Paradoxes in the development of gullies

• Autorzy: Starkel L.
• Języki publikacji: EN

Abstrakty

EN

Gullies in the temperate zone are the products of linear erosion, piping and mass movements active mostly during heavy rains. On dominant role of one of those three co-operating processes decide the parameters of rainfalls and permability of substratum. The diversity of gullying depends also on the inherited relief and stage of development of gully forms. In the cultivated areas the formation of gullies is initiated also by cart-roads.

Słowa kluczowe

EN

gully formation; linear erosion; piping; mass movements; rainfall intensity; permability of substratum

• Wydawca: Stowarzyszenie Geomorfologów Polskich
• Czasopismo: Landform Analysis
• Rocznik: 2011
• Tom: Vol. 17
• Strony: 11--13
• Opis fizyczny: Bibliogr. 6 poz., rys.

Twórcy

autor

Starkel L.

• Department of Geomorphology and Hydrology, Polish Academy of Sciences, Poland,

Bibliografia

• SłupikJ., 1981. Role of slope in the formation of runoff in the Flysch Carpathians. Prace Geograficzne IGiPZ PAN 142: 1–89.
• Starkel L., 1959. Development of the relief of the Polish Carpathians in the Holocene. Przegląd Geograficzny 31: 121–141.
• Starkel L., 2005. Periglacial relief features inherited in the present-day relief of Poland. Przegląd Geograficzny 77, 11–19.
• Starkel L., 2006. Geomorphic hazards in the Polish Flysch Carpathians. Studia Geomorphologica Carpatho-Balcanica 40: 7–19.
• Starkel L., 2011. Searching for regularities of slope modelling by extreme events (diversity of rainfall intensity-duration and physical properties of the substrate). Geomorphology: in press.
• Starkel L. & Basu S. (eds.), 2000. Rains, landslides and floods in Darjeeling Himalaya. Indian National Science Academy, New Delhi: 168 pp.