{"id":536,"date":"2020-05-10T07:34:57","date_gmt":"2020-05-10T07:34:57","guid":{"rendered":"http:\/\/pelister.development.ivote.mk\/?post_type=geomorphologies&#038;p=536"},"modified":"2020-09-09T05:34:26","modified_gmt":"2020-09-09T05:34:26","slug":"%d1%82%d0%b5%d0%ba%d1%82%d0%be%d0%bd%d0%b8%d0%ba%d0%b0","status":"publish","type":"geomorphologies","link":"https:\/\/park-pelister.com\/sq\/geomorphologies\/%d1%82%d0%b5%d0%ba%d1%82%d0%be%d0%bd%d0%b8%d0%ba%d0%b0\/","title":{"rendered":"Granit\u00ebt e malit Baba"},"content":{"rendered":"<p>N\u00eb shtrirjen e gjer\u00eb t\u00eb PK &#8220;Pelister&#8221;, zona m\u00eb e madhe \u00ebsht\u00eb e mbuluar nga shk\u00ebmbinjt\u00eb e argjil\u00ebs Paleozoike. Ato kan\u00eb nj\u00eb p\u00ebrb\u00ebrje lithologjike t\u00eb larmishme, dhe sipas hart\u00ebs themelore gjeologjike 1: 100000, Rethet e Manastirit dhe e Florin\u00ebs dallohen k\u00ebtu: nj\u00eb seri shalle kuarci-serikiti dhe jeshile dhe nj\u00eb seri phyllitoid. P\u00ebr m\u00eb tep\u00ebr, nj\u00eb zon\u00eb e konsiderueshme \u00ebsht\u00eb e z\u00ebn\u00eb nga shk\u00ebmbinj granitoid\u00eb, t\u00eb cil\u00ebt jan\u00eb gjithashtu t\u00eb epok\u00ebs Paleozoike. Granit\u00ebt formojn\u00eb b\u00ebrtham\u00ebn e ndezur t\u00eb malit Baba n\u00eb form\u00ebn e nj\u00eb trupi t\u00eb madh ndez\u00ebs &#8211; batolit. Masa e granitit \u00ebsht\u00eb e zgjatur n\u00eb drejtimin veri &#8211; jug, me prishje p\u00ebrgjat\u00eb gjith\u00eb gjat\u00ebsis\u00eb s\u00eb malit, dhe gjer\u00ebsia \u00ebsht\u00eb nga 5 deri n\u00eb 10 km.<\/p>\n<p><img loading=\"lazy\" class=\"alignnone size-medium wp-image-371\" src=\"http:\/\/pelister.development.ivote.mk\/wp-content\/uploads\/2020\/04\/1-150_Page_036-1-300x293.jpg\" alt=\"\" width=\"300\" height=\"293\" srcset=\"https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/1-150_Page_036-1-300x293.jpg 300w, https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/1-150_Page_036-1.jpg 492w\" sizes=\"(max-width: 300px) 100vw, 300px\" \/><\/p>\n<p>P\u00ebrve\u00e7 Paleozoikut, si nj\u00eb p\u00ebrb\u00ebr\u00ebs i dyt\u00eb themelor stratigrafik n\u00eb pjes\u00ebn e PK &#8220;Pelister&#8221; jan\u00eb formacionet Triasike, t\u00eb cilat jan\u00eb duksh\u00ebm m\u00eb pak t\u00eb pranishme.<\/p>","protected":false},"featured_media":547,"template":"","_links":{"self":[{"href":"https:\/\/park-pelister.com\/sq\/wp-json\/wp\/v2\/geomorphologies\/536"}],"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\/547"}],"wp:attachment":[{"href":"https:\/\/park-pelister.com\/sq\/wp-json\/wp\/v2\/media?parent=536"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}