mauna lowa is a volcano in hawaii
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Mauna Loa is a shield volcano, and as such it has comparatively gentle eruptions (as compared to stratovolcanoes, such as Mt. St. Helens.)  Shield volcanoes also produce high temperature low-viscosity basaltic lava, which contributes to the eruptions being gentle (except in the case of gas in the lava, which can cause fire fountains).\nMore information on shield volcanoes can be found here:\nhttp://en.wikipedia.org/wiki/Shield_volcano
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The two most likely volcanoes in the US (other than Hawaii) are Mt St Helens and Mt Hood. Either could erupt next year or in 30 years, it's only a matter of time.
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Georgia... I hate it... I want to move to a personal island somewhere around Hawaii :)\n\nshh, I can dream :P
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The Sandwich Islands is the name of the chain Also refered to as The Hawaiian Archipelago Or simply the Hawaiian Islands\n\nHawaii, Kahoolawe, Maui, Lanai, Molokai, Oahu, Kauai, and Niihau. The Northwestern Hawaiian Islands, other than Midway, are administratively part of Hawaii.\n\nThe oldest Island is Kure where you find the oldest volcano, Suiko (central) 64.7 Million years old.\n\nThe youngest Island is "The Big Island" of Hawaii, Kilauea volcano is 0.4 Million years old  Mauna Kea is 0.375 Years old
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See the link below for damage related to this Volcano:\n\nhttp://www.volcano.si.edu/world/volcano.cfm?vnum=0202-12=&volpage=erupt&VErupt=Y&VSources=Y&VRep=Y&VWeekly=Y
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Volcano: Mt. St. Helens.\nFold Mountain: Appalachians.\nPlateau: Tibetian.\nShield: Hawaii (take your pick)\nPlain: Great Plains.\nValley: Death Valley.
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Paroreomyza maculata is now known as the Oahu Alauahio\n\nTotal population estimated as fewer than 100 in 1988.\nEstimated as fewer than 10 individuals in 1992\nNone were detected in a 1991 survey. \nLast probable sighting in 1990.\n:-(\n\nSee link for references.
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Sakurajima, Japan \nSantamaria/Santiaguito, Guatemala \nSantorini, Greece \nTaal Volcano, Philippines \nTeide, Canary Islands, Spain \nUlawun, Papua New Guinea \nMount Unzen, Japan \nVesuvius, Italy \nMerapi, Indonesia \nAvachinsky-Koryaksky, Kamchatka, Russia \nColima, Mexico \nMount Etna, Italy \nGaleras, Colombia \nMauna Loa, Hawaii, USA  \nNyiragongo, Democratic Republic of the Congo \nMount Rainier, Washington, USA
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Hawaii maybe but not alaska
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Check this out..\nIt says that someone died during the 1924 eruption,  and that it caused property damage and stuff. A few villages were destroyed. Because of its low slopes the lava dosent flow very fast so most people and wildlife make it out ok. To find the specific info that you need your probably gonna have to pick a handful of eruptions to research each sepratley, and find out the effects that way. \nAlso try looking up Hawian volcano history on the net and see what you can find. \nHope that helps...its not much and I know homework sucks but life uneducated sucks much, much worse. Good luck!\n\nhttp://en.wikipedia.org/wiki/Mauna_Loa
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Mount Merapi did erupted and will be erupt in the next few weeks.\nMostly Merapi (means: Fire Mountain) misunderstood that it will explode and blasting volcanic materials to the atmosphere like a bomb.\nSo far only one "big bomb" explotion of Merapi recognise in the history time, during midlle ages that destroyed Hindus Kindom in Central Java. Even today we can find many of the Hindus and Budhis Temples around the area discovered burried in the ass / volcanic material from that explotion, from few inches up to several feet deep.\nNOwadays, Merapi eruption "only" resulting less then 1 mil plume. It happen because its craters are "open" and the magma/lava can easily flows out of the montain. The good things from Merapi beeing one of THe MOst Active Volcano in the world is that it is "very alife" and nothing really blocking the lava flow.\nThe most deadliest things from Merapi nowadays is the "Nue Ardante" or Piroclastic Flow, fllowing the eruption and Crater falls. Some volcalogist said that if you are accidently cought in the middle of this Piroclastic Flow, it is like you are hited by a hurrican and a hot furnice in the same time!\nIt is very hot! (300 - 600 degree Celcius) and its travel at the min. speed of 120 km per hours!\neven if you drive a car, you can not escape!\nIts only need 3 minutes (sometimes less) to travel from the crater in the top of the mountain to the leg/bottom!\nIts burn eveything! Even seeds 2 feet deep in the ground found death in the eruption in 1994.\nFor more information about Volcanos in Indonesia and how violent its explosion, you may find in some web pages below!\nNote: Indonesia Archipelago has the most Volcanoes in the worlds and also the deadliest
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Mount Pelee Information\nMount Pelee is a lava dome volcano. Mount Pelee, on the Carribbean island of Martinique, is one of about a dozen recently active volcanoes in the 700 kilometer long Lesser Antilles island arc, formed as result of westward subduction of oceanic crust of the South American plate under the oceanic crust of the small Carribean plate.\n\nMartinique was a prosperous French colony at the time of the 1902 eruption. The town of St. Pierre had a population of over 20000, and was located 6 kilometers to the south of the peak of Pelee, a volcano had that a mild eruption in 1851 with little significant damage. On April 25, 1902, minor explosive eruptions started and the following days saw a steady increase in activity. By May 3rd, there were frequent loud explosions from Mt. Pelee and substantial amounts of ash were accumulating in the streets of St. Pierre. On May 5th, a very large mudflow originating from the crater of Mt. Pelee swept down the valley of Riviere Blanche, to the north of St. Pierre. Although many of the residents of St. Pierre attempted to leave the town, the city administration actively discouraged them from doing so, and evacuees from the surrounding country side had swelled the population of the town by May 8th. \n\nAt 7:50 local time on May 8th, a series of deafening explosions were heard from Mt. Pelee, and a huge black cloud issued from the summit of the volcano. The cloud, known as a nuee ardente, or pyroclastic flow, of searing superheated gas and incandescent volcanic ash and dust rushed down the southern and southeastern slopes of Mt. Pelee, and within two minutes (the clocks in the town stopped at 7:52), swept over and engulfed St. Pierre. It set the town ablaze, and killed by intense heat, all but 2 of the population. Masonry walls one meter thick were blown down by the blast, and a 3-ton statue was moved 16 meters! The only survivors were a prisoner in the town jail and a man from a part of town on the fringe of the nuee ardente. A number of ships at anchor off St. Pierre were also devastated, the crew on deck killed and ships caught on fire. \n\nThe eruption continued after May 8th, and on May 20th, a second powerful pyroclastic flow hit St. Pierre, but the damage had already been done by the first cloud. On August 3rd, another pyroclastic flow engulfed the village of Morne Rouge and 2000 people died in almost identical circumstances to those in St. Pierre. The eruption continued well into 1903. Mt. Pelee erupted in 1792 and 1851 but did no damage.
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How about The Aloha Hawaii Festival?
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There are many found in Hawaiian music. Three of my favorites:\n\nBeauty of Mauna Kea - Keola Beamer\nFires of Pele - Ernie Cruz Jr.\nKalapana Sands*- Ernie Cruz Jr.\n\n*Kalapana was a town with black sand beach near Kilauea that was swallowed up by lava flows in 1990. The song is actually about the place before the lava flows, but it has taken on a special poignancy since then. \n\nKîlauea - Alice Nâmakelua\nFirelady- "Sistah" Robi Kahakalau\nKaimana Hila* - Charles E. King \nMauna Loa - Helen Lindsey Parker\n \n* This is a transliteration of "Diamond Head", the famous tuff ring at the end of  Waikiki. The original Hawaiian name of the extinct volcano was Leahi or "forehead of the yellowfin tuna".
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There aren't too many good beginners spots that are sand bottom. Waikiki wave to learn on because the waves are slow and non-threatening. The bottom is rock/coral and the break is CROWDED. There are other breaks like Cockroach Bay (near Sea Life Park), Bellows, and Kalama Beach (north Kailua Beach) that are well known beginners spots. The waves there are non-threatening but are sometimes sloppy because of the winds. Both Bellows and Kalama Beaches are sand bottom and the scenery is awesome.
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The "Ring of Fire" is an arc stretching from New Zealand, along the eastern edge of Asia, north across the Aleutian Islands of Alaska, and south along the coast of North and South America. It is composed over 75% of the world's active and dormant volcanoes.
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Mt. Whitney, Mt. Shasta, Mt Everest & Mt. Kentega