What factors control mechanical erosion rates?

Mechanical erosion rates are important factors in understanding how continents evolve. Mechanical erosion is much faster than chemical erosion, especially for highly elevated regions of the Earth's surface. It is a principal way in which mountain ranges are removed, exposing deep metamorphic roots, which comprise much of the older portions of the continental masses. In addition, there has to be a long-term balance between erosion and mountain building. A new data set allows us to explore in greater detail some of the many factors which control mechanical erosion rates. The most important factors are some expression of the average slope of a drainage basin, some measurement of the amount of water available for erosion, some environmental measurements, and also a measurement of basin length, for which we have no good explanation. The estimate of global mechanical erosion rate obtained here is considerably lower than those obtained by some other workers, some of whom have concentrated on the fact that smaller river basins tend to get eroded faster than larger basins, and it is mainly smaller basins which have not been measured and which are therefore not allowed for by simple arithmetic averaging of observed erosion rates. It is shown here that although smaller basins are eroded faster, this is mainly because they are steeper than larger basins. We also show that extrapolation of current data to smaller basins does not work because the observed continental area which is draining to the ocean cannot be attained by the simplest extrapolation scheme. Received: 23 October 1998 / Accepted: 29 June 1999     

What is responsible for increasing flood risks? The case of Gangwon Province,Korea

We examined the anthropogenic and natural causes of flood risks in six representative cities in the Gangwon Province of Korea. Flood damage per capita is mostly explained by cumulative upper 5% summer precipitation amount and the year. The increasing flood damage is also associated with deforestation in upstream areas and intensive land use in lowlands. Human encroachment on floodplains made these urban communities more vulnerable to floods. Without changes in the current flood management systems of these cities, their vulnerability to flood risks will remain and may even increase under changing climate conditions.     

What is responsible for development of the Asian–Pacific transition zone: The geodynamics of oceanic plates or the Asian continent?

The main unusual feature of tectogenesis of the Asian–Pacific transition zone in the Mesozoic–Cenozoic consists in the formation of left-lateral strike-slip faults, which form the East Asian global shear zone with paragenesis of its constituent variously oriented fault systems. Paragenetic analysis has revealed that continental blocks of the Asian–Pacific transition zone were displaced along systems of transit left-lateral strike-slip faults of the East Asian global shear zone by hundreds of kilometers in the southerly to southwesterly direction due to tectonic activity of the Asian continent, which drifted southwestward. This process was accompanied by the formation of compression and extension structures. Otherwise, it is difficult to explain the structuring of the overhanging margin of the continent by subduction of oceanic lithospheric plates in the northerly to northwesterly direction opposite relative to the displacement of the continental crust as is usually thought.     

Who are we responsible to? Locals’ tales of volunteer tourism

Existing studies have often suggested that volunteer tourism, with strong overtones of “social”, “justice” and “pro-poor” tourism, has the capacity to bring about positive impacts to local communities in host destinations. Wearing, for example, advocates volunteer tourism “as a development strategy leading to sustainable development and centering the convergence of natural resource qualities, locals and the visitors that all benefit from tourism activity” (Wearing, 2001: p. 12). Indeed, underlying assumptions in volunteer tourism suggest that it is a form of tourism that allows the empowering of locals in host-communities, and when compared to conventional modes of tourism, volunteer tourism allows cultural interaction and understanding to be developed between hosts and tourists in the longer period and more intimate form of contact. This, together with very direct and tangible outcomes of volunteer projects, appears to put in place a platform where locals and tourists both have the power to actively negotiate their identities and relations with each other.However, despite these deep-seated assumptions about the positive value in volunteer tourism, little empirical research has been conducted to assess the situation on the ground. Existing literature is largely centered on the volunteer tourist, with little works directly regarding the perspectives of host-communities. This places much uncertainty on whether the assumed benefits of volunteer tourism are indeed realized. Adopting a geographical approach, this paper begins with a review of existing discussions on the geographies of care and responsibility, and its intersections with literature on responsible tourism (of which volunteer tourism is often seen to be a part of). Opinions re-presented in this paper are based on interviews with 14 respondents in Cambodia (including local Cambodians, non-government organizations’ (NGO) and missionary workers that have previously hosted volunteer tourists in Cambodia. This paper thus explores both positive and negative opinions of volunteer tourism from the perspective of host-communities, and endeavors to contribute a balanced discussion to the limited literature regarding host-communities’ perspectives in tourism development.     

What do geologists do when the coronavirus bites? Ideas for educators

The spread of the 2020 Covid-19 pandemic has had a major effect on the way that geologists carry out their work—and particularly those engaged in educating the next generation of geologists. There are a number of resources available, and some, focussed on fostering interest in budding geologists, are presented here.     

Crisis? What crisis? Displacing the spatial imaginary of the fiscal state

This paper argues that there is an immanent and evolving relationship between the prevailing form of taxation and the economic geographies of the state. Despite this, the geographic significance of taxation has been obscured by the language in which its historic transformation tends to be couched. Prevailing fiscal systems tend to be presented as essentially static – institutionally and spatially fixed and routinely inscribed within the fixed boundaries and territories of the ‘sovereign’ fiscal state. Any threat to, or change in the nature or geography of the fiscal state tends to be couched in terms of ‘crisis’ – of negative and discontinuous change. This paper contends that these related and essentially conservative discourses of fiscal geography mask the degree to which fiscal spaces are both multiple and continuously evolving. More importantly, it argues, this fluidity and multiplicity does not threaten the stability and viability of state form, but it is an essential process in its maintenance and reproduction. Running counter to the prevailing discourse of the ‘national economy’, the practice of fiscal geography is an under-analysed but key aspect of the historical evolution and transformation of the imagined geographies of economies.     

What is the ‘Just Transition’?

The ‘just transition’ is a concept receiving more attention in the literature to-date. This critical review discusses this and how there are overlaps with literature on energy, environmental and climate justice. Within the separate energy, environment and climate change scholar communities, there is too much distortion of what the ‘transition’ means and what ‘justice’ means, and they all should be understood within the just transition concept. To increase public understanding and public acceptance of a just transition, these research communities need to unite rather than continue alone.     

Coarse clast ridge sequences as suitable archives for past storm events? Case study on the Houtman Abrolhos,Western Australia

Prehistoric storm records are relatively scarce in most parts of the world. This article presents storm records derived from coral rubble‐based geological archives of the Houtman Abrolhos Archipelago located off the west coast of Australia, where the southernmost coral reefs of the Indian Ocean are found. Winter storm swell from the circum‐Antarctic ‘Brave Westerlies’, as well as tropical cyclone waves, have left numerous ridge systems on dozens of islands of the archipelago, all composed of coral rubble from adjacent reefs. At three islands, seven ridge systems were dated by three different methods: U‐series (68 dates), radiocarbon (64 dates), electron spin resonance (7 dates); 139 radiometric dates span the last 5500 years of the Holocene. In contrast to the geomorphological interpretation, the age sequences show ‘inversions’, hiatuses and different ages for the same ridge, all pointing to complicated ridge formation processes. Time gaps, some exceeding 1000 years, are interpreted as phases of erosion and not as phases without storm activity. Copyright © 2012 John Wiley & Sons, Ltd.     

How Alpine or Himalayan are the Central Andes?

 Although non-collisional mountain belts, such as the Andes, and collisional mountain belts, such as the Alps and the Himalayas–Tibet, have been regarded as fundamentally different, the Central Andes share several features with the Himalayas–Tibet. The most important of these are extremely thickened (≥70 km) continental crustal roots supporting high plateaus and mountain fronts characterized by large basement thrusts. The main prerequisite for very thick crustal roots and extreme mountainous topography appears to be large-scale underthrusting of continental crust of normal thickness, irrespective of whether the crustal thrusts are antithetic with respect to subduction as in the Andes, or synthetic with respect to preceding subduction of oceanic lithosphere as in the Himalayas. In both cases sole thrusts near the base of the continental crust nucleated in thermally anomalous zones of the hinterland and then propagated across ramps into shallower detachments located within thick sedimentary or metasedimentary cover rocks. In contrast to the Central Andes and the Himalayas, the Alps are characterized by intracrustal detachment which allowed both the subduction of lower crust and a stacking of relatively thin upper crustal slivers, which make up a narrow mountain chain with a more subdued topography. Received: 10 August 1998 / Accepted: 1 March 1999     

Why are the continents just so…?

Variations in gravitational potential energy contribute to the intraplate stress field thereby providing the means by which lithospheric density structure is communicated at the plate scale. In this light, the near equivalence in the gravitational potential energy of typical continental lithosphere with the mid‐ocean ridges is particularly intriguing. Assuming this equivalence is not simply a chance outcome of continental growth, it then probably involves long‐term modulation of the density configuration of the continents via stress regimes that are able to induce significant strains over geological time. Following this notion, this work explores the possibility that the emergence of a chemically, thermally and mechanically structured continental lithosphere reflects a set of thermally sensitive feedback mechanisms in response to Wilson cycle oscillatory forcing about an ambient stress state set by the mid‐ocean ridge system. Such a hypothesis requires the continents are weak enough to sustain long‐term (10⁸ years) strain rates of the order of ～10^?17 s^?1 as suggested by observations that continental lithosphere is almost everywhere critically stressed, by estimates of seismogenic strain rates in stable continental interiors such as Australia and by the low‐temperature thermochronological record of the continents that requires significant relief generation on the 10⁸ year time‐scale. Furthermore, this notion provides a mechanism that helps explain interpretations of recently published heat flow data that imply the distribution of heat‐producing elements within the continents may be tuned to produce a characteristic thermal regime at Moho depths.     

What Makes Nearshore Habitats Nurseries for Nekton? An Emerging View of the Nursery Role Hypothesis

Estuaries and other coastal habitats are considered essential for the survival of early life stages of commercial, recreational, and other ecologically important species. While early designations simply referred to habitats with higher densities of juveniles as nurseries, the definition was improved by arguing that contribution per unit area to the production of individuals that recruit to adult populations is greater, on average, in nursery habitats. However, this and related approaches typically consider critical habitats as individual, homogeneous entities that are static in nature and do not specifically incorporate important dynamics that determine nursery function. The latter include environmental variability, estuarine hydrodynamics, trophic coupling, ontogenetic habitat shifts, and spatially explicit usage of habitat patches and corridors within larger seascapes. Subsequent studies have identified important factors that regulate nursery value, and researchers working independently across the globe have not only supported the advances made in defining the processes underlying nursery function but, as set forth in this narrative, have advanced it while suggesting that much work still needs to be done to improve our understanding of the links between juvenile nekton survival and the estuarine-coastal seascape. We discuss the current nursery role hypothesis and the data supporting (or refuting) it along with the implications for management of estuarine habitats for the conservation or restoration of nursery function.     

Top-/bottom-soil ratios and enrichment factors: What do they really show?

High top-/bottom-soil ratios, or high values of “enrichment factors” (EFs), are used as a proof for major anthropogenic impact on the geochemistry of the Earth surface. The idea behind calculating such ratios is that soils taken at depth or “average crust” can provide the geochemical background for the soils collected at the Earth surface. However, a soil profile is not a closed system, element exchange between the different layers, depending on and varying with the chemical properties of the different elements, and their turnover in the biosphere is the essence of soil formation. High top-/bottom-soil ratios, or EFs, may thus highlight the geochemical de-coupling of the lithosphere from the biosphere rather than contamination. This is demonstrated by using regional data from 258 soil O- and B-horizon samples collected from the Czech Republic (76,800 km²). Results show no relationship between the ratios and the magnitude of anthropogenic emissions. The visible relationship between element concentrations and sources in a map of the spatial distribution of the elements is lost when maps for the top-/bottom-soil ratio or EFs are constructed. The value of the data lies in the spatial elemental distribution, and not in ratios calculated based on misconceptions.     

How global are the Jurassic–Cretaceous unconformities?

The reality of the global‐scale sedimentation breaks remains controversial. A compilation of data on the Jurassic–Cretaceous unconformities in a number of regions with different tectonic settings and character of sedimentation, where new or updated stratigraphic frameworks are established, permits their correlation. Unconformities from three large reference regions, including North America, the Gulf of Mexico, and Western Europe, were also considered. The unconformities, which encompass the Jurassic‐Cretaceous, the Lower–Upper Cretaceous and the Cretaceous–Palaeogene transitions are of global extent. Other remarkable unconformities traced within many regions at the base of the Jurassic and at the Santonian–Campanian transition are not known from reference regions. A correlation of the Jurassic–Cretaceous global‐scale sedimentation breaks and eustatic curves is quite uncertain. Therefore, definition of global sequences will not be possible until eustatic changes are clarified. Activity of mantle plumes is among the likely causes of the documented unconformities.     

What drives low-carbon consumption behavior of Chinese college students? The regulation of situational factors

Carbon dioxide contributes about 90% of global warming, which is mainly generated by residents’ daily consumption activities. This article explores the factors of low-carbon consumer behavior among college students and situational factors which contribute to explain intention–behavior gap. Combined with the existing research literature and the Model of Responsible Environmental Behavior, a model of the factors of Chinese college students’ low-carbon consumption behavior was constructed through a sample survey of college students in Jiangsu Province. Analysis results show that (1) College students’ low-carbon behavior intention has a significant positive effect on low-carbon consumption behaviors; (2) Attitudes, emotions, and habits indirectly affect low-carbon consumer behaviors through low-carbon behavior intention; (3) Low-carbon behavior ability and habits can also affect low-carbon consumption behaviors in a direct way; (4) The study of situational factors found that policies and regulations, economic costs, goals and feedback, and social norms have a significant regulating effect in the process of low-carbon behavior intention which has an impact on low-carbon consumption behaviors; (5) In terms of demographic factors, gender and education have a significant effect on low-carbon consumption behavior. Finally, this article discusses the policy measures to guide college students’ low-carbon consumption behavior from the government and the school level, respectively, and place a high hope on college students who can positively influence the entire social group to carry out low-carbon consumption and achieve the realization of China’s low-carbon goals.