Tourism planning and place making: place-making or placemaking?

ABSTRACT

Tourism destination planning and marketing are fundamentally place making actions intended to shape the image and imageability of a place. Place making is an innate human behavior, ranging from the organic and unplanned actions of individuals, defined here as ‘place-making,’ to planned and intentional global theming by governments and tourism authorities, defined here as ‘placemaking.’ Place-making and placemaking are ends on a continuum of options, with most places have a mix of local and global elements. These elements also range from the tangible (base in urban design) to the intangible (peoplescapes and imaginations). The tools of place making are essentially the same for both organic place-making and planned placemaking, but the intentions and outcomes can vary enormously. Tourism development, as an economic activity, almost always has a neoliberal planned placemaking agenda. Organic place-making emerges through individual agency, which if allowed to proceed, will make its imprint even in a heavily master planned tourism landscape. An understanding of place-making and placemaking gives insight into research questions on the political economy of tourism and the roles of hosts and guest in co-producing tourism places. Examining the elements of place making in a tourism landscape can more clearly identify how different worldview perspectives have contribute over time to the making of tourism places, and thereby assist in planning for the future development of destination communities.     

Beyond the everyday? Rethinking place meanings in tourism

ABSTRACT

Existing tourism scholarship on place meanings seems to retain an underlying assumption of a contradiction between tourist places and the mundane world. In contrast, this paper contends that the production of the meanings of tourist places is also closely related to everyday life. To make its case, it interrogates the creation of meanings of two scenic sites of Tianya Haijiao and Nanshan in Sanya, a famous coastal destination in southern China. Although both scenic sites have been recently developed, their significance stems from historical and cultural meanings in traditional Chinese culture, which are frequently communicated in people's daily conversations and practices. Besides, the meanings of the tourist sites are neither fixed by legitimate discourses nor dominated by tourism publicity; they are continuously shaped by wider socio-spatial events in mundane societies and re-interpreted through tourism mobilities in accordance with tourists’ everyday concerns. This paper echoes the ‘new mobilities turn’ in tourism studies and contributes to the discussions of the mundaneness of tourist places.     

An experimental and modeling study of Na-rich hydrothermal alteration

Sodic alteration assemblages including clinoptilolite, mordenite, analcime and Na‐montmorillonite were locally observed in sediments in the eastern part of the Hachimantai geothermal region, northeast Japan. This study investigated the mechanisms of sodic enrichment in the sediments during alteration. Kinetic results for water/rock interaction experiments are reported here. Batch‐type experiments were conducted at 150–250°C under saturated vapor pressure. Pyroclastic rocks dissolved incongruently in these experiments, and the solubility and dissolution rates among elements varied as follows: the apparent steady‐state concentrations of major elements are Si > Na ? K > Ca > Al and the order of the dissolution rates is Si > Al > Na ? K > Ca. Na had the highest steady‐state concentration and fastest dissolution rate of the alkali and alkali earth metal ions. Based on surface analysis of plagioclase, dissolution was effected via a reaction layer of Na‐montmorillonite on the mineral surface. Additionally, a reaction model constructed based on the experimentally observed reaction mechanism quantitatively explains the dissolution behavior. These results show that Na‐montmorillonite can be precipitated by pyroclastic rock/meteoric water interactions without seawater involvement: the Na is derived from the host rocks.