Mount St. HelensMount St. Helens the day before the May 18, 1980, eruption that removed much of the top of the mountainMount St. Helens is an active stratovolcano in Skamania County, Washington, in the Pacific Northwest region of the United States. It is located 96 miles (154 km) south of Seattle and 53 miles (85 km) northeast of Portland, Oregon. The mountain is part of the Cascade Range and was initially known as Louwala-Clough which means "smoking or fire mountain" in the language of the local native Americans, the Klickitats. It was named for British diplomat Lord St Helens who was a friend of George Vancouver, an explorer who made a survey of the area in the late 18th century. This volcano is well known for its ash explosions and pyroclastic flows. It is most famous for the catastrophic eruption on May 18, 1980. That eruption was the most deadly and economically destructive volcanic eruption in the history of the United States. Fifty-seven people were killed and 250 homes, 47 bridges, 15 miles (24 km) of railways and 185 miles (300 km) of highway were destroyed. The eruption caused a massive debris avalanche, reducing its summit from 9,677 feet (2,950 m) to 8,364 feet (2,550 m) in elevation and replacing it with a mile-wide (1.5 km-wide) horseshoe-shaped crater (see geology section or 1980 eruption of Mount St. Helens for more detail). The debris avalanche from the 1980 eruption was up to 0.7 cubic miles (2.3 km3) in volume, making it the largest in recorded history. However, the scale of it still pales in comparison to far larger debris avalanches that have occurred in the geological past elsewhere on Earth. Like most other volcanoes in the Cascade Range, St. Helens is a great cone of rubble consisting of lava rock interlayered with ash, pumice and other deposits. Mount St. Helens includes layers of basalt and andesite through which several domes of dacite lava have erupted. The largest of the dacite domes formed the previous summit; another formed Goat Rocks dome on the northern flank. These were destroyed in St. Helens' 1980 eruption. Mount St. Helens is a part of the Pacific Ring of Fire which includes over 160 active volcanoes. Geographic setting and descriptionLocation of St. Helens within WashingtonMount St. Helens is 34 miles (55 km) almost due west of Mount Adams, which is in the eastern part of the Cascade Range. These "sister and brother" volcanic mountains are each about 50 miles (80 km) from Mount Rainier, the giant of Cascade volcanoes. Mount Hood, the nearest major volcanic peak in Oregon, is about 60 miles (95 km) southeast of Mount St. Helens. Mount St. Helens is geologically young compared to the other major Cascade volcanoes. It was formed only within the last 40,000 years, and the pre-1980 summit cone started to grow only about 2200 years ago. The volcano is also known to have been the most active in the Cascades within the last 10,000 years. Even before its loss of height, Mount St. Helens was not one of the highest peaks in the Cascade Range. Its summit altitude made it only the fifth highest peak in Washington. It stood out prominently, however, from surrounding hills because of the symmetry and the extensive snow and ice-cover of the pre-1980 summit cone, earning it the nickname, "Fujiyama of America" or "Mount Fuji of America". The peak rose more than 5,000 feet (1500 m) above its base, where the lower flanks merge with adjacent ridges. The mountain is about 6 miles (9.5 km) across at its base which is at an altitude of about 4,400 feet (1340 m) on the northeastern side and about 4,000 feet (1220 m) elsewhere. At the pre-eruption timberline (upper limit of trees) the width of the cone was about 4 miles (6.4 km). A view of St Helens and the nearby area from spaceStreams that head on the volcano enter three main river systems — the Toutle River on the north and north-west, the Kalama River on the west, and the Lewis River on the south and east. The streams are fed by abundant rain and snow that dump an average of about 140 inches (3.6 m) of water on Mount St. Helens a year, according to National Weather Service data. The Lewis River is impounded by three dams for hydroelectric power generation. The southern and eastern sides of the volcano drain into an upstream impoundment, the Swift Reservoir, which is directly south of the volcano's peak. Although Mount St. Helens is in Skamania County, Washington the best access routes to the mountain run through Cowlitz County, Washington on the west. Washington State Route 504, locally known as the Spirit Lake Memorial Highway, connects with the heavily traveled Interstate 5 at Exit 49, about 34 miles (55 km) to the west of the mountain. That major north-south highway skirts the low-lying cities of Castle Rock, Longview and Kelso along the Cowlitz River and passes through Vancouver, Washington-Portland, Oregon, metropolitan area less than 50 miles (80 km) to the southwest. The community nearest the volcano is Cougar, Washington which is in the Lewis River valley about 11 miles (18 km) south-southwest of the peak. Gifford Pinchot National Forest surrounds Mount St. Helens, but some land owned by Washington is in private hands. Human historyThe first recorded sighting of Mount St. Helens by Europeans was by Royal Navy Commander George Vancouver and the officers of HMS Discovery on May 19, 1792, while they were surveying the northern Pacific Ocean coast from 1792 to 1794. Vancouver named the mountain for British diplomat Alleyne Fitzherbert, 1st Baron St Helens on October 20, 1792, as it came into view when the Discovery passed into the mouth of the Columbia River. Years later, the mountain was visited by its first major eruption after explorers, traders, and missionaries heard reports of an erupting volcano in the area. Much later geologists and historians determined that the eruption took place in 1800 and was the start of the 57 year long Goat Rocks Eruptive Period (see geology section below). Alarmed by the "dry snow", the Nespelim of northeastern Washington spent a great deal of time in prayer and dance instead of collecting food for winter and therefore had a hard winter. In late 1805 and early 1806 members of the Lewis and Clark Expedition spotted St. Helens from the Columbia River but did not report any eruption in progress or recent evidence of one. They did report the presence of quicksand and clogged channel conditions at the mouth of the Sandy River near Portland, suggesting an eruption by Mount Hood sometime in the previous decades. The first authenticated eyewitness report of a St. Helens eruption was made in March 1835 by Dr. Meredith Gairdner, then working for the Hudson's Bay Company stationed at Fort Vancouver (the first geologist apparently viewed the volcano 6 years later). He sent an account to the Edinburgh New Philosophical Journal, which published his letter in January 1836. James Dwight Dana of Yale University, while sailing with the Charles Wilkes U.S. Exploring Expedition, saw the peak (then quiescent) from off the mouth of the Columbia River in 1841. Another member of the expedition later described "cellular basaltic lavas" at the mountain's base. In either late fall or early winter 1842 the so-called "Great Eruption" was seen by settlers and missionaries in the area. Large ash clouds were reported for this small volume outburst and mild explosions followed for 15 years. All these eruptions were likely phreatic (steam explosions). The Reverend Josiah Parrish in Champoeg, Oregon witnessed Mount St. Helens in eruption on November 22, 1842. Ash from this eruption may have reached The Dalles, Oregon 48 miles (80 km) southeast of the volcano. Future California governor Peter H. Burnett in October 1843 recounted a story of a Native American man who badly burned his foot and leg in either lava or hot ash while hunting for deer. The story went that the injured man sought treatment at Fort Vancouver but the contemporary fort commissary steward, Napolean McGilvery, disclaimed knowledge of the incident. British lieutenant Henry J. Warre sketched the eruption in 1845 and two years later Canadian painter Paul Kane created watercolors of the gently smoking mountain. Warre's work showed erupting material from a vent about a third of the way down from the summit on the mountain's west or northwest side (possibly at Goat Rocks), while one of Kane's field sketches shows smoke emanating from about the same location. On April 17, 1857 the Republican, a Steilacoom, Washington newspaper, reported that "Mount St. Helens, or some other mount to the southward, is seen . . . to be in a state of eruption". The lack of a significant ash layer associated with this event indicates that it was a small eruption, which may have been nothing more than billowing clouds of steam and dust. This was the first reported activity from the volcano since 1854 and the last until 1980. During the lead-up to the 1980 Mount St. Helens eruption, 84 year old innkeeper Harry Truman, who had lived near the mountain for over 50 years, became nationally famous when he decided not to evacuate before the impending eruption, despite repeated pleas by local authorities. His body was never found after the May 18, 1980 eruption, which left a huge crater open to the north (see geology section below). In total, 57 people were killed or never found. Had the eruption occurred one day later, when loggers would have been at work, rather than on a Sunday, the death toll would almost certainly have been much higher. U.S. President Jimmy Carter surveyed the damage and stated it looked more desolate than a moonscape. A film crew, led by Seattle filmmaker Otto Seiber, was dropped by helicopter on St. Helens on May 23 to document the destruction. Their compasses, however, spun in circles and they quickly became lost. A second eruption occurred on May 25, but the crew survived and were rescued two days following the second eruption by National Guard helicopter pilots. Their film became a popular and top-selling documentary "The Eruption of Mount St. Helens." In 1982, President Ronald Reagan and the U.S. Congress established the Mount St. Helens National Volcanic Monument, a 110,000 acre (445 km2) area around the mountain and within the Gifford Pinchot National Forest. Following the 1980 eruption, the area was left to gradually return to its natural state preceding the devastation. Geologic historyAccording to geological evidence, St. Helens started growth in the Pleistocene 37,600 years ago with dacite and andesite eruptions of pumice and ash. 36,000 years ago a large mudflow cascaded down the volcano (mudflows were very significant forces in all of St. Helens' eruptive cycles). Parts of this ancestral cone were fragmented and transported by glaciers 14,000 to 18,000 years ago during the last ice age. Mt. St. Helens is known to have erupted in four major stages, the present having begun around 2500 BC after 6000 years of dormancy. The four stages were interspersed with very long periods of dormancy or low activity levels lasting for up to a few thousand years. Repeated eruptions of pyroclastic flows, pumice, and ash followed until about 8500 BC when the volcano went dormant for roughly 6000 years. The early eruptive stages of the volcano are known as the "Ape Canyon Stage" (around 40–35,000 years ago), the "Cougar Stage" (ca. 20–18,000 years ago), and the "Swift Creek Stage" (roughly 13–8,000 years ago). The period since about 2500 BC is called the "Spirit Lake Stage". Smith Creek and Pine Creek Eruptive PeriodsStarting around 2500 BC, the Smith Creek Eruptive Period began with eruptions of large amounts of ash and yellowish-brown pumice covered thousands of square miles. An eruption in 1900 BC was the largest known eruption from Mt. St. Helens during the Holocene, judging by the volume of one of the tephra layers from that eruptive period. This eruptive cycle lasted until about 1600 BC and left 18 inch (46 cm) deep deposits of material 50 miles (80 km) distant in what is now Mt. Rainier National Park and trace amounts have been found as far northeast as Banff National Park in Alberta and as far southeast as eastern Oregon. All told there may have been up to 2.5 cubic miles (10 km3) of material ejected in this cycle. At the beginning of the Pine Creek Eruptive Period, St. Helens came alive again around 1200 BC after 400 years of dormancy. This cycle, which lasted until about 800 BC, is characterized by smaller volume eruptions. Numerous dense nearly red hot pyroclastic flows sped down St. Helens' flanks and came to rest in nearby valleys. A large mudflow partly filled 40 miles (65 km) of the Lewis River valley sometime between 1000 BC to 500 BC. Castle Creek and Sugar Bowl Eruptive PeriodsThe next eruptive cycle, the Castle Creek Eruptive Period, began roughly around 400 BC and is characterized by a change in composition of St. Helens' lava, which diversified by adding olivine and basalt to the mix. It was during the Castle Creek Period that the pre-1980 summit cone started to form. Also different was the presence of significant lava flows in addition to the previously much more common fragmented and pulverized lavas and rocks (tephra). Large lava flows of andesite and basalt covered parts of the mountain, including one around the year 100 that traveled all the way into the Lewis and Kalama river valleys. Others, such as Cave Basalt (known for its system of lava tubes), flowed up to 8 to 9 miles (13 to 15 km) from their vents. Also around the 1st century, mudflows moved 30 miles (50 km) down Toutle and Kalama river valleys and may have reached the Columbia River. Another 400 or so years of dormancy ensued. Sometime around the year 400, the Sugar Bowl Eruptive Period began with small quantities of ash and lava erupted from St. Helens' north flank. This period ended with the emplacement of dacite domes, including Sugar Bowl around the year 800. Kalama and Goat Rocks Eruptive PeriodsThe symmetrical appearance of St. Helens prior to the 1980 eruption earned it the nickname Mount Fuji of America. The once familiar shape was finalized by the Kalama and Goat Rocks eruptive periods.Roughly 700 years of dormancy was broken about the year 1480 when large amounts of pale gray dacite pumice and ash started to erupt in the Kalama eruptive cycle. The eruption in 1480 was several times larger than the May 18, 1980 eruption. In 1482, another large eruption rivaling the 1980 eruption in volume is known to have occurred. At least seven different beds were laid down in the most voluminous eruptive cycle for 3000 years. Ash and pumice piled to a thickness of three feet (1 m) six miles (9.5 km) northeast from the volcano and two inches (5 cm) deep 50 miles (80 km) away in the same direction. Large pyroclastic flows and mudflows subsequently rushed down St. Helens' west flanks and into the Kalama River drainage system. The source for at least some of these debris flows may have come from the explosion of a dacite dome close to or at the summit. The next phase of this 150 year long cycle saw the eruption of less silica-rich lava in the form of andesitic ash that formed at least eight alternating light and dark-colored layers of ash. After that, blocky andesite lava flowed from St. Helens' summit crater down the volcano's southeast flank. Later, pyroclastic flows raced down over the andesite lava and into the Kalama River valley. This cycle ended with the emplacement of a large dacite dome at the volcano's summit. The several hundred foot high dome filled and overtopped an explosion crater already at the summit. Large parts of the dome's sides broke away and mantled parts of the volcano's cone with talus. Lateral explosions excavated a notch in southeast crater wall. St. Helens reached its greatest height and highly symmetrical form by the time the Kalama eruptive cycle ended on or around 1647. 150 years of quiet returned to the volcano. The 57 year long Goat Rocks Eruptive Period started in 1800 and is the first cycle for which oral and written records exist. As with the Kalama cycle, the sequence of events started with an explosion of dacite tephra followed by an andesite lava flow and then culminated with the emplacement of a dacite dome. The 1800 eruption probably rivalled the May 18, 1980 eruption in size, although unlike the 1980 eruption, it did not result in massive destruction of the cone. The ash drifted northeast over central and eastern Washington, northern Idaho and western Montana. There were at least a dozen small eruptions between 1831 to 1857 of ash reported as well, including a fairly large one in 1842. The vent apparently was at or near Goat Rocks on the northeast flank. The 1980 eruptionMount St. Helens erupted on May 18, 1980, at 8:32 a.m. Pacific Daylight TimeMount St. Helens woke up on March 20, 1980, with a Richter magnitude 5.1 earthquake. Steam venting started on March 27. By the end of April, the north side of the mountain started to bulge. With little warning, a second Richter magnitude 5.1 earthquake triggered a massive collapse of the north face of the mountain on May 18. This was the largest known debris avalanche in recorded history. The magma inside of St. Helens burst forth into a large-scale pyroclastic flow which flattened vegetation and buildings in an area of over 230 square miles (600 km2). This eruption was a 5 on the Volcanic Explosivity Index scale. View of the hillside at the Johnston Ridge Observatory 25 years after the eruption.For more than nine hours, a vigorous plume of ash erupted, eventually reaching 12 to 15 miles (20 to 25 km) above sea level. The plume moved eastward at an average speed of 60 miles per hour (95 km/h), with ash reaching Idaho by noon. The collapse of the northern flank of St. Helens mixed with ice, snow, and water to create lahars (volcanic mudflows). The lahars flowed many miles down the Toutle River and Cowlitz River, destroying bridges and lumber camps. A total of 3.9 million cubic yards (3.0 million m3) of material was transported by the lahars. By around 5:30 p.m. on May 18 the vertical ash column declined in stature and less severe outbursts continued through the night and following several days. In all, St. Helens released an amount of energy equivalent to 27,000 Hiroshima-sized atomic bombs and ejected more than a cubic kilometer of material. The removal of the north side of the mountain reduced St. Helens' height by about 1300 feet (400 m) and left a 1 to 2 mile (1.6 to 3.2 km) wide and 0.5 mile (800 m) deep crater with its north end open in a huge breach. Fifty-seven people were killed along with 1500 elk, 5000 deer, and an estimated 11 million fish. In addition, 200 homes, 47 bridges, and 185 miles (300 km) of highway were destroyed. Post-1980 activityMount St. Helens as seen from the International Space Station in 2002. Lava dome growth profile from 1980-1986.Between 1980 and 1986, activity continued on St. Helens, with a new lava dome forming in the crater. Numerous small explosions and dome-building eruptions occurred during this time. Beginning with the winter snows of 1980-1981, a still unnamed horse shoe-shaped glacier began to evolve in the shadow of the crater. As of 2004, it covers about 0.36 square mile (0.93 km2). Until the beginning of the volcanic activity of 2004, it was considered the only glacier in the lower 48 states of the U.S. that is growing. Between 1989 and 1991, a series of seismic events occurred, sometimes accompanied by small explosions from the dome. Later, in 1995, 1998, and 2001, earthquake swarms were recorded beneath the crater, though without explosive activity. 2004-present activityMount St. Helens became active again in autumn 2004, indicated initially by hundreds and then thousands of localized earthquakes, and followed by several significant emissions of steam and ash. A steam plume rises from the mountain in December 2004 'Whaleback' feature on February 22, 2005.Magma reached the surface of the volcano around October 11, 2004, resulting in the building of a new lava dome on the existing dome's south side. Included in the new dome was a feature dubbed the 'whaleback' (named such due to its close resemblance to the back of a whale), which was a long shaft of solidified magma being exuded by pressure of magma underneath it. This interesting feature was very hot but fragile. The edges of it began crumbling rapidly, forming loose material around the new dome. Currently, the whaleback is still growing but crumbling nearly as rapidly as it is growing. On February 1, 2005, the new lava dome on Mount Saint Helens measured 7,642 feet (2,329 m) in elevation. This brought its elevation to 1,363 feet (415 m) above the 1980 crater floor, approximately 2,000 feet (610 meters) above the surface of the crater glacier, and 721 feet (220 meters) below the highest point of the volcano. The 'whaleback' feature measured approximately 1,550 feet (472 m) in length and 500 feet (152 m) in width. The diameter of the new dome was about 1,700 feet (518 m) at this time and it then contained about 50 million cubic yards (38.5 million m3) of material. The total amount of glacier lost by this date was estimated to be between 5 and 10 percent, but the flow of water out from the crater had changed by almost nothing as the porous nature of the floor of the crater caused the water to be absorbed like a giant sponge. Mount St. Helens had major activity again on March 8, 2005 when a 36,000-foot plume of steam and ash emerged, which was visible from Seattle, Washington and rained ash on Yakima, Washington. This activity was not considered a large eruption, merely a minor release of pressure consistent with the nature of ongoing dome building. The release was accompanied by a 2.5 earthquake. As of May 5, 2005, the highest point on the new dome was 7,675 feet (2339 m), 688 feet (210 m) below the highest point of the volcano. Growth of the new dome continues steadily and has not abated, and small earthquakes continue to be observed every few minutes. The 'whaleback' feature is disintegrating steadily but continues to be extruded as solidified lava pushes upward from underneath it. If the growth of the new dome continues at its current pace, the new dome could replace the amount of material lost in the 1980 eruption (estimated at 3.7 billion cubic yards or 2.85 km3) within the next 40-50 years. The Mount St. Helens VolcanoCam [1] located at Johnston Ridge is able to view the new dome especially at night when the glow of new magma is visible via the camera's infrared capabilities. While geologists warn that an eruption similar to the May 1980 eruption is still possible, the chances are low. On July 2, 2005, the tip of the whaleback feature broke off, causing a rockfall that sent ash and dust several hundred meters into the air. [2] This page about Mt. Saint Helens includes information from a Wikipedia article. Additional articles about Mt. Saint Helens News stories about Mt. Saint Helens External links for Mt. Saint Helens Videos for Mt. Saint Helens Wikis about Mt. Saint Helens Discussion Groups about Mt. Saint Helens Blogs about Mt. Saint Helens Images of Mt. Saint Helens |
|
[2]. The Mount St. The sequel uses a refined camera system, and includes a Drive ability that gives Sora the ability to merge with one of his party members for a short time. If the growth of the new dome continues at its current pace, the new dome could replace the amount of material lost in the 1980 eruption (estimated at 3.7 billion cubic yards or 2.85 km3) within the next 40-50 years. There are new levels exclusive to the sequel, such as Pirates of the Caribbean's Port Royal and The Lion King's Pride Land, as well as new places to visit in old levels; those include the Underworld in the Hercules world and the palace garden in Agrabah. The 'whaleback' feature is disintegrating steadily but continues to be extruded as solidified lava pushes upward from underneath it. The Heartless are still running loose and a mysterious group, Organization XIII, is plotting against Sora. Growth of the new dome continues steadily and has not abated, and small earthquakes continue to be observed every few minutes. Taking place a year after Kingdom Hearts: Chain of Memories, Kingdom Hearts II features Sora, Donald and Goofy, as well as a new cast of characters, including King Mickey himself and familiar faces. As of May 5, 2005, the highest point on the new dome was 7,675 feet (2339 m), 688 feet (210 m) below the highest point of the volcano. A second sequel, Kingdom Hearts II for the PlayStation 2, was officially released in Japan on 22 December 2005 and will be released in USA on 28 March 2006. The release was accompanied by a 2.5 earthquake. The game was released on December 7, 2004. This activity was not considered a large eruption, merely a minor release of pressure consistent with the nature of ongoing dome building. These cards can be used to create new worlds, open doors, and attack Heartless. Helens had major activity again on March 8, 2005 when a 36,000-foot plume of steam and ash emerged, which was visible from Seattle, Washington and rained ash on Yakima, Washington. The game abandoned the Kingdom Hearts battle system, focusing instead on card-based game play. Mount St. As both Sora and Riku fight their ways through the castle, piecing together what is real and what is not, they are unaware that they are being targeted by a mysterious organization. The total amount of glacier lost by this date was estimated to be between 5 and 10 percent, but the flow of water out from the crater had changed by almost nothing as the porous nature of the floor of the crater caused the water to be absorbed like a giant sponge. At the same time, Riku escapes from Kingdom Hearts and finds his own way to Castle Oblivion, where he must contend with the lingering darkness of Xehanort in his heart. The diameter of the new dome was about 1,700 feet (518 m) at this time and it then contained about 50 million cubic yards (38.5 million m3) of material. There, the group visits replicas of the worlds in the original game, created by Sora's memories. The 'whaleback' feature measured approximately 1,550 feet (472 m) in length and 500 feet (152 m) in width. In the beginning, Sora, Donald and Goofy meet a mysterious man who leads them to Castle Oblivion, a strange castle where even memories cannot be trusted. This brought its elevation to 1,363 feet (415 m) above the 1980 crater floor, approximately 2,000 feet (610 meters) above the surface of the crater glacier, and 721 feet (220 meters) below the highest point of the volcano. Kingdom Hearts: Chain of Memories, the Game Boy Advance sequel to the original game, takes place directly after the plot of Kingdom Hearts, and provides the link between Kingdom Hearts and Kingdom Hearts II. On February 1, 2005, the new lava dome on Mount Saint Helens measured 7,642 feet (2,329 m) in elevation. It is unknown how many of them have been made in Japan. Currently, the whaleback is still growing but crumbling nearly as rapidly as it is growing. Currently, two volumes of the English version of the manga are available. The edges of it began crumbling rapidly, forming loose material around the new dome. The manga is published in English in the United States by TOKYOPOP (ISBN 1598162179) and in English in Singapore by Chuang Yi. This interesting feature was very hot but fragile. There is a manga based off of the video game written and illustrated by Shiro Amano. Included in the new dome was a feature dubbed the 'whaleback' (named such due to its close resemblance to the back of a whale), which was a long shaft of solidified magma being exuded by pressure of magma underneath it. Although he apologized to Square (not yet merged with Enix at that point) in the radio interview, he firmly believed that the game did not deserve its Japanese sales or its (then) 6800 Yen price tag. Magma reached the surface of the volcano around October 11, 2004, resulting in the building of a new lava dome on the existing dome's south side. He expressed disappointment because Kingdom Hearts outsold his GameCube remake of Resident Evil in Japan, believing that his game was the superior product. Helens became active again in autumn 2004, indicated initially by hundreds and then thousands of localized earthquakes, and followed by several significant emissions of steam and ash. Shinji Mikami, creator of Capcom's Resident Evil series, criticized Kingdom Hearts on Japanese radio in 2002. Mount St. The developers seem to have taken these comments onboard as the sequel, Kingdom Hearts II, features an overhaul of this aspect of the series by making the ship missions much more fast paced then in the original Kingdom Hearts. Later, in 1995, 1998, and 2001, earthquake swarms were recorded beneath the crater, though without explosive activity. Another criticism levelled by reviewers and players alike revolves around the Gummi ship missions, with the main complaint being that they are not up to the same standard of play as the rest of game. Between 1989 and 1991, a series of seismic events occurred, sometimes accompanied by small explosions from the dome. Elements of the combat system were also criticized, particularly the use of menu-based items and magic in what was a frequently hectic real-time battle scenario, and the awkward camera angles that could occur during battle. that is growing. Some Final Fantasy fans were critical of the combination of the Final Fantasy mythos and the role-playing genre with Disney characters and other elements that they considered to be for children. Until the beginning of the volcanic activity of 2004, it was considered the only glacier in the lower 48 states of the U.S. Some also felt that, while original, the combination of Square and Disney did not work as well as it could have, with aspects of both the story and gameplay swinging between 'Disney-style' and 'Square-style', without reaching an acceptable middle ground for most of the game. As of 2004, it covers about 0.36 square mile (0.93 km2). Some fans also disapproved of the casting of the voice actors for the more popular Final Fantasy characters: in particular, the casting of pop music singers Mandy Moore as Aerith Gainsborough and Lance Bass as Sephiroth. Beginning with the winter snows of 1980-1981, a still unnamed horse shoe-shaped glacier began to evolve in the shadow of the crater. For example, several prominent characters are made much younger and do not play a major role in the story. Numerous small explosions and dome-building eruptions occurred during this time. Kingdom Hearts has been criticized by some Final Fantasy fans for making poor use of the Final Fantasy characters placed in it. Helens, with a new lava dome forming in the crater. The emphasis on characters from later Final Fantasy installments disappointed fans; the refusal to use earlier characters stems from character designer Tetsuya Nomura's hesitation to use characters he did not design. Between 1980 and 1986, activity continued on St. The names of various spells are the names of Gummi blocks, and various summons, weapons, bosses, and monsters are the names of Gummi ships blueprints. In addition, 200 homes, 47 bridges, and 185 miles (300 km) of highway were destroyed. Cure, Cura, Curaga, etc.) is also in place. Fifty-seven people were killed along with 1500 elk, 5000 deer, and an estimated 11 million fish. The Final Fantasy magic naming system (ie. Helens' height by about 1300 feet (400 m) and left a 1 to 2 mile (1.6 to 3.2 km) wide and 0.5 mile (800 m) deep crater with its north end open in a huge breach. This and several other weapons, such as Lionheart and Save the Queen, share names with other weapons from previous entries in the Final Fantasy series. The removal of the north side of the mountain reduced St. Moogles make an appearance and help the player obtain the ultimate weapon (the aptly named Ultima Weapon). Helens released an amount of energy equivalent to 27,000 Hiroshima-sized atomic bombs and ejected more than a cubic kilometer of material. The game also uses other Final Fantasy icons. In all, St. Cloud and Sephiroth make appearances, including a cutscene fight between both in Final Mix. on May 18 the vertical ash column declined in stature and less severe outbursts continued through the night and following several days. Rikku from Final Fantasy X and Irvine Kinneas from Final Fantasy VIII were both originally set to make cameo appearances, but were replaced by Yuffie and Wakka respectively. By around 5:30 p.m. In Traverse Town, the player encounters Squall (under the alias of "Leon") from Final Fantasy VIII, as well as Aerith, Cid, and Yuffie from Final Fantasy VII. A total of 3.9 million cubic yards (3.0 million m3) of material was transported by the lahars. On Destiny Islands, the player meets younger versions of Tidus, Wakka (both from Final Fantasy X), and Selphie (from Final Fantasy VIII). The lahars flowed many miles down the Toutle River and Cowlitz River, destroying bridges and lumber camps. It is in these cameos that gamers base arguments on the inclusion of this game in the Final Fantasy series. Helens mixed with ice, snow, and water to create lahars (volcanic mudflows). One of the less important quests of the game is to find the 99 lost dalmatian puppies from all over the game, while there is a statue of Lady and the Tramp in the Third District of Traverse Town. The collapse of the northern flank of St. The title roles of One Hundred and One Dalmatians and Lady and the Tramp have cameo appearances in the game, too. The plume moved eastward at an average speed of 60 miles per hour (95 km/h), with ash reaching Idaho by noon. Only the Genie and Tinkerbell summons are automatically obtained; the others must be gained by obtaining unique gems and giving them to the Fairy Godmother from Cinderella. For more than nine hours, a vigorous plume of ash erupted, eventually reaching 12 to 15 miles (20 to 25 km) above sea level. The player can summon Simba from The Lion King, the Genie from Aladdin, Bambi, Dumbo, Tinkerbell from Peter Pan, and Mushu from Mulan. This eruption was a 5 on the Volcanic Explosivity Index scale. These characters replace Sora's two companions for the duration of the summon. Helens burst forth into a large-scale pyroclastic flow which flattened vegetation and buildings in an area of over 230 square miles (600 km2). In addition, various Disney characters can be temporarily summoned during battle. The magma inside of St. For instance, Jack Skellington joins the player's party in the Nightmare Before Christmas world, but will not accompany the player elsewhere. This was the largest known debris avalanche in recorded history. Most worlds have a unique computer-controlled party member who can be chosen to replace Goofy or Donald in the party. With little warning, a second Richter magnitude 5.1 earthquake triggered a massive collapse of the north face of the mountain on May 18. Goofy and Donald are the only computer-controlled characters that are usable on every world. By the end of April, the north side of the mountain started to bulge. The computer controlled characters can have their behavior altered by the player, changing their item usages from "frequently" to "occasionally" for example. Steam venting started on March 27. Sora is the only character directly controlled by the player; other members in the party are computer controlled. Helens woke up on March 20, 1980, with a Richter magnitude 5.1 earthquake. Several traits can also be altered further by permanent boost items or equipped item effects. Mount St. Sora's stats are more customizable; the player can select what attribute to excel in and which attribute to be lacking in, such as defense, magic or strength, at the beginning of the game. The vent apparently was at or near Goat Rocks on the northeast flank. The main characters are Sora, Donald Duck, and Goofy. There were at least a dozen small eruptions between 1831 to 1857 of ash reported as well, including a fairly large one in 1842. Examples such as this convey a stronger sense of nostalgia when paired with characters, settings and voice clips from popular Disney films. The ash drifted northeast over central and eastern Washington, northern Idaho and western Montana. For instance, when in Atlantica (The world from The Little Mermaid), the background music is a non-lyrical reinterpretation of the song 'Under the Sea'. The 1800 eruption probably rivalled the May 18, 1980 eruption in size, although unlike the 1980 eruption, it did not result in massive destruction of the cone. While there are many original themes written specifically for the game by Shimomura, most of the soundtrack is comprised of popular melodies derived from classic disney films. As with the Kalama cycle, the sequence of events started with an explosion of dacite tephra followed by an andesite lava flow and then culminated with the emplacement of a dacite dome. Both versions of the song were composed and performed by Utada Hikaru. The 57 year long Goat Rocks Eruptive Period started in 1800 and is the first cycle for which oral and written records exist. The music is composed by Yoko Shimomura, the ending credits theme and opening orchestration is by Kaoru Wada, and the main vocal theme is "Hikari" (Light) known as "Simple and Clean" in Western releases. 150 years of quiet returned to the volcano. The original worlds:. Helens reached its greatest height and highly symmetrical form by the time the Kalama eruptive cycle ended on or around 1647. The Disney-based worlds:. St. The many worlds in which the game takes place include various Disney settings (nearly all of which are part of the Disney animated features canon), as well as some original ones. Lateral explosions excavated a notch in southeast crater wall. Other changes include new abilities, new weapons, new items, additional and recolored enemies; and gameplay tweaks to make the game easier for the player, along with two new difficulty levels. Large parts of the dome's sides broke away and mantled parts of the volcano's cone with talus. The Night on the Bald Mountain track from the English version has been included as well. The several hundred foot high dome filled and overtopped an explosion crater already at the summit. New music was incorporated; the tracks are Disappeared and Another Side. This cycle ended with the emplacement of a large dacite dome at the volcano's summit. In another attempt at foreshadowing, a video called Another Side, Another Story: Deep Dive will play along with Another Side, Another Story if the player accomplishes certain tasks. Later, pyroclastic flows raced down over the andesite lava and into the Kalama River valley. The optional bosses first included in the English version were introduced to Japanese players for the first time, along with the "Engimatic Man", in an attempt to raise interest for the sequel. Helens' summit crater down the volcano's southeast flank. A gameplay tweak allows the player to skip cutscenes after seeing them once. After that, blocky andesite lava flowed from St. New scenes, clarifying certain plot points, such as Riku's journey and foreshadowing of Kingdom Hearts II, were included. The next phase of this 150 year long cycle saw the eruption of less silica-rich lava in the form of andesitic ash that formed at least eight alternating light and dark-colored layers of ash. Spoken dialogue was in English, with Japanese subtitles. The source for at least some of these debris flows may have come from the explosion of a dacite dome close to or at the summit. Kingdom Hearts was re-released in Japan as Kingdom Hearts: Final Mix, this version had several events and a number of gameplay tweaks that were not in the American, European and Australian releases. Helens' west flanks and into the Kalama River drainage system. Yoko Shimomura's arrangement of Night on Bald Mountain was set as the background music for the Chernabog boss fight, whereas the original Japanese version uses generic boss music. Large pyroclastic flows and mudflows subsequently rushed down St. Besides English localization, three additional optional bosses were added, notably Sephiroth. Ash and pumice piled to a thickness of three feet (1 m) six miles (9.5 km) northeast from the volcano and two inches (5 cm) deep 50 miles (80 km) away in the same direction. The English version of Kingdom Hearts had new features that were not found in the original version of Kingdom Hearts in Japan. At least seven different beds were laid down in the most voluminous eruptive cycle for 3000 years. Sora promises to return to Kairi once he finds a way to bring Riku out of Kingdom Hearts. In 1482, another large eruption rivaling the 1980 eruption in volume is known to have occurred. Sora and Kairi's reunion is cut extremely short as they are pulled apart by the reforming Destiny Islands. The eruption in 1480 was several times larger than the May 18, 1980 eruption. Before the door is locked, Riku tells Sora to take care of Kairi. Roughly 700 years of dormancy was broken about the year 1480 when large amounts of pale gray dacite pumice and ash started to erupt in the Kalama eruptive cycle. Using his own Keyblade, Mickey locks Kingdom Hearts from the inside, but this forces himself and Riku to stay inside. This period ended with the emplacement of dacite domes, including Sugar Bowl around the year 800. Riku, who has regained his body, helps the others close the door on the other side, along with King Mickey Mouse. Helens' north flank. Sora, Donald and Goofy attempt to close the door, but their strength is not enough. Sometime around the year 400, the Sugar Bowl Eruptive Period began with small quantities of ash and lava erupted from St. Though the light of Kingdom Hearts defeated Ansem, the door threatens to unleash millions upon millions of Heartless onto the universe. Another 400 or so years of dormancy ensued. They return to lock the keyhole and later travel to Kingdom Hearts itself, facing Ansem in a climactic final battle. Also around the 1st century, mudflows moved 30 miles (50 km) down Toutle and Kalama river valleys and may have reached the Columbia River. They flee Hollow Bastion in face of the immense number of Heartless pouring through the pathway to Kingdom Hearts. Others, such as Cave Basalt (known for its system of lava tubes), flowed up to 8 to 9 miles (13 to 15 km) from their vents. Knowing that it was truly Sora, Kairi's light pulled him from the infinite darkness and restores Sora. Large lava flows of andesite and basalt covered parts of the mountain, including one around the year 100 that traveled all the way into the Lewis and Kalama river valleys. Now a Heartless, Sora scampered to Kairi's protection. Also different was the presence of significant lava flows in addition to the previously much more common fragmented and pulverized lavas and rocks (tephra). However, the pathway to Kingdom Hearts was opened. It was during the Castle Creek Period that the pre-1980 summit cone started to form. In order to free Kairi's heart, Sora impales himself on Ansem's Keyblade, losing his own heart while restoring Kairi and freeing the other Princesses' hearts, as the Keyblade was composed of their hearts. Helens' lava, which diversified by adding olivine and basalt to the mix. Sora and Ansem battle, with Sora as the victor. The next eruptive cycle, the Castle Creek Eruptive Period, began roughly around 400 BC and is characterized by a change in composition of St. Kairi is revealed to be a Princess of Heart, and her heart was trapped in Sora's body ever since they got separated. A large mudflow partly filled 40 miles (65 km) of the Lewis River valley sometime between 1000 BC to 500 BC. Ansem desires to become part of what he believes to be the primordial phase of existence, the darkness that he believes to compose Kingdom Hearts. Helens' flanks and came to rest in nearby valleys. Only, this time, it is not truly Riku; it is actually Ansem, the scientist who was researching Heartless, occupying Riku's body. Numerous dense nearly red hot pyroclastic flows sped down St. Sora confronts Riku again. This cycle, which lasted until about 800 BC, is characterized by smaller volume eruptions. Sora's party meets and exceeds the challenge, destroying Maleficent. Helens came alive again around 1200 BC after 400 years of dormancy. This transformed Maleficent into a dragon that reflected the darkness in her heart. At the beginning of the Pine Creek Eruptive Period, St. Sora and his teammates face and defeat Maleficent, allowing a strangely-behaved Riku to strike her with a unique type of Keyblade, one that opened hearts. All told there may have been up to 2.5 cubic miles (10 km3) of material ejected in this cycle. Riku impulsively accepts. Rainier National Park and trace amounts have been found as far northeast as Banff National Park in Alberta and as far southeast as eastern Oregon. It is during this time that a mysterious being offers him greater power with which he could use to defeat Sora. This eruptive cycle lasted until about 1600 BC and left 18 inch (46 cm) deep deposits of material 50 miles (80 km) distant in what is now Mt. Unfettered by the loss of his weapon, Sora puts his faith into his friends and wins back the Keyblade, sending Riku to run off and lick his wounds. Helens during the Holocene, judging by the volume of one of the tephra layers from that eruptive period. Finally reaching Hollow Bastion, Maleficent's headquarters, Sora confronts Riku directly, ending with the revelation that Riku is also a Keyblade master and with the loss of Sora's own Keyblade. St. The goal of Maleficent and her group is to collect seven maidens of the purest heart, the "Princesses of Heart", in order to open the pathway to Kingdom Hearts, which is supposedly a repository of power and knowledge Maleficent intends to use in her plan to rule all worlds. An eruption in 1900 BC was the largest known eruption from Mt. Seeing Sora as apathetic towards Kairi's fate, Riku has taken reponsibility into his hands and struck a deal with Maleficent, in order to help Kairi regain her sense of self. Starting around 2500 BC, the Smith Creek Eruptive Period began with eruptions of large amounts of ash and yellowish-brown pumice covered thousands of square miles. Standing in their way, however, is a cabal of Disney villains, with Maleficent as their leader and Riku as her apprentice. The period since about 2500 BC is called the "Spirit Lake Stage". Along their way, they lock "keyholes" to the heart of those worlds, preventing the Heartless from consuming their worlds. 20–18,000 years ago), and the "Swift Creek Stage" (roughly 13–8,000 years ago). In their adventure, the trio explore many Disney-themed worlds, including Aladdin's Agrabah and The Little Mermaid's Atlantica. The early eruptive stages of the volcano are known as the "Ape Canyon Stage" (around 40–35,000 years ago), the "Cougar Stage" (ca. From the Destiny Islands, Sora lands in Traverse Town, where he joins Goofy and Donald Duck in their quest to find King Mickey Mouse and defeat the Heartless. Repeated eruptions of pyroclastic flows, pumice, and ash followed until about 8500 BC when the volcano went dormant for roughly 6000 years. After the battle, Sora receives his weapon, the mystical Keyblade, and sets out to defeat the Heartless and be reunited with his friends. The four stages were interspersed with very long periods of dormancy or low activity levels lasting for up to a few thousand years. When Sora finds Riku surrounded by darkness, Riku disappears and Sora has to fight the Heartless, who are being used to tear down the walls between worlds. Helens is known to have erupted in four major stages, the present having begun around 2500 BC after 6000 years of dormancy. The three friends are separated. St. The night before the voyage, a storm sweeps through the island, and evil shadow-creatures called the Heartless appear. Mt. The three children wish to leave the island that they have been confined to all their life, so they build a raft to escape. Parts of this ancestral cone were fragmented and transported by glaciers 14,000 to 18,000 years ago during the last ice age. Kingdom Hearts begins on the lush, tropical islands called "Destiny Islands", home to the main characters Sora, Riku, and Kairi. Helens' eruptive cycles). . 36,000 years ago a large mudflow cascaded down the volcano (mudflows were very significant forces in all of St. The game features real-time rendered backgrounds and scenery. Helens started growth in the Pleistocene 37,600 years ago with dacite and andesite eruptions of pumice and ash. Although the game's primary plotlines follow characters who were created specifically for Kingdom Hearts, characters from both companies play major roles in the game and its storyline. According to geological evidence, St. The game combines characters and settings from Disney's animated features and films with those from Square's Final Fantasy RPG series. Following the 1980 eruption, the area was left to gradually return to its natural state preceding the devastation. Kingdom Hearts (Japanese: キングダムハーツ Kingudamu Hātsu) is a hybrid action/RPG that was released in 2002, which is notable for being the result of a collaboration between the video game developer and publisher Square and Disney. Helens National Volcanic Monument, a 110,000 acre (445 km2) area around the mountain and within the Gifford Pinchot National Forest. as Mickey Mouse. Congress established the Mount St. Yakashi Aoyagi .. In 1982, President Ronald Reagan and the U.S. as Piglet. Helens.". Kiyoshi Komiyama .. Their film became a popular and top-selling documentary "The Eruption of Mount St. as Tigger. A second eruption occurred on May 25, but the crew survived and were rescued two days following the second eruption by National Guard helicopter pilots. Tesshō Genda .. Their compasses, however, spun in circles and they quickly became lost. as Winnie the Pooh. Helens on May 23 to document the destruction. Shun Yashiro .. A film crew, led by Seattle filmmaker Otto Seiber, was dropped by helicopter on St. as Wendy. President Jimmy Carter surveyed the damage and stated it looked more desolate than a moonscape. Yuriko Fuchisaki .. U.S. Smee. Had the eruption occurred one day later, when loggers would have been at work, rather than on a Sunday, the death toll would almost certainly have been much higher. as Mr. In total, 57 people were killed or never found. Kazuo Kumakura .. His body was never found after the May 18, 1980 eruption, which left a huge crater open to the north (see geology section below). as Captain Hook. Helens eruption, 84 year old innkeeper Harry Truman, who had lived near the mountain for over 50 years, became nationally famous when he decided not to evacuate before the impending eruption, despite repeated pleas by local authorities. Chikao Ohtsuka .. During the lead-up to the 1980 Mount St. as Peter Pan. This was the first reported activity from the volcano since 1854 and the last until 1980. Mitsuo Iwata .. The lack of a significant ash layer associated with this event indicates that it was a small eruption, which may have been nothing more than billowing clouds of steam and dust. as Barrel. to be in a state of eruption". Shigeo Matsuzawa .. Helens, or some other mount to the southward, is seen . . . as Lock. On April 17, 1857 the Republican, a Steilacoom, Washington newspaper, reported that "Mount St. Shintaro Sono'oka .. Warre's work showed erupting material from a vent about a third of the way down from the summit on the mountain's west or northwest side (possibly at Goat Rocks), while one of Kane's field sketches shows smoke emanating from about the same location. as Oogie Boogie. Warre sketched the eruption in 1845 and two years later Canadian painter Paul Kane created watercolors of the gently smoking mountain. Hiroshi Hatanaka .. British lieutenant Henry J. Finklestein. The story went that the injured man sought treatment at Fort Vancouver but the contemporary fort commissary steward, Napolean McGilvery, disclaimed knowledge of the incident. as Dr. Burnett in October 1843 recounted a story of a Native American man who badly burned his foot and leg in either lava or hot ash while hunting for deer. Yuji Mitsuya .. Future California governor Peter H. as the Mayor. Ash from this eruption may have reached The Dalles, Oregon 48 miles (80 km) southeast of the volcano. Toru Ohira .. Helens in eruption on November 22, 1842. as Jack Skellington. The Reverend Josiah Parrish in Champoeg, Oregon witnessed Mount St. Masachika Ichimura .. All these eruptions were likely phreatic (steam explosions). as Flotsam and Jetsam. Large ash clouds were reported for this small volume outburst and mild explosions followed for 15 years. Shuichiro Moriyama .. In either late fall or early winter 1842 the so-called "Great Eruption" was seen by settlers and missionaries in the area. as Ursula. Another member of the expedition later described "cellular basaltic lavas" at the mountain's base. Kujira .. Exploring Expedition, saw the peak (then quiescent) from off the mouth of the Columbia River in 1841. as King Triton. James Dwight Dana of Yale University, while sailing with the Charles Wilkes U.S. Taro Ishida .. He sent an account to the Edinburgh New Philosophical Journal, which published his letter in January 1836. as Geppetto. Meredith Gairdner, then working for the Hudson's Bay Company stationed at Fort Vancouver (the first geologist apparently viewed the volcano 6 years later). Kazuo Kumakura .. Helens eruption was made in March 1835 by Dr. as Pinocchio, Flounder. The first authenticated eyewitness report of a St. Yuki Tokiwa .. They did report the presence of quicksand and clogged channel conditions at the mouth of the Sandy River near Portland, suggesting an eruption by Mount Hood sometime in the previous decades. as Iago. Helens from the Columbia River but did not report any eruption in progress or recent evidence of one. Akira Kamiya .. In late 1805 and early 1806 members of the Lewis and Clark Expedition spotted St. as Jafar. Alarmed by the "dry snow", the Nespelim of northeastern Washington spent a great deal of time in prayer and dance instead of collecting food for winter and therefore had a hard winter. Akira Takarada .. Much later geologists and historians determined that the eruption took place in 1800 and was the start of the 57 year long Goat Rocks Eruptive Period (see geology section below). as Jasmine. Years later, the mountain was visited by its first major eruption after explorers, traders, and missionaries heard reports of an erupting volcano in the area. Kaori Aso .. Vancouver named the mountain for British diplomat Alleyne Fitzherbert, 1st Baron St Helens on October 20, 1792, as it came into view when the Discovery passed into the mouth of the Columbia River. as Aladdin. Helens by Europeans was by Royal Navy Commander George Vancouver and the officers of HMS Discovery on May 19, 1792, while they were surveying the northern Pacific Ocean coast from 1792 to 1794. Shinichiro Miki .. The first recorded sighting of Mount St. as Terk, Sally, Shock. Helens, but some land owned by Washington is in private hands. Yuko Doi .. Gifford Pinchot National Forest surrounds Mount St. as Jane Porter, Ariel. The community nearest the volcano is Cougar, Washington which is in the Lewis River valley about 11 miles (18 km) south-southwest of the peak. Mayumi Suzuki .. That major north-south highway skirts the low-lying cities of Castle Rock, Longview and Kelso along the Cowlitz River and passes through Vancouver, Washington-Portland, Oregon, metropolitan area less than 50 miles (80 km) to the southwest. as Clayton. Washington State Route 504, locally known as the Spirit Lake Memorial Highway, connects with the heavily traveled Interstate 5 at Exit 49, about 34 miles (55 km) to the west of the mountain. Banjō Ginga .. Helens is in Skamania County, Washington the best access routes to the mountain run through Cowlitz County, Washington on the west. as Tarzan. Although Mount St. Juurouta Kosugi .. The southern and eastern sides of the volcano drain into an upstream impoundment, the Swift Reservoir, which is directly south of the volcano's peak. as Hades. The Lewis River is impounded by three dams for hydroelectric power generation. Kyusaku Shimada .. Helens a year, according to National Weather Service data. as Philoctetes (Phil). The streams are fed by abundant rain and snow that dump an average of about 140 inches (3.6 m) of water on Mount St. Ichiro Nagai .. Streams that head on the volcano enter three main river systems — the Toutle River on the north and north-west, the Kalama River on the west, and the Lewis River on the south and east. as Hercules. At the pre-eruption timberline (upper limit of trees) the width of the cone was about 4 miles (6.4 km). Yasunori Matsumoto .. The mountain is about 6 miles (9.5 km) across at its base which is at an altitude of about 4,400 feet (1340 m) on the northeastern side and about 4,000 feet (1220 m) elsewhere. as the Doorknob. The peak rose more than 5,000 feet (1500 m) above its base, where the lower flanks merge with adjacent ridges. Takehiro Koyama .. It stood out prominently, however, from surrounding hills because of the symmetry and the extensive snow and ice-cover of the pre-1980 summit cone, earning it the nickname, "Fujiyama of America" or "Mount Fuji of America". as the Queen Of Hearts. Its summit altitude made it only the fifth highest peak in Washington. Sumie Ozawa .. Helens was not one of the highest peaks in the Cascade Range. as the White Rabbit. Even before its loss of height, Mount St. Shigeru Ushiyama .. The volcano is also known to have been the most active in the Cascades within the last 10,000 years. as Daisy Duck and Alice. It was formed only within the last 40,000 years, and the pre-1980 summit cone started to grow only about 2200 years ago. Mika Doi .. Helens is geologically young compared to the other major Cascade volcanoes. as Minnie Mouse. Mount St. Yuko Mizutani .. Helens. as Wakka. Mount Hood, the nearest major volcanic peak in Oregon, is about 60 miles (95 km) southeast of Mount St. Kazuya Nakai .. These "sister and brother" volcanic mountains are each about 50 miles (80 km) from Mount Rainier, the giant of Cascade volcanoes. as Tidus. Helens is 34 miles (55 km) almost due west of Mount Adams, which is in the eastern part of the Cascade Range. Masakazu Morita .. Mount St. as Selphie. . Mayuko Aoki .. Helens is a part of the Pacific Ring of Fire which includes over 160 active volcanoes. as Cloud Strife. Mount St. Takahiro Sakurai .. Helens' 1980 eruption. as Aerith Gainsborough. These were destroyed in St. Maaya Sakamoto .. The largest of the dacite domes formed the previous summit; another formed Goat Rocks dome on the northern flank. as Yuffie Kisaragi. Helens includes layers of basalt and andesite through which several domes of dacite lava have erupted. Yumi Kakazu .. Mount St. as Squall Leonhart (Leon). Helens is a great cone of rubble consisting of lava rock interlayered with ash, pumice and other deposits. Hideo Ishikawa .. Like most other volcanoes in the Cascade Range, St. as Jiminy Cricket. However, the scale of it still pales in comparison to far larger debris avalanches that have occurred in the geological past elsewhere on Earth. Kaneta Kimotsuki .. The debris avalanche from the 1980 eruption was up to 0.7 cubic miles (2.3 km3) in volume, making it the largest in recorded history. as Maleficent. Helens for more detail). Toshiko Sawada .. The eruption caused a massive debris avalanche, reducing its summit from 9,677 feet (2,950 m) to 8,364 feet (2,550 m) in elevation and replacing it with a mile-wide (1.5 km-wide) horseshoe-shaped crater (see geology section or 1980 eruption of Mount St. as Ansem. Fifty-seven people were killed and 250 homes, 47 bridges, 15 miles (24 km) of railways and 185 miles (300 km) of highway were destroyed. Akio Otsuka .. That eruption was the most deadly and economically destructive volcanic eruption in the history of the United States. as Kairi. It is most famous for the catastrophic eruption on May 18, 1980. Risa Uchida .. This volcano is well known for its ash explosions and pyroclastic flows. as Riku. It was named for British diplomat Lord St Helens who was a friend of George Vancouver, an explorer who made a survey of the area in the late 18th century. Mamoru Miyano .. The mountain is part of the Cascade Range and was initially known as Louwala-Clough which means "smoking or fire mountain" in the language of the local native Americans, the Klickitats. as Goofy. It is located 96 miles (154 km) south of Seattle and 53 miles (85 km) northeast of Portland, Oregon. Yutaka Shimaka .. Helens is an active stratovolcano in Skamania County, Washington, in the Pacific Northwest region of the United States. as Donald Duck, Genie, Mushu, Beast, Sebastian. Mount St. Koichi Yamadera .. as Sora. Miyu Irino .. as Mickey Mouse. Wayne Allwine .. as Mushu. Mark Moseley .. as Beast. Robby Benson .. as Piglet. John Fiedler .. as Winnie the Pooh and Tigger. Jim Cummings .. as Captain Hook, Doorknob, Flotsam, Jetsam, and White Rabbit. Corey Burton .. as Peter Pan. Christopher Steele .. as Oogie Boogie. Ken Page .. Smee. as The Mayor, Barrel, and Mr. Jeff Bennett .. Finkelstein and Lock. as Dr. Jess Harnell .. as Sally. Rita Rudner .. as Jack Skellington. Chris Sarandon .. as Ursula. Pat Carroll .. as King Triton. Ken Mars .. as Sebastian. Kevin Michael Richardson .. as Flounder. Eli Linnetz .. as Ariel. Jodi Benson .. as Geppetto. Tony Pope .. as Pinocchio. Seth Adkins .. as Iago. Gilbert Gottfried .. as Jafar. Jonathan Freeman .. as Jasmine. Linda Larkin .. as Genie. Dan Castellaneta .. as Aladdin. Scott Weinger .. as Sora's mother and Shock. Kath Soucie .. as Terk. Audrey Wasilewski .. as Jane Porter. Naia Kelly .. as Clayton. Brian Blessed .. as Tarzan. Tony Goldwyn .. as Hades. James Woods .. as Philoctetes (Phil). Robert Costanzo .. as Hercules. Sean Astin .. as Alice and Wendy Darling. Kathryn Beaumont .. as Daisy Duck and Queen of Hearts. Tress MacNeille .. as Minnie Mouse. Russi Taylor .. as Wakka. Dee Bradley Baker .. as Tidus. Shaun Flemming .. as Selphie. Molly Keck .. as Sephiroth. James Lance Bass .. as Cloud Strife. Steve Burton .. as Aerith Gainsborough. Mandy Moore .. as Yuffie Kisaragi. Christy Carlson Romano .. as Squall Leonhart (Leon). David Boreanaz .. as Jiminy Cricket. Eddie Carroll .. as Maleficent. Susan Blakeslee .. as Ansem. Billy Zane .. as Kairi. Hayden Panettiere .. as Riku. David Gallagher .. as Goofy. Bill Farmer .. as Donald Duck. Tony Anselmo .. as Sora. Haley Joel Osment .. In the Final Mix release, an additional video, Another Side, Another Story: Deep Dive, is included if the player peforms other specific tasks. In the North American release, a bonus Kingdom Hearts II teaser titled Another Side, Another Story could be unlocked by peforming certain tasks. The optional boss Kurt Zisa was named after the winner of a publicity contest held by Squaresoft to promote the game. They were included in Final Mix along with another optional boss. While the Phantom and Coliseum bosses are present in the original Japanese version, the rest of the optional bosses were added later in the English version. Optional bosses in the game include Kurt Zisa, a Heartless; the Phantom, a Heartless; Ice Titan, from Hercules; Sephiroth, from Final Fantasy VII; and various Final Fantasy and Hercules characters in Coliseum matches. The homeland of Mickey, Donald and Goofy. Disney Castle (non-playable, not to be confused with Sleeping Beauty Castle). The World Terminus is located here, providing access to small areas of other worlds. The final battles with Ansem are fought here. Kingdom Hearts is near the center of this world. It is where many Heartless and evil beings reside. A large, dark world created from the assimilation of various worlds consumed in darkness. End of the World. This is also Maleficent's headquarters. This is the world that has been created for the Square characters as well as a sort of stand-in for the movie Beauty and the Beast as the Beast is a playable character there. Hollow Bastion. Several Final Fantasy and Disney characters reside here, including Aerith Gainsborough, Gepetto from Pinnochio, Yuffie Kisaragi, Squall Leonheart, Cid Highwind, The Fairy Godmother from Cinderella, and Merlin from The Sword in the Stone. A sort of "resting place" to come back to in between worlds, Traverse Town is where Sora first meets Donald and Goofy and truly starts his quest. Traverse Town. This world is home not only to Sora, Riku, and Kairi, but also Final Fantasy characters, Selphie Tilmitt, Tidus, and Wakka. This is where the Sora starts his journey, and although only accessible near the beginning and end of the game, the islands and the events in them are critical to the entire game's storyline. Destiny Islands. It is also one of the more important Disney-based worlds in the game, storyline-wise. Captain Hook, Peter Pan, Wendy, Smee and Tinkerbell call this world home, with Peter Pan able to join your party. The world's name is somewhat a misnomer because the action takes place on Captain Hook's ship and a minor bit in London; as such, the actual Neverland is not actually visited. Neverland, from Peter Pan. It features Jack Skellington, Sally, Lock, Shock, Barrel, Doctor Finklestein, Zero, the two-faced Mayor and Oogie Boogie, with Jack able to join your party. This world includes the town square, Oogie Boogie's Manor, Moonlit Hill and a graveyard. The movie's cast make their video game debut in the level. Halloween Town, from The Nightmare Before Christmas. This level has often been criticized by fans as a difficult level to play because the controls vary underwater. Ariel, King Triton, Ursula, Sebastian, Flounder, Flotsam and Jetsam appear in this world, with Ariel being the only female character in the game to join your party. This was a distinctive underwater level that consists of Ursula's cave, several grottos, and the city of Atlantica. Atlantica, from The Little Mermaid. Monstro is not a true world by Kingdom Hearts' definition, and thus does not contain a keyhole to be sealed. The infamous little wooden puppet Pinocchio and his maker Gepetto can be found here. This world brings the player through the bowels of a whale. Monstro, from Pinocchio. Aladdin, Abu, Jasmine, Jafar, Iago and Genie are introduced here, with Aladdin being a possible party member. This world includes Agrabah and the Cave of Wonders. Agrabah, from Aladdin. A variety of mini games open up as you proceed through the game. This world is unlike the others; there are no Heartless here and it takes place in the pages of a book. 100 Acre Wood, from Winnie the Pooh. This is a slightly longer world than the first, and includes Tarzan, as the first character that can be added to your party, Jane, Clayton and Several gorillas. Deep Jungle, from Tarzan. Phil), Cerberus, and Cloud Strife. This includes Hades, Hercules, Philoctetes (a.k.a. Olympus Coliseum, from Hercules. It features the Cheshire Cat, the Doorknob, Alice, The Queen of Hearts, and several cards as well as the White Rabbit. This is the first level that can be closed to the Heartless. This is a surreal level in which the player is shrunk down to a miniscule size. Wonderland, from Alice in Wonderland. |