Expensive Private Schools

Expensive Private Schools August 8, 2012 Do you think your child attends one of the most expensive private schools? Maybe they go to Harvard-Westlake School in Los Angeles or The Dalton School in New York. Or Deerfield Academy in Massachusetts. Its expensive to go to Deerfield! But what are the most expensive private schools in the world, you ask? Wonder no longer. The Huffington Post has an article out listing what they believe to be the ten most expensive private schools (high schools) on the globe. So which school do you think is the single most expensive? They better have some fancy cheese! Tuition at Institut Le Rosey (a rather older photo of the institute is featured) in Switzerland is not cheap! Itll cost you a hundred grand. In Rolle, Switzerland, Institut Le Rosey has an annual tuition of $99,566. You read that right. Annual. But, dont worry it includes room and board. Also in Switzerland (in Villars-sur-Ollon), College Alpin International Beau Soleil might get some beautiful sun but tuition is at $93,158 a year. That, too, includes room and board. Middlesex School in Concord, Massachusetts charges $50,320 a year, while Eton College in Windsor, England charges $50,213 a year. Lawrence Academy in Groton, Massachusetts charges $52,640 annually, while The Hotchkiss School in Lakeville, Connecticut charges $45,350 a year. The United World College of South East Asia in Singapore charges an annual tuition of $48,403. The Lawrenceville School in New Jersey charges $51,025 a year. Appleby College in Ontario, Canada is more expensive than Applebees. They charge $53,911 each year. And in the Bronx, New York, Riverdale School charges $42,000 a year. These figures are all according to The Huffington Post. We actually know of some schools that should be on this list schools that charge more than $42,000 a year. But you get the idea about expensive private schools. What do you think about these tuition costs? What do you think about spending almost $100,000 a year to go to school? Let us know your thoughts on the matter by posting below! Check out this article on Private School Rejects.

Facts About Mount St. Helens

Mount St. Helens is an active volcano located in the United States Pacific Northwest region. It is positioned about 96 miles (154 km) south of Seattle, Washington and 50 miles (80 km) northeast of Portland, Oregon. Mount St. Helens is found within the Cascade Mountain Range, which runs from northern California through Washington and Oregon into British Columbia, Canada. This range, as part of the curved stretch of extreme seismic activity known as the Pacific ​Ring of Fire, features many active volcanoes. In fact, the Cascadia Subduction Zone itself was formed by plate convergence along the North American coast. Today, the land surrounding Mount St. Helens is rebounding and most of it has been preserved as a part of the Mount St. Helens National Volcanic Monument. Geography of Mount St. Helens Compared to other volcanoes in the Cascades, Mount St. Helens is fairly young geologically speaking because it was formed only 40,000 years ago. Its top cone, which was destroyed in the 1980 eruption, began developing only 2,200 years ago. Due to its rapid growth, many scientists consider Mount St. Helens the most active volcano in the Cascades within the last 10,000 years. There are three main river systems in the vicinity of Mount St. Helens. These include the Toutle, Kalama, and Lewis Rivers. These were all significantly impacted by the eruption of 1980. The nearest town to Mount St. Helens is Cougar, Washington, which is around 11 miles (18 km) away. Gifford Pinchot National Forest comprises the rest of the immediate area. Other nearby but much farther cities such as Castle Rock, Longview, and Kelso, Washington were affected by the 1980 eruption because they are low-lying and near the regions rivers. 1980 Eruption On May 18 of 1980, the eruption of Mount St. Helens removed 1,300 feet of mountaintop and ravaged surrounding forests and cabins in a destructive avalanche. In addition to avalanches, the area endured the aftermath of earthquakes, pyroclastic flow, and ash for several years. Activity on the mountain began on March 20, 1980, when a magnitude 4.2 earthquake struck. Steam soon began to vent from the mountain and by April, a bulge appeared on the north side of Mount St. Helens. This bulge would cause a historically catastrophic avalanche. When another strong earthquake struck on May 18, the entire north face of the volcano tumbled into a debris avalanche that is believed to have been the largest in history. Reawakening This massive landslide caused Mount St. Helens to erupt in a violent explosion on the same day. The volcanos pyroclastic flow—a swift river of hot ash, lava, rock, and gas—leveled the surrounding area almost instantly. The blast zone of this deadly eruption spanned 230 square miles (500 sq km): rocks were hurled, waterways flooded, the air poisoned, and more. 57 people were killed. Ash alone had disastrous effects. During its first eruption, the plume of ash from Mount St. Helens rose as high as 16 miles (27 km) and moved east until it spread upwards of 35 miles. Volcanic ash is highly toxic and thousands of humans were exposed. Mount St. Helens continued erupting ash from 1989 to 1991. In addition to the spread of ash, heat from eruptions and force from numerous avalanches caused the mountains ice and snow to melt, which led to the formation of fatal volcanic mudflows called lahars. These lahars poured into neighboring rivers—the Toutle and Cowlitz, in particular—and caused widespread flooding. This devastation blanketed miles and miles of land. Material from Mount St. Helens was found 17 miles (27 km) south  in the Columbia River along the Oregon-Washington border. Five smaller explosions, accompanied by countless eruptive episodes, would follow this reawakening in the next six years. Activity on the mountain continued until 1986 and a giant lava dome formed in the newly-developed crater at the volcanos summit. Recovery The land around this volcano has almost fully rebounded since 1980. The area that was once completely scorched and barren is now a thriving forest. Just five years after the initial eruption, surviving plants sprouted through the thick layer of ash and debris and flourished. Since 1995, biodiversity within the previously damaged area has even increased—there are many trees and shrubs growing successfully and animals that inhabited the land pre-eruption have returned and resettled. Most Recent Activity Mount St. Helens devastating 1980 modern eruption was not its most recent activity. The volcano has continued to make its presence known. Since its historic explosion, Mount St. Helens experienced a period of much smaller eruptions lasting from 2004 to 2008. During this four-year period, the mountain was again very active and eruptive. Fortunately, none of the explosions were particularly severe and the land has not suffered too greatly because of them. Most of these smaller eruptions only added on to the growing lava dome at Mount St. Helens summit crater. In 2005, however, Mount St. Helens erupted a 36,000 foot (11,000 m) plume of ash and steam. A minor earthquake accompanied this event. Ash and steam have been visible on the mountain several times in more recent years. Sources Diggles, Michael.  Mount St. Helens–From the 1980 Eruption to 2000. U.S. Geological Survey, 1 Mar. 2005.Dzurisin, Daniel. â€Å"Mount St. Helens Retrospective: Lessons Learned Since 1980 and Remaining Challenges.†Ã‚  Frontiers in Earth Science, Volcanology, 10 Sept. 2018.â€Å"Mount St. Helens Area.†Ã‚  Gifford Pinchot National Forest, United States Department of Agriculture Forest Service.â€Å"Mount St. Helens Information Resource Center and Visitor Guide.†Ã‚  Welcome to Mount St. Helens, 2019 Mount St. Helens Discovery LLC, 2019.Volcanic Hazards Program. â€Å"2004-2008 Renewed Volcanic Activity.†Ã‚  Cascades Volcano Observatory Mount St. Helens, United States Geological Survey | U.S. Department of the Interior.

Camping For Their Lives By Scott Bransford - 980 Words

In â€Å"Camping for Their Lives† by Scott Bransford it states that there has been a development of tent cities throughout the American West and how the lives of the people who dwell in them are affected. Bransford uses many different techniques to make his point to the readers. The author also uses valid evidence to support all of his claims. This reading overall is credible and informative to its readers. The author begins by discussing the lives of two individuals that reside in the tent homes of Fresno, California. He goes on to state that many other people also live similar lives in these tent houses not only in Fresno California but all across America. Bransford continues to inform the readers of how this is not a recent trend but an ongoing one that continues to affect people and gives some perspectives from people who are involved either by living in one of these tent cities or by working with the homeless. This topic is important because homelessness affects the lives of many people throughout society. Today with the cost of living being high and minimum wage being low, homelessness is not as uncommon as most people would like it to be. Tent cities are areas where people have gathered to build informal habitats. One of the main points the author begins with is that in any other country these kinds of areas would be called slums but in the United States they are called â€Å"tent cities â€Å"which is a form of doublespeak. These areas are without the luxuries of electricity,Show MoreRelatedCamping For Their Lives By Scott Bransford883 Words   |  4 PagesUpon reading the title â€Å"Camping for Their Lives† by Scott Bransford, A lot of images come to mind as they do for many people. Whether it be family outings, military experience or just plain adventure. Scott Bransford takes a good long look at camping in a different way. The author’s topic is about the tent cities and their homeless populations. He argues the struggles that they have with little or no help from the government and highlights a location in Central Valley California. The authorRead MoreCamping For Their Lives By Scott Bransford881 Words   |  4 Pages Upon reading the title to the reading â€Å"Camping for Their Lives† by Scott Bransford, A lot of images come to mind as they do for many people. Whether it be family outings, military experience or just plain adventure. Scott Bransford takes a good long look at camping in a different way. The author’s topic is about tent cities and their homeless populations. He argues the struggles that they have with little or no help from the government and highlights a location in Central Valley California.

Dido and Aeneas free essay sample

Musical Example of this texture: Music example 8 Act 1 figure 11 onwards Cupid only throws the dart Dialogue/Antiphonal e. G. Double Chorus In our deep vaulted cell This playschool :more than one choir) movement features effective antiphonal (the alternation of different groups of instruments) exchanges. The Echo Dance of the Furies which follows this uses dialogue to great musical effect. Musical Example of this texture: Music example 9 Act 2 figures 25-7 Many of the chorus and instrumental movements often combine both homophobic and polyphonic textures. DYNAMICS: In the Baroque period dynamics were either loud or soft.This is called terraced dynamics. Second section of overture and end of Act 1 Echo Dance of the Furies figure 27 STRUCTURE: The work is made up of six dramatic scenes in three acts and lasts for Just one hour. The main musical structures used in this work include: Overture this follows the conventions of the French and Italian Overtures of two sections (slow with dotted rhythms and fast Straight rhythms) and this second section repeated). We will write a custom essay sample on Dido and Aeneas or any similar topic specifically for you Do Not WasteYour Time HIRE WRITER Only 13.90 / page Compare this structure to the overture from the oratorio Messiah by Handel. It is essentially the same. Recitative- Nards are of importance in telling the story through recitative.Musical interest is kept to the minimum. Aria- Melody is all important to convey the affection or mood of the music Chorus- Homophobic four part vocal sections in the main with some Imitation. The chorus takes the part of the courtiers, witches or sailors depending on the scene! Dance movement- Sometimes the music for the chorus is repeated as a dance and sometimes there is a separate specific dance piece, such as the sailors dance and dance of the witches and sailors. (Act 3 figures 41 and 45 respectively). It is thought that several of the dances to this opera have been lost. The Key points The context The Text nationally submitted by Katherine to stressing. Co. UK; edited by Beth Worth. Past Questions Discuss the musical features of English court masque, opera or theatre music of the late seventeenth century, referring to the music of at least two composers. Discuss the expressive use of harmony and tonality in Dido and Names, supporting your answer with reference to two extended passages from the text. Give detailed account of the vocal writing in at least two works for the English stage composed in the late seventeenth and early eighteenth centuries.