How Many Miles Is 190 Km
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How Many Miles Is 190 Km
Haiti, a country in the Caribbean Sea that includes the western third of the island of Hispaniola and smaller islands such as Gonawe, Tortu (Tortuga), Grande Caye, and Vache. The capital is Port-au-Prince.
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Haiti, whose population was made up almost entirely of African slaves, gained independence from France in 1804, making it the second country in the United States after the United States seceded from governing. However, over the centuries, economic, political and social conditions as well as various natural disasters have left Haiti suffering from chronic poverty and other serious problems.
Haiti borders the Dominican Republic to the east, which encompasses all of Hispaniola, the Caribbean to the south and west, and the Atlantic Ocean to the north. Cuba is located about 50 miles (80 km) west of the northern peninsula of Haiti across the Windward Passage connecting the Atlantic to the Caribbean. Jamaica is about 120 miles (190 km) west of the southern peninsula, across the Jamaica Channel, and about 70 miles (110 km) north of Great Inagua Island (of the Bahamas). Haiti claims control of Navassa (Navasey) Island, an uninhabited American territory about 35 miles (55 km) west of the Jamaica Channel.
The generally rugged topography of central and western Hispaniola is reflected in Haiti’s name, which derives from the original Arawak place-name Ayiti (“high mountain”). About two-thirds of the entire area is above 1,600 feet (490 m) in elevation. Haiti’s irregular coastline leads to long, peninsular stretches in the south and short stretches in the north, separated by the triangular-shaped Gulf of Gonave. In the bay is Gonâve Island, which has an area of about 290 square miles (750 sq km). Haiti’s shores are often rocky, strewn with reefs, and indented by many excellent harbors. The surrounding beaches are famous for their coral reefs. The less restricted plains are the best agricultural land and the most populated areas. The rivers are numerous but short, and often not navigable.
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The spine of the island of Hispaniola consists of four large mountains that stretch from west to east. The northernmost, called the Cordillera Septentrional in the Dominican Republic, occurs on the island of Tortu, just off the north coast of Haiti. Tortu Island has an area of approximately 70 square miles (180 square kilometers). In the 17th century it was a stronghold of privateers and pirates from many countries.
A second major range, the Massif du Nord (“Northern Massif”) in Haiti, is one of the chains known as the Cordillera Central in the Dominican Republic. Its average elevation is about 4,000 feet (1,200 m). The Citadel (Citadelle Laferrière), a fortress built by Haitian ruler Henri Christophe in the early 19th century, stands on a peak overlooking Cap-Haitian city and the narrow coast.
An inland basin known as the Central Plateau of Haiti and the San Juan Valley of the Dominican Republic occupies an area of about 150 square miles (390 sq km) in the center of the country. The average elevation of the plateau is about 1,000 feet (300 m), and access to it by winding roads is difficult. It is bounded on the west and south by two small mountains – Chos Mountain and Noires Mountain respectively. The Artibonite River – the longest island, about 175 miles (280 km) long – rises in the Cordillera Central in the western Dominican Republic and follows a southwesterly course to the border with Haiti. Its rivers flow east and south through the Haitian Central Plateau to a point near the Dominican border, where they join the larger river as it meanders west. Artibonite covers the Noires Mountains as it flows into the Gulf of Gonave. In eastern Haiti the river was captured in the mid-20th century as Lake Péligre; A hydroelectric plant began operating at Pelligre in 1971, but its power output was unreliable during the dry season. Flowing only through the Delta of Artibonite to the Bay of Gonave, some of its water is used to irrigate the triangular Artibonite Plain.
A third major range, called the Matheux Mountains (Chaîne des Matheux) in west-central Haiti and the Trou d’Eau Mountains (Chaîne du Trou d’Eau) in the east, corresponds to the Sierra de Neiba in the Dominican Republic. The line runs north to the narrow Cul-de-Sac Plain, which immediately borders Port-au-Prince and includes the brackish lake Saumatre on the Dominican border.
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To the south of the Cul-de-Sac plain are four large ranges, the Massif de la Selle in Haiti and the Sierra de Baoruco in the Dominican Republic. It reaches 8,773 feet (2,674 m) at Mount Sele, the country’s highest point. The western part continues into the southern peninsula known as the Massif de la Hote (Massif du Sud), which rises to 7,700 feet (2,345 m) at Macaya Peak. Cage Plain is located on the coast southeast of the summit.
Haiti’s mountains are mostly limestone, although some volcanic formations can be seen, especially in the Massif du Nord. Karstic features such as limestone caves, caverns and underground rivers are found in many parts of the country. A long fault line crosses southeast and passes south of Port-au-Prince. Haiti will be affected during the earthquake; Earthquakes destroyed Cap-Haitian in 1842 and Port-au-Prince in 1751 and 1770. In January 2010, another major earthquake and its aftershocks caused extensive damage to Port-au-Prince. Buildings are scattered throughout the city and surrounding areas, including many buildings as well as major buildings such as the National Palace, the city’s cathedral and the hospital. Estimates of the dead have reached 200,000, and millions of people have been injured. More than 100,000 people have become homeless. In the western part of the city, near the epicenter, the town of Léogâne has been almost completely destroyed.
Hill soils are thin and lose fertility quickly when cultivated. The landscape consists of red clays and loams. The alluvial soils of the Terai and valleys are fertile but highly cultivated, due to the high population in these areas. Deforestation has caused much soil erosion, and as much as one-third of Haiti’s land may be degraded beyond recovery. GPS, GLONASS, Galileo, BeiDou-2, and Iridium constellations, the International Space Station, the Orbit Size Ratio Telescope of the Hubble Space, and the Geostationary Orbit (and its Grayyard Orbit), Van all along the Electric Belt and the world to measure.
Low Earth Orbit (LEO) is an Earth orbit with a period of 128 minutes or less (at least 11.25 orbits per day) and an eccentricity of less than 0.25.
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Most objects produced in outer space are in LEO, which has an altitude of no more than one-third the radius of Earth.
The term LEO region is also used for the space region below an altitude of 2,000 km (1,200 mi) (about one-third the radius of Earth).
Objects in orbits passing through this region, whether they have extra apogee or sub-orbital, are carefully tracked because they have dangerous collisions for many LEO satellites.
All of the office’s stations are in LEO as of today. From 1968 to 1972, the Apollo program’s lunar missions put humans beyond LEO. Since d the Apollo program, no manned space flights have gone beyond LEO.
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Define LEO in terms of altitude. The height of an object in an elliptical orbit can vary greatly from orbit to orbit. For orbits, the height above the ground can vary by about 30 km (19 mi) (especially for interstellar orbits) due to the Earth’s spherical shape and surface area imperfections. While the altitude-based definition is inherently imprecise, most of them fall within the hour range from an orbital period of 128 minutes because, according to Kepler’s third law, it corresponds to a semi-major axis of 8,413 km (5,228 mi). . For orbit, this translates to an altitude of 2,042 km (1,269 mi) above Earth’s maximum radius, which is included in some altitude limits in some LEO definitions.
Some elliptical orbits will pass through the LEO region near their maximum altitude (or perigee) but not in LEO orbit because their maximum altitude (or apogee) is greater than 2,000 km (1,200 mi). Sub-orbital objects can still reach the LEO region but are not in LEO orbit because they re-enter the atmosphere. The difference between LEO
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