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Analysis on Hibok-Hibok Volcano- History and Eruptions, Exercises of Geology

A short analysis on Hibok-Hibok Volcano in Camiguin, Philippines, including its History and Eruptions.

Typology: Exercises

2019/2020

Available from 05/31/2024

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CAMIGUIN POLYTECHNIC STATE COLLEGE
Mambajao, Camiguin
Analysis on Hibok-Hibok Volcano: History and Eruptions
Hibok-Hibok volcano, also known as Catarman, is the youngest and only historically
active stratovolcano in Camiguin, Philippines. Rising to approximately 1,332 meters with a
base diameter of 10 kilometers, it is situated about 6 km northwest of Mt. Mambajao. This
dome-shaped volcanic complex is composed of andesitic to rhyolitic materials (Castillo et al.,
1999). The volcano features sharp-edged ridges formed by previous magma flows and boasts
six summit hot springs: Ardent Spring, Bugong, Tagdo, Tangob, Naasag, and Kiyab. Eruptions
over the years have formed the Kanangkaan, Itum, and Ilihan Craters, which were originally
small cracks at the peak. The 1871 eruption notably caused lava flows that hardened into bowl
shapes, later filling with water (Neri et al., 2010). Numerous steam vents and outlets are
observed on the volcano’s sides and apex. Recognized as a major natural landmark in Central
Mindanao, Mt. Hibok-Hibok was declared an ASEAN Heritage Park in 2015.
Fig. 1. Steam Vents and Fumaroles on the Slopes of Mt. Hibok-Hibok.
Early Formation and Activity
The initial formation of Mt. Hibok-Hibok remains undocumented, but it is inferred that
Camiguin volcanoes formed parallel to the Central Mindanao Arcs on a northwest-southwest
trend (Macdonald et al., 1956). Over time, volcanic vents shifted from the south west to the
northwest, indicating a dynamic volcanic history. The earliest eruption center, the now-
submerged Camiguin Tanda volcano, significantly impacted the surrounding areas. This
activity was succeeded by the formation of Mt. Butay and Ginsilba on Camiguin Island’s
southeast tip, and the Binone cinder cone volcano on the southeast coast (Alcatraz, 1995). The
highest peak, Mt. Mambajao, has no known historic eruptions, suggesting a relatively recent
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Mambajao, Camiguin

Analysis on Hibok-Hibok Volcano: History and Eruptions

Hibok-Hibok volcano, also known as Catarman, is the youngest and only historically active stratovolcano in Camiguin, Philippines. Rising to approximately 1,332 meters with a base diameter of 10 kilometers, it is situated about 6 km northwest of Mt. Mambajao. This dome-shaped volcanic complex is composed of andesitic to rhyolitic materials (Castillo et al., 1999). The volcano features sharp-edged ridges formed by previous magma flows and boasts six summit hot springs: Ardent Spring, Bugong, Tagdo, Tangob, Naasag, and Kiyab. Eruptions over the years have formed the Kanangkaan, Itum, and Ilihan Craters, which were originally small cracks at the peak. The 1871 eruption notably caused lava flows that hardened into bowl shapes, later filling with water (Neri et al., 2010). Numerous steam vents and outlets are observed on the volcano’s sides and apex. Recognized as a major natural landmark in Central Mindanao, Mt. Hibok-Hibok was declared an ASEAN Heritage Park in 2015. Fig. 1. Steam Vents and Fumaroles on the Slopes of Mt. Hibok-Hibok.

Early Formation and Activity

The initial formation of Mt. Hibok-Hibok remains undocumented, but it is inferred that Camiguin volcanoes formed parallel to the Central Mindanao Arcs on a northwest-southwest trend (Macdonald et al., 1956). Over time, volcanic vents shifted from the southwest to the northwest, indicating a dynamic volcanic history. The earliest eruption center, the now- submerged Camiguin Tanda volcano, significantly impacted the surrounding areas. This activity was succeeded by the formation of Mt. Butay and Ginsilba on Camiguin Island’s southeast tip, and the Binone cinder cone volcano on the southeast coast (Alcatraz, 1995). The highest peak, Mt. Mambajao, has no known historic eruptions, suggesting a relatively recent

Mambajao, Camiguin formation. Approximately six kilometers northwest lies the young Hibok-Hibok stratovolcano, which includes several lava domes, notably Mt. Vulcan on its northwest flank. The significant eruptions from 1871-75 and 1948-53 were crucial in depositing pyroclastic flows and forming new lava domes. Fig. 2. Close-Up View of a Lava Dome on Mt. Hibok-Hibok.

Documented Eruptive Events

Table 1. An overview of the historical eruptions ( 1827 - 1951 ) on Mt. Hibok-Hibok. NO. OF ERUPTIONS DATE TYPE OF ERUPTION

DEATH TOLL

1 1827 Unlisted Unlisted 2 1862 Peléan 326 3 1948 Unlisted 0 4 1949 Unlisted 79 5 Dec. 4, 1951 Pelean Greater than 3000

Mambajao, Camiguin The fifth and most violent eruption occurred on December 4, 1951. This Peléan-type eruption was the most catastrophic, releasing poisonous gases, landslides, and lava reaching temperatures up to 800 °C. This event destroyed nearly 19 square kilometers in Mambajao and resulted in over 3,000 deaths. The eruption caused extensive property damage, with deposits containing large amounts of pumice and ash, indicating pyroclastic flows primarily from fresh magma explosions rather than dome collapse (Scarpa & Gasparini, 1996). Lava flows covered almost 10 square kilometers between Mambajao and Yumbing, destroying several villages. Figure 4. The Catastrophic 1951 Eruption of Mt. Hibok-Hibok.

Summary and Impact

Following the 1951 eruption, the local population decreased dramatically from 69,000 to about 34,000 due to massive emigration. The severe casualties and extensive damage led to the establishment of a national institution to monitor and study active volcanoes in the country. In 1982, President Ferdinand Marcos issued Executive Order 784, reorganizing the National Science Development Board into the National Science and Technology Authority (NSTA). The Commission on Volcanology (ComVol) was restructured and renamed the Philippine Institute of Volcanology (PHIVOLCS), tasked with formulating detailed action and relief plans for potential volcanic eruptions. PHIVOLCS installed a monitoring station on Mt. Hibok-Hibok to observe seismic activities. Despite the tragic history, local communities gradually recovered, and the provincial government began developing Camiguin’s natural resources to boost tourism.

Mambajao, Camiguin

REFERENCES:

  1. Bull Volcanol 12, 215–225 (1952). A preliminary report on the recent eruptions of Hibok-Hibok volcano, Camiguin Island, Philippines. https://doi.org/10.1007/BF
  2. Aguilar, F. (2016). Disasters as Contingent Events Volcanic Eruptions, State Advisories, and Public Participation in the Twentieth-Century Philippines. Philippine Studies: Historical & Ethnographic Viewpoints, 64, 593 - 624. Retrieved from JSTOR. http://www.jstor.org/stable/
  3. Alcaraz, A. P. (1995). VOLCANOLOGY WORK IN THE PHILIPPINES. Journal of the Geological Society of the Philippines, 50, 121.
  4. Arguillas, C. O. (2020, November 10). Camiguin's Mt. Hibok-hibok eruption gave birth to today's Phivolcs. Retrieved from https://www.mindanews.com/top-stories/2020/01/camiguins-mt- hibok-hibok-eruption-gave-birth-to-todays-phivolcs/
  5. Camiguin Philippines Mt. Hibok-Hibok. (n.d.). Retrieved from https://www.bohol- philippines.com/mt-hibok-hibok.html
  6. Castillo, P., Janney, P. & Solidum, R. Petrology and geochemistry of Camiguin Island, southern Philippines: insights to the source of adakites and other lavas in a complex arc setting. Contrib Mineral Petrol 134, 33–51 (1999). https://doi.org/10.1007/s
  7. Corpuz, E. S. G. (1992). Petrology and geochemistry of the central Mindano volanic arc, southern Philippines.
  8. Hibok-Hibok. (n.d.). Retrieved from https://www.volcanodiscovery.com/hibok-hibok.html
  9. Macdonald, G. A., & Alcaraz, A. (1956). Nuées ardentes of the 1948–1953 eruption of Hibok- Hibok. Bulletin Volcanologique, 18(1), 169-178. doi:10.1007/bf