Corneal hill is a mountain range with an area of ​​over 30 km ², consisting of several scenic hills of up to 660 m above sea level, located in the basin of the Nysa Kłodzka and its tributaries. Frequency response extends over a length of about 9 km from the village to the east Droszkowa Nysa Kłodzka in the west. From the north it borders with Bardzkimi Mountains, south of Krowiarkami, and to the east of the Golden Mountains, from which streams are separated and Brodek Skrzynczana, are separated from Krowiarek White Lądecka. In the west, gradually move in the right Kłodzko Valley. The middle part of the hills is a clear ridge of climax Sarnicy (552 m), from which the northwest Sarnicy, to the upper stretches Jaszkową second perpendicular ridge of hills with kulminacjami chatterbox (536 m), timothy (536 m) and Szubieniczna (412 m). Hills slopes are too steep Corneal and irregular dorsal line. The most north-easternmost is the culmination of the how to lose weight fast  and west culmination of pine stands.
The geological structure of [edit]

Corneal hills lie within the Massif Kłodzko-złotostockiego, and small fragments of the south and east to metamorfiku Lądek and Śnieżnik. They are made from different varieties of granitoids, mainly granodioritic pluton amfibolowych, subordinate granite, and tonalitów monzodiorytów. Within the granitoids are of different size patches of metamorphic rocks - hornfelsów, hornfelsowych slate, gneiss migmatycznych, which are fragments of roof intrusion. Within the granitoid veins occur aplitów and lamprofirów and kataklazy and mylonityzacji zone.

In the south and east of the metamorphic rocks are metamorfiku Ladek and Śnieżnik - gneiss, mica schists, amphibolites, which have been heavily modified as a result of the impact of intrusion. In this way arose hornfelsy, shale hornfelsowe, migmatyczne gneiss, gneiss hornfelsowe, skarny. Little changed, with the lasts a its mineral composition, quartzites and amphibolites remainder occurring in the region Ołdrzychowic.

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