What type of eruption does Kick em-Jenny have?
Submarine volcanic eruptions
Submarine volcanic eruptions occurred at Kick-’em-Jenny during 4-6 December 2001 (BGVN 26:11).
What happens if Kick em-Jenny erupts?
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 5 km from the volcano, and would pose a great danger to nearby ships or boats.
How was Kick Em-Jenny volcano formed?
Kick-’em-Jenny and the other volcanoes in the arc are associated with a subduction zone. The subduction zone is formed by an oceanic plate created at the Mid-Atlantic Ridge as it is pushed under the Caribbean Plate. This figure is a geologic map of Kick-’em-Jenny by Sigurdsson and Shepherd (1974).
Why is it called Kick em Jenny?
The exact origins of the name ‘Kick-’em-Jenny’ are unknown, but it may relate to the waters in this region which are sometimes extremely rough. It may be a corruption of the French: cay que gêne, ‘the turbulent cay (shoal)’, or it may be a reference to a kicking donkey “Jenny”.
Why is the volcano called Kick em Jenny?
Where’s its name from? The volcano was named after a nearby island called Diamond Rock. The UWI says the island used to be called Kick ‘Em Jenny and the name is possibly related to the rough waters in the area.
Are there underwater volcanoes in the Caribbean?
Kick’em Jenny is a dangerous and active volcano sitting roughly 6,000 feet below the surface of the Caribbean Sea, and located off the coast of the island of Grenada, south of St. Lucia.
Is Kick em Jenny active right now?
Currently, Kick-’em-Jenny’s summit is 197 m below sea level and the diameter of the crater is 300 m. Between the 1960’s and the late 1970’s the depth to the summit of the volcano was approximately 180-190 m.
What is the current status of Kick em Jenny?
Is Kick em Jenny active?
Kick’em Jenny is the most active volcano in the Antilles Volcanic Arc. Since its debut eruption in 1939, it has provided scientists with a rare opportunity to learn about the growth and development of submarine volcanoes into eventual islands.