Draft:Calabash resonances
Submission declined on 18 November 2024 by Memer15151 (talk).
Where to get help
How to improve a draft
You can also browse Wikipedia:Featured articles and Wikipedia:Good articles to find examples of Wikipedia's best writing on topics similar to your proposed article. Improving your odds of a speedy review To improve your odds of a faster review, tag your draft with relevant WikiProject tags using the button below. This will let reviewers know a new draft has been submitted in their area of interest. For instance, if you wrote about a female astronomer, you would want to add the Biography, Astronomy, and Women scientists tags. Editor resources
|  |
A calabash resonance is a prolonged seismic oscillation that can occur within the magma chamber-conduit system of a volcano. These resonances potentially arise when seismic waves, slowed and trapped by the contrast in velocities between magma and surrounding rock, undergo multiple reflections inside the magma-filled structures. External seismic events, like volcanic-tectonic earthquakes, trigger these oscillations, which persist as distinct resonance frequencies.
The calabash resonance is named for its resemblance to the shape of the calabash fruit.[1]
References
[edit]- ^ Fabian Limberger, Georg Rümpker (2024-07-19), "Numerical modeling predicts seismic resonances in the magma chamber-conduit system due to wavefield capturing", Volcanica, vol. 7, no. 2, pp. 461–470, Bibcode:2024Volca...7..461L, doi:10.30909/vol.07.02.461470, ISSN 2610-3540, retrieved 2024-11-18
- in-depth (not just passing mentions about the subject)
- reliable
- secondary
- independent of the subject
Make sure you add references that meet these criteria before resubmitting. Learn about mistakes to avoid when addressing this issue. If no additional references exist, the subject is not suitable for Wikipedia.