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Произведения автора580880
Gettysburg Address
High Quality Content by WIKIPEDIA articles! The Gettysburg Address is a speech by U.S. President Abraham Lincoln and is one of the most well-known speeches in United States history. It was delivered by Lincoln during the American Civil War, on the afternoon of Thursday, November 19, 1863, at the dedication of the Soldiers` National Cemetery in Gettysburg, Pennsylvania, four and a half months after the Union armies defeated those of the Confederacy at the Battle of Gettysburg.
Getting It: The Psychology of est
High Quality Content by WIKIPEDIA articles! Getting It: The Psychology of est is a non-fiction book by American psychologist Sheridan Fenwick, first published in 1976, analyzing Werner Erhard`s Erhard Seminars Training or est. It is based on Fenwick`s own experience of attending a four-day session of the est training, an intensive 60-hour personal development course in the self-help genre. Large groups of up to 250 people took the est training at one time.
German occupation of Luxembourg in World War I
High Quality Content by WIKIPEDIA articles! The German occupation of Luxembourg in World War I was the first of two military occupations of the Grand Duchy of Luxembourg by Germany in the twentieth century. From August 1914 until the end of World War I in November 1918, Luxembourg was under full occupation by the German Empire. The German government justified the occupation by citing the need to support their armies in neighbouring France, although many Luxembourgers, contemporary and present, have interpreted German actions otherwise.
Gerard (archbishop of York)
High Quality Content by WIKIPEDIA articles! Gerard (died 21 May 1108) was Archbishop of York between 1100 and 1108 and Lord Chancellor of England from 1085 until 1092. A Norman, he was a member of the cathedral clergy at Rouen before becoming a royal clerk under King William I of England and subsequently his son King William II Rufus. Gerard was appointed Lord Chancellor by William I, and he continued in that office under Rufus, who rewarded him with the Bishopric of Hereford in 1096. Gerard may have been with the king`s hunting party when William II was killed, as he is known to have witnessed the first charter issued by the new king, Henry I of England, within days of William`s death.
Georgetown University
High Quality Content by WIKIPEDIA articles! Georgetown University is a private, Jesuit, research university whose main campus is in the Georgetown neighborhood of Washington, D.C. Founded in 1789, it is the oldest Catholic university in the United States. Georgetown administers 180 academic programs in four undergraduate and three graduate and professional schools, and the programs in international affairs and law are particularly selective and well regarded. In addition to its main campus, renowned for the neo-Romanesque Healy Hall, Georgetown operates a law center on Capitol Hill, as well as auxiliary campuses in Italy, Turkey, and Qatar.
George VI
High Quality Content by WIKIPEDIA articles! George VI (Albert Frederick Arthur George; 14 December 1895 – 6 February 1952) was King of the United Kingdom and the Dominions of the British Commonwealth from 11 December 1936 until his death. He was the last Emperor of India, and the first Head of the Commonwealth.
George V
High Quality Content by WIKIPEDIA articles! George V (George Frederick Ernest Albert; 3 June 1865 – 20 January 1936) was King of the United Kingdom and the British Dominions, and Emperor of India, from 6 May 1910 through the First World War (1914–1918) until his death in 1936.
George IV of the United Kingdom
High Quality Content by WIKIPEDIA articles! George IV (George Augustus Frederick; 12 August 1762 – 26 June 1830) was the King of the United Kingdom of Great Britain and Ireland and also of Hanover from the death of his father, George III, on 29 January 1820 until his own death ten years later. From 1811 until his accession, he served as Prince Regent during his father`s relapse into mental illness.
Geology of the Zion and Kolob canyons area
High Quality Content by WIKIPEDIA articles! The geology of the Zion and Kolob canyons area includes nine known exposed formations, all visible in Zion National Park in the U.S. state of Utah. Together, these formations represent about 150 million years of mostly Mesozoic-aged sedimentation in that part of North America. Part of a super-sequence of rock units called the Grand Staircase, the formations exposed in the Zion and Kolob area were deposited in several different environments that range from the warm shallow seas of the Kaibab and Moenkopi formations, streams and lakes of the Chinle, Moenave, and Kayenta formations to the large deserts of the Navajo and Temple Cap formations and dry near shore environments of the Carmel Formation.
Geology of the Lassen volcanic area
High Quality Content by WIKIPEDIA articles! The geology of the Lassen volcanic area presents a record of sedimentation and volcanic activity in the area in and around Lassen Volcanic National Park in Northern California, U.S. The park is located in the southernmost part of the Cascade Mountain Range in the Pacific Northwest region of the United States. Pacific Oceanic tectonic plates have plunged below the North American Plate in this part of North America for hundreds of millions of years. Heat from these subducting plates have fed scores of volcanoes in California, Oregon, Washington and British Columbia over at least the past 30 million years (see Geology of the Pacific Northwest) and is also responsible for activities in the Lassen...
Geology of the Grand Canyon area
High Quality Content by WIKIPEDIA articles! The geology of the Grand Canyon area exposes one of the most complete and studied sequences of rock on Earth. The nearly 40 major sedimentary rock layers exposed in the Grand Canyon and in the Grand Canyon National Park area range in age from about 200 million to nearly 2 billion years old. Most were deposited in warm, shallow seas and near ancient, long-gone sea shores in western North America. Both marine and terrestrial sediments are represented, including fossilized sand dunes from an extinct desert. There are at least 14 known unconformities in the geologic record found in the Grand Canyon area.
Geology of the Death Valley area
High Quality Content by WIKIPEDIA articles! The exposed geology of the Death Valley area presents a diverse and complex set of at least 23 formations of sedimentary units, two major gaps in the geologic record called unconformities, and at least one distinct set of related formations geologists call groups. The oldest rocks in the area that now includes Death Valley National Park are extensively metamorphosed by intense heat and pressure and are at least 1700 million years old. These rocks were intruded by a mass of granite 1400 Ma (million years ago) and later uplifted and exposed to nearly 500 million years of erosion.
Geology of the Capitol Reef area
High Quality Content by WIKIPEDIA articles! The exposed geology of the Capitol Reef area presents a record of mostly Mesozoic-aged sedimentation in an area of North America in and around Capitol Reef National Park. Nearly 10,000 feet (3,000 m) of sedimentary strata are found in the Capitol Reef area, representing nearly 200 million years of geologic history of the south-central part of the U.S. state of Utah. These rocks range in age from Permian (as old as 270 million years old) to Cretaceous (as young as 80 million years old.) Rock layers in the area reveal ancient climates as varied as rivers and swamps (Chinle Formation), Sahara-like deserts (Navajo Sandstone), and shallow ocean (Mancos Shale).
Geology of the Bryce Canyon area
High Quality Content by WIKIPEDIA articles! The exposed geology of the Bryce Canyon area in Utah shows a record of deposition that covers the last part of the Cretaceous Period and the first half of the Cenozoic era in that part of North America. The ancient depositional environment of the region around what is now Bryce Canyon National Park varied from the warm shallow sea (called the Cretaceous Seaway) in which the Dakota Sandstone and the Tropic Shale were deposited to the cool streams and lakes that contributed sediment to the colorful Claron Formation that dominates the park`s amphitheaters.
Geography and ecology of the Everglades
High Quality Content by WIKIPEDIA articles! The geography and ecology of the Everglades involve the complex elements affecting the natural environment throughout the southern region of the U.S. state of Florida. Before drainage, the Everglades were an interwoven mesh of marshes and prairies covering 4,000 square miles (10,000 km2). The Everglades is simultaneously a vast watershed that has historically extended from Lake Okeechobee 100 miles (160 km) south to Florida Bay (around one-third of the southern Florida peninsula), and many interconnected ecosystems within a geographic boundary. It is such a unique meeting of water, land, and climate that the use of either singular or plural to refer to the Everglades is appropriate. When...
Geoffrey (archbishop of York)
High Quality Content by WIKIPEDIA articles! Geoffrey (sometimes Geoffrey Plantagenet,Geoffrey fitzPlantagenet, or Geoffrey fitzRoy;c. 1152 – 12 December 1212) was an illegitimate son of Henry II, King of England, who became Bishop-elect of Lincoln and Archbishop of York. The identity of his mother is uncertain, but she may have been named Ykenai. Geoffrey held a number of minor clerical offices before becoming Bishop of Lincoln in 1173, although he was not ordained a priest until 1189. In 1173–1174 he led a campaign in the north of England to help put down a rebellion by his legitimate half-brothers; this campaign led to the capture of the King of Scots. By 1182 Pope Lucius III had ordered that Geoffrey either resign Lincoln or be...
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