8 [1] We propose a methodology for upscaling biomass in a 9 river using a combination of dimensional analysis and 10 hydro-geomorphologic scaling laws. We first demonstrate 11 the use of dimensional analysis for determining local scaling 12 relationships between Nostoc biomass and hydrologic and 13 geomorphic variables. We then combine these relationships 14 with hydraulic geometry and streamfl...

There is strong empirical evidence on the importance of spatial pattern vegetation in dryland hydrologic and geomorphologic dynamics. However, changes cover are often linked, making it difficult to disentangle assess their independent hydro-geomorphologic roles. We used synthetic sponges placed soil surface mimic aboveground structure patches, manipulated patch as well sink capacity patches a s...

Landslide inventories provide the knowledge basis for many geomorphological applications and also planning emergency management. Detailed landslide should be prepared where pre-existing are available, as updates. In this paper, we present a new inventory an area of High Agri Valley, Southern Italian Apennines. The map was through systematic interpretation historical aerial photographs testing e...

river of the most important factors in the cycle of erosion and geomorphologic process and present their studies on the wide are. in this research , the purpose of understanding factors that influence changes geomorphologic middle part of the river bed and atrak river review these changes has been the domain. this area is located between the villages of ghazan ghaye to chat in golestan province...

REGIONAL SCALE. R. D. Capitan, G. R. Osinski, M. J. Van De Wiel, M. Kerrigan, N. Barry, S. Blain, Centre for Planetary Science and Exploration University of Western Ontario, London, ON, Canada N6A 5B7 ([email protected]), 2 Dept. of Earth Sciences/Physics and Astronomy, University of Western Ontario, London, ON, Canada N6A 5B7, Dept. of Geography, University of Western Ontario, London, ON, Canada ...

[1] Folds are one of the obvious and common manifestations of deformation of the continental crust, and attempts to understand the origins of these structures extend back to the very beginnings of geology as a discipline within the Earth Sciences. In particular, the relationship between faults and folds, and the manner in which fault-related folds grow and evolve through time, has been the subj...