Fogo

by Casey Davidow

Eruption of 1995

Eruption of 1995:

Weak earthquakes were felt starting March 25th, 1995.  On April 2nd the earthquakes became stronger and more frequent, and were felt by the people surrounding Fogo.  On the night of April 1st a red glow was emitted from the volcano and the eruptive vents were noticeably open.  The eruption began on April 3rd with a fissure eruption followed by some lava flow.  The volcano then sent of bursts of gases followed by large blocks of rock, and eventually a large lava flow.  Fine dark ash was falling and an eruption cloud that covered 2,500 meters was formed around the volcano.  People near the volcano described the volcano as sounding like an "old stove" and observed "mushroom-shaped ash" coming from the volcano.  There was one long fissure vent that produced "lava fountains" and three smaller vents that produced fine dark ash, small pahoe lavas, and large plastic bombs that were thrown up to 500 meters from the volcano.  Brown pyroclastic material was produced as more vents opened until the morning of April 4th, when the volcano continued to experience strong effusive activity but the amount of pyroclastic fragments produced decreased.  The lava flowed at a fairly constant rate until April 7th when the lava began to flow even faster and by April 10th the seismic activity had increased significantly and earthquakes of higher intensities began to occur (Mercalli intensity 3-4).  On the morning of April 10th Fogo would have been considered a Strombolian eruption, but by the afternoon it looked more like an Hawaiian eruption and was producing fire fountains (see picture below).  A cone was forming that continued to grow as the fire fountains continued through April 16th.  By April 17th there was an even higher tremor amplitude and the volcano produced louder bursts.  Through early May the lava flow was slightly slower and there were some calm periods, but not until May 17th did the lava stop flowing.  On May 17th clouds of gas and dust surrounded Fogo and a strong Sulfur smell was emitted.  This continues until May 28th, when the eruption finally ended.¹

The eruption of 1995 destroyed 1.6 square miles of productive farmland and caused the evacuation of 5,000 people.²²

 

A fire fountain during Fogo's eruption.²

 

fogo

Dust and smoke being produced during Fogo's eruption.³

VEI: 2

Fogo has a VEI of 2 because it is explosive and  produces a large, but not enormous, amount of Tephra.  Fogo has periods when it seems characteristically strombolian, but then it also has some lava fountains which are very characteristic of a Hawaiian volcano, which are very non-explosive.  During different periods of Fogo's eruption it could be categorized under a variety of different VEI ratings, but overall it probably falls best under the level 2 category of volcanoes.

Mercalli Eruption Style Name:  Strombolian.

Fogo is a Strombolian style volcano because the eruption is noisy, it produces some fragments of plastic lava and dusty tephra, it produces low viscosity magmas, and a cinder cone is formed.

 

 

Questions about this site? Contact me @ cdavidow@mail.colgate.edu