{"id":61620,"date":"2024-09-16T19:41:57","date_gmt":"2024-09-16T17:41:57","guid":{"rendered":"https:\/\/guidevulcanologicheetna.it\/cronologia-delle-eruzioni-recenti-dei-crateri-sommitali-delletna\/"},"modified":"2026-01-17T07:08:10","modified_gmt":"2026-01-17T06:08:10","slug":"chronologie-van-recente-uitbarstingen-van-de-kraters-op-de-top-van-de-etna","status":"publish","type":"post","link":"https:\/\/guidevulcanologicheetna.it\/nl\/chronologie-van-recente-uitbarstingen-van-de-kraters-op-de-top-van-de-etna\/","title":{"rendered":"Chronologie van recente uitbarstingen van de kraters op de top van de Etna"},"content":{"rendered":"

[et_pb_section fb_built=”1″ fullwidth=”on” _builder_version=”4.27.4″ _module_preset=”default” transform_scale=”103%|100%” transform_scale_tablet=”103%|100%” transform_scale_phone=”112%|100%” transform_scale_last_edited=”on|phone” transform_scale_linked=”off” transform_translate_tablet=”” transform_translate_phone=”” transform_translate_last_edited=”on|desktop” transform_rotate_tablet=”” transform_rotate_phone=”” transform_rotate_last_edited=”on|desktop” transform_skew_tablet=”” transform_skew_phone=”” transform_skew_last_edited=”on|desktop” transform_origin_tablet=”” transform_origin_phone=”” transform_origin_last_edited=”on|desktop” transform_styles_last_edited=”on|phone” width=”100%” max_width=”100%” transform_styles_tablet=”” transform_styles_phone=”” global_colors_info=”{}”][et_pb_fullwidth_code _builder_version=”4.27.4″ _module_preset=”default” custom_margin=”|||0px||” global_colors_info=”{}”] Chronologie Etna Uitbarstingen 2024 | Gedetailleerde Tijdlijn van de Centrale Krater<\/title><!-- [et_pb_line_break_holder] --> <meta name=\"description\" content=\"Volledige chronologie van de Etna-uitbarstingen van 14 juni tot 18 augustus 2024. Interactieve tijdlijn van paroxysmale gebeurtenissen van de Centrale Krater, lavafontijnen en Stromboliaanse activiteit met wetenschappelijke INGV-gegevens.\"><!-- [et_pb_line_break_holder] --> <meta name=\"keywords\" content=\"Etna, uitbarstingen 2024, vulkaan, Centrale Krater, Voragine, Bocca Nuova, CNE, lavafontijnen, Stromboliaanse activiteit, INGV, vulkanieten, lavastromen\"><!-- [et_pb_line_break_holder] --> <script type=\"application\/ld+json\"><!-- [et_pb_line_break_holder] -->{<!-- [et_pb_line_break_holder] --> \"@context\": \"https:\/\/schema.org\",<!-- [et_pb_line_break_holder] --> \"@type\": \"Article\",<!-- [et_pb_line_break_holder] --> \"mainEntityOfPage\": {<!-- [et_pb_line_break_holder] --> \"@type\": \"WebPage\",<!-- [et_pb_line_break_holder] --> \"@id\": \"https:\/\/guidevulcanologicheetna.it\/nl\/chronologie-van-recente-uitbarstingen-van-de-kraters-op-de-top-van-de-etna\/\"<!-- [et_pb_line_break_holder] --> },<!-- [et_pb_line_break_holder] --> \"headline\": \"Chronologie van Recente Uitbarstingen van de Kraters op de Top van de Etna\",<!-- [et_pb_line_break_holder] --> \"description\": \"Gedetailleerde chronologie van de paroxysmale sequentie van de Etna van 14 juni tot 18 augustus 2024, met technische analyse van de eruptieve activiteit van de topkraters, lavafontijnen en vulkaniet-kartografie.\",<!-- [et_pb_line_break_holder] --> \"image\": {<!-- [et_pb_line_break_holder] --> \"@type\": \"ImageObject\",<!-- [et_pb_line_break_holder] --> \"url\": \"https:\/\/guidevulcanologicheetna.it\/wp-content\/uploads\/2025\/09\/Cronologia-Eruzioni-Etna-2024.jpg\",<!-- [et_pb_line_break_holder] --> \"width\": 1200,<!-- [et_pb_line_break_holder] --> \"height\": 800,<!-- [et_pb_line_break_holder] --> \"caption\": \"Chronologie van Etna-uitbarstingen 2024\"<!-- [et_pb_line_break_holder] --> },<!-- [et_pb_line_break_holder] --> \"author\": {<!-- [et_pb_line_break_holder] --> \"@type\": \"Organization\",<!-- [et_pb_line_break_holder] --> \"name\": \"Vulkanologische Gidsen Etna Noord\",<!-- [et_pb_line_break_holder] --> \"url\": \"https:\/\/guidevulcanologicheetna.it\/nl\/\"<!-- [et_pb_line_break_holder] --> },<!-- [et_pb_line_break_holder] --> \"publisher\": {<!-- [et_pb_line_break_holder] --> \"@type\": \"Organization\",<!-- [et_pb_line_break_holder] --> \"name\": \"Vulkanologische Gidsen Etna Noord\",<!-- [et_pb_line_break_holder] --> \"logo\": {<!-- [et_pb_line_break_holder] --> \"@type\": \"ImageObject\",<!-- [et_pb_line_break_holder] --> \"url\": \"https:\/\/guidevulcanologicheetna.it\/wp-content\/uploads\/logo.png\"<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --> },<!-- [et_pb_line_break_holder] --> \"datePublished\": \"2024-08-18\",<!-- [et_pb_line_break_holder] --> \"dateModified\": \"2025-09-15\",<!-- [et_pb_line_break_holder] --> \"articleSection\": \"Vulkanologie\",<!-- [et_pb_line_break_holder] --> \"wordCount\": 1200,<!-- [et_pb_line_break_holder] --> \"inLanguage\": \"nl-NL\",<!-- [et_pb_line_break_holder] --> \"about\": [<!-- [et_pb_line_break_holder] --> {<!-- [et_pb_line_break_holder] --> \"@type\": \"Place\",<!-- [et_pb_line_break_holder] --> \"@id\": \"https:\/\/nl.wikipedia.org\/wiki\/Etna\",<!-- [et_pb_line_break_holder] --> \"name\": \"Etna\",<!-- [et_pb_line_break_holder] --> \"description\": \"Actieve vulkaan gelegen op Sicili\u00eb, Itali\u00eb\",<!-- [et_pb_line_break_holder] --> \"geo\": {<!-- [et_pb_line_break_holder] --> \"@type\": \"GeoCoordinates\",<!-- [et_pb_line_break_holder] --> \"latitude\": \"37.7510\",<!-- [et_pb_line_break_holder] --> \"longitude\": \"14.9934\"<!-- [et_pb_line_break_holder] --> },<!-- [et_pb_line_break_holder] --> \"containedInPlace\": {<!-- [et_pb_line_break_holder] --> \"@type\": \"Place\",<!-- [et_pb_line_break_holder] --> \"name\": \"Sicili\u00eb\",<!-- [et_pb_line_break_holder] --> \"containedInPlace\": {<!-- [et_pb_line_break_holder] --> \"@type\": \"Country\",<!-- [et_pb_line_break_holder] --> \"name\": \"Itali\u00eb\"<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --> },<!-- [et_pb_line_break_holder] --> {<!-- [et_pb_line_break_holder] --> \"@type\": \"Event\",<!-- [et_pb_line_break_holder] --> \"name\": \"Etna Paroxysmale Sequentie 2024\",<!-- [et_pb_line_break_holder] --> \"startDate\": \"2024-06-14\",<!-- [et_pb_line_break_holder] --> \"endDate\": \"2024-08-18\",<!-- [et_pb_line_break_holder] --> \"location\": {<!-- [et_pb_line_break_holder] --> \"@type\": \"Place\",<!-- [et_pb_line_break_holder] --> \"name\": \"Topkraters van de Etna\",<!-- [et_pb_line_break_holder] --> \"geo\": {<!-- [et_pb_line_break_holder] --> \"@type\": \"GeoCoordinates\",<!-- [et_pb_line_break_holder] --> \"latitude\": \"37.7510\",<!-- [et_pb_line_break_holder] --> \"longitude\": \"14.9934\"<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --> },<!-- [et_pb_line_break_holder] --> \"description\": \"Intense eruptieve activiteit van de Etna topkraters met lavafontijnen, lavastromen en as-emissies\"<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --> ],<!-- [et_pb_line_break_holder] --> \"mentions\": [<!-- [et_pb_line_break_holder] --> {<!-- [et_pb_line_break_holder] --> \"@type\": \"Place\",<!-- [et_pb_line_break_holder] --> \"name\": \"Centrale Krater (Voragine)\",<!-- [et_pb_line_break_holder] --> \"description\": \"Hoofdkrater en protagonist van de eruptieve sequentie 2024\"<!-- [et_pb_line_break_holder] --> },<!-- [et_pb_line_break_holder] --> {<!-- [et_pb_line_break_holder] --> \"@type\": \"Place\", <!-- [et_pb_line_break_holder] --> \"name\": \"Bocca Nuova\",<!-- [et_pb_line_break_holder] --> \"description\": \"Aangrenzende krater die de initi\u00eble lavastromen herbergde\"<!-- [et_pb_line_break_holder] --> },<!-- [et_pb_line_break_holder] --> {<!-- [et_pb_line_break_holder] --> \"@type\": \"Place\",<!-- [et_pb_line_break_holder] --> \"name\": \"Noordoost Krater\",<!-- [et_pb_line_break_holder] --> \"description\": \"Krater met intermitterende explosieve episodes\"<!-- [et_pb_line_break_holder] --> },<!-- [et_pb_line_break_holder] --> {<!-- [et_pb_line_break_holder] --> \"@type\": \"Place\",<!-- [et_pb_line_break_holder] --> \"name\": \"Catania\",<!-- [et_pb_line_break_holder] --> \"description\": \"Stad getroffen door vulkanische asval\"<!-- [et_pb_line_break_holder] --> },<!-- [et_pb_line_break_holder] --> {<!-- [et_pb_line_break_holder] --> \"@type\": \"Place\",<!-- [et_pb_line_break_holder] --> \"name\": \"Syracuse\", <!-- [et_pb_line_break_holder] --> \"description\": \"Stad bereikt door vulkanische asval\"<!-- [et_pb_line_break_holder] --> },<!-- [et_pb_line_break_holder] --> {<!-- [et_pb_line_break_holder] --> \"@type\": \"Organization\",<!-- [et_pb_line_break_holder] --> \"name\": \"INGV\",<!-- [et_pb_line_break_holder] --> \"description\": \"Nationaal Instituut voor Geofysica en Vulkanologie\"<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --> ],<!-- [et_pb_line_break_holder] --> \"keywords\": [<!-- [et_pb_line_break_holder] --> \"Etna\",<!-- [et_pb_line_break_holder] --> \"vulkaan\",<!-- [et_pb_line_break_holder] --> \"uitbarsting\",<!-- [et_pb_line_break_holder] --> \"2024\",<!-- [et_pb_line_break_holder] --> \"lavafontijnen\",<!-- [et_pb_line_break_holder] --> \"Stromboliaanse activiteit\",<!-- [et_pb_line_break_holder] --> \"topkraters\",<!-- [et_pb_line_break_holder] --> \"Voragine\",<!-- [et_pb_line_break_holder] --> \"Bocca Nuova\",<!-- [et_pb_line_break_holder] --> \"vulkanologie\",<!-- [et_pb_line_break_holder] --> \"Sicili\u00eb\",<!-- [et_pb_line_break_holder] --> \"lavastromen\",<!-- [et_pb_line_break_holder] --> \"vulkanische as\",<!-- [et_pb_line_break_holder] --> \"paroxysme\",<!-- [et_pb_line_break_holder] --> \"vulkanische monitoring\",<!-- [et_pb_line_break_holder] --> \"INGV\"<!-- [et_pb_line_break_holder] --> ],<!-- [et_pb_line_break_holder] --> \"temporalCoverage\": \"2024-06-14\/2024-08-18\",<!-- [et_pb_line_break_holder] --> \"spatialCoverage\": {<!-- [et_pb_line_break_holder] --> \"@type\": \"Place\",<!-- [et_pb_line_break_holder] --> \"name\": \"Etna en omgeving\",<!-- [et_pb_line_break_holder] --> \"geo\": {<!-- [et_pb_line_break_holder] --> \"@type\": \"GeoShape\",<!-- [et_pb_line_break_holder] --> \"box\": \"37.6 14.8 37.8 15.1\"<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --> },<!-- [et_pb_line_break_holder] --> \"genre\": [<!-- [et_pb_line_break_holder] --> \"Wetenschappelijk artikel\",<!-- [et_pb_line_break_holder] --> \"Vulkanologische documentatie\",<!-- [et_pb_line_break_holder] --> \"Wetenschappelijke kroniek\"<!-- [et_pb_line_break_holder] --> ],<!-- [et_pb_line_break_holder] --> \"educationalLevel\": \"Gevorderd\",<!-- [et_pb_line_break_holder] --> \"audience\": {<!-- [et_pb_line_break_holder] --> \"@type\": \"Audience\",<!-- [et_pb_line_break_holder] --> \"audienceType\": [<!-- [et_pb_line_break_holder] --> \"Vulkanologie studenten\",<!-- [et_pb_line_break_holder] --> \"Geologie liefhebbers\",<!-- [et_pb_line_break_holder] --> \"Etna toeristen\",<!-- [et_pb_line_break_holder] --> \"Lokale bevolking\",<!-- [et_pb_line_break_holder] --> \"Wetenschappers\",<!-- [et_pb_line_break_holder] --> \"Onderzoekers\"<!-- [et_pb_line_break_holder] --> ]<!-- [et_pb_line_break_holder] --> },<!-- [et_pb_line_break_holder] --> \"isPartOf\": {<!-- [et_pb_line_break_holder] --> \"@type\": \"Website\",<!-- [et_pb_line_break_holder] --> \"name\": \"Vulkanologische Gidsen Etna Noord\",<!-- [et_pb_line_break_holder] --> \"url\": \"https:\/\/guidevulcanologicheetna.it\/nl\/\"<!-- [et_pb_line_break_holder] --> },<!-- [et_pb_line_break_holder] --> \"mainEntity\": {<!-- [et_pb_line_break_holder] --> \"@type\": \"VolcanicEruption\",<!-- [et_pb_line_break_holder] --> \"name\": \"Etna Topkraters Uitbarsting 2024\",<!-- [et_pb_line_break_holder] --> \"startDate\": \"2024-06-14\",<!-- [et_pb_line_break_holder] --> \"endDate\": \"2024-08-18\",<!-- [et_pb_line_break_holder] --> \"location\": {<!-- [et_pb_line_break_holder] --> \"@type\": \"Volcano\",<!-- [et_pb_line_break_holder] --> \"name\": \"Etna\",<!-- [et_pb_line_break_holder] --> \"geo\": {<!-- [et_pb_line_break_holder] --> \"@type\": \"GeoCoordinates\",<!-- [et_pb_line_break_holder] --> \"latitude\": \"37.7510\",<!-- [et_pb_line_break_holder] --> \"longitude\": \"14.9934\"<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --> },<!-- [et_pb_line_break_holder] --> \"citation\": [<!-- [et_pb_line_break_holder] --> {<!-- [et_pb_line_break_holder] --> \"@type\": \"Organization\",<!-- [et_pb_line_break_holder] --> \"name\": \"INGV - Istituto Nazionale di Geofisica e Vulcanologia\",<!-- [et_pb_line_break_holder] --> \"url\": \"https:\/\/www.ingv.it\"<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --> ],<!-- [et_pb_line_break_holder] --> \"alternativeHeadline\": \"Eruptieve Sequentie van de Etna Topkraters 2024\",<!-- [et_pb_line_break_holder] --> \"abstract\": \"Volledige wetenschappelijke documentatie van de paroxysmale vulkanische activiteit van de Etna tussen juni en augustus 2024, inclusief technische gegevens over lavafontijnen, lavastromen en pyroclastische afzettingen.\",<!-- [et_pb_line_break_holder] --> \"speakable\": {<!-- [et_pb_line_break_holder] --> \"@type\": \"SpeakableSpecification\",<!-- [et_pb_line_break_holder] --> \"cssSelector\": [\"h1\", \".description\"]<!-- [et_pb_line_break_holder] --> },<!-- [et_pb_line_break_holder] --> \"isAccessibleForFree\": true<!-- [et_pb_line_break_holder] -->}<!-- [et_pb_line_break_holder] --><\/script><!-- [et_pb_line_break_holder] --> <\/p>\n<style><!-- [et_pb_line_break_holder] --> * {<!-- [et_pb_line_break_holder] --> margin: 0;<!-- [et_pb_line_break_holder] --> padding: 0;<!-- [et_pb_line_break_holder] --> box-sizing: border-box;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> body {<!-- [et_pb_line_break_holder] --> font-family: 'Georgia', 'Times New Roman', serif;<!-- [et_pb_line_break_holder] --> background: #000000;<!-- [et_pb_line_break_holder] --> color: #ffffff;<!-- [et_pb_line_break_holder] --> line-height: 1.6;<!-- [et_pb_line_break_holder] --> overflow-x: hidden;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .hero-section {<!-- [et_pb_line_break_holder] --> background: #000000;<!-- [et_pb_line_break_holder] --> padding: 40px 0;<!-- [et_pb_line_break_holder] --> text-align: center;<!-- [et_pb_line_break_holder] --> position: relative;<!-- [et_pb_line_break_holder] --> overflow: hidden;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .container {<!-- [et_pb_line_break_holder] --> max-width: 100%;<!-- [et_pb_line_break_holder] --> margin: 0 auto;<!-- [et_pb_line_break_holder] --> padding: 0 15px;<!-- [et_pb_line_break_holder] --> position: relative;<!-- [et_pb_line_break_holder] --> z-index: 2;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> h1 {<!-- [et_pb_line_break_holder] --> font-size: 3rem;<!-- [et_pb_line_break_holder] --> font-weight: 700;<!-- [et_pb_line_break_holder] --> margin-bottom: 30px;<!-- [et_pb_line_break_holder] --> color: #f4d03f;<!-- [et_pb_line_break_holder] --> letter-spacing: 2px;<!-- [et_pb_line_break_holder] --> font-family: 'Georgia', serif;<!-- [et_pb_line_break_holder] --> position: relative;<!-- [et_pb_line_break_holder] --> padding: 30px 20px;<!-- [et_pb_line_break_holder] --> background: #000000;<!-- [et_pb_line_break_holder] --> text-align: center;<!-- [et_pb_line_break_holder] --> border: none !important;<!-- [et_pb_line_break_holder] --> outline: none !important;<!-- [et_pb_line_break_holder] --> box-shadow: none !important;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .subtitle {<!-- [et_pb_line_break_holder] --> font-size: 1.8rem;<!-- [et_pb_line_break_holder] --> color: #ffa500;<!-- [et_pb_line_break_holder] --> margin-bottom: 40px;<!-- [et_pb_line_break_holder] --> font-weight: 300;<!-- [et_pb_line_break_holder] --> font-style: italic;<!-- [et_pb_line_break_holder] --> letter-spacing: 1px;<!-- [et_pb_line_break_holder] --> text-shadow: 2px 2px 4px rgba(0,0,0,0.6);<!-- [et_pb_line_break_holder] --> font-family: 'Georgia', serif;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .intro {<!-- [et_pb_line_break_holder] --> font-size: 1.2rem;<!-- [et_pb_line_break_holder] --> max-width: 800px;<!-- [et_pb_line_break_holder] --> margin: 0 auto 40px;<!-- [et_pb_line_break_holder] --> color: #e0e0e0;<!-- [et_pb_line_break_holder] --> text-shadow: 1px 1px 2px rgba(0,0,0,0.8);<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .photo-hero {<!-- [et_pb_line_break_holder] --> margin: 40px auto;<!-- [et_pb_line_break_holder] --> text-align: center;<!-- [et_pb_line_break_holder] --> max-width: 900px;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .photo-hero img {<!-- [et_pb_line_break_holder] --> width: 100%;<!-- [et_pb_line_break_holder] --> max-width: 100%;<!-- [et_pb_line_break_holder] --> height: auto;<!-- [et_pb_line_break_holder] --> border: 3px solid #ff6b35;<!-- [et_pb_line_break_holder] --> border-radius: 15px;<!-- [et_pb_line_break_holder] --> box-shadow: 0 10px 30px rgba(255, 107, 53, 0.3);<!-- [et_pb_line_break_holder] --> transition: transform 0.3s ease;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .photo-hero img:hover {<!-- [et_pb_line_break_holder] --> transform: scale(1.02);<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .photo-section {<!-- [et_pb_line_break_holder] --> background: #000000;<!-- [et_pb_line_break_holder] --> padding: 40px 0;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .photo-timeline {<!-- [et_pb_line_break_holder] --> margin: 40px auto;<!-- [et_pb_line_break_holder] --> text-align: center;<!-- [et_pb_line_break_holder] --> max-width: 800px;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .photo-timeline img {<!-- [et_pb_line_break_holder] --> width: 100%;<!-- [et_pb_line_break_holder] --> height: auto;<!-- [et_pb_line_break_holder] --> border: 3px solid #dc143c;<!-- [et_pb_line_break_holder] --> border-radius: 15px;<!-- [et_pb_line_break_holder] --> box-shadow: 0 8px 25px rgba(220, 20, 60, 0.3);<!-- [et_pb_line_break_holder] --> transition: transform 0.3s ease;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .photo-timeline img:hover {<!-- [et_pb_line_break_holder] --> transform: scale(1.02);<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .timeline {<!-- [et_pb_line_break_holder] --> padding: 40px 0;<!-- [et_pb_line_break_holder] --> background: #000000;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .section-title {<!-- [et_pb_line_break_holder] --> text-align: center;<!-- [et_pb_line_break_holder] --> font-size: 2.5rem;<!-- [et_pb_line_break_holder] --> margin-bottom: 50px;<!-- [et_pb_line_break_holder] --> color: #ff6b35;<!-- [et_pb_line_break_holder] --> text-shadow: 2px 2px 4px rgba(0,0,0,0.8);<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .timeline-container {<!-- [et_pb_line_break_holder] --> position: relative;<!-- [et_pb_line_break_holder] --> max-width: 1000px;<!-- [et_pb_line_break_holder] --> margin: 0 auto;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .timeline-line {<!-- [et_pb_line_break_holder] --> position: absolute;<!-- [et_pb_line_break_holder] --> left: 50%;<!-- [et_pb_line_break_holder] --> top: 0;<!-- [et_pb_line_break_holder] --> bottom: 0;<!-- [et_pb_line_break_holder] --> width: 4px;<!-- [et_pb_line_break_holder] --> background: linear-gradient(to bottom, #ff6b35, #dc143c, #8b0000);<!-- [et_pb_line_break_holder] --> transform: translateX(-50%);<!-- [et_pb_line_break_holder] --> box-shadow: 0 0 10px rgba(255, 107, 53, 0.5);<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .timeline-item {<!-- [et_pb_line_break_holder] --> position: relative;<!-- [et_pb_line_break_holder] --> margin: 80px 0;<!-- [et_pb_line_break_holder] --> opacity: 0;<!-- [et_pb_line_break_holder] --> animation: fadeInUp 0.8s ease forwards;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .timeline-item:nth-child(odd) {<!-- [et_pb_line_break_holder] --> animation-delay: 0.2s;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .timeline-item:nth-child(even) {<!-- [et_pb_line_break_holder] --> animation-delay: 0.4s;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> @keyframes fadeInUp {<!-- [et_pb_line_break_holder] --> from {<!-- [et_pb_line_break_holder] --> opacity: 0;<!-- [et_pb_line_break_holder] --> transform: translateY(50px);<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --> to {<!-- [et_pb_line_break_holder] --> opacity: 1;<!-- [et_pb_line_break_holder] --> transform: translateY(0);<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .timeline-content {<!-- [et_pb_line_break_holder] --> background: #000000;<!-- [et_pb_line_break_holder] --> border: 2px solid #ff6b35;<!-- [et_pb_line_break_holder] --> border-radius: 15px;<!-- [et_pb_line_break_holder] --> padding: 30px;<!-- [et_pb_line_break_holder] --> width: 45%;<!-- [et_pb_line_break_holder] --> position: relative;<!-- [et_pb_line_break_holder] --> box-shadow: 0 10px 30px rgba(255, 107, 53, 0.3);<!-- [et_pb_line_break_holder] --> backdrop-filter: blur(10px);<!-- [et_pb_line_break_holder] --> transition: all 0.3s ease;<!-- [et_pb_line_break_holder] --> margin-top: 50px;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .timeline-content:hover {<!-- [et_pb_line_break_holder] --> transform: translateY(-5px);<!-- [et_pb_line_break_holder] --> box-shadow: 0 15px 40px rgba(255, 107, 53, 0.3);<!-- [et_pb_line_break_holder] --> border-color: #ffa500;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .timeline-item:nth-child(odd) .timeline-content {<!-- [et_pb_line_break_holder] --> margin-left: 0;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .timeline-item:nth-child(even) .timeline-content {<!-- [et_pb_line_break_holder] --> margin-left: 55%;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .timeline-content::before {<!-- [et_pb_line_break_holder] --> content: '';<!-- [et_pb_line_break_holder] --> position: absolute;<!-- [et_pb_line_break_holder] --> top: 30px;<!-- [et_pb_line_break_holder] --> width: 0;<!-- [et_pb_line_break_holder] --> height: 0;<!-- [et_pb_line_break_holder] --> border: 15px solid transparent;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .timeline-item:nth-child(odd) .timeline-content::before {<!-- [et_pb_line_break_holder] --> right: -30px;<!-- [et_pb_line_break_holder] --> border-left-color: #ff6b35;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .timeline-item:nth-child(even) .timeline-content::before {<!-- [et_pb_line_break_holder] --> left: -30px;<!-- [et_pb_line_break_holder] --> border-right-color: #ff6b35;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .timeline-date {<!-- [et_pb_line_break_holder] --> position: absolute;<!-- [et_pb_line_break_holder] --> left: 50%;<!-- [et_pb_line_break_holder] --> top: 0;<!-- [et_pb_line_break_holder] --> transform: translateX(-50%);<!-- [et_pb_line_break_holder] --> background: linear-gradient(135deg, #ff6b35, #f7931e);<!-- [et_pb_line_break_holder] --> color: #000;<!-- [et_pb_line_break_holder] --> padding: 12px 25px;<!-- [et_pb_line_break_holder] --> border-radius: 25px;<!-- [et_pb_line_break_holder] --> font-weight: bold;<!-- [et_pb_line_break_holder] --> font-size: 1rem;<!-- [et_pb_line_break_holder] --> box-shadow: 0 5px 15px rgba(255, 107, 53, 0.4);<!-- [et_pb_line_break_holder] --> z-index: 10;<!-- [et_pb_line_break_holder] --> white-space: nowrap;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .event-title {<!-- [et_pb_line_break_holder] --> color: #ffa500;<!-- [et_pb_line_break_holder] --> font-size: 1.4rem;<!-- [et_pb_line_break_holder] --> font-weight: bold;<!-- [et_pb_line_break_holder] --> margin-bottom: 15px;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .event-description {<!-- [et_pb_line_break_holder] --> color: #e0e0e0;<!-- [et_pb_line_break_holder] --> line-height: 1.6;<!-- [et_pb_line_break_holder] --> margin-bottom: 15px;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .technical-details {<!-- [et_pb_line_break_holder] --> background: #000000;<!-- [et_pb_line_break_holder] --> border: 1px solid #dc143c;<!-- [et_pb_line_break_holder] --> border-left: 4px solid #ff6b35;<!-- [et_pb_line_break_holder] --> padding: 15px;<!-- [et_pb_line_break_holder] --> margin-top: 15px;<!-- [et_pb_line_break_holder] --> border-radius: 5px;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .technical-details h4 {<!-- [et_pb_line_break_holder] --> color: #ffa500;<!-- [et_pb_line_break_holder] --> margin-bottom: 10px;<!-- [et_pb_line_break_holder] --> font-size: 1.1rem;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .technical-details p {<!-- [et_pb_line_break_holder] --> font-size: 0.95rem;<!-- [et_pb_line_break_holder] --> color: #d0d0d0;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .highlight {<!-- [et_pb_line_break_holder] --> background: linear-gradient(120deg, rgba(255, 107, 53, 0.2) 0%, rgba(247, 147, 30, 0.2) 100%);<!-- [et_pb_line_break_holder] --> padding: 3px 8px;<!-- [et_pb_line_break_holder] --> border-radius: 5px;<!-- [et_pb_line_break_holder] --> font-weight: bold;<!-- [et_pb_line_break_holder] --> color: #ffa500;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .stats-section {<!-- [et_pb_line_break_holder] --> background: #000000;<!-- [et_pb_line_break_holder] --> padding: 40px 0;<!-- [et_pb_line_break_holder] --> border-top: 1px solid #333;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .stats-grid {<!-- [et_pb_line_break_holder] --> display: grid;<!-- [et_pb_line_break_holder] --> grid-template-columns: repeat(auto-fit, minmax(280px, 1fr));<!-- [et_pb_line_break_holder] --> gap: 30px;<!-- [et_pb_line_break_holder] --> margin-top: 40px;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .stat-card {<!-- [et_pb_line_break_holder] --> background: #000000;<!-- [et_pb_line_break_holder] --> border: 2px solid #dc143c;<!-- [et_pb_line_break_holder] --> border-radius: 15px;<!-- [et_pb_line_break_holder] --> padding: 30px;<!-- [et_pb_line_break_holder] --> text-align: center;<!-- [et_pb_line_break_holder] --> transition: all 0.3s ease;<!-- [et_pb_line_break_holder] --> position: relative;<!-- [et_pb_line_break_holder] --> overflow: hidden;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .stat-card::before {<!-- [et_pb_line_break_holder] --> content: '';<!-- [et_pb_line_break_holder] --> position: absolute;<!-- [et_pb_line_break_holder] --> top: 0;<!-- [et_pb_line_break_holder] --> left: -100%;<!-- [et_pb_line_break_holder] --> width: 100%;<!-- [et_pb_line_break_holder] --> height: 100%;<!-- [et_pb_line_break_holder] --> background: linear-gradient(90deg, transparent, rgba(255, 107, 53, 0.3), transparent);<!-- [et_pb_line_break_holder] --> transition: left 0.5s;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .stat-card:hover::before {<!-- [et_pb_line_break_holder] --> left: 100%;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .stat-card:hover {<!-- [et_pb_line_break_holder] --> transform: translateY(-5px);<!-- [et_pb_line_break_holder] --> border-color: #ff6b35;<!-- [et_pb_line_break_holder] --> box-shadow: 0 15px 30px rgba(220, 20, 60, 0.3);<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .stat-number {<!-- [et_pb_line_break_holder] --> font-size: 2.2rem;<!-- [et_pb_line_break_holder] --> font-weight: bold;<!-- [et_pb_line_break_holder] --> color: #ff6b35;<!-- [et_pb_line_break_holder] --> margin-bottom: 10px;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .stat-label {<!-- [et_pb_line_break_holder] --> color: #e0e0e0;<!-- [et_pb_line_break_holder] --> font-size: 1rem;<!-- [et_pb_line_break_holder] --> line-height: 1.3;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .footer {<!-- [et_pb_line_break_holder] --> background: #000000;<!-- [et_pb_line_break_holder] --> padding: 40px 0;<!-- [et_pb_line_break_holder] --> text-align: center;<!-- [et_pb_line_break_holder] --> border-top: 2px solid #ff6b35;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .footer-content {<!-- [et_pb_line_break_holder] --> color: #888;<!-- [et_pb_line_break_holder] --> font-size: 0.9rem;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .footer-highlight {<!-- [et_pb_line_break_holder] --> color: #ff6b35;<!-- [et_pb_line_break_holder] --> font-weight: bold;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .crater-info {<!-- [et_pb_line_break_holder] --> background: #000000;<!-- [et_pb_line_break_holder] --> padding: 30px 0;<!-- [et_pb_line_break_holder] --> border-top: 1px solid #333;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .crater-grid {<!-- [et_pb_line_break_holder] --> display: grid;<!-- [et_pb_line_break_holder] --> grid-template-columns: repeat(auto-fit, minmax(300px, 1fr));<!-- [et_pb_line_break_holder] --> gap: 30px;<!-- [et_pb_line_break_holder] --> margin-top: 30px;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .crater-card {<!-- [et_pb_line_break_holder] --> background: #000000;<!-- [et_pb_line_break_holder] --> border: 1px solid #ff6b35;<!-- [et_pb_line_break_holder] --> border-radius: 10px;<!-- [et_pb_line_break_holder] --> padding: 25px;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .crater-card h3 {<!-- [et_pb_line_break_holder] --> color: #ffa500;<!-- [et_pb_line_break_holder] --> margin-bottom: 15px;<!-- [et_pb_line_break_holder] --> font-size: 1.3rem;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> @media (max-width: 768px) {<!-- [et_pb_line_break_holder] --> h1 {<!-- [et_pb_line_break_holder] --> font-size: 2rem !important;<!-- [et_pb_line_break_holder] --> padding: 20px 15px !important;<!-- [et_pb_line_break_holder] --> letter-spacing: 1px !important;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .subtitle {<!-- [et_pb_line_break_holder] --> font-size: 1.2rem;<!-- [et_pb_line_break_holder] --> margin-bottom: 20px;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .intro {<!-- [et_pb_line_break_holder] --> font-size: 1rem;<!-- [et_pb_line_break_holder] --> padding: 0 10px;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .section-title {<!-- [et_pb_line_break_holder] --> font-size: 1.6rem;<!-- [et_pb_line_break_holder] --> margin-bottom: 30px;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .timeline-line {<!-- [et_pb_line_break_holder] --> left: 20px;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .timeline-content {<!-- [et_pb_line_break_holder] --> width: calc(100% - 60px);<!-- [et_pb_line_break_holder] --> margin-left: 50px !important;<!-- [et_pb_line_break_holder] --> margin-top: 10px !important;<!-- [et_pb_line_break_holder] --> padding: 20px;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .timeline-content::before {<!-- [et_pb_line_break_holder] --> display: none !important;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .timeline-date {<!-- [et_pb_line_break_holder] --> left: 20px;<!-- [et_pb_line_break_holder] --> transform: translateX(0);<!-- [et_pb_line_break_holder] --> position: relative;<!-- [et_pb_line_break_holder] --> margin-bottom: 15px;<!-- [et_pb_line_break_holder] --> font-size: 0.8rem;<!-- [et_pb_line_break_holder] --> padding: 8px 12px;<!-- [et_pb_line_break_holder] --> display: block;<!-- [et_pb_line_break_holder] --> width: fit-content;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .timeline-item {<!-- [et_pb_line_break_holder] --> margin: 30px 0;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .event-title {<!-- [et_pb_line_break_holder] --> font-size: 1.2rem;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .event-description {<!-- [et_pb_line_break_holder] --> font-size: 0.9rem;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .technical-details {<!-- [et_pb_line_break_holder] --> padding: 12px;<!-- [et_pb_line_break_holder] --> margin-top: 10px;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .technical-details h4 {<!-- [et_pb_line_break_holder] --> font-size: 1rem;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .technical-details p {<!-- [et_pb_line_break_holder] --> font-size: 0.85rem;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .stats-grid {<!-- [et_pb_line_break_holder] --> grid-template-columns: 1fr;<!-- [et_pb_line_break_holder] --> gap: 20px;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .stat-card {<!-- [et_pb_line_break_holder] --> padding: 20px;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .stat-number {<!-- [et_pb_line_break_holder] --> font-size: 1.8rem;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .stat-label {<!-- [et_pb_line_break_holder] --> font-size: 0.9rem;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .crater-grid {<!-- [et_pb_line_break_holder] --> grid-template-columns: 1fr;<!-- [et_pb_line_break_holder] --> gap: 20px;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .crater-card {<!-- [et_pb_line_break_holder] --> padding: 20px;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .crater-card h3 {<!-- [et_pb_line_break_holder] --> font-size: 1.1rem;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .hero-section {<!-- [et_pb_line_break_holder] --> padding: 20px 0;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .timeline {<!-- [et_pb_line_break_holder] --> padding: 30px 0;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .crater-info {<!-- [et_pb_line_break_holder] --> padding: 20px 0;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .stats-section {<!-- [et_pb_line_break_holder] --> padding: 30px 0;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .footer {<!-- [et_pb_line_break_holder] --> padding: 20px 0;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .photo-hero, .photo-timeline {<!-- [et_pb_line_break_holder] --> margin: 30px auto;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> @media (max-width: 480px) {<!-- [et_pb_line_break_holder] --> h1 {<!-- [et_pb_line_break_holder] --> font-size: 1.8rem !important;<!-- [et_pb_line_break_holder] --> padding: 15px 10px !important;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .subtitle {<!-- [et_pb_line_break_holder] --> font-size: 1.1rem;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .intro {<!-- [et_pb_line_break_holder] --> font-size: 0.95rem;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .section-title {<!-- [et_pb_line_break_holder] --> font-size: 1.4rem;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .timeline-content {<!-- [et_pb_line_break_holder] --> width: calc(100% - 50px);<!-- [et_pb_line_break_holder] --> margin-left: 40px !important;<!-- [et_pb_line_break_holder] --> padding: 15px;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .timeline-date {<!-- [et_pb_line_break_holder] --> left: 15px;<!-- [et_pb_line_break_holder] --> font-size: 0.75rem;<!-- [et_pb_line_break_holder] --> padding: 6px 10px;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .event-title {<!-- [et_pb_line_break_holder] --> font-size: 1.1rem;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .event-description {<!-- [et_pb_line_break_holder] --> font-size: 0.85rem;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .stat-number {<!-- [et_pb_line_break_holder] --> font-size: 1.6rem;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .stat-label {<!-- [et_pb_line_break_holder] --> font-size: 0.85rem;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .intensity-indicator {<!-- [et_pb_line_break_holder] --> display: inline-block;<!-- [et_pb_line_break_holder] --> width: 12px;<!-- [et_pb_line_break_holder] --> height: 12px;<!-- [et_pb_line_break_holder] --> border-radius: 50%;<!-- [et_pb_line_break_holder] --> margin-right: 8px;<!-- [et_pb_line_break_holder] --> animation: pulse 2s infinite;<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> .intensity-low { background: #ffa500; }<!-- [et_pb_line_break_holder] --> .intensity-medium { background: #ff6b35; }<!-- [et_pb_line_break_holder] --> .intensity-high { background: #dc143c; }<!-- [et_pb_line_break_holder] --> .intensity-extreme { background: #8b0000; }<!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> @keyframes pulse {<!-- [et_pb_line_break_holder] --> 0%, 100% { opacity: 1; }<!-- [et_pb_line_break_holder] --> 50% { opacity: 0.5; }<!-- [et_pb_line_break_holder] --> }<!-- [et_pb_line_break_holder] --> <\/style>\n<p><!-- [et_pb_line_break_holder] --><\/head><!-- [et_pb_line_break_holder] --><body><!-- [et_pb_line_break_holder] --> <\/p>\n<header class=\"hero-section\"><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"container\"><!-- [et_pb_line_break_holder] --> <\/p>\n<h1>Chronologie Etna Uitbarstingen 2024<\/h1>\n<p><!-- [et_pb_line_break_holder] --> <pee class=\"subtitle\">De Paroxysmale Sequentie van de Topkraters van de Etna<\/pee><!-- [et_pb_line_break_holder] --> <pee class=\"intro\"><!-- [et_pb_line_break_holder] --> De Etna, Europa’s meest actieve vulkaan, doorliep een periode van intense eruptieve activiteit <!-- [et_pb_line_break_holder] --> tussen 14 juni en 18 augustus 2024. De Centrale Krater, ook bekend als Voragine (VOR), <!-- [et_pb_line_break_holder] --> speelde een centrale rol in deze eruptieve fase en betrok ook de aangrenzende kraters, <!-- [et_pb_line_break_holder] --> zoals de Bocca Nuova (BN) en de Noordoost Krater (CNE).<!-- [et_pb_line_break_holder] --> <\/pee><!-- [et_pb_line_break_holder] --> <!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"photo-hero\"><!-- [et_pb_line_break_holder] --> <img decoding=\"async\" src=\"https:\/\/guidevulcanologicheetna.it\/wp-content\/uploads\/2025\/09\/Cronologia-Eruzioni-Etna-2024.jpg\" alt=\"Etna 2024\"><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/header>\n<p><!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> <\/p>\n<section class=\"crater-info\"><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"container\"><!-- [et_pb_line_break_holder] --> <\/p>\n<h2 class=\"section-title\">De Protagonist Kraters<\/h2>\n<p><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"crater-grid\"><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"crater-card\"><!-- [et_pb_line_break_holder] --> <\/p>\n<h3>Centrale Krater (Voragine – VOR)<\/h3>\n<p><!-- [et_pb_line_break_holder] --> <pee>De hoofdprotagonist van de eruptieve sequentie van 2024, gekenmerkt door intense lavafontijnen en continue Stromboliaanse activiteit.<\/pee><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"crater-card\"><!-- [et_pb_line_break_holder] --> <\/p>\n<h3>Bocca Nuova (BN)<\/h3>\n<p><!-- [et_pb_line_break_holder] --> <pee>Aangrenzende krater die de aanvankelijke lavastromen herbergde en de evolutie van de meest geavanceerde paroxysmale activiteit meemaakte.<\/pee><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"crater-card\"><!-- [et_pb_line_break_holder] --> <\/p>\n<h3>Noordoost Krater (CNE)<\/h3>\n<p><!-- [et_pb_line_break_holder] --> <pee>Toonde intermitterende explosieve episodes en wierp lithische blokken tot bijna 1 km afstand tijdens de meest intense fasen.<\/pee><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/section>\n<p><!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> <\/p>\n<section class=\"photo-section\"><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"container\"><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"photo-timeline\"><!-- [et_pb_line_break_holder] --> <img decoding=\"async\" src=\"https:\/\/guidevulcanologicheetna.it\/wp-content\/uploads\/2025\/09\/Cronologia-Eruzioni-Etna.png\" alt=\"Etna Kraters\"><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/section>\n<p><!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> <\/p>\n<section class=\"timeline\"><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"container\"><!-- [et_pb_line_break_holder] --> <\/p>\n<h2 class=\"section-title\">Gedetailleerde Tijdlijn van Eruptieve Gebeurtenissen<\/h2>\n<p><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"timeline-container\"><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"timeline-line\"><\/div>\n<p><!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"timeline-item\"><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"timeline-date\">14 Juni 2024<\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"timeline-content\"><!-- [et_pb_line_break_holder] --> <\/p>\n<h3 class=\"event-title\"><!-- [et_pb_line_break_holder] --> <span class=\"intensity-indicator intensity-low\"><\/span><!-- [et_pb_line_break_holder] --> Begin van de Eruptieve Activiteit<!-- [et_pb_line_break_holder] --> <\/h3>\n<p><!-- [et_pb_line_break_holder] --> <pee class=\"event-description\"><!-- [et_pb_line_break_holder] --> De activiteit van de <span class=\"highlight\">Centrale Krater<\/span> begint met een geleidelijke <!-- [et_pb_line_break_holder] --> maar constante toename van de intensiteit en frequentie van Stromboliaanse explosies. Deze explosies <!-- [et_pb_line_break_holder] --> goten lavastromen in de <span class=\"highlight\">Bocca Nuova<\/span>, waarbij de activiteit <!-- [et_pb_line_break_holder] --> gedurende meerdere weken binnen deze krater bleef. <!-- [et_pb_line_break_holder] --> De explosies werden steeds frequenter en krachtiger.<!-- [et_pb_line_break_holder] --> <\/pee><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"timeline-item\"><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"timeline-date\">4 Juli 2024<\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"timeline-content\"><!-- [et_pb_line_break_holder] --> <\/p>\n<h3 class=\"event-title\"><!-- [et_pb_line_break_holder] --> <span class=\"intensity-indicator intensity-medium\"><\/span><!-- [et_pb_line_break_holder] --> Evolutie naar Lavafontijn<!-- [et_pb_line_break_holder] --> <\/h3>\n<p><!-- [et_pb_line_break_holder] --> <pee class=\"event-description\"><!-- [et_pb_line_break_holder] --> Vanaf <span class=\"highlight\">16:15 UTC<\/span> evolueerde de Stromboliaanse activiteit bij de Centrale <!-- [et_pb_line_break_holder] --> Krater (Voragine) naar een lavafontijn, die een eruptieve kolom produceerde <!-- [et_pb_line_break_holder] --> die een hoogte van ongeveer <span class=\"highlight\">4500 meter boven zeeniveau<\/span> bereikte. <!-- [et_pb_line_break_holder] --> De eruptieve kolom breidde zich uit in zuidoostelijke richting en veroorzaakte aanzienlijke asval <!-- [et_pb_line_break_holder] --> op verschillende nederzettingen in het zuidoostelijke gebied van de Etna, tot <!-- [et_pb_line_break_holder] --> <span class=\"highlight\">Syracuse en daarbuiten<\/span>.<!-- [et_pb_line_break_holder] --> <\/pee><!-- [et_pb_line_break_holder] --> <pee class=\"event-description\"><!-- [et_pb_line_break_holder] --> De lavafontijn-activiteit verzwakte geleidelijk tijdens de nacht tussen <!-- [et_pb_line_break_holder] --> 4 en 5 juli en stopte volledig rond <span class=\"highlight\">01:50 UTC op 5 juli<\/span>. <!-- [et_pb_line_break_holder] --> Na het einde van de fontijn zette de Stromboliaanse activiteit zich ongeveer een uur voort <!-- [et_pb_line_break_holder] --> voordat het volledig stopte.<!-- [et_pb_line_break_holder] --> <\/pee><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"timeline-item\"><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"timeline-date\">5-8 Juli 2024<\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"timeline-content\"><!-- [et_pb_line_break_holder] --> <\/p>\n<h3 class=\"event-title\"><!-- [et_pb_line_break_holder] --> <span class=\"intensity-indicator intensity-low\"><\/span><!-- [et_pb_line_break_holder] --> Onderzoek en Kartering van Vulkanieten<!-- [et_pb_line_break_holder] --> <\/h3>\n<p><!-- [et_pb_line_break_holder] --> <pee class=\"event-description\"><!-- [et_pb_line_break_holder] --> Op 5 en 8 juli werden <span class=\"highlight\">drone-onderzoeken<\/span> uitgevoerd <!-- [et_pb_line_break_holder] --> om de vulkanieten van de eruptieve gebeurtenissen van 4 en 7 juli in kaart te brengen en de topografie <!-- [et_pb_line_break_holder] --> van de topkraters bij te werken.<!-- [et_pb_line_break_holder] --> <\/pee><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"technical-details\"><!-- [et_pb_line_break_holder] --> <\/p>\n<h4>Technische Gegevens van de Onderzoeken:<\/h4>\n<p><!-- [et_pb_line_break_holder] --> <pee><strong>Oppervlakte extrakraterische stroom:<\/strong> 0,4 \u00d7 10\u2075 m\u00b2 met volume van ongeveer 1 \u00d7 10\u2075 m\u00b3<\/pee><!-- [et_pb_line_break_holder] --> <pee><strong>Oppervlakte intrakraterische stroom:<\/strong> 0,6 \u00d7 10\u2075 m\u00b2<\/pee><!-- [et_pb_line_break_holder] --> <pee><strong>Oppervlakte proximale pyroclastische afzetting:<\/strong> 0,8 \u00d7 10\u2075 m\u00b2<\/pee><!-- [et_pb_line_break_holder] --> <pee><strong>Hoogte stroomfront (8 juli, 16:00 UTC):<\/strong> 3016 meter b.z.n.<\/pee><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"timeline-item\"><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"timeline-date\">10 Juli 2024<\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"timeline-content\"><!-- [et_pb_line_break_holder] --> <\/p>\n<h3 class=\"event-title\"><!-- [et_pb_line_break_holder] --> <span class=\"intensity-indicator intensity-high\"><\/span><!-- [et_pb_line_break_holder] --> Piek van de Eruptieve Activiteit<!-- [et_pb_line_break_holder] --> <\/h3>\n<p><!-- [et_pb_line_break_holder] --> <pee class=\"event-description\"><!-- [et_pb_line_break_holder] --> De uitbarsting bereikte een nieuwe intensiteitspiek. De lavafontijnen overschreden <!-- [et_pb_line_break_holder] --> <span class=\"highlight\">1000 meter hoogte<\/span> en een eruptieve kolom van as en gassen <!-- [et_pb_line_break_holder] --> steeg tot <span class=\"highlight\">10 kilometer de atmosfeer in<\/span>, wat aanzienlijke overlast veroorzaakte <!-- [et_pb_line_break_holder] --> voor het vliegverkeer, inclusief de <span class=\"highlight\">tijdelijke sluiting van de luchthaven <!-- [et_pb_line_break_holder] --> van Catania<\/span>. De lavastromen bleven oprukken, waarbij vegetatie werd vernietigd <!-- [et_pb_line_break_holder] --> en landbouwgebieden werden bedreigd.<!-- [et_pb_line_break_holder] --> <\/pee><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"timeline-item\"><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"timeline-date\">15 Juli 2024<\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"timeline-content\"><!-- [et_pb_line_break_holder] --> <\/p>\n<h3 class=\"event-title\"><!-- [et_pb_line_break_holder] --> <span class=\"intensity-indicator intensity-medium\"><\/span><!-- [et_pb_line_break_holder] --> Afname van de Activiteit<!-- [et_pb_line_break_holder] --> <\/h3>\n<p><!-- [et_pb_line_break_holder] --> <pee class=\"event-description\"><!-- [et_pb_line_break_holder] --> De eruptieve activiteit van de Centrale Krater begon af te nemen en stopte volledig <!-- [et_pb_line_break_holder] --> rond <span class=\"highlight\">2 uur ’s ochtends<\/span>. In de dagen daarna, v\u00f3\u00f3r de <!-- [et_pb_line_break_holder] --> lavafontijn van 23 juli, hervatte de asemissie, gevolgd door intermitterende Stromboliaanse activiteit. <!-- [et_pb_line_break_holder] --> Deze emissies wezen op een fase van minder intense maar continue activiteit.<!-- [et_pb_line_break_holder] --> <\/pee><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"timeline-item\"><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"timeline-date\">23 Juli 2024<\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"timeline-content\"><!-- [et_pb_line_break_holder] --> <\/p>\n<h3 class=\"event-title\"><!-- [et_pb_line_break_holder] --> <span class=\"intensity-indicator intensity-high\"><\/span><!-- [et_pb_line_break_holder] --> Lavafontijn en Hervatting van Explosies bij CNE<!-- [et_pb_line_break_holder] --> <\/h3>\n<p><!-- [et_pb_line_break_holder] --> <pee class=\"event-description\"><!-- [et_pb_line_break_holder] --> Op de ochtend van 23 juli, na een nacht van intense Stromboliaanse activiteit, begon een nieuwe lavafontijn <!-- [et_pb_line_break_holder] --> rond <span class=\"highlight\">7:45<\/span>. Deze gebeurtenis produceerde <!-- [et_pb_line_break_holder] --> een kolom van gassen en as die aanhield tot <span class=\"highlight\">12:00<\/span>, <!-- [et_pb_line_break_holder] --> om vervolgens geleidelijk af te nemen tot volledig uitgeput.<!-- [et_pb_line_break_holder] --> <\/pee><!-- [et_pb_line_break_holder] --> <pee class=\"event-description\"><!-- [et_pb_line_break_holder] --> Vervolgens, zoals gebeurd na de gebeurtenis van 15 juli, hervatte de <span class=\"highlight\">Noordoost <!-- [et_pb_line_break_holder] --> Krater<\/span> plotselinge explosies, waarbij lithische blokken werden gelanceerd tot <!-- [et_pb_line_break_holder] --> <span class=\"highlight\">bijna 1 km afstand<\/span>.<!-- [et_pb_line_break_holder] --> <\/pee><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"timeline-item\"><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"timeline-date\">25 Juli 2024<\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"timeline-content\"><!-- [et_pb_line_break_holder] --> <\/p>\n<h3 class=\"event-title\"><!-- [et_pb_line_break_holder] --> <span class=\"intensity-indicator intensity-low\"><\/span><!-- [et_pb_line_break_holder] --> Explosies en Asemissies<!-- [et_pb_line_break_holder] --> <\/h3>\n<p><!-- [et_pb_line_break_holder] --> <pee class=\"event-description\"><!-- [et_pb_line_break_holder] --> De eruptieve activiteit ging door met explosies en asemissies zowel vanuit de <!-- [et_pb_line_break_holder] --> <span class=\"highlight\">Voragine<\/span> als, sporadisch, vanuit de <span class=\"highlight\">Noordoost <!-- [et_pb_line_break_holder] --> Krater<\/span>. De uitgestoten as loste op in de atmosfeer zonder grote neerslag <!-- [et_pb_line_break_holder] --> in de omliggende gebieden te veroorzaken.<!-- [et_pb_line_break_holder] --> <\/pee><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"timeline-item\"><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"timeline-date\">5 Augustus 2024<\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"timeline-content\"><!-- [et_pb_line_break_holder] --> <\/p>\n<h3 class=\"event-title\"><!-- [et_pb_line_break_holder] --> <span class=\"intensity-indicator intensity-extreme\"><\/span><!-- [et_pb_line_break_holder] --> De Krachtigste Lavafontijn<!-- [et_pb_line_break_holder] --> <\/h3>\n<p><!-- [et_pb_line_break_holder] --> <pee class=\"event-description\"><!-- [et_pb_line_break_holder] --> De eruptieve activiteit bereikte een nieuw hoogtepunt met <span class=\"highlight\">de krachtigste lavafontijn <!-- [et_pb_line_break_holder] --> van de gehele paroxysmale reeks<\/span>. De gloeiende stralen overschreden <!-- [et_pb_line_break_holder] --> <span class=\"highlight\">2000 meter hoogte boven de kraterrand<\/span>, wat verdere <!-- [et_pb_line_break_holder] --> lavastromen naar de zuidwestelijke en westelijke hellingen veroorzaakte. Deze gebeurtenis markeerde <!-- [et_pb_line_break_holder] --> (tot op dit moment) het meest intense fenomeen van de paroxysmale sequentie.<!-- [et_pb_line_break_holder] --> <\/pee><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"technical-details\"><!-- [et_pb_line_break_holder] --> <\/p>\n<h4>Definitieve Kaart van Vulkanieten (4 augustus 2024):<\/h4>\n<p><!-- [et_pb_line_break_holder] --> <pee>Tijdens de week daarna werd de definitieve kaart van de vulkanieten gerelateerd aan <!-- [et_pb_line_break_holder] --> de eruptieve gebeurtenis van 4 augustus geproduceerd. De kaart werd verkregen door analyse van de beelden in het <!-- [et_pb_line_break_holder] --> thermische infrarood veld die op 4 augustus via drone werden verkregen door het Laboratorium voor Cartografie en Drones, <!-- [et_pb_line_break_holder] --> en de Sentinel-2 satellietbeelden van 9 augustus.<\/pee><!-- [et_pb_line_break_holder] --> <pee><strong>Formatie:<\/strong> Een enkel extrakraterisch lavaveld, onderverdeeld in drie hoofdtakken <!-- [et_pb_line_break_holder] --> die de weg op 3000 meter hoogte op drie verschillende punten kruisten, samen met een extrakraterische reomorfische stroom.<\/pee><!-- [et_pb_line_break_holder] --> <pee><strong>Bereikte minimumhoogtes:<\/strong><\/pee><!-- [et_pb_line_break_holder] --> <pee>\u2022 Weststroom: <strong>2922 m b.z.n.<\/strong> (laagste hoogte)<\/pee><!-- [et_pb_line_break_holder] --> <pee>\u2022 Noordweststroom: <strong>3042 m b.z.n.<\/strong><\/pee><!-- [et_pb_line_break_holder] --> <pee>\u2022 Zuidweststroom: <strong>2988 m b.z.n.<\/strong><\/pee><!-- [et_pb_line_break_holder] --> <pee><strong>Bedekte oppervlakten:<\/strong><\/pee><!-- [et_pb_line_break_holder] --> <pee>\u2022 Extrakraterische stroom: <strong>3,7 \u00d7 10\u2075 m\u00b2<\/strong><\/pee><!-- [et_pb_line_break_holder] --> <pee>\u2022 Reomorfische stroom: <strong>0,7 \u00d7 10\u2075 m\u00b2<\/strong><\/pee><!-- [et_pb_line_break_holder] --> <pee>\u2022 Proximale pyroclastische afzetting: <strong>1,1 \u00d7 10\u2075 m\u00b2<\/strong><\/pee><!-- [et_pb_line_break_holder] --> <pee><strong>Totaal uitgestoten volume:<\/strong> <strong>2,7 \u00d7 10\u2076 m\u00b3<\/strong> (lavastromen + pyroclastische afzetting)<\/pee><!-- [et_pb_line_break_holder] --> <pee><strong>Gemiddelde diktes:<\/strong> 4 meter (extrakraterische en reomorfische stromen), 9 meter (proximale pyroclastische afzettingen)<\/pee><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"timeline-item\"><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"timeline-date\">12-13 Augustus 2024<\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"timeline-content\"><!-- [et_pb_line_break_holder] --> <\/p>\n<h3 class=\"event-title\"><!-- [et_pb_line_break_holder] --> <span class=\"intensity-indicator intensity-medium\"><\/span><!-- [et_pb_line_break_holder] --> Hernieuwde Stromboliaanse Activiteit<!-- [et_pb_line_break_holder] --> <\/h3>\n<p><!-- [et_pb_line_break_holder] --> <pee class=\"event-description\"><!-- [et_pb_line_break_holder] --> Op 12 en 13 augustus werd de Stromboliaanse activiteit van de Centrale Krater <!-- [et_pb_line_break_holder] --> gekenmerkt door het <span class=\"highlight\">lanceren van lavaflarden langs de flanken van de sinterkegel <!-- [et_pb_line_break_holder] --> van de Bocca Nuova<\/span>. Deze activiteit voedde de uitbarsting verder en <!-- [et_pb_line_break_holder] --> bereidde de grond voor voor een nieuwe paroxysmale episode.<!-- [et_pb_line_break_holder] --> <\/pee><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"timeline-item\"><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"timeline-date\">14-15 Augustus 2024<\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"timeline-content\"><!-- [et_pb_line_break_holder] --> <\/p>\n<h3 class=\"event-title\"><!-- [et_pb_line_break_holder] --> <span class=\"intensity-indicator intensity-high\"><\/span><!-- [et_pb_line_break_holder] --> Laatste Paroxysmale Gebeurtenis<!-- [et_pb_line_break_holder] --> <\/h3>\n<p><!-- [et_pb_line_break_holder] --> <pee class=\"event-description\"><!-- [et_pb_line_break_holder] --> In de middag van 14 augustus, rond <span class=\"highlight\">18:00 UTC<\/span>, werd een <!-- [et_pb_line_break_holder] --> intensivering van de Stromboliaanse activiteit waargenomen, die geleidelijk evolueerde naar een lavafontijn <!-- [et_pb_line_break_holder] --> vanaf <span class=\"highlight\">22:30 UTC<\/span>. Tijdens deze fase werden lavastromen geproduceerd <!-- [et_pb_line_break_holder] --> die de westelijke rand van de Bocca Nuova overschreden en gedeeltelijk overlapten <!-- [et_pb_line_break_holder] --> met het lavaveld dat op 5 augustus was gevormd.<!-- [et_pb_line_break_holder] --> <\/pee><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"timeline-item\"><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"timeline-date\">18 Augustus 2024<\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"timeline-content\"><!-- [et_pb_line_break_holder] --> <\/p>\n<h3 class=\"event-title\"><!-- [et_pb_line_break_holder] --> <span class=\"intensity-indicator intensity-low\"><\/span><!-- [et_pb_line_break_holder] --> Explosies bij Bocca Nuova – Einde van de Cyclus<!-- [et_pb_line_break_holder] --> <\/h3>\n<p><!-- [et_pb_line_break_holder] --> <pee class=\"event-description\"><!-- [et_pb_line_break_holder] --> In de vroege ochtend van 18 augustus 2024 vonden twee significante explosieve sequenties plaats <!-- [et_pb_line_break_holder] --> bij de <span class=\"highlight\">Bocca Nuova<\/span>. De eerste explosie vond plaats om <!-- [et_pb_line_break_holder] --> <span class=\"highlight\">02:30 UTC<\/span>, gevolgd door een tweede om <span class=\"highlight\">02:59 UTC<\/span>, <!-- [et_pb_line_break_holder] --> beide met een duur van ongeveer <span class=\"highlight\">4-6 minuten<\/span>.<!-- [et_pb_line_break_holder] --> <\/pee><!-- [et_pb_line_break_holder] --> <pee class=\"event-description\"><!-- [et_pb_line_break_holder] --> Deze gebeurtenissen markeerden de laatste significante fase van explosieve activiteit van de Centrale Krater <!-- [et_pb_line_break_holder] --> in de beschouwde periode. We zullen de komende dagen zien of de vulkaan van plan is <!-- [et_pb_line_break_holder] --> de eruptieve activiteiten te hervatten of deze cyclus van episodes te be\u00ebindigen die werden gekenmerkt door <!-- [et_pb_line_break_holder] --> Stromboliaanse activiteit en lavafontijnen.<!-- [et_pb_line_break_holder] --> <\/pee><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/section>\n<p><!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> <\/p>\n<section class=\"photo-section\"><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"container\"><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"photo-timeline\"><!-- [et_pb_line_break_holder] --> <img decoding=\"async\" src=\"https:\/\/guidevulcanologicheetna.it\/wp-content\/uploads\/2025\/09\/Cronologia-Eruzioni-Etna-nord-est.jpg\" alt=\"Etna Noord-Oost\"><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/section>\n<p><!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> <\/p>\n<section class=\"stats-section\"><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"container\"><!-- [et_pb_line_break_holder] --> <\/p>\n<h2 class=\"section-title\">Wetenschappelijke Gegevens en INGV-metingen<\/h2>\n<p><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"stats-grid\"><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"stat-card\"><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"stat-number\">2000m<\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"stat-label\">Maximum Hoogte Lavafontijnen (5 augustus)<\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"stat-card\"><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"stat-number\">10km<\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"stat-label\">Hoogte Eruptieve Kolom (10 juli)<\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"stat-card\"><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"stat-number\">4.5km<\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"stat-label\">Hoogte Eruptieve Kolom Tijdens Gebeurtenis van 4 Juli<\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"stat-card\"><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"stat-number\">2.7\u00d710\u2076m\u00b3<\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"stat-label\">Totaal Volume Uitgestoten Materiaal<\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"stat-card\"><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"stat-number\">3.7\u00d710\u2075m\u00b2<\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"stat-label\">Oppervlakte Bedekt door Extrakraterische Stromen<\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"stat-card\"><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"stat-number\">2922m<\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"stat-label\">Minimum Bereikte Hoogte (Weststroom)<\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"stat-card\"><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"stat-number\">1.1\u00d710\u2075m\u00b2<\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"stat-label\">Oppervlakte Proximale Pyroclastische Afzetting<\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"stat-card\"><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"stat-number\">66 dagen<\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"stat-label\">Totale Duur Eruptieve Sequentie<\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"stat-card\"><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"stat-number\">3 takken<\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"stat-label\">Hoofdtakken van het Lavaveld (4 augustus)<\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"stat-card\"><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"stat-number\">~1km<\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"stat-label\">Maximum Afstand Lithische Blokken (CNE)<\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"stat-card\"><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"stat-number\">9m<\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"stat-label\">Gemiddelde Dikte Pyroclastische Afzettingen<\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"stat-card\"><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"stat-number\">4m<\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"stat-label\">Gemiddelde Dikte Lavastromen<\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/section>\n<p><!-- [et_pb_line_break_holder] --><!-- [et_pb_line_break_holder] --> <\/p>\n<footer class=\"footer\"><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"container\"><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"footer-content\"><!-- [et_pb_line_break_holder] --> <pee><!-- [et_pb_line_break_holder] --> Wetenschappelijke gegevens verstrekt in samenwerking met <!-- [et_pb_line_break_holder] --> <span class=\"footer-highlight\">INGV – Osservatorio Etneo<\/span><!-- [et_pb_line_break_holder] --> <\/pee><!-- [et_pb_line_break_holder] --> <pee style=\"margin-top: 15px;\"><!-- [et_pb_line_break_holder] --> Nederlandse vertaling van vulkanologische documentatie over Etna-activiteit 2024<!-- [et_pb_line_break_holder] --> <\/pee><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/footer>\n<p><!-- [et_pb_line_break_holder] --><\/body><!-- [et_pb_line_break_holder] --><\/html>[\/et_pb_fullwidth_code][\/et_pb_section]<\/p>\n","protected":false},"excerpt":{"rendered":"","protected":false},"author":2,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_et_pb_use_builder":"on","_et_pb_old_content":"<h1 style=\"text-align: center;\">Cronologia delle Eruzioni Recenti del Cratere Centrale dell'Etna (14 giugno - 18 agosto 2024)<\/h1>\r\nL'Etna, il vulcano pi\u00f9 attivo d'Europa, ha attraversato un periodo di intensa attivit\u00e0 eruttiva tra il 14 giugno e il 18 agosto 2024. Il Cratere Centrale, noto anche come Voragine (VOR), ha svolto un ruolo centrale in questa fase eruttiva, coinvolgendo anche i crateri adiacenti, come la Bocca Nuova (BN) e il Cratere di Nord-Est (CNE). Di seguito viene fornita una cronologia dettagliata degli eventi eruttivi.\r\n\r\n14 giugno 2024: Inizio dell'attivit\u00e0 eruttiva\r\n\r\nL'attivit\u00e0 del Cratere Centrale \u00e8 iniziata il 14 giugno 2024, con un incremento graduale ma costante dell'intensit\u00e0 e della frequenza delle esplosioni stromboliane. Queste esplosioni hanno riversato colate di lava all'interno della Bocca Nuova, mantenendo l'attivit\u00e0 confinata all'interno di questo cratere per diverse settimane. Le esplosioni sono diventate sempre pi\u00f9 frequenti e vigorose.\r\n\r\n4 luglio 2024: Evoluzione a fontana di lava\r\n\r\nA partire dalle 16:15 UTC del 4 luglio, l'attivit\u00e0 stromboliana al Cratere Centrale (Voragine) si \u00e8 evoluta in una fontana di lava, producendo una colonna eruttiva che ha raggiunto un'altezza di circa 4500 metri sul livello del mare. La colonna eruttiva si \u00e8 propagata in direzione sud-est, provocando una significativa ricaduta di cenere su diversi abitati dell'area sud-orientale dell'Etna, fino a raggiungere Siracusa e oltre.\r\n\r\nL'attivit\u00e0 della fontana di lava si \u00e8 gradualmente affievolita nel corso della notte tra il 4 e il 5 luglio, cessando del tutto intorno alle 01:50 UTC del 5 luglio. Dopo la fine della fontana, l'attivit\u00e0 stromboliana \u00e8 proseguita per circa un'ora prima di cessare completamente.\r\n\r\n5-8 luglio 2024: Rilievi e mappatura delle vulcaniti\r\n\r\nNei giorni 5 e 8 luglio, sono stati eseguiti rilievi con droni per mappare le vulcaniti degli eventi eruttivi del 4 e del 7 luglio e aggiornare la topografia dei crateri sommitali. I rilievi hanno rivelato che l'area ricoperta dalla colata extracraterica \u00e8 pari a 0,4 x 10^5 m\u00b2, con un volume di circa 1 x 10^5 m\u00b3 (in rosso in Figura 3.1). L'area ricoperta dalla colata intracraterica \u00e8 pari a 0,6 x 10^5 m\u00b2 (in arancione in Figura 3.1), mentre l'area ricoperta dal deposito piroclastico prossimale \u00e8 pari a 0,8 x 10^5 m\u00b2 (in giallo in Figura 3.1). Al giorno 8 luglio, alle 16:00 UTC, la quota del fronte della colata si attestava a 3016 metri s.l.m.\r\n\r\n10 luglio 2024: Picco dell'attivit\u00e0 eruttiva\r\n\r\nIl 10 luglio, l'eruzione ha raggiunto un nuovo picco di intensit\u00e0. Le fontane di lava hanno superato i 1000 metri di altezza e una colonna eruttiva di cenere e gas si \u00e8 elevata fino a 10 chilometri nell'atmosfera, causando disagi significativi al traffico aereo, inclusa la chiusura temporanea dell'aeroporto di Catania. Le colate laviche hanno continuato ad avanzare, distruggendo vegetazione e minacciando aree agricole.\r\n\r\n15 luglio 2024: Diminuzione dell'attivit\u00e0\r\n\r\nIl 15 luglio, l'attivit\u00e0 eruttiva del Cratere Centrale ha iniziato a diminuire, cessando completamente intorno alle 2 del mattino. Nei giorni successivi, prima della fontana di lava del 23 luglio, sono riprese le emissioni di cenere, seguite da un'attivit\u00e0 stromboliana intermittente. Queste emissioni hanno indicato una fase di attivit\u00e0 meno intensa ma continua.\r\n\r\n23 luglio 2024: Fontana di lava e ripresa delle esplosioni al Cratere di Nord-Est\r\n\r\nLa mattina del 23 luglio, dopo una notte di intensa attivit\u00e0 stromboliana, una nuova fontana di lava ha avuto inizio intorno alle 7:45. Questo evento ha prodotto una colonna di gas e ceneri che \u00e8 rimasta sostenuta fino alle 12:00, per poi diminuire gradualmente fino a esaurirsi completamente. Successivamente, come avvenuto dopo l'evento del 15 luglio, il Cratere di Nord-Est ha ripreso le esplosioni improvvise, lanciando blocchi litici a quasi 1 km di distanza.\r\n\r\n25 luglio 2024: Esplosioni ed emissioni di cenere\r\n\r\nIl 25 luglio, l'attivit\u00e0 eruttiva \u00e8 proseguita con esplosioni e emissioni di cenere sia dalla Voragine che, sporadicamente, dal Cratere di Nord-Est. Le ceneri emesse si sono dissolte nell'atmosfera senza causare grosse ricadute nelle aree circostanti.\r\n\r\n5 agosto 2024: La fontana di lava pi\u00f9 potente\r\n\r\nIl 5 agosto, l'attivit\u00e0 eruttiva ha raggiunto un nuovo culmine con la fontana di lava pi\u00f9 potente dell'intera serie parossistica. I getti incandescenti hanno superato i 2000 metri di altezza sopra l'orlo craterico, causando ulteriori colate laviche verso i versanti sud-occidentale e occidentale. Questo evento ha segnato (fino in questo momento) \u00a0il fenomeno pi\u00f9 intenso della sequenza parossistica.\r\n\r\nMappa finale delle vulcaniti dell'evento del 4 agosto 2024\r\n\r\nDurante la settimana successiva, \u00e8 stata prodotta la mappa finale delle vulcaniti relative all'evento eruttivo del 4 agosto. La mappa \u00e8 stata ottenuta analizzando le immagini nel campo dell\u2019infrarosso termico acquisite il 4 agosto tramite drone dal Laboratorio di Cartografia e Droni, e le immagini satellitari Sentinel-2 del 9 agosto. Si \u00e8 formato un unico campo lavico extracraterico, suddiviso in tre bracci principali che hanno attraversato la strada a quota 3000 in tre punti distinti, insieme a una colata reomorfica extracraterica.\r\n\r\nIl flusso lavico che ha raggiunto la quota minima pi\u00f9 bassa \u00e8 quello diretto verso ovest, che si \u00e8 arrestato a 2922 m s.l.m. I flussi diretti verso nord-ovest e sud-ovest hanno invece raggiunto rispettivamente le quote minime di 3042 m e 2988 m s.l.m. L'area totale coperta dalla colata extracraterica \u00e8 stata stimata in circa 3,7 x 10^5 m\u00b2, mentre l'area coperta dalla colata reomorfica \u00e8 di circa 0,7 x 10^5 m\u00b2. L'area coperta dal deposito piroclastico prossimale \u00e8 pari a 1,1 x 10^5 m\u00b2.\r\n\r\nIl volume totale di materiale emesso, tra colate laviche e deposito piroclastico prossimale, \u00e8 stato stimato in circa 2,7 x 10^6 m\u00b3, con spessori medi di 4 metri per le colate extracrateriche e reomorfica, e di 9 metri per i depositi piroclastici prossimali. Questi valori sono stati ottenuti dal confronto dei modelli digitali del terreno estratti dalle immagini acquisite tramite drone, in collaborazione con l'INGV - Osservatorio Etneo.\r\n\r\n12-13 agosto 2024: Rinnovata attivit\u00e0 stromboliana\r\n\r\nNelle giornate del 12 e 13 agosto, l'attivit\u00e0 stromboliana del Cratere Centrale \u00e8 stata caratterizzata dal lancio di brandelli di lava lungo i fianchi del cono di scorie della Bocca Nuova. Questa attivit\u00e0 ha alimentato ulteriormente l'eruzione, preparando il terreno per un nuovo episodio parossistico.\r\n\r\n14-15 agosto 2024: Ultimo evento parossistico\r\n\r\nNel pomeriggio del 14 agosto, intorno alle 18:00 UTC, si \u00e8 osservata un'intensificazione dell'attivit\u00e0 stromboliana, che \u00e8 gradualmente evoluta in una fontana di lava a partire dalle 22:30 UTC. Durante questa fase, sono stati prodotti flussi lavici che hanno oltrepassato l'orlo occidentale della Bocca Nuova, sovrapponendosi in parte al campo lavico formatosi il 5 agosto.\r\n\r\n18 agosto 2024: Esplosioni alla Bocca Nuova\r\n\r\nNella prima mattinata del 18 agosto 2024, si sono verificate due sequenze esplosive significative alla Bocca Nuova. La prima esplosione \u00e8 avvenuta alle 02:30 UTC, seguita da una seconda alle 02:59 UTC, entrambe della durata di circa 4-6 minuti.\r\n\r\nQuesti eventi hanno segnato l'ultima fase significativa di attivit\u00e0 esplosiva del Cratere Centrale nel periodo considerato, staremo a vedere nei prossimi giorni, se il vulcano avr\u00e0 intenzione di riprendere le attivit\u00e0 eruttive o concludere questo ciclo di episodi caratterizzati da attivit\u00e0 stromboliana e fontane di lava.","_et_gb_content_width":"2880","footnotes":""},"categories":[11],"tags":[607,623],"class_list":["post-61620","post","type-post","status-publish","format-standard","hentry","category-non-classifiee","tag-etna-fr","tag-trekking-fr"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.3 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>Chronologie van recente uitbarstingen van de kraters op de top van de Etna - Guide Vulcanologiche Etna Nord<\/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:\/\/guidevulcanologicheetna.it\/nl\/chronologie-van-recente-uitbarstingen-van-de-kraters-op-de-top-van-de-etna\/\" \/>\n<meta property=\"og:locale\" content=\"nl_NL\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Chronologie van recente uitbarstingen van de kraters op de top van de Etna - Guide Vulcanologiche Etna Nord\" \/>\n<meta property=\"og:url\" content=\"https:\/\/guidevulcanologicheetna.it\/nl\/chronologie-van-recente-uitbarstingen-van-de-kraters-op-de-top-van-de-etna\/\" \/>\n<meta property=\"og:site_name\" content=\"Guide Vulcanologiche Etna Nord\" \/>\n<meta property=\"article:publisher\" content=\"https:\/\/www.facebook.com\/guidevulcanologiche\/?ref=ts&amp%3bamp%3bamp%3bfref=ts\" \/>\n<meta property=\"article:published_time\" content=\"2024-09-16T17:41:57+00:00\" \/>\n<meta property=\"article:modified_time\" content=\"2026-01-17T06:08:10+00:00\" \/>\n<meta property=\"og:image\" content=\"https:\/\/guidevulcanologicheetna.it\/wp-content\/uploads\/2025\/09\/Cronologia-Eruzioni-Etna-2024.jpg\" \/>\n<meta name=\"author\" content=\"GuideV\" \/>\n<meta name=\"twitter:card\" content=\"summary_large_image\" \/>\n<meta name=\"twitter:label1\" content=\"Geschreven door\" \/>\n\t<meta name=\"twitter:data1\" content=\"GuideV\" \/>\n\t<meta name=\"twitter:label2\" content=\"Geschatte leestijd\" \/>\n\t<meta name=\"twitter:data2\" content=\"7 minuten\" \/>\n<script type=\"application\/ld+json\" class=\"yoast-schema-graph\">{\"@context\":\"https:\\\/\\\/schema.org\",\"@graph\":[{\"@type\":\"Article\",\"@id\":\"https:\\\/\\\/guidevulcanologicheetna.it\\\/nl\\\/chronologie-van-recente-uitbarstingen-van-de-kraters-op-de-top-van-de-etna\\\/#article\",\"isPartOf\":{\"@id\":\"https:\\\/\\\/guidevulcanologicheetna.it\\\/nl\\\/chronologie-van-recente-uitbarstingen-van-de-kraters-op-de-top-van-de-etna\\\/\"},\"author\":{\"name\":\"GuideV\",\"@id\":\"https:\\\/\\\/guidevulcanologicheetna.it\\\/nl\\\/#\\\/schema\\\/person\\\/100399a111d4a3ff97a15cc8bd91e86f\"},\"headline\":\"Chronologie van recente uitbarstingen van de kraters op de top van de Etna\",\"datePublished\":\"2024-09-16T17:41:57+00:00\",\"dateModified\":\"2026-01-17T06:08:10+00:00\",\"mainEntityOfPage\":{\"@id\":\"https:\\\/\\\/guidevulcanologicheetna.it\\\/nl\\\/chronologie-van-recente-uitbarstingen-van-de-kraters-op-de-top-van-de-etna\\\/\"},\"wordCount\":1178,\"commentCount\":0,\"image\":{\"@id\":\"https:\\\/\\\/guidevulcanologicheetna.it\\\/nl\\\/chronologie-van-recente-uitbarstingen-van-de-kraters-op-de-top-van-de-etna\\\/#primaryimage\"},\"thumbnailUrl\":\"https:\\\/\\\/guidevulcanologicheetna.it\\\/wp-content\\\/uploads\\\/2025\\\/09\\\/Cronologia-Eruzioni-Etna-2024.jpg\",\"keywords\":[\"Etna\",\"Trekking\"],\"articleSection\":[\"Non classifi\u00e9(e)\"],\"inLanguage\":\"nl-NL\",\"potentialAction\":[{\"@type\":\"CommentAction\",\"name\":\"Comment\",\"target\":[\"https:\\\/\\\/guidevulcanologicheetna.it\\\/nl\\\/chronologie-van-recente-uitbarstingen-van-de-kraters-op-de-top-van-de-etna\\\/#respond\"]}]},{\"@type\":\"WebPage\",\"@id\":\"https:\\\/\\\/guidevulcanologicheetna.it\\\/nl\\\/chronologie-van-recente-uitbarstingen-van-de-kraters-op-de-top-van-de-etna\\\/\",\"url\":\"https:\\\/\\\/guidevulcanologicheetna.it\\\/nl\\\/chronologie-van-recente-uitbarstingen-van-de-kraters-op-de-top-van-de-etna\\\/\",\"name\":\"Chronologie van recente uitbarstingen van de kraters op de top van de Etna - Guide Vulcanologiche Etna Nord\",\"isPartOf\":{\"@id\":\"https:\\\/\\\/guidevulcanologicheetna.it\\\/nl\\\/#website\"},\"primaryImageOfPage\":{\"@id\":\"https:\\\/\\\/guidevulcanologicheetna.it\\\/nl\\\/chronologie-van-recente-uitbarstingen-van-de-kraters-op-de-top-van-de-etna\\\/#primaryimage\"},\"image\":{\"@id\":\"https:\\\/\\\/guidevulcanologicheetna.it\\\/nl\\\/chronologie-van-recente-uitbarstingen-van-de-kraters-op-de-top-van-de-etna\\\/#primaryimage\"},\"thumbnailUrl\":\"https:\\\/\\\/guidevulcanologicheetna.it\\\/wp-content\\\/uploads\\\/2025\\\/09\\\/Cronologia-Eruzioni-Etna-2024.jpg\",\"datePublished\":\"2024-09-16T17:41:57+00:00\",\"dateModified\":\"2026-01-17T06:08:10+00:00\",\"author\":{\"@id\":\"https:\\\/\\\/guidevulcanologicheetna.it\\\/nl\\\/#\\\/schema\\\/person\\\/100399a111d4a3ff97a15cc8bd91e86f\"},\"breadcrumb\":{\"@id\":\"https:\\\/\\\/guidevulcanologicheetna.it\\\/nl\\\/chronologie-van-recente-uitbarstingen-van-de-kraters-op-de-top-van-de-etna\\\/#breadcrumb\"},\"inLanguage\":\"nl-NL\",\"potentialAction\":[{\"@type\":\"ReadAction\",\"target\":[\"https:\\\/\\\/guidevulcanologicheetna.it\\\/nl\\\/chronologie-van-recente-uitbarstingen-van-de-kraters-op-de-top-van-de-etna\\\/\"]}]},{\"@type\":\"ImageObject\",\"inLanguage\":\"nl-NL\",\"@id\":\"https:\\\/\\\/guidevulcanologicheetna.it\\\/nl\\\/chronologie-van-recente-uitbarstingen-van-de-kraters-op-de-top-van-de-etna\\\/#primaryimage\",\"url\":\"https:\\\/\\\/guidevulcanologicheetna.it\\\/wp-content\\\/uploads\\\/2025\\\/09\\\/Cronologia-Eruzioni-Etna-2024.jpg\",\"contentUrl\":\"https:\\\/\\\/guidevulcanologicheetna.it\\\/wp-content\\\/uploads\\\/2025\\\/09\\\/Cronologia-Eruzioni-Etna-2024.jpg\"},{\"@type\":\"BreadcrumbList\",\"@id\":\"https:\\\/\\\/guidevulcanologicheetna.it\\\/nl\\\/chronologie-van-recente-uitbarstingen-van-de-kraters-op-de-top-van-de-etna\\\/#breadcrumb\",\"itemListElement\":[{\"@type\":\"ListItem\",\"position\":1,\"name\":\"Home\",\"item\":\"https:\\\/\\\/guidevulcanologicheetna.it\\\/nl\\\/\"},{\"@type\":\"ListItem\",\"position\":2,\"name\":\"Chronologie van recente uitbarstingen van de kraters op de top van de Etna\"}]},{\"@type\":\"WebSite\",\"@id\":\"https:\\\/\\\/guidevulcanologicheetna.it\\\/nl\\\/#website\",\"url\":\"https:\\\/\\\/guidevulcanologicheetna.it\\\/nl\\\/\",\"name\":\"Guide Vulcanologiche Etna Nord\",\"description\":\"Guide Etna Abilitate\",\"potentialAction\":[{\"@type\":\"SearchAction\",\"target\":{\"@type\":\"EntryPoint\",\"urlTemplate\":\"https:\\\/\\\/guidevulcanologicheetna.it\\\/nl\\\/?s={search_term_string}\"},\"query-input\":{\"@type\":\"PropertyValueSpecification\",\"valueRequired\":true,\"valueName\":\"search_term_string\"}}],\"inLanguage\":\"nl-NL\"},{\"@type\":\"Person\",\"@id\":\"https:\\\/\\\/guidevulcanologicheetna.it\\\/nl\\\/#\\\/schema\\\/person\\\/100399a111d4a3ff97a15cc8bd91e86f\",\"name\":\"GuideV\",\"image\":{\"@type\":\"ImageObject\",\"inLanguage\":\"nl-NL\",\"@id\":\"https:\\\/\\\/secure.gravatar.com\\\/avatar\\\/90bb4feedf91f89b8c0278587564128202b29365bc37ea86a60ca3ef42414475?s=96&d=mm&r=g\",\"url\":\"https:\\\/\\\/secure.gravatar.com\\\/avatar\\\/90bb4feedf91f89b8c0278587564128202b29365bc37ea86a60ca3ef42414475?s=96&d=mm&r=g\",\"contentUrl\":\"https:\\\/\\\/secure.gravatar.com\\\/avatar\\\/90bb4feedf91f89b8c0278587564128202b29365bc37ea86a60ca3ef42414475?s=96&d=mm&r=g\",\"caption\":\"GuideV\"},\"url\":\"https:\\\/\\\/guidevulcanologicheetna.it\\\/nl\\\/author\\\/guidev\\\/\"}]}<\/script>\n<!-- \/ Yoast SEO plugin. -->","yoast_head_json":{"title":"Chronologie van recente uitbarstingen van de kraters op de top van de Etna - Guide Vulcanologiche Etna Nord","robots":{"index":"index","follow":"follow","max-snippet":"max-snippet:-1","max-image-preview":"max-image-preview:large","max-video-preview":"max-video-preview:-1"},"canonical":"https:\/\/guidevulcanologicheetna.it\/nl\/chronologie-van-recente-uitbarstingen-van-de-kraters-op-de-top-van-de-etna\/","og_locale":"nl_NL","og_type":"article","og_title":"Chronologie van recente uitbarstingen van de kraters op de top van de Etna - Guide Vulcanologiche Etna Nord","og_url":"https:\/\/guidevulcanologicheetna.it\/nl\/chronologie-van-recente-uitbarstingen-van-de-kraters-op-de-top-van-de-etna\/","og_site_name":"Guide Vulcanologiche Etna Nord","article_publisher":"https:\/\/www.facebook.com\/guidevulcanologiche\/?ref=ts&%3bamp%3bamp%3bfref=ts","article_published_time":"2024-09-16T17:41:57+00:00","article_modified_time":"2026-01-17T06:08:10+00:00","og_image":[{"url":"https:\/\/guidevulcanologicheetna.it\/wp-content\/uploads\/2025\/09\/Cronologia-Eruzioni-Etna-2024.jpg","type":"","width":"","height":""}],"author":"GuideV","twitter_card":"summary_large_image","twitter_misc":{"Geschreven door":"GuideV","Geschatte leestijd":"7 minuten"},"schema":{"@context":"https:\/\/schema.org","@graph":[{"@type":"Article","@id":"https:\/\/guidevulcanologicheetna.it\/nl\/chronologie-van-recente-uitbarstingen-van-de-kraters-op-de-top-van-de-etna\/#article","isPartOf":{"@id":"https:\/\/guidevulcanologicheetna.it\/nl\/chronologie-van-recente-uitbarstingen-van-de-kraters-op-de-top-van-de-etna\/"},"author":{"name":"GuideV","@id":"https:\/\/guidevulcanologicheetna.it\/nl\/#\/schema\/person\/100399a111d4a3ff97a15cc8bd91e86f"},"headline":"Chronologie van recente uitbarstingen van de kraters op de top van de Etna","datePublished":"2024-09-16T17:41:57+00:00","dateModified":"2026-01-17T06:08:10+00:00","mainEntityOfPage":{"@id":"https:\/\/guidevulcanologicheetna.it\/nl\/chronologie-van-recente-uitbarstingen-van-de-kraters-op-de-top-van-de-etna\/"},"wordCount":1178,"commentCount":0,"image":{"@id":"https:\/\/guidevulcanologicheetna.it\/nl\/chronologie-van-recente-uitbarstingen-van-de-kraters-op-de-top-van-de-etna\/#primaryimage"},"thumbnailUrl":"https:\/\/guidevulcanologicheetna.it\/wp-content\/uploads\/2025\/09\/Cronologia-Eruzioni-Etna-2024.jpg","keywords":["Etna","Trekking"],"articleSection":["Non classifi\u00e9(e)"],"inLanguage":"nl-NL","potentialAction":[{"@type":"CommentAction","name":"Comment","target":["https:\/\/guidevulcanologicheetna.it\/nl\/chronologie-van-recente-uitbarstingen-van-de-kraters-op-de-top-van-de-etna\/#respond"]}]},{"@type":"WebPage","@id":"https:\/\/guidevulcanologicheetna.it\/nl\/chronologie-van-recente-uitbarstingen-van-de-kraters-op-de-top-van-de-etna\/","url":"https:\/\/guidevulcanologicheetna.it\/nl\/chronologie-van-recente-uitbarstingen-van-de-kraters-op-de-top-van-de-etna\/","name":"Chronologie van recente uitbarstingen van de kraters op de top van de Etna - Guide Vulcanologiche Etna Nord","isPartOf":{"@id":"https:\/\/guidevulcanologicheetna.it\/nl\/#website"},"primaryImageOfPage":{"@id":"https:\/\/guidevulcanologicheetna.it\/nl\/chronologie-van-recente-uitbarstingen-van-de-kraters-op-de-top-van-de-etna\/#primaryimage"},"image":{"@id":"https:\/\/guidevulcanologicheetna.it\/nl\/chronologie-van-recente-uitbarstingen-van-de-kraters-op-de-top-van-de-etna\/#primaryimage"},"thumbnailUrl":"https:\/\/guidevulcanologicheetna.it\/wp-content\/uploads\/2025\/09\/Cronologia-Eruzioni-Etna-2024.jpg","datePublished":"2024-09-16T17:41:57+00:00","dateModified":"2026-01-17T06:08:10+00:00","author":{"@id":"https:\/\/guidevulcanologicheetna.it\/nl\/#\/schema\/person\/100399a111d4a3ff97a15cc8bd91e86f"},"breadcrumb":{"@id":"https:\/\/guidevulcanologicheetna.it\/nl\/chronologie-van-recente-uitbarstingen-van-de-kraters-op-de-top-van-de-etna\/#breadcrumb"},"inLanguage":"nl-NL","potentialAction":[{"@type":"ReadAction","target":["https:\/\/guidevulcanologicheetna.it\/nl\/chronologie-van-recente-uitbarstingen-van-de-kraters-op-de-top-van-de-etna\/"]}]},{"@type":"ImageObject","inLanguage":"nl-NL","@id":"https:\/\/guidevulcanologicheetna.it\/nl\/chronologie-van-recente-uitbarstingen-van-de-kraters-op-de-top-van-de-etna\/#primaryimage","url":"https:\/\/guidevulcanologicheetna.it\/wp-content\/uploads\/2025\/09\/Cronologia-Eruzioni-Etna-2024.jpg","contentUrl":"https:\/\/guidevulcanologicheetna.it\/wp-content\/uploads\/2025\/09\/Cronologia-Eruzioni-Etna-2024.jpg"},{"@type":"BreadcrumbList","@id":"https:\/\/guidevulcanologicheetna.it\/nl\/chronologie-van-recente-uitbarstingen-van-de-kraters-op-de-top-van-de-etna\/#breadcrumb","itemListElement":[{"@type":"ListItem","position":1,"name":"Home","item":"https:\/\/guidevulcanologicheetna.it\/nl\/"},{"@type":"ListItem","position":2,"name":"Chronologie van recente uitbarstingen van de kraters op de top van de Etna"}]},{"@type":"WebSite","@id":"https:\/\/guidevulcanologicheetna.it\/nl\/#website","url":"https:\/\/guidevulcanologicheetna.it\/nl\/","name":"Guide Vulcanologiche Etna Nord","description":"Guide Etna Abilitate","potentialAction":[{"@type":"SearchAction","target":{"@type":"EntryPoint","urlTemplate":"https:\/\/guidevulcanologicheetna.it\/nl\/?s={search_term_string}"},"query-input":{"@type":"PropertyValueSpecification","valueRequired":true,"valueName":"search_term_string"}}],"inLanguage":"nl-NL"},{"@type":"Person","@id":"https:\/\/guidevulcanologicheetna.it\/nl\/#\/schema\/person\/100399a111d4a3ff97a15cc8bd91e86f","name":"GuideV","image":{"@type":"ImageObject","inLanguage":"nl-NL","@id":"https:\/\/secure.gravatar.com\/avatar\/90bb4feedf91f89b8c0278587564128202b29365bc37ea86a60ca3ef42414475?s=96&d=mm&r=g","url":"https:\/\/secure.gravatar.com\/avatar\/90bb4feedf91f89b8c0278587564128202b29365bc37ea86a60ca3ef42414475?s=96&d=mm&r=g","contentUrl":"https:\/\/secure.gravatar.com\/avatar\/90bb4feedf91f89b8c0278587564128202b29365bc37ea86a60ca3ef42414475?s=96&d=mm&r=g","caption":"GuideV"},"url":"https:\/\/guidevulcanologicheetna.it\/nl\/author\/guidev\/"}]}},"_links":{"self":[{"href":"https:\/\/guidevulcanologicheetna.it\/nl\/wp-json\/wp\/v2\/posts\/61620","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/guidevulcanologicheetna.it\/nl\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/guidevulcanologicheetna.it\/nl\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/guidevulcanologicheetna.it\/nl\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/guidevulcanologicheetna.it\/nl\/wp-json\/wp\/v2\/comments?post=61620"}],"version-history":[{"count":8,"href":"https:\/\/guidevulcanologicheetna.it\/nl\/wp-json\/wp\/v2\/posts\/61620\/revisions"}],"predecessor-version":[{"id":62203,"href":"https:\/\/guidevulcanologicheetna.it\/nl\/wp-json\/wp\/v2\/posts\/61620\/revisions\/62203"}],"wp:attachment":[{"href":"https:\/\/guidevulcanologicheetna.it\/nl\/wp-json\/wp\/v2\/media?parent=61620"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/guidevulcanologicheetna.it\/nl\/wp-json\/wp\/v2\/categories?post=61620"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/guidevulcanologicheetna.it\/nl\/wp-json\/wp\/v2\/tags?post=61620"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}