The University of the West Indies Seismic Research Centre

Kick 'em Jenny is the source of a number of potential dangers. The most immediate and frequent danger is to marine vessels in the vicinity of the volcano during eruptions and during the 'quiet' periods between eruptions. The volcano lies directly beneath one of the main inter-island shipping routes and the area is popular both with recreational sailors and fishermen. For this reason Kick 'em Jenny is carefully monitored and a 1.5km exclusion zone around the summit of the volcano is currently in place. Although scientists continue to stress the improbability of an eruption generating a tsunami (a giant sea wave) this hazard also remains of great public concern.

Ballistic Projectiles
If Kick 'em Jenny erupts, it might throw hot rocks up through the water column into the air above the surface of the sea. Such rocks could travel as far as 5km from the volcano, and would pose a great danger to nearby ships or boats. Any ship which happened to be over the vent of Kick 'em Jenny during the 1939 eruption would certainly have been destroyed.

In September 1952 a Japanese research ship was passing over the active Myojinsho volcano in the Pacific Ocean south of Japan when that volcano erupted ripping the hull apart. All 31 people on board were killed. This volcano is similar to Kick 'em Jenny but of a slightly less violent type.

This picture shows an eruption from a submarine vent off the south coast of Iceland in 1963 which eventually led to the formation of Surtsey Island. This picture closely resembles the description of the 1939 eruption of Kick 'em Jenny. An eruption such as this one would present a clear hazard to shipping.

Lowered Water Density
Submarine volcanoes release large quantities of gas bubbles into the water, even in quiet times between eruptions. This can lower the density of the seawater above the vent. This is very dangerous to shipping, because boats entering a zone of lowered water density will lose buoyancy and may sink.

Tragedy of the Island Queen
One of Grenada's worst maritme tragedies may have resulted from just this phenomenon. On the 5th August 1944, the wooden schooner Island Queen, with over 60 people on board, disappeared between Grenada and St. Vincent. At the time it was thought that a German or allied submarine had torpedoed the boat. These theories, however, cannot easily explain the total lack of debris after the boat's disappearance. However, if a boat sinks because of lowered water density everything would sink.

Kick 'em Jenny had, in fact erupted the year before (1943) and it is highly likely that it was still actively degassing in 1944, without any signs at the sea surface of such activity.

A degassing submarine volcano can lower the
water density above the volcano. This possibility
of lowered water density above the volcano is an
ever-present hidden hazard.

Tsunamis
In addition to the vulnerability of the shipping industry many people are also concerned about sea waves or tsunamis. While it is probable that large explosions or landslides at Kick 'em Jenny could generate tsunamis, the threat from tsunamis has been largely over exaggerated. Not all eruptions at Kick 'em Jenny will generate tsunamis and not all tsunamis will be large.

Studies show that the worst eruption that Kick 'em Jenny is capable of under any circumstances might generate a wave with an amplitude of 10m in open waters at a distance of 10km from the vent. Waves of this amplitude could be generated only if the volcano began to erupt in water depths of less than about 130m. Currently the depth to the vent is 268m.

Prior to recent bathymetric measurements it was thought that Kick 'em Jenny was growing steadily towards the surface and thus approaching depths at which previous workers (e.g. Smith and Shepherd 1996) had suggested that eruptions could become more explosive. Thus in addition to direct hazards caused by volcanic activity, such as water disruptions and ballistic projectiles over the volcano, there was some speculation that the probability of an eruption-generated tsunami was increasing. However, with the re-evaluation of previous surveys showing clearly that the volcano is not growing towards the surface, together with the results of the most-recent survey which revealed that the vent region of the volcano (the crater floor) is 268m below sea level, the likelihood of a tsunamigenic explosive eruption is now considerably lower (see figure below). Eruption-generated tsunamis may, of course, become a more significant hazard if Kick 'em Jenny does begin to grow closer to the surface.

The best-studied example of underwater dome growth in the West Indies occurred at the Soufriere volcano in St. Vincent in 1971. On that occasion a dome began to grow at the bottom of the 175 metre deep crater lake in early October 1971 and reached the surface in late September. By analogy with this episode we would expect a period of one to two months of steady eruption before Kick 'em Jenny grows into the violently explosive range of depths.

For a detailed study of the potential effects of eruptions of Kick 'em Jenny, particularly its potential for generating tsunamis, go to the bibliography section of this site.

This figure shows that Kick 'em Jenny would need to grow a considerable amount (approximately 138m) before it could potentially produce explosive eruptions which may trigger tsunamis. Scientists do not know how long this growth could take.