ADVERTISEMENT

Phivolcs chief highlights potential scenarios following Kanlaon Volcano eruption

Published Jun 4, 2024 06:00 am
IMG_3858.jpeg
Screenshot of the time-lapse IP camera footage from 6:51 p.m. to 6:57 p.m. of the explosive eruption at the Kanlaon Volcano summit crater, taken by the Canlaon City (VKCC) observation station on June 3, 2024. The plume can be seen rising 5,000 meters above the vent. (Phivolcs/Facebook)

Following an "explosive eruption" on Monday evening, June 3, Kanlaon Volcano was placed on Alert Level 2, indicating "increasing unrest.”

This prompted Philippine Institute of Volcanology and Seismology (Phivolcs) Director Teresito Bacolcol to highlight three possible scenarios for the coming days.

“After ng eruption yesterday, hindi na nasundan. Sana ganun na lamang. Sana hindi na maulit pa but we are still closely monitoring the activity of Kanlaon (After yesterday’s eruption, there hasn’t been any subsequent activity. We hope it remains that way. We hope it doesn’t happen again, but we are still closely monitoring the activity of Kanlaon),” Bacolcol said in a televised public briefing on Tuesday, June 4.

Between midnight and noon on Tuesday, Phivolcs only recorded 43 volcanic earthquakes, indicating heightened seismic activity in Kanlaon Volcano.

Scenarios

Based on Kanlaon Volcano’s monitoring parameters, Bacolcol outlined three possible scenarios that may occur in the next few days.

Firstly, if the current parameters are sustained, phreatic and short-lived explosive eruptions similar to the recent activity may occur within the next few days, he said.

In such a scenario, Phivolcs will maintain Alert Level 2 until significant changes in monitoring parameters are observed, he added.

In the second scenario, Bacolcol said if seismic, ground deformation and volcanic gas parameters worsen, a magmatic eruption could ensue, prompting Phivolcs to raise the alert level from 2 to 3.

However, he emphasized the historical rarity of magmatic eruptions at Kanlaon, with the majority of past eruptions being phreatic.

“If you look at the eruption history of Kanlaon Volcano, from 1866 until yesterday (June 3), isang beses lamang nagkaroon ng magmatic eruption, that was in 1902. Karamihan ng eruption ng Kanlaon Volcano is phreatic eruption (If you look at the eruption history of Kanlaon Volcano, from 1866 until yesterday (June 3), there has been only one magmatic eruption, which occurred in 1902. The majority of eruptions of Kanlaon Volcano are phreatic eruptions),” Bacolcol said.

In the third scenario, he noted that if monitoring parameters decline, Phivolcs will consider lowering the alert level from 2 to 1, but only after at least two weeks of sustained decrease in the parameters.

Phreatic vs magmatic eruption

Meanwhile, Bacolcol said further analysis of the June 3 eruption is required to accurately determine whether the volcanic activity was a phreatic or magmatic eruption.

“‘Yung phreatic eruption involves water coming into contact with hot volcanic materials—hot gases or hot rocks—leading to explosive steam. ‘Yung magmatic eruption naman is driven by the release of magma and volcanic gases (The phreatic eruption involves water coming into contact with hot volcanic materials—hot gases or hot rocks—leading to explosive steam. On the other hand, the magmatic eruption is driven by the release of magma and volcanic gases),” he explained.

“For now, ‘yung nangyaring volcanic eruption kahapon hindi pa natin mai-classify if it’s phreatic or magmatic or if its a combination of both. We need more data, we need to analyze the ash samples na binuga kahapon and check if may bagong magma or old materials ‘yung binuga kahapon (For now, we cannot yet classify yesterday's volcanic eruption as either phreatic or magmatic, or if it's a combination of both. We need more data; we need to analyze the ash samples emitted yesterday and check if there are new magma or old materials within the emitted ash),” Bacolcol said.

The Phivolcs chief noted that the last significant eruption of Kanlaon Volcano occurred on Dec. 9, 2017, which produced a four-kilometer eruption column.

He added that because of the cloudy conditions on Dec. 20, 2017, no eruption column was visible despite the recording of 412 volcanic earthquakes.

Precautions

Phivolcs explained that Kanlaon Volcano’s unrest is caused by shallow magmatic processes, which could eventually lead to more explosive eruptions or even a hazardous magmatic eruption.

The public is strongly advised to remain vigilant and avoid the four-kilometer-radius permanent danger zone to reduce the risk of "sudden" explosions, rockfalls, and landslides.

In the event of ashfall events that may affect communities near Kanlaon’s crater, people should cover their noses and mouths with a damp, clean cloth or dust mask.

Related Tags

Kanlaon Volcano PHIVOLCS Phivolcs Director Teresito Bacolcol
ADVERTISEMENT
.most-popular .layout-ratio{ padding-bottom: 79.13%; } @media (min-width: 768px) and (max-width: 1024px) { .widget-title { font-size: 15px !important; } }

{{ articles_filter_1561_widget.title }}

.most-popular .layout-ratio{ padding-bottom: 79.13%; } @media (min-width: 768px) and (max-width: 1024px) { .widget-title { font-size: 15px !important; } }

{{ articles_filter_1562_widget.title }}

.most-popular .layout-ratio{ padding-bottom: 79.13%; } @media (min-width: 768px) and (max-width: 1024px) { .widget-title { font-size: 15px !important; } }

{{ articles_filter_1563_widget.title }}

{{ articles_filter_1564_widget.title }}

.mb-article-details { position: relative; } .mb-article-details .article-body-preview, .mb-article-details .article-body-summary{ font-size: 17px; line-height: 30px; font-family: "Libre Caslon Text", serif; color: #000; } .mb-article-details .article-body-preview iframe , .mb-article-details .article-body-summary iframe{ width: 100%; margin: auto; } .read-more-background { background: linear-gradient(180deg, color(display-p3 1.000 1.000 1.000 / 0) 13.75%, color(display-p3 1.000 1.000 1.000 / 0.8) 30.79%, color(display-p3 1.000 1.000 1.000) 72.5%); position: absolute; height: 200px; width: 100%; bottom: 0; display: flex; justify-content: center; align-items: center; padding: 0; } .read-more-background a{ color: #000; } .read-more-btn { padding: 17px 45px; font-family: Inter; font-weight: 700; font-size: 18px; line-height: 16px; text-align: center; vertical-align: middle; border: 1px solid black; background-color: white; } .hidden { display: none; }
function initializeAllSwipers() { // Get all hidden inputs with cms_article_id document.querySelectorAll('[id^="cms_article_id_"]').forEach(function (input) { const cmsArticleId = input.value; const articleSelector = '#article-' + cmsArticleId + ' .body_images'; const swiperElement = document.querySelector(articleSelector); if (swiperElement && !swiperElement.classList.contains('swiper-initialized')) { new Swiper(articleSelector, { loop: true, pagination: false, navigation: { nextEl: '#article-' + cmsArticleId + ' .swiper-button-next', prevEl: '#article-' + cmsArticleId + ' .swiper-button-prev', }, }); } }); } setTimeout(initializeAllSwipers, 3000); const intersectionObserver = new IntersectionObserver( (entries) => { entries.forEach((entry) => { if (entry.isIntersecting) { const newUrl = entry.target.getAttribute("data-url"); if (newUrl) { history.pushState(null, null, newUrl); let article = entry.target; // Extract metadata const author = article.querySelector('.author-section').textContent.replace('By', '').trim(); const section = article.querySelector('.section-info ').textContent.replace(' ', ' '); const title = article.querySelector('.article-title h1').textContent; // Parse URL for Chartbeat path format const parsedUrl = new URL(newUrl, window.location.origin); const cleanUrl = parsedUrl.host + parsedUrl.pathname; // Update Chartbeat configuration if (typeof window._sf_async_config !== 'undefined') { window._sf_async_config.path = cleanUrl; window._sf_async_config.sections = section; window._sf_async_config.authors = author; } // Track virtual page view with Chartbeat if (typeof pSUPERFLY !== 'undefined' && typeof pSUPERFLY.virtualPage === 'function') { try { pSUPERFLY.virtualPage({ path: cleanUrl, title: title, sections: section, authors: author }); } catch (error) { console.error('ping error', error); } } // Optional: Update document title if (title && title !== document.title) { document.title = title; } } } }); }, { threshold: 0.1 } ); function showArticleBody(button) { const article = button.closest("article"); const summary = article.querySelector(".article-body-summary"); const body = article.querySelector(".article-body-preview"); const readMoreSection = article.querySelector(".read-more-background"); // Hide summary and read-more section summary.style.display = "none"; readMoreSection.style.display = "none"; // Show the full article body body.classList.remove("hidden"); } document.addEventListener("DOMContentLoaded", () => { let loadCount = 0; // Track how many times articles are loaded const offset = [1, 2, 3, 4, 5, 6, 7, 8, 9, 10]; // Offset values const currentUrl = window.location.pathname.substring(1); let isLoading = false; // Prevent multiple calls if (!currentUrl) { console.log("Current URL is invalid."); return; } const sentinel = document.getElementById("load-more-sentinel"); if (!sentinel) { console.log("Sentinel element not found."); return; } function isSentinelVisible() { const rect = sentinel.getBoundingClientRect(); return ( rect.top < window.innerHeight && rect.bottom >= 0 ); } function onScroll() { if (isLoading) return; if (isSentinelVisible()) { if (loadCount >= offset.length) { console.log("Maximum load attempts reached."); window.removeEventListener("scroll", onScroll); return; } isLoading = true; const currentOffset = offset[loadCount]; window.loadMoreItems().then(() => { let article = document.querySelector('#widget_1690 > div:nth-last-of-type(2) article'); intersectionObserver.observe(article) loadCount++; }).catch(error => { console.error("Error loading more items:", error); }).finally(() => { isLoading = false; }); } } window.addEventListener("scroll", onScroll); });

Sign up by email to receive news.