Waikiki Beach Marriott Resort

Overview of Waikiki Beach Marriott Resort & Spa Traditions established by Queen Lili'uokalani, the last Hawaiian monarch, continue to flourish at our resort. home over view -- -- Let us show you exclusive offers & updates tailored to your interests. resort services fast facts testimonials map & directions A century ago, Queen Lili'uokalani, the last Hawaiian monarch, inherited the lands at Hamohamo, the area in which the Waikiki Beach Marriott Resort now stands, from her grandfather, 'Aikanaka. The land on which the Hotel is directly built was once the Ku'ekaunahi stream, which ran through the Queen's property. There were two summer homes on Lili'uokalani's property, one called Kealohilani and the other Paoakalani (literally translated as "heavenly fragrance"). Here she retreated to relax and informally entertain family, friends, and on occasion, visiting royalty. She also spent much of her time composing her songs and translating Hawaiian stories into English, surrounded by lily ponds and elaborate gardens, and when the trade winds blew, the fragrance of the topical flowers was carried throughout the estate. According to Queen Lili'uokalani, the large inviting living room was a place where "all could gather in joy and hospitality." Her home served as a comforting getaway from the pressures of business at I'olani Palace, several miles away. Nearby stood another one-story guest cottage, Kealohilani ("heavenly brightness"), where visitors enjoyed the tranquility of old Hawaii. In 1966, the Lili'uokalani Trust revealed plans for turning 16 acres of "old Waikiki" into a multi-million dollar resort development. American International Travel Services, Inc. (AITS) broke ground at this site in 1968 with plans for a twin towers, 23-story hotel at a cost of $12 million. Only one tower was initially completed. In October 1971, and at a cost of close to double the original estimate, the hotel officially opened. The grand opening ceremony took place on February 9-10, 1972. Reverend Abraham Akaka of the Kawaiahao Church conducted the blessing in the Garden Courtyard and Princess Abigail Kawananakoa, the niece of the late Queen Lili'uokalani, ceremoniously untied the maile lei. Eight years later, in 1979, the Kuhio Tower was added to the Resort, bringing the total room count to 1,346. In November 2000, Marriott International, Inc. assumed management of the hotel. Today, the area surrounding the resort bears little resemblance to the neighborhood at the turn of the century, but the traditions established by the queen continues to flourish at our resort. Diverse food and beverage outlets Business Center 24-hour Internet access 24-hour Fitness Center Live Entertainment Hawaiian cultural activities Concierge services Shops and Boutiques Two heated fresh-water swimming pools Valet service In-room safe deposit box Rental car desk 24-hour Laundromat Doctors On-Call medical service Property Address Waikiki Beach Marriott Resort and Spa 2552 Kalakaua Avenue Honolulu, Hawaii 96815 Telephone (808) 922-6611 Phone (808) 921-5255 Facsimile 1-800-367-5370 Toll Free Reservations in the Continental U.S. & Canada Website: www.MarriottWaikiki.com Credit Cards Accepted American Express, Diners Club, JCB, Mastercard, Visa and Discover. Hotel Tax 11.41% Location Overlooking Waikiki Beach near Diamond Head. Located on 5.2 acres of prime Waikiki property. Eight miles from Honolulu International Airport. Built October 1971 Architect Shimokawa Architects Date Marriott Assumed Management November 2000 Number of Rooms 1,310 rooms Kealohilani Tower Floors: 25 Rooms: 656 Suites: 10 Non-smoking rooms: 452 ADA Rooms: 5 Paoakalani Tower Floors: 33 Rooms: 654 Suites: 3 Non-smoking rooms: 326 ADA Rooms: 22 home resort overview accommodations check rates reserve now packages specials meetings & events weddings spa olakino things to do resort dining resort activities news press room take a tour contact privacy policy site map 2552 Kalakaua Avenue Honolulu, Hawaii 96815-3699 RES 1.800.367.5370 PH: 1.808.922.6611 FAX: 1.808.921-5255 ©2005 Waikiki Beach Marriott Resort & Spa Developed by Symbolic

Hawaii Resort and Spa

Diamond Hawaii Resort and Spa: Wailea, HI Hotel search select review reserve confirm Print this page We're here 24/7 Book online or call: 800-456-7029 Privacy Policy Hotel Details Diamond Hawaii Resort and Spa 555 KAUKAHI STREET Wailea, HI 96753 Map this Property South Maui: Wailea / Makena Rates from $269 starting Fri, Jan 27 Price this hotel = Required * Hotel Only Flight + Hotel Book Flight + Hotel together and save! * From: To: Maui, HI Choose a different city for your hotel I prefer to stay in a city other than my destination airport. 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(Maximum 6 travelers) Rooms: 1 2 3 4 Room 1: Adults (18+) Adults (18-64) 1 2 3 4 5 6 Children (0-17) Children (2-17) 0 1 2 3 4 5 Seniors (65+) 0 1 2 3 4 5 6 Room 2: Adults (18+) Adults (18-64) 1 2 3 4 5 6 Children (0-17) Children (2-17) 0 1 2 3 4 5 Seniors (65+) 0 1 2 3 4 5 6 Room 3: Adults (18+) Adults (18-64) 1 2 3 4 5 6 Children (0-17) Children (2-17) 0 1 2 3 4 5 Seniors (65+) 0 1 2 3 4 5 6 Room 4: Adults (18+) Adults (18-64) 1 2 3 4 5 6 Children (0-17) Children (2-17) 0 1 2 3 4 5 Seniors (65+) 0 1 2 3 4 5 6 Price this Flight+Hotel Price this Hotel Rates will be based on single or double occupancy. Extra person charges may apply. Features Photos Maps & Directions Hotel Description | Hotel Amenities | Dining Options Hotel Description Star Rating Traveler Reviews: Read 3 Reviews More Photos 72 rooms, 2 floors The Japanese-themed all-suite Diamond Resort Hawaii is comprised of 15 acres of landscaped grounds nestled 300 feet above the coast of Wailea, approximately 20 miles from Kahului Airport, and 25 miles from Lahaina. Nearby are the Humpback Whale Education Center, Makena State Park, and Maui Ocean Center. Hotel amenities include 24-hour front desk, car rental desk, concierge, currency exchange, babysitting, limited room service, baggage hold, and local shuttle service. Dining is available at any of three onsite restaurants including Le Gunji, Capische, and the Restaurant Taiko, which offers Japanese and French cuisine, as well as an extensive sushi bar. Recreation and relaxation are provide by the onsite Diamond Spa, providing a variety of facial and massage treatments, and the REPS Fitness and Training Center, where guests can take advantage of workout routines customized by professional personal trainers. All suites have spectacular views and feature A/C, telephones with voicemail, dataports, TVs, VCRs, irons and ironing boards, hairdryers, coffeemakers, Japanese Green Tea sets, umbrellas, bathrobes, washlette toilets, complete bathroom amenities, spacious lanai (deck) shower areas, spa tubs, chaise lounges, and chairs. Children are considered 12 and younger at this resort. Hotel Amenities Dining Room No Fitness center Swimming Pool Additional Amenities Modem / Data Port Free Parking All-Suites Property Jacuzzi Wheelchair Accessible Business Center Meeting Rooms Dry Cleaning/Laundry Kitchenette Dining Options Taiko -location * On Property -cuisine * Japanese -breakfast * Daily Except Tuesday -lunch * Daily Except Tuesday -dinner * Daily Except Tuesday Le Gunji -location * On Property -cuisine * French/Japanese -dinner * Two Seating At 1800 And 2000 Nightly Except Wednesday Capische -location * On Property -cuisine * Alfresco Italian Cuisine And Cocktail Lounge -dinner * Dinner And Cocktails Daily -dress Code * Casual More Information About this Hotel Maps & Directions Photos Features * Note: The rates shown above are based on double occupancy unless otherwise noted and may not include taxes, service charges, fees, extra person charges, or any other incidentals. Any currency conversion for the above rates is based on today's exchange rate. 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MAUI schools extend study

maui - utrecht network information sheets MAUI-Utrecht Exchange INFORMATION SHEETS FOR MAUI-UTRECHT EXCHANGE PARTNERS From year to year, some schools may not be participating in the exchange. Please check the information page or contact Traci Faschingbauer at faschingbauert@umsl.edu . Some MAUI schools extend study abroad oppourtunities to students not currently enrolled in their schools. To find out more about these programs, check out their websites or contact their international offices directly. Contact information and websites for each school can be accessed by clicking the links below. UTRECHT SCHOOLS Austria, Karl Franzens Universität Graz Belgium, Universiteit Antwerpen Czech Republic, Masaryk Univerzita Denmark, Aarhus Universitet Finland, University of Helsinki France, Université des Sciences et Techologies de Lille France, Université Louis Pasteur (Strasbourg I) France, Université Marc Bloch (Strasbourg II) France, Unitersité Robert Schuman (Strasbourg III) Germany, Ruhr Universität Bochum Germany, Universität Leipzig Greece, Aristotle University of Thessaloniki not participating Iceland, University of Iceland Ireland, National University of Ireland, Cork Italy, Università di Bologna Lithuania, Vilnius University Malta, University of Malta The Netherlands, University of Utrecht The Netherlands, Utrecht School of the Arts Norway, University of Bergen Portugal, Universidade de Coimbra Slovenia, Univerza Ljubljana Spain, Universidad Complutense de Madrid Sweden, Lund University Switzerland, Universität Basel MAUI SCHOOLS Baylor University Southern Illinois University at Carbondale Kansas State University University of Kansas University of Missouri-Columbia University of Missouri-Kansas City University of Missouri-Rolla University of Missouri-St. Louis University of Nebraska at Kearney University of Nebraska at Lincoln University of Nebraska at Omaha University of Oklahoma Oklahoma State University Texas Tech University Maui-Utrecht Exchange Homepage Study Abroad Office Center for International Studies 261 Millennium Student Center One University Blvd St. Louis, MO 63121-4499 314-516-6497 314-516-5636 FAX

Hawaii Volcano Obervatory web

Updates on Kilauea Eruptions Recent Highlights from the "Pu`u `O`o" eruption ofKilauea's East Rift Zone One Fine Daybreak at the Pu`u `O`o cone Eruption Episode 55: 24 Feb 1997 to Dec 2005 Happy 23nd Birthday to Pu`u `O`o on 3 Jan 2006 Current eruption information for thosevisiting Hawai`i Volcanoes National Park can be obtained from theNational Park Service at 808-985-6000 or at their web site: Hawai`i Volcanoes National Park . Additional updates, and detailed eruption and background informationcan be obtained from the USGS Hawaii Volcano Obervatory web site at: http://hvo.wr.usgs.gov/kilauea/update/ . View near real-time images of the Big Island obtained by the NOAA GOES-9 satellite at: http://virtual1.pgd.hawaii.edu/goes/ . For most recent updates, please visit the HVO website. Overview    Episode 55 of the 18 year old Pu`u `O`o eruption started on 24Feb 1997. The USGS Hawaiian Volcano Observatory (HVO) has identied each distinct phase of the Pu`u `O`o eruption with an episode number; For a summary ofprevious episodes, see our compilation .    This latest phase of eruptive activity at Kilauea volcano started unceremoniously on 24 Feb with the appearance of a small amount of molten lava deep within the Pu`u `O`o crater, visible only from above. Yet the ensuing 9 years have seen multiple spectactular periods of eruptive activity. The first couple of years of activity are detailed on our episode 55 page . PLEASE NOTE: HCV discontinued making detailed eruption updates in late 1999, once web capability was established at HVO. Synopsis of events    1997 through 1998 saw increased activity, a resumption of the ocean entry, lava bench formation and collapse (at the seashore), crater overflows and a general collapse of the large main crater cone bulit in priot episodes of the eruption.    1999 through 2001 saw continue eruptions from a crater flank vent, lava flows exiting the National Park on the East Flank and new ocean entries.    2002 and 2003 saw a shift of activity from the coast to upslope, with new surface flows and associated activity    2004 and 2005 saw resumption of vigorous ocean entries, including a new addition to the wester margin of the flow field. Activity upslope also continued, off and on, through the period. some more details    Episode 55 arrived after a 24 day-long hiatus in eruptive activity. This hiatus in turn followed a brief but spectacular fissure eruption (Episode 54) at Napau Crater in late January 1997. This last long hiatus had many volcano watchers presuming that the multi-year Pu`u `O`o eruption was finally Pau ( Pau in Hawaiian means over, or finished). This is because long hiatuses have not occurred duringthe last decade at Pu`u `O`o (the last long one was in mid-1986, when volcanism switched from episodic, 300-500m high, fire fountains of lava to continuous effusion).    Episode 55 has seen shifting vent locations on flanks of Pu`u `O`o cone and abuild up of the lava shield mostly on the south flank of the Pu`u `O`ocone. The lava pond within the Pu`u `O`o crater has intermittently risento produce flows on its east and west margins as well. The lava shield is the low bulge beneath the cone in the photo at the top ofthe page (taken on 26 May 1997).     Surface volcanic activity was extremely limited in the early days of Episode 55, occurring only deep within the Pu`u `O`o crater. On 28 March 1997, the lava level in the Pu`u `O`o crater rose and began feeding the subterreanean channels ("lava tubes") that fed small cones just south of the cone. Lava began erupting from several of these cones,enlarging the lava shield formed over the past 16 years.    In early July of 1997, lava began flowing down toward the coast, resulting in a resumption of ocean entry on July 12 near the eastern edge of the national park. This was the first time since January that surface flows at Kilaueareached the sea; prior to that, episode 55 had been restricted mostly tothe area around the Pu`u `O`o cone at elevations over 2000 feet. Between 29 July and 4 Aug the lava-sea entry had temporarily ceased, but restarted and on 11 Auga lava flow overran a 700 year-old Hawaiian temple ("Waha'ula heiau"), almost completely obscuring the ancient rock walled structure.Additionally, lava from within the Pu`u `O`o lava lake has risenhigh enough to have spilled out of the crater within the Pu`u `O`o cone and over the side at least twice in the past month.    Between early August and October 1997, the volcano experienced a number of lava overflowsfrom the Pu`u `O`o crater, which initiate with molten lava ponding inthe crater until it spills over the rim, issuing rivulets of lava to theeast and west of the crater. Although spectacular, these particular flows have yet to reach more than about 0.7 km from the crater. The lava that isfeeding the ocean entries issues from vents just outside of the Pu`u `O`ocone into lava tubes that run to the coast. These tubes experienceoccasional short-lived breakouts where lava flows on the surface. Otherwise,surface activity is typically very limited in locations away from the Pu`u `O`o vents. Both ocean entries have repeatedly formed lava benches, where new land is building out beyond the former seacliffs. Some or all of these unstable land masses have repeatedly collapsed into the sea. An example of whatthe benches looked like as of October 1997 is in the image to the left (outlined by white lines). Early in November 1997, one of the two lava benches suffered a large collapsed into the sea, taking some 4.75 acres of new landscape with it. Later, lava from the same tube system rebuilt a shelf at the foot of the cliffs formed during the collapse.Additional large collapses have occurred, such as on 15 January andbetween 16 and 19 February, 1998. These episode 55 photos of the two active benches (posted 3 and 18 Nov 97)can be viewed at the USGS-HVO web site or by clicking on the small versionsto the left. ( images Courtesy of the USGS-HVO ) The cliffs formed during the 18 Nov. collapse can be seen in the lower small photo to the left. This latest collapse illustrates that lavabenches form and then collapse at unpredictable intervals. HVO warns visitors that "these benches can collapse into the sea without warning, triggering steam explosions that hurl dense rock and molten spatter tens of meters inland. No one should venture onto the benches, no matter how stable the new land may appear." Additionally, the photos (to the right) are of the two activesea entries as they appeared in late March of 1998. Click on the images to view full size (photos by Ken Rubin)    In mid Jan 1998, there was a breif surge in activity at Kilauea, whereina lava intrusion caused rapid inflation of the summit, followed by defaltion.A summit eruption did not occur. Rather, the lava appeared to have enteredthe East Rift Zone and caused enhanced activity at the Pu`u `O`o vent (17 km to the east) and an increase in surface flow activity at pointsbetween Pu`u `O`o and the coast. The earthquakes and magma surge disrupted the steady-state pattern of activity that has characterized most of the past6 months of the eruption. This latest disruption subsided in (Feb. 1998) and the eruption is returned to a pattern more typical of previous months.    By Feb 1998 the eruption had settled into a routine of fairlysteady magma supply to the Pu`u `O`o crater and the sea entriesnear the coast. A number of additional bench collapses, brieferuption hiatuses and surface flow breakout episodes have also occurred,as well as a short period of enhance lava-lake activity at the craterin May 1998 that did not affect the overall effusion rate at the ocean entries.In early July, one of the two ocean entries that have been activefor most of Episode 55 (the Wah`aula entry) died but the other remained active.    1999 through 2001 saw continue eruptions from a crater flank vent. There was a brief hiatus in eruptive activity during a new intrusion of magma on the East Rift Zone, closer to the Kilauea caldera (Sept 1999) but activity resumed a week and a half later with spectacular surface flows, that made it to the sea by December of that year. Flows exited the park in early 2000 and for the next couple of years overran five abandoned houses in Royal Gardens subdivision (thus increasing to 189 the total number of structures destroyed by this eruption). A new ocean entry began on the eastern edge of Kupapa`u, marking the first ocean entry outside the national park since 1991.    In early 2002 tube flow slowed and ocean entries stopped. Breakouts occured higher upslope and by march had created a nearly 3km long ridge of lava shields above 2000 ft. elevation. Crater activity also picked up and fed new flows into Royal Gardens. By Mother's Day, another flow (this time on the western edge of the flow field) issued from a flank vent on the west of Puu Oo and entered forested lands and took over most of the lava supply from the other parts of the flow. It reach the sea in July 2002 and continued for the next year. A second breakout from this same lava tube sent a new flow seaward in early 2003 for a few weeks. By later in the year, activity had diminished near the coast activity shifted upslope again as surface flows and spatter cones.    Jan 2004 saw resumption of flows directly from the crater for the first time since 1998 and activity there continued through March 2004. A flow named for Martin Luther King Day (the MLK flow) began during this period. A second breakout occured on Prince Kuhio Day in March, producing what HVO calls the "PKK" flow. It was the main flow through by Aug 2004, and continued through 2005, with ocean entries from two branches begining in Nov 2004 and June 2005. This became the dominant tube by August 2004. The Mother's day tube also once again began producing "rootless" shields in early 2004, producing a flow that entered the sea from May to July 2004. Activity resumed in and around Pu`u `O`o crater in Jan 2005, with spattering through Feb. 2005 and the formation of sevaral small lava ponds. The PKK flow remained active through Dec 2005. Activity remains intermittent as well on the MLK flow. A detailed chronological summary of events (most recent first)during the first two years of 'episode 55' of the Pu`u `O`o eruption is given on the episode 55 page . PLEASE NOTE: HCV had been posting detailed eruption updates in the 1990s before web capability was established at HVO on the Big Island. HCV discontinued these detailed updates in late 1999 The latest updates can be now obtained from the Kilauea Update page of the USGS-HVO website Visit our LISTING of Pu`u `O`o eruption episodes for a summary of previous activity andlinks to previous eruption update pages (where available). CREDITS and DISCLAIMER: This synopsis was written by Ken Rubin and Mike Garcia using someinformation kindly provided by the U.S.Geological Survey's Hawaii Volcano Observatory (in the form of formal press releases, personal communicationsand information from their HVO web site). The US Geological Survey-Hawaiian Volcano Observatory is not directly responsible foreditorial changes or enhancements made by the HCV (the Hawaii Center forVolcanology) web staff, nor does it claim responsiblity in any way for the interpretive content of these pages. HCV Home Hawaiian Volcanoes Loihi Kilauea Mauna Loa Hualalai This page created and maintained by Ken Rubin ©, krubin@soest.hawaii.edu Other credits for this web site. Last page update on 7 Jan 2006

Hawaii Honeymoon Planning, Hawaii

Honeymoons in Hawaii example: Newark Wedding Photographers Need Help? Click Here and The Professionals Will Come to the Rescue! Party Themes Party Vendors Letter to Editor Vendor Registration Greeting Cards Party Tips Budget Calculator Seating Arrangement Message Boards Bridal Shows Address Book We Recommend Contact Me Please Vendors by Region Link to Us Wine Member Registration Popular Searches Search results for Honeymoons in Hawaii . Travel > Honeymoons Local and National Listing of Travel Agents, Travel Service, Travel Packages For Honeymoon Planning. 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