{"id":14569,"date":"2023-11-20T13:36:14","date_gmt":"2023-11-20T12:36:14","guid":{"rendered":"https:\/\/www.gorykaczawskie.pl\/leszczyna-basalt-vein\/"},"modified":"2023-11-20T13:36:14","modified_gmt":"2023-11-20T12:36:14","slug":"leszczyna-basalt-vein","status":"publish","type":"post","link":"https:\/\/www.gorykaczawskie.pl\/en\/leszczyna-basalt-vein\/","title":{"rendered":"LESZCZYNA &#8211; BASALT VEIN"},"content":{"rendered":"<p>LESZCZYNA &#8211; BASALT VEIN<\/p>\n<p>The abandonem quarry approx. 700 m to NNW of the asphalt road junction in Leszczyna (next to the mining open-air museum), next to the ruins of the infrastructure of the &#8220;Lena&#8221; Mining Plant.  The southern slopes of the unnamed elevation with a height of 288 meters above sea level. The basalt vein is located near the abandoned premises of the plant.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>LESZCZYNA &#8211; BASALT VEIN The abandonem quarry approx. 700 m to NNW of the asphalt road junction in Leszczyna (next to the mining open-air museum), next to the ruins of the infrastructure of the &#8220;Lena&#8221; Mining Plant. The southern slopes of the unnamed elevation with a height of 288 meters above sea level. The basalt&#8230;<\/p>\n","protected":false},"author":3,"featured_media":0,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"_seopress_titles_title":"","_seopress_titles_desc":"","_seopress_robots_index":"","_seopress_robots_follow":"","_seopress_robots_imageindex":"","_seopress_robots_snippet":"","_seopress_robots_primary_cat":"","_seopress_robots_breadcrumbs":"","_seopress_robots_freeze_modified_date":"","_seopress_robots_custom_modified_date":"","_seopress_robots_canonical":"","_seopress_social_fb_title":"","_seopress_social_fb_desc":"","_seopress_social_fb_img":"","_seopress_social_fb_img_attachment_id":0,"_seopress_social_fb_img_width":0,"_seopress_social_fb_img_height":0,"_seopress_social_twitter_title":"","_seopress_social_twitter_desc":"","_seopress_social_twitter_img":"","_seopress_social_twitter_img_attachment_id":0,"_seopress_social_twitter_img_width":0,"_seopress_social_twitter_img_height":0,"_seopress_redirections_value":"","_seopress_redirections_enabled":"","_seopress_redirections_enabled_regex":"","_seopress_redirections_logged_status":"","_seopress_redirections_param":"","_seopress_redirections_type":0,"_seopress_analysis_target_kw":"","_seopress_news_disabled":"","_seopress_video_disabled":"","_seopress_video":[],"_seopress_pro_schemas_manual":[],"_seopress_pro_rich_snippets_disable_all":"","_seopress_pro_rich_snippets_disable":[],"_seopress_pro_schemas":[],"inline_featured_image":false,"footnotes":""},"categories":[65],"tags":[213,215],"class_list":["post-14569","post","type-post","status-publish","format-standard","category-pozostalosci-dawnego-wulkanizmu","tag-cenozoic-volcanism","tag-igneous-rocks"],"acf":[],"_links":{"self":[{"href":"https:\/\/www.gorykaczawskie.pl\/en\/wp-json\/wp\/v2\/posts\/14569","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.gorykaczawskie.pl\/en\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.gorykaczawskie.pl\/en\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.gorykaczawskie.pl\/en\/wp-json\/wp\/v2\/users\/3"}],"replies":[{"embeddable":true,"href":"https:\/\/www.gorykaczawskie.pl\/en\/wp-json\/wp\/v2\/comments?post=14569"}],"version-history":[{"count":0,"href":"https:\/\/www.gorykaczawskie.pl\/en\/wp-json\/wp\/v2\/posts\/14569\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.gorykaczawskie.pl\/en\/wp-json\/wp\/v2\/media?parent=14569"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.gorykaczawskie.pl\/en\/wp-json\/wp\/v2\/categories?post=14569"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.gorykaczawskie.pl\/en\/wp-json\/wp\/v2\/tags?post=14569"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}