This paper investigates a puzzling and still-unresolved phenomenon: the presence of large plume-like features visible in the layers of the Greenland Ice Sheet. Although previous studies have proposed various explanations for these features, none have been confirmed to date. In this study, the authors investigate an unconventional and debated hypothesis: That local thermal convection may be responsible for the observed layer disruptions. This work opens new avenues for research and provides a fresh perspective on an intriguing scientific problem.