Abstract

By the example of Tara National Park (NP), we present how the geoheritage can and should be presented in a NP where the primary role is played by biology. Tara NP has a rich geoheritage, especially its karst phenomena, which include gorges (e.g. the 1000-m-deep Drina Gorge), plateaus with dolines, dry valleys, and uvalas as well as springs and travertines. In addition, ophiolites also enrich the geoheritage; hence, the area has a high geodiversity. Large reservoirs of the territory provide an opportunity to study the anthropogenic impact on hydrology and geomorphology. After presenting the geoheritage elements of the area, we examine the views and knowledge of local people and visitors about karst and geotourism with the help of a questionnaire survey. The results show that local residents support the further development of tourism, but geotourism is a rather new concept for them. On the contrary, tourists are more familiar with geotourism. Among the development perspectives, tourists support those that involve only minor environmental changes, that is in agreement with NP policy. Finally, we formulate some suggestions about geotourism development in the area. First, we outline some plans for new geo-educational trails and viewpoints. Second, we highlight the possibility to increase the geo-content of some already existing programs (e.g. boat tours). Third, we emphasize that geotourism of Tara should be connected to neighbouring areas. A new geopark is already under planning, which would include the area of Tara NP as well.

Highlights

  • Tara National Park (NP) in western Serbia was established in 1981

  • Tara NP is a protected area where the primary role is played by the preservation of biological values, and forestry plays a key role in the NP’s budget

  • One is that local residents unambiguously support the further development of tourism, and they expect the help of the NP in this issue

Read more

Summary

Introduction

The most important aspect of the designation was that there are few settlements in the area, which is largely made up of karst plateaus, mostly covered by mixed forest (PicetoAbieti-Fagetum association is dominant), with high biodiversity and many endemic species. Among the forest species, the endemic and relict Serbian (Pančić) spruce (Picea Omorika) is the most special, which was described from here (Pančić 1876; Blagojević 2012). The geoheritage of the area is rich in significant values, the most important of which, but by no means exclusive, are the forms and phenomena related to karstification (Zeremski 1956; Milić 1980; Radović et al 2005; Blagojević 2012).

Objectives
Methods
Results
Discussion
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call