Abstract
Diverse sources of information, which describes landslide movement, hillslope-channel connectivity and sedimentation rates, are analyzed to detect trends that took place during the last 12,000 years. We estimate the landslide-related sediment production rates by combining measured landslide velocities and geometries and historical landslide frequency. Coarse sediment deposition rates are measured throughout the Holocene by means of dating and stratigraphy of the alluvial fan and terraced deposits. The comparison between present-day hillslope sediment production and Holocene averaged sediment deposition rates confirms that landsliding is the main agent conveying sediments to higher order trunk streams. The connectivity between hillslopes and the stream network is well developed and no significant sediment sinks influence the sediment transport process. However fluctuations of sediment delivery rates at the outlet of the catchment took place during Holocene and are likely associated to periods of increased hillslope sediment production and channel discharge caused by climatic forcing.
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References
Brardinoni F, Church M (2004) Representing the landslide magnitude-frequency relation: Capilano River basin, British Columbia. Earth Surf Process Land 29:115–124
Bertolini G, Guida M, Pizziolo M (2005) Landslides in Emilia-Romagna region (Italy): strategies for hazard assessment and risk management. Landslides 2:302–312
Cruden DM, Varnes DJ (1996) Landslide types and processes. In: Turner AK, Schuster RL (eds) Landslides: investigation and mitigation. National Academy Press, Washington, DC, pp 36–71
Cyr AJ, Granger DE (2008) Dynamic equilibrium among erosion, river incision, and coastal uplift in the northern and central Apennines, Italy. Geology 36(2):103–106. doi:10.1130/G24003A.1
D’Anastasio E, De Martini PM, Selvaggi G, Pantosti D, Marchioni A, Maseroli R (2006) Short-term vertical velocity field in the Apennines (Italy) revealed by geodetic levelling data. Tectonophysics 418:219–234. doi:10.1016/j.tecto.2006.02.008
de Vente J, Poesen J, Bazzoffi P, van Rompaey A, Verstraeten G (2006) Predicting catchment sediment yield in Mediterranean sediment sources and basins. Earth Surf Process Land 31:1017–1034
Goswami R, Mitchell NC, Brocklehurst SH (2011) Distribution and causes of landslides in the eastern Peloritani of NE Sicily and western Aspromonte of SW Calabria, Italy. Geomorphology 132(3–4):111–122. doi:10.1016/j.geomorph.2011.04.036
Guzzetti F, Malamud BD, Turcotte DL, Reichenbach P (2002) Power-law correlations of landslide areas in central Italy. Earth Planet Sci Lett 195:169–183
Guzzetti F, Ardizzone F, Cardinali M, Rossi M, Valigi D (2009) Landslide volumes and landslide mobilization rates in Umbria, central Italy. Earth Planet Sci Lett 279:222–229
Hungr O, Evans SG, Bovis MJ, Hutchinson JN (2001) A review of the classification of landslides of the flow type. Environ Eng Geosci 7(3):221–238
Iverson RM, Major JJ (1987) Rainfall, groundwater flow, and seasonal movement at Minor Creek landslide, northwestern California: physical interpretation of empirical relations. Geol Soc Am Bull 99:579–594
Korup O, Densmore AL, Schlunegger F (2010) The role of landslides in mountain range evolution. Geomorphology 120:77–90
Larsen IJ, Montgomery DR, Korup O (2010) Landslide erosion controlled by hillslope material. Nat Geosci 3:247–251. doi:10.1038/NGEO776
Mackey BH, Roering JJ (2011) Sediment yield, spatial characteristics, and the long-term evolution of active earthflows determined from airborne LiDAR and historical aerial photographs, Eel River, California. GSA Bulletin 123(7/8):1560–1576. doi:10.1130/B30306.1
Parker RN, Densmore AL, Rosser NJ, de Michele M, Li Y, Huang R, Whadcoat S, Petley DN (2011) Mass wasting triggered by the 2008 Wenchuan earthquake is greater than orogenic growth. Nat Geosci, advance online publication, 4 pages, doi:10.1038/NGEO1154
Picotti V, Pazzaglia FJ (2008) A new active tectonic model for the construction of the Northern Apennines mountain front near Bologna (Italy). J Geophys Res 113, B08412, 24 pages, doi:10.1029/2007JB005307
Pini GA (1999) Tectonosomes and olistostromes in the Argille Scagliose of Northern Apennines, Italy. Geological Society of America Special Paper 335, 70 p
Regione Emilia-Romagna (2011) Inventario del dissesto. URL: http://www.regione.emilia-romagna.it/wcm/geologia/canali/cartografia/sito_cartografia/web_gis_dissesto.htm. Last accessed 17 June 2011
Reid LM, Page MJ (2002) Magnitude and frequency of landsliding in a large New Zealand catchment. Geomorphology 49:71–88
Rossi M, Witt A, Guzzetti G, Malamud BD, Peruccacci S (2010) Analysis of historical landslide time series in the Emilia-Romagna region, northern Italy. Earth Surf Process Land 35:1123–1137. doi:10.1002/esp.1858
Van Asch TWJ (2005) Modelling the hysteresis in the velocity pattern of slow-moving earth flows: the role of excess pore pressure. Earth Surf Process Land 30:403–411
Zattin M, Picotti V, Zuffa GG (2002) Fission-track reconstruction of the front of the northern Apennine thrust wedge and overlying Ligurian Unit. Am J Sci 302:346–379. doi:10.2475/ajs.302.4.346
Acknowledgments
This work has been done in the framework of the Sedymont Project (TOPO-EUROPE) and we would like to thank all the participants who shared our opinion and promoted fruitful discussions.
We would like to thank Emilia-Romagna Region for kindly supplying the following data: landslide inventory map and historical archive, inclinometer readings, borehole logs and dating results on the alluvial fan.
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Simoni, A., Ponza, A., Picotti, V., Berti, M. (2013). Landslide-Related Sediment Yield Rate in a Large Apenninic Catchment. In: Margottini, C., Canuti, P., Sassa, K. (eds) Landslide Science and Practice. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-31337-0_39
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DOI: https://doi.org/10.1007/978-3-642-31337-0_39
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