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1 June 2003
This 'n that at Highcastle
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Left. A minute or two after lava has
broken from beneath crust and started to cascade down sea cliff at
Highcastle. Crust at very top of image is point of breakout at top of
cliff. Lava is gushing out, not simply oozing. Its volume is small,
however, so only a weak cascade ultimately develops. Width of flowing lava,
about 1.5 m. 0544. Right. Upper part of cascade is now two streams
that flow around cooler crust (see left image for early version of that
crust) and join below. See video. 0546. |
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Left. Same cascade as above, in
context of Highcastle entry. Steam rises from entry point. Lava flow covers
old beach and has built a narrow delta beyond. Lava flows under crust
across buried beach to point of entry. 0550. Right. About 13
minutes after cascade began, it has obviously slackened in both flux and
vigor. Image taken from same place as first image above but at less
magnification. Width of flowing lava, about 80 cm. 0557. |
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Views of arching, solidified toe of pahoehoe
in breakout just above Highcastle sea cliff. You can make up your own pet
name for this stony creature. Length of toe in image, 30 cm. 0600. |
4 June 2003
Highcastle lava delta and breakouts inland
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Left. Looking southeast across
Highcastle lava delta. Small breakout from inflating flow on surface of
delta is in lower right, and glow from one of two ocean entries creates
moderate plume of laze at front of delta. 0528. Right. Optical zoom
of lava entering water at entry site shown in left image. A small point is
being constructed by the lava at the front of the delta. 0541. |
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Left. Rising sun behind laze plume
from ocean entry at Highcastle lava delta. 0549. Right. Wide-angle
view of Highcastle lava delta looking southwest, taken from same point as
first image of May 25 and last image of May 22. Compare with those images
to see widening of lava delta. (Note: the other two images are not so
extreme a wide angle.) 0601. |
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Left. Family of lava toes breaking out
from sluggish Highcastle lobe 450 m inland from Highcastle delta. 0621. Right.
Close view of two small toes moving down moderate local slope, taken from
ground view. Width of moving lava, about 0.6 m. 0622. |
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Left. Ground-level view of leftmost
toe in right image above, but too close for comfort. Lava is dropping into
small depression. Width of dropping toe, 20 cm. 0623. Right.
Visitor from Chicago enjoying his last day in Hawai`i, observing channeled
breakout along east margin of Highcastle lobe 450 m inland of lava delta.
0625. |
5 June 2003
Upper flow field
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Left. Small hornito in West Gap Pit, west of crater of Pu`u `O`o. Hornito is about 50 cm high. 0929.
Right. Tongues of lava breaking out of upper Mother's Day flow at 2300-foot elevation. This lava, which has been stored in inflating flow
and has cooled slightly and lost some gas, will solidify to dense "blue pahoehoe." 1246. |
6 June 2003
Aerials of Highcastle and Pu`u `O`o
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Left. Aerial view looking north-northeast across Highcastle entry area. Lava delta is small, building out
from beach that is now covered by new flow. To west, the Highcastle and West Highcastle areas blend into one. 1308. Right. Looking west
into crater of Pu`u `O`o, showing several heavily fuming old spatter cones and other vents. 1314. |
7 June 2003
Cascades over old sea cliff at Highcastle
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Left. Small cascade on old sea cliff
at Highcastle feeds equally small surface flows on Highcastle lava delta.
In background is large tumulus on defunct West Highcastle delta. 0535. Right.
Base of cascade, taken from same place as left image but at higher
magnification 6 minutes later. 0541. |
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Left. Starting point for new cascade
slightly nearer camera than cascade shown above. This cascade started 5
minutes or less before image was taken. Lava gushes from crusted hot flow
at very brink of old sea cliff. Width of gush is about 1 m. 0553. Right.
Continuation of cascade in left image, only 2-3 m farther downstream. On
left, lava is starting to plummet to base of cliff. Width of view, about
2.5 m. 0554. |
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Left. Looking across top of cascade
shown above, with laze from ocean entries in background. Image taken at
approximate peak of activity. Compare with left image below, taken as lava
flux is waning. 0556. Right. Cascade shown in left image in
early morning sunlight. Image taken from same place as first image this
morning. 0602. |
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Left. Looking across top of cascade
shown above, with laze from ocean entries in background. Image taken as
lava flux is waning. Compare with left image above, taken as lava
flux was at its peak. 0606. Right. Start of same cascade as
shown to left but 3 minutes later. Crust is growing from right to left from
point of lava emergence (right side of image) as
flux declines, and sluggish lava develops ropes where gradient slackens.
Three minutes later, all lava was hidden by crust, and cascade was a mere
dribble. 0609. |
11 June 2003
Scenes at Highcastle on a beautiful morning
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Left. Looking southwest at main
ocean-entry point about halfway along front of Highcastle lava delta. Note,
however, that other smaller entries are also taking place. 0535. Right.
Same main entry area but with digital zoom. 0535. |
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Left. Seconds after small gushing
breakout has started about 50 m upstream of top of old Highcastle sea
cliff. Plate of crust surrounded by lava capped roof of small tube but
finally gave way. Width of plate of crust, about 1 m. 0546:54. Right.
Twenty seconds later, left prong of breakout is rapidly developing into
small channeled stream. 0547:14. |
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Left. Twenty-more seconds later, side
view of left prong of breakout shown above. Note developing wrinkles on
crust as flow slows on gentler slope. Width of stream, about 80 cm.
0547:34. Right. Head-on view of left prong of breakout, 106 seconds
after first image of breakout above. Note that plate of crust
remains intact, though it has slumped a little from its original position.
0548:40. |
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Left. Another breakout but in same
general area. This one has developed channeled flow and shows continued
growth of crust downstream from point of emergence from under crust. Width
of flow, about 1.3 m. 0559. Right. Same channeled breakout as shown
to left, showing streaming pattern in crust. 0601. |
13 June 2003
Start and finish of Mother's Day flow
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Left. Skylight in main Mother's Day
tube not far below place where lava first enters the tube. Figures in
distance are measuring flux of lava in tube using a VLF instrument. Right.
Eastern two-thirds of Highcastle lava delta. Point on delta is main entry
point for lava into water. |
1 June 2003
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June 1, 2003; 0545. Two strands of flowing lava come together to form single
cascade on upper part of old sea cliff at Highcastle. Still taken at 0546 shows same scene.
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7 June 2003
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June 7, 2003; 0555. Gushing start of cascade
shown in image taken at 0553. Lava comes from crusted flow to right. Width
of flowing lava, about 1 m.
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June 7, 2003; 0559. Downstream from first clip
about 2 m. Same as shown in image taken at 0554.
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Map of flows from Pu`u `O`o: 16 May 2003

Map shows lava flows erupted during 1983-present activity of Pu`u `O`o
and Kupaianaha (see
large map). Red colors, both dark and light, denote Mother's Day flow, which
began erupting on May 12, 2002 and continues to the present. The darkest color
represents flows active since January 21, 2003.
Most recent--and ongoing--activity has produced two flows, one along western
edge of flow field and one slightly farther east. Kohola flow, along western
margin, entered sea late on Valentine's Day to form short-lived Kohola ocean
entry. This flow shortened the road still more. Visitors now can drive to Holei Sea Arch, 1.1 km from Kohola flow, and walk
to see flow. Breakouts have been visible in various parts of Kohola flow,
shifting from time to time across width and length of flow.
Other dark red flow is main active part of Mother's Day flow. Fed by
breakouts from lava tube in main Mother's Day flow, it advanced along eastern
margin of main flow and down Pulama pali and Paliuli. Western of two forks below
Paliuli dripped over sea cliff at Highcastle on May 19, 2003, after map was
made.
Lava from earlier, pre-January 21, 2003 Mother's Day flow (light red) reached sea at West Highcastle early on July 19, at Wilipe`a early on
July 21, and at Highcastle on August 8. From near southwest base of Pu`u `O`o, Mother's Day flow passes along west side of flow field and into forest, where it started large wildfire in May that continued into late July. By June 10,
Mother's Day flow had reached base
of Paliuli, the steep slope and cliff below Pulama pali and just above coastal flat. At base of Paliuli, Mother's Day flow abruptly spread
laterally in series of small budding flows to cover an area nearly 2 km
wide, gradually moving seaward until West Highcastle and Wilipe`a lobes
finally reached water and started building lava deltas. Activity at West
Highcastle ended in early August, but entry began soon thereafter at Highcastle,
eventually burying tiny kipuka of Chain of Craters Road. Wilipe`a entry
died away slowly and had ended by mid-August. Highcastle and neighboring
Highcastle Stairs entries ended on about August 23. For a time there were no
active entries. Then Wilipe`a was reactivated on September 3 but stopped in
December. West Highcastle likewise renewed activity on September
16-17, died away during night of September 18-19, and returned soon
thereafter to continue through March 21. East arm of Mother's Day flow
branched from Highcastle lobe in late October and sent three fingers into ocean
at Highcastle on November 15, West Lae`apuki on November 19, and Lae`apuki on
November 20. Lae`apuki entries had stopped by November 29. If this sounds
like soap opera, the truth is even more confusing than the simplified version
of activity given here.
Eruption-viewing opportunities change constantly, refer to the HVO home page for
current information. Those readers planning a visit to Kilauea or Mauna Loa volcanoes can get much useful
information from Hawai`i Volcanoes National Park.
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