Mysterious Mud Volcano Island Emerges Off Trinidad Coast After Earthquakes
A temporary mud volcano island has emerged from the sea off the coast of Palo Seco in southwestern Trinidad, following earthquakes off the northern coast of Venezuela on June 24.
According to information attributed to The University of the West Indies Seismic Research Centre (UWI-SRC), mud was expelled from the seabed following the seismic activity, creating a temporary formation above the water.
Geologists and local hikers were photographed examining the formation off Palo Seco on July 10, providing a striking view of the mass of mud rising above the surrounding sea.
The event has attracted attention because mud volcanoes are different from the more commonly known volcanic systems that erupt molten rock or lava. Mud volcanoes generally form when underground pressure forces mixtures of mud, water and gases upward through weaknesses in the Earth’s surface.
Reuters reported, citing the UWI-SRC, that the Palo Seco formation emerged after mud was expelled from the seabed following the June 24 earthquakes off Venezuela’s northern coast. The available information describes the formation as a temporary mud volcano island, meaning its appearance above sea level may not be permanent as waves and erosion reshape the material.
The location is also significant because Trinidad sits within a seismically active region. The UWI-SRC identifies the Gulf of Paria and Paria Peninsula as a seismogenic zone where earthquakes occur at varying depths. The Centre says approximately 40 earthquakes of magnitude 2.1 and above are located within this zone annually.
The new formation should not be confused with an eruption involving lava, and there is currently no indication in the information reviewed that Trinidad is experiencing a conventional magmatic volcanic eruption.
The UWI Seismic Research Centre is the official source of information on earthquakes and volcanoes in the English-speaking Eastern Caribbean.
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