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The discussion about the scientific opportunities explaining the rise of fumes from Mount Kawkab involves scientific explanations for the phenomenon of gas emissions from the mountain. These emissions may be linked to volcanic activity or subsurface geological processes. Studies indicate that these fumes are produced by the heating of underground water or chemical reactions within the rocks, with the possibility of influences from ongoing or temporary volcanic activity in the area. This phenomenon is considered a potential indicator of internal geological activity, and scientific research can help predict additional natural phenomena related to the volcano. It is also essential to monitor the situation regularly to ensure safety.
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