplishments, resolute personality and a tight network of influential friends and supporters enabled him to become the first person in Sweden to hold a university chair in Palaeontology and Historical Geology. He also managed to amass large numbers of unique fossil vertebrate specimens culminating in an extensive Chinese collection of both world famous dinosaurs and Neogene mammals deposited at Uppsala University. Joint scientific Sino-Swedish collaboration and a deliberate Swedish scientific agenda ensured this unprecedented situation in an opportune moment. Governmental support and initiative allowed Uppsala University and Carl Wiman’s Palaeontological Institute to erect a museum building dedicated foremost to the Chinese material, now known as the Lagrelius Collection in recognition of the patron behind Wiman’s ambitious endeavours. In addition, the museum served as a permanent repository for seminal collections of Mesozoic fossils from Svalbard and North America. Collectively, these represent a landmark research and teaching resource that remains of intense scientific interest even today.

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 This paper focuses on the continental shelf of NW Australia, and on models for change in littoral and offshore environments of relevance to human occupation over the last 50 kyr. Major island groups occur on the shelf including the Montebello and Barrow islands, and those of the Dampier Archipelago. At lowest sea level around 22 ka, these would have been uplands that then became progressively isolated by subsequent sea-level rise. By integrating archaeological and zooarchaeological records from excavations on these islands with the geology and geomorphology, we interpret palaeoeconomic resource potential in relation to changing sea level and coastline morphology. The preservation potential for submerged archaeological sites and features is also assessed. Current archaeological evidence from these offshore islands indicates that the submerged coastal landscape is likely to have been a potentially rich environment for resources and human occupation, even at times of lowest sea level and regional aridity. Should any exploration of submerged archaeology be carried out in this region, it is likely to be rewarding, offering unique insights into Late Pleistocene coastal occupation.

Abstract Sealed, submerged palaeoenvironmental deposits date the time range for lithic technologies and enable inferences about cultural change – potentially more accurately than radiometric methods. Sea-level rises triggered by global warming reduce available land, and change the availability of flora, fauna, geological resources, rivers and wetlands. Australian archaeological studies on human adaptation to climate change focus mainly on terrestrial sites, coastal intensification and the few archaeological sites that were not inundated. The South West Arm project at Port Hacking, south of Sydney, looks at the potential for rock shelters to survive inundation and expand the sites available for studying human adaption to climate change. Site prediction was based on recorded terrestrial rock-shelter landforms at South West Arm. Underwater surveys were conducted by divers who located, photographed and mapped similar formations. No excavation was conducted. The pre-disturbance survey examined approximately 1800 m of seabed, between water depths of 0 and 9 m, primarily along the eastern shoreline of South West Arm where the seabed emulates the steep slope, with sandstone rock outcrops that form terraces and rock overhangs above water. Twelve submerged rock overhangs were recorded and confirmed the potential for rock-shelter sites to survive the process of inundation.

The scientific study of Texas caves and karst has passed two distinct periods and is on the verge of crossing into a third. The first period dates from 1849 to 1982. At that time, the word “karst” was unknown to most geologists in the state. Caves were occasionally mentioned in geological reports until 1948, but they were rarely studied. In the 1960s, cave explorers-turned-scientists began investigating Texas caves, but their work was often seen as lightweight science because caves were usually considered geologic curiosities of little importance. However, extensive exploration and documentation of caves, plus some respected cave research outside of the geosciences, led to the second period of research, dating from 1983 to the present. This was a transitional period where karst was increasingly recognized and karst research methods were pioneered, although often by people lacking sufficient understanding of karst to be fully accurate or effective. During this period, the expertise of karst scientists gained respect despite the persistence of some old prejudices, and caves began to reappear with greater frequency in technical reports. Many of these changes were prompted by the listing of several karst invertebrates as endangered species, which required detailed hydrogeological cave and karst research, in addition to biological research, across much of the Edwards Aquifer region. The third period of karst research has nearly arrived. It will be recognized when most geoscientists understand karst, that it requires specialized training and experience like other geological disciplines, and when research of karst areas routinely uses karst-appropriate tools, theories, and consideration for the many degrees of permeability that occur. The future of cave and karst research in Texas will see important technological advances and a focus on hydrological and biological karst resource management as the combined impacts of population growth and climate change increasingly affect the state.

Extract from beginning of chapter: THE DREAM Japan! The dream of my life since the time my father had imported a collection of curios and things Japanese, because of their artistic beauty and strangeness, and had given them to me, a boy in his teens, an incipient collector of everything interesting. The grace and beauty of Japanese decorations and utensils; the charm of the scenery as it appeared in pictures; and the attractiveness of the people and the friendliness of those I had met, developed a longing to visit the country and live among them as several of my older cousins had. The strangeness of the hermit people had been learned from the illustrations in the report of Commander Perry's 1 visit, and a familiarity with their [culture] had been gotten from a college mate in the Sheffield Scientific School, Mitsukuri Kakichi, 2 afterwards professor of biology in the university at Tokyo; he was a boy of fine culture who at college could write better English than I. There could be no feeling of aloofness toward a people having the qualities of Mitsukuri, and it was a source of sad regret when I reached Tokyo that my college mate was too ill for me to visit and soon passed away. Dr. Kochibe, formerly director of the Imperial Geological Survey, and I had met in Chicago and afterwards traveled together in Russia; and Professor Kotō 3 of the University of Tokyo had also visited me in Chicago. Japan, as a region of volcanoes, of lordly Fujisan, naturally excited the