Mayon Volcano

A series of mild eruptions at Mayon Volcano, the most active volcano in the Philippines, has recently forced nearly 3,000 villagers to evacuate from areas near its foothills.

Location and Geological Setting of Mayon Volcano

Mayon Volcano is an active stratovolcano located in Albay province on Luzon Island in the Philippines. It lies within the Pacific Ring of Fire, a region known for frequent earthquakes and volcanic eruptions due to tectonic plate interactions.

Physical Characteristics of Mayon Volcano

Mayon Volcano is often referred to as the world’s most perfect volcanic cone because of the remarkable symmetry of its shape. It has a base circumference of about 130 kilometres and rises to a height of 2,462 metres from the shores of the Albay Gulf. The volcano has steep upper slopes and is capped by a small summit crater.

Ecological and Economic Significance

The volcano is a major attraction for climbers and campers and forms the central feature of the Mayon Volcano National Park. The lower slopes of the volcano support large abaca plantations, which are economically important to the local population.

Eruptive History of Mayon Volcano

Historical records show that Mayon Volcano has been erupting since 1616 CE. Its eruptions have typically included Strombolian activity, lava flows, pyroclastic flows, and mudflows (lahars).

The most violent eruption occurred in 1814, resulting in the death of more than 1,200 people and the destruction of several towns. Another major eruption in 1993 caused 79 deaths. Subsequent eruptions in 2000, 2006, 2009, 2014, 2018, and 2022 led to the evacuation of tens of thousands of residents from nearby villages.

What is a Stratovolcano?

A stratovolcano is a tall, steep, cone-shaped volcano with a high peak, unlike flat shield volcanoes. These volcanoes are typically found above subduction zones and are commonly associated with large volcanically active regions such as the Pacific Ring of Fire.

Stratovolcanoes constitute approximately 60% of the Earth’s individual volcanoes. They are usually composed of andesite and dacite lava, which are cooler and more viscous than basaltic lava. Due to this high viscosity, gases become trapped easily, leading to explosive eruptions.

Structure of Stratovolcanoes

Stratovolcanoes are also known as composite volcanoes because they are formed by alternating layers of lava flows and pyroclastic material. This layered structure gives them steep sides, and they usually have a small summit crater at the peak.