{"id":9092,"date":"2023-01-17T13:53:36","date_gmt":"2023-01-17T12:53:36","guid":{"rendered":"http:\/\/zavod-parnas.org\/w\/?page_id=9092"},"modified":"2023-01-18T15:35:11","modified_gmt":"2023-01-18T14:35:11","slug":"podrobnejsi-opis-tock-ob-geoloski-poti-v-kobilji-curek-slo-en","status":"publish","type":"page","link":"http:\/\/zavod-parnas.org\/w\/podrobnejsi-opis-tock-ob-geoloski-poti-v-kobilji-curek-slo-en\/","title":{"rendered":"PODROBNEJ\u0160I OPIS TO\u010cK ob Geolo\u0161ki poti v Kobilji curek (slo\/en)"},"content":{"rendered":"\n<p>Geolo\u0161ko pot v Kobilji curek odlikuje izjemna geolo\u0161ka pestrost, na kratki razdalji se zamenja<strong> \u0161est razli\u010dnih kamnin<\/strong>:<\/p>\n\n\n\n<figure class=\"wp-block-image size-large\"><img fetchpriority=\"high\" decoding=\"async\" width=\"630\" height=\"473\" src=\"http:\/\/zavod-parnas.org\/w\/wp-content\/uploads\/2023\/01\/IMG_7959-630x473.jpg\" alt=\"\" class=\"wp-image-9145\" srcset=\"http:\/\/zavod-parnas.org\/w\/wp-content\/uploads\/2023\/01\/IMG_7959-630x473.jpg 630w, http:\/\/zavod-parnas.org\/w\/wp-content\/uploads\/2023\/01\/IMG_7959-300x225.jpg 300w, http:\/\/zavod-parnas.org\/w\/wp-content\/uploads\/2023\/01\/IMG_7959-252x189.jpg 252w, http:\/\/zavod-parnas.org\/w\/wp-content\/uploads\/2023\/01\/IMG_7959-1536x1152.jpg 1536w, http:\/\/zavod-parnas.org\/w\/wp-content\/uploads\/2023\/01\/IMG_7959.jpg 2048w\" sizes=\"(max-width: 630px) 100vw, 630px\" \/><\/figure>\n\n\n\n<p class=\"has-drop-cap\"><strong>1. PE\u0160\u010cENJAK, MULJEVEC \/sandstone, mudstone<\/strong><\/p>\n\n\n\n<p>Vijoli\u010dno rde\u010da barva sedimentnih kamnin in tal je najve\u010dkrat posledica primesi \u017eeleza oziroma \u017eelezovih mineralov, predvsem hematita. Plasti sedimentnih kamnin so bile v \u010dasu nastajanja horizontalne, sedaj pa le redko kje opazujemo vodoravne plasti. Nagnjenost plasti je posledica tektonskih procesov, ob katerih so se plasti nagibale, gubale in prelamljale.<\/p>\n\n\n\n<p><em>The violet red colour comes most often from iron and iron minerals, mostly hematite, that are mixed within the rocs. The layers of sedimentary rocks were in horizontal position when they were formed but now we can only rarely see horizontal layers. Tilting layers are a result of tectonic processes that leaned, folded and fractured horizontal layers.\u00a0<\/em><\/p>\n\n\n\n<figure class=\"wp-block-image size-large\"><img decoding=\"async\" width=\"630\" height=\"473\" src=\"http:\/\/zavod-parnas.org\/w\/wp-content\/uploads\/2023\/01\/IMG_5047-630x473.jpg\" alt=\"\" class=\"wp-image-9147\" srcset=\"http:\/\/zavod-parnas.org\/w\/wp-content\/uploads\/2023\/01\/IMG_5047-630x473.jpg 630w, http:\/\/zavod-parnas.org\/w\/wp-content\/uploads\/2023\/01\/IMG_5047-300x225.jpg 300w, http:\/\/zavod-parnas.org\/w\/wp-content\/uploads\/2023\/01\/IMG_5047-252x189.jpg 252w, http:\/\/zavod-parnas.org\/w\/wp-content\/uploads\/2023\/01\/IMG_5047-1536x1152.jpg 1536w, http:\/\/zavod-parnas.org\/w\/wp-content\/uploads\/2023\/01\/IMG_5047-2048x1536.jpg 2048w\" sizes=\"(max-width: 630px) 100vw, 630px\" \/><\/figure>\n\n\n\n<p class=\"has-drop-cap\"><strong>2. TUF\u00a0 \/ tuff, volcanic rock<\/strong><\/p>\n\n\n\n<p>Trdoto in ostrino tufa so poznali \u017ee v starej\u0161i kameni dobi. Tedaj so iz tufa izdelovali razli\u010dna primitivna orodja: strgala, no\u017ee, svedre in drugo. Poleg ro\u017eenca je tuf najpogostej\u0161a kamnina, ki jo je pra\u010dlovek uporabljal na na\u0161em prostoru.<\/p>\n\n\n\n<p><em>Because of this characteristics it was used by people already in the Early Stone Age. It was used for tools, such as scrapers, knives, drills and others. Tuff and chert were the two most often used stones by early men in the area.<\/em><\/p>\n\n\n\n<figure class=\"wp-block-image size-large\"><img decoding=\"async\" width=\"630\" height=\"473\" src=\"http:\/\/zavod-parnas.org\/w\/wp-content\/uploads\/2023\/01\/IMG_9526-630x473.jpg\" alt=\"\" class=\"wp-image-9148\" srcset=\"http:\/\/zavod-parnas.org\/w\/wp-content\/uploads\/2023\/01\/IMG_9526-630x473.jpg 630w, http:\/\/zavod-parnas.org\/w\/wp-content\/uploads\/2023\/01\/IMG_9526-300x225.jpg 300w, http:\/\/zavod-parnas.org\/w\/wp-content\/uploads\/2023\/01\/IMG_9526-252x189.jpg 252w, http:\/\/zavod-parnas.org\/w\/wp-content\/uploads\/2023\/01\/IMG_9526-1536x1152.jpg 1536w, http:\/\/zavod-parnas.org\/w\/wp-content\/uploads\/2023\/01\/IMG_9526-2048x1536.jpg 2048w\" sizes=\"(max-width: 630px) 100vw, 630px\" \/><\/figure>\n\n\n\n<p class=\"has-drop-cap\"><strong>3. \u010cRNI PLASTNAT APNENEC \/layered limestone\u00a0 in<br>5. fosili \/ fossils,<\/strong><\/p>\n\n\n\n<p>Temno siva ali \u010drna barva apnenca (in tudi dolomita) je obi\u010dajno posledica prisotnosti humuznih snovi ali bitumna. \u017de majhna koli\u010dina (manj kot 1 %) drobno razpr\u0161enega bitumna lahko kamnino obarva povsem \u010drno.<\/p>\n\n\n\n<p>Fosili se obi\u010dajno ne pojavljajo v vseh plasteh neke kamnine. Pogosteje so le v dolo\u010denih plasteh, tam pa jih je zelo veliko. Zato je pri iskanju fosilov potrebna vztrajnost.<\/p>\n\n\n\n<p><em>Limestone or dolomite is coloured dark grey or black when it contains traces of bitumen. Small quantities of bitumen (less then 1 %) of well dispersed bitumen can can colour the rock to black.<\/em><\/p>\n\n\n\n<p><em>Fossils are usually not present in all layers of a rock. They are mostly found in a single layer but then in larger quantities. That is why we have to be persistent when looking for fossils.<\/em><\/p>\n\n\n\n<p><strong>4. beli neplastnat apnenec \/ massive limestone<\/strong><\/p>\n\n\n\n<p>Apnenec je&nbsp; sestavljen iz kalcijevega karbonata, bolj natan\u010dno iz minerala kalcita, kemi\u010dno CaCO3. Raztaplja ga ogljikova kislina, ki nastaja ob reakciji de\u017eevnice z ogljikovim dioksidom.&nbsp; Plastnati apnenec se lepo kroji v ravne plasti, povr\u0161ina neplastnatega pa je nepravilno oblikovana.<\/p>\n\n\n\n<p><em>Limestone is composed of calcium carbonate, more precisely from the mineral calcite (CaCO3). It is soluble in carbonic acid that is formed when rainwater reacts with carbon dioxide. Layered limestone is arranged in level layers, while the surface of masive limestone is irregular.\u00a0<\/em><\/p>\n\n\n\n<figure class=\"wp-block-image size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"630\" height=\"472\" src=\"http:\/\/zavod-parnas.org\/w\/wp-content\/uploads\/2023\/01\/IMG_5077-630x472.jpg\" alt=\"\" class=\"wp-image-9150\" srcset=\"http:\/\/zavod-parnas.org\/w\/wp-content\/uploads\/2023\/01\/IMG_5077-630x472.jpg 630w, http:\/\/zavod-parnas.org\/w\/wp-content\/uploads\/2023\/01\/IMG_5077-300x225.jpg 300w, http:\/\/zavod-parnas.org\/w\/wp-content\/uploads\/2023\/01\/IMG_5077-252x189.jpg 252w, http:\/\/zavod-parnas.org\/w\/wp-content\/uploads\/2023\/01\/IMG_5077-1536x1152.jpg 1536w, http:\/\/zavod-parnas.org\/w\/wp-content\/uploads\/2023\/01\/IMG_5077-2048x1536.jpg 2048w\" sizes=\"(max-width: 630px) 100vw, 630px\" \/><\/figure>\n\n\n\n<p class=\"has-drop-cap\"><strong>6. RIMSKI ZAPORNI ZID (Claustra Alpium Iuliarum) \/ roman deffence system<\/strong><\/p>\n\n\n\n<p>Neplastnat apnenec, ki ga povezuje malta, je glavni gradbeni material, ki so ga Rimljani v 4. stoletju uporabili za gradnjo zapor, ki bi rimski imperij ubranile pred vdori barbarskih plemen. V bli\u017eini je stal obrambni stolp.<\/p>\n\n\n<div class=\"ast-oembed-container \" style=\"height: 100%;\"><iframe title=\"GRADI\u0160\u010cE PRI ROBU - Claustra Alpium Iuliarum\" width=\"500\" height=\"281\" src=\"https:\/\/www.youtube.com\/embed\/f19MmL6T4Vw?feature=oembed\" frameborder=\"0\" allow=\"accelerometer; autoplay; clipboard-write; encrypted-media; gyroscope; picture-in-picture; web-share\" referrerpolicy=\"strict-origin-when-cross-origin\" allowfullscreen><\/iframe><\/div>\n\n\n\n<p><em>Nonlayered limestone plestered with with mortar was the main construction materiale that Romans used for their defence walls that were supposed to protect the Roman Empire against Barbarian tribes. The defence tower stood nearby.\u00a0<\/em><\/p>\n\n\n\n<figure class=\"wp-block-image size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"630\" height=\"473\" src=\"http:\/\/zavod-parnas.org\/w\/wp-content\/uploads\/2023\/01\/IMG_7997-630x473.jpg\" alt=\"\" class=\"wp-image-9151\" srcset=\"http:\/\/zavod-parnas.org\/w\/wp-content\/uploads\/2023\/01\/IMG_7997-630x473.jpg 630w, http:\/\/zavod-parnas.org\/w\/wp-content\/uploads\/2023\/01\/IMG_7997-300x225.jpg 300w, http:\/\/zavod-parnas.org\/w\/wp-content\/uploads\/2023\/01\/IMG_7997-252x189.jpg 252w, http:\/\/zavod-parnas.org\/w\/wp-content\/uploads\/2023\/01\/IMG_7997-1536x1152.jpg 1536w, http:\/\/zavod-parnas.org\/w\/wp-content\/uploads\/2023\/01\/IMG_7997.jpg 2016w\" sizes=\"(max-width: 630px) 100vw, 630px\" \/><\/figure>\n\n\n\n<p class=\"has-drop-cap\"><strong>7. DOLOMIT \/ dolomite<\/strong><\/p>\n\n\n\n<p>Dolomit je tako mineral kot tudi kamnina, sestavljena iz minerala dolomita, ki je kemi\u010dno kalcijevo magnezijev karbonat. Kemi\u010dna razlika med apnencem in dolomitom je razlog, da solna (klorovodikova) kislina apnenec topi, dolomita pa ne. Za preizkus uporabljamo razred\u010deno 10% solno kislino.<\/p>\n\n\n\n<p><em>Dolomite is a mineral and a rockof the same name composed of calcium magnesium carbonate. This chemical difference is the reason why hydrochloric acid dissolves limestone but not dolomite. In field tests, a diluted 10% hydrocloric acid is used.<\/em><\/p>\n\n\n\n<figure class=\"wp-block-image size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"630\" height=\"473\" src=\"http:\/\/zavod-parnas.org\/w\/wp-content\/uploads\/2023\/01\/IMG_7989-630x473.jpg\" alt=\"\" class=\"wp-image-9152\" srcset=\"http:\/\/zavod-parnas.org\/w\/wp-content\/uploads\/2023\/01\/IMG_7989-630x473.jpg 630w, http:\/\/zavod-parnas.org\/w\/wp-content\/uploads\/2023\/01\/IMG_7989-300x225.jpg 300w, http:\/\/zavod-parnas.org\/w\/wp-content\/uploads\/2023\/01\/IMG_7989-252x189.jpg 252w, http:\/\/zavod-parnas.org\/w\/wp-content\/uploads\/2023\/01\/IMG_7989-1536x1152.jpg 1536w, http:\/\/zavod-parnas.org\/w\/wp-content\/uploads\/2023\/01\/IMG_7989.jpg 2016w\" sizes=\"(max-width: 630px) 100vw, 630px\" \/><\/figure>\n\n\n\n<p class=\"has-drop-cap\"><strong>8. SLAP KOBILJI CUREK \/ Kobilji curek waterfall<\/strong><\/p>\n\n\n\n<p>Za gozdni rezervat Kobilji curek (3ha) velja poseben varstveni re\u017eim. Na koncu grape je slap Kobilji curek, najvi\u0161ji slap na Dolenjskem. Slap ima dve stopnji, vsaka je visoka okoli 15 m. V celoti pada preko apnen\u010dastega skalnega roba, ki je nastal ob prelomu. V bli\u017eini je nahajali\u0161\u010de slovenskega endemita kranjskega jegli\u010da Primula carniolica. Cveti od aprila oziroma maja do junija.<\/p>\n\n\n<div class=\"ast-oembed-container \" style=\"height: 100%;\"><iframe title=\"Kobilji curek zgornji slap\" width=\"500\" height=\"281\" src=\"https:\/\/www.youtube.com\/embed\/iA-YSVt8Sbo?feature=oembed\" frameborder=\"0\" allow=\"accelerometer; autoplay; clipboard-write; encrypted-media; gyroscope; picture-in-picture; web-share\" referrerpolicy=\"strict-origin-when-cross-origin\" allowfullscreen><\/iframe><\/div>\n\n\n<div class=\"ast-oembed-container \" style=\"height: 100%;\"><iframe title=\"Kobilji curek spodnji slap\" width=\"500\" height=\"281\" src=\"https:\/\/www.youtube.com\/embed\/IukxoRckWqI?feature=oembed\" frameborder=\"0\" allow=\"accelerometer; autoplay; clipboard-write; encrypted-media; gyroscope; picture-in-picture; web-share\" referrerpolicy=\"strict-origin-when-cross-origin\" allowfullscreen><\/iframe><\/div>\n\n\n\n<p><em>The Kobilji curek forest reserve (3ha) is protected by special regulations. At the and of the valley, there is the Kobilji curek waterfall, the highest waterfall in Dolenjska region. The waterfall has two steps, each about 15 m. tha water falls over limestone rock edge that was formed when rock layers ruptured. Nearby we can find the Slovenian endemic flower, Carniolan Primrose (Primula carniolica). It flowers from April -May to June.\u00a0<\/em><\/p>\n\n\n\n<p class=\"has-drop-cap\"><strong>9. LEHNJAK \/ tufa<\/strong><\/p>\n\n\n\n<p>Lehnjak najve\u010dkrat nastaja ob izvirih. Kemi\u010dno je lehnjak kalcijev karbonat, enako kot apnenec. Nastajanje lehnjaka je obraten proces od raztapljanja apnenca. Za nastanek lehnjaka so obi\u010dajno potrebne vodne rastline, ki spreminjajo kemijsko ravnote\u017eje v izvirski vodi in tako omogo\u010dijo izlo\u010danje lehnjaka.<\/p>\n\n\n\n<p>Tufa forms mostly around water springs. Chemically it is calcium carbonate, the same as limestone. Its formation is a reverse chemical process of limestone dissolution. Usually it needs vegetation to form , because plants change chemical balance in the water and cause tufa to form.<\/p>\n\n\n\n<p><strong>10. MEANDER \/ meander<\/strong><\/p>\n\n\n\n<p>Meander je re\u010dni zavoj oziroma okljuk. Voda v potoku ali reki ima vedno ve\u010djo hitrost in mo\u010d na zunanji strani meandra, zato tam odna\u0161a kamninski material in erodira bre\u017eino. Na notranji strani meandra pa ima potok manj\u0161o mo\u010d, zato tam odlaga svoje naplavine v obliki meandrskega nasipa.<\/p>\n\n\n\n<p><em>Meander is a river bend. The water is always faster and stronger on the outer side of a meander, that is why it erodes the river bank. The stream is weaker on the inner side, that is why it deposits its sediments here.<\/em><\/p>\n\n\n\n<div class=\"wp-block-buttons is-layout-flex wp-block-buttons-is-layout-flex\">\n<div class=\"wp-block-button\"><a class=\"wp-block-button__link\" href=\"http:\/\/zavod-parnas.org\/w\/geoloska-pot-v-kobilji-curek\/\">Nazaj na Geolo\u0161ko pot<\/a><\/div>\n<\/div>\n\n\n\n<p><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Geolo\u0161ko pot v Kobilji curek odlikuje izjemna geolo\u0161ka pestrost, na kratki razdalji se zamenja \u0161est razli\u010dnih kamnin: 1. PE\u0160\u010cENJAK, MULJEVEC [&hellip;]<\/p>\n","protected":false},"author":2,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"site-sidebar-layout":"default","site-content-layout":"","ast-site-content-layout":"default","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-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":"","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-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":"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":""},"mobile":{"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":""}},"footnotes":""},"class_list":["post-9092","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"http:\/\/zavod-parnas.org\/w\/wp-json\/wp\/v2\/pages\/9092","targetHints":{"allow":["GET"]}}],"collection":[{"href":"http:\/\/zavod-parnas.org\/w\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"http:\/\/zavod-parnas.org\/w\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"http:\/\/zavod-parnas.org\/w\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"http:\/\/zavod-parnas.org\/w\/wp-json\/wp\/v2\/comments?post=9092"}],"version-history":[{"count":3,"href":"http:\/\/zavod-parnas.org\/w\/wp-json\/wp\/v2\/pages\/9092\/revisions"}],"predecessor-version":[{"id":9155,"href":"http:\/\/zavod-parnas.org\/w\/wp-json\/wp\/v2\/pages\/9092\/revisions\/9155"}],"wp:attachment":[{"href":"http:\/\/zavod-parnas.org\/w\/wp-json\/wp\/v2\/media?parent=9092"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}