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  Excluded from the sampling broad valleys of large streams of higher orders, powerful alluvial fans, moraines, and the territories adjacent to industrial facilities. In the first case of river valleys are filled with recycled material long-range transport, having no direct connection with the surrounding geological formations, while the latter plays an important role of anthropogenic factors are not identifiable when interpreting the results of searches.
Usually being tested psephytic, relatively few assorted deposits that accumulate in areas of lower carrying capacity of water flow and enriched with heavy minerals.
Not subject to testing schlich well sorted fine-clastic rocks - clays, silts, fine-grained quartz sand further transportation. They contain virtually no heavy fraction, and washing them does not give representative concentrates. The depth of selection schlich samples depends on the distribution of vertical heavy fraction of detrital material. Usually schlich samples are taken from the surface of parts of channel deposits. Particularly favorable in this respect the spit, as they always wash up flowing waters of the river and moved, resulting in the most mobile grain light minerals are washed out, the most superficial layer of Kosovo sediments enriched with heavy minerals. Often the sand spit is visible black plaque laundered river concentrate. Such naturally formed concentrates congregate at the head of the spit, on its convex edge, above the large blocks of bedrock or driftwood lying on it. In selecting schlich samples in the shallows, yarn, in rivers of the clastic sediment surface cleaned to remove silt-clay sediments and alluvial turf Education opened a small snail, with removed soil horizon. In addition, a significant concentration of heavy fraction is observed in the coarse rocks lying on false raft. In view of this schlich sample usually taken from the mine workings, clearings, revealing, perhaps, the deeper horizons of alluvium, close to the true raft or above the false rafts, which provides a more reliable material on the quantitative content of heavy fractions in the clastic rocks and the enrichment of its useful components.