{"id":537,"date":"2020-05-10T07:47:12","date_gmt":"2020-05-10T07:47:12","guid":{"rendered":"http:\/\/pelister.development.ivote.mk\/?post_type=geomorphologies&#038;p=537"},"modified":"2020-09-09T05:35:57","modified_gmt":"2020-09-09T05:35:57","slug":"%d1%82%d0%b5%d0%ba%d1%82%d0%be%d0%bd%d0%b8%d0%ba%d0%b0-2","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%b0-2\/","title":{"rendered":"Tektonika"},"content":{"rendered":"<p>Aktivitetet komplekse dhe tektonike n\u00eb malin e Bab\u00ebs, si nj\u00eb struktur\u00eb par\u00ebsore (batholith), rezultuan n\u00eb krijimin e strukturave dyt\u00ebsore: shtresa rajonale dhe lokale, antiklin\u00eb dhe sinklin.<\/p>\n<p>P\u00ebrgjat\u00eb korniz\u00ebs veriore t\u00eb malit Baba shtrihet nj\u00eb shtres\u00eb rajonal, ose zon\u00eb , i cili n\u00eb vende \u00ebsht\u00eb i gjer\u00eb deri n\u00eb 1000 m i gjer\u00eb. dhe karakterizohet nga defektet tektonike. Kjo zon\u00eb e defektit fillon nga Pellgu i Presp\u00ebs, pastaj kalon n\u00ebp\u00ebr fshatin Kazani n\u00eb fshatin Trnovo nga per\u00ebndimi n\u00eb lindje. Nga Trnovo kthehet n\u00eb juglindje dhe n\u00eb at\u00eb drejtim l\u00ebviz n\u00eb fshatin Krstoar, m\u00eb tej kthehet n\u00eb jug dhe l\u00ebviz p\u00ebrgjat\u00eb korniz\u00ebs lindore t\u00eb malit Baba, n\u00eb kufirin shtet\u00ebror me Republik\u00ebn e Greqis\u00eb, nga ku kthehet p\u00ebrs\u00ebri n\u00eb juglindje. Kjo shtres\u00eb\u00a0 n\u00eb an\u00ebn veriore predispozonte kresht\u00ebn asimetrike Gjavato, dhe n\u00eb an\u00ebn lindore Lugin\u00ebn e Pelagonis\u00eb. Nj\u00eb shtres\u00eb rajonale shkon p\u00ebrgjat\u00eb korniz\u00ebs per\u00ebndimore t\u00eb Malit t\u00eb Bab\u00ebs, i cili predispozonte Lugin\u00ebn e Presp\u00ebs. Sot, kjo shtres\u00eb \u00ebsht\u00eb e mbuluar me material kuaternar (fluvio-periglacial dhe deluvial), duke e b\u00ebr\u00eb t\u00eb v\u00ebshtir\u00eb p\u00ebr gjurmimin.<\/p>\n<p>Sinklina e Lart\u00eb Chuka \u00ebsht\u00eb nj\u00eb struktur\u00eb e madhe, e nd\u00ebrtuar me argjil\u00eb t\u00eb gjelb\u00ebrt, argjil\u00eb kuarci, kuarcite, graniti, gabbro, diabaza dhe ryolite. N\u00eb pjes\u00ebn verilindore t\u00eb struktur\u00ebs jan\u00eb zhvilluar dy beteja sekondare horizontale, boshtet e t\u00eb cilave kan\u00eb nj\u00eb drejtim zgjatjeje n\u00eb veriper\u00ebndim &#8211; juglindje.<\/p>\n<p>Struktura m\u00eb e madhe sekondare n\u00eb mal \u00ebsht\u00eb Antiklina e Pelisterit. \u00cbsht\u00eb e p\u00ebrb\u00ebr\u00eb nga kuarcitet, shistrat kuarc, granit, granodioritet, gabbro dhe diabazat. Ka nj\u00eb form\u00eb asimetrike me nj\u00eb krah lindor shum\u00eb m\u00eb t\u00eb theksuar. Pjesa veriore e krahut lindor formon nj\u00eb monoklin, e cila bje n\u00eb m\u00ebnyr\u00eb t\u00eb pjerr\u00ebt n\u00eb veri.<\/p>\n<p>P\u00ebrgjat\u00eb lugin\u00ebs s\u00eb lumit Braj\u00e7inska ndodhet antiklina Braj\u00e7inska, boshti i s\u00eb cil\u00ebs \u00ebsht\u00eb t\u00ebrthor n\u00eb boshtin e antiklin\u00ebs Pelister.<\/p>\n<p>Disa l\u00ebnd\u00eb t\u00eb para minerale metalike (Fe, Mn, Cu, Pb, Zn) dhe jo metalike (asbest, feldspar, kaolin, kuarc, dolerite) jan\u00eb gjetur gjithashtu n\u00eb Malin Baba.<\/p>","protected":false},"featured_media":510,"template":"","_links":{"self":[{"href":"https:\/\/park-pelister.com\/sq\/wp-json\/wp\/v2\/geomorphologies\/537"}],"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\/510"}],"wp:attachment":[{"href":"https:\/\/park-pelister.com\/sq\/wp-json\/wp\/v2\/media?parent=537"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}