Multibeam (1 m resolution) and side scan data collected from an autonomous underwater vehicle, and
lava samples, radiocarbon-dated sediment cores, and observations of flow contacts collected by remotely
operated vehicle were combined to reconstruct the geologic history and flow emplacement processes on
Axial Seamount’s summit and upper rift zones. The maps show 52 post-410 CE lava flows and 20
precaldera lava flows as old as 31.2 kyr, the inferred age of the caldera. Clastic deposits 1–2 m thick
accumulated on the rims postcaldera. Between 31 ka and 410 CE, there are no known lava flows near the
summit. The oldest postcaldera lava (410 CE) is a pillow cone SE of the caldera. Two flows erupted on
the W rim between ~800 and 1000 CE. From 1220 to 1300 CE, generally small eruptions of plagioclase
phyric, depleted, mafic lava occurred in the central caldera and on the east rim. Larger post-1400 CE
eruptions produced inflated lobate flows of aphyric, less-depleted, and less mafic lava on the upper rift
zones and in the N and S caldera. All caldera floor lava flows, and most uppermost rift zone flows,
postdate 1220 CE. Activity shifted from the central caldera to the upper S rift outside the caldera, to the N rift and caldera floor, and then to the S caldera and uppermost S rift, where two historical eruptions
occurred in 1998 and 2011. The average recurrence interval deduced from the flows erupted over the last
800 years is statistically identical to the 13 year interval between historical eruptions.Keywords: Lava flows, Juan de Fuca Ridge, Geologic, Mapping, Axial Seamoun