FIELD STOP 13: NAPAU TRAIL
We began our hike in hopes of seeing the active Pu'u O'o Cone, but with
rainy weather
all morning we did not see much at the top of Pu'u Huluhulu. The following pictures show
the features we saw during the hike.
Fig.1: Napau Trail. Blue dots mark the trailhead (975 m) and Pu'u Huluhulu (1049 m). The
red line marks the 1 mile hike. The blue circles highlight the three features we wanted to see. Mauna
Ulu was the only visible feature (Fig 6).
ALONG THE TRAIL . . .

Fig 2: Our guide Tom Mcauliffe, University of Hilo-Hawaii graduate, begins to lead the way.
Note the aa flow, characterized by angular, jagged blocks, in the background. Pahoehoe flow, a Hawaiian term, is lava with a smooth or ropy
surface. See lava hike pictures for a comparison.

Fig. 3: Tumulus. Ashley Wong for scale. Tumulus are formed in two ways. One, fast
flowing lava gets clogged and bunched up by trees and other vegetation, much like debris is held
up by vegetation during a flood. Two, a bulge can inflate from lava flowing into an area that is blocked by something
on one or more sides from behind. The clumps solidify and the ground around them subside.
There were numerous tumuli in varying sizes along the trail.
 Fig. 4: Napau Trail.
Capstone class hiking in the rain on the lava!

Fig. 5: The northeast side of the Pu'u Huluhulu Cone viewing what should be the
active Pu'u O'o vent about 2.5 miles away. The Pu'u O'o Cone's continuous activity is unusal for
a shield volcano. It has been flowing continuously since 1978 and holds the longest recorded
eruption in history.

Fig. 6: View of Mauna Ulu from atop Pu'u Huluhulu facing east.
Refer to Fig. 1 for orientation. The red line marks an active (lava) lake rim, held up by spatter
ramparts, at the base of Mauna Ulu. Blue arrow shows the direction to where the Pu'u O'o vent
should be visible.
ADDITIONAL LINKS
[Day 3 Home Page] [FS 11: Southwest Rift] [FS12: Halemaumau Crater]
[FS 13: Napau Trail] [FS 14: Holei Sea Arch] [Lava Hike!] [Capstone Home Page]
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