Morphometric study of landslide monitoring using remote sensing (Case Study Hardang Village South West Isfahan Province)
Subject Areas : Climatology
1 - Assistant professor of geomorphology, Islamic azad university, maybod branch, maybod, iran
Keywords: landslide, morphometric, village Hardang,
Abstract :
Landslide is one of natural hazards that cause fatality, compensation and natural resources damages. By combination of natural and human factors, the event of geomorphic transport processes is occurred by instability condition of hillside. The aim of this study was to Morphometry and determining heave and evaluating changes of an old active landslide in Hardang area which is located 75 kilometers from southern west of Isfahan Province. Various types of hillside instability have been seen in the region, and one of the giant heave is a coluvial near the Hardong village which has been greatly threatening the village. Investigation of Morphometry of the phenomenon and determining the mechanism of these heaves will guide us to control and prevent risks. To assessing the land slide, the scale of heave was determined using aerial photographs of the two periods in 1334 and 1370. Then, the landslide scale at the present time was determined using field works, Google Earth and GIS software. The changes of land slide can be evaluated by comparing the size and volume of the landslide. The results of this study indicates that average heave of this land slide in duration of 56 years was about 32/837 centimeters in year and differences in length, width, perimeter, area and volume of this landslide since 1334 to 1390 the upside is increased (respectively, from 18/389 to 885235/316 cubic meters) indicates that the rotational motion is translational landslides during these years.
1- امیدوار،ابراهیم و عطا الله کاویان، (1389)، برآورد حجم زمین لغزش بر پایه مساحت در مقیاس منطقه ای (بررسی موردی: استان مازندران)، نشریه مرتع و آبخیزداری ، مجله منابع طبیعی ایران، دوره 63، شماره 4، زمستان 89، 439-455.
2- شادفر، ص و همکاران، 1384، پهنه بندی خطر زمین لغزش در حوضه آبخیز لاکتراشان، نشریه علمی ترویجی حفاظت آب و خاک، شماره 1.
3- مهدوی فر،محمد رضا، 1376، پهنه بندی خطر زمین لغزش منطقه خورش رستم (جنوب غربی شهرستان خلخال)، پایان نامه کارشناسی ارشد زمین شناسی مهندسی، دانشگاه تربیت مدرس، تهران.
_||_1- Abele, G., 1974. Bergsturze in den Alpen – ihre Verbreitung, Morphologie und Folgeerscheinungen, Wiss. Alpenvereinshefte, 25,p 247.
2- Avanzi, G.D., Giannecchini, R., and Pucchnelli, A. 2004. The influence of the geological and geomorphological settings on shallow landslides.An example of a temperate climate environment: The June 19,1996 event in northwestern Tuscany (Italy). Engineering geology, 73:215-228.
3- Ayalw, L., Ymagishi, H., and Kanno, T. 2005. Landslides in Sado island of Japan : part II. GIS- based susceptibility mapping with comparisons of results from two methods and verifications. Engineering Geology, 81:432-445.
4- Bonnard, Ch., and Noverraz, F. 2001.Influence of climate change on large landslides: assessment of long term movements and trends. P 121-138, Proceeding of the International Conference on Landslides: causes impact and countermeasures, Gluckauf, Essen, Davose
5- Brand, E.W., Premchitt, J., and Phillipson, H.B. 1984. Relationship between rainfall and landslides in Hong Kong. P 377-384, Procceeding of the IV International Symposium on Lndslides,Toronto.
6- Cancelli, A., and Nova, R. 1985. Landslides in soil debris cover triggered by rainstorm in Valtellina (Central Alps, Italy). P 267-272, Proceeding of the IV International Conference on Landslides, Tokyo. Rotterdam.
7- Cannon, S.H., and Ellen, S.D. 1985. Rainfall conditions for abundant debris avalanches, San Francisco Bay region, California Geology. 38:12. 267-272.
8- Chau,K.T., Sze, Y.L., Fung, M.K., W.Y., Fong, E.L., and Chan, L.C.2004. Landslide hazard analysis for hong kong using landslide inventory and GIS. Computers and Geosciences, 30: 429-443.
9- Garfi, G., and Bruno, D.E. 2007. Fan morfodynamics and slop instsbility in the Mucone River basin (Sila Massif, southern Italy): significant of wealthering and role of land use changes. Catena, 50:181-196.
10- Guthrie, R.H., Evans, S.G., 2004a. Analysis of Landslide frequencies and characteristics in a natural system, coastal British Columbia. Earth Surface Processes and Landforms 29,1321-1339.
11- Guzzetti, F., Ardizzone, F., Cardinali, M., Galli, M., Reichenbach, P., Rossi, M., 2008. Distribution of landslides in the Upper Tiber River basin, central Italy. Geomorphology 96, 105-122.
12- Guzzetti, F., Ardizzone, F., Cardinali, M., Rossi, M., Valigi,D., 2009. Landslide volumes and landslide mobilization rates in Umbria, central Italy, Earth and Planetary Science Letters, vol. 279,pp. 222–229.
13- Hovius,N., Stark, C.P., Allen, P.A., 1997. Sediment flux from a mountain belt derived by Landslide mapping. Geology 25, 231-234.
14- Imaizumi, F., Sidle, R.C., 2007.Linkage of sediment supply and transport processes in Miyagawa Dam catchment, Japan. Journal Geophsical Research 112 (F03012). doi: 10.1029.2006JF000495.
15- Imaizumi, F., Sidle, R.C., Kamei, R., 2008. Effects of forest harvesting on the occurrence of landslide and debris flows in steep terrain of central Japan. Earth Surface Processes and Landforms 33, 827-840. doi:10.1002/esp.1574.
16- Innes, J.N., 1983. Lichenometric dating of debris-flow deposits in the Scottish Highlands. Earth Surface Processes and Landforms 8,579-588.
17- Kanungo, D.P., Arora, M.K., Sarcar, S., and Gupta, R.P. 2006. A comparative study of conventional, ANN black box, fuzzy and combined neural and fuzzy weighting procedures for landslide susceptibility zonation In Darjeeling Himalayas. Engineering Geology, 85:347-366.
18- Korup,O.,2005b.Distribution of landslides in southwest New Zealand. Landslides 2,43-51.
19- Malamud, B.D., Turcotte, D.L., Guzzetti,F., Reichenbach, P. 2004a. Landslide inventories and their statistical properties. Earth Surface Processes and Landforms 29, 687-711.
20- Martin, Y., Rood, K., Schwab, J.W., Church, M., 2002. Sediment transfer by shallow landsliding in the Queen Charlotte Islands, British Columbia. Canadian Journal of Earth Sciences 39 (2), 189–205.
21- Morgan, B.A., Wieczorek, G.f., Campbell, R.H., and Gori, P.L.1997. Debris flow hazards in areas affected by the June 27,1995 storm in Madison County, Virginia. USGS Open File Report, 97-438.
22- Paronuzzi, P., Del Fabbro, M., and Maddaleni, P. 2002. Frane superficialitipo slide debris flow causate dal nubifragio del 21/22 giugno 1996 nella Val Chiarso (Alpi Carniche, Friuli). Memorie della Societa Geologica Italiana, 57: 443-452.
23- Peart, M.R., Ng,K.Y., and Zhang, D.D. 2005. Landslides and sediment delivery to a drainage system: some observations from Hong Kong. Asian Earth Sciences, 25:821-836.
24- Polloni, G., Ceriani, M., Lauzi, S., Padovan, N., and Crosta, G. 1992. Rainfall and soil slipping events in Valtellina. P183-188, In Proc. Of the VI International Symposium on Landslides. Christchurch.
25- Remondo. J., Bonachea. J., Cendrero. A/2 (2007). Quantitative landslide risk assessment and mapping on the basis of resent occurrences, Geomorphology, Vol 8.
26- Rice,R.M., Corbett, E.S., Bailey, R.G., 1969. Soil slips related to vegetation, topography, and soil in Southern California. Water Resources Research 5 (3), 647-659.
27- Rice, R.M., Foggin III, G.T., 1971. Effects of high intensity storms on soil slippage on mountainous watersheds in Southern California. Water Resources Research 7(6),1485-1496.
28- Simonett, D.S., 1967. Landslide distribution and earthquakes in the Bewani and Torricelli Mountains, New Guinea. In: Jennings,J .N., Mabbutt,J.A. (Eds.), Landform Studies from Australa and New Guinea. Cambridge University Press, Cambridge, pp. 64-84.
29- Singhrory, V., Glenn, N., and Ohkura, H. 2004. Landslide hazard team report of the CEOS disaster management support group. CEOS Disaster Information Server. National Academy Press, Washington, D.C. Pp: 130-132
30- Soeters, R., and Van Westen, CJ. 1996. Slope instability recognition, analysis and zonation. In: Keith, T.A, Schuster, R.L. (eds.), Landslide investigation and mitigation. Special Report, 247p.
31- Ten Brink, U.S., Geist, E.L., Andrews, B.D., 2006. Size distribution of submarine landslides and its implication to tsunami hazard in Puerto Rico. Geophysical Research Letters 33,L11307.
32- Wieczorek, G.F. 1987. Effect of rainfall intensity and duration on debris flows in central Santa Cruz Mountains, California. In: Costa, Wieczorek. (ed.) , Debris Flows/ Avalanches: Processes, Recognition and Mitigation. Reviews in Engineering Geology, Geological Society of America, 7:23-104.
33- Zolfagari. A HEATH. A. C. A G I S application for assessing Landslide over alarg earea computer and geomorphology. 2007.
