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Science
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This period of summit overflows may end when a large flank eruption occurs low on the flanks and robs Mauna Loa of the high-standing magma required for shield building.
The sudden lowering of the magma column associated with caldera collapse results in a major shift of surface activity as both rift zones become characterized by frequent eruptive activity (an estimated average of one rift zone eruption each 20-25 years over the past 1,000 years)...
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Summit activity probably continues during times of increased rift activity (as it has during the 19th-20th centuries - Barnard, 1995), but all erupted lavas are trapped within the summit caldera, and no trace of this activity remains at the surface.
As stresses increase across the rift zones over time, magma again rises more easily within the edifice, and the caldera is filled...
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