Geological dimension of the cultural heritage: A case example of the Ajanta Caves (Maharashtra, India)
Main Article Content
Abstract
International development for the both geoconservation and geotourism requires attention to all kinds of (potential) geological heritage. The Ajanta Caves (western Maharashtra, India) is a famous cultural object consisting of 30 caves carved in the Deccan Traps and inscribed to the UNESCO list of the World Heritage Sites. Its examination permits to indicate four geological features, which are the artificial caves themselves (these mark geological activity of the man in the historical past), the end-Cretaceous floot basalts (these demonstrate the emplacement of Large Igneous Province and the relevant palaeoenvironmental catastrophe), the gorge of the Waghora River (this is peculiar landform resulted from the river erosion of hard rocks), and the rockfall hazard (this is an interesting engineering geological phenomenon linked to the caves construction/maintenance). Geological heritage value of these features is argued. Unfortunately, there is not any geotourism activity at the Ajanta Caves presently. The content analysis of the principal on-line resources (web pages) devoted to this cultural site reveals the absence of sufficient geological information that would facilitate geotourism. Generally, judgements about the Ajanta Caves and the other similar sites in the geological dimension permit to consider the wide spectrum of the geological heritage. They also highlight some extra opportunities for geotourism, which can benefit by its development at cultural sites with thousands of visitors.
Keywords:
Downloads
Article Details
References
Abbott, D.H., Isley, A.E. (2002). The intensity, occurrence, and duration of superplume events and eras over geological time. Journal of Geodynamics, 34: 265-307.
Alvarez, W. (2008). T. rex and the Crater of Doom. Princeton University Press, Princeton, 185 pp.
Ansari, M.K., Ahmad, M., Singh, R., Singh, T.N. (2014). Rockfall hazard assessment at Ajanta Cave, Aurangabad, Maharashtra, India. Arabian Journal of Geosciences, 7: 1773-1780.
Baksi, A.K. (2014). The Deccan Trap – Cretaceous–Paleogene boundary connection; new 40Ar/39Ar ages and critical assessment of existing argon data pertinent to this hypothesis. Journal of Asian Earth Sciences, 84: 9-23.
Bondre, N.R., Duraiswami, R.A., Dole, G., Phadnis, V.M., Kale, V.S. (2000). Inflated Pahoehoe lavas from the Sangam ner area of the western Deccan volcanic province. Current Science, 78: 1004-1007.
Bondre, N.R., Duraiswami, R.A., Dole, G. (2004). Morphology and emplacement of flows from the Deccan volcanic province, India. Bulletin of Volcanology, 66: 29-45.
Courtillot, V. (2007). Evolutionary catastrophes the science of mass extinction. Cambridge University Press, Cambridge, 173 pp.
Courtillot, V.E., Renne, P.R. (2003). On the ages of flood basalt events. Comptes Rendus Geosciences, 335: 113-140.
Dowling, R., Newsome, D. (2010). Geotourism: a Global Activity. In: Dowling, R. & Newsome, D. (Eds.). Global geotourism perspectives. Goodfellow Publishers, Woodeaton, pp. 1-17.
Gordon, J.E. (2012). Rediscovering a Sense of Wonder: Geoheritage, Geotourism and Cultural Landscape Experiences. Geoheritage, 4: 65-77.
Goudie, A. (2002). Aesthetics and relevance in geomorphological outreach. Geomorphology, 47: 245-249.
Goudie, A. (2013). The Human Impact on the Natural Environment: Past, Present and Future. Wiley-Blackwell, Chichester, 410 pp.
Gray, M. (2013). Geodiversity: Valuing and conserving abiotic nature. Wiley-Blackwell, Chichester, 495 pp.
GSI. (2001). Geoscientific studies for the conservation of Ajanta Caves. Report Submitted by the Central region of GSI, Nagpur.
Guzzetti, F. (2013). Rockfall. In: Bobrowsky, P.T. (Ed.). Encyclopedia of Natural Hazards. Springer, Dordrecht, pp. 875-877.
Hallam, A., Wignall, P.B. (1997). Mass extinctions and their aftermath. Oxford University Press, Oxford, 320 pp.
Hooke, R. Le B. (2000). On the history of humans as geomorphic agents. Geology, 28: 843-846.
Hose, T.A. (2000). European ‘geotourism’geological interpretation and conservation promotion for tourists. In: Barettino, D., Wimbledon, W.A.P., Gallego, E. (Eds.). Geological heritage: its conservation and management. ITGE, Madrid, pp. 127-146.
Hose, T.A., Vasiljević, D.A. (2012). Definig the nature and purpose of modern geotourism with particular reference to the United Kingdom and south-east Europe. Geoheritage, 4: 25-43.
Jerram, D.A., Widdowson, M. (2005). The anatomy of Continental Flood Basalt Provinces: geological constraints on the processes and products of flood volcanism. Lithos, 79: 385-405.
Keller, G. (2003). Biotic effects of impacts and volcanism. Earth and Planetary Science Letters, 215: 249-264.
Keller, G., Adatte, T., Gardin, S., Bartolini, A., Bajpai, S. (2008). Main Deccan volcanism phase ends near the K-T boundary: Evidence from the KrishnaGodavari Basin, SE India. Earth and Planetary Science Letters, 268: 293-311.
Lubova, K.A., Zayats, P.P., Ruban, D.A., Tiess, G. (2013). Megaclasts in geoconservation: sedimentological questions, anthropogenic influence, and geotourism potential. Geologos, 19: 321-335.
Migon, P. (2009). Geomorphosites and the World Heritage List of UNESCO. In: Reynard, E., Coratza, P. & Regolini-Bissig, G. (Eds.). Geomorphosites. F. Pfeil, München, pp. 119-130.
Necheć, I.-M., Erdeli, G. (2014). Geolandscapes and Geotourism: Intergrating Nature and Culture in the Bucegi Mountains of Romania. Landscape Research. doi: https://doi.org/10.1080/01426397.2014.939616.
Panizza, M., Piacente, S. (2009). Cultural geomorphology and geodiversity. In: Reynard, E., Coratza, P. & Regolini-Bissig, G. (Eds.). Geomorphosites. F. Pfeil, München, pp. 35-48.
Poria, Y., Reichel, A., Cohen, R. (2013). Tourists perceptions of World Heritage Site and its designation. Tourism Management, 35: 272-274.
Prosser, C.D. (2013). Our rich and varied geoconservation portfolio: the foundation for the future. Proceedings of the Geologists' Association, 124: 568-580.
Rana, R.S., Vishwakarma, L.L. (1990). Occurrence of artesian conditions in the Sina river basin of drought prone Karjat Taluka, Ahmednagar district in Maharashtra. In: Proceedings of the all Indian seminar on modern techniques of rainwater harvesting, water conservation and artificial recharge for drinking water, afforestation, horticulture and agriculture. Groundwater Survey and Development Agency (GSDA), Pune, pp. 207-213.
Ruban, D.A. (2010). Quantification of geodiversity and its loss. Proceedings of the Geologists’ Association, 121: 326-333.
Ruban, D.A. (2013). Geokonservatsionnyj aspekt nedropol’zovanija: ob’ekty geologitcheskogo nasledija i vzaimosvjaz’ ikh tipov [Geoconservation aspect of the interiors exploitation: geological heritage objects and combination of their types]. Nedropol’zovanie XXI vek, 2: 108-113. (in Russian)
Ruban, D.A., Kuo, I. (2010). Essentials of geological heritage site (geosite) management: a conceptual assessment of interests and conflicts. Natura Nascosta, 41: 16-31.
Su, Y.-W., Lin, H.-L. (2014). Analysis of international tourist arrivals worldwide: The role of world heritage sites. Tourism Management, 40: 46-58.
Tang, C.M. (2000). Ugly Fossil Syndrome. Palaios, 15: 175-176.
Vajda, V., Bercovici, A. (2014). The global vegetation pattern across the Cretaceous–Paleogene mass extinction interval: A template for other extinction events. Global and Planetary Change, 122: 29-49.
Walker, G.P.L. (1971). Compound and simple lava flows and flood basalts. Bulletin of Volcanology, 35: 579-590.
Wignall, P.B. (2001). Large igneous provinces and mass extinctions. Earth-Science Reviews, 53: 1-33.
Wilkinson, B.H. (2005). Humans as geologic agents: A deep-time perspective. Geology, 33: 161-164.
Wimbledon, W.A.P., Smith-Meyer, S. (Eds.) (2012). Geoheritage in Europe and its conservation. ProGEO, Oslo, 405 pp.
Yang, C.-H., Lin, H.-L., Han, C.-C. (2010). Analysis of international tourist arrivals in China: The role of World Heritage Sites. Tourism Management, 31: 827-837.