Download Yagnob Valley – Nature, history, and chances of a mountain by A. Gunya PDF

By A. Gunya

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Extra info for Yagnob Valley – Nature, history, and chances of a mountain community development in Tajikistan

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On typical light brown soils with low detritus contents; used as arable lands, hayfields and settlement lands. 16. , асе. ) used up and beaten down to a large extent, on light brown carbonaceous soils with low detritus contents; used as pasture lands for cattle, sheep and goats (May – October). 17. , Ribes), on typical light brown soils with high detritus contents; used as pasture lands for cattle, sheep and goats (May – September). 18. , Festuca sulcata), frequently with Ferula Jaeschkeana Vatke, beaten down, on light brown carbonaceous soils with high detritus contents; used as pasture lands for cattle, sheep and goats, less frequently as arable lands.

Melanantha, etc. They are widespread in conditions of permanently excessive humidification forming dense herbaceous associations. 7. Tall-herbs ephemeroids – umbrelliferous, representatives of the ephemeroid vegetation. This group comprises two species of herbaceous perennials: kamol – Ferula jaeschkeana and yougan – Prangos pabularia. They are fairly widespread in Yagnob (principally in its lower belt and to a smaller extent in high mountain area). Nevertheless, the vegetation with these species’ predominance is developed only within the bounds of a limited territory of the north-oriented slope of the Hissar Range – in basins of the rivers Kul and Tagob.

31 32 Landslip deposits are the most important for the formation of modern landscape among all Quaternary deposits (Fig. 9). The development of landslips and crumblings indicates an ample activity of denudation processes. Landslips dated by the latter Pleistocene have a compact loam and sandy loam aggregate, landslips of the Holocene consist of blocks, packets, clods and detritus with gravelly-loamy aggregate that designate their higher mobility and instability in the actual period. Slopes formed on the alteration crust of Paleozoic schist are predominant among landslip slopes.

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