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2 August 2001
Still more changes in 1880-foot skylight
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July 27. This view matches that of July 14 (see
update archive), but crust
now completely hides molten lava. Glow can faintly be seen far back in the
skylight. Most of the crust formed between July 19 and July 27.
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August 2. Perspective is similar to that of last
image taken on July 5 (see update archive). Two streams of lava meet just downstream of the
skylight, flowing from right to left. Thick crust supports geophysicist
using a Very Low Frequency (VLF) instrument that measures the electrical
conductivity of the ground beneath, in order to determine the
cross-sectional area of molten lava in the tube. Combined with radar-gun
measurements of the velocity of the lava stream, this information gives us
the flux of lava passing through the tube.
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9 August 2001
Surface of lava continues to lower in 1880-foot skylight
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August 9. The view is similar to that of August 2,
though closer, and shows that the level of lava has dropped still farther.
The depth of the lava remains about the same, because the the stream is
eroding into its bed.
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14 August 2001
Great view of East Kupapa`u bench from safe viewing area
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View of the active bench--sometimes called a lava delta-- from behind the safety barrier
at the viewing area (August 16, top). From here, people are treated to wonderful views of
lava flowing into the sea and of tephra-jet
explosions when lava interacts violently with sea water. The viewing
area is safe, because it is atop an older sea cliff and beyond the
margin of the active lava bench. The viewers should NOT be wearing
shorts, however, because a fall onto glassy lava flows along the trail to
the viewing area could result in lacerated legs.
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16 August 2001
Lava continues to pour into sea at East Kupapa`u bench
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View looking southwest of the active bench and the newly
created viewing area behind a safety barrier near the sea
cliff. The two clouds of blue fume issue from skylights along the lava tube before it
drops onto the bench and spills into the sea. The viewing area will be
opened to the public on August 17.
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View looking west shows bench, coastal flat, and Pulama
pali. The bench is about 600 m long and more than 100 m wide. The
landward edge of the bench is marked by the former
sea cliff. In the large view (click "large" at right), a
small incandescent surface flow is visible on the bench behind the ocean-entry plume.
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30 August 2001
Aerial view of active flow lobe moving toward access road
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Active flow lobe is the thin, light gray strand inland of the access road. The
flow front is 150 m from the edge of the road.
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Aerial view showing relationship between access road and advancing flow lobe (light, shiny
gray).
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31 August 2001
Lava flow advancing toward Kalapana road
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Budding pahoehoe flow front slowly moving toward the Kalapana
road, which provides access to a viewing area for the East Kupapa`u ocean
entry.
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Ground view of access road with advancing flow (light shiny
gray) in the background. The flow front is 55 m from the edge of the road.
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Map of flows from Pu`u `O`o: June 2001

Large
map Map shows lava flows erupted during the 1983-present activity of Pu`u `O`o and
Kupaianaha. The flows active from December 17, 2000 through June 30, 2001 are shown in
red,
above and on Pulama pali and on the coastal plain,. Most of the recent flows are fed from
breakout points at 1920-1700 feet, above the pali in the northern part of the large red area.
Lava re-entered the sea just west of Kamokuna on January 21, 2001, but soon stopped when activity
shifted from the western to the eastern branch of the flow. Since then, activity
has been divided between the eastern and western branches. Breakouts from the
eastern tube system have destroyed hundreds of meters of the Royal Gardens
access road. Lava fed through the eastern system has been entering the ocean
since April 25, a few hundred meters northeast of Kupapa`u Point. Since then, a
large bench has developed at the E. Kupapa`u entry site. On May 31, a
tiny trickle of lava fed through the western tube system dripped into the water
about 500 m west of the Kamokuna bench but stopped within a day. Since then, all
lava entering the sea has gone through the E. Kupapa`u entry.
The shatter ring
is a prominent tumulus near the western branch of the active flow that is a handy reference point for some of our observations.
Eruption-viewing opportunities change constantly, so refer to this page
often. Those readers planning
a visit to Kilauea or Mauna Loa volcanoes can get much useful information from Hawai`i
Volcanoes National Park; be sure to click on the inDEPTH button.
The URL of this page is
http://hvo.wr.usgs.gov/multimedia/archive/2000/Aug/
Contact:
hvowebmaster@usgs.gov
Updated: 19 September 2001 (DAS)
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