Hawaiian music lover, the

The Hawaiian Language Web Site - Awarded 'Best of the Net' -http://hawaiianlanguage.com -- E Komo Mai! Welcome! The Hawaiian LanguageWeb Site Ke Kahua Pûnâwelewele `Ôlelo Hawai`i http://hawaiianlanguage.com October18, 2003: Beginning Hawaiian Language Workshop Notes: 2nd Annual Southern California `Ukulele Festival The Hawaiian Home Page: Comprehensive Cultural Links - The Hula Pages What's New? Updated: 10/2003 Aunty D He mai! Mai! Mai! He mai e ku`u hoaaloha o ka`ôlelo Hawai`i. Ua ao kêia `ao`ao `upena nei, ua hiki mai la `oe. Mai, mai! Eia nô au nei." Translation The Call to the Hawaiian Language How This Site Came to Be Greetings and Invitation to Learn the Language Kûkahi (Standing Alone) `96 , Waikîkî Shell Keali`i Reichel haku mele (composer), pû`ukani (vocalist), kumu hula (hula master), kumu oli (master chanter), kanaka maoli " A loha kâkou! Ua lohe au: `O kêia ka makahiki `ôlelo Hawai`i. He ho`omaka maika`i kêlâ, akâ na`e, `a`ale lawa. `O kêia ka wâ `ôlelo Hawai`i, `eâ? No leila, pehea lâ ma hope o kêia makahiki? Pau ka `ôlelo Hawai`i? `A`ole loa. Inâ `a`ale `oe `ôlelo Hawai`i, pehea `oe `ike `ai i ka nani o nâ mele. Pehea `oe `ike `ai i ka loina o kô mâkou kûpuna. `Eâ, no laila, e hele `oukou `ao mai i ka `ôlelo Hawai`i. If you nevah undahstan', ah shucks!" Translation >> Keali`i's Songbook >> An mp3 sampling of Keali`i's music E `Ôlelo Kâua I Ka `Ôlelo Hawai`i ! Let's Speak Hawaiian! " A n interminable language...it is one of the oldest living languages of the earth, as some conjecture, and may well be classed among the best ...the thought to displace it, or to doom it to oblivion by substituting the English language, ought not for a moment to be indulged. L ong live the grand old, sonorous, poetical Hawaiian language." ~The Rev. Lorenzo Lyons(Makua Laiana), 1878, composer of "Hawai`i Aloha" , missionary. Why Learn Hawaiian? 20 Pono Reasons T he reasons to learn and cherish the Hawaiian language are many and varied. Ultimately, the desire... or the need... comes from within. I received the call to return home , "gift-wrapped in song and chant." Keali`i Reichel was my `ânela (angel, which means "messenger") and my desire to learn Hawaiian was ignited. Whether your desire burns like a raging fire, glows softly, or just barely smolders, it is enough to get you started here. Perhaps, for you, too, the need will become apparent. What's New? W hat's new on this site will be listed here for the convenience of frequenters. Hawaiian Language Lessons T hese beginner lessons are for the curious, the "local", the visitor, the expatriate, the homesick, the Hawaiian music lover, the hula aficionado, the `ukulele player, the culturally-aware, the unaware, and the-somewhere-in-between...the casual or the serious student. Browse through the Table of Contents ; there's something there for just about everyone ... including, maybe, you. Frequenters to this site tell us that these are their favorites: Mahalo & Aloha - How to Say "I Love You" in Hawaiian Hawaiian Idioms Greetings and Sentiments in Hawaiian - More Hawaiian Greetings Hawai`i Aloha - More Hawaiian Music Lyrics & Chords Speak Hawaiian like a "Local" ;- ) Say "Hawai`i" correctly - Common Mispronunciations The Aloha Spirit Nâ `Ânela Kelekî : Sheltie Angels The Hula Pages Commitment: Ho'okô If nothing else, learn the myriad meanings of " Aloha ." The Lânai C ome visit! E kipa mai! On the lânai, you will find journal musings... but only if you care to listen. Here's a sampling: Voice of an Angel tells of a series of synchronistic events, "bread crumbs leading home," which then lead to the creation of this site. Kalapana recalls nostalgic memories of a past Hawai`i, with a hopeful glimpse to the future, with hope that by learning well from the past, a brighter future is possible. A Hawaiian Love Story , a fond retelling. Brahdahs BU & IZ , cherished memories of the forging of unique friendships during the last year of a gentle Hawaiian's life. Hawaiian Cultural Links More T hese are the cyber-places to return time and time again ... to link up with friends and "talk story", listen to Hawaiian music, brush up on cultural knowledge, look up recipes, gaze dreamily at photographs of wahi pana (celebrated, noted, or legendary places), and read Hawai`i's daily newspapers and magazines. Hawaiian Language Links I 've searched the web and book-marked these URLs. They are collected here on one page for your convenience and perusal. If you are interested in a real-time class, check Hawaiian Language Classes . Aloha Cyber-card Hawaiian E-Cards S pread The Aloha Spirit ...and learn some Hawaiian too. Send an Aloha "cybercard" with an `ôlelo no`eau (words of wisdom / proverbs) to someone who lives Aloha; or who you have Aloha for; or those may be in need of some Aloha to brighten their day. Kôkua mai - Help W ill you help? E kôkua mai ana `oe? Here's my outstretched hand. Grab onto it and hop on to the Hawaiian Language bandwagon ... together, we will make a positive difference. Spread the word. Use the words. Sing them. Love them. Make them live.... mau loa (forever). E-mail Translation Requests E -mail. Your comments and thoughts are welcome, but I must apologize ahead of time. The volume of e-mail has been quite staggering. While the interest generated by this site is surprising and gratifying, try as I might, I am unable to keep up with replies back to you. This site is maintained during my free time, which is, unfortunately, as limited as yours. Do know that each e-mail is, however, read and much appreciated. Please click here if you have Translation Requests . Aloha Notes A n unexpected joy of this experience is hearing from you. Hawaiians believe that words have power. And indeed they do. Your expressions of mahalo and aloha serve as powerful incentives to "keep keeping on" with these pages. Your shared experiences inspire me and others who frequent these pages. >> Sign Guestbook - View Guestbook >> Previous Guestbook Entries Mahalo iâ `oe no ke kipa`ana mai. E kipa mai hou! Thank you for visiting. Come and visit again. Aloha kekahi i kekahi. Love one another. Me ke aloha pumehana, Aunty D About.com / TMC has graciously given this site its Best of the Net Award . Mahalo! Mahalo nui loa no kâu kôkua, e ku`u hoaaloha, Yoda . Mahalo to Suite 101 and Tony Kwak for this award. © 1997-2003. Created and maintained by volunteers with the intention of perpetuating the Hawaiian culture, language, and The Aloha Spirit, this is a not-for-profit educational site. Materials on this web site is to be used for personal and educational purposes only. No permission is required to link this site to other sites. Linking to this site to yours is 100% OK! As an ever-evolving work, information on this web site is subject to change without notice. This site honors our kûpuna (elders, ancestors) by providing world-wide access to a now thriving, beautiful language of the spirit that once almost met with certain extinction, this web site is a makana aloha ( fig., a gift from the heart); thus, any commercial or exploitative use is strictly kapu (prohibited). Back to the Top This URL: http://hawaiianlanguage.com >> the hawaiian home page: cultural links reasons | what's new | hawaiian language lessons | word lists | lânai | links | language links | help | aloha notes | nâ `ânela kelekî | pronunciation guide | the aloha spirit | EMERGENCY dog links | the hula pages | hawaiian music lyrics & chords Disclaimer © 1996-2000 Mahalo nui to GeoCities for hosting this web site. Get your own Free Home Page ! Mahalo nui to you for visiting.

Hawaii Resort

Catering Meetings and Events at Waikiki Beach Hawaii Resort & Spa A meeting facility with more than 50,000 square feet of indoor and outdoor function: the Waikiki Beach Marriott Resort and Spa. home meetings & events catering -- -- Let us show you exclusive offers & updates tailored to your interests. RFP meeting services meeting rooms hot dates catering floor plans Looking for a venue for that special occasion such as a luncheon, fundraising dinner, 1st birthday, theme parties or weddings, the Waikiki Beach Marriott Resort and Spa has the Request a Proposal Fact Sheet Floor Plans Capacity Chart Book a Meeting perfect venue for you. With over 50,000 square feet of indoor / outdoor function space, your event will have just the right setting. Our professional sales and service managers are dedicated to making your event a memorable experience and are here to assist in the planning of your event. Our renowned Chef has created menus that will satisfy anyone's taste. Come and see why the Waikiki Beach Marriott Resort & Spa is the talk of the Island when it comes to catering and themed events. 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

Hawaiian Islands are volcanic

The Formation of the Hawaiian Islands The Formation of the Hawaiian Islands [ HCV Home ][Formation of the Islands][ Active Hawaiian Volcanoes ][ General Info ]    The Hawaiian Islands are volcanic in origin. Each island ismade up of at least one primary volcano, although many islandsare composites of more than one. The Big Island, for instance,is constructed of 5 major volcanoes: Kilauea, Mauna Loa, Mauna Kea,Hualalai and Kohala. Mauna Loa is the largest active volcano onEarth. Kilauea is presently one of the most productive volcanoeson Earth (in terms of how much lava it erupts each year). The primary volcanoes on eachof the islands are known as a shield volcanoes, which are gently sloping mountains produced from a large number of generally very fluid lava flows.    Hawaiian volcanoes primarily erupt a type of rock known as basalt. When molten, basalt produces liquids of relatively high fluidity, compared to volcanoesthat erupt more silica rich magma types such as andesite, dacite or rhyolite. The fluidity of molten basalt favors the formation of lava flows,which is why the Hawaiian volcanoes generally have gentle sloping sides. Bycontrast, lavas with higher silica content are more viscous and commonly produce either thicker, shorter lava flows, thick blocky deposits and/orthick beds of ash that fall from the sky following explosive eruptions.These other types of volcanoes (common outside of Hawaii) are typically steepersided.    The Hawaiian volcanoes were produced by the Hawaiian hot spot, which is presently under the Big Island of Hawaii.The image below shows the islands of the Hawaiian chainand the intervening shallows, banks and reefs along a line from southeastto northwest. Note that the islands of Lanai and Kahoolawe are not shownbecause they would "overlap" with Molokai and Maui, respectively( see the map of the Islands on the Hawaiian Volcanoes page )In general, when you move along the island chain from southeast (Hawaii) to northwest, (Kure), the volcanoes become older and older.     The aging of the islands with distance from the current hot spotis demonstrated in the diagram below, where distance along thechain is approximated as distance away from Kilauea volcano (theyoungest above-sea-level Hawaiian volcano). In fact, even beyond Kurethe Hawaiian chain continues as a series of now-submergedformer islands known collectively as the Emperorseamounts. The two primary volcanoes that make up Oahu (where Honolulu is) have not erupted for well over a million years!    The age trend of the volcanoes is thought to be due tothe way in which the islands are built on the moving sea floor of the NorthPacific Ocean: the Pacific Ocean is mostly floored by a single tectonic plate(known as the "Pacific Plate")that is moving over the layer in the Earth known as the Asthenosphere.This movement takes it to the northwest compared to the layers below itat a rate of 5 to 10 cm/yr (the rate depends on where you are on it). As theplate moves over a fixed spot deeper in the Earth where magma (moltenlava) forms, a new volcano can punch through this plate and createan island. The Hawaiian Islands are believed to be formed from onesuch 'hot spot'. As the plate moves away, the volcano stops eruptingand a new one is formed in its place. With time, the volcanoes keepdrifting westward and getting older relative to the one active volcanothat is over the hot spot. As they age, the crust upon which they sitcools and subsides. This, combined with erosion of the islands onceactive volcanism stops, leads to a shrinking of the islands with ageand their eventual submergence below the ocean surface.    Importantly, the time over which various active volcanoes on the islandsremain active is long (hunders of thousands of years) so that significantoverlap in ages occur on neighboring islands. For instance although Haleakala volcano on Mauiis a great distance away from the presently erupting Kilauea, Haleakalalast erupted only about 200 years ago. Currently there are 3 Hawai'ian volcanoes that we can easily classify as active: Kilauea, actively erupting since 1983 Mauna Loa, which last erupted in 1984 and is building for a new eruption inthe next few years Loihi, which erupted in 1996   All three of these active Hawaiian volcanoes sharethe Hawaiian hot spot, but retain unique volcanic histories and compositions.You can view a schematic representationof the geometry of this situation HERE The most likely Dormant volcanoes are: Hualalai, which last erupted in 1801 Haleakala, which last erupted in about 1790 Mauna Kea, which last erupted about 4,000 years ago.    Here is some additional general age information from USGS Professional Paper 1350 , Chapter 1 by Clague and Dalrymple, pages 5-54 (1987). Data from that source has been augmented by data and information in Garcia et al. Lithos , vol 20, pages 323-336 (1987) and Clague (1996) in The Origin and Evolution of Pacific Island biotas, New Guniea to Eastern Polynesia, patterns and processes (Keast and Miller, editors), pages 35-50. Ages of some of the Hawaiian Islands and outer seamounts Volcano Number (see note at table bottom) Volcano Name Distance from Kilauea along trend of chain (km) Best K-Ar age (Ma) Data Source (tabulated below) 1 Kilauea 0 0-0.4 -- 3 Mauna Kea 54 0.375 + 0.05 1 5 Kohala 100 0.43 + 0.02 2 6 Haleakala 182 0.75 + 0.04 3 7 Kahoolawe 185 > 1.03 + 0.18 3 8 West Maui 221 1.32 + 0.04 4 9 Lanai 226 1.28 + 0.04 5 10 East Molokai 256 1.76 + 0.04 3 11 West Molokai 280 1.90 + 0.06 3 12 Koolau 339 2.6 + 0.1 4,6 13 Waianae 374 3.7 + 0.1 6 14 Kauai 519 5.1 + 0.20 7 15 Niihau 565 4.89 + 0.11 8 15A Kaula 600 4.0 + 0.2 21 17 Nihoa 780 7.2 + 0.3 9 20 Unnamed 913 9.2 + 0.8 20 930 9.6 + 0.8 22 23 Necker 1,058 10.3 + 0.4 9 26 La Perouse Pinnacles 1,209 12.0 + 0.4 9 27 Brooks Bank 1,256 13.0 + 0.6 20 1,330 13.0 + 0.6 22 30 Gardner Pinnacles 1,435 12.3 + 1.0 20 1,460 12.3 + 1.0 22 36 Laysan 1,818 19.9 + 0.3 10 37 Northampton Bank 1,841 26.6 + 2.7 10 50 Pearl and Hermes Reef 2,281 20.6 + 2.7 11 52 Midway 2,432 27.7 + 0.6 12 57 Unnamed 2,600 28.0 + 0.4 11 63 Unnamed 2,825 27.4 + 0.5 11 65 Colohan 3,128 38.6 + 0.3 13 65A Abbott 3,280 38.7 + 0.9 13 67 Daikakuji 3,493 42.4 + 2.3 14 69 Yuryaku 3,520 43.4 + 1.6 11 72 Kimmei 3,668 39.9 + 1.2 14 74 Koko (southern) 3,758 48.1 + 0.8 14,15 81 Ojin 4,102 55.2 + 0.7 16 83 Jingu 4,175 55.4 + 0.9 17 86 Nintoku 4,452 56.2 + 0.6 16 90 Suiko (southern) 4,794 59.6 + 0.6 18,19 91 Suiko (central) 4,860 64.7 + 1.1 16 Data Sources: 1. Porter and others (1977) 12. Dalrymple and others (1977) 2. McDougall and Swanson (1972) 13. Duncan and Clague (1984) 3. Naughton and others (1980) 14. Dalrymple and Clague (1976) 4. Mcdougall (1964) 15. Clague and Dalrymple (1973) 5. Bonhommet and others (1977) 16. Dalrymple and others (1980a) 6. Doel and Dalrymple (1973) 17. Dalrymple and Garcia (1980) 7. McDougall (1979) 18. Saito and Ozima (1975) 8. G.B. Dalrymple (unpub. Data, 1982) 19. Saito and Ozima (1977) 9. Dalrymple and others (1974) 20. Garcia and others (1986b) 10. Dalrymple and others (1981) 21.Garcia and others (1986a) 11. Clague and others (1975) 22. Garcia and Others (1987) Other Notes: "Volcano Number" refers to the number in sequence along the HawaiianChain. Loihi, the youngest expression of the Hawaiian hot spot isnumber 0, Kilauea is number 1, etc.. Note that not all volcanoesare listed in the table (e.g., number 2 = Mauna Loa and number 4 =Hualalai); also note that further up the chain, the numbering schemebecomes more subjective. 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 4 Apr 2005

Honolulu Chapter 21 (3MB

Revised Ordinances of Honolulu, City and County of Honolulu Revised Ordinances of Honolulu Database description Disclaimer Search: RECENTLY ENACTED ORDINANCES Tables of Contents Chapter 1 General Provisions Chapter 2 Executive Agencies..Additional Powers,Duties and Functions Chapter 3 Additional Boards, Commissions andCommittees Chapter 4 Additional Powers and Duties of Counciland Legislative Agencies Chapter 5 Salaries of Elected Officials, Non-CivilService Officers and Employment and Bonding Requirements Chapter 6 Revolving Special Funds, Housing MortgageLoans and Fees Chapter 7 Animals and Fowl Chapter 8 Real Property Tax (Articles 5-9 , 10 , 11-16 ) Chapter 9 Collection and Disposal of Refuse Chapter 10 Rules, Regulations, Charges and Fees forPublic Parks and Recreation Facilities Chapter 10A Botanical Gardens Chapter 11 Child Care Chapter 12 Regulations of Common Carriers and TheirFees Chapter 13 Public Transit Chapter 14 Public Works InfrastructureRequirements Including Fees and Services (Articles 10-19 , 20-Appendix ) Chapter 15 Traffic Code (Articles 10-20 , 21-27 ) Chapter 16 Building Code (Article 2 , 3 , 4 , 5 , 6 , 7 , 8 , 9 , 10 , 11 , 12 ) Chapter 17 Electrical Code Chapter 18 Fees and Permits for Building,Electrical, Plumbing and Sidewalk Codes Chapter 19 Plumbing Code Chapter 20 Fire Code of the City and County ofHonolulu Chapter 21 (3MB PDF) Land Use Ordinance, Exhibits and Article 10 (2.68 MB PDF) (Appendix A , B , C , D , E , F-Kakaako Special Design District , G , H , I ; Index ) Chapter 22 Subdivision of Land Chapter 23 Shoreline Setbacks Chapter 24 Development Plans (Ordinance provisions: Central Oahu ; East Honolulu ; Ewa ; Ko'olau Loa ; Ko'olaupoko ; North Shore ; Primary Urban Center ; Northwestern Hawaiian Islands ; Waianae ) (Plan documents: Central Oahu ; East Honolulu ; Ewa ; Ko'olau Loa ; Ko'olaupoko ; North Shore ; Primary Urban Center ; Waianae ) Chapter 25 Special Management Area Chapter 26 State Land Use Classification Chapter 27 Housing Code Chapter 28 Lease and Rental of City Real Property,Including Fees Chapter 29 Streets, Sidewalks, Malls and OtherPublic Places Chapter 30 Water Management Chapter 31 Community Economic Development Chapter 32 Building Energy Efficiency Standards (Articles 4-7 , 8-14 ) Chapter 33 Development Agreements Chapter 33A Impact Fees for Traffic and Roadway Improvements in Ewa Chapter 34 Community Facilities Districts Chapter 35 Incentives for Businesses to Create NewJobs Chapter 36 Special Improvement Districts Chapter 37 Real Property Transactions Involving theCity and County of Honolulu ( Chapter 38 Residential Condominium, Cooperative Housing and Residential Planned Development Leasehold Conversion. Repealed by Ordinance 05-001) Chapter 38 (Reserved) Chapter 39 Maximum Annual Renegotiated Lease Rent Chapter 40 Prohibited Activities in the City Chapter 41 Regulated Activities Within theCity (Articles 26-42 ) GENERAL APPENDIX INDEX TABLES Ordinance List and Disposition Table Current Table of Sections Affected Previous Table of Sections Affected + Adobe Acrobat Portable DocumentFormat (PDF) requires the Acrobat Reader file viewer from Adobe Systems,Incorporated.

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. Write a letter to the editor | Subscribe to the Tribune | Place an Ad Online TBO.com AdLinks Site Tools Advertise with us Web site feedback Make TBO.com my homepage RSS Feeds: Feed for this channel All feeds/RSS FAQ Most Popular: This feature requires the Macromedia Flash Plugin. Please visit http://www.macromedia.com/go/getflashplayer to download this plugin. 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