Identyfikatory
Warianty tytułu
Języki publikacji
Abstrakty
Geoconservation enhances tourist knowledge of a site’s geology, going beyond surface appreciation. Geotourism emphasizes geology and landscape, contributing to geodiversity conservation through various activities. While the Pokhara Ghandruk area in Gandaki Province is renowned for tourism, it remains unexplored from a geotourism perspective. The study focuses on identifying key geoconservation and geotourism sites for national economic development by systematic geological survey with map preparation highlighting distinctive geological, geomorphic, cultural, heritage and site-seeing features of each site. The region boasts several significant sites, such as Pokhara Valley known for its caves, lakes, and the Seti River gorge. Pokhara canyoning provides thrilling water geoadventures on quartzite cliffs. Naudanda offers breathtaking views of Pokhara Valley and the Annapurna range. Poon Hill and Khumai Danda serve as stunning vantage points for observing snow-capped mountains. The Mardi and Annapurna trek routes, along with Ghandruk Landruk Lwang Dhampus, offers geologically significant sites, including unique rock outcrops due to its passage through the Mahabharat Thrust and the Main Central Thrust (MCT) and exhibit potentiality for rock climbing centers, hot springs, and geocultural parks capitalizing on Gurung hospitality and rich traditions to boost tourism and preserve geoheritage. The study recommends the establishment of geotrails and a geopark within this region.
Słowa kluczowe
Czasopismo
Rocznik
Tom
Strony
71--82
Opis fizyczny
Bibliogr. 16 poz., rys., zdj.
Twórcy
autor
- Central Department of Geology, Tribhuvan University, Kirtipur, Kathmandu, Nepal
autor
- Central Department of Geology, Tribhuvan University, Kirtipur, Kathmandu, Nepal
Bibliografia
- [1] Acharya M. & Paudyal K.R., 2023. Inventory of geotouristic routes along the southern hills of the Kathmandu Valley. Geotourism/ Geoturystyka, 3–4(66–67): 47–61. https://doi.org/10.7494/geotour.2021.3-4(66-67).47.
- [2] 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.
- [3] Dewey J.F. & Bird J.M., 1970. Mountain belts and the new global tectonics. Journal of Geophysical Research, 75(14): 2625–2647. https://doi.org/10.1029/jb075i014p02625.
- [4] Drumm A. & Moore A., 2005. Ecotourism Development: A Manual for Conservation Planners and Managers. Volume I: An Introduction to Ecotourism Planning (2nd ed.). The Nature Conservancy, Arlington, VA. https://www.researchgate.net/publication/277786951_Ecotourism_Development_-_A_Manual_for_Conservation_Planners_and_Managers_Volume_I_-An_Introduction_to_Ecotourism_Planning.
- [5] Gautam B.P., 2011. Tourism and economic growth in Nepal. NRB Economic Review, 23(2): 18–30. https://doi.org/10.3126/nrber.v23i2.52743.
- [6] Hashimoto S., Ohta Y. & Akiba C., 1973. Geology of Nepal Himalayas. Saikon, Tokyo.
- [7] Le Fort P., 1975. Himalayas: the collided range. Present knowledge of the continental arc. American Journal of Science, 275(1): 1–44.
- [8] Paudel L.P. & Arita K., 1998. Geology, structure and metamorphism of the Lesser Himalayan metasedimentary sequence in Pokhara region, western Nepal. Journal of Nepal Geological Society, 18: 97–112. https://doi.org/10.3126/jngs.v18i0.32202.
- [9] Reynard E. & Brilha J., 2018. Geoheritage: Assessment, Protection, and Management. Elsevier, Amsterdam. https://doi.org/10.1016/C2015-0-04543-9.
- [10] Sakai H., 1983. Geology of the Tansen Group of the Lesser Himalaya in Nepal. Memoirs of the Faculty of Science, Kyushu University (Japan). Series D, Geology, 25(1): 27–74. https://doi.org/ 10.5109/1546083.
- [11] Stöcklin J., 1980. Geology of Nepal and its regional frame. Journal of Geology Society of London, 137(1): 1–34. https://doi.org/10.1144/gsjgs.137.1.0001.
- [12] Stöcklin J. & Bhattarai K., 1977. Geology of the Kathmandu area and central Mahabharat range, Nepal Himalaya. Report of Department of Mines and Geology/UNDP [unpublished].
- [13] Thapa D., Paudyal K.R., Sah R.B., Dhungana U. & Chetri R.K., 2023. A revised Quaternary stratigraphy in and around Pokhara valley, Gandaki province, Nepal. Himalayan Geology, 44(2): 89–103.
- [14] Upreti B.N. & Le Fort P., 1999. Lesser Himalayan crystalline nappes of Nepal: Problem of their origin. In: Macfarlane A., Quade J. & Sorkhabi R. (eds), Himalaya and Tibet: Mountain roots to mountain tops, Special Paper, 328, Geological Society of America, Boulder, CO, 225–238. https://doi.org/10.1130/0-8137-2328-0.225.
- [15] Valdiya K.S., 1980. The two intracrustal boundary thrusts of the Himalaya. Tectonophysics, 66(4): 323–348. https://doi.org/10.1016 0040-1951(80)90248-6.
- [16] Yin A., 2006. Cenozoic tectonic evolution of the Himalayan orogen as constrained by along-strike variation of structural geometry, exhumation history, and foreland sedimentation. Earth-Science Reviews, 76(1–2): 1–131. https://doi.org/10.1016/j.earscirev.2005.05.004.
Uwagi
Opracowanie rekordu ze środków MNiSW, umowa nr POPUL/SP/0154/2024/02 w ramach programu "Społeczna odpowiedzialność nauki II" - moduł: Popularyzacja nauki i promocja sportu (2025).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-bc9c73c8-2bf4-470d-92cb-44d9a4adc7b0
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