{"id":1559,"date":"2025-05-05T13:39:40","date_gmt":"2025-05-05T12:39:40","guid":{"rendered":"https:\/\/sga.cuni.cz\/?p=1559"},"modified":"2025-11-03T13:41:11","modified_gmt":"2025-11-03T12:41:11","slug":"field-trip-to-the-au-vms-deposit-zlate-hory-czech-republic","status":"publish","type":"post","link":"https:\/\/sga.cuni.cz\/?p=1559","title":{"rendered":"Field Trip to the Au-VMS deposit Zlat\u00e9 Hory, Czech Republic"},"content":{"rendered":"\n<p><strong>Jakub Pt\u00e1\u010dek, SGA Student Chapter Prague<\/strong><\/p>\n\n\n\n<p>At the end of April 2025, the SGA Student Chapter Prague organised another of its many excursions \u2013<br>this time to Zlat\u00e9 Hory (Golden Mountains), located in the northern part of the Jesen\u00edky Mountains.<br>The goal of the excursion was to explore local geological points of interest, including minerals of<br>Alpine paragenesis and those associated with the rock listvenite (\u201ekrupn\u00edk\u201c in Czech). The highlight of<br>the trip was a descent into the Zlat\u00e9 Hory gold mine, where exploration is currently underway on a<br>previously unmined gold-bearing body. Nine chapter members participated in the three-day excursion,<br>on which members Jan Mr\u00e1\u010dek, Jan Kamensk\u00fd, and Michal \u010curda took charge of both the logistical<br>coordination and the provision of expert guidance. The Zlat\u00e9 Hory area geologically belongs to the<br>Variscan orogenic zone of the Bohemian Massif, also known as the Moravo-Silesian Zone. It lies in<br>the highly deformed contact zone between the Keprn\u00edk and Desn\u00e1 units (domes). The area\u2019s geological<br>evolution is highly complex and remains an active subject of scientific discussion.<\/p>\n\n\n\n<p>From a geological perspective, the two units differ significantly and undoubtedly had distinct origins.<br>The Keprn\u00edk Unit is composed primarily of strongly metamorphosed sedimentary and volcanic rocks,<br>such as paragneisses, phyllites, and amphibolites, which are characterised by a high-grade<br>metamorphism typical of the amphibolite facies. In contrast, the younger Desn\u00e1 Unit consists mainly<br>of weakly metamorphosed sediments, including phyllites, schists, and greenschists, corresponding to<br>the greenschist facies. The most widely accepted interpretation suggests that the Keprn\u00edk Unit forms a<br>nappe structure thrust eastward over the (para)autochthonous Desn\u00e1 Unit.<\/p>\n\n\n\n<p>The first stop of the excursion was the locality Sobot\u00edn, known for its well-formed epidote crystals and<br>as a classic site for the preview of Alpine paragenesis minerals. Although previous extensive<br>collecting by mineral enthusiasts has reduced the locality\u2019s productivity, several noteworthy specimens<br>were nevertheless obtained for the collection. The epidote veins at this site were originally discovered<br>by chance during the construction of a road leading to the next stop of the excursion \u2013 the nearby<br>Smr\u010dina quarry. The primary focus at this locality was the rock listvenite, which was historically<br>utilised in local ironworks. In addition to listvenite, collectors can also find talc and small but well-<br>formed magnetite crystals. The final stop of the day was the beryl-bearing pegmatites of St\u0159eleck\u00fd D\u016fl<br>near Mar\u0161\u00edkov and its surroundings. While the pegmatite at St\u0159eleck\u00fd D\u016fl was historically mined<br>primarily for feldspar, the locality is best known for its exceptional beryl crystals, including occasional<br>aquamarine, which could reach lengths of up to 10\u00a0cm.<\/p>\n\n\n\n<p>The second day of the excursion was dedicated entirely to the modern gold mine operated by the state-<br>owned company DIAMO, located in the Zlat\u00e9 Hory ore district. Between 1990 and 1993, underground<br>mining was conducted here, targeting gold hosted in quartz veins alongside pyrite, sphalerite, galena,<br>and other sulfide minerals. Currently, exploration of the deposit is underway in the previously<br>unmined sections of the ore body due to its potential for future extraction. The investigation involves<br>drilling across the old mine adits to estimate the remaining reserves. According to information from<br>DIAMO, as of 2025, approximately 4 tonnes of gold, 500 tonnes of copper, and significant quantities<br>of other commodities, such as zinc, germanium, and gallium, have been identified as potential<br>resources.<\/p>\n\n\n\n<p>Upon arrival at the site, we received comprehensive training and were equipped with all necessary<br>safety gear, including a rescue breathing apparatus. In the mine, we received an overview of the<br>deposit along with a detailed explanation of all activities related to its exploration. They also showed<br>us several quartz veins filled with various sulphides, primarily pyrite and chalcopyrite, that often<\/p>\n\n\n\n<p>contain microscopic grains of gold. Our time underground was, for safety reasons, limited, so the rest<br>of the briefing took place in an outdoor building where DIAMO stores the drill cores from the<br>exploration (Fig. 1). Visiting the mine was an unforgettable experience for all of us, and we are very<br>grateful to Tom\u00e1\u0161 \u017ditn\u00fd, as well as whole DIAMO for making it possible (Fig.\u00a02).<\/p>\n\n\n\n<p>At the end of the second day, we visited the nearby Po\u0161tovn\u00ed \u0161tola adit from the medieval ages (Fig.\u00a03).<br>The earliest records of copper and other ore mining at this site date back to the early 16 th century. This<br>brief stop enriched our geological knowledge with the historical development of mining in the Zlat\u00e9<br>Hory ore district. On the final day, we made one last stop at a marble quarry near the town of Lipov\u00e1,<br>where we learned interesting details about the local marble, its extraction methods, and the<br>reclamation efforts carried out after mining operations.<\/p>\n\n\n\n<figure class=\"wp-block-image size-large\"><a href=\"https:\/\/sga.cuni.cz\/wp-content\/uploads\/2025\/11\/Fig.1-scaled.jpg\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"768\" src=\"https:\/\/sga.cuni.cz\/wp-content\/uploads\/2025\/11\/Fig.1-1024x768.jpg\" alt=\"\" class=\"wp-image-1558\" srcset=\"https:\/\/sga.cuni.cz\/wp-content\/uploads\/2025\/11\/Fig.1-1024x768.jpg 1024w, https:\/\/sga.cuni.cz\/wp-content\/uploads\/2025\/11\/Fig.1-300x225.jpg 300w, https:\/\/sga.cuni.cz\/wp-content\/uploads\/2025\/11\/Fig.1-768x576.jpg 768w, https:\/\/sga.cuni.cz\/wp-content\/uploads\/2025\/11\/Fig.1-1536x1152.jpg 1536w, https:\/\/sga.cuni.cz\/wp-content\/uploads\/2025\/11\/Fig.1-2048x1536.jpg 2048w, https:\/\/sga.cuni.cz\/wp-content\/uploads\/2025\/11\/Fig.1-150x113.jpg 150w, https:\/\/sga.cuni.cz\/wp-content\/uploads\/2025\/11\/Fig.1-200x150.jpg 200w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/a><figcaption class=\"wp-element-caption\">Fig. 1 &#8211; A drill core containing macroscopic grains of gold<\/figcaption><\/figure>\n\n\n\n<figure class=\"wp-block-image size-large\"><a href=\"https:\/\/sga.cuni.cz\/wp-content\/uploads\/2025\/11\/Fig.2-scaled.jpg\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"683\" src=\"https:\/\/sga.cuni.cz\/wp-content\/uploads\/2025\/11\/Fig.2-1024x683.jpg\" alt=\"\" class=\"wp-image-1560\" srcset=\"https:\/\/sga.cuni.cz\/wp-content\/uploads\/2025\/11\/Fig.2-1024x683.jpg 1024w, https:\/\/sga.cuni.cz\/wp-content\/uploads\/2025\/11\/Fig.2-300x200.jpg 300w, https:\/\/sga.cuni.cz\/wp-content\/uploads\/2025\/11\/Fig.2-768x512.jpg 768w, https:\/\/sga.cuni.cz\/wp-content\/uploads\/2025\/11\/Fig.2-1536x1024.jpg 1536w, https:\/\/sga.cuni.cz\/wp-content\/uploads\/2025\/11\/Fig.2-2048x1365.jpg 2048w, https:\/\/sga.cuni.cz\/wp-content\/uploads\/2025\/11\/Fig.2-150x100.jpg 150w, https:\/\/sga.cuni.cz\/wp-content\/uploads\/2025\/11\/Fig.2-225x150.jpg 225w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/a><figcaption class=\"wp-element-caption\">Fig. 2 &#8211; A group photo with our guides from DIAMO<\/figcaption><\/figure>\n\n\n\n<figure class=\"wp-block-image size-large\"><a href=\"https:\/\/sga.cuni.cz\/wp-content\/uploads\/2025\/11\/Fig.3.png\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"683\" src=\"https:\/\/sga.cuni.cz\/wp-content\/uploads\/2025\/11\/Fig.3-1024x683.png\" alt=\"\" class=\"wp-image-1562\" srcset=\"https:\/\/sga.cuni.cz\/wp-content\/uploads\/2025\/11\/Fig.3-1024x683.png 1024w, https:\/\/sga.cuni.cz\/wp-content\/uploads\/2025\/11\/Fig.3-300x200.png 300w, https:\/\/sga.cuni.cz\/wp-content\/uploads\/2025\/11\/Fig.3-768x512.png 768w, https:\/\/sga.cuni.cz\/wp-content\/uploads\/2025\/11\/Fig.3-1536x1024.png 1536w, https:\/\/sga.cuni.cz\/wp-content\/uploads\/2025\/11\/Fig.3-2048x1365.png 2048w, https:\/\/sga.cuni.cz\/wp-content\/uploads\/2025\/11\/Fig.3-150x100.png 150w, https:\/\/sga.cuni.cz\/wp-content\/uploads\/2025\/11\/Fig.3-225x150.png 225w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/a><figcaption class=\"wp-element-caption\">Fig. 3. The Po\u0161tovn\u00ed \u0161tola adit in Zlat\u00e9 Hory<\/figcaption><\/figure>\n\n\n\n<p><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Jakub Pt\u00e1\u010dek, SGA Student Chapter Prague At the end of April 2025, the SGA Student Chapter Prague organised another of its many excursions \u2013this time to Zlat\u00e9 Hory (Golden Mountains), located in the northern part of the Jesen\u00edky Mountains.The goal of the excursion was to explore local geological points of \u2026 <a class=\"continue-reading-link\" href=\"https:\/\/sga.cuni.cz\/?p=1559\"> Continue reading <span class=\"meta-nav\">&rarr; <\/span><\/a><\/p>\n","protected":false},"author":7,"featured_media":0,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"ngg_post_thumbnail":0,"footnotes":""},"categories":[3,6,1,4,7],"tags":[59,22,38,18,21,87],"class_list":["post-1559","post","type-post","status-publish","format-standard","hentry","category-events","category-news","category-nezarazene","category-our-activities","category-significant-chapter-events","tag-deposits","tag-gold","tag-prague","tag-sga","tag-zlate-hory","tag-zlato"],"_links":{"self":[{"href":"https:\/\/sga.cuni.cz\/index.php?rest_route=\/wp\/v2\/posts\/1559","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/sga.cuni.cz\/index.php?rest_route=\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/sga.cuni.cz\/index.php?rest_route=\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/sga.cuni.cz\/index.php?rest_route=\/wp\/v2\/users\/7"}],"replies":[{"embeddable":true,"href":"https:\/\/sga.cuni.cz\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=1559"}],"version-history":[{"count":2,"href":"https:\/\/sga.cuni.cz\/index.php?rest_route=\/wp\/v2\/posts\/1559\/revisions"}],"predecessor-version":[{"id":1564,"href":"https:\/\/sga.cuni.cz\/index.php?rest_route=\/wp\/v2\/posts\/1559\/revisions\/1564"}],"wp:attachment":[{"href":"https:\/\/sga.cuni.cz\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=1559"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/sga.cuni.cz\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=1559"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/sga.cuni.cz\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=1559"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}