Airborne surveys of volcanic gases reveal that levels of magmatic carbon dioxide have decreased since June. However carbon dioxide is still present and measurable. The carbon dioxide is probably being released from magma that entered the magma reservoir during the past few months. The top of the magma chamber is about 7 kilometers (4 miles) below the crater. Because carbon dioxide is heavier than air, it can concentrate in surface depressions on the dome or crater floor, especially under calm conditions, and pose an asphyxiation hazard. Poorly ventilated cavities, such as caves in the mass of snow and ice behind the dome, could also be hazardous.
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