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Dnia 15 sierpnia 2007 roku, między godz. 21:00 a 22:30 w Górach Sowich obserwowano dwie popielice żerujące na końskim nawozie. Ssaki pobierały fragmenty nawozu z ziemi, około 20 m od ściany lasu, a następnie siedząc w środku pobliskiego krzaka róży na wysokości 0,5–1 m, wybierały z nich fragmenty roślin. Czynność tę powtórzyły dwu–trzykrotnie, po czym wróciły do lasu
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Terasy rolne w Górach Sowich

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Creation or agricultural terraces is one of the main method of anti-erosional protection in the mountain regions. In the Sudetes Mountains the terraces are in many places relict landforms, which developed during previous centuries, when the extent of settlements and agricultural land use was much more widespread. The article presents the agricultural terraces in the Sowie Mts in the context of other, very few studies, which were conductcd in the Sudetes referring to agricultural terraces. Terracing leads to changes of slope longitudinal profiles, dividing them into separate units with erosion dominating in their upper parts and accumulation in lower parts, behind the upper edge of every terrace. The steeper and the longer is the slope, the higher is the terrace. Also the thickness of agricultural sandy-silty layer, which originates from slope wash and ploughing, and accumulates over the terrace edge, increases according to the increase or slope inclination and slope length. The material which is stored within the terraces is enriched with fine-grained particles (sandy-silty), due to the selective character or surface wash. In contrast, the upper parts of slope are left more coarsegrained. The material accumulated within the terraces allows for estimation of the minimum anthropogenic denudation from slopes under present or former ploughing. The values of denudation for the Sudetes range from 0,09 to 2,7 mm year⁻¹ and depend strongly on lithology, slope inclination and length.
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The aim of the research was to assess the degree of damage to spruce trees and stands and to study their growth responses to the changing environmental conditions in the Sowie Mountains (Central Sudety Mts.). To assess the degree of damage to trees, three methods based on crown characteristics were used. The types of growth responses of trees to changing environmental conditions were additionally taken into account in one of the methods. Regardless of the assessment method, spruce stands in the Sowie Mountains demonstrated a high level of damage. The poorest growth conditions were found in the period 1966−1980 when a large number of trees showed negative growth responses, indicating a decrease in radial increment. The period 1996−2010 showed an improvement in the growth conditions of trees because the proportion of trees with negative growth responses decreased, while the proportion of trees with positive growth responses increased. It was also found that the growth conditions for spruce were more favourable in the lower montane forest zone (above 600 m a.s.l.), and less favourable at the foothills (below 600 m a.s.l.), which may be caused by the competition of beech replacing spruce in the lower locations in the mountains.
The influence of the edge effect on the meadow vegetation pattern was studied in the forest glades in the central part of the Middle Sudety Mts. (SW Poland). The spectacular edge effect is seen in the range of 4 m from the forest border towards the center of the glades. Within that belt we observed decrease in tree and bush species number, increase in share of graminoids and Fabaceae species, as well as increase in share of species generally related to grassland communities. A significant increase in species number and values of Shannon−Wiener diversity index was noticed within the distance of eight meters from the edges of glades.
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