Hawaii Volcano

Current update of the eruption of Kilauea Volcano, Hawai`i `o Eruption Summary Hazards History Panorama Images Eruption Update and Image Archive | deformation | images | maps | Pu`u `O`o camera | 0555 January 14[Note: Your observer will be way south of the border, almost astraddle the equator, for the next two weeks. The next regularly scheduled morning update will be on Monday, January 30. Updates may occur at irregular intervals in the interim.]The Full Wolf Moon is the brightest object visible this morning, for lava on Pulama pali is confined to small patches and rivulets in the west string of breakouts. The breakouts reache from about the 1400-foot elevation down to about the 900-foot elevation, with small lava patches down to about 300 feet, as noted by yesterday's field workers. Glow comes from just above the top of the pali, probably at about the 1900-foot elevation, and testifies to surface lava there, too. Yesterday's observers noted some lava along the far east side of the PKK flow just outside the national park at about the 200-foot elevation 3.8 km from the end of the Kalapana access road.Moderate glow comes from East Lae`apuki this morning. Lava rose from cracks that cut the front half of the delta on Thursday and added perhaps as much as 80 m to the west side of the delta. The observers estimated that at least a third of the delta is new or resurfaced by lava. Lava enters the ocean at numerous spots along most of the front of the delta, so that the laze plume is spread almost continuously along the water's edge. The delta is now about 500 m long (parallel to shore) but still only 140 m wide. The crater of Pu`u `O`o is badly socked in this morning, but glimpses appear of all vents except Beehive. Conditions were similar yesterday, and the field observers were skunked. They did witness, however, a breakout from the PKK tube at the base of the flank shield. It was not active at 0900, was going strong at ~1030, and was over by 1130. The breakout came from a shatter ring immediately down-tube from the bend in the tube at the base of the flank shield. This shatter ring may be the source for all the breakouts from the upper tube that have occurred since mid-December. The shatter ring is 60 m x 75 m across, and its southwest side is a 3-4-m-high, nearly vertical rubble wall. This area was very noisy, with cracking and scraping and lots of rock falling off, both during and after the breakout. Background volcanic tremor is about normal at Kilauea's summit this morning. Volcanic tremor is at a moderate level at Pu`u `O`o.Inflation at Kilauea's summit continued for the past 24 hours and has now recovered the 5.2 microradians lost during the deflation of January 9-10. In contrast, Pu`u `O`o is having a rocky, slow deflation that started midday January 12 and by this writing has lost almost 1 microradian. 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 December 19 Current Deformation Electronic Tilt Global Positioning System (GPS) Images and Chronology Looking for images you could swear you saw here but can't find now? Check Image Archive 13 January 2006 East Lae`apuki lava delta | med | large | | med | large | Left . Looking northeast across lava delta at East Lae`apuki. Note smooth, new surface on near part of delta, created when lava welled from cracks a couple of days ago. These cracks are shown in first image for January 6. Note also that most of delta front is source of laze; this is because lava pours into the water at many places. 0905. Right . Looking west at lava delta, showing how it nestles against cliff bounding embayment. Much of the cliff was created during collapse of earlier lava delta and adjacent "mainland" on November 28. As such, only part of the cliff is a true "sea cliff," formed by erosion. 0907. 6 January 2006 East Lae`apuki lava delta and Petunia skylight | med | large | | med | large | Left . Looking east across lava delta at East Lae`apuki. Note the cracks cutting the outer part of the delta. The cracks have formed in the last week or two as the delta has grown larger and become more unstable. Similar cracks cut the delta before its wholesale collapse on November 28, 2005. Steam (laze) rises at points where lava is entering the water. 0910. Right . Pretty Petunia skylight in roof of PKK lava tube, upper part of PKK flow. View looks downstream. Some of the lava visible through the skylight will eventually end up at East Lae`apuki 1-2 hr later. 1122. 29 December 2005 East Lae`apuki and MLK vent area | med | large | | med | large | Left . Lava delta at East Lae`apuki, built since November 28. White color on delta is from salt and other minerals precipitating on surface. Inland, note the scattered puffs of fume coming from points along lava tube feeding the delta. Actual point where tube enters delta is hidden by large laze plume. Note lopsided nature of delta; most is built right (east) of tube. Pulama pali in distance. 0938. Right . Treacherous lip of pit at MLK vent. Is it any wonder that geologists take care in this area? Southwest slope of Pu`u `O`o in background. 1016. 22 December 2005 East Lae`apuki and Pu`u `O`o area | med | large | | med | large | Left . Head-on view of East Lae`apuki lava delta. Four main ocean-entry points, and several smaller ones, generate plumes of laze, mainly steam. 1249. Right . Long-shore view of East Lae`apuki lava delta, looking east. Almost all of this delta has been rebuilt since the collapse of November 28. 1249. | med | large | | med | large | Left . Low-level fountaining in East Pond Vent on floor of Pu`u `O`o. Image taken through thick fume, which enhances red color. 1329. Right . Treacherous MLK vent area at southwest base of Pu`u `O`o (cone behind MLK crater.) Note highly cracked surface adjacent to MLK crater. In upper right is Kupaianaha shield, built in late 1980s. 1226. 16 December 2005 Growing lava delta and collapsing Pu`u `O`o | med | large | | med | large | Left . Aerial view looking west at new East Lae`apuki lava delta, built in scar left after collapse of original delta and adjacent old sea cliff on November 28. 0915. Right . Slump blocks on south rim of Pu`u `O`o's crater. Most of the south rim of the cone is badly cracked and waiting to fall, and gaping cracks also cut the south flank of the cone below the rim. 1048. 2 December 2005 East Lae`apuki and Pu`u `O`o | med | large | | med | large | Left . Aerial view of embayment left after destruction of east Lae`apuki lava delta on November 28. Compare with last image taken on November 1. Column of steam and other gases rises from site of new, growing lava delta. 1021. Right . Head-on aerial view of new lava delta and sea cliff behind. The cliff retreated several tens of meters during the November 28 collapse. 1021. | med | large | | med | large | Left . New lava delta and feeding stream of lava emerging from tube high on cliff. 1023. Right . Closer view lava spilling from tube and flowing down fan created by the stream. Note that stream flows into a new tube that is being created by cooling of the surface of the lava. 1023. | med | large | | med | large | Left . Incandescent hole at MLK vent at southwest base of Pu`u `O`o. Hole is 1-2 m across. 1201. Right . Aerial view of East Pond Vent in crater of Pu`u `O`o. 1251. Current Deformation Map of selected deformation stations Electronic Tiltmeter Pu`u `O`o experienced bumpy tilt on January 7, 8, and early January 9; the bumps average out to flat tilt. Uwekahuna inflated slightly until noon January 7, deflated in the afternoon, inflated until early January 8, and then flattened and stayed flat for most of the day. It then started to inflated before midnight and continued up until 2141 January 9. Then Uwekahuna started a rapid, large deflation that finally ended at 2345 January 10 after a loss of 5.2 microradians. Pu`u `O`o inflated during January 8, following Uwekahuna, but it did not plummet when the summit started to deflate, instead maintaining flat to gently declining tilt throughout January 10 and into the 11th. Kilauea's summit began to inflate steeply at 2345 January 10, ending the deflation. The inflation continued through January 11-12-13 and into January 14 and had recovered all the tilt lost by the January 9-10 deflation by early January 14. Pu`u `O`o had pretty flat tilt until about noon January 11 and then began a slow inflation that continued until late morning January 12. The tilt that more or less stabilized before dropping a little that night and through January 13 into January 14, though the deflation was very irregular. 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. Global Positioning System (GPS) Two years of data are shown in the plot. Between June 2003 and July 2004 the lengthening between the two stations was generally at a gradually increasing rate. The distance then became stable for nearly a month, but then extension resumed at a slightly slower rate than before the brief stable period. Extension picked up significantly in December 2004 and continued to lengthen rapidly until late February 2005. Then the line rather abruptly started to contract. The contraction ended in mid-March 2005, and the line remained steady until early May, when it began to lengthen once more. The lengthening continued until early July 2005, when the distance stabilized, coincident with a flattening of the tilt at Uwekahuna. Extension then resumed at a quickened rate in late July-early August 2005 and continued to late September. Then the rate of lengthening sharply reduced and perhaps even became zero for a time. Then, in November 2005, the line began to lengthen once more, only to stabilize once more at the end of the year. This graph shows the change in distance between two Global Positioning System (GPS) stations located on opposite ides 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. For more information on how electronic tiltmeters and GPS receivers help monitor the deformation of Kilauea and Mauna Loa volcanoes, see a summary of the inflation-deflation of magma chambers . Maps of lava-flow field, Kilauea Volcano Map of flows from Pu`u `O`o: 19 December 2005 Map shows lava flows erupted during 1983-present activity of Pu`u `O`o and Kupaianaha ( see large map ). Yellow, brown, and red colors indicate lava flows erupted from October 2003 to December 16, 2005. Yellow indicates the currently active Kuhio (PKK) flow, active most of the time from March 20, 2004 to the present. The east and west arms of the PKK flow, once widely separated, began to merge and overlap on the coastal flat in March 2005. The east arm feeds the East Lae`apuki ocean entry. Activity on the west arm declined through mid-August, and the last surface flow on that arm was observed on August 21. The recent (November-December 2005) breakouts on Pulama pali described as "eastern" and "western" are all on the east arm of the PKK flow. The brown shade denotes Martin Luther King (MLK ) flows, which first erupted in January 2004 from flank vents on the south slope of Pu`u `O`o. Since then, several more vents have formed in the MLK area and continue to erupt intermittently. Red indicates the Mother's Day and Banana flows, last active in September 2004. Short flows from the crater, West Gap, and Puka Nui vents are also shown in red. In recent months, only the Puka Nui vent has produced infrequent, small flows. Map of Pu`u `O`o and vicinity: 19 December 2005 Map shows vents, lava flows, and other features near Pu`u `O`o frequently referred to in updates ( see large map ). These features can change quickly, but this map should help those viewers lost in the terminology. The vents, lava tubes, and flows active in 2005 include the numbered vents in the crater, the MLK vent complex and associated flows, the Puka Nui vent, and the upper Kuhio (PKK) tube, which feeds the lava flows eventually reaching the ocean. 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 January 2006 (DAS)

Lahaina Hotels Lahaina HI

Lahaina HI Hotels - Discount Hotels in Lahaina HI Affiliate Program E-mail Us! Toll Free | 1-877-372-1115 Hotels By City.com Home Hotels Airfares Car Rentals Vacations Last Minute Deals Hot Rate Hotels Book By Phone Tell A Friend Bookmark Home > US Hotels > Hawaii Hotels > Lahaina Hotels Lahaina HI Hotels Hotels All hot rate hotels are outlined in yellow . Hot Rates Regular Rates Airport Pet Friendly Family Sort by: Name Star Rating Price Best Western Pioneer Inn 658 Wharf Street, Lahaina Hotels, HI US, 96761 Located at the waters edge across from the famous Lahaina Harbor and next to Banyan Tree Park (the oldest Banyan Tree in Hawaii), the Best Western Pioneer ...More hotel info Kaanapali Beach Hotel 2525 Kaanapali Parkway, Lahaina Hotels, HI US, 96761 Ocean front on the best stretch of world-famous Ka'anapali Beach, the 430 room hotel was awarded the "Most Hawaiian Hotel" in the state by the Waiaha Foundation. ...More hotel info Lahaina Shores Beach Resort 475 Front Street, Lahaina Hotels, US, 96761 MARKETING DESCRIPTION This plantation - style mansion turned resort is the only beachfront hotel located in the historic whaling town of Lahaina. Savvy ...More hotel info Marriott Maui Ocean Club 100 Nohea Kai Drive, Lahaina Hotels, US, 96761 The Maui Marriott Resort and Ocean Club is a casual, full-service resort located on breathtaking Kaanapali Beach directly opposite the thirty-six hole ...More hotel info Ohana Maui Islander Hotel 660 Wainee Street, Lahaina Hotels, US, 96761 The Ohana Maui Islander Hotel Is Away From It All, But Close To Everything. Beautifully Landscaped On 10 Acres, The Grounds Are A Hawaiian Haven Of ...More hotel info Outrigger Royal Kahana Resort 4365 Lower Honoapiilani Road, Lahaina Hotels, US, 96761 vip International S P O T L I G H T Outrigger Royal Kahana Resort -the marc Resorts Royal Kahana Is A Beachfront Property Surrounded By Lush Landscaping ...More hotel info Sheraton Maui Resort 2605 Kaanapali Pkwy, Lahaina Hotels, US, 96761 The Sheraton Maui us an ideal, 510-room resort on 23 beachfront acres, offering spectacular views of white sand, blue Pacific Ocean, and neighboring islands ...More hotel info More Lahaina Hotels City: Check In: Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 Check Out: Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 Advanced Search Submit Navigation Home Travel Forum Hotel Search How To Book U.S. Hotels Canada Hotels Europe Hotels Austrailia Hotels International Hotels Hotels By Chain Disney Hotels Travel Tools Lahaina Hotels Help Cancel Reservation Contact Us Privacy Policy City Guide Shows and Events News Letter Name: Email: Learn More Travel Tips Tip 1 - Book Early and Save. Booking early on Lahaina Hotels is no different then booking early on Airfares. Sometimes you can save a lot of money by preplanning your trip and looking for the best rate in advance. Tip 2 - After you make a Lahaina hotel reservation you will receive a confirmation email. This email has valuable information like your confirmation number, and the Hotel's phone number. Print a copy of this email and take it along to confirm your reservation with the hotel. Tip 3 - If a Lahaina hotel shows no availability it may mean that the Lahaina hotel requires you to stay more then 2 nights. Try increasing the number of nights, you may find rooms are available. Tip 4 - Most of the time your credit card will not be billed until you check out of the hotel. Exceptions to this are the best rate guaranteed hotels which are prepaid to reserve the room. More Tips Home | Airfares | Car Rentals | Hot Rates | Last Minute Travel Deals | City Guides | Cancel Reservation | Help © Hotels By City.com 2005, All Rights Reserved

Hawaii Rental

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Tropic Hawaiian

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Hawaii Honeymoon

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