Hawaii honeymoon. Princeville Honeymoon

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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)

Hawaii Wedding

"Destination Wedding in Hawaii" planning articles ask the newlyweds bachelor/ette parties beauty & health bridal party bridal shower catering & cakes ceremony ceremony vows consultants craft & decorations destination weddings engagement flowers formalwear & attire general planning invitations jewelry & accessories legal & financial music & dance photo & video reception rehearsal dinners relationships traditions & customs travel & honeymoon vow renewals wedding song collections top songs of 2005 wedding prose & poetry vows & ceremonies photo gallery favor ideas local vendors wedding blogs & websites on sale this week ! 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Hewitt Inspirational Invitations Invitation Papers Jewelry Keepsakes Lillian Rose Music & Books Napkins & Coasters Party Supplies Pens & Bases Photograph Albums Picture Frames Placecards Placecard Frames Placecard Holders Programs & Bulletins Reception Essentials Ribbons & Bows Ring Pillows Ringbearer Gifts Rose Petals Shoes & Sandals Shower Activities Stationery Thank You Notes Tiaras Tussie Mussies Unity Candles ... over 1500 items ! Main > Destination Weddings > Destination Wedding in Hawaii Destination Wedding in Hawaii Home | Submit Search Written by Global Aloha Weddings A destination wedding in Hawaii is fast becoming the choice for couples from all around the world to say "I DO." Brides see themselves in a simple Hawaiian Wedding Dress, draped in a fragrant flower lei and with a Haku (head lei) veil of white orchids to accent her bouquet. Envisioning an oceanfront gazebo adorned with tropical flowers, she can almost hear the clear falsetto voices singing the Hawaiian Wedding Song- first in English, then in Hawaiian. The Bride and Groom kiss and are whisked away in an Outrigger Canoe into the sunset. Imagine the video of this ceremony! Just a romantic notion? Too far, too costly, too complicated? Not really, the vacation location wedding/honeymoon is becoming more popular and is usually less expensive than the big family hometown wedding-reception-dinner extravaganzas of the 80's. It can also be a lot more fun for everyone. If a Hawaiian wedding is your dream, a good place to start is with one of the many wedding planners in the islands. Try the First Hawaiian Wedding and Bridal Directory, or type "Hawaiian Weddings" into the search field in Yahoo. According to Scott Tambling, a local coordinator who has planned literally thousands of Hawaiian weddings, "the best place to start is with your making your travel and room arrangements. Once you have a definite date, you can contact a reputable wedding company such as Global Aloha Weddings and make arrangements for your ceremony." Tambling suggests you shop around to compare prices and packages and says "a couple can easily arrange their dream ceremony, complete with professional photography and videography for under $1000." Tambling goes on to say "Picking an island is another question that is hard for people who have never been to Hawaii before." He suggests you have your ceremony and reception if any on Oahu (the island on which the city of Honolulu and the resort area of Waikiki is based) and then fly over to Maui, Kauai or the Big Island of Hawaii for an official honeymoon. "The prices for wedding services are generally much higher on the outer islands and it is easier to obtain a marriage license in Honolulu. It also enables the couple to visit more than one island and really have a honeymoon within a honeymoon." The most popular sites on Oahu include Diamond Head Park, at the end of Waikiki, best of all it is free of charge; The Royal Hawaiian Hotel, for a more elaborate ceremony, but on the expensive side; and Haiku Gardens, in the Tropical Forests of the Windward Side of the Island. Another option is to have your ceremony onboard one of the many pleasure boats based in Waikiki. A wedding at sea with the Hawaiian sunset as a backdrop can make wedding photos appear as if out of a Fairy tale. To begin planning, answer the following: How many will attend? What is your budget? Where will you stay, hotel or condo? How does the wedding look in your dreams? On the beach, in a Gazebo or Church, by a waterfall or a rain forest, at sunset or on a bright Hawaiian morning? What type of amenities do you desire, photography, videography, florals, entertainment and transportation? These are the questions a wedding planner will need to get your "vision" and put together a proposal just for you. Want to be notified when new articles are added? Find Related Items at the UW Wedding Mall Ask a question regarding this topic! Read more articles on this topic See what others say about Destination Weddings! Rate this article: 5 -- Excellent 4 -- Very Good 3 -- Good 2 -- Fair 1 -- Poor Section Jump: Ask the Newlyweds General Planning Beauty and Health Invitations and Announcements Bridal Party (for Bride/Groom) Jewelry and Accessories Bridal Party (for Attendants) Legal and Financial Catering and Cakes Music and Dance Wedding Song & Dance Suggestions Ceremony Photography and Videography Ceremony Vows Traditional Vows Non-Traditional Vows Personalized Vows & Cermonies Specialty Passages TV & Movie Vows Reception Checklists Rehearsals Consultants and Coordinators Relationships Crafts and Decorations Travel and Honeymoon Destination Weddings Traditions, Themes & Customs African American Weddings Christian Weddings Interfaith Weddings Jewish Weddings Military Weddings Renaissance/Victorial Weddings Engagement Showers & Bachelor/ette Parties Co-ed Fun Activities Design & Create Activities Ice Breaker Activities Just for Fun Activities Personalized Games Wild & Bachelorette Activities Flowers Vow Renewals and Anniversaries Formalwear and Attire Miscellaneous Guests Your Wedding on TV community | shopping | articles | stories | site index | search | coupon club | couple pages | local services | contact us © 1996-2005 - All Rights Reserved UltimatePublishing.com - Legal Information

Lanai Island of Lanai

Lanai Island CRAMP is developing and applying standard scientific techniques that will enable us to compare the results of many different coral reef studies. This site will look much better in a browser that supports web standards , but it is accessible to any browser or Internet device. please scroll down to view the web page home overview results study sites bibliography search Manele-Hulopoe Shipwreck Home > Study Sites > Lanai Island of Lanai CRAMP is not monitoring any sites on Lanai at thepresent time. Two sites, however, have been monitored previously. Hulopoe-Manele has been monitored by Dr. Richard Brock and by the State of Hawaii, Division ofAquatic Resources (HDAR) for a number of years. A second site at ShipwreckBeach has been monitored by HDAR. These studies could form abasis for future work on Lanai. View a photo of Lanai and Molokai from space. Geographic Name: Lanai CRAMP site code: La Geographic Location: (20° 50'N, 157° 57'W) Lanai is located west of Maui and approximately 15 km south of Molokai. Physical Features (Physiography): Lanai is the sixth largest of the eightmain Hawaiian Islands with an area of 36,520 ha. Lanai Island is the emergentportion of a single volcano. The highest point is Lanaihale Peak at 1020 m (3370ft). Island slopes on the easterly side are steep and cutby gulches. Western slopes are gentler. The south central portion of the islandbetween elevations of 300 m and 600 m is a flat plain known as the PalawaiBasin, which was the major pineapple-growing region of the island untilrecently. Reef Structure, Habitat Classification: Reef development is best alongthe north and north-east coasts because these areas fall into the "waveshadow" of Molokai and Maui and are partially protected from the winternorth swell. Sandy beaches occur along the he north and northwest coastline.Coral reefs are less developed on the south and west sides of the island due toexposure to the summer south swell. Steep cliffs occur along the west and southcoasts. These are eroding volcanic coastlines due to extreme wave erosion andpresence of deep water offshore. Physical Oceanography: North shores partially protected by Molokai andMaui from winter storm surf. South shores receive full impact of summer southswell. Storm surf from Hurricane Iniki damaged reef communities along the southcoast in September 1992. Recovery of the damaged areas took nearly 5 years. Adjacent Land Tenure, Land Use: Most of the land on Lanai (98%) is ownedby the Castle and Cooke Inc., a privately held company headed by David Murdock.David Murdock has announced plans to build new roads, sidewalks and apartmenthouses on the island ("Massive Investment Planed for Lanai" by FrankCho, Honolulu Advertiser, Nov. 19, 2000, p. A1). Approximately one-fifth of the island was formerly undercultivation for pineapple, but economics led to abandonment of pineapple growingand a shift to development of resorts and diversified agriculture. Human Use Patterns: Commercial tours originating on Maui conduct snorkel,SCUBA and fishing excursions to Lanai. Increased resort development is leadingto more frequent use by visitors and residents on Lanai. Private boats fromvarious islands frequent Manele Harbor and visit various sites along the Lanaicoastline. Sustenance fishing and gathering of seaweed and opihi (limpets) is acommon activity by local residents. Economic Value and Social Benefits: The recent phasing out of pineappleand shift toward resort development places increased economic value on the reefsas resource for tourist development. Some of the best diving in Hawaiian watersis found off Lanai, which is a regular destination for many diving and fishingcharters coming from Maui. Large beds of the black corals Antipathesdichotoma and Antipathes grandis occur at depths of 40 m to 110 m offthe north coast. Status (Degree of Legal Protection): Open access for most of thecoastline. The submerged lands and overlying waters of Hulopoe Bay and ManeleBay are regulated as a Marine Life Conservation District. Manele Boat Harbor hasbeen designated as a Marine Fisheries Management Area. Management Concerns: The major focus is on human use, especially inthose areas with good reef development. Concern over exploitation of the richreef areas of Hulopoe and Manele Bays led to declaration of Hulopoe Bay andManele Bay as Marine Life Conservation Districts (MLCDs) in 1976. With thedemise of pineapple growing and the shift to resort and residential development, there isincreasing focus on effects of increasing human contact with the reefs andincreasing resort development. The rich reefs of Lanai are increasingly beingvisited by excursion boats from Maui.

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