Maui

Introduction to Skin Cancer An Introduction to Skin Cancer And Related Topics ________________________________________________________ Daily UV Forecast Recent News News Search . . . Site Index . Reusable UV Card $4.95 NEW! Digital UV Monitor $29.95 About This Page What Causes Skin Cancer? Sunburn, Sunlight, and Tanning Heredity Environment What is Skin Cancer? Basal Cell & Squamous Cell Melanoma How can I determine my personal risk? Are there precautions that will reduce my risk? The UV Index Daily Forecast for 30 U.S. Cities Ultra Violet Sensometer Diagnosis and Treatment Information A Glossary of Terms Additional Information Always consult a physician with your questions concerning the health effects of UV exposure About This Page Our intention is to provide a general introduction to Skin Cancer, with links to specific information available around the Net. Please send us your comments, suggestions, and information about sites not listed here. E-mail form here. We would like to make this page a gathering place for all available information about skin cancer and related subjects. Your help will make it as complete as possible. What Causes Skin Cancer? Sunburn and Sunlight Very simply, sunburn and UV light can damage your skin, and this damage can lead to skin cancer. There are of course other determining factors, including your heredity and the environment you live in. However, both the total amount of sun received over the years, and overexposure resulting in sunburn can cause skin cancer. Most people receive 80% of their lifetime exposure to the sun by 18 years of age. The message to parents from this is to protect your children. Tanning is your skin's response to UV light. It is a protective reaction to prevent further injury to your skin from the sun. However, it does not prevent skin cancer. Remember, skin cancer is very slow to develop. The sunburn you receive this week may take 20 years or more to become skin cancer. Heredity If there is a history of skin cancer in your family, you are probably at a higher risk. People with fair skin, with a northern European heritage appear to be most susceptible. Environment The level of UV light today is higher than it was 50 or 100 years ago. This is due to a reduction of ozone in the earth's atmosphere (the Ozone Hole). Ozone serves as a filter to screen out and reduce the amount of UV light that we are exposed to. With less atmospheric ozone, a higher level of UV light reaches the earth's surface. Other influencing factors include elevation, latitude, and cloud cover. Ultra Violet light is stronger as elevation increases. The thinner atmosphere at higher altitudes cannot filter UV as effectively as it can at sea level. The rays of the sun are also strongest near the equator, as you might guess. But even in Antarctica, Chile, and New Zealand, the UV level is much higher than normal especially in the springtime due to the ozone hole in the southern hemisphere. One factor that actually reduces UV is cloud cover. Climates and micro-climates with regular cloud cover may have a 50% lower level of UV light. The actual amount is affected by the density of the clouds. September 1995 Measurements of Antarctic Ozone The latest HALOE data in the form of a 100 mb surface cross section of column ozone (DU) is available. Please consult the data interpretation page for more information about the sampling pattern of HALOE. United Nations World Meteorological Organization (WMO) Press Release Measurements of the Ozone Hole this year show it "was so far the most rapid depletion on record." An area the size of Europe received significantly higher levels of ultra violet exposure. Environmental Protection Agency - Ozone Depletion Page This web site contains information about the science of ozone depletion, regulations in the US designed to protect the ozone layer, flyers about the UV index, information for consumers, and other topics. What is Skin Cancer? (From the National Cancer Institute PDQ Statement) Skin cancer is a disease in which cancer (malignant) cells are found in the outer layers of your skin. Your skin protects your body against heat, light, infection, and injury. It also stores water, fat, and vitamin D. The skin has two main layers and several kinds of cells. The top layer of skin is called the epidermis. It contains three kinds of cells: flat, scaly cells on the surface called squamous cells; round cells called basal cells; and cells called melanocytes, which give your skin its color. BASAL CELL & SQUAMOUS CELL (From the National Cancer Institute PDQ Statement) There are several types of cancer that start in the skin. The most common are basal cell cancer and squamous cell cancer, which are covered in this PDQ patient information statement. Skin cancer is more common in people with light colored skin who have spent a lot of time in the sunlight. Skin cancer can occur anywhere on your body, but it is most common in places that have been exposed to more sunlight, such as your face, neck, hands, and arms. Skin cancer can look many different ways. The most common sign of skin cancer is a change on the skin, such as a growth or a sore that won't heal. Sometime there may be a small lump. This lump can be smooth, shiny and waxy looking, or it can be red or reddish brown. Skin cancer may also appear as a flat red spot that is rough or scaly. Not ail changes in your skin are cancer, but you should see your doctor if you notice changes in your skin. Full Text Available Here MELANOMA (From the National Cancer Institute PDQ Statement) Melanoma is a disease of the skin in which cancer (malignant) cells are found in the cells that color the skin (melanocytes). Melanoma usually occurs in adults, but it may occasionally be found in children and adolescents. Your skin protects your body against heat, light, infection, and injury. It is made up of two main layers: the epidermis (the top layer) and dermis (the inner layer). Melanocytes are found in the epidermis and they contain melanin, which gives the skin its color. Melanoma is sometimes called cutaneous melanoma or malignant melanoma. Melanoma is a more serious type of cancer than the more common skin cancers, basal cell cancer or squamous cell cancer, which begin in the basal or squamous cells of the epidermis. If you have basal cell or squamous cell cancer of the skin, refer to the patient information statement for skin cancer. Like most cancers, melanoma is best treated when it is found (diagnosed) early. Melanoma can spread (metastasize) quickly to other parts of the body through the lymph system or through the blood. (Lymph nodes are small, bean-shaped structures that are found throughout the body; they produce and store infection-fighting cells.) You should see your doctor if you have any of the following warning signs of melanoma: change in the size, shape, or color of a mole; oozing or bleeding from a mole; or a mole that feels itchy, hard, lumpy, swollen, or tender to the touch. Melanoma can also appear on the body as a new mole. Men most often get melanoma on the trunk (the area of the body between the shoulders and hips) or on the head or neck; women most often get melanoma on the arms and legs. If you have signs of skin cancer, your doctor will examine your skin carefully. If a mole or pigmented area doesn't look normal, your doctor will cut it out (called local excision) and look at it under the microscope to see if it contains cancer. This is usually done in a doctor's office. It is important that this biopsy is done correctly. Full Text Available Here How can I determine my personal risk? It is estimated that 1 out of 7 people in the United States will develop some form of this cancer during their lifetime. One serious sunburn can increase the risk by as much as 50%. The effect UV light has on your skin is dependent both upon the intensity and the duration of your exposure. How your skin reacts to the amount of exposure received is related to your genetic background. Even if you rarely sunburn however, sensitive areas such as your lips, nose, and palms of the hands should be protected. Details about determining your skin type and accompanying risk can be found at: THE EXPERIMENTAL ULTRAVIOLET INDEX FACTSHEET: EXPLAINING THE INDEX TO THE PUBLIC Are there precautions that will reduce my risk? The following six steps have been recommended by the American Academy of Dermatology and the Skin Cancer Foundation to help reduce the risk of sunburn and skin cancer. Minimize your exposure to the sun at midday and between the hours of 10:00AM and 3:00PM. Apply sunscreen with at least a SPF-15 or higher, to all areas of the body which are exposed to the sun. Reapply sunscreen every two hours, even on cloudy days. Reapply after swimming or perspiring. Wear clothing that covers your body and shades your face. (Hats should provide shade for both the face and back of the neck.) Avoid exposure to UV radiation from sunlamps or tanning parlors. Protect your children. Keep them from excessive sun exposure when the sun is strongest (10:00AM and 3:00PM), and apply sunscreen liberally and frequently to children 6 months of age and older. Do not use sunscreen on children under 6 months of age. Parents with children under 6 months of age should severely limit their children's sun exposure. The UV Index The UV Index provides a forecast of your likely UV exposure at noon. This forecast can help you determine what level SPF sunscreen will best protect your skin. The forecast is based on a scale of 1 (low) to 15 (high). Here is an explanation of how the UV Index works. Forecast for 30 U.S. Cities The United States Environmental Protection Agency recently began issuing a daily UV FORECAST for 30 metropolitan areas around the country. This rating is also broadcast by weather radio, and on local television weather programs. The Ultra Violet Sensometer You may also determine the UV level for your area and conditions with a measuring device such as the Ultra Violet Sensometer . The Sensometer is an inexpensive, credit card sized device that measures UV light. As with the UV Forecast, you may then determine the proper SPF sunscreen. The Sensometer can also be used to test the effectiveness of your sunscreen, and when it is time to apply more sunscreen. Diagnosis and Treatment Information ALWAYS see your personal physician or dermatologist with any questions you may have about skin cancer, it's causes, diagnosis, and treatment. The following sites may provide supplemental reading. Skin Cancers - A Medical Education Service for the Public By Singapore National Skin Centre - With Photos The National Cancer Institute PDQ Statement - Basal And Squamous Cell The National Cancer Institute PDQ Statement - Melanoma The National Cancer Institute PDQ Statement - Screening for Skin Cancer CancerGuide - Treatment of Melanoma Welcome to Cancer Links Many of the links included here are from cancer-faq. Maintained by E. Loren Buhle, Jr. Ph.D. Co-Creater of ONCOLINK, buhlel01@mcrcr6.med.nyu.edu This list is updated monthly in usenet group - sci.med.diseases.cancer and subsequetially posted world wide in BBS, Echos, Usenet Groups, gophers and Home Pages. This list is recommended and available from many of the sources listed. ________________________________________________________ Always consult a physician with your questions concerning the health effects of UV exposure. ________________________________________________________

Air Hawaiian

Cheap vacations to Hawaii - discount hotel + air deals - TripAdvisor Hawaii vacation discounts and deals Sign in • Sign up Home > United States > Hawaii > SmartDeals > Vacation packages Hawaii tourism: Overview Hotels Flights Attractions Dining Deals Forums Maps, etc. Discount hotels | Hotel + air deals | All travel offers Search (e.g., Boston hotels, Las Vegas, Paris art museum) Hawaii Hawaii Overview Hawaii Hotels Flights to Hawaii Hawaii Deals Discount hotels Hotel + air deals All travel offers Hawaii Attractions Hawaii Restaurants Hawaii Forums Hawaii Maps Hawaii Discount Hotels Hawaii Vacation Packages e-mail this page to a friend Hawaii vacation packages Acapulco vacation packages Alaska vacation packages Amsterdam vacation packages Anaheim vacation packages Arizona vacation packages Aruba vacation packages Aspen vacation packages Atlanta vacation packages Atlantic City vacation packages Bahamas vacation packages Barbados vacation packages Belgium vacation packages Bermuda vacation packages Boston vacation packages Branson vacation packages Breckenridge vacation packages British Virgin Islands vacation packages Cabo San Lucas vacation packages California vacation packages Canada vacation packages Cancun vacation packages Caribbean vacation packages Colorado vacation packages Costa del Sol vacation packages Cozumel vacation packages Dallas vacation packages Daytona Beach vacation packages Dominican Republic vacation packages Florida vacation packages Florida Keys vacation packages Fort Lauderdale vacation packages France vacation packages Germany vacation packages Grand Canyon National Park vacation packages Greece vacation packages Grenada vacation packages Hawaii vacation packages Hilton Head vacation packages Ibiza vacation packages Ireland vacation packages Italy vacation packages Ixtapa vacation packages Jamaica vacation packages Kauai vacation packages Key West vacation packages Lake Placid vacation packages Lake Tahoe vacation packages Las Vegas vacation packages London vacation packages Los Angeles vacation packages Los Cabos vacation packages Maui vacation packages Mazatlan vacation packages Melbourne vacation packages Mexico vacation packages Miami vacation packages Montreal vacation packages Myrtle Beach vacation packages Nashville vacation packages Nassau vacation packages New York vacation packages New York City vacation packages Niagara Falls vacation packages Nova Scotia vacation packages Oahu vacation packages Orlando vacation packages Paris vacation packages Park City vacation packages Philadelphia vacation packages Phoenix vacation packages Pigeon Forge vacation packages Puerto Rico vacation packages Puerto Vallarta vacation packages Punta Cana vacation packages Quebec City vacation packages Reno vacation packages Rome vacation packages Salt Lake City vacation packages San Antonio vacation packages San Diego vacation packages San Francisco vacation packages Santa Fe vacation packages Scotland vacation packages Seattle vacation packages Spain vacation packages St. Croix vacation packages St. Lucia vacation packages St. Maarten/St. Martin vacation packages St. Thomas vacation packages Sydney vacation packages Texas vacation packages Toronto vacation packages Tucson vacation packages U.S. Virgin Islands vacation packages Vail vacation packages Virginia Beach vacation packages Washington DC vacation packages Whistler vacation packages Read more Hawaii tourism Hotel + air deals to Hawaii * Choose a specific destination Select one of the following destinations within Hawaii: --choose-one-- ---------- Island of Hawaii -- Hawaii Volcanoes National Park -- Hilo -- Honomu -- Kailua-Kona -- Kamuela -- Pahala -- Volcano -- Waikoloa ---------- Kauai -- Hanalei -- Kapaa -- Koloa -- Lihue -- Poipu -- Princeville -- Waimea ---------- Lanai -- Lanai City ---------- Maui -- Hana -- Kahului -- Kapalua -- Kihei -- Lahaina ---------- Molokai -- Kaunakakai -- Maunaloa ---------- Oahu -- Aiea -- Honolulu -- Kahuku -- Kapolei -- Waianae Featured specials - January 25, 2006 Hawaii : Save on hotel + air Expedia Vacations Don't just travel. 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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 Cruises Cruises Hawaii

Cruisegal specializes in Hawaii Cruise Packages. Things to Do Cruises Tours Packages Resorts The World North America United States Hawaii Cruises Cruises Hawaii Cruise Packages Register | Profile I want more information Email page to a friend Call Cruisegal toll free at 1-888-255-3148. There are many Hawaii Cruise Packages to choose from. Cruisegal will help you choose the one that fits your needs. Search Cruises Cruise Line Any Above and Beyond American Rivers American Safari Cruises Atlantis Events Carnival Cruise Line Celebrity Cruises Christian Travel Finder Clear Channel Entertainment, SFX Touring Inc. Costa Cruises Cruceros Australis Cruise West Crystal Cruises Cunard Line Discovery World Cruises Disney Cruise Line Gayribbean Cruises GNL Cruises Gto Travel Holland America Line Imperial River Cruises In The Wild Adventures Maharaja Cruise MSC Cruises Norwegian Cruise Line Oceania Cruises, Inc. 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Lauderdale Galveston Honolulu Houston Jacksonville Los Angeles Miami Mobile Montreal New Orleans New Jersey New York City Norfolk Philadelphia Port Canaveral San Diego San Francisco San Juan Seattle Seward Tampa Vancouver Promotions Only Sort By Select one Price (Low to High) Price (High to Low) Featured Promotions Cruise Line Cruise Destination Cruise Duration Departure Date Prev Cruises 1-10 of 53 1 | 2 | 3 | 4 | 5 | Next 5 Pages Next 10-Day Hawaii Honolulu round-trip from $799.00 (USD) Select Ship Name : Norwegian Wind Destination : Hawaii Departures : Mar 22, Oct 18, Nov 08, Nov 29, Dec 20, Jan 10, Jan 31, Feb 21, Mar 14, Apr 04 Ports of Call : Starting in Honolulu with stops in Hilo, Fanning Island, Nawiliwili, Lahaina, Kona Duration : 10 11 Night Eastbound Hawaii Cruise from $1,119.00 (USD) Select Ship Name : Serenade of the Seas Destination : Hawaii Departures : Oct 05 Ports of Call : Starting in Honolulu (Oahu) with stops in Nawiliwili (Kauai), Lahaina (Maui), Hilo, Kailua Kona, Ensenada Duration : 11 11 Night Southbound Hawaii Cruise from $2,359.00 (USD) Select Ship Name : Serenade of the Seas Destination : Hawaii Departures : Sep 24 Ports of Call : Starting in Vancouver with stops in Kailua Kona, Hilo, Lahaina (Maui), Honolulu (Oahu) Duration : 11 11-Day Hawaii Honolulu round-trip from $849.00 (USD) Select Ship Name : Norwegian Wind Destination : Hawaii Departures : Oct 07, Oct 28, Nov 18, Dec 09, Dec 30, Jan 20, Feb 10, Mar 03, Mar 24, Apr 14 Ports of Call : Starting in Honolulu with stops in Hilo, Lahaina, Nawiliwili, Fanning Island, Kona Duration : 11 11-Day Hawaiian Escape, Honolulu to Ensenada from $649.00 (USD) Select Ship Name : Norwegian Wind Destination : Hawaii Departures : Apr 01 Ports of Call : Starting in Honolulu with stops in Hilo, Lahaina, Nawiliwili, Ensenada Duration : 11 11-Day Hawaiian Escape, Kahuli to San Francisco from $3,099.00 (USD) Select Ship Name : Pride of Aloha Destination : Hawaii Departures : Apr 22 Ports of Call : Starting in Kahului with stops in Honolulu, Nawiliwili, Hilo, Kona, San Francisco Duration : 11 11-Day Hawaiian Islands, San Francisco to Honolulu from $1,089.00 (USD) Select Ship Name : Pride of Aloha Destination : Hawaii Departures : May 17 Ports of Call : Starting in San Francisco with stops in Nawiliwili, Hilo, Kona, Kahului, Honolulu Duration : 11 12 Day Hawaii from Ensenada from $1,299.00 (USD) Select Ship Name : Carnival Spirit Destination : Hawaii Departures : Apr 16 Ports of Call : Starting in Ensenada with stops in Hilo, Maui, Kona, Kauai, Honolulu Duration : 12 12 Day Hawaii from Ensenada from $1,099.00 (USD) Select Ship Name : Carnival Spirit Destination : Hawaii Departures : Apr 15 Ports of Call : Starting in Ensenada with stops in Kauai, Maui, Kona, Hilo, Honolulu Duration : 12 12 Day Hawaii from Honolulu from $1,449.00 (USD) Select Ship Name : Carnival Spirit Destination : Hawaii Departures : Apr 28 Ports of Call : Starting in Honolulu with stops in Maui, Hilo, Kona, Kauai, Vancouver Duration : 12 Prev Cruises 1-10 of 53 1 | 2 | 3 | 4 | 5 | Next 5 Pages Next Cruises 14 Night Hawaii Circle Cruise Onboard Summit from $1,900.00 (USD) Hawaii is a land of fascinating contrasts. 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Hawaiian Barbecue 4 review(s)

Evite - View venue information and reviews on L & L Hawaiian Barbecue. Keyword(s) Keyword(s) (required) Category Select a Category --- PLACES --- Arts and Culture Attractions Bars & Clubs Hotels Movie Theaters Other Restaurants Sports & Outdoors --- EVENTS --- Career & Classes Charity/ Volunteer Family Festivals and Fairs Gay & Lesbian Music & Dancing Other Events Performing Arts Singles Sports Travel & Leisure Visual Arts City, State or Zip L & L Hawaiian Barbecue 4 review(s) 6893 Mission St Daly City, CA 94014 (650) 756-7188 Plan An Event Here Tell A Friend Map/Driving Directions Avg. Rating 4 review(s) Plate Lunch anyone? 5/19/05 -- nifares Reason to Come Back: chicken katsu "you can't go wrong w/island grubin'" 3/25/05 -- charlestonchan from San Francisco, CA 3/8/05 -- chickichicky Reason to Come Back: short ribs!! Viewing 1 - 3 of 4 | View All Reviews Rate It! Reason to Come Back: Review Title Comment: Locals who like L & L Hawaiian Barbecue also like: Harris' in San Francisco, CA Pork Store Cafe in San Francisco, CA Tonga Restaurant & Bar in San Francisco, CA La Folie in San Francisco, CA Mitchell's Ice Cream in San Francisco, CA Kitaro Sushi in San Francisco, CA Get Party Tips, Recipes and gift ideas Advertise on Evite | About Us | FAQ | Contact Us | Site Map | Privacy Policy | Terms of Service Users of alcohol-endorsed Evite designs must be of legal drinking age. Golden Globes is a registered trademark of Hollywood Foreign Press. Hollywood Foreign Press is not affiliated with and does not endorse Evite. Super Bowl is a registered trademark of National Football League. National Football League is not affiliated with and does not endorse Evite. ©2006 Evite. All Rights Reserved. Partner sites: Alsto's Ask Jeeves Ballard Designs Citysearch ClassicVacations.com CondoSaver.com Entertainment.com Expedia Find Gifts Frontgate Garnet Hill HomeFocus Hotels.com Hotwire HSN ImprovementsCatalog.com Isabella Bird LendingTree liveDaily Match.com RealEstate.com ReserveAmerica ServiceMagic Smith+Noble The Territory Ahead Ticketmaster TravelSmith TripAdvisor