Commenced in January 2007
Frequency: Monthly
Edition: International
Paper Count: 33093
Changing Geomorphosites in a Changing Lake: How Environmental Changes in Urmia Lake Have Been Driving Vanishing or Creating of Geomorphosites
Authors: D. Mokhtari
Abstract:
Any variation in environmental characteristics of geomorphosites would lead to destabilisation of their geotouristic values all around the planet. The Urmia lake, with an area of approximately 5,500 km2 and a catchment area of 51,876 km2, and to which various reasons over time, especially in the last fifty years have seen a sharp decline and have decreased by about 93 % in two recent decades. These variations are not only driving significant changes in the morphology and ecology of the present lake landscape, but at the same time are shaping newly formed morphologies, which vanished some valuable geomorphosites or develop into smaller geomorphosites with significant value from a scientific and cultural point of view. This paper analyses and discusses features and evolution in several representative coastal and island geomorphosites. For this purpose, a total of 23 geomorphosites were studied in two data series (1963 and 2015) and the respective data were compared and analysed. The results showed, the total loss in geomorphosites area in a half century amounted to a loss of more than 90% of the valuable geomorphosites. Moreover, the comparison between the mean yearly value of coastal area lost over the entire period and the yearly average calculated for the shorter period (1998- 2014) clearly indicates a pattern of acceleration. This acceleration in the rate of reduction in lake area was seen in most of the southern half of the lake. In the region as well, the general water-level falling is not only causing the loss of a significant water resource, which is followed by major impact on regional ecosystems, but is also driving the most marked recent (last century) changes in the geotouristic landscapes. In fact, the disappearance of geomorphosites means the loss of tourism phenomenon. In this context attention must be paid to the question of conservation. The action needed to safeguard geomorphosites includes: 1) Preventive action, 2) Corrective action, and 3) Sharing knowledge.Keywords: Changing lake, environmental changes, geomorphosite, northwest of Iran, Urmia lake.
Digital Object Identifier (DOI): doi.org/10.5281/zenodo.1107029
Procedia APA BibTeX Chicago EndNote Harvard JSON MLA RIS XML ISO 690 PDF Downloads 1709References:
[1] Fars news agency. com
[2] D. Newsome, S.A. Moore, R.K. Dowling,. Natural Area Tourism: Ecology, Impacts and Management (2nd edn). Channel View Publications, Clevedon, England. 2013.
[3] UNEP- GEAS, The drying of Iran’s Lake Urmia and its environmental consequences. Environmental Development 2, 2012, pp. 128 –137.
[4] D. A. Vasiljević, S.B. Marković, T.A. Hose, Z.L. Ding, Z.T. Guo, X. M. Liu, I. Smalley, T. Lukić, M. D. Vujičić, Loess-palaeosol sequences in China and Europe: Common values and geoconservation issues. Catena 117, 2014, pp. 108-118.
[5] R. Buckley, Tourism and environment. Annual Review of Environment and Resources, 36. doi:10.1146/annurev-environ-041210-132637E., 2011
[6] J. Jedari Eyvazi, Geomorphology of. Payame-Noor Pub. 2011.
[7] Y. Ghavidel Rahimi, The effect of Remote communication link of the NAO on the annual rainfall anomalies in the basin of Lake Urmia. Journal of Humanities and Social Sciences, No. 10. 2005.
[8] A. M. Khourshiddoost, Y. Ghavidel Rahimi, R. Saniee, T. Yasari, H. Nouri, Analysis of the role of the NAO phenomenon in annual fluctuations in the Urmia lake basin. Geographical space, No. 19. 2007.
[9] M. Delavar, S. Morid, M. Shafieefar, Risk assessment of the level of Lake Urmia and impact of climate change on it. Agricultural Sciences, 39 (2), 2008, pp.379-388.
[10] R. Lak, J. Darvishi Khatooni, A. Mohammadi, PalaeoLimnology Studies and causes of sudden decrease in lake water level. Applied Geology, 7 (4), 2001, pp. 343-358.
[11] M. Abbaspour, A. H. Javid, S. A. Mirbagheri, F. A. Givi, P. Moghimi, Investigation of lake drying attributed to climate change. International Journal of Environmental Science and Technology 9 (2), 2012, pp. 257- 266.
[12] A. H. Delju, A. Ceylan, E. Piguet, M. Rebetez, Observed climate variability and change in Urmia Lake Basin, Iran.Theoretical and Applied Climatology, 2012, pp. 1-12.
[13] P. Rahimzadeh Bajgiran, A. A. Darvishsefat, A. Khalili, M. F. Makhdoum, Using AVHRR-based vegetation indices for drought monitoring in the Northwest of Iran. Journal of Arid Environments 72, 2008, pp. 1086 – 1096
[14] S. Farzin, P. Ifaei, N. Farzin, Y. Hassanzadeh, M. T. Aalami, An investigation on changes and prediction of Urmia lake water surface evaporation by chaos theory.International Journal of Environmental Research 6 (3), 2012, pp. 815-824
[15] J. Nikbakht,H. Tabari, P. H. Talaee, Streamflow drought severity analysis by percent of normal index (PNI) in northwest Iran.Theoretical and Applied Climatology, 2012, pp. 1-9.
[16] S. Khalighi Sigaroodi, S. Ebrahimi, Effects of land use change on surface water regime (Case study Orumieh Lake of Iran. Procedia Environmental Sciences 2, 2010, pp. 256–261.
[17] D. Mokhtari., F. Karami, M. Bayati Khatibi, Different forms of alluvial fans around the Mishow mountain (North West of Iran), with emphasis on the role of Quaternary tectonic activities in their creation. Quarterly Journal of Humanities, No. 53, 2007, pp. 257.
[18] M. Rajabi, C. Aqhajani, Evaluation of faults, earthquake generating power and seismic hazard on alluvial fans in the North East of Lake Urmia. Physical Geography, 3 (7), 2010, pp. 1-14.