By Ewgienij Proczko
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Additional info for No. 304 - Focke-Wulf Ta 154 "Moskito" - Tank Power
The basins of the Zomaro Province, however, sharply cut, are first order basins that reach the main divide Altitude and Slopes 42 (Appendix B 09-12). Because the high plains of this province drain mainly towards the west, these distributions end abruptly with the high gradients of the valley heads. The combined point cluster of all basins 01 - 19 (Appendix B 20) permit a complex interpretation. It displays a homogeneous segment of a half circle with a somewhat diffuse, but still distinct upper limitation.
Data Base. 04%--------~ . 5 -_ •• t=============~~~~-~ Percent drainage area of the entire region per 5 km coast unit . 5 1 100 I I I "" I l 807 I I II 11 111 100 10 ! II! 1% Rec iprocal drainage ratio Increasing size of drainage area Fig. 7 A, B. Size of drainage basins and shelf configuration. A The 100-m and 200-m depth contour lines come close to the coast where large rivers flow into the sea and vice versa, the shelf widens off smaller source areas. Hatched line the line of the reciprocal drainage ratio is a calculated data line.
12). 4 Conclusion Order, size and shape of the Calabrian basins have no visible influence on the river-mouth sediments; the same is true for all channel network characteristics. This is disappointing, because the digitization of these properties and their quantitative treatment should have made it possible to detect such relationships. We expected at least maximum grain sizes and properties such as bimodality to be possibly dependent on geomorphology. This is discussed in Chapter 10. In short, the broad range 29 of grain sizes of the river-mouth sediments should be sensitive to the hydrodynamic conditions of the rivers and these in turn should be sensitive to or shaped by the most important basin characteristics.
No. 304 - Focke-Wulf Ta 154 "Moskito" - Tank Power by Ewgienij Proczko