Portal:North America
The North America Portal
North America is a continent in the Northern and Western Hemispheres. North America is bordered to the north by the Arctic Ocean, to the east by the Atlantic Ocean, to the southeast by South America and the Caribbean Sea, and to the west and south by the Pacific Ocean. The region includes the Bahamas, Bermuda, Canada, the Caribbean, Central America, Clipperton Island, Greenland, Mexico, Saint Pierre and Miquelon, Turks and Caicos Islands, and the United States.
North America covers an area of about 24,709,000 square kilometers (9,540,000 square miles), representing approximately 16.5% of the Earth's land area and 4.8% of its total surface area. It is the third-largest continent by size after Asia and Africa, and the fourth-largest continent by population after Asia, Africa, and Europe. , North America's population was estimated as over 592 million people in 23 independent states, or about 7.5% of the world's population. In human geography, the terms "North America" and "North American" sometimes refer to just Canada, the United States, Mexico, and Greenland.
It is unknown with certainty how and when first human populations first reached North America. People were known to live in the Americas at least 20,000 years ago, but various evidence points to possibly earlier dates. The Paleo-Indian period in North America followed the Last Glacial Period, and lasted until about 10,000 years ago when the Archaic period began. The classic stage followed the Archaic period, and lasted from approximately the 6th to 13th centuries. Beginning in 1000 AD, the Norse were the first Europeans to begin exploring and ultimately colonizing areas of North America.
In 1492, the exploratory voyages of Christopher Columbus led to a transatlantic exchange, including migrations of European settlers during the Age of Discovery and the early modern period. Present-day cultural and ethnic patterns reflect interactions between European colonists, indigenous peoples, enslaved Africans, immigrants from Europe, Asia, and descendants of these respective groups. (Full article...)
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The Panic of 1907, also known as the 1907 Bankers' Panic or Knickerbocker Crisis, was a financial crisis that took place in the United States over a three-week period starting in mid-October, when the New York Stock Exchange suddenly fell almost 50% from its peak the previous year. The panic occurred during a time of economic recession, and there were numerous runs affecting banks and trust companies. The 1907 panic eventually spread throughout the nation when many state and local banks and businesses entered bankruptcy. The primary causes of the run included a retraction of market liquidity by a number of New York City banks and a loss of confidence among depositors, exacerbated by unregulated side bets at bucket shops.
The panic was triggered by the failed attempt in October 1907 to corner the market on stock of the United Copper Company. When the bid failed, banks that had lent money to the cornering scheme suffered runs that later spread to affiliated banks and trusts, leading a week later to the downfall of the Knickerbocker Trust Company, New York City's third-largest trust. The collapse of the Knickerbocker spread fear throughout the city's trusts as regional banks withdrew reserves from New York City banks. The panic then extended across the nation as vast numbers of people withdrew deposits from their regional banks, causing the 8th-largest decline in U.S. stock market history. (Full article...) Featured picture -
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Joseph Georges Gonzague Vézina (/ˈvɛzɪnə/; French: [ʒɔʁʒ vezina]; January 21, 1887 – March 27, 1926) was a Canadian professional ice hockey goaltender who played seven seasons in the National Hockey Association (NHA) and nine in the National Hockey League (NHL), all with the Montreal Canadiens. After being signed by the Canadiens in 1910, Vézina played in 327 consecutive regular season games and a further 39 playoff games, before leaving early during a game in 1925 due to illness. Vézina was diagnosed with tuberculosis, and died on March 27, 1926.
The only goaltender to play for the Canadiens between 1910 and 1925, Vézina helped the team win the Stanley Cup in 1916 and 1924, while reaching the Stanley Cup Finals three more times. Nicknamed the "Chicoutimi Cucumber" for his calm composure while in goal, Vézina allowed the fewest goals in the league seven times in his career: four times in the NHA and three times in the NHL. In 1918, Vézina became the first NHL goaltender to both record a shutout and earn an assist on a goal. At the start of the 1926–27 NHL season, the Canadiens donated the Vezina Trophy to the NHL as an award to the goaltender who allowed the fewest goals during the season. Since 1981, the award has been given to the most outstanding goaltender as determined by a vote of NHL general managers. In Vézina's hometown of Chicoutimi, the sports arena is named the Centre Georges-Vézina in his honour. When the Hockey Hall of Fame opened in 1945, Vézina was one of the original nine inductees, and in 2017 the NHL included him on their list of the 100 greatest players in league history. (Full article...)
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Mount Garibaldi (known as Nch'ḵay̓, IPA: [n̩.ʧʼqɛˀj̰], to the indigenous Squamish people) is a dormant stratovolcano in the Garibaldi Ranges of the Pacific Ranges in southwestern British Columbia, Canada. It has a maximum elevation of 2,678 metres (8,786 feet) and rises above the surrounding landscape on the east side of the Cheakamus River in New Westminster Land District. In addition to the main peak, Mount Garibaldi has two named sub-peaks. Atwell Peak is a sharp, conical peak slightly higher than the more rounded peak of Dalton Dome. Both were volcanically active at different times throughout Mount Garibaldi's eruptive history. The northern and eastern flanks of Mount Garibaldi are obscured by the Garibaldi Névé, a large snowfield containing several radiating glaciers. Flowing from the steep western face of Mount Garibaldi is the Cheekye River, a tributary of the Cheakamus River. Opal Cone on the southeastern flank is a small volcanic cone from which a lengthy lava flow descends. The western face is a landslide feature that formed in a series of collapses between 12,800 and 11,500 years ago. These collapses resulted in the formation of a large debris flow deposit that fans out into the Squamish Valley.
Mount Garibaldi has been the focus of intermittent volcanic activity over the last 260,000 years. This activity produced mostly dacite, the main type of volcanic rock forming Mount Garibaldi. Volcanism between 260,000 and 220,000 years ago constructed an ancestral cone that was subsequently destroyed. Another growth period began with the eruption of Atwell Peak about 13,000 years ago when Mount Garibaldi was surrounded by an ice sheet during the last glacial period. The latest period of volcanic activity took place about 10,000 years ago with eruptions from Dalton Dome and Opal Cone after the ice sheet retreated. Although the mountain is not known to have been volcanically active since that time, it could erupt again, which could endanger the nearby populace. If this were to happen, relief efforts could be organized by teams such as the Interagency Volcanic Event Notification Plan who are prepared to notify people threatened by volcanic eruptions in Canada. (Full article...)Did you know...
- ...that in 1869 the Spanish colonial authorities banned Baseball in Cuba because Cubans began to prefer baseball to viewing bullfights, the Spaniards' national sport?
- ...that Castillo de los Tres Reyes Magos del Morro (pictured), a fortress which guards the entrance to Havana bay in Havana, was named after the biblical Magi?
- ...that the French West Indies refers to the two French overseas departments of Guadeloupe and Martinique, and also includes the Guadeloupean dependencies of French St. Martin, Saint-Barthélemy, Les Saintes, Marie-Galante and La Désirade?
- ... that Bésame Mucho, a song written in 1940 by Consuelo Velazquez, is according to some sources the most interpreted and performed song of the 20th century?
- ... that secondary students can take Yup'ik studies in the Yupiit School District, which is located in the Bethel Census Area of Alaska?
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