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Note: Check Photo
Glossary or a good dictionary for any terms unfamiliar to you. See
Maps and accompanying caption for place names.
Maps updated on August 24
Looking for images you could swear you saw here but can't find now? Check
Image
Archive
8 October 2004
Pu`u `O`o and PKK
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Left. Fume, thick enough to
require a gas mask, issues from cracks between June 25 spatter cone
and south base of Pu`u `O`o, visible at upper right edge of image.
Sulfur lines many cracks. 0814.
Right. Aerial view looking northwestward at Pu`u `O`o. Lava
flows surround lighter cone, made of scoria and spatter. Part of
crater visible in upper right; largest fume column comes from East
Pond Vent. June 25 cone, shown in left image, is barely visible at
distant base of Pu`u `O`o. 1242. |
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Left. Small breakout along edge
of PKK flow at 1650-foot elevation on Pulama pali. Ferns grow on
flow surface about 2 yr old. 0959.
Right. Another breakout within confines of PKK flow at same
elevation. 1001. |
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Left. Sluggish lava emerges from
elephant-skinned toe of pahoehoe, 1540-foot elevation, Pulama pali.
Such sluggish lava is common in this area and reflects somewhat
cooler temperature than for the breakouts shown above.
Right. Several small breakouts near east edge of PKK flow at
1540-foot elevation. Note mound of small tongues built over past
several days. 1016. |
27 September 2004
Harvest Moon through vog
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Full Harvest Moon typically appears brown-yellow through smoke from burning fields after harvest. At Kilauea,
that color often indicates vog. In these views, nearly full moon takes on dirty amber
cast as viewed through plume of vog
coming from Pu`u `O`o. Photo location is Kealakomo overlook. Left. Just starting to set behind Mauna Loa's southwest rift zone. 0515:30.
Right. Going, going... 0516:14. |
24 September 2004
Down the PKK flow from Puka Nui
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Left. June 25 spatter cone near
Puka Nui on south side of Pu`u `O`o. This cone grew substantially in
past week and is emitting sloshing sounds from lava just below it.
Flank of Pu`u `O`o in background, through fume. Figure preparing to
take image shown to right. 0955.
Right. Close view of hole in June 25 spatter cone. 0959. |
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Left. Looking up PKK lava tube
toward Pu`u `O`o (upper left). Newly formed skylight in lower left.
Fume and altered rock (white) define course of tube. 1431.
Right. Small breakout in western arm of PKK flow downstream
from area shown in left image. Pu`u `O`o in background. 0914. |
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Left. Aerial view of several
breakouts near terminus of western arm of PKK flow. Note the two
distinctly different shades of gray. Darker hue is older crust, but
lava is still flowing under it. 1258.
Right. Aerial view looking up the western arm of PKK flow
(center of image, lighter toned than surroundings. Terminus is along
small kipuka in lower center. Pu`u `O`o in background. 0856. |
Map of selected deformation stations
Electronic Tiltmeter
The
Uwekahuna tilt flattened early on October 6 and remained flat until
October 7. Pu`u `O`o showed net deflation through the 6th and into
the 7th, with a midday deflation-inflation superposed on the overall
trend. Both stations deflated for most of October 7, Pu`u `O`o
eventually losing about 0.8 microradians since late October 6 and
1.3 microradians since early October 5. The deflation turned into
inflation in the afternoon of October 7 at Pu`u `O`o and in the
evening at Uwekahuna. The inflation continued into the morning of October 8.
Then the tilt at Pu`u `O`o leveled off, and both stations showed
flat tilt into October 9. The tilt remained flat at Uwekahuna
through the 9th and into October 10, but it deflated irregularly at
Pu`u `O`o during the same time. Pu`u `O`o continued to deflate until
just before noon and then started to inflate. The inflation lasted
until early October 11, when it turned over into slow deflation.
Uwekahuna was flat to gently deflating for the first half of October
10, but it then began an inflation that lasted into the 11th. The
tilt at Uwekahuna leveled off early on October 11, and that at Pu`u
`O`o started to deflate. A M4.0 earthquake at 1020 caused a spike at
Uwekahuna and a permanent offset of about 0.3 microradians at Pu`u`
O`o. Later in the day, heavy rain at Pu`u `O`o, about 18 cm in 5
hours, induced a spurious tilt that clouded the Pu`u `O`o record for
the rest of the day and into October 12. Uwekahuna maintained its flat
tilt into October 12. Another earthquake, of M4.5, offset both
tiltmeters at 1318 on the 12th. Tilt trends continued after the
earthquake. Uwekahuna slowly inflated through October 13 into
October 14. Pu`u `O`o, on the other hand, continued its recovery
from the October 11 rainfall, eventually bottoming out at midday on
October 13 and starting a slow inflation that lasted into the 14th. |
This graph shows the radial tilt at Uwekahuna (UWE), on the northwest
rim of Kilauea's caldera, and at Pu`u `O`o cone (POC), on the northwest
flank of the active vent along the east rift zone, as recorded by
continuously operating electronic tiltmeters. Positive changes indicate
inflation of the magma storage areas beneath the caldera or Pu`u
`O`o. Data are shown for a one-week period. A long-term trend of
constant-rate, large deflation at Pu`u `O`o used to be removed for
scale reasons, but starting on May 24, 2002, the tilt is shown as
recorded, including the long-term deflation. The graph is refreshed
at the same time as the eruption update at the top of this page,
usually daily. The Y-axis is in microradians, an angular measure
in parts per million; for example, one microradian represents the
tilt of a 1-km-long bar, one end of which is lifted up or down 1
mm.
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Global Positioning System (GPS)
Two years of data are shown in the plot.
Slow inflation ended in late May 2002, and by late June deflation
began, causing the distance to shorten gradually. The distance may
have lengthened a little in September and early October 2002 before
resuming its slow contraction. Slow lengthening resumed in
mid-November and continued for a month or so. A brief period of
contraction followed, but by early January 2003 the distance had
become stable. Thereafter it started to lengthen as the summit began
to swell. The lengthening has been at a gradually increasing rate,
broken only by a brief period of slowing in March 2004. Starting in
late April or May, the rate of extension noticeably picked up but
then slowed to its normal rate. At the end of July, the extension
ended rather abruptly, and currently very slow contraction is taking
place. |
This graph shows the change in distance between two Global Positioning
System (GPS) stations located on opposite sides of Kilauea's caldera.
A rapid increase in distance can be interpreted as inflation of
the summit magma reservoir. The graph is refreshed at the same time
as the eruption update at the top of this page, usually daily.
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Map of flows from Pu`u `O`o: 24 August 2004
Map shows lava flows erupted during 1983-present activity of Pu`u `O`o
and Kupaianaha (see
large map).
Shades of red and bright yellow denote Mother's Day flow field, which began erupting on May 12,
2002 and continues to the present. Darkest red indicates lava flows
erupted in November 2003-24 August 2004, including the labeled Banana flow,
which developed gradually starting in the middle of April. Orange shade
denotes MLK flow, erupted in January and, in brief spurts, subsequently. Yellow shade indicates Kuhio (PKK) flow, active most of the time from March 20 to
August
24. As of August 24, most activity was located in the Banana flow, fed by the Banana branch of the Mother's Day
tube. The PKK flow remains active, too.
Through September and into early October 2003, lava was moving along
the east and west sides of the Mother's Day flow. The east-side lava (known
as the August 9 breakout) came from the August 9 rootless shield, itself
fed by the main Mother's Day tube from Pu`u `O`o. The west side lava,
known as the Kohola arm of the Mother's Day flow, branched off the tube
system below the rootless shield.
In early October 2003, the August 9 breakout stopped moving, the Kohola
died back to a trickle, and the one labeled rootless shield gained prominence.
By October 16, however, the shield had partly collapsed, leaving several
drained perched ponds behind. Upstream from the shield, many hornitos
and small flows formed over the Mother's Day tube. Soon thereafter, other
rootless shields began to form over the Mother's Day, August 9, and Kohola
tubes.
New vents opened at the southern base of Pu`u `O`o on January 19 and
fed Martin Luther King (MLK) flows, which remained active until March
5. Several small vents formed during this time. On March 20, Kuhio (PKK) flow originated from two vents, main one about 250
m south of base of Pu`u `O`o. This flow has remained active most of the
time to the August 24 date of this map.
The Banana flow developed from breakouts from the Mother's Day lava tube,
centered near the former Banana Tree kipuka. The breakouts become prominent
in the middle of April, and lava started down Pulama pali shortly thereafter.
This is the time that we assigned the name Banana to the flow.
Vents in West Gap Pit became active in early October, were quiet for
3 weeks, and then resumed intermittent activity that continued well into
December. Other vents were also sporadically active in Puka Nui (near
West Gap Pit) and in the crater of Pu`u `O`o.
Map of Pu`u `O`o and vicinity: 24 August 2004
Map shows vents, lava flows, and other features near Pu`u `O`o frequently
referred to in updates (see
large map). These features change often, but this map should help
those viewers lost in the terminology. The cones in West Gap are just
outside the boundary of the crater--the oval-shaped depression containing
the seven numbered vents (now down to 6, as Humble Vent has been buried
by a mound of lava flows erupted from Dave's Pit/Vent in March. Red color
denotes flows--the Mother's Day flows--erupted since May 12, 2002. Light
orange color indicates episode-55 flows erupted between March 1997 and
August 2002 (exclusive of Mother's Day flows). Darker orange represents MLK
flows; yellow, PKK flow; purple, Puka Nui flow. Vents for these sets of flows shown
by indicated symbols. Gray shows flows of earlier episodes.
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.
The URL of this page is http://hvo.wr.usgs.gov/kilauea/update/
Contact: hvowebmaster@usgs.gov
Updated: 14 October 2004 (DAS)
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