{"id":61610,"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":"2025-09-15T11:41:37","modified_gmt":"2025-09-15T09:41:37","slug":"chronologie-der-jungsten-ausbruche-der-gipfelkrater-des-atna","status":"publish","type":"post","link":"https:\/\/guidevulcanologicheetna.it\/de\/chronologie-der-jungsten-ausbruche-der-gipfelkrater-des-atna\/","title":{"rendered":"Chronologie der j\u00fcngsten Ausbr\u00fcche der Gipfelkrater des \u00c4tna"},"content":{"rendered":"

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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 der \u00c4tna-Ausbr\u00fcche 2024<\/h1>\n<p><!-- [et_pb_line_break_holder] --> <pee class=\"subtitle\">Die Paroxysmale Sequenz der Gipfelkrater<\/pee><!-- [et_pb_line_break_holder] --> <pee class=\"intro\"><!-- [et_pb_line_break_holder] --> Der \u00c4tna, Europas aktivster Vulkan, durchlief zwischen dem 14. Juni und 18. August 2024 <!-- [et_pb_line_break_holder] --> eine Periode intensiver Eruptionst\u00e4tigkeit. Der Zentralkrater, auch bekannt als Voragine (VOR), <!-- [et_pb_line_break_holder] --> spielte eine zentrale Rolle in dieser eruptiven Phase und bezog auch die benachbarten Krater <!-- [et_pb_line_break_holder] --> wie Bocca Nuova (BN) und den Nordostkrater (NEC) mit ein.<!-- [et_pb_line_break_holder] --> <\/pee><!-- [et_pb_line_break_holder] --> <!-- [et_pb_line_break_holder] --> <!-- FOTO 1 - Unter dem Titel --><!-- [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=\"\u00c4tna 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\">Die Protagonisten-Krater<\/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>Zentralkrater (Voragine – VOR)<\/h3>\n<p><!-- [et_pb_line_break_holder] --> <pee>Der Hauptprotagonist der eruptiven Sequenz 2024, charakterisiert durch intensive Lavafont\u00e4nen und kontinuierliche strombolianische Aktivit\u00e4t.<\/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>Benachbarter Krater, der die anf\u00e4nglichen Lavastr\u00f6me beherbergte und die Entwicklung der fortgeschrittensten paroxysmalen Aktivit\u00e4t miterlebte.<\/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>Nordostkrater (NEC)<\/h3>\n<p><!-- [et_pb_line_break_holder] --> <pee>Zeigte intermittierende explosive Episoden und schleuderte w\u00e4hrend der intensivsten Phasen lithische Bl\u00f6cke bis zu fast 1 km weit.<\/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] --> <!-- FOTO 2 - Vor der Zeitleiste --><!-- [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=\"\u00c4tna-Krater\"><!-- [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\">Detaillierte Zeitleiste der Eruptiven Ereignisse<\/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] --> Beginn der Eruptiven Aktivit\u00e4t<!-- [et_pb_line_break_holder] --> <\/h3>\n<p><!-- [et_pb_line_break_holder] --> <pee class=\"event-description\"><!-- [et_pb_line_break_holder] --> Die Aktivit\u00e4t des <span class=\"highlight\">Zentralkraters<\/span> beginnt mit einer graduellen, <!-- [et_pb_line_break_holder] --> aber konstanten Zunahme der Intensit\u00e4t und Frequenz strombolianischer Explosionen. Diese Explosionen <!-- [et_pb_line_break_holder] --> ergossen Lavastr\u00f6me in die <span class=\"highlight\">Bocca Nuova<\/span> und hielten die Aktivit\u00e4t <!-- [et_pb_line_break_holder] --> mehrere Wochen lang in diesem Krater eingeschlossen. <!-- [et_pb_line_break_holder] --> Die Explosionen wurden zunehmend h\u00e4ufiger und kr\u00e4ftiger.<!-- [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] --> Entwicklung zur Lavafont\u00e4ne<!-- [et_pb_line_break_holder] --> <\/h3>\n<p><!-- [et_pb_line_break_holder] --> <pee class=\"event-description\"><!-- [et_pb_line_break_holder] --> Ab <span class=\"highlight\">16:15 UTC<\/span> entwickelte sich die strombolianische Aktivit\u00e4t am Zentralkrater <!-- [et_pb_line_break_holder] --> (Voragine) zu einer Lavafont\u00e4ne, die eine eruptive S\u00e4ule erzeugte, <!-- [et_pb_line_break_holder] --> die eine H\u00f6he von etwa <span class=\"highlight\">4.500 Metern \u00fcber dem Meeresspiegel<\/span> erreichte. <!-- [et_pb_line_break_holder] --> Die eruptive S\u00e4ule breitete sich nach S\u00fcdosten aus und verursachte bedeutende Aschenf\u00e4lle <!-- [et_pb_line_break_holder] --> auf mehrere Siedlungen im s\u00fcd\u00f6stlichen Bereich des \u00c4tna, die bis nach <!-- [et_pb_line_break_holder] --> <span class=\"highlight\">Syrakus und dar\u00fcber hinaus<\/span> reichten.<!-- [et_pb_line_break_holder] --> <\/pee><!-- [et_pb_line_break_holder] --> <pee class=\"event-description\"><!-- [et_pb_line_break_holder] --> Die Lavafont\u00e4nen-Aktivit\u00e4t schw\u00e4chte sich allm\u00e4hlich w\u00e4hrend der Nacht zwischen <!-- [et_pb_line_break_holder] --> dem 4. und 5. Juli ab und h\u00f6rte gegen <span class=\"highlight\">01:50 UTC am 5. Juli<\/span> v\u00f6llig auf. <!-- [et_pb_line_break_holder] --> Nach dem Ende der Font\u00e4ne setzte sich die strombolianische Aktivit\u00e4t etwa eine Stunde lang fort, <!-- [et_pb_line_break_holder] --> bevor sie vollst\u00e4ndig aufh\u00f6rte.<!-- [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] --> Vermessungen und Kartierung der Vulkanite<!-- [et_pb_line_break_holder] --> <\/h3>\n<p><!-- [et_pb_line_break_holder] --> <pee class=\"event-description\"><!-- [et_pb_line_break_holder] --> An den Tagen 5. und 8. Juli wurden <span class=\"highlight\">Drohnenvermessungen<\/span> durchgef\u00fchrt, <!-- [et_pb_line_break_holder] --> um die Vulkanite der eruptiven Ereignisse vom 4. und 7. Juli zu kartieren und die Topographie <!-- [et_pb_line_break_holder] --> der Gipfelkrater zu aktualisieren.<!-- [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 Vermessungsdaten:<\/h4>\n<p><!-- [et_pb_line_break_holder] --> <pee><strong>Extrakraterische Stromfl\u00e4che:<\/strong> 0,4 \u00d7 10\u2075 m\u00b2 mit einem Volumen von etwa 1 \u00d7 10\u2075 m\u00b3<\/pee><!-- [et_pb_line_break_holder] --> <pee><strong>Intrakraterische Stromfl\u00e4che:<\/strong> 0,6 \u00d7 10\u2075 m\u00b2<\/pee><!-- [et_pb_line_break_holder] --> <pee><strong>Proximale pyroklastische Ablagerungsfl\u00e4che:<\/strong> 0,8 \u00d7 10\u2075 m\u00b2<\/pee><!-- [et_pb_line_break_holder] --> <pee><strong>Stromfront-H\u00f6he (8. Juli, 16:00 UTC):<\/strong> 3.016 Meter \u00fc.M.<\/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] --> H\u00f6hepunkt der Eruptiven Aktivit\u00e4t<!-- [et_pb_line_break_holder] --> <\/h3>\n<p><!-- [et_pb_line_break_holder] --> <pee class=\"event-description\"><!-- [et_pb_line_break_holder] --> Die Eruption erreichte einen neuen Intensit\u00e4tsh\u00f6hepunkt. Die Lavafont\u00e4nen \u00fcberschritten <!-- [et_pb_line_break_holder] --> <span class=\"highlight\">1.000 Meter H\u00f6he<\/span> und eine eruptive S\u00e4ule aus Asche und Gas <!-- [et_pb_line_break_holder] --> stieg bis zu <span class=\"highlight\">10 Kilometer in die Atmosph\u00e4re<\/span> auf und verursachte erhebliche <!-- [et_pb_line_break_holder] --> St\u00f6rungen des Flugverkehrs, einschlie\u00dflich der <span class=\"highlight\">vor\u00fcbergehenden Schlie\u00dfung des Flughafens <!-- [et_pb_line_break_holder] --> Catania<\/span>. Die Lavastr\u00f6me setzten ihr Vordringen fort, zerst\u00f6rten Vegetation <!-- [et_pb_line_break_holder] --> und bedrohten landwirtschaftliche Gebiete.<!-- [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] --> Abnahme der Aktivit\u00e4t<!-- [et_pb_line_break_holder] --> <\/h3>\n<p><!-- [et_pb_line_break_holder] --> <pee class=\"event-description\"><!-- [et_pb_line_break_holder] --> Die eruptive Aktivit\u00e4t des Zentralkraters begann abzunehmen und h\u00f6rte gegen <!-- [et_pb_line_break_holder] --> <span class=\"highlight\">2 Uhr morgens<\/span> vollst\u00e4ndig auf. In den folgenden Tagen, vor der <!-- [et_pb_line_break_holder] --> Lavafont\u00e4ne vom 23. Juli, setzten Ascheemissionen wieder ein, gefolgt von intermittierender <!-- [et_pb_line_break_holder] --> strombolianischer Aktivit\u00e4t. Diese Emissionen zeigten eine weniger intensive, <!-- [et_pb_line_break_holder] --> aber kontinuierliche Aktivit\u00e4tsphase an.<!-- [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] --> Lavafont\u00e4ne und Wiederaufnahme der NEC-Explosionen<!-- [et_pb_line_break_holder] --> <\/h3>\n<p><!-- [et_pb_line_break_holder] --> <pee class=\"event-description\"><!-- [et_pb_line_break_holder] --> Am Morgen des 23. Juli, nach einer Nacht intensiver strombolianischer Aktivit\u00e4t, begann eine neue <!-- [et_pb_line_break_holder] --> Lavafont\u00e4ne gegen <span class=\"highlight\">7:45 Uhr<\/span>. Dieses Ereignis erzeugte <!-- [et_pb_line_break_holder] --> eine Gas- und Asches\u00e4ule, die bis <span class=\"highlight\">12:00 Uhr<\/span> anhielt <!-- [et_pb_line_break_holder] --> und dann allm\u00e4hlich abnahm, bis sie v\u00f6llig ersch\u00f6pft war.<!-- [et_pb_line_break_holder] --> <\/pee><!-- [et_pb_line_break_holder] --> <pee class=\"event-description\"><!-- [et_pb_line_break_holder] --> Anschlie\u00dfend, wie nach dem Ereignis vom 15. Juli, nahm der <span class=\"highlight\">Nordostkrater<\/span> <!-- [et_pb_line_break_holder] --> pl\u00f6tzliche Explosionen wieder auf und schleuderte lithische Bl\u00f6cke in <!-- [et_pb_line_break_holder] --> <span class=\"highlight\">fast 1 km Entfernung<\/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] --> Explosionen und Ascheemissionen<!-- [et_pb_line_break_holder] --> <\/h3>\n<p><!-- [et_pb_line_break_holder] --> <pee class=\"event-description\"><!-- [et_pb_line_break_holder] --> Die eruptive Aktivit\u00e4t setzte sich mit Explosionen und Ascheemissionen sowohl von der <!-- [et_pb_line_break_holder] --> <span class=\"highlight\">Voragine<\/span> als auch sporadisch vom <span class=\"highlight\">Nordostkrater<\/span> fort. <!-- [et_pb_line_break_holder] --> Die emittierte Asche l\u00f6ste sich in der Atmosph\u00e4re auf, ohne gr\u00f6\u00dfere <!-- [et_pb_line_break_holder] --> Niederschl\u00e4ge in den umliegenden Gebieten zu verursachen.<!-- [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. August 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] --> Die M\u00e4chtigste Lavafont\u00e4ne<!-- [et_pb_line_break_holder] --> <\/h3>\n<p><!-- [et_pb_line_break_holder] --> <pee class=\"event-description\"><!-- [et_pb_line_break_holder] --> Die eruptive Aktivit\u00e4t erreichte einen neuen H\u00f6hepunkt mit <span class=\"highlight\">der m\u00e4chtigsten Lavafont\u00e4ne <!-- [et_pb_line_break_holder] --> der gesamten paroxysmalen Serie<\/span>. Gl\u00fchende Strahlen \u00fcberschritten <!-- [et_pb_line_break_holder] --> <span class=\"highlight\">2.000 Meter H\u00f6he \u00fcber dem Kraterrand<\/span> und verursachten zus\u00e4tzliche <!-- [et_pb_line_break_holder] --> Lavastr\u00f6me zu den s\u00fcdwestlichen und westlichen Flanken. Dieses Ereignis markierte <!-- [et_pb_line_break_holder] --> (bis zu diesem Moment) das intensivste Ph\u00e4nomen der paroxysmalen Sequenz.<!-- [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>Finale Vulkanit-Karte (4. August 2024):<\/h4>\n<p><!-- [et_pb_line_break_holder] --> <pee>W\u00e4hrend der folgenden Woche wurde die finale Karte der Vulkanite des <!-- [et_pb_line_break_holder] --> eruptiven Ereignisses vom 4. August erstellt. Die Karte wurde durch Analyse von W\u00e4rmebildern <!-- [et_pb_line_break_holder] --> erstellt, die am 4. August per Drohne vom Labor f\u00fcr Kartographie und Drohnen aufgenommen wurden, <!-- [et_pb_line_break_holder] --> sowie Sentinel-2-Satellitenbildern vom 9. August.<\/pee><!-- [et_pb_line_break_holder] --> <pee><strong>Formation:<\/strong> Ein einziges extrakraterisches Lavafeld, unterteilt in drei Haupt\u00e4ste, <!-- [et_pb_line_break_holder] --> die die Stra\u00dfe auf 3.000 m H\u00f6he an drei verschiedenen Punkten \u00fcberquerten, zusammen mit einem extrakraterischen remorphen Strom.<\/pee><!-- [et_pb_line_break_holder] --> <pee><strong>Erreichte Mindesth\u00f6hen:<\/strong><\/pee><!-- [et_pb_line_break_holder] --> <pee>\u2022 Westlicher Strom: <strong>2.922 m \u00fc.M.<\/strong> (niedrigste H\u00f6he)<\/pee><!-- [et_pb_line_break_holder] --> <pee>\u2022 Nordwestlicher Strom: <strong>3.042 m \u00fc.M.<\/strong><\/pee><!-- [et_pb_line_break_holder] --> <pee>\u2022 S\u00fcdwestlicher Strom: <strong>2.988 m \u00fc.M.<\/strong><\/pee><!-- [et_pb_line_break_holder] --> <pee><strong>Bedeckte Fl\u00e4chen:<\/strong><\/pee><!-- [et_pb_line_break_holder] --> <pee>\u2022 Extrakraterischer Strom: <strong>3,7 \u00d7 10\u2075 m\u00b2<\/strong><\/pee><!-- [et_pb_line_break_holder] --> <pee>\u2022 Remorphischer Strom: <strong>0,7 \u00d7 10\u2075 m\u00b2<\/strong><\/pee><!-- [et_pb_line_break_holder] --> <pee>\u2022 Proximale pyroklastische Ablagerung: <strong>1,1 \u00d7 10\u2075 m\u00b2<\/strong><\/pee><!-- [et_pb_line_break_holder] --> <pee><strong>Gesamtes emittiertes Volumen:<\/strong> <strong>2,7 \u00d7 10\u2076 m\u00b3<\/strong> (Lavastr\u00f6me + pyroklastische Ablagerung)<\/pee><!-- [et_pb_line_break_holder] --> <pee><strong>Durchschnittliche Dicken:<\/strong> 4 Meter (extrakraterische und remorphische Str\u00f6me), 9 Meter (proximale pyroklastische Ablagerungen)<\/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. August 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] --> Erneuerung der Strombolianischen Aktivit\u00e4t<!-- [et_pb_line_break_holder] --> <\/h3>\n<p><!-- [et_pb_line_break_holder] --> <pee class=\"event-description\"><!-- [et_pb_line_break_holder] --> An den Tagen 12. und 13. August war die strombolianische Aktivit\u00e4t des Zentralkraters <!-- [et_pb_line_break_holder] --> charakterisiert durch <span class=\"highlight\">das Schleudern von Lavafetzen entlang der Flanken des Schlackenkegels <!-- [et_pb_line_break_holder] --> der Bocca Nuova<\/span>. Diese Aktivit\u00e4t n\u00e4hrte die Eruption weiter <!-- [et_pb_line_break_holder] --> und bereitete den Boden f\u00fcr eine neue paroxysmale Episode vor.<!-- [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. August 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] --> Letztes Paroxysmales Ereignis<!-- [et_pb_line_break_holder] --> <\/h3>\n<p><!-- [et_pb_line_break_holder] --> <pee class=\"event-description\"><!-- [et_pb_line_break_holder] --> Am Nachmittag des 14. August, gegen <span class=\"highlight\">18:00 UTC<\/span>, wurde eine Intensivierung <!-- [et_pb_line_break_holder] --> der strombolianischen Aktivit\u00e4t beobachtet, die sich ab <span class=\"highlight\">22:30 UTC<\/span> <!-- [et_pb_line_break_holder] --> allm\u00e4hlich zu einer Lavafont\u00e4ne entwickelte. W\u00e4hrend dieser Phase entstanden <!-- [et_pb_line_break_holder] --> Lavastr\u00f6me, die den westlichen Rand der Bocca Nuova \u00fcberfluteten und sich teilweise <!-- [et_pb_line_break_holder] --> mit dem am 5. August gebildeten Lavafeld \u00fcberlagerten.<!-- [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. August 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] --> Bocca Nuova-Explosionen – Ende des Zyklus<!-- [et_pb_line_break_holder] --> <\/h3>\n<p><!-- [et_pb_line_break_holder] --> <pee class=\"event-description\"><!-- [et_pb_line_break_holder] --> In den fr\u00fchen Morgenstunden des 18. August 2024 ereigneten sich zwei bedeutende explosive Sequenzen <!-- [et_pb_line_break_holder] --> an der <span class=\"highlight\">Bocca Nuova<\/span>. Die erste Explosion ereignete sich um <!-- [et_pb_line_break_holder] --> <span class=\"highlight\">02:30 UTC<\/span>, gefolgt von einer zweiten um <span class=\"highlight\">02:59 UTC<\/span>, <!-- [et_pb_line_break_holder] --> beide mit einer Dauer von etwa <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] --> Diese Ereignisse markierten die letzte bedeutende Phase explosiver Aktivit\u00e4t des Zentralkraters <!-- [et_pb_line_break_holder] --> im betrachteten Zeitraum. Wir werden in den kommenden Tagen sehen, ob der Vulkan beabsichtigt, <!-- [et_pb_line_break_holder] --> die eruptive Aktivit\u00e4t wieder aufzunehmen oder diesen Zyklus von Episoden abzuschlie\u00dfen, <!-- [et_pb_line_break_holder] --> der durch strombolianische Aktivit\u00e4t und Lavafont\u00e4nen charakterisiert war.<!-- [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] --> <!-- FOTO 3 - Nach der Zeitleiste --><!-- [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=\"\u00c4tna-Nordost\"><!-- [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\">Wissenschaftliche Daten und INGV-Messungen<\/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\">Maximale H\u00f6he der Lavafont\u00e4nen (5. August)<\/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\">H\u00f6he der Eruptiven S\u00e4ule (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\">H\u00f6he der Eruptiven S\u00e4ule beim Ereignis vom 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\">Gesamtvolumen des Emittierten Materials<\/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\">Von Extrakraterischen Str\u00f6men Bedeckte Fl\u00e4che<\/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\">Erreichte Mindesth\u00f6he (Westlicher Strom)<\/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\">Proximale Pyroklastische Ablagerungsfl\u00e4che<\/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 Tage<\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"stat-label\">Gesamtdauer der Eruptiven Sequenz<\/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 \u00c4ste<\/div>\n<p><!-- [et_pb_line_break_holder] --> <\/p>\n<div class=\"stat-label\">Haupt\u00e4ste des Lavafelds (4. August)<\/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\">Maximale Entfernung der Lithischen Bl\u00f6cke (NEC)<\/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\">Durchschnittliche Dicke der Pyroklastischen Ablagerungen<\/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\">Durchschnittliche Dicke der Lavastr\u00f6me<\/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] --> Wissenschaftliche Daten bereitgestellt in Zusammenarbeit mit <!-- [et_pb_line_break_holder] --> <span class=\"footer-highlight\">INGV – \u00c4tna-Observatorium<\/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] --> <\/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":[989,2120,993],"tags":[],"class_list":["post-61610","post","type-post","status-publish","format-standard","hentry","category-atna-jungste-eruptionen","category-de","category-evolutionsgeschichte-des-vulkans-etna"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.4 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>Chronologie der j\u00fcngsten Ausbr\u00fcche der Gipfelkrater des \u00c4tna - 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\/de\/chronologie-der-jungsten-ausbruche-der-gipfelkrater-des-atna\/\" \/>\n<meta property=\"og:locale\" content=\"de_DE\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Chronologie der j\u00fcngsten Ausbr\u00fcche der Gipfelkrater des \u00c4tna - 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