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Zona turistic\u0103 Padi\u015f este situat\u0103 \u00een Mun\u0163ii Apuseni, mai precis \u00een partea nordic\u0103 a Mun\u0163ilor Bihor. Administrativ, Padi\u015ful este situat \u00een zona sud-estic\u0103 a jude\u0163ului Bihor la circa 10-15 km est de comuna Pietroasa. Zona turistic\u0103 Padi\u015f cuprinde: Bazinul \u00eenchis Padi\u015f-Cet\u0103\u0163ile Ponorului, cu o suprafa\u0163\u0103 de 36 kmp, \u00eempreun\u0103 cu Cheile Galbenei \u015fi Poiana Florilor, situate la sud-vest \u015fi zona Cheile Some\u015fului Cald – Poiana V\u0103r\u0103\u015foaia – Poiana Cuciulata situat\u0103 la nord. De asemenea turi\u015ftii mai includ \u00een zona turistic\u0103 Padi\u015f ob\u00e2r\u015fia V\u0103ii Boga, situat\u0103 \u00een partea nord-vestic\u0103 a bazinului \u00eenchis, sub abruptul Pietrelor Boghii.<\/p>\n
Zona este delimitat\u0103 de:<\/p>\n
\u00a0<\/p>\n
Bazinul \u00eenchis Padi\u015f-Cet\u0103\u0163ile Ponorului reprezint\u0103 un teritoriu din care nu exist\u0103 nici o scurgere la suprafa\u0163\u0103, fiind \u00eenchis de culmi cu \u00een\u0103l\u0163imi variind \u00eentre 1642 m (V\u0103rful M\u0103gura V\u00e2n\u0103t\u0103) \u015fi 1100 m (creasta din nord-vestul v\u00e2rfului Piatra Galbenei). El este \u00eenconjurat de bazinele hidrografice ale Some\u015fului Cald, Arie\u015fului \u015fi Cri\u015fului Pietros, drenajul tuturor apelor ce curg pe suprafa\u0163a bazinului f\u0103c\u00e2ndu-se pe sub munte \u00een Valea Galben\u0103 (peste 80%) \u015fi Valea Boga. Bazinul Padi\u015f-Cet\u0103\u0163ile Ponorului este format la r\u00e2ndul lui din opt bazine \u00eenchise \u00eentre care apele nu str\u0103bat dec\u00e2t prin canale subterane. Condi\u0163iile climatice \u00een zona Padi\u015fului difer\u0103 \u00een func\u0163ie de pozi\u0163ie. \u00cen general clima este tipic\u0103 de munte, umed\u0103 \u015fi rece<\/strong>. Bazinul \u00eenchis Padi\u015f-Cetatile Ponorului prezint\u0103 \u00eens\u0103 caracteristici climatice aparte datorit\u0103 lipsei ventila\u0163iei pe v\u0103i (acestea fiind \u00eenchise \u00eemprejur) \u015fi existen\u0163ei unor depresiuni cu doline. Aerul rece se acumuleaz\u0103 pe fundul acestora, neput\u00e2ndu-se scurge, temperatura cre\u015fte cu altitudinea, cre\u00e2ndu-se fenomenul de inversiune termic\u0103. Un fenomen deosebit \u00eel constituie “cea\u0163a padi\u015fan\u0103” care apare seara, constituit\u0103 \u00eentr-un strat dens de circa un metru \u00een\u0103l\u0163ime care se t\u00e2r\u0103\u015fte lent pe sol. Ea se datoreaz\u0103 tot reliefului alc\u0103tuit din depresiuni \u00eenchise cu doline, acestea acumul\u00e2nd c\u0103ldura ziua; seara aerul cald se ridic\u0103 \u015fi condenseaz\u0103 \u00een contactul cu capacul termic de aer rece captiv \u00een depresiuni. M-\u0163ii Bihorului prezint\u0103 vegeta\u0163ia etajat\u0103 pe vertical\u0103 dup\u0103 schema general\u0103 din Carpa\u0163i: p\u0103duri de foioase (carpineto-gorunete, carpineto-fagete), p\u0103duri de fag, p\u0103duri de amestec (fageto-br\u0103de\u0163e, fageto-molidi\u015fe), p\u0103duri de molid, tuf\u0103ri\u015furi \u015fi paji\u015fti subalpine. Acest cadru general prezint\u0103 modific\u0103ri, perturba\u0163ii \u015fi inversiuni datorit\u0103 condi\u0163iilor locale de subsol, clim\u0103 \u015fi topografie, frecvent \u015fi datorit\u0103 influen\u0163ei antropice, aceasta fiind o caracteristic\u0103 general\u0103 a Mun\u0163ilor Apuseni. O alt\u0103 caracteristic\u0103 este marea varietate a componentelor florei, aici d\u00e2ndu-\u015fi m\u00e2na elemente nordice, sudic-mediteraneene, sudic-balcanice, central-europene \u015fi orientale, eurasiatice etc., dar \u015fi cele endemice \u015fi relictare.<\/p>\n P\u0103durile \u00eentinse ce \u00eembrac\u0103 zona Padi\u015fului ad\u0103postesc numeroase specii de animale s\u0103lbatice. Ur\u015fii s\u0103l\u0103\u015fluiesc pe Muntele M\u0103gura V\u00e2n\u0103t\u0103, Boghii \u015fi \u00een Groapa Barsa, put\u00e2nd fi \u00eent\u00e2lni\u0163i \u00een mai toate zonele Padi\u015fului, \u00een afara traseelor turistice (ursul este foarte speriat de contactul cu oamenii evit\u00e2nd pe c\u00e2t se poate apropierea de zonele circulate). \u00cen aproape toate poienile se g\u0103sesc r\u00e2m\u0103turi de mistre\u0163, \u00een timp ce \u00een p\u0103durile de altitudine tr\u0103iesc coco\u015fii de munte \u015fi veveri\u0163ele. Nu demult a fost introdus\u0103 capra neagr\u0103 \u00een zona de izvoare a V\u0103ii Boga, unde s-a adaptat bine \u015fi r\u00e2sul. Cerbii \u015fi c\u0103prioarele \u00eentregesc patrimoniul cinegetic al Padi\u015fului.<\/p>\n Zona este str\u0103b\u0103tuta de la est la vest de \u015foseaua forestier\u0103 R\u0103chitele – IC Ponor – Padi\u015f – Boga – Pietroasa, \u00een lungime total\u0103 de 53 km, dintre care R\u0103chitele – Padi\u015f 31 km si Padi\u015f – Pietroasa 22 km. De la capetele \u015foselei forestiere, care este \u00een prezent greu practicabil\u0103 pentru autoturisme, exist\u0103 leg\u0103turi pe drumuri jude\u0163ene: din R\u0103chitele spre Huedin (27 km, drum par\u0163ial modernizat) \u015fi spre Sudrigiu (12 km, asfalt). \u00cen 1996 aceasta sosea forestier\u0103, prost \u00eentre\u0163inut\u0103, a fost din nou exclus\u0103 din lista drumurilor \u00een curs de modernizare, exist\u00e2nd pu\u0163ine \u015fanse ca ea s\u0103 fie reabilitat\u0103 \u00een urm\u0103torii ani. [\/et_pb_text][\/et_pb_column][\/et_pb_row][\/et_pb_section]<\/p>\n","protected":false},"excerpt":{"rendered":"
Cheile Some\u015fului Cald<\/strong>, \u00eempreun\u0103 cu Cet\u0103\u0163ile R\u0103desei reprezint\u0103 cursul superior al r\u00e2ului Some\u015ful Cald, p\u00e2n\u0103 la confluen\u0163a cu primul s\u0103u afluent “serios” – Alunul Mare, pe o lungime de circa 3 km.
Cheile Galbenei<\/strong> \u00eencep cu Izbucul Galbenei, care dreneaz\u0103 cea mai mare parte a apelor din Bazinul \u00eenchis Padi\u015f-Cet\u0103\u0163ile Ponorului. Pe primul sector, cel mai spectaculos, ele au o lungime de circa 1,5 km \u00eenconjur\u00e2nd practic pe laturile est-sud-vest Poiana Florilor. Dup\u0103 dep\u0103\u015firea Poienii Florilor, cheile continu\u0103 cu un sector deosebit de s\u0103lbatic de circa 6 km p\u00e2n\u0103 la confluen\u0163a cu Valea Bulzului.<\/p>\nClima<\/strong><\/h1>\n
Temperatura medie<\/strong> anual\u0103 este de 3 grade Celsius, vara urc\u00e2nd p\u00e2n\u0103 la 22 – 25, iar iarna sc\u0103z\u00e2nd p\u00e2n\u0103 sub -10.
V\u00e2nturile dominante<\/strong> sunt cele de la vest, aduc\u00e2nd precipita\u0163ii abundente. Din acest punct de vedere Padi\u015ful se situeaz\u0103 pe primele locuri \u00een \u0163ar\u0103 \u00een ceea ce prive\u015fte cantitatea de precipita\u0163ii.<\/p>\nFlora<\/strong><\/h1>\n
Fauna<\/strong><\/h1>\n
C\u0103i de acces<\/strong><\/h1>\n
Din \u015foseaua forestier\u0103 se desfac c\u00e2teva ramuri favoriz\u00e2nd accesul auto spre Cet\u0103\u0163ile Ponorului (de la cantonul Ponor drumul este \u00eenchis circula\u0163iei publice \u00een scopul protec\u0163iei zonei Cet\u0103\u0163ilor Ponorului), Poiana V\u0103r\u0103\u015foaia, Poiana Florilor (din Valea Bulzului), Cheile Some\u015fului Cald (de la IC Ponor) \u015fi Valea Boga (din satul Boga).
Pe potecile marcate, accesul \u00een zona Padi\u015f se poate face dinspre: Cabana Vl\u0103deasa (32 km), St\u00e2na de Vale (20 km), Pietroasa (20 km), \u015faua V\u00e2rtop (24 km), Arie\u015feni (16 km), Comuna G\u00e2rda (23 km), Pe\u015ftera Ghe\u0163arul Sc\u0103ri\u015foara (20 km).<\/p>\n