Hawaiian Islands,which are entirely

Hotspots [This Dynamic Earth, USGS] The vast majority of earthquakes and volcanic eruptions occur near plateboundaries, but there are some exceptions. For example, the Hawaiian Islands,which are entirely of volcanic origin, have formed in the middle of thePacific Ocean more than 3,200 km from the nearest plate boundary. How dothe Hawaiian Islands and other volcanoes that form in the interior of platesfit into the plate-tectonics picture? Space Shuttle photograph of the Hawaiian Islands, the southernmostpart of the long volcanic trail of the "Hawaiian hotspot" (seetext). Kauai is in the lower right corner (edge) and the Big Island of Hawaiiin the upper left corner. Note the curvature of the Earth (top edge). (Photographcourtesy of NASA.) In 1963, J. Tuzo Wilson, the Canadian geophysicist who discovered transformfaults, came up with an ingenious idea that became known as the "hotspot"theory. Wilson noted that in certain locations around the world, such asHawaii, volcanism has been active for very long periods of time. This couldonly happen, he reasoned, if relatively small, long-lasting, and exceptionallyhot regions -- called hotspots -- existed below the plates that wouldprovide localized sources of high heat energy (thermal plumes) tosustain volcanism. Specifically, Wilson hypothesized that the distinctivelinear shape of the Hawaiian Island-Emperor Seamounts chain resulted fromthe Pacific Plate moving over a deep, stationary hotspot in the mantle,located beneath the present-day position of the Island of Hawaii. Heat fromthis hotspot produced a persistent source of magma by partly melting theoverriding Pacific Plate. The magma, which is lighter than the surroundingsolid rock, then rises through the mantle and crust to erupt onto the seafloor,forming an active seamount. Over time, countless eruptions cause the seamountto grow until it finally emerges above sea level to form an island volcano.Wilson suggested that continuing plate movement eventually carries the islandbeyond the hotspot, cutting it off from the magma source, and volcanismceases. As one island volcano becomes extinct, another develops over thehotspot, and the cycle is repeated. This process of volcano growth and death,over many millions of years, has left a long trail of volcanic islands andseamounts across the Pacific Ocean floor. According to Wilson's hotspot theory, the volcanoes of the Hawaiian chainshould get progressively older and become more eroded the farther they travelbeyond the hotspot. The oldest volcanic rocks on Kauai, the northwesternmostinhabited Hawaiian island, are about 5.5 million years old and are deeplyeroded. By comparison, on the "Big Island" of Hawaii -- southeasternmostin the chain and presumably still positioned over the hotspot -- the oldestexposed rocks are less than 0.7 million years old and new volcanic rockis continually being formed. Above: Artist's conception of the movement of the PacificPlate over the fixed Hawaiian "Hot Spot," illustrating the formationof the Hawaiian Ridge-Emperor Seamount Chain. (Modified from a drawing providedby Maurice Krafft, Centre de Volcanologie, France). Below: J. TuzoWilson's original diagram (slightly modified), published in 1963, to showhis proposed origin of the Hawaiian Islands. (Reproduced with permissionof the Canadian Journal of Physics .) The possibility that the Hawaiian Islands become younger to the southeastwas suspected by the ancient Hawaiians, long before any scientific studieswere done. During their voyages, sea-faring Hawaiians noticed the differencesin erosion, soil formation, and vegetation and recognized that the islandsto the northwest (Niihau and Kauai) were older than those to the southeast(Maui and Hawaii). This idea was handed down from generation to generationin the legends of Pele, the fiery Goddess of Volcanoes. Pele originallylived on Kauai. When her older sister Namakaokahai, the Goddess of the Sea,attacked her, Pele fled to the Island of Oahu. When she was forced by Namakaokahaito flee again, Pele moved southeast to Maui and finally to Hawaii, whereshe now lives in the Halemaumau Crater at the summit of Kilauea Volcano.The mythical flight of Pele from Kauai to Hawaii, which alludes to the eternalstruggle between the growth of volcanic islands from eruptions and theirlater erosion by ocean waves, is consistent with geologic evidence obtainedcenturies later that clearly shows the islands becoming younger from northwestto southeast. Prominentworld hotspots [54 k] Although Hawaii is perhaps the best known hotspot, others are thought toexist beneath the oceans and continents. More than a hundred hotspots beneaththe Earth's crust have been active during the past 10 million years. Mostof these are located under plate interiors (for example, the African Plate),but some occur near diverging plate boundaries. Some are concentrated nearthe mid-oceanic ridge system, such as beneath Iceland, the Azores, and theGalapagos Islands. A few hotspots are thought to exist below the North American Plate. Perhapsthe best known is the hotspot presumed to exist under the continental crustin the region of Yellowstone National Park in northwestern Wyoming. Hereare several calderas (large craters formed by the ground collapseaccompanying explosive volcanism) that were produced by three gigantic eruptionsduring the past two million years, the most recent of which occurred about600,000 years ago. Ash deposits from these powerful eruptions have beenmapped as far away as Iowa, Missouri, Texas, and even northern Mexico. Thethermal energy of the presumed Yellowstone hotspot fuels more than 10,000hot pools and springs, geysers (like Old Faithful), and bubbling mudpots (pools of boiling mud). A large body of magma, capped by a hydrothermalsystem (a zone of pressurized steam and hot water), still exists beneaththe caldera. Recent surveys demonstrate that parts of the Yellowstone regionrise and fall by as much as 1 cm each year, indicating the area is stillgeologically restless. However, these measurable ground movements, whichmost likely reflect hydrothermal pressure changes, do not necessarily signalrenewed volcanic activity in the area. Authors' Note: Since this booklet's publication in 1996, vigorous scientific debate has ensued regarding volcanism at "hotspots." New studies suggest that hotspots are neither deep phenomena nor "fixed" in position over geologic time, as assumed in the popular plume model. See http://www.mantleplumes.org/ ." Mauna Loa Volcano [36 k] | J. Tuzo Wilson | Longtrail of Hawaiian hotspot | "Contents" "Some unanswered questions" USGS Home Page Top of this Page URL: http://pubs.usgs.gov/publications/text/hotspots.html Last updated: 05.05.99 Contact: jmwatson@usgs.gov

hawaii cruise trip all-inclusive,

hawaii cruise trip hawaii cruise trip Back home | Bookmark | Start page | Site map Services Free postcards News Online games User's forum Free wallpapers Channels Home & Family Family Health Home Kitchen Self help Women Leisure Entertainment Holidays Travel Technology Computers Freeware Internet -- Personal tech Webmastering Business Business Job & Career -- Money & Finance Real estate Science Astronomy Biology Chemistry Ecology & Geology Engineering Medicine Math & Physics Paleo & Archeology Site Search Website directory Submit your site Free email Username: Password: Help Lost password? A Lifetime Cruise Hawaiian Cruise Colin Hartness An Exotic Hawaiian Cruise Trip by Colin Hartness Hawaiian Cruises are everyone's dream cruise to the Hawaiian Islands on an exquisite ocean liner. Being pampered from dawn to dusk with exemplary cuisine, entertainment and fun for all that too for a moderate sum on a Hawaiian Cruise is definitely something out of the world. An increasing number of cruisers and liners are now regularly calling on the Hawaiian ports as also at the neighboring islands of Kaua'i, Maui, Kona and Hilo. Hawaiian Islands, a cluster of 137, provide adventure sports, relaxation and a new insight to oneself. The islands make one wonder whether you are at land or at sea. Hawaiian Cruises transport you to a heavenly state. Because of the tropical latitude, the weather remains the same through most of the year. The eastern side has more rainfall while the western part is the dry land. Locals enjoy skiing and snowboard in the snow-covered areas of the Big Island. The Hawaiian culture is very diverse and almost every nation's culture is found here. Hence, any newcomer is automatically drawn into the Hawaiian culture, which is enjoyment and adventure. Honolulu is the capital city. It is believed that the first permanent inhabitants of this island had sailed in from the islands of Marquesas in the southern hemisphere between 300 and 800 A.D. Hawaiian Cruises along the different yet distinct islands provide an insight into the uniqueness of each island. Hawaii Island is a big one with Kilauea crater, said to be the home of the fire Goddess, Pele. Maui, once the sole property of the royals, is famous for its exquisite swimming spots. The rainbows across the cliffs and waterfalls of Honolulu are nature's splendor. In spite of the diversity the common thing of these islands is 'aloha', the spirit of welcoming. World know Hawaiian people for their hospitality and friendliness. They can mingle easily and in no time have others dancing to their music and enjoying themselves thoroughly with their cuisine. The Hawaiian Cruise enables the visitors to participate in the Hawaiian culture. The vacationing people get unlimited happiness aboard the floating cruise liners and fabulous treatment for little fare. U.S and Canadian citizens need both proofs of citizenship and identity to board Hawaiian Cruise. Proof of identity could be driving license, Government's identification card and in case of children between ages 6 to 17, a school identity card is good enough. In addition to these, a valid passport to sail is also necessary. Permanent residents of the United States need to have on them their Alien Resident Card (ARC). In cases of children traveling without their parents, the legal guardian with them should possess the parent's consent letter authorizing the minor to travel with the guardian, which is also important in case of emergency of any kind. About the Author 2004 All rights reserved Colin Hartness, info@whatcruisers.com Looking for information about cruises? Go to: http://www.whatcruises.com 'What Cruises' is published by Colin Hartness - An excellent resource for Cruises! More articles Syria, travel, Aleppo, Demascus Dining etiquette abroad Hotel ratings holidays vacation checking home security fall georgia pumpkin patches corn mazes farmers visitors halloween hawaii cruise trip all-inclusive, riviera maya, mexico georgia visitors attractions travel terms definition ancient egypt wonders Greece Greek Islands Treck across Tibet Frankfurt Germany Winter road trips Cape Town Carnival cruises Easter Island Orlando Florida Fishing Visiting Memphis Jamaica Dunn's Falls Quotes I thought I had a great idea today, but it never really took off. In fact, it didnt even get on the runway. I guess you could say it exploded in the hangar. - Calvin and Hobbes I refuse to engage in structural engineering discussion of a banana over breakfast.-- Aaron Marsh, Swarthmore 98 Writers If you are a writer and want to see your article published at Theallineed.com, just click here to submit . Info Contact us Privacy policy Terms of use Lexur Today... In the news... Canada's Conservatives oust Liberals after 12 years Canada's right-wing Conservative Party surged to victory in a general election, smashing the 12-year rule of Prime Minister Paul Martin's Liberals, television projections showed. What's your favorite fast food? Hamburger Fried chicken Macaronni Pizza Hot dogs Other Things to ponder Age is a very high price to pay for maturity. Did you know... All race horses become one year older on New Year's Day, no matter when they were born. (see Kentucky Derby Winners) Quote of the day The man who insists on seeing with perfect clearness before he decides, never decides. Henri-Fr?d?ric Amiel Featured article Plants have a double line of defence Max Planck researchers in Cologne, Germany demonstrate that a multi-step defence system underlies the durable resistance of plants to fungal parasites. © 2002/2006 Lexur

Hawaiian Islands,which are entirely

Hotspots [This Dynamic Earth, USGS] The vast majority of earthquakes and volcanic eruptions occur near plateboundaries, but there are some exceptions. For example, the Hawaiian Islands,which are entirely of volcanic origin, have formed in the middle of thePacific Ocean more than 3,200 km from the nearest plate boundary. How dothe Hawaiian Islands and other volcanoes that form in the interior of platesfit into the plate-tectonics picture? Space Shuttle photograph of the Hawaiian Islands, the southernmostpart of the long volcanic trail of the "Hawaiian hotspot" (seetext). Kauai is in the lower right corner (edge) and the Big Island of Hawaiiin the upper left corner. Note the curvature of the Earth (top edge). (Photographcourtesy of NASA.) In 1963, J. Tuzo Wilson, the Canadian geophysicist who discovered transformfaults, came up with an ingenious idea that became known as the "hotspot"theory. Wilson noted that in certain locations around the world, such asHawaii, volcanism has been active for very long periods of time. This couldonly happen, he reasoned, if relatively small, long-lasting, and exceptionallyhot regions -- called hotspots -- existed below the plates that wouldprovide localized sources of high heat energy (thermal plumes) tosustain volcanism. Specifically, Wilson hypothesized that the distinctivelinear shape of the Hawaiian Island-Emperor Seamounts chain resulted fromthe Pacific Plate moving over a deep, stationary hotspot in the mantle,located beneath the present-day position of the Island of Hawaii. Heat fromthis hotspot produced a persistent source of magma by partly melting theoverriding Pacific Plate. The magma, which is lighter than the surroundingsolid rock, then rises through the mantle and crust to erupt onto the seafloor,forming an active seamount. Over time, countless eruptions cause the seamountto grow until it finally emerges above sea level to form an island volcano.Wilson suggested that continuing plate movement eventually carries the islandbeyond the hotspot, cutting it off from the magma source, and volcanismceases. As one island volcano becomes extinct, another develops over thehotspot, and the cycle is repeated. This process of volcano growth and death,over many millions of years, has left a long trail of volcanic islands andseamounts across the Pacific Ocean floor. According to Wilson's hotspot theory, the volcanoes of the Hawaiian chainshould get progressively older and become more eroded the farther they travelbeyond the hotspot. The oldest volcanic rocks on Kauai, the northwesternmostinhabited Hawaiian island, are about 5.5 million years old and are deeplyeroded. By comparison, on the "Big Island" of Hawaii -- southeasternmostin the chain and presumably still positioned over the hotspot -- the oldestexposed rocks are less than 0.7 million years old and new volcanic rockis continually being formed. Above: Artist's conception of the movement of the PacificPlate over the fixed Hawaiian "Hot Spot," illustrating the formationof the Hawaiian Ridge-Emperor Seamount Chain. (Modified from a drawing providedby Maurice Krafft, Centre de Volcanologie, France). Below: J. TuzoWilson's original diagram (slightly modified), published in 1963, to showhis proposed origin of the Hawaiian Islands. (Reproduced with permissionof the Canadian Journal of Physics .) The possibility that the Hawaiian Islands become younger to the southeastwas suspected by the ancient Hawaiians, long before any scientific studieswere done. During their voyages, sea-faring Hawaiians noticed the differencesin erosion, soil formation, and vegetation and recognized that the islandsto the northwest (Niihau and Kauai) were older than those to the southeast(Maui and Hawaii). This idea was handed down from generation to generationin the legends of Pele, the fiery Goddess of Volcanoes. Pele originallylived on Kauai. When her older sister Namakaokahai, the Goddess of the Sea,attacked her, Pele fled to the Island of Oahu. When she was forced by Namakaokahaito flee again, Pele moved southeast to Maui and finally to Hawaii, whereshe now lives in the Halemaumau Crater at the summit of Kilauea Volcano.The mythical flight of Pele from Kauai to Hawaii, which alludes to the eternalstruggle between the growth of volcanic islands from eruptions and theirlater erosion by ocean waves, is consistent with geologic evidence obtainedcenturies later that clearly shows the islands becoming younger from northwestto southeast. Prominentworld hotspots [54 k] Although Hawaii is perhaps the best known hotspot, others are thought toexist beneath the oceans and continents. More than a hundred hotspots beneaththe Earth's crust have been active during the past 10 million years. Mostof these are located under plate interiors (for example, the African Plate),but some occur near diverging plate boundaries. Some are concentrated nearthe mid-oceanic ridge system, such as beneath Iceland, the Azores, and theGalapagos Islands. A few hotspots are thought to exist below the North American Plate. Perhapsthe best known is the hotspot presumed to exist under the continental crustin the region of Yellowstone National Park in northwestern Wyoming. Hereare several calderas (large craters formed by the ground collapseaccompanying explosive volcanism) that were produced by three gigantic eruptionsduring the past two million years, the most recent of which occurred about600,000 years ago. Ash deposits from these powerful eruptions have beenmapped as far away as Iowa, Missouri, Texas, and even northern Mexico. Thethermal energy of the presumed Yellowstone hotspot fuels more than 10,000hot pools and springs, geysers (like Old Faithful), and bubbling mudpots (pools of boiling mud). A large body of magma, capped by a hydrothermalsystem (a zone of pressurized steam and hot water), still exists beneaththe caldera. Recent surveys demonstrate that parts of the Yellowstone regionrise and fall by as much as 1 cm each year, indicating the area is stillgeologically restless. However, these measurable ground movements, whichmost likely reflect hydrothermal pressure changes, do not necessarily signalrenewed volcanic activity in the area. Authors' Note: Since this booklet's publication in 1996, vigorous scientific debate has ensued regarding volcanism at "hotspots." New studies suggest that hotspots are neither deep phenomena nor "fixed" in position over geologic time, as assumed in the popular plume model. See http://www.mantleplumes.org/ ." Mauna Loa Volcano [36 k] | J. Tuzo Wilson | Longtrail of Hawaiian hotspot | "Contents" "Some unanswered questions" USGS Home Page Top of this Page URL: http://pubs.usgs.gov/publications/text/hotspots.html Last updated: 05.05.99 Contact: jmwatson@usgs.gov

WAIKIKI BEACH TOWER ASTON

ASTON WAIKIKI BEACH TOWER - HONOLULU - HONOLULU Hotel Reservations Search Hotels: Hotels | My Account UNITED STATES : HAWAII : HONOLULU : ASTON WAIKIKI BEACH TOWER ASTON WAIKIKI BEACH TOWER 2470 KALAKAUA AVENUE HONOLULU, HI 96815 United States Display Map Property Type: Condominiums Guest Rooms: 140 Additional Photos From the metro city center, this property is located: Direction: Southeast Distance: 0 - 15 minutes Area Airport: Honolulu International Features and Amenities 24 Hour Front Desk Free Local Calls Free Parking Non-smoking Rooms Outdoor Pool Meeting Facilities Laundry/Valet Service Safe Deposit Box Tour Desk/Concierge Full Kitchens Available AM/FM Clock/Radio in Rooms Coffee Maker in Rooms Hair Dryer In Rooms Microwave Oven In Rooms Refrigerator in Rooms Cable Television Hot Tub on site Other Features: Overlooks Waikiki Beach, Washer & Dryer in Rooms Area Attractions Waikiki Beach - adjacent Convention Center - nearby Paddle Tennis - on site International Marketplace - nearby Beach - 1 block Nearby Restaurants Many Restaurants - nearby Meeting Facilities Number of Meeting Rooms: 2 Total Capacity of Meeting Rooms: 40 Room Rates Range (Actual Rate Provided upon Reservation Confirmation) Standard Room Rate Range: USD 411.99 to 1,350.00 Nightly Convert Currency Discounts Available: AAA, AARP Credit Cards Check-in Time: 3:00 PM Check-out Time: 12:00 PM Guarantee Required Cancellation Policy (Local Time): 72 Hours Prior to Arrival Cancel Current Reservation | About The Reservation Function -- Thank you for using cityinsider.com for your worldwide hotels search. If needed, please use our partner websites. Las Vegas Hotels Estate Homes Nevada Real Estate 2003-2004 © cityinsider.com All rights reserved.

Kauai HI

Hanalei Kauai Hawaii Vacation Rental House - Private House Hanalei Kauai Hawaii Vacation Rental House Property Owners Join us VRBO ® is Vacation Rentals by Owner ® Home USA Hawaii Kauai North Kauai Hanalei Edit Vacation Rentals by Owner Listing #25135 On the Beach on Hanalei Bay! Location: Hanalei, North Kauai, Kauai, Hawaii, USA (situated in the center of Beautiful Hanalei Bay) Accommodations: Private House - 2 Bedrooms + Loft - 2 Baths - (Sleeps 6) Bali Hai! Beautiful North Shore Kauai - Hanalei, Kauai, HI - Hawaii Vacation Rental House This charming home is surrounded by the famous lush beauty of Northshore Kauai. Awesome Hanalei Bay spreads out in front of you and majestic waterfall mountains hug you from the back. Located at world famous Pine Trees surf spot in the middle of Hanalei Bay. From this home you can see the tip of Puff the Magic Dragon's famous nose across the beautiful bay to the historic, picturesque Hanalei Pier. This home has been lovingly renovated yet retains all of the old charm and quaintness that has made Hanalei special. Watch whales and world-class surfers from the wrap around lanai all winter and enjoy beautiful sailboats and sunbathers all summer. People watching is a favorite pastime. Sunsets are magical. Rainbows and waterfalls are yours to be experienced. The home has a traditional, Hawaiian plantation style exterior with a lovely, private gated garden. Relax in the hammock and let the swaying palm tree fronds serenade you. Inside every necessary modern convenience has been provided with aloha. There are sumptuous touches that create a real sense of getting away from it all. Here you are in a private, stylish home, in the middle of everything Hanalei! Hanalei is everything that you have read and/or imagined! Hanalei 'town' is minutes walk away so that if you want a 'shave ice' and others want to cruise the shops and still others in your party want to relax at home it all can be done from your perfectly located beach house. This home is one of those 'old Hawaii style' special finds -- it's even better in person than the pictures can show -- can you imagine . . . Chosen by the Fine Living Channel as one of "THE MOST ROMANTIC HOUSES IN THE WORLD!" Great for couples and also a great family house. Please click on our link below for more information and photos. Hanalei Bay! Beautiful North Shore Kauai - Hanalei, Kauai, HI - Hawaii Vacation Rental House Amenities: All the standard amenities PLUS! This non-smoking home includes everything you need to insure an enjoyable holiday. Fully stocked kitchen, just add food (although we provide this service too if you'd like)! Granite Slab Countertops, Microwave, Dishwasher, Refrigerator with Filtered Water, Filtered Ice Maker, Gourmet Cooking Utensils, Gas bbq/grill, phone, tv, DVD, Playstation2, Cable, CD Player, Washer, Dryer, Jetted Tub in Bath, Large walk in shower and an Outdoor shower, Hotel grade linens provided, Hammock, Bamboo Meditation Garden. Activities (on site or nearby): We are located IN the town of Hanalei on Hanalei Bay -- lots of great things to do within walking distance. The guide books are chock full of things to do on Kauai. It's all here! All levels of Surfing, Hiking, Rock Climbing, Biking, Golf, Tennis, Basketball, Yoga, Pilates, Fitness Center/Gym, Fishing, Hunting, Wildlife Viewing, Horseback Riding, Kilauea Lighthouse, Zipline Tour, Shopping, Restaurants, Live Theater, Cinemas, Sightseeing, of course Swimming, Boogey Boarding, Snorkeling, Diving, Boating, Sailing, Waterskiing, Wakeboarding, Windsurfing, Jet Skiing, Shelling and more, or less if you prefer. Rates (in US Dollars): Personal Currency Assistant ™ On the Beach! On Hanalei Bay!Minimum one week stay.Weekly rate is $3800.Extra days are prorated accordingly. Add on services available.Standard 25% Security Deposit,Taxes (Hawaii 11.416%),and $200 Cleaning p/w are only additional fees.Aloha!Note: Until confirmed, rates are subject to change without notice. Just outside your door, the bay greets you! - Hanalei, Kauai, HI - Hawaii Vacation Rental House Links to more information: Click Here to see All My Rental Listings Go to our own site,more photos,more info at kauaichill.com CLICK HERE for a Virtual Tour Note: Each property is individually owned or managed. Dates available:  Thanks for your interest. NOT too early to book Holidays 2006! Before contacting us, please check our calendar for your desired dates. Phone: (808) 482-1888 (Hawaii, USA) Please say: "I saw your listing #25135 on VRBO" Clean! Bright! Hawaii! At Pine Trees Surf Spot! Your Hawaiian Beach Bungalow! The Secluded Hammock in the Gated, Private Garden! Exotic Tropical Hardwood Furniture-The Mango Wave Bedroom! Home USA Hawaii Kauai North Kauai Hanalei Edit Vacation Rentals by Owner Listing #25135 There have been 46756 visitors to this page since the counter was last reset on January 19, 2004 This listing was first published here on June 03, 2003. Hanalei Kauai Hawaii Vacation Rental House Date last modified - January 13, 2006 VRBO® is Vacation Rentals by Owner® - The largest and most popular vacation rental site. Specializing in BY OWNER vacation rentals, homes, condos, cabins, villas and apartments ALSO privately owned properties offered thru rental agencies and management companies. To report any problems with this site contact webmaster@vrbo.com URL: http://www.vrbo.com/25135 ©1995-2006 by VRBO International LLC - all rights reserved