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L. Starkel

Fig. 3. Areas investigated and surveyed in the project MR 1 — 25: 1 — paleogeographic research, 2 — studies of present-day processes, 3 — field stations with monitoring of hydrologie and geomorphic processes, 4 — detailed topoclimatic studies, 5 — detailed phytogeographic studies, 6 — detailed applied environmental studies, 7 — areas covered by generał maps of geomorphic processes, 8 — areas covered by generał climatological maps, 9 — areas covcred by generał mapping of potential vegetation, 10 — areas covered by generał mapping of geosystems (physico-geographic typology)

deposits (Kostrzewski and Zwoliński 1984) as well as the ratę of inter-soil circulation (Froehlich 1982) have been recognized. The measurements on the cart roads and the splash experiment enabled one to State that 80 — 90% of the suspended loads in the channel loriginate from the roads in many regions (Froehlich and Slupik 1985; Froehlich — in press).

The gravitational processes were subject to the detail studies of E. Gil and A. Kotarba. These studies were continued in a cooperation with E. Thiel of the Institute of the Hydroengineering, Polish Academy of Sciences. Based on the measurements of the rockfalls and of the transfer on the alluvial cones in the Tatra Mts several models of the modifications of the high-mountain slope have been elaborated (Kotarba et al. 1983; Kotarba et al. — in press). The photogrametric studies of the cliff on the Wolin Island allowed to recognize the role of the lithology on the type of the cliff modelling

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