Titlebook: Slope-Channel Coupling as a Factor in the Evolution of Mountains; The Western Carpathi Ma?gorzata Wistuba Book 2014 Springer International

cortex

The Evolution of Relief in Mid-Altitude Mountains as a Result of the Delivery of Slope Material to pter, I have attempted to prepare a schema of evolution of mid-mountain relief due to the interaction of slopes and stream channels in small catchments. Detailed results of the thesis are discussed here as the premises of the schema. The schema itself is presented to describe the evolution of mid-mo

KEGEL

Ma?gorzata WistubaNominated as an outstanding Ph. D. thesis by the University of Silesia in Katowice, Poland.Dendrochronological record of lateral slope-channel (landsliding-erosion) coupling - the work presents result

seruting

978-3-319-38296-8Springer International Publishing Switzerland 2014

convert

Slope-Channel Coupling as a Factor in the Evolution of Mountains978-3-319-05819-1Series ISSN 2190-5053 Series E-ISSN 2190-5061

浪費時間

Springer Theseshttp://image.papertrans.cn/s/image/868421.jpg

PACK

到婚嫁年齡

偽造

Materials and Methods,s), middle and lower (outlet fans) sections of catchments. Due to the diversity of sites studied in each of them, different sets of research methods were used. The methods applied were divided into four groups according to their objectives. Methods used for: relief analysis (geomorphic mapping, morp

殘廢的火焰

Study Catchments,ents and valleys of small streams which are areas with the strongest potential for coupling, high energy and strong dynamics of geomorphic processes. Studies were conducted in two mid-altitude mountain massifs: in the Moravskoslezské Beskydy Mts. (Western Carpathians) and in the Hruby Jeseník Mts. (

吃掉

The Delivery of Slope Material to the Valley Floors of Small Mid-Mountain Catchments: Record in Rel (upper—valley heads, middle and lower—outlet fans) and two study areas (Western Carpathians and Sudetes). In valley heads: debris flows and their impact on fluvial processes were analysed in the catchment of ?erny stream (Sudetes), while landsliding, lateral and linear erosion were discussed based