Maui The Island of
Maui and Kahoolawe, Hawaii Maui and Kahoolawe, Hawaii Elevation: 1,476 feet (450 m) - Kahoolawe 10,023 feet (3,055 m) - Maui The Island of Maui is made of two volcanoes: West Maui and East Maui.Most of the West Maui shield (20.9N, 156.6W) formed between 2-1.3 millionyears ago. A central caldera has been identified roughly in the area ofthe present-day Iao Valley. Alkalic basalts capped the volcano about 1.2million years ago. Four small eruptions occurred during the rejuvenatedstage on West Maui, probably about 1 million years ago. The volcano isdeeply dissected by numerous valleys. West Maui has not erupted inhistoric time and is considered to be extinct . East Maui Volcano, often also (but incorrectly) called Haleakala, is the easternmost of the twoshield volcanoes that make the Island of Maui. East Maui Volcano (20.7N, 156.2W)is the third largest Hawaiian shield volcano. Three rift zones can beclearly seen in the above Space Shuttle photograph(compare with map below). Most of thevolcanic activity has been concentrated along the southwest and east riftzones. The impressive Haleakala Crater is at the summit of the volcano.Haleakala Crater is an erosional caldera, formed by the coalescence ofthe heads of two large valleys as they eroded into the volcano. The mainshield of Haleakala is more than 800,000 years old. Lava flows andpyroclastics of the capping stage range in age from 930,000 to 350,000years old. Rejuvenated-stage volcanic rocks occur along the rift zonesand in the crater. The most recent eruption of Haleakala was in about1790 at La Perouse Bay. Haleakala is considered an active volcanobecause this eruption is in historic time for Hawaii. Kahoolawe (20.5N, 156.6W) is one of the smallest shield volcanoes in theHawaiian Islands. Kahoolawe is the island near the bottom of the slide.The lava flows that make the main shield are 1-2 million years old. Waveerosion has exposed a caldera on the eastside of the island . Kahoolawehas not erupted in historic time and is considered to be extinct. Source of information: Volcanoes of North America by Wood and Kienle. Images of Volcanoes To VolcanoWorld Honolulu Chapter 21 (3MBRevised 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. Hawaiian Quilt Cushion: VolumeHawaiian Quilt Cushion (Volume 4) by Poakalani & John Serrao Arts & Crafts Index | FAQ | Help Desk | View Search BROWSE SUBJECTS Arts & Crafts Art & Literature Business Children's Cookbooks Color & Activity Guidebooks Gardening History Humor & Games Language Maps Music Natural History Paperbacks Pearl Harbor Pictorial Self Help Sea Life Spirituality/Religion Sports/Recreation Wildlife NEED HELP? Help Desk FAQ Privacy Policy Hawaiian Quilt Cushion: Volume Four by Poakalani & John Serrao Retail Price: $ 6 .95 In Stock: Ships within 72 hours ISBN: 1566476445 Format: Softcover, 56 pages Pub. Date: October 2003 Pub.: Mutual Publishing Buy it today! you can always remove it later SAFE SECURE SHOPPING Synopsis : Aloha and welcome to the Poakalani family of Hawaiian quilt patterns and designs. To continue our commitment and legacy to all quilters we are proud to introduce to you Poakalani Hawaiian Quilt Cushion Patterns & Designs Volume 4-fifteen brand new Hawaiian Cushion Patterns. Some designs were specially requested by our students like the poinsettia, ukulele, daffodils, ku'uipo and African tulip, and other designs were inspired from the traditions of old Hawai'i like the ipu puniu , mahiole koa, uli uli and ipu . While all the quilt designs are new these patterns have all been tested and quilted by our students. The patterns are the larger 22" x 22" designs, but if you'd like a smaller 18" x 18" design, just reduce the pattern by 15% on the photocopier machine-it's as simple as that. Should you have any questions, feel free to contact us at (808) 521-1568 PO Box 22670, Honolulu, HI 96823-2370 or visit our website at www.poakalani.com . We hope you enjoy the Poakalani Hawaiian Quilt Cushion Patterns & Designs, Volume 4. Poakalani & John Serrao He Hana Ohana Kanaka Maoli A Hawaiian-Owned Family Business More Books on the Subject / Arts & Crafts For Our Entire Arts & Crafts Index - Click Here back to top Books | Music | DVD | Gifts | Links | Help Desk For Info and Orders Call Toll-Free: 1-877-828-HULA (4852) 1998 - 2005 by Booklines Hawaii, Ltd ., all rights reserved. Hawaii VolcanoCurrent update of the eruption of Kilauea Volcano, Hawai`i `o Eruption Summary Hazards History Panorama Images Eruption Update and Image Archive | deformation | images | maps | Pu`u `O`o camera | 0555 January 14[Note: Your observer will be way south of the border, almost astraddle the equator, for the next two weeks. The next regularly scheduled morning update will be on Monday, January 30. Updates may occur at irregular intervals in the interim.]The Full Wolf Moon is the brightest object visible this morning, for lava on Pulama pali is confined to small patches and rivulets in the west string of breakouts. The breakouts reache from about the 1400-foot elevation down to about the 900-foot elevation, with small lava patches down to about 300 feet, as noted by yesterday's field workers. Glow comes from just above the top of the pali, probably at about the 1900-foot elevation, and testifies to surface lava there, too. Yesterday's observers noted some lava along the far east side of the PKK flow just outside the national park at about the 200-foot elevation 3.8 km from the end of the Kalapana access road.Moderate glow comes from East Lae`apuki this morning. Lava rose from cracks that cut the front half of the delta on Thursday and added perhaps as much as 80 m to the west side of the delta. The observers estimated that at least a third of the delta is new or resurfaced by lava. Lava enters the ocean at numerous spots along most of the front of the delta, so that the laze plume is spread almost continuously along the water's edge. The delta is now about 500 m long (parallel to shore) but still only 140 m wide. The crater of Pu`u `O`o is badly socked in this morning, but glimpses appear of all vents except Beehive. Conditions were similar yesterday, and the field observers were skunked. They did witness, however, a breakout from the PKK tube at the base of the flank shield. It was not active at 0900, was going strong at ~1030, and was over by 1130. The breakout came from a shatter ring immediately down-tube from the bend in the tube at the base of the flank shield. This shatter ring may be the source for all the breakouts from the upper tube that have occurred since mid-December. The shatter ring is 60 m x 75 m across, and its southwest side is a 3-4-m-high, nearly vertical rubble wall. This area was very noisy, with cracking and scraping and lots of rock falling off, both during and after the breakout. Background volcanic tremor is about normal at Kilauea's summit this morning. Volcanic tremor is at a moderate level at Pu`u `O`o.Inflation at Kilauea's summit continued for the past 24 hours and has now recovered the 5.2 microradians lost during the deflation of January 9-10. In contrast, Pu`u `O`o is having a rocky, slow deflation that started midday January 12 and by this writing has lost almost 1 microradian. Note: Check Photo Glossary or a good dictionary for any terms unfamiliar to you. See Maps and accompanying caption for place names. Maps updated on December 19 Current Deformation Electronic Tilt Global Positioning System (GPS) Images and Chronology Looking for images you could swear you saw here but can't find now? Check Image Archive 13 January 2006 East Lae`apuki lava delta | med | large | | med | large | Left . Looking northeast across lava delta at East Lae`apuki. Note smooth, new surface on near part of delta, created when lava welled from cracks a couple of days ago. These cracks are shown in first image for January 6. Note also that most of delta front is source of laze; this is because lava pours into the water at many places. 0905. Right . Looking west at lava delta, showing how it nestles against cliff bounding embayment. Much of the cliff was created during collapse of earlier lava delta and adjacent "mainland" on November 28. As such, only part of the cliff is a true "sea cliff," formed by erosion. 0907. 6 January 2006 East Lae`apuki lava delta and Petunia skylight | med | large | | med | large | Left . Looking east across lava delta at East Lae`apuki. Note the cracks cutting the outer part of the delta. The cracks have formed in the last week or two as the delta has grown larger and become more unstable. Similar cracks cut the delta before its wholesale collapse on November 28, 2005. Steam (laze) rises at points where lava is entering the water. 0910. Right . Pretty Petunia skylight in roof of PKK lava tube, upper part of PKK flow. View looks downstream. Some of the lava visible through the skylight will eventually end up at East Lae`apuki 1-2 hr later. 1122. 29 December 2005 East Lae`apuki and MLK vent area | med | large | | med | large | Left . Lava delta at East Lae`apuki, built since November 28. White color on delta is from salt and other minerals precipitating on surface. Inland, note the scattered puffs of fume coming from points along lava tube feeding the delta. Actual point where tube enters delta is hidden by large laze plume. Note lopsided nature of delta; most is built right (east) of tube. Pulama pali in distance. 0938. Right . Treacherous lip of pit at MLK vent. Is it any wonder that geologists take care in this area? Southwest slope of Pu`u `O`o in background. 1016. 22 December 2005 East Lae`apuki and Pu`u `O`o area | med | large | | med | large | Left . Head-on view of East Lae`apuki lava delta. Four main ocean-entry points, and several smaller ones, generate plumes of laze, mainly steam. 1249. Right . Long-shore view of East Lae`apuki lava delta, looking east. Almost all of this delta has been rebuilt since the collapse of November 28. 1249. | med | large | | med | large | Left . Low-level fountaining in East Pond Vent on floor of Pu`u `O`o. Image taken through thick fume, which enhances red color. 1329. Right . Treacherous MLK vent area at southwest base of Pu`u `O`o (cone behind MLK crater.) Note highly cracked surface adjacent to MLK crater. In upper right is Kupaianaha shield, built in late 1980s. 1226. 16 December 2005 Growing lava delta and collapsing Pu`u `O`o | med | large | | med | large | Left . Aerial view looking west at new East Lae`apuki lava delta, built in scar left after collapse of original delta and adjacent old sea cliff on November 28. 0915. Right . Slump blocks on south rim of Pu`u `O`o's crater. Most of the south rim of the cone is badly cracked and waiting to fall, and gaping cracks also cut the south flank of the cone below the rim. 1048. 2 December 2005 East Lae`apuki and Pu`u `O`o | med | large | | med | large | Left . Aerial view of embayment left after destruction of east Lae`apuki lava delta on November 28. Compare with last image taken on November 1. Column of steam and other gases rises from site of new, growing lava delta. 1021. Right . Head-on aerial view of new lava delta and sea cliff behind. The cliff retreated several tens of meters during the November 28 collapse. 1021. | med | large | | med | large | Left . New lava delta and feeding stream of lava emerging from tube high on cliff. 1023. Right . Closer view lava spilling from tube and flowing down fan created by the stream. Note that stream flows into a new tube that is being created by cooling of the surface of the lava. 1023. | med | large | | med | large | Left . Incandescent hole at MLK vent at southwest base of Pu`u `O`o. Hole is 1-2 m across. 1201. Right . Aerial view of East Pond Vent in crater of Pu`u `O`o. 1251. Current Deformation Map of selected deformation stations Electronic Tiltmeter Pu`u `O`o experienced bumpy tilt on January 7, 8, and early January 9; the bumps average out to flat tilt. Uwekahuna inflated slightly until noon January 7, deflated in the afternoon, inflated until early January 8, and then flattened and stayed flat for most of the day. It then started to inflated before midnight and continued up until 2141 January 9. Then Uwekahuna started a rapid, large deflation that finally ended at 2345 January 10 after a loss of 5.2 microradians. Pu`u `O`o inflated during January 8, following Uwekahuna, but it did not plummet when the summit started to deflate, instead maintaining flat to gently declining tilt throughout January 10 and into the 11th. Kilauea's summit began to inflate steeply at 2345 January 10, ending the deflation. The inflation continued through January 11-12-13 and into January 14 and had recovered all the tilt lost by the January 9-10 deflation by early January 14. Pu`u `O`o had pretty flat tilt until about noon January 11 and then began a slow inflation that continued until late morning January 12. The tilt that more or less stabilized before dropping a little that night and through January 13 into January 14, though the deflation was very irregular. This graph shows the radial tilt at Uwekahuna (UWE), on the northwest rim of Kilauea's caldera, and at Pu`u `O`o cone (POC), on the northwest flank of the active vent along the east rift zone, as recorded by continuously operating electronic tiltmeters. Positive changes indicate inflation of the magma storage areas beneath the caldera or Pu`u `O`o. Data are shown for a one-week period. A long-term trend of constant-rate, large deflation at Pu`u `O`o used to be removed for scale reasons, but starting on May 24, 2002, the tilt is shown as recorded, including the long-term deflation. The graph is refreshed at the same time as the eruption update at the top of this page, usually daily. The Y-axis is in microradians, an angular measure in parts per million; for example, one microradian represents the tilt of a 1-km-long bar, one end of which is lifted up or down 1 mm. Global Positioning System (GPS) Two years of data are shown in the plot. Between June 2003 and July 2004 the lengthening between the two stations was generally at a gradually increasing rate. The distance then became stable for nearly a month, but then extension resumed at a slightly slower rate than before the brief stable period. Extension picked up significantly in December 2004 and continued to lengthen rapidly until late February 2005. Then the line rather abruptly started to contract. The contraction ended in mid-March 2005, and the line remained steady until early May, when it began to lengthen once more. The lengthening continued until early July 2005, when the distance stabilized, coincident with a flattening of the tilt at Uwekahuna. Extension then resumed at a quickened rate in late July-early August 2005 and continued to late September. Then the rate of lengthening sharply reduced and perhaps even became zero for a time. Then, in November 2005, the line began to lengthen once more, only to stabilize once more at the end of the year. This graph shows the change in distance between two Global Positioning System (GPS) stations located on opposite ides of Kilauea's caldera. A rapid increase in distance can be interpreted as inflation of the summit magma reservoir. The graph is refreshed at the same time as the eruption update at the top of this page, usually daily. For more information on how electronic tiltmeters and GPS receivers help monitor the deformation of Kilauea and Mauna Loa volcanoes, see a summary of the inflation-deflation of magma chambers . Maps of lava-flow field, Kilauea Volcano Map of flows from Pu`u `O`o: 19 December 2005 Map shows lava flows erupted during 1983-present activity of Pu`u `O`o and Kupaianaha ( see large map ). Yellow, brown, and red colors indicate lava flows erupted from October 2003 to December 16, 2005. Yellow indicates the currently active Kuhio (PKK) flow, active most of the time from March 20, 2004 to the present. The east and west arms of the PKK flow, once widely separated, began to merge and overlap on the coastal flat in March 2005. The east arm feeds the East Lae`apuki ocean entry. Activity on the west arm declined through mid-August, and the last surface flow on that arm was observed on August 21. The recent (November-December 2005) breakouts on Pulama pali described as "eastern" and "western" are all on the east arm of the PKK flow. The brown shade denotes Martin Luther King (MLK ) flows, which first erupted in January 2004 from flank vents on the south slope of Pu`u `O`o. Since then, several more vents have formed in the MLK area and continue to erupt intermittently. Red indicates the Mother's Day and Banana flows, last active in September 2004. Short flows from the crater, West Gap, and Puka Nui vents are also shown in red. In recent months, only the Puka Nui vent has produced infrequent, small flows. Map of Pu`u `O`o and vicinity: 19 December 2005 Map shows vents, lava flows, and other features near Pu`u `O`o frequently referred to in updates ( see large map ). These features can change quickly, but this map should help those viewers lost in the terminology. The vents, lava tubes, and flows active in 2005 include the numbered vents in the crater, the MLK vent complex and associated flows, the Puka Nui vent, and the upper Kuhio (PKK) tube, which feeds the lava flows eventually reaching the ocean. Eruption-viewing opportunities change constantly, so refer to this page often. Those readers planning a visit to Kilauea or Mauna Loa volcanoes can get much useful information from Hawai`i Volcanoes National Park . The URL of this page is http://hvo.wr.usgs.gov/kilauea/update/ Contact: hvowebmaster@usgs.gov Updated: 14 January 2006 (DAS) Molokai Ranch Beach VillageMolokai Travel & Tourism: WorldWeb.com Travel Guide for Molokai, Hawaii MolokaiTravel & Tourism Guide Molokai Ranch Beach Village A special escape with two-bedroom canvas tentalows! Island Divers Hawaii Join us for some fun and exciting scuba diving in Oahu! Island Divers Hawaii Join us for some fun and exciting scuba diving in Oahu! Molokai is the fifth largest island of the Hawaiian archipelago, located between Oahu , Maui and Lanai . Spanning 38 mi (61 km) in length and 10 mi (16 km) in width, Molokai boasts a variety of terrains, from the rainforests of Kamakou Preserve to the sandy shores of Papohaku and Murphy's beaches to rocky hillsides at Pala'au State Park . Beneath its beautiful exterior lies a tragic past, as the island once held native Hawaiians who were exiled in the 1800s. From 1895 to 1969, the island harbored a leper colony, and today visitors can learn about this history at Kalaupapa National Historical Park . Molokai's pristine and undeveloped natural environment makes it popular with eco-tourists. Local companies add to Molokai's enjoyment, such as Molokai Outdoor Adventures , Gypsy Sailing Adventures and Molokai Mule Ride . As birthplace of hula, Molokai hosts the Ka Hula Piko festival each May to celebrate the Hawaiian dance. 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