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Cheap Hawaii Tickets offers the discerning Hawaii traveler complete Hawaii vacation packages to all the major Hawaiian islands at the absolute best prices. The truth is that wholesale ticket suppliers have the cheapest tickets but most retailers are marking them up drastically. We operate on a straight commission with no markup and we rely on volume to keep our prices as low as they are. Our wholesale suppliers have negotiated the best contract discount prices on bulk airline tickets, hotels, condos, resort properties, car rentals and local activities throughout Hawaii. We offer an array of packages to all the major Hawaiian islands from the continental United States that are assembled together with you by one of our trained staff members before your quote is issued. In this way we are able to produce a quote that's perfect for you and the process is painless and efficient. We're able to produce a Hawaii vacation package that's best suited to your specific needs at a price that is hard to beat because we live here. Having contracts with local suppliers that we have developed over the years assures that we can provide our customers the very best prices and finest Hawaii vacation packages. combine that with our wholesale airline ticket prices and you get Hawaii vacation deals that are hard to beat. We take pride in knowing that we have helped our customers find a Hawaii vacation package at the best possible price in the least amount of time and still be able to personalize it for them. We have found that our system allows for the best of both worlds. We use technology to communicate via email during the preliminary stages of the process and then finalize your vacation quote with personal contact via phone before your package is assembled. That way you'll get a personalized vacation package in the quickest amount of time for the least amount of money. 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Please fill out our Contact Form for a Hawaii Vacation Package quote Call toll free (866) 826-7900 to speak to one of our staff personally Kauai Vacation Rentals, Honeymoons, and Weddings Wholesale Hawaii Vacation Packages Cheap Hawaii Tickets · 3691 Emmalani Drive, Princeville, Hi, 96722 ·Toll Free: 866.826.7900 · 808.826.7900 Licensed Hawaii Travel Agency #TAR 5684 · Member of the Hawaii Visitors and Convention Bureau and the Kauai Chamber of Commerce info@cheaphawaiitickets.com resourses Hawaii Volcanoes National Park.Hawaii's Volcano Parks Let Visitors Go With The Flow Welcome to TBO.com. Skip directly to: our Keyword Search , Section Navigation , Content . TBO.com Life TBO.com WFLA The Tampa Tribune Search: Keyword Site News | Weather | Hurricane Guide | Things to Do | Sports | Jobs | Cars | Homes | Shopping | Classified Travel TBO.com Life Travel Hawaii's Volcano Parks Let Visitors Go With The Flow Skip directly to the full story . By TANYA BRICKING LEACH For The Associated Press Published: Dec 18, 2005 ADVERTISEMENT More from this channel: This feature requires the Macromedia Flash Plugin. Please visit http://www.macromedia.com/go/getflashplayer to download this plugin. Search our archives: Type keyword(s) 30 days 6 months 2005 2004 2003 2002 2001 2000 1999 1998 1997 1996 1995 1994 1993 1992 1991 1990 All Past 7 days most viewed | Tribune archive from 1990 VOLCANO, HAWAII - About the time jagged edges started poking through my T-shirt as I wormed my way through a tight spot in a lava tube, I began to wonder: What am I doing here? We could have been relaxing on the famous Green Sand Beach at South Point of the Big Island of Hawaii. But in the spirit of adventure, we were instead exploring the world underground. I had convinced my husband that it would be neat to go hiking to see flowing lava at the Kilauea Volcano on the first night of our weekend getaway, and then get up early the next morning to go caving in 1,000-year-old lava tubes. He was agreeable, even after twisting his ankle on the initial hiking excursion, which lasted past midnight. Once we got back to our cabin at Volcanoes National Park, we understood why each room had a Jacuzzi. But we weren't about to let our sore muscles get the best of us. Watching the orange glow of waxy-looking lava hiss into the ocean had intoxicated us. We wanted to see tunnels formed by the molten stuff. The Dawn Patrol So we caught just enough sleep to wake at the crack of dawn and drive to South Point in search of a labyrinth of lava tubes at a place called Kula Kai Caverns. To get there, we punched in a pass code and entered a remote neighborhood built on lava rock. Then we saw our guide's landmark, a thatched hut that looked like something out of "Gilligan's Island." Our tour guide, Kathlyn Richardson, led us into the yurt and handed us spelunking helmets, lights, gloves and kneepads to gear up. We looked like coal miners without the soot, and we were about to go on a two-hour spelunking tour. So she tested us a little. Would we like to try shimmying up parts of the cave and crawling around in tunnels? We were game. Let me just say my previous experience in caves was limited to a guided tour years earlier on a heavily traveled pathway at Kentucky's Mammoth Cave. Although it is considered the granddaddy of American caves - and the longest cave in the world - I saw only the easy-access "tourist" part of it. No shimmying through narrow passageways was involved. And I had seen Thurston Lava Tube, a major attraction on the drive around Crater Rim Drive at Hawaii Volcanoes National Park. But that was just a peek into a cavelike shell. I had never seen much of caves or could explain the difference between stalactites and stalagmites. Somehow, the idea of exploring a pitch-black volcanic cavern still appealed to me. That's just the kind of tourist Kula Kai Cavern founder Ric Elhard wants to educate. "I started crawling around in caves when I was 12 years old," said Elhard, a California native who bought property on the Big Island because he knew there were caves underneath it. He and other cavers have since mapped out miles of lava tubes that crisscross the area. "We're not doing big numbers, but we saw huge potential," Elhard said. "We want to be more of an educational tour. We want people to learn and understand about the archaeological aspects of caves." Treks Of Your Choice He and other guides lead small groups, even children as young as 5, through parts of the caves on tours that last from easy half-hour strolls to more challenging half-day explorations. When my husband and I were there, it was just the two of us, following Richardson into a braided maze she knew by heart and getting a taste of massive chambers and small spaces formed by volcanic gases rising through cooling magma 1,000 years ago. A National Park tour, it is not. It's a fledgling operation that's loosely organized, and sometimes the battery-powered lights on the well-used equipment go out. But it's definitely an adventure tour. We broke a sweat, despite the cool 68-degree temperature inside the cave, and had to watch our footing navigating craggy rocks that seemed to grow out from above and below. One of the most interesting parts was when we turned off our head lamps and sat in the dark, listening closely to dripping water and the sound of ourselves breathing. I'll admit I liked climbing and scrambling over loose rocks much better than belly-crawling through the tight spots. The crawling part made me think about being swallowed by hot lava as I tried to untangle myself from its pointy fingers. Underground Point Of View But squirming around on my hands and knees gave me a feeling not just for overcoming claustrophobia, but also for looking at a volcanic island from a different perspective. I thought about the cave dwellers who must have used the spaces for shelter. I wondered how long the kukui nuts, which contained oil that Hawaiians used to light like candles, had been left on the rock shelves that we passed. I pictured the lava flowing through the walls I could now touch. The tour captured my imagination. Yes, I could have spent the day relaxing on the beach. What I did instead made me feel like an explorer. And to me, discovering a world I had never seen before made the vacation feel complete. FOR LOVE OF LAVA KULA KAI CAVERNS AND LAVA TUBES: www.kulakai caverns.com or (808) 929-7539. Located off Highway 11 in Ocean View, Hawaii. Tours by appointment ranging from $15 half-hour walking tours to $95 half-day tours. The two-hour spelunking tour is $65. Discounts for Hawaii residents and groups. Wear a T-shirt, long pants and sturdy shoes. WHERE TO STAY: For the full Kilauea experience, stay in a B&B in Volcano Village or in a cabin at Hawaii Volcanoes National Park. •Carson's Volcano Cottages: www.carsonscottage.com or 1-800-845-5282 or (808) 967-7683. B&B accommodations, from one-room spaces to family cottages with kitchens and storybook cottages nestled in the tropical rain forest. Breakfast is served in a dining room beside the fire. Rates range from $115 to $170 a night. •Volcano House: (808) 967-7321. This historical hotel sits on the edge of a crater, and the rooms are heated by volcanic steam. Rooms range from $95 to $225. Its cabins are among the few available in the park, but the rooms are a bit worn. Cabins are $50. •Kilauea Military Camp: www.kmc-volcano.com or (808) 967-8333. A joint services recreation center in Volcanoes National Park, open to military members and Department of Defense workers and retirees. Rates are based on rank, and accommodations range from dorms to cottages. WHERE TO EAT: After a spelunking tour, drive to the Kona side of the island for food. •The Coffee Shack: A casual coffeehouse with a sweeping view of the ocean. The staff is friendly, and the portions are big. •Cafe Pesto in Hilo: Whether you're in Kawaihae near the harbor on the scenic South Kohala coast or in historic Hilo on the Big Island's east side, find this restaurant. It has gourmet pizzas, an assortment of pasta and seafood. Most items are about $10. •Ken's House of Pancakes: Ken's is like a local Denny's. It's open 24 hours a day, and most items are less than $7. 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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) |
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