Lej Wielki

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Lej Wielki - a geological form of nature in south-western Poland in the Eastern Sudetes, in the Śnieżnik Massif.

Lej Wielki, located in the Eastern Sudetes, in Śnieżnicki Landscape Park in the middle east of the Śnieżnik Massif, about 1.2 km, north-east of Śnieżnik. On the north side of the Black Ridge.

The poorly developed knight's niche in the Gniezno rocks of the Śnieżnik Massif, in the shape of a funnel, splitting in the eastern slope of Śnieżnik, "Devil Gon" or "Devil's Downhill". Lej is a natural slope reduction, created during the last glaciation and carved by the descending winter avalanche. At the moment no avalanches are recorded.

The hoppers are covered with tall grass and sparse lowland spruce forest with beech, fir and pine. The forest in the 1980's during the ecological disaster was partially destroyed. Lejem flows the nameless left tributary of the Kamienica River, whose sources are situated on the eastern slope of Śnieżnik called Czarci Gon.

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