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Kick 'em Jenny

Kick 'em Jenny is a earth science topic covered in the lgStudy science library. This page brings together a partial reference excerpt, illustrations, worked examples, real-world applications and a short study plan, so you can understand Kick 'em Jenny rather than just read about it. In short: Kick 'em Jenny (also: Kick-'em-Jenny or Mt. Kick-'Em-Jenny) is an active submarine volcano or seamount on the Caribbean Sea floor, located 8 km (5 mi) north of the island of Grenada and about 8 km (5 mi) west of Ronde Island in the Grenadines.

Kick 'em Jenny — main illustration
Kick 'em Jenny — illustration

Key takeaways

  • Kick 'em Jenny belongs to earth science; place it in that map before memorising details.
  • Learn the definition first, then one example that makes the definition concrete.
  • Connect Kick 'em Jenny to a quantity you can measure, compute or draw — that is where exam questions come from.
  • Reproduce the core statement of Kick 'em Jenny from memory before moving on to harder problems.

Reference excerpt

Kick 'em Jenny (also: Kick-'em-Jenny or Mt. Kick-'Em-Jenny) is an active submarine volcano or seamount on the Caribbean Sea floor, located 8 km (5 mi) north of the island of Grenada and about 8 km (5 mi) west of Ronde Island in the Grenadines. Kick-'em-Jenny rises 1,300 m (4,265 ft) above the sea floor on the steep inner western slope of the Lesser Antilles ridge. The South American tectonic plate is subducting the Caribbean tectonic plate to the east of this ridge and under the Lesser Antilles island arc.

Etymology The volcano was unknown before 1939, although "Kick 'em Jenny" appeared on earlier maps as either the name of a small island now called Diamond Rock (or Île Diamante), or the name of the strait between Grenada and Ronde Island (or Île de Ronde). The name itself may be a reference to the waters sometimes being extremely rough.

Activity The first record of the volcano was in 1939, although it must have erupted many times before that date. On 23–24 July 1939 an eruption broke the sea surface, sending a cloud of steam and debris 275 m (902 ft) into the air and generating a series of tsunamis around two metres (6.6 ft) high when they reached the coastlines of northern Grenada and the southern Grenadines. A small tsunami also reached the west coast of nearby Barbados, where "a sea-wave" suddenly washed over a coastal road, most likely at Paynes Bay. The volcano has erupted on at least twelve occasions between 1939 and 2017 (the last being on April 29, 2017), although no subsequent eruption has been as large as the 1939 one, and most were only detected by seismographs. The larger eruptions have also been heard underwater or on land close to the volcano as a deep rumbling sound. A submersible survey in 2003 detected a crater with active fumaroles releasing cold and hot gas bubbles. Samples of fresh olivine basalt were collected. An arc-shaped collapse structure appears on the west flank and was the apparent source of a submarine debris avalanche extending 15 km (49,000 ft) down the ridge slope to the west toward the Grenada Basin. The Global Volcanism Program reports the summit to be 185 m (607 ft) below the sea surface. Signs of elevated seismicity began July 11, 2015, and on July 23 a strong continuous signal was recorded by instruments observing Kick 'em Jenny, prompting authorities to raise the alert level to orange, which is the second-highest level. The following day, July 24, at 02:00 an hourlong explosion event was recorded, scientists from the University of the West Indies Seismic Research Centre observed nothing out of the ordinary at the surface above the volcano during an overflight on 25 July, and by 18:00 no activity was recorded. On 26 July the Alert Level was lowered to Yellow. In 2017, a team of researchers on the RRS James Cook led by marine geophysicist Jenny Collier observed ongoing volcanic activity at the site.

Maritime exclusion zone The volcano is on the shipping route from St Vincent to Grenada. There is a Maritime Exclusion Zone monitored by the Seismic Research Centre of the University of the West Indies, Trinidad and Tobago. The zone normally encompasses a circle with a radius of 1.5 km (1 mi) from the centre of the volcano. Bubbles of volcanic gases can lower water density, creating a sinking hazard. This is marked on marine charts. During periods of high seismic activity, the zone is expanded to a 5-kilometre (3.1 mi) radius.

See also List of volcanoes in Grenada

References

Illustrations

Kick 'em Jenny illustration
Kick 'em Jenny illustration

Worked examples

Example 1 — a first encounter with Kick 'em Jenny

Start with the simplest possible case. Write down what Kick 'em Jenny claims or describes in one sentence, then invent the smallest concrete situation in which that sentence is true. In earth science, the smallest case is usually a single object, a single equation or a single measurement. Check that every symbol or term in your sentence has a meaning in that case.

Example 2 — changing one variable

Take the situation from Example 1 and change exactly one quantity: double it, halve it, or set it to zero. Predict what should happen to Kick 'em Jenny before you calculate. Comparing your prediction with the result is the fastest way to find out whether you understand the idea or only the words.

Example 3 — an exam-style question

Typical questions about Kick 'em Jenny ask you to (a) state it precisely, (b) apply it to given data, and (c) explain a limitation. Practise writing all three answers in under five minutes; the third part is what separates a full-mark answer from an average one.

Applications of Kick 'em Jenny

In research
Kick 'em Jenny appears in earth science research whenever the underlying quantities have to be modelled precisely. Papers usually cite it as a starting assumption and then explore where it breaks down.
In technology and industry
Engineering practice reuses Kick 'em Jenny in design rules, simulations and safety margins. Knowing the idea lets you read a specification sheet and understand why the numbers look the way they do.
In the classroom
Kick 'em Jenny is common in secondary-school and first-year university syllabi. It links to neighbouring topics Active volcanoes, Former islands from the last glacial maximum, Seamounts of the Atlantic Ocean, so understanding it makes those chapters shorter.
In everyday life
Look for Kick 'em Jenny outside the textbook — in sport, cooking, traffic, electronics or the sky above you. An example you found yourself is remembered far longer than one you were given.
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How to study Kick 'em Jenny in 20 minutes

  1. Read the reference excerpt below once, without taking notes.
  2. Close the page and write down what Kick 'em Jenny means in your own words.
  3. Compare your version with the excerpt and mark what you missed.
  4. Work through the three examples above with pen and paper.
  5. Explain Kick 'em Jenny out loud to somebody else — or to Teacher Smith in the lgStudy chat.

Frequently asked questions

What is Kick 'em Jenny in simple terms?

Kick 'em Jenny (also: Kick-'em-Jenny or Mt. Kick-'Em-Jenny) is an active submarine volcano or seamount on the Caribbean Sea floor, located 8 km (5 mi) north of the island of Grenada and about 8 km (5 mi) west of Ronde Island in the Grenadines.

Why does Kick 'em Jenny matter?

Because it connects several earth science ideas at once: it gives you a definition you can apply, a quantity you can calculate, and a way to check whether a result is plausible.

How should I study Kick 'em Jenny?

Read the excerpt, restate it from memory, then work through the examples and applications listed on this page. The five-step study plan above takes about twenty minutes.

What does this page cover?

It gives you a compact reference excerpt plus original lgStudy explanations, examples, applications and study material on Kick 'em Jenny.

Tags

  • Active volcanoes
  • Former islands from the last glacial maximum
  • Seamounts of the Atlantic Ocean
  • Seamounts of the Caribbean
  • Submarine volcanoes
  • Volcanoes of Grenada

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