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DRINI I BARDH

Ujรซvara Drini i Bardhรซ Bukuri natyrore dhe atraksion turistik i komunรซs sรซ Pejรซs padyshim รซshtรซ โ€œUjรซvara e Drinit tรซ Bardhรซโ€. Ajo รซshtรซ njรซ nga ujรซvarat mรซ spektakolare tรซ Kosovรซs, e cila vizitohet nga turistรซt gjatรซ gjithรซ vitit. Burimi i Drinit tรซ Bardhรซ รซshtรซ njรซ nga burimet mรซ tรซ rรซndรซsishme tรซ Kosovรซs dhe njรซ nga burimet, qรซ furnizon qytetin e Pejรซs me ujรซ tรซ pijes. Vlenรซ tรซ theksohet se me ujin e kรซtij burimi prodhohet edhe โ€œBirra Pejaโ€ e njohur pรซr kualitetin e lartรซ tรซ saj. Buron rrรซnzรซ bjeshkรซs sรซ Rusolisรซ, nga gurra e shpellรซs sรซ Radacit nรซ lartรซsi mbidetare prej 586 m. Burimi krijon edhe ujรซvaren e bukur tรซ Drinit nรซ gjatรซsi prej 30 m. Nรซ territorin e Kosovรซs โ€“ Drini i Bardhรซ gjarpรซron pรซr 122 km nรซ drejtim veri-jug. Ai mbledh nรซ vete edhe ujรซrat e Lumbardhit tรซ Pejรซs, Erenikut dhe Lumbardhit tรซ Prizrenit. Me njรซ madhรซsi prej 4646 km2 dhe bazeni i Drinit รซshtรซ mรซ i madhi nga 4 bazenet ujรซmbledhรซse tรซ Kosovรซs. Qasja pรซr nรซ burim apo โ€œUjรซvara e Drinit tรซ Bardhรซโ€ mund tรซ bรซhet nga dy anรซ: ku njรซra anรซ tรซ shpie nga rruga e hidrocentralit apo restaurant โ€œUjรซvara e Drinitโ€ pรซr tรซ ndjekur pastaj shtegun e kรซmbรซsorรซve pรซrgjatรซ bukurisรซ sรซ lumit Drini i Bardhรซ nรซn hijen e pemรซve dhe freskut, qรซ qarkullon pรซrmes kanjonit nรซ gjatรซsi deri nรซ 400 m, si dhe qasja tjetรซr nรซ drejtim tรซ restaurantit โ€œTrofta e Drinitโ€ ku mund tรซ afroheni me makinรซ deri te shtegu pรซr tรซ vazhduar ecjen deri te ujรซvara. SHPELLA

โ€œBUKUROSHJA E FJETURโ€ Shpella e Radacit gjendet afรซr ujรซvarรซs sรซ Drinit tรซ Bardhรซ. Shtrihet nรซ pjesรซn verilindore tรซ vargmaleve tรซ Bjeshkรซve tรซ Nemuna. Shpella รซshtรซ e thelluar nรซ shkrepa, tรซ cilรซt e pรซrbรซjnรซ majen e Rusolisรซ me lartรซsi mbidetare 2381 m ndรซr, tรซ cilรซn shtrihet fusha e Drinit tรซ Bardhรซ. Me vetitรซ e veta morfologjike รซshtรซ e radhitur me disa degรซ dhe galeri, salla, korridore dhe kanale. Formimi i shpellรซs รซshtรซ i lidhur me evolucionin hidrologjik tรซ pjesรซs perรซndimore tรซ krasit gรซlqeror tรซ majรซs sรซ Rusolisรซ. Rrjedha nรซntokรซsore ka formuar kanale mรซ tรซ mรซdha, tรซ cilat janรซ ndรซrtuar nรซ kohรซn e para Levantit, kanalet mรซ tรซ mรซdha tรซ shpellรซs janรซ krijuar nรซ kohรซn e liqeneve mรซ tรซ ulรซta kur รซshtรซ formuar galeria e dytรซ e shpellรซs. E pasuruar me dekorime prej รงfarรซdo shpelle nรซ shkrepat e kรซtij territori, shpella e Radacit me lidhjet e shumta tรซ kanaleve nรซntokรซsore, galerive tรซ lehta pรซr ecje, kushteve dhe vetive mikroklimatike, paraqet njรซ objekt mjaft tรซrheqรซs turistik. Tani kjo shpellรซ รซshrtรซ e hapur pรซr vizita gjatรซ gjithรซ vitit.

Shkarko Broshuren Kร‹TU

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