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Northwestern Hawaiian Islands Multi-Agency Education Project Aloha! Welcome to the Northwestern Hawaiian Islands! This site is a collaborative effort of many agencies and organizations working together to malama (care for) this special place and bring it to you. Current Event: NWHI 2005 Reef Assessment and Monitoring Program (RAMP) From September through October 6th 2005, the NOAA (National Oceanic and Atmospheric Administration) Ship Hi`ialakai ("embracing pathways to the sea," pictured to left), will be conducting reef assessment and monitoring in the Northwestern Hawaiian Island. Click here to follow the expedition . Previous Events: NWHI 2005 Education Expedition NWHI Maritime Archaeology, Ecosystem Connectivity, Mapping and Coral Disease Expedition 2005 NWHI RAMP Ecological Assessment and Monitoring Expedition 2004 NOWRAMP 2002 Research Expedition See the journals and feature stories or watch the great videos developed in collaboration with Bishop Museum and NASA! Curriculum: The goal of Navigating Change is to motivate, encourage and challenge people to take action to improve the environmental conditions in their own backyards, especially as it pertains to our coral reef ecosystems. We want people to take responsibility for the stewardship and sustainability of our islands and our ocean. We are targeting our message to the youth of Hawai`i because the future is in their hands. Classroom videos, teacher curriculum and more are available . To learn more about Navigating Change click here . View the Navigating Change Modules online! Click here . Ask About It! You can participate! On many pages you will see an "Ask About It" link that looks like this: Ask About It! You can use the link to ask a question about the topic of the page you are reading, and our reply will appear on the same page. So, start browsing to learn more about the NWHI! Recent Interviews and Journals Shark barf Passion Kupuna Islands Interview: Chad Yoshinaga, NOAA Scientist Also see the other journals! Things you can do See our Activities page! Lesson and Unit Plans Seafloor Profiling Grasshopper science NWHI Interdisciplinary unit See also the Resources page! Features from Previous Expeditions Mapping an Unnamed Seamount Brooks Bank Mapping NWHI Flora and Fauna Encyclopedia A Trophic Detective Story Laysan Ducks Make New Home on Midway Interviews (from 2002) Randall Kosaki, Ph.D., NOWRAMP PI Nainoa Thompson Home | News | About | Expeditions | Photos | Video | Maps Discussions | Partners | Teachers | Keiki | More Info | Search Contact Us | Privacy Policy This site is hosted by the Laboratory for Interactive Learning Technologies at the University of Hawai`i Hawaiian Quilting Journey: WeekMokihana’s Garden » Blog Archive » Mokihana’s Hawaiian Quilting Journey: Week Two Mokihana’s Garden A Mānoa Valley Wahine Writes of Past and Present « Mokihana’s Hawaiian Quilting Journey: Week One Mokihana’s Hawaiian Quilting Journey: Class! » Mokihana’s Hawaiian Quilting Journey: Week Two I thought I’d come out the winner this week. And I did, sorta. Eventually. I got my new fabric all washed and ready and started cutting. Unfortunately, I musta been half asleep at the time, because I cut it wrong and had to go back to the fabric store yet again! Sheesh! Fabric 6, Mokihana O. However, the next day I was much more successful, and got my applique piece all properly cut out - Mokihana 1, Fabric 6. The following day I cut out my background piece - Mokihana 2, Fabric 6 (I’m catching up!). I carefully unfolded my green ulu applique piece and voila! There it was, waiting for me to baste it onto the background fabric. I think I should get a point for that. K’den. Mokihana 3 - Fabric 6. Then, the next day of quiet basting with my friend, I got the whole pattern basted onto the background! Pau! Mokihana 4, Fabric 6. Now I am ready to start appliqueing the pattern to the background. And I fully expect to have my score keep climbing! This is turning out to be a very rewarding project for me. I feel very spiritually connected to it, feeling a real connection to Hawaiian women years and years before me designing and quilting their own works of art. I couldn’t make it out to The Gathering this week. I was buried with work and a very large truck with a cherry picker and shredder attached to it was parked in my long, narrow driveway while a crew from Portland General Electric trimmed branches from the firs, maples, alders and willows away from the power lines. I was very disappointed that I couldn’t get out; it would have been a lovely day. However, there is next week. And I have a quilt square ready to be appliqued. The colors are just what I wanted and I feel so good about starting this. It is a song to me, and I am loving the singing of it. This entry was posted on Thursday, July 17th, 2003 at 8:52 amand is filed under Hawaiian Quilting .You can follow any responses to this entry through the RSS 2.0 feed. You can leave a response , or trackback from your own site. 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Lanai Langkawi > TravelerLangkawi: The Lanai Langkawi - Traveler Reviews - 10 nights at the Lanai - TripAdvisor The Lanai Langkawi: Traveler Reviews Sign in • Sign up Home > Asia > Malaysia > Kedah > Langkawi > Hotels > The Lanai Langkawi > Traveler Reviews Langkawi tourism: Overview Hotels Flights Attractions Deals Forums Maps, etc. Search (e.g., Boston hotels, Las Vegas, Paris art museum) Langkawi Langkawi Overview Langkawi Hotels The Lanai Langkawi All Langkawi Hotels Flights to Langkawi Langkawi Deals Langkawi Attractions Langkawi Forum Langkawi Maps Langkawi Discount Hotels Langkawi Vacation Packages Free Newsletter Get deals, news and articles on The Lanai Langkawi Plus weekend trip ideas from your hometown The Lanai Langkawi Hotel e-mail this page to a friend Traveler Reviews Write a review . What was your experience with The Lanai Langkawi? Tell others what's hot and what's not. Langkawi The Lanai Langkawi Pantai Tengah, P.O. Box 143 Langkawi, Kedah 07000 Malaysia Deals on Langkawi Hotels The Datai Langkawi Pelangi Beach Resort Langkawi Casa Del Mar Langkawi The Andaman Langkawi Tanjung Rhu Hotel Sheraton Perdana Resort Four Seasons Resort Langkawi Bon Ton Resort Berjaya Langkawi Beach and Spa Resort Sheraton Langkawi Beach Resort Mutiara Burau Bay Holiday Villa Langkawi Aseania Resort City Bayview Hotel Federal Villa Langkawi Kampung Tok Senik Resort Langkawi Langkawi Lagoon Resort The Lanai Langkawi More Langkawi Hotels Beach Garden Resort Langkawi Village Resort Sunset Beach Resort Pondok Keladi Tanjung Sanctuary Resort Hotel Awana Porto Malai Langkawi Rebak Marina Resort Helang Hotel Beringin Beach Resort Black Sand Beach Motel Burau Bay Resort Chandek Kura Resort Konda Istana Langkawi Chalet Nadias Inn Beach Resort Nagoya City Hotel Singgahsana KUB Resort Langkawi Sunrise Island Resort Tanjung Mali Beach Motel The Garden Hotel Tiara Langkawi Hotel Langkapuri Beach Resort Grand Continental Langkawi AB Motel Langkasuka Resort Central Hotel (Eagle Bay Hotel) Charlie Motel & Restaurant Langkawi Seaview Hotel Twin Peaks Island Resort Read more Langkawi tourism The Lanai Langkawi : Traveler Reviews #40 of 46 hotels in Langkawi Pantai Tengah, P.O. Box 143, Langkawi, Kedah 07000, Malaysia Rooms: 104 TripAdvisor traveler rating: Sponsored links * Hotel deal search: The Lanai Langkawi The Lanai Langkawi : Hot Deals HotelClub Discount Hotels WorldWide Recommended deals: Langkawi Langkawi : Hotel Deals from $214 Expedia.com Don't just travel. Travel right! Langkawi : Low Hotel Prices Made Easy Orbitz.com The faster, easier way to find the hotel you want. Just Orbitz and go! Langkawi : Great Prices, Great Rooms hotels.com We Know Hotels Inside And Out. View Maps, Photos, Rates. Book Now! All results: View all 82 Langkawi travel deals TripAdvisor Traveler Rating Based on 1 review worldwide What to expect Rooms Service Value Cleanliness Pool Recommendations couples and romantics budget travelers students seniors families with teenagers Traveler Reviews (1-1 of 1) (English) Traveler reviews (1-1 of 1) RATING: DATE: Show: All languages English (1) Traveler rating: Langkawi: The Lanai Langkawi : "10 nights at the Lanai" Apr 19, 2005 : A TripAdvisor Member, Norwich U.K. I stayed at this hotel in: April, 2005 My ratings for this hotel are: Rooms Service Value Cleanliness Dining Pool I traveled to this hotel with: spouse/partner I recommend this hotel for: couples and romantics, gay and lesbian, students, budget travelers, active/adventure travelers My visit was for: leisure The first thing we noticed on our arrival was how quiet and clean this hotel was in the middle of the afternoon. Staff were all extremely helpful, welcoming and friendly. Because this resort is goverment owned, the standards are not what you would expect from a five star, but the rooms are cleaned daily, new linnen on the beds, and four clean towels each morning. Also, the air conditioning works well, which is essential. There was plenty of hot water and the fridge worked perfectly. Be prepared to endure the wardrobe door collapsing, ditto the shower door. No baths or bidet, by the way. Any problems, once reported to the desk, were dealt with promptly. The patios and balconies all have the A/C vent emptying onto them, so you have to switch it off if you want to sit there.The t.v. in the room shows only local stuff. The location of the Lanai is fantastic - the best on Tengah beach, which is itself a delight. The grounds are well maintained and the central swimming pool is very clean. The beach bar is great for lunch, with an extensive menu which is sooo cheap but delicious. It also serves a good variety of fruit drinks and beer. There are numerous eateries within walking distance, such as Sheelas, The Lighthouse, Mata - Hari, and the Sun Cafe, all of which I enjoyed. Fat Mammas is close too, and I've heard only good things about it. We loved the time we spent at the Lanai and would happily go again. We would, I think, prefer a two bedroomed chalet, for the extra space and comfort. This review is the subjective opinion of a TripAdvisor member and not of TripAdvisor, Inc. 24 out of 24 TripAdvisor users found this review to be helpful. Write a review of this hotel Post your photos of this hotel Did you find this review helpful? Traveler reviews (1-1 of 1) Sponsored links * Hotel deal search: The Lanai Langkawi The Lanai Langkawi : Hot Deals HotelClub Discount Hotels WorldWide Recommended deals: Langkawi Langkawi : Hotel Deals from $214 Expedia.com Don't just travel. Travel right! Langkawi : Low Hotel Prices Made Easy Orbitz.com The faster, easier way to find the hotel you want. Just Orbitz and go! Langkawi : Great Prices, Great Rooms hotels.com We Know Hotels Inside And Out. View Maps, Photos, Rates. Book Now! All results: View all 82 Langkawi travel deals About TripAdvisor TripAdvisor provides recommendations for hotels, resorts, inns, vacations, travel packages, vacation packages, travel guides and lots more. Recommendations for hotels, resorts, inns, vacations, travel packages, travel guides and lots more! Visit TripAdvisor's international sites: About Us | Membership | Site Map | Become an Affiliate | Top Cities | Hotel Reservations | Hotel Deals | TripAdvisor Gear Popular Hotels: 1 , 2 , 3 , 4 , 5 , 6 , 7 , 8 , 9 , 10 , 11 , 12 , 13 , 14 , 15 , 16 , 17 , 18 , 19 , 20 , by city TripAdvisor Recommends: Las Vegas hotels , London hotels , Paris hotels , Rome hotels , New York City hotels , Chicago hotels , Orlando hotels © 2005 TripAdvisor, Inc. All rights reserved. TripAdvisor Terms of Use and Privacy Policy . * TripAdvisor, Inc. is not a booking agent and does not charge any service fees to users of our site... ( more ) TripAdvisor, Inc. is not responsible for content on external web sites. Hawaii Volcano Obervatory webUpdates 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 |
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