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Inventory of geotouristic routes along the southern hills of the Kathmandu Valley

Treść / Zawartość
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
An inventory map of geotouristic sites was prepared on the scale of 1 : 25 000 along the Chandragiri-Chitlang Range, southwestern part of the Kathmandu Valley of central Nepal. From the ridges and peaks of the Chandragiri-Chitlang range, visitors can witness breathtaking views of the surrounding hills, modern buildings, and ancient temples of the Kathmandu Valley from a distance. The objective of the study was to explore the geotouristic sites around the Kathmandu Valley. For this purpose, all the available information related to geology, environment, geography, culture, religion, and other touristic components was reviewed thoroughly, and extensive fieldwork was carried out with the purpose of geological mapping and data collection. The Chandragiri-Chitlang range is a renowned place and open book not only for geologists but also for the nature lover, climbers, trekkers, photographers, videographers, cultural tourists, biologists, and ayurvedic and it has a great prospect for tourism due to its geomorphological variation, unique geological features, beautiful natural scene, unique trekking trails, culture, biodiversity, adventurous way, heritage, and historical sites. Major geotouristic sites, which attract tourists throughout the year in this range are the lush green Chandragiri Hill, Chandragiri Temple with children’s playground and exciting recreational equipment, snowfall, on the winter season, Chitlang Homestay, Chobhar Hill, Taudaha natural pond, Pharping Hill, Champadevi Temple, Gupteshwor cave, Chobhar cave, Thankot, and Matatirtha Temple, etc. Geologically, the study area comprises the lower four geological units of the Phulchoki Group of the Kathmandu Complex from older to younger sequences i.e. the Tistung Formation, the Sopyang Formation, the Chandragiri Limestone, and the Chitlang Formation along with alluvial fan deposits and Kathmandu Lake sediments. The basin of Kathmandu is filled with the lacustrine-fluvial deposits of ancient lakes followed by river deposits. The Chandragiri Thrust, Chitlang Syncline, Kirtipur Anticline are the major regional-scale geological structures within the study area. Unique oldfashioned footrail attracts tourists and increased the charm of traveling in this place. The homestays in Chitlang village, joyful of culture and environment, provide a tranquil retreat away from the bustling crowds of Kathmandu. Preparation of a tourist guidebook and planning and development from the perspective of a geotouristic approach is recommended after this research. Reconstruction and establishment of trekking foot trails and tourist information centers based on currently available natural and human resources without investing high costs can be carried out for sustainable tourism development in this range.
Rocznik
Strony
47--61
Opis fizyczny
Bibliogr. 14 poz., rys., zdj.
Twórcy
  • Central Department of Geology, Tribhuvan University, Kirtipur, Kathmandu, Nepal
  • Central Department of Geology, Tribhuvan University, Kirtipur, Kathmandu, Nepal
Bibliografia
  • [1] Acharya M., & Paudyal K.R., 2019a. Geological setting of the Chandragiri-Chitlang Range, southwest of Kathmandu Valley, central Nepal. Journal of Nepal Geological Society, 58: 199–207. https://doi.org/10.3126/jngs.v58i0.24605.
  • [2] Acharya M., & Paudyal K.R., 2019b. Industrial rocks and minerals in Chandragiri-Chitlang Range, southwest of Kathmandu Valley. Bulletin of Nepal Geological Society, 36: 251–257.
  • [3] Bhote G.R., 2018. Perceptions of Tourism Stakeholders towards Tourism Industry in Nepal. Journal of Business and Social Sciences Research, 1(1): 129–143. https://doi.org/10.3126/jbssr.v1i1.20953.
  • [4] Bulatović D.S.D., 2017. Ecotourism and ecolodge accommodation. ILIRIA International Review, 7(2), 247–260.
  • [5] Dowling R.K., 2011. Geotourism’s global growth. Geoheritage, 3(1): 1–13. https://doi.org/10.1007/s12371-010-0024-7.
  • [6] Drumm A., & Moore A., 2005. Ecotourism development: A manual for conservation planners and managers. Volume l: An introduction to ecotourism planning, second edition. The Nature Conservancy. https://www.researchgate.net/publication/277786951_Ecotourism_Development_-_A_Manual_for_Conservation_Planners_and_Managers_Volume_I_-_An_Introduction_to_Ecotourism_Planning.
  • [7] Gansser A., 1964. Geology of the Himalayas. Interscience Publisher, London.
  • [8] Gautam B.P., 2011. Tourism and economic growth in Nepal. NRB Economic Review, 23(2): 18–30.
  • [9] Joyce E.B., 2006. Geological heritage of Australia: selecting the best for Geosites and World Heritage, and telling the story for geotourism and Geoparks. ASEG Extended Abstracts, 1: 1–4. https://doi.org/10.1071/ASEG2006ab078.
  • [10] Nepal S.K., 2002. Mountain ecotourism and sustainable development: Ecology, economics, and ethics. Mountain Research and Development, 22(2): 104–109.
  • [11] Reynard E., & Brilha J., 2018. Geoheritage: Assessment, Protection, and Management. Elsevier, Amsterdam.
  • [12] Stöcklin J., 1980. Geology of Nepal and its regional frame. Journal of Geology Society of London, 137: 1–34.
  • [13] Stöcklin J., & Bhattarai K.D., 1977. Geology of Kathmandu area and Central Mahabharat Range, Nepal, Himalaya. Unpublished technical report, DMG/UNDP Mineral Exploration Project.
  • [14] Stöcklin J., & Bhattarai K.D., 1982. Photogeological map of part of Central Nepal, scale 1:100,000. U. N. Dev. Program, Tehran.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-54d085e0-2a5d-4c12-a96a-ee703e7ab46d
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