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1 August 2002
Lava, lava everywhere, not only at the coast

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Two streams of lava in Mother's Day flow pour down Pulama
pali inland of Paliuli, lighting the predawn (0448) sky in most spectacular
display of flow in some time. This is view visitors get from end of pavement
after short walk from parking area.
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West Highcastle bench. Left.
Lava dribble and falls into water off front of bench at 0524. Right.
Mostly crusted breakout on bench, and same falls shown in left image, with
dawning sky behind at 0528. |
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Wilipe`a bench. Left. View at
0543 from east end of bench, showing lava entries on east side of leading
tip of bench. Right. Visitors watch lava flow cover black sand beach
at west end of Wilipe`a bench, 0604. |
2 August 2002
Aerial view of active flow and benches, and a hornito or spatter cone

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Aerial view of active flow field between Wilipe`a and
West Highcastle benches and Paliuli. The shiny gray color of the new flows
makes it easy to distinguish them from the vegetated flows on left
(probably 600-900 years old) and the dark 1992-97 flows. View looks northeast.
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A roofed spatter cone--termed a hornito by some--built above
upper part of Mother's Day lava tube just southwest of Pu`u `O`o and about
10 km from Wilipe`a bench.
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5 August 2002
Viewers at Wilipe`a bench

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Viewers cluster atop sea cliff for best view of lava
entering sea off southwest part of Wilipe`a bench. 0539, just before dawn.
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6 August 2002
Lava near Highcastle

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Dawn over slowly advancing lava 170 m inland from eastern
Highcastle kipuka. 0541.
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Left. Toes of lava emerge from
pahoehoe along edge of Highcastle lobe of Mother's Day flow at 0551. Toes
are fed from liquid interior of flow, which is both moving seaward and
inflating. Right. View inland at 0552 from tip of Highcastle lobe.
In middle distance, tops of four or five Paliuli cascades are visible.
Pulama pali in background. |
7 August 2002
Mother's Day descent, and finger into the sea
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Left. Looking inland, over Paliuli (middleground)
to slope above. Steep slope is Pulama pali. View shows main branch of
Mother's Day flow. West branch is just left of view. Right. Shiny
active tongue of West Highcastle flow nears sea cliff on east side of West
Highcastle entry area. |
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Left. Only a matter of minutes now
before lava plunges down sea cliff to Pacific below. Right.
Tongue feeds dribble of lava onto rocky base of sea cliff. |
8 August 2002
Highcastle lobe, in night and day
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Left. Bubbly lava toe at leading edge
of most active tongue of Highcastle lobe at 0556. In large view, note
incandescent wrinkles in crust on lava. Width of view about 70 cm. Right.
Head-on view of most active tongue of Highcastle lobe, heading toward sea
but still 85 m away.
Pulama pali in background. 0603. |
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Left. Branch of most active tongue
burning vegetation at 0611. Right. Most active tongue, though
slithering quickly downslope, is dwarfed in context of entire flow field.
Pulama pali in background. 0622. |
Map of flows from Pu`u `O`o: 21 July 2002

Map shows lava flows erupted during the 1983-present activity of Pu`u `O`o
and Kupaianaha (see
large map). Lava from the Mother's Day flow (red flow on west side of flow field)
reached the sea at West Highcastle early on July 19 and at Wilipe`a early on
July 21. Active flows in May-July (shown in red) originate from two
sourcesthe area of the rootless shields and an area just southwest
of Pu`u `O`o. The two flows from the rootless shields are the Boundary flow,
the longer flow along the edge of the national park, and the HALP flow, which
moved into Royal Gardens subdivision on May 21. From near the southwest base of Pu`u `O`o, the
Mother's Day flow passes along the west side of the flow field and into the
forest, where it started a large wildfire in May that continued into late July. By June 10,
the Mother's Day flow had reached the base
of Paliuli, the steep slope and cliff below Pulama pali and just above the
coastal flat. At the base of Paliuli, the Mother's Day flow abruptly spread
laterally in a series of small budding flows to cover an area nearly 2 km
wide, gradually moving seaward until the West Highcastle and Wilipe`a lobes
finally reached the ocean and started building benches.
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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