{"id":34318,"date":"2019-06-05T07:18:50","date_gmt":"2019-06-05T05:18:50","guid":{"rendered":"https:\/\/pmza.sk\/?p=34318"},"modified":"2019-06-05T07:18:50","modified_gmt":"2019-06-05T05:18:50","slug":"sedimentarne-horniny","status":"publish","type":"post","link":"https:\/\/pmza.sk\/?p=34318","title":{"rendered":"Predmet mesiaca: sediment\u00e1rne horniny"},"content":{"rendered":"<p>Sediment\u00e1rne horniny s\u00fa najroz\u0161\u00edrenej\u0161\u00edmi horninami na zemskom povrchu. Vznikali predov\u0161etk\u00fdm v\u00a0moriach usadzovan\u00edm r\u00f4zne ve\u013ek\u00fdch \u010dast\u00edc miner\u00e1lov a\u00a0horn\u00edn. Okrem toho vznikaj\u00fa aj rozru\u0161ovan\u00edm in\u00fdch horn\u00edn alebo usadzovan\u00edm odumret\u00fdch organizmov, respekt\u00edve ich schr\u00e1nok. Samotn\u00fd proces sediment\u00e1cie prebieha v\u00a0\u0161tyroch f\u00e1zach: rozru\u0161ovanie, premiest\u0148ovanie, usadzovanie a\u00a0spevnenie. Syst\u00e9m sediment\u00e1rnych horn\u00edn je zalo\u017een\u00fd na ve\u013ekosti \u010dast\u00edc a\u00a0miery ich spevnenia. Rozozn\u00e1vame pelity, aleurity, psamity a\u00a0psefity. Pelity maj\u00fa ve\u013ekos\u0165 jednotliv\u00fdch zrniek menej ako 0,01mm, aleurity od 0,01 do 0,05 mm, psamity od 0,05 do 2 mm a\u00a0psefity viac ako 2 mm.<\/p>\n<p>V mesiaci j\u00fan v\u00e1m predstavujeme \u00falomkovit\u00e9 usaden\u00e9 horniny.<\/p>\n<p>K\u00a0jemnozrnn\u00fdm \u00falomkovit\u00fdm hornin\u00e1m (Pelity) patr\u00ed <strong>bridlica slienit\u00e1 <\/strong>z\u00a0lokality Rajeck\u00e1 Lesn\u00e1 (orograf. celok Mal\u00e1 Fatra) a\u00a0usaden\u00e1 hornina <strong>bridlica \u00edlovito-pies\u010dit\u00e1<\/strong> z\u00a0lokality Kamenn\u00e1 Poruba (orograf. celok Mal\u00e1 Fatra).<\/p>\n<p>K\u00a0strednozrnn\u00fdm \u00falomkovit\u00fdm hornin\u00e1m (Psamity) zara\u010fujeme <strong>pieskovec<\/strong> poch\u00e1dzaj\u00faci z\u00a0lokality Kras\u0148any (orograf. celok Mal\u00e1 Fatra) \u00a0a\u00a0<strong>pieskovec glaukonick\u00fd<\/strong> z\u00a0lokality Kysuck\u00e9 Nov\u00e9 Mesto (orograf. celok Javorn\u00edky).<\/p>\n<p>K\u00a0hrubozrnn\u00fdm \u00falomkovit\u00fdm hornin\u00e1m (Psefity) rad\u00edme <strong>zlepence<\/strong> z\u00a0lokal\u00edt Kras\u0148any (orograf. celok Mal\u00e1 Fatra) a\u00a0z\u00a0Divinky (orograf. celok Javorn\u00edky). K\u00a0nespevnen\u00fdm patr\u00ed <strong>morsk\u00fd strednozrnn\u00fd piesok<\/strong> \u017eltosivej farby z\u00a0lokality Hel v\u00a0Po\u013esku.<\/p>\n<p><img fetchpriority=\"high\" decoding=\"async\" class=\"aligncenter size-thumbnail wp-image-34320\" src=\"https:\/\/pmza.sk\/wp-content\/uploads\/2019\/06\/IMG_0607-475x300.jpg\" alt=\"\" width=\"475\" height=\"300\" \/><\/p>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Sediment\u00e1rne horniny s\u00fa najroz\u0161\u00edrenej\u0161\u00edmi horninami na zemskom povrchu. Vznikali predov\u0161etk\u00fdm v\u00a0moriach usadzovan\u00edm r\u00f4zne ve\u013ek\u00fdch \u010dast\u00edc miner\u00e1lov a\u00a0horn\u00edn. Okrem toho vznikaj\u00fa aj rozru\u0161ovan\u00edm in\u00fdch horn\u00edn alebo usadzovan\u00edm odumret\u00fdch organizmov, respekt\u00edve ich schr\u00e1nok. Samotn\u00fd proces sediment\u00e1cie prebieha v\u00a0\u0161tyroch f\u00e1zach: rozru\u0161ovanie, premiest\u0148ovanie, usadzovanie a\u00a0spevnenie. Syst\u00e9m sediment\u00e1rnych horn\u00edn je zalo\u017een\u00fd na ve\u013ekosti \u010dast\u00edc a\u00a0miery ich spevnenia. Rozozn\u00e1vame pelity, aleurity, [&hellip;]<\/p>\n","protected":false},"author":2,"featured_media":34319,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"site-sidebar-layout":"default","site-content-layout":"","ast-site-content-layout":"","site-content-style":"default","site-sidebar-style":"default","ast-global-header-display":"","ast-banner-title-visibility":"","ast-main-header-display":"","ast-hfb-above-header-display":"","ast-hfb-below-header-display":"","ast-hfb-mobile-header-display":"","site-post-title":"","ast-breadcrumbs-content":"","ast-featured-img":"","footer-sml-layout":"","theme-transparent-header-meta":"","adv-header-id-meta":"","stick-header-meta":"","header-above-stick-meta":"","header-main-stick-meta":"","header-below-stick-meta":"","astra-migrate-meta-layouts":"default","ast-page-background-enabled":"default","ast-page-background-meta":{"desktop":{"background-color":"var(--ast-global-color-4)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"tablet":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"mobile":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""}},"ast-content-background-meta":{"desktop":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"tablet":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"mobile":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""}},"footnotes":""},"categories":[31],"tags":[],"class_list":["post-34318","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-aktuality"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.4 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>Predmet mesiaca: sediment\u00e1rne horniny - Pova\u017esk\u00e9 m\u00fazeum<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/pmza.sk\/?p=34318\" \/>\n<meta property=\"og:locale\" content=\"sk_SK\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Predmet mesiaca: sediment\u00e1rne horniny - Pova\u017esk\u00e9 m\u00fazeum\" \/>\n<meta property=\"og:description\" content=\"Sediment\u00e1rne horniny s\u00fa najroz\u0161\u00edrenej\u0161\u00edmi horninami na zemskom povrchu. Vznikali predov\u0161etk\u00fdm v\u00a0moriach usadzovan\u00edm r\u00f4zne ve\u013ek\u00fdch \u010dast\u00edc miner\u00e1lov a\u00a0horn\u00edn. Okrem toho vznikaj\u00fa aj rozru\u0161ovan\u00edm in\u00fdch horn\u00edn alebo usadzovan\u00edm odumret\u00fdch organizmov, respekt\u00edve ich schr\u00e1nok. Samotn\u00fd proces sediment\u00e1cie prebieha v\u00a0\u0161tyroch f\u00e1zach: rozru\u0161ovanie, premiest\u0148ovanie, usadzovanie a\u00a0spevnenie. Syst\u00e9m sediment\u00e1rnych horn\u00edn je zalo\u017een\u00fd na ve\u013ekosti \u010dast\u00edc a\u00a0miery ich spevnenia. 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Vznikali predov\u0161etk\u00fdm v\u00a0moriach usadzovan\u00edm r\u00f4zne ve\u013ek\u00fdch \u010dast\u00edc miner\u00e1lov a\u00a0horn\u00edn. Okrem toho vznikaj\u00fa aj rozru\u0161ovan\u00edm in\u00fdch horn\u00edn alebo usadzovan\u00edm odumret\u00fdch organizmov, respekt\u00edve ich schr\u00e1nok. Samotn\u00fd proces sediment\u00e1cie prebieha v\u00a0\u0161tyroch f\u00e1zach: rozru\u0161ovanie, premiest\u0148ovanie, usadzovanie a\u00a0spevnenie. Syst\u00e9m sediment\u00e1rnych horn\u00edn je zalo\u017een\u00fd na ve\u013ekosti \u010dast\u00edc a\u00a0miery ich spevnenia. 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