{"id":92,"date":"2020-04-23T10:16:17","date_gmt":"2020-04-23T10:16:17","guid":{"rendered":"http:\/\/localhost\/pelister\/?post_type=geomorphologies&#038;p=92"},"modified":"2020-09-09T05:30:39","modified_gmt":"2020-09-09T05:30:39","slug":"test","status":"publish","type":"geomorphologies","link":"https:\/\/park-pelister.com\/sq\/geomorphologies\/test\/","title":{"rendered":"Gjeologjia dhe litologjia"},"content":{"rendered":"<p>Struktura gjeologjike t\u00eb malit Baba p\u00ebrb\u00ebhet kryesisht nga shistrat dhe granitet Paleozoike, t\u00eb cilat u zbuluan n\u00eb m\u00ebnyr\u00eb tektonike dhe erozive n\u00eb pjes\u00ebn e mesme. Kreshta kryesore n\u00eb veri fillon me maj\u00ebn Kozji Kamen (2137 m) dhe p\u00ebrfundon n\u00eb territorin e Greqis\u00eb. N\u00eb lindje dhe per\u00ebndim, ka kreshta an\u00ebsore q\u00eb ndahen nga luginat e lumenjve.<\/p>\n<p><img loading=\"lazy\" class=\"alignnone wp-image-435\" src=\"http:\/\/pelister.development.ivote.mk\/wp-content\/uploads\/2020\/04\/94753004_1353206024877952_6230756511400853504_n-300x247.jpg\" alt=\"\" width=\"256\" height=\"211\" srcset=\"https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/94753004_1353206024877952_6230756511400853504_n-300x247.jpg 300w, https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/94753004_1353206024877952_6230756511400853504_n.jpg 511w\" sizes=\"(max-width: 256px) 100vw, 256px\" \/>\u00a0 \u00a0 \u00a0 \u00a0 \u00a0 \u00a0 <img loading=\"lazy\" class=\"alignnone wp-image-436\" src=\"http:\/\/pelister.development.ivote.mk\/wp-content\/uploads\/2020\/04\/27164551_10204191419863600_4023709918307131162_o-300x199.jpg\" alt=\"\" width=\"321\" height=\"212\" srcset=\"https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/27164551_10204191419863600_4023709918307131162_o-300x199.jpg 300w, https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/27164551_10204191419863600_4023709918307131162_o-768x509.jpg 768w, https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/27164551_10204191419863600_4023709918307131162_o.jpg 960w\" sizes=\"(max-width: 321px) 100vw, 321px\" \/><\/p>\n<p>Kreshta kryesore malore \u00ebsht\u00eb gjithashtu nj\u00eb pellg uj\u00ebmbledh\u00ebs midis pellgjeve Adriatik dhe Egje. Nj\u00eb element i r\u00ebnd\u00ebsish\u00ebm n\u00eb relievin e malit Baba jan\u00eb rrafsh\u00ebt e vjet\u00ebr t\u00eb denudimit t\u00eb l\u00ebngjeve n\u00eb nj\u00eb lart\u00ebsi prej 1660 deri n\u00eb 1900 m, t\u00eb cilat ndahen thell\u00ebsisht nga lugina pothuajse paralele. Struktura e relievit t\u00eb malit, p\u00ebrve\u00e7 kreshtave t\u00eb spikatura, mbizot\u00ebrohet nga lugina me mure t\u00eb thella, kryesisht t\u00eb predispozuara. T\u00eb tilla jan\u00eb luginat e lumit Malovishka, pjesa burimore e lumit Dragor, lumi Brajcinska etj. Nga element\u00ebt morfo-skulpturor\u00eb, dallohen lumenjt\u00eb prej guri n\u00eb nj\u00eb lart\u00ebsi prej 1300 deri 2000 m, t\u00eb cilat jan\u00eb nj\u00eb nga m\u00eb t\u00eb goditshmet n\u00eb Gadishullin Ballkanik.<\/p>\n<p><img loading=\"lazy\" class=\"alignnone size-medium wp-image-434\" src=\"http:\/\/pelister.development.ivote.mk\/wp-content\/uploads\/2020\/04\/6-146-300x225.jpg\" alt=\"\" width=\"300\" height=\"225\" srcset=\"https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/6-146-300x225.jpg 300w, https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/6-146-768x576.jpg 768w, https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/6-146.jpg 800w\" sizes=\"(max-width: 300px) 100vw, 300px\" \/>\u00a0 \u00a0 \u00a0 \u00a0 \u00a0 \u00a0 <img loading=\"lazy\" class=\"alignnone wp-image-433\" src=\"http:\/\/pelister.development.ivote.mk\/wp-content\/uploads\/2020\/04\/167-300x200.jpg\" alt=\"\" width=\"333\" height=\"222\" srcset=\"https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/167-300x200.jpg 300w, https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/167.jpg 640w\" sizes=\"(max-width: 333px) 100vw, 333px\" \/><\/p>\n<p>P\u00ebrmbytjet jan\u00eb gjithashtu nj\u00eb tipar i r\u00ebnd\u00ebsish\u00ebm leht\u00ebsimi, q\u00eb ndodhin n\u00eb nj\u00eb rrip t\u00eb gjat\u00eb p\u00ebrgjat\u00eb ult\u00ebsir\u00ebs lindore, veriore dhe per\u00ebndimore. Pjes\u00ebt e larta malore t\u00eb Bab\u00ebs, gjat\u00eb Pleistocenit ishin t\u00eb pushtuara nga akullnajat, t\u00eb cilat lan\u00eb gjurm\u00ebt e saj n\u00eb relievin e sot\u00ebm, n\u00eb format fosile akullnajore: cirk dhe morin\u00eb. Gjurm\u00ebt e cirk\u00ebve jan\u00eb mbi 1900 m mbi nivelin e detit. dy prej t\u00eb cilave mbushen vazhdimisht me uj\u00eb dhe n\u00eb to jan\u00eb Liqeni i Madh dhe i Vog\u00ebl. N\u00eb pjes\u00ebt e larta t\u00eb Pelisterit, p\u00ebrve\u00e7 lumenjve dhe deteve shk\u00ebmbor\u00eb, jan\u00eb t\u00eb pranishme forma t\u00eb shumta t\u00eb vogla periglaciale.<\/p>\n<p><img loading=\"lazy\" class=\"alignnone size-medium wp-image-437\" src=\"http:\/\/pelister.development.ivote.mk\/wp-content\/uploads\/2020\/04\/73145414_1185924644939425_6497368354351742976_n-300x225.jpg\" alt=\"\" width=\"300\" height=\"225\" srcset=\"https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/73145414_1185924644939425_6497368354351742976_n-300x225.jpg 300w, https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/73145414_1185924644939425_6497368354351742976_n-768x576.jpg 768w, https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/73145414_1185924644939425_6497368354351742976_n.jpg 960w\" sizes=\"(max-width: 300px) 100vw, 300px\" \/>\u00a0 \u00a0 \u00a0 \u00a0 \u00a0 \u00a0 \u00a0 <img loading=\"lazy\" class=\"alignnone size-medium wp-image-438\" src=\"http:\/\/pelister.development.ivote.mk\/wp-content\/uploads\/2020\/04\/73082558_1192428997622323_3869094891732598784_n-300x225.jpg\" alt=\"\" width=\"300\" height=\"225\" srcset=\"https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/73082558_1192428997622323_3869094891732598784_n-300x225.jpg 300w, https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/73082558_1192428997622323_3869094891732598784_n.jpg 640w\" sizes=\"(max-width: 300px) 100vw, 300px\" \/><\/p>","protected":false},"featured_media":374,"template":"","_links":{"self":[{"href":"https:\/\/park-pelister.com\/sq\/wp-json\/wp\/v2\/geomorphologies\/92"}],"collection":[{"href":"https:\/\/park-pelister.com\/sq\/wp-json\/wp\/v2\/geomorphologies"}],"about":[{"href":"https:\/\/park-pelister.com\/sq\/wp-json\/wp\/v2\/types\/geomorphologies"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/park-pelister.com\/sq\/wp-json\/wp\/v2\/media\/374"}],"wp:attachment":[{"href":"https:\/\/park-pelister.com\/sq\/wp-json\/wp\/v2\/media?parent=92"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}