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  Drawing on preliminary results of the search card allows you to highlight promising for further search of the river valleys and to identify the role of tributaries in the removal of valuable minerals. At the stage of general searches as well as search and search and evaluation studies schlich samples located within the study area as possible evenly, covering the entire area in accordance with the condition. Even distribution of samples in the area reached the systematic testing of the entire river system - permanent streams of all orders, down to very low, temporary water and dry gullies, beams and gully. Schlich sampling of alluvial deposits is accompanied by testing of deluvial sides of river valleys and watersheds eluvia spaces. Schlich sampling of alluvium in the valleys of small tributaries with steep longitudinal profile, complicated by the presence psephytic Svalov, in which case it is expedient to obtain samples from deluvial, proalluvial and solifluction formations in the side of the valley and gully. In some cases, samples are taken from natural outcrops of bedrock in order to obtain artificial concentrates to identify the root sources of mineralization. The correct choice of selecting the sample determines schlich to obtain reliable results. Schlich samples have in those parts of the river channel, where reduced water flow rate and accumulation of river transported clastic material. It is here that there is a maximum enrichment of alluvial material with heavy minerals, and flushing schlich samples gives a significant yield of the concentrate. These favorable to schlich testing are areas located downstream regions of morphological changes in the structure of river valleys - their excesses of the longitudinal profile (below the thresholds, sills), a dramatic expansion of the valleys, steep bends of the river bed and so on.
Thus, schlich samples were taken at the head of braids on convex bends the shore in areas of abrupt turns the channel on the beaches, sandbanks, oxbow in, areas that lie above the obstacles in the water flow (debris, snags, large boulders), the outputs of the indigenous breeds bed channel.