Taal Volcano, situated within a large caldera occupied by Taal Lake in the Philippines' Batangas province, stands as the country's second most active volcano. Positioned approximately 50 kilometers south of Manila, it has a recorded history of 38 eruptions, all confined to Volcano Island at the heart of Taal Lake. The caldera's formation is attributed to prehistoric eruptions occurring between 140,000 and 5,380 years ago.
In 1904, an eruption created a new outlet in the southeastern wall of Taal Volcano's principal crater, marking a significant change in its structure.
In January 1911, Taal Volcano experienced one of its most destructive eruptions. Starting in the late hours of January 27th, the Manila Observatory recorded escalating seismic disturbances. The increasing frequency and intensity of these earthquakes, with 26 shocks on the 27th and 217 on the 28th, caused widespread fear in Manila.
Before the 1911 eruption, Taal Volcano's crater floor was higher than Taal Lake and featured multiple openings with colorful lakes and steaming hot water holes. The eruption dramatically altered the crater, replacing these features with a single large lake. This lake, initially about ten feet below the surrounding lake level, gradually rose. A popular but later debunked theory suggested this water cooled volcanic material, reducing eruption risks.
The eruption in 1911 led to the obliteration of the crater floor on Volcano Island, resulting in the formation of the present Main Crater Lake.
The last eruption from the main crater of Taal Volcano prior to 2020 occurred in 1911, resulting in the creation of the current lake by obliterating the previous crater floor.
A powerful explosion in 1965 significantly altered Taal Volcano by removing a large portion of the island and causing volcanic activity to shift to a new eruption center, Mount Tabaro.
A significant event, likely a volcanic eruption, occurred in 1965, resulting in the formation of a bay in the landscape.
An American geologist, present at an atomic bomb test during his military service, observed Taal Volcano's 1965 eruption. He identified "base surge," now known as pyroclastic surge, as a volcanic process, highlighting a connection between nuclear and volcanic phenomena.
Following the 1911 eruption and the formation of the crater lake, Taal Volcano's activity shifted to Mount Tabaro. The 1965 eruption and subsequent activity originated from this new center, demonstrating a significant change in the volcano's behavior.
Taal Volcano experienced a period of volcanic activity from 1965 to 1977, centered around Mount Tabaro. The 1965 eruption, categorized as phreatomagmatic, occurred when magma interacted with lake water, triggering a massive explosion. This event carved an embayment on Volcano Island and generated destructive "cold" base surges that traveled several kilometers across Lake Taal, resulting in significant damage to lakeside villages and the loss of around one hundred lives.
After nine months of inactivity, Taal Volcano became active again on July 5, 1966, with a phreatomagmatic eruption from Mount Tabaro.
Taal Volcano experienced another phreatomagmatic eruption on August 16, 1967, originating from Mount Tabaro, further indicating heightened volcanic activity during this period.
On January 31, 1968, Taal Volcano displayed Strombolian eruptions, which led to the first historical observation of lava fountaining at the volcano, marking a significant event in its eruptive history.
A year after the first recorded instance of lava fountaining, Taal Volcano experienced another Strombolian eruption on October 29, 1969. The substantial lava flows from both eruptions eventually filled the bay formed by the 1965 eruption, reaching the shores of Lake Taal, significantly altering the surrounding landscape.
Taal Volcano experienced a phreatic eruption in 1976, characterized by the expulsion of steam and volcanic material, indicating continued volcanic unrest during this period.
Between 1572 and 1977, Taal Volcano experienced 54 recorded eruptions. This period saw significant volcanic activity, shaping the landscape and history of the region.
Following the eruption in 1977, Taal Volcano entered a period of relative inactivity. However, despite the reduced volcanic activity, the volcano still showed signs of unrest starting in 1991.
The final major activity in this period of heightened volcanic activity at Taal was a phreatic eruption in 1977, marking the end of a period of frequent eruptions and unrest.
Despite a period of reduced volcanic activity following the 1977 eruption, Taal Volcano began showing signs of unrest starting in 1991. These included increased seismic activity, ground fracturing, and the emergence of small mud pots and geysers on the island. This unrest prompted the Philippine Institute of Volcanology and Seismology (PHIVOLCS) to issue regular notices and warnings about the volcano's activity.
In October 1994, a significant increase in radon gas concentration was detected in the soil of Volcano Island, followed by the magnitude 7.1 Mindoro earthquake on November 15th, 1994. This event suggested a possible correlation between radon emissions and seismic activity.
On August 8, 2018, the Philippine Institute of Volcanology and Seismology (PHIVOLCS) released information on "Taal Volcano Alert Signals."
The original source for the information on Taal Volcano Alert Signals was archived on December 17, 2019.
The archived information on Taal Volcano Alert Signals was retrieved on January 15, 2020.
By January 26, 2020, PHIVOLCS observed a decline in volcanic activity at Taal, leading to the downgrade of the alert level from Level 4 to Level 3. While the eruption had impacted a large region, including Calabarzon, Metro Manila, and parts of Central Luzon and Ilocos Region, causing disruptions in daily life and prompting evacuations, the decreasing activity offered a sign of potential stabilization.
After temporarily disappearing due to the 2020 eruption, the Main Crater Lake on Volcano Island reappeared in March 2020.
In February, as Taal Volcano showed signs of heightened activity, residents of Taal Volcano Island were evacuated as a precautionary measure. On March 9, 2021, PHIVOLCS raised the alert level from 1 to 2, reflecting the increased volcanic unrest.
On May 6, 2024, due to a series of wildfire devastations near the Binintiang Munti observation station, Hermilando Mandanas declared Taal Volcano Island (TVI), which was under Alert Level 1-Low-level unrest, a "no man's land."