1.
NASA
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President Dwight D. Eisenhower established NASA in 1958 with a distinctly civilian orientation encouraging peaceful applications in space science. The National Aeronautics and Space Act was passed on July 29,1958, disestablishing NASAs predecessor, the new agency became operational on October 1,1958. Since that time, most US space exploration efforts have led by NASA, including the Apollo Moon landing missions, the Skylab space station. Currently, NASA is supporting the International Space Station and is overseeing the development of the Orion Multi-Purpose Crew Vehicle, the agency is also responsible for the Launch Services Program which provides oversight of launch operations and countdown management for unmanned NASA launches. NASA shares data with various national and international such as from the Greenhouse Gases Observing Satellite. Since 2011, NASA has been criticized for low cost efficiency, from 1946, the National Advisory Committee for Aeronautics had been experimenting with rocket planes such as the supersonic Bell X-1. In the early 1950s, there was challenge to launch a satellite for the International Geophysical Year. An effort for this was the American Project Vanguard, after the Soviet launch of the worlds first artificial satellite on October 4,1957, the attention of the United States turned toward its own fledgling space efforts. This led to an agreement that a new federal agency based on NACA was needed to conduct all non-military activity in space. The Advanced Research Projects Agency was created in February 1958 to develop technology for military application. On July 29,1958, Eisenhower signed the National Aeronautics and Space Act, a NASA seal was approved by President Eisenhower in 1959. Elements of the Army Ballistic Missile Agency and the United States Naval Research Laboratory were incorporated into NASA, earlier research efforts within the US Air Force and many of ARPAs early space programs were also transferred to NASA. In December 1958, NASA gained control of the Jet Propulsion Laboratory, NASA has conducted many manned and unmanned spaceflight programs throughout its history. Some missions include both manned and unmanned aspects, such as the Galileo probe, which was deployed by astronauts in Earth orbit before being sent unmanned to Jupiter, the experimental rocket-powered aircraft programs started by NACA were extended by NASA as support for manned spaceflight. This was followed by a space capsule program, and in turn by a two-man capsule program. This goal was met in 1969 by the Apollo program, however, reduction of the perceived threat and changing political priorities almost immediately caused the termination of most of these plans. NASA turned its attention to an Apollo-derived temporary space laboratory, to date, NASA has launched a total of 166 manned space missions on rockets, and thirteen X-15 rocket flights above the USAF definition of spaceflight altitude,260,000 feet. The X-15 was an NACA experimental rocket-powered hypersonic research aircraft, developed in conjunction with the US Air Force, the design featured a slender fuselage with fairings along the side containing fuel and early computerized control systems
2.
Geographic coordinate system
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A geographic coordinate system is a coordinate system used in geography that enables every location on Earth to be specified by a set of numbers, letters or symbols. The coordinates are chosen such that one of the numbers represents a vertical position. A common choice of coordinates is latitude, longitude and elevation, to specify a location on a two-dimensional map requires a map projection. The invention of a coordinate system is generally credited to Eratosthenes of Cyrene. Ptolemy credited him with the adoption of longitude and latitude. Ptolemys 2nd-century Geography used the prime meridian but measured latitude from the equator instead. Mathematical cartography resumed in Europe following Maximus Planudes recovery of Ptolemys text a little before 1300, in 1884, the United States hosted the International Meridian Conference, attended by representatives from twenty-five nations. Twenty-two of them agreed to adopt the longitude of the Royal Observatory in Greenwich, the Dominican Republic voted against the motion, while France and Brazil abstained. France adopted Greenwich Mean Time in place of local determinations by the Paris Observatory in 1911, the latitude of a point on Earths surface is the angle between the equatorial plane and the straight line that passes through that point and through the center of the Earth. Lines joining points of the same latitude trace circles on the surface of Earth called parallels, as they are parallel to the equator, the north pole is 90° N, the south pole is 90° S. The 0° parallel of latitude is designated the equator, the plane of all geographic coordinate systems. The equator divides the globe into Northern and Southern Hemispheres, the longitude of a point on Earths surface is the angle east or west of a reference meridian to another meridian that passes through that point. All meridians are halves of great ellipses, which converge at the north and south poles, the prime meridian determines the proper Eastern and Western Hemispheres, although maps often divide these hemispheres further west in order to keep the Old World on a single side. The antipodal meridian of Greenwich is both 180°W and 180°E, the combination of these two components specifies the position of any location on the surface of Earth, without consideration of altitude or depth. The grid formed by lines of latitude and longitude is known as a graticule, the origin/zero point of this system is located in the Gulf of Guinea about 625 km south of Tema, Ghana. To completely specify a location of a feature on, in, or above Earth. Earth is not a sphere, but a shape approximating a biaxial ellipsoid. It is nearly spherical, but has an equatorial bulge making the radius at the equator about 0. 3% larger than the radius measured through the poles, the shorter axis approximately coincides with the axis of rotation
3.
Amateur Radio Lighthouse Society
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Founded in 2000 by Jim Weidner, K2JXW, the Amateur Radio Lighthouse Society is devoted to maritime communications, amateur radio, lighthouses, and lightships. Its members travel to lighthouses around the world where they operate amateur radio equipment at or near the light, collecting lighthouse QSLs is popular for some amateur radio operators. ARLHS is a organization with over 1665 members worldwide as of July 2009. A convention is held in October each year, in 2010 the gathering was in Biloxi, Mississippi. In earlier years it has held in Solomons, Maryland, St. Simons, Georgia, Port Huron, Michigan. The ARLHS has been featured in magazines, such as CQ. Jim Weidner is its founding President, and Jim Buffington, K5JIM, is Vice President, the club call sign is W7QF and the website is The ARLHS maintains a catalog of lighthouses called The World List of Lights. Its main feature is a short, and easily transmitted identification number for each lighthouse, the WLOL lists any lighthouse that is or was an Aid to Navigation and can reasonably accommodate an amateur radio operation. Lights that are no longer in existence, but were once an ATN, also show up on the list, with over 15,000 entries, the WLOL is one of the most complete lighthouse catalogs in existence. Amateur Radio Lighthouse Society Website ARLHS Convention web site Indias First ARLHS activation in Mahaballipuram, Chennai, India Aug 2008 Kadalur Lighthouse Centenary and ILLW operation Aug 2009
4.
Pacific Ocean
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The Pacific Ocean is the largest and deepest of the Earths oceanic divisions. It extends from the Arctic Ocean in the north to the Southern Ocean in the south and is bounded by Asia and Australia in the west, the Mariana Trench in the western North Pacific is the deepest point in the world, reaching a depth of 10,911 metres. Both the center of the Water Hemisphere and the Western Hemisphere are in the Pacific Ocean, the oceans current name was coined by Portuguese explorer Ferdinand Magellan during the Spanish circumnavigation of the world in 1521, as he encountered favourable winds on reaching the ocean. He called it Mar Pacífico, which in both Portuguese and Spanish means peaceful sea, important human migrations occurred in the Pacific in prehistoric times. Long-distance trade developed all along the coast from Mozambique to Japan, trade, and therefore knowledge, extended to the Indonesian islands but apparently not Australia. By at least 878 when there was a significant Islamic settlement in Canton much of trade was controlled by Arabs or Muslims. In 219 BC Xu Fu sailed out into the Pacific searching for the elixir of immortality, from 1404 to 1433 Zheng He led expeditions into the Indian Ocean. The east side of the ocean was discovered by Spanish explorer Vasco Núñez de Balboa in 1513 after his expedition crossed the Isthmus of Panama and he named it Mar del Sur because the ocean was to the south of the coast of the isthmus where he first observed the Pacific. Later, Portuguese explorer Ferdinand Magellan sailed the Pacific East to West on a Castilian expedition of world circumnavigation starting in 1519, Magellan called the ocean Pacífico because, after sailing through the stormy seas off Cape Horn, the expedition found calm waters. The ocean was often called the Sea of Magellan in his honor until the eighteenth century, sailing around and east of the Moluccas, between 1525 and 1527, Portuguese expeditions discovered the Caroline Islands, the Aru Islands, and Papua New Guinea. In 1542–43 the Portuguese also reached Japan, in 1564, five Spanish ships consisting of 379 explorers crossed the ocean from Mexico led by Miguel López de Legazpi and sailed to the Philippines and Mariana Islands. The Manila galleons operated for two and a half centuries linking Manila and Acapulco, in one of the longest trade routes in history, Spanish expeditions also discovered Tuvalu, the Marquesas, the Cook Islands, the Solomon Islands, and the Admiralty Islands in the South Pacific. In the 16th and 17th century Spain considered the Pacific Ocean a Mare clausum—a sea closed to other naval powers, as the only known entrance from the Atlantic the Strait of Magellan was at times patrolled by fleets sent to prevent entrance of non-Spanish ships. On the western end of the Pacific Ocean the Dutch threatened the Spanish Philippines, Spain also sent expeditions to the Pacific Northwest reaching Vancouver Island in southern Canada, and Alaska. The French explored and settled Polynesia, and the British made three voyages with James Cook to the South Pacific and Australia, Hawaii, and the North American Pacific Northwest, one of the earliest voyages of scientific exploration was organized by Spain in the Malaspina Expedition of 1789–1794. It sailed vast areas of the Pacific, from Cape Horn to Alaska, Guam and the Philippines, New Zealand, Australia, and the South Pacific. Growing imperialism during the 19th century resulted in the occupation of much of Oceania by other European powers, and later, Japan, in Oceania, France got a leading position as imperial power after making Tahiti and New Caledonia protectorates in 1842 and 1853 respectively. After navy visits to Easter Island in 1875 and 1887, Chilean navy officer Policarpo Toro managed to negotiate an incorporation of the island into Chile with native Rapanui in 1888, by occupying Easter Island, Chile joined the imperial nations
5.
Hawaii
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Hawaii is the 50th and most recent state to have joined the United States of America, having received statehood on August 21,1959. Hawaii is the only U. S. state located in Oceania and it is the northernmost island group in Polynesia, occupying most of an archipelago in the central Pacific Ocean. Hawaii is the only U. S. state not located in the Americas, the state encompasses nearly the entire volcanic Hawaiian archipelago, which comprises hundreds of islands spread over 1,500 miles. At the southeastern end of the archipelago, the eight main islands are—in order from northwest to southeast, Niʻihau, Kauaʻi, Oʻahu, Molokaʻi, Lānaʻi, Kahoʻolawe, Maui, and the Island of Hawaiʻi. The last is the largest island in the group, it is called the Big Island or Hawaiʻi Island to avoid confusion with the state or archipelago. The archipelago is physiographically and ethnologically part of the Polynesian subregion of Oceania, Hawaii has over a million permanent residents, along with many visitors and U. S. military personnel. Its capital is Honolulu on the island of Oʻahu, Hawaii is the 8th-smallest and the 11th-least populous, but the 13th-most densely populated of the fifty U. S. states. It is the state with an Asian plurality. The states coastline is about 750 miles long, the fourth longest in the U. S. after the coastlines of Alaska, Florida, the state of Hawaii derives its name from the name of its largest island, Hawaiʻi. A common Hawaiian explanation of the name of Hawaiʻi is that was named for Hawaiʻiloa and he is said to have discovered the islands when they were first settled. The Hawaiian language word Hawaiʻi is very similar to Proto-Polynesian *Sawaiki, cognates of Hawaiʻi are found in other Polynesian languages, including Māori, Rarotongan and Samoan. According to linguists Pukui and Elbert, lsewhere in Polynesia, Hawaiʻi or a cognate is the name of the underworld or of the home, but in Hawaii. A somewhat divisive political issue arose in 1978 when the Constitution of the State of Hawaii added Hawaiian as an official state language. The title of the constitution is The Constitution of the State of Hawaii. Article XV, Section 1 of the Constitution uses The State of Hawaii, diacritics were not used because the document, drafted in 1949, predates the use of the okina and the kahakō in modern Hawaiian orthography. The exact spelling of the name in the Hawaiian language is Hawaiʻi. In the Hawaii Admission Act that granted Hawaiian statehood, the government recognized Hawaii as the official state name. Official government publications, department and office titles, and the Seal of Hawaii use the spelling with no symbols for glottal stops or vowel length
6.
Cook Islands
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The Cook Islands is a self-governing island country in the South Pacific Ocean in free association with New Zealand. It comprises 15 islands whose total area is 240 square kilometres. The Cook Islands Exclusive Economic Zone, however, covers 1,800,000 square kilometres of ocean, the Cook Islands defence and foreign affairs are the responsibility of New Zealand, but they are exercised in consultation with the Cook Islands. In recent times, the Cook Islands have adopted an independent foreign policy. Although Cook Islanders are citizens of New Zealand, they have the status of Cook Islands nationals, the Cook Islands main population centres are on the island of Rarotonga, where there is an international airport. There is a population of Cook Islanders in New Zealand. In the 2006 census,58,008 self-identified as being of ethnic Cook Islands Māori descent, the Cook Islands are in the South Pacific Ocean, northeast of New Zealand, between French Polynesia and American Samoa. There are 15 major islands spread over 2,200,000 km2 of ocean, the islands were formed by volcanic activity, the northern group is older and consists of six atolls, which are sunken volcanoes topped by coral growth. The climate is moderate to tropical, palmerston Island sometimes grouped with the Northern Group. Manuae Winslow Reef The Cook Islands were first settled in the 6th century by Polynesian people who migrated from Tahiti, in 1813 John Williams, a missionary on the Endeavour made the first recorded sighting of Rarotonga. The first recorded landing on Rarotonga by Europeans was in 1814 by the Cumberland, the islands saw no more Europeans until missionaries arrived from England in 1821. Christianity quickly took hold in the culture and many continue to be Christian believers today. The Cook Islands became a British protectorate in 1888, due largely to community fears that France might occupy the territory as it had Tahiti, on 6 September 1900, the leading islanders presented a petition asking that the islands should be annexed as British territory. These instruments did not include Aitutaki and it appears that, though the inhabitants regarded themselves as British subjects, the Crowns title was uncertain, and the island was formally annexed by Proclamation dated 9 October 1900. The islands were included within the boundaries of the Colony of New Zealand in 1901 by Order in Council under the Colonial Boundaries Act,1895 of the United Kingdom. The boundary change became effective on 11 June 1901 and the Cook Islands have had a relationship with New Zealand ever since. When the British Nationality and New Zealand Citizenship Act 1948 came into effect on 1 January 1949, the country remained a New Zealand dependent territory until 1965, when the New Zealand Government decided to offer self-governing status to its colony. In that year, Albert Henry of the Cook Islands Party was elected as the first Premier, Henry led the country until he was accused of vote-rigging
7.
Territories of the United States
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Territories of the United States are sub-national administrative divisions directly overseen by the United States federal government. These territories are classified by whether they are incorporated and whether they have a government through an Organic Act passed by the U. S. Congress. Currently, the United States has sixteen territories, five of which are inhabited, Puerto Rico, Guam, Northern Mariana Islands, the U. S. Virgin Islands. They are classified as unincorporated territories and they are organized, self-governing territories with locally elected governors and territorial legislatures. Each also elects a member to the U. S. House of Representatives. Eleven territories are small islands, atolls and reefs, spread across the Caribbean and Pacific, the status of some are disputed by Colombia, Haiti, Honduras, Jamaica, Nicaragua, and the Marshall Islands. The Palmyra Atoll is the territory currently incorporated. Historically, territories were created to govern newly acquired land while the borders of the United States were still evolving, other territories administered by the United States went on to become independent countries, such as the Philippines, Micronesia, Marshall Islands and Palau. Many organized incorporated territories of the United States existed from 1789 to 1959, currently, the United States has sixteen territories, five of which are permanently inhabited, Puerto Rico, Guam, Northern Mariana Islands, United States Virgin Islands and American Samoa. The 11 uninhabited territories administered by the Interior Department are Palmyra Atoll, Baker Island, Howland Island, Jarvis Island, Johnston Atoll, Kingman Reef, while claimed by the US, Navassa Island, Wake Island, Serranilla Bank and Bajo Nuevo Bank are disputed. Territories have always been a part of the United States, by Act of Congress, the term United States, when used in a geographical sense, means the continental United States, Alaska, Hawaii, Puerto Rico, Guam, and the Virgin Islands of the United States. Since political union with the Northern Mariana Islands in 1986, they too are treated as a part of the U. S, an Executive Order in 2007 includes American Samoa as U. S. geographical extent duly reflected in U. S. State Department documents. Approximately 4 million islanders are U. S. citizens, about 32,000 U. S. non-citizen nationals live in American Samoa, under current law among the territories, only persons born in American Samoa and Swains Island are non-citizen U. S. nationals. American Samoans are under the protection of the U. S. with freedom of U. S. travel without visas. The five inhabited U. S. territories have local voting rights and protections under U. S. courts, pay some U. S. taxes, depending on the congress, they may also vote on the floor in the House Committee of the Whole. S. Every four years, the Democratic and Republican political parties nominate their candidates at conventions which include delegates from the five major territories. The citizens there, however, do not vote in the election for U. S. President. S. Incorporated territories are considered a part of the United States
8.
United States Fish and Wildlife Service
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The United States Fish and Wildlife Service is an agency of the federal government within the U. S. Department of the Interior dedicated to the management of fish, wildlife, and natural habitats. The mission of the agency is working with others to conserve, protect, and enhance fish, wildlife, plants and their habitats for the continuing benefit of the American people. The leader of the FWS is the director of the U. S. Fish and Wildlife Service Daniel M. Ashe, of Maryland, bavin National Fish and Wildlife Forensic Laboratory Landscape Conservation Cooperatives The vast majority of fish and wildlife habitat is on non-federal lands. The FWS employs approximately 9,000 people and is organized into an administrative office, eight regional offices. Spencer Fullerton Baird was appointed its first commissioner, in 1903, the Fish Commission was reorganized as the United States Bureau of Fisheries. In 1885–1886, the Division of Economic Ornithology and Mammalogy was established within the United States Department of Agriculture, in 1896 it became the Division of Biological Survey. Its early work focused on the effect of birds in controlling pests and mapping the geographical distribution of plants. Clinton Hart Merriam headed the Bureau for 25 years and became a figure for improving the scientific understanding of birds. Under Darlings guidance, the Bureau began a legacy of protecting vital natural habitat throughout the country. The USFWS was finally created in 1940, when the Bureaus of Fisheries, however, these exceptions often only apply to Native Americans that are registered with the federal government and are enrolled with a federally recognized tribe. Therefore, many people that wish to practice their religion continue to face persecution. This has become a source of conflict between many tribes and the US Fish and Wildlife Service. In the late 1990s and early 2000s, the USFWS began to incorporate the research of scientists into conservation decisions. Additionally, other natural resource agencies within the United States government, such as the USDA, have taken steps to be inclusive of tribes, native people. This has marked a transition to a relationship of more cooperation rather than the tension between tribes and government agencies seen historically, today, these agencies work closely with tribal governments to ensure the best conservation decisions are made and that tribes retain their sovereignty
9.
United States Department of the Interior
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The United States Department of the Interior is the United States federal executive department of the U. S. About 75% of federal land is managed by the department. The Department is administered by the United States Secretary of the Interior, the current Secretary is Ryan Zinke. The Inspector General position is vacant, with Mary Kendall serving as acting Inspector General. Despite its name, the Department of the Interior has a different role from that of the ministries of other nations. In the United States, national security and immigration functions are performed by the Department of Homeland Security primarily, the Department of the Interior has often been humorously called The Department of Everything Else because of its broad range of responsibilities. A department for domestic concern was first considered by the 1st United States Congress in 1789, the idea of a separate domestic department continued to percolate for a half-century and was supported by Presidents from James Madison to James Polk. The 1846–48 Mexican–American War gave the new steam as the responsibilities of federal government grew. Polks Secretary of the Treasury, Robert J. Walker, became a champion of creating the new department. In 1849, Walker stated in his report that several federal offices were placed in departments with which they had little to do. Walker argued that these and other bureaus should be together in a new Department of the Interior. A bill authorizing its creation of the Department passed the House of Representatives on February 15,1849, the Department was established on March 3,1849, the eve of President Zachary Taylors inauguration, when the Senate voted 31 to 25 to create the Department. Its passage was delayed by Democrats in Congress who were reluctant to create more patronage posts for the incoming Whig administration to fill, the first Secretary of the Interior was Thomas Ewing. Many of the concerns the Department originally dealt with were gradually transferred to other Departments. Other agencies became separate Departments, such as the Bureau of Agriculture, however, land and natural resource management, American Indian affairs, wildlife conservation, and territorial affairs remain the responsibilities of the Department of the Interior. As of mid-2004, the Department managed 507 million acres of surface land, energy projects on federally managed lands and offshore areas supply about 28% of the nations energy production. Within the Interior Department, the Bureau of Indian Affairs handles some federal relations with Native Americans, the current acting Assistant Secretary for Indian Affairs is Lawrence S. Roberts, an enrolled member of the Oneida Tribe in Wisconsin. Several cases have sought accounting of such funds from the departments of Interior, in addition, some Native American nations have sued the government over water-rights issues and their treaties with the US
10.
National Wildlife Refuge
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National Wildlife Refuge System is a designation for certain protected areas of the United States managed by the United States Fish and Wildlife Service. The National Wildlife Refuge System is the system of lands and waters set aside to conserve Americas fish, wildlife. National Wildlife Refuges manage a range of habitat types, including wetlands, prairies, coastal and marine areas. Among these hundreds of national refuges are home to some 700 species of birds,220 species of mammals,250 reptile and amphibian species and more than 1000 species of fish. Endangered species are a priority of National Wildlife Refuges in that nearly 60 refuges have been established with the purpose of conserving 280 threatened or endangered species. National Wildlife Refuges are also places where visitors can participate in a variety of outdoor recreational activities. The National Wildlife Refuge System welcomes nearly 50 million visitors each year, hunters visit more than 350 hunting programs on refuges and on about 36,000 Waterfowl Production Areas. Opportunities for fresh or saltwater fishing are available at more than 340 refuges, there is at least one wildlife refuge in each of the fifty states. The agency has created Comprehensive Conservation Plans for each refuge, developed through consultation with private and these began a review process by stakeholders beginning in 2013. The CCCPs must be consistent with the Fish and Wildlife Service goals for conservation, the CCPs outline conservation goals for each refuge for fifteen years into the future, with the intent that they will be revised every fifteen years thereafter. Additionally, NEPA requires FWS planners and refuge staff to engage the public in planning process to assist them with identifying the most appropriate alternative. Completed CCPs are available to the public and can be found on the FWS website, equally important is an intimate understanding of the social and economic drivers that impact and are impacted by management decisions and can facilitate or impede implementation success. Consideration of these contributes to the success of the Service’s mission to protect wildlife. The Refuge System works collaboratively internally and externally to leverage resources, according to the Services 2013 Banking on Nature Report, visitors to refuges positively impact the local economies. Prevention and control of fires is also a very active part of refuge management. Completion of controlled burns to reduce fuel loading, and participation in the wildland fire suppression efforts, are vital for management of refuge lands. A considerable infrastructure of physical structures is also essential to management of refuge lands. As of September 30,2015 there were 13,030 roads, bridges and trails,5,284 buildings,8,007 water management structures, the overall facility infrastructure is valued at nearly $30 billion
11.
Lagoon
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A lagoon is a shallow body of water separated from a larger body of water by barrier islands or reefs. Lagoons are commonly divided into coastal lagoons and atoll lagoons and they have also been identified as occurring on mixed-sand and gravel coastlines. There is an overlap between bodies of water classified as coastal lagoons and bodies of water classified as estuaries, lagoons are common coastal features around many parts of the world. Lagoons can also be man-made and used for treatment, as is the case for e. g. aerated lagoons. Lagoons are shallow, often elongated bodies of water separated from a body of water by a shallow or exposed shoal, coral reef. Some authorities include fresh water bodies in the definition of lagoon, the distinction between lagoon and estuary also varies between authorities. Richard A. Davis Jr. restricts lagoon to bodies of water with little or no fresh water inflow, and little or no tidal flow, Davis does state that the terms lagoon and estuary are often loosely applied, even in scientific literature. Timothy M. Kusky characterizes lagoons as normally being elongated parallel to the coast, while estuaries are usually drowned river valleys, coastal lagoons are classified as inland bodies of water. Many lagoons do not include lagoon in their common names, in England, The Fleet at Chesil Beach has also been described as a lagoon. In Latin America, the term laguna in Spanish, which translates to. However, sometimes it is used to describe a full-sized lake, such as Laguna Catemaco in Mexico. The brackish water lagoon may be explicitly identified as a coastal lagoon. In Portuguese the same usage is found, lagoa may be a body of sea water. Lagoon is derived from the Italian laguna, which refers to the waters around Venice, Laguna is attested in English by at least 1612, and had been Anglicized to lagune by 1673. In 1697 William Dampier referred to a Lagune or Lake of Salt water on the coast of Mexico, captain James Cook described an island of Oval form with a Lagoon in the middle in 1769. Atoll lagoons form as coral reefs grow upwards while the islands that the reefs surround subside, unlike the lagoons that form shoreward of fringing reefs, atoll lagoons often contain some deep portions. Coastal lagoons form along gently sloping coasts where barrier islands or reefs can develop off-shore, coastal lagoons do not form along steep or rocky coasts, or if the range of tides is more than 4 metres. Due to the slope of the coast, coastal lagoons are shallow
12.
United States Minor Outlying Islands
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Among them, Palmyra Atoll is the only incorporated territory. As of 2017, none of the islands have any permanent residents, the only human population consists of temporarily stationed scientific and military personnel. The 2000 census counted 315 people on Johnston Atoll and 94 people on Wake Island, there has been no modern indigenous population, except at the 1940 census. In 1936 a colonization program began to settle Americans on Baker, Howland, and Jarvis, the islands are grouped together as a statistical convenience. They are not administered collectively, nor do they share a cultural or political history beyond being uninhabited islands under the sovereignty of the United States. They are collectively represented by the ISO 3166-1 alpha-2 code UM, the individual islands have ISO 3166-2 numerical codes, see ISO 3166-2, UM. The Internet country code top-level domain. um has historically been assigned to the islands, however, ISO introduced the term United States Minor Outlying Islands in 1986. From 1974 until 1986, five of the islands were grouped under the term United States Miscellaneous Pacific Islands, the code of Midway Atoll was MI, the code of Johnston Atoll was JT, and the code of Wake Island was WK. The Pacific islands are surrounded by large Exclusive Economic Zones, see also Organized incorporated territories, Unincorporated territories and List of territorial disputes in North America. The following is a list of airports with ICAO codes, PJON, Johnston Atoll Airport, Johnston Atoll PMDY, Henderson Field, Sand Island. Kingman Reef and Navassa Island have offshore anchorage only. S, Pacific Island Wildlife Refuges CIA World Factbook, United States Pacific Island Wildlife Refuges
13.
Day beacon
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A day beacon is an unlighted nautical sea mark. A signboard attached to a day beacon is called a day mark and are used to identify them, typically, day beacons mark channels whose key points are marked by lighted buoys. Day beacons may also mark smaller navigable routes in their entirety and they are the most common aid to nautical navigation in shallow water as they are relatively inexpensive to install and maintain. Navigation around day beacons is the same as all other navigational aids. For historical reasons, there are two systems for lateral day beacons, when proceeding from open water towards harbor, marks with cylindrical topmarks or square dayboards are kept to port in both regions, but colors and numbers are reversed. When lateral beacons are paired, vessels should pass between the pairing, however, beacons are also frequently placed individually. Generally, single lateral beacons are at the corner of a turn. Interior or exterior placement can be determined based upon the passing side dictated by beacon designation, however, a current chart should always be consulted for all but the shallowest-draft vessels, as channel conditions are rarely ideal. Cardinal day beacons are used to indicate the position of a hazard and this makes them meaningful regardless of the direction or position of the approaching vessel, in contrast to the lateral mark system
14.
Guano
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Guano is the accumulated excrement of seabirds, seals, or cave-dwelling bats. As a manure, guano is an effective fertilizer due to its exceptionally high content of nitrogen, phosphate and potassium. During the twentieth century, guano-producing birds became an important target of conservation programs, today, guano is increasingly sought after by organic farmers. Seabird guano consists of nitrogen-rich ammonium oxalate and urate, phosphates, as well as some earth salts, the word guano originates from the Andean indigenous language Quechua, which refers to any form of dung used as an agricultural fertilizer. Archaeological evidence suggests that Andean people have collected guano from small islands, spanish colonial documents suggest that the rulers of the Inca Empire assigned great value to guano, restricted access to it, and punished any disturbance of the birds with death. The Guanay cormorant has historically been the most abundant and important producer of guano, other important guano producing species off the coast of Peru are the Peruvian pelican and the Peruvian booby. At that time, massive deposits of guano existed on some islands, in this context the United States passed the Guano Islands Act in 1856, which gave U. S. citizens discovering a source of guano on an unclaimed island exclusive rights to the deposits. Nine of these islands are still officially U. S. territories, control over guano played a central role in the Chincha Islands War between Spain and a Peruvian-Chilean alliance. Indentured workers from China played an important role in guano harvest, the first group of 79 Chinese workers arrived in Peru in 1849, by the time that trade ended a quarter of a century later, over 100,000 of their fellow countrymen had been imported. There is no evidence that enslaved Pacific Islanders participated in guano mining. Between 1847 and 1873, there was a significant increase in Peruvian guano exports, after 1870, the use of Peruvian guano as a fertilizer was eclipsed by saltpeter in the form of caliche extraction from the interior of the Atacama Desert, not far from the guano areas. Since 1909, when the Peruvian government took over guano extraction for use by Peru farmers, South Africa independently developed its own guano industry based on sustained-yield production from marine birds during this period, as well. Both industries eventually collapsed due to pressure from overfishing, DNA testing has suggested that new potato varieties imported alongside Peruvian seabird guano in 1842 brought a virulent strain of potato blight that began the Irish Potato Famine. The ideal type of guano is found in dry climates. Post-depositional decomposition and ammonia volatilization of penguin guano also plays an important role in the evolution of ornithogenic sediments in the cold, Bat guano is usually mined in caves and this mining is associated with a corresponding loss of troglobytic biota and diminishing of biodiversity. Guano deposits support a variety of cave-adapted invertebrates that rely on bat feces as their sole source of nutrition. The greatest damage caused by mining to caves with extant guano deposits is to the bat colonies themselves, bats are highly vulnerable to regular disturbance to their roosts. Some species, such as Phyllonycteris aphylla, have low fat reserves, many species will drop pups when in panic, with subsequent death, leading to a steady reduction in population
15.
Desert island
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A desert island, deserted island or uninhabited island is an island that is not permanently populated by humans. Uninhabited islands are used in movies or stories about shipwrecked people. Some uninhabited islands are protected as reserves and some are privately owned. Devon Island in Canada is claimed to be the largest uninhabited island in the world, small coral atolls or islands usually have no source of fresh water, but at times a fresh water lens can be reached with a well. Uninhabited islands are also called deserted islands or desert islands. In the latter, the adjective desert connotes not desert climate conditions, the word desert has been formerly applied more widely to any wild, uninhabited region, including forest-land, and it is this archaic meaning that appears in the phrase desert island. Similarly, the deserted island does not imply that the island was previously inhabited. The term desert island is commonly used figuratively to refer to objects or behavior in conditions of social isolation. Behavior on an island is a common thought experiment, for example. Appat Island, Greenland Kermadec Islands in the South Pacific, part of New Zealand Astola Island, Baluchistan Devon Island,55,247 km2, many small islands off the coast of Greece A majority of islands in the Barra Isles archipelago. The most famous of abandoned islands is located at the southernmost point of the outer Hebrides. The protagonists in both are children living in seclusion on a deserted island, until they eventually come in contact with castaways from the outside world who are stranded on the island. The story of Theologus Autodidactus, however, extends beyond the island setting when the castaways take Kamil back to civilization with them. William Shakespeares 1610–11 play, The Tempest, uses the idea of being stranded on an island as a pretext for the action of the play. In the late 17th century, Philosophus Autodidactus inspired Robert Boyle, Ibn al-Nafis Theologus Autodidactus was also eventually translated into English in the early 20th century. The novel features Man Friday, Crusoes personal assistant and it is also likely that he was inspired by the Latin or English translations of Ibn Tufails Philosophus Autodidactus. Tom Neale was a New Zealander who voluntarily spent 16 years in three sessions in the 1950s and 1960s living alone on the island of Suwarrow in the northern Cook Islands group and his time there is documented in his autobiography, An Island To Oneself. Significant novels set on deserted islands include The Swiss Family Robinson, The Coral Island, The Mysterious Island, Lord of the Flies, The Cay, juana Maria, a Native American woman, was stranded for 18 years on San Nicolas Island off California in the 19th century
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Topographic isolation
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The topographic isolation of a summit is the minimum great-circle distance to a point of equal elevation, representing a radius of dominance in which the peak is the highest point. It can be calculated for small hills and islands as well as for major mountain peaks, the following sortable table lists the Earths 40 most topographically isolated summits. The nearest peak to Germanys highest mountain, the 2, 962-metre-high Zugspitze, the distance between the Zugspitze and this contour is 25.8 km, the Zugspitze is thus the highest peak for a radius of 25.8 km around. Its isolation is thus 25.8 km, because there are no higher mountains than Mount Everest, it has no definitive isolation. Many sources list its isolation as the circumference of the earth over the poles or – questionably, after Mount Everest the Aconcagua, highest mountain of the American continents, has the greatest isolation of all mountains. There is no land for 16,534 kilometres when its height is first exceeded by Tirich Mir in the Hindu Kush. Mont Blanc is the highest mountain of the Alps, the geographically nearest higher mountains are all in the Caucasus. The Kukurtlu, which rises near the Elbrus, is the peak for Mont Blanc. com Canadian Mountain Encyclopedia peakbagger. com peaklist. org peakware. com World Mountain Encyclopedia summitpost. org
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Reef
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A reef is a bar of rock, sand, coral or similar material, lying beneath the surface of water. Reefs may be up to 261 feet below the surface, artificial reefs such as shipwrecks are sometimes created to enhance physical complexity on generally featureless sand bottoms in order to attract a diverse assemblage of organisms, especially fish. There is a variety of reef types, including oyster reefs. These biotic reef types take on additional names depending upon how the reef lies in relation to the land, Reef types include fringing reef, barrier reefs, as well as atolls. A fringing reef is a reef that is attached to an island, a barrier reef forms a calcareous barrier around an island resulting in a lagoon between the shore and the reef. An atoll is a reef with no land present. The reef front is a high energy locale whereas the internal lagoon will be at an energy with fine grained sediments. One useful definition distinguishes reefs from mounds as follows, reefs are held up by a macroscopic skeletal framework. Coral reefs are an excellent example of this kind, corals and calcareous algae grow on top of one another and form a three-dimensional framework that is modified in various ways by other organisms and inorganic processes. By contrast, mounds lack a macroscopic skeletal framework, mounds are built by microorganisms or by organisms that dont grow a skeletal framework. A microbial mound might be built exclusively or primarily by cyanobacteria, excellent examples of biostromes formed by cyanobacteria occur in the Great Salt Lake of Utah, and in Shark Bay, Western Australia. Cyanobacteria do not have skeletons and individuals are microscopic, cyanobacteria encourage the precipitation or accumulation of calcium carbonate and can produce distinct sediment bodies in composition that have relief on the seafloor. Cyanobacterial mounds were most abundant before the evolution of shelly macroscopic organisms, bryozoans and crinoids, common contributors to marine sediments during the Mississippian, produced a very different kind of mound. Bryozoans are small and the skeletons of crinoids disintegrate, however, bryozoan and crinoid meadows can persist over time and produce compositionally distinct bodies of sediment with depositional relief. The Proterozoic Belt Supergroup contains evidence of microbial mat and dome structures similar to stromatolite reef complexes. Ancient reefs buried within stratigraphic sections are of considerable interest to geologists because they provide information about the location in Earths history. Corals, including some major extinct groups Rugosa and Tabulata, have been important reef builders through much of the Phanerozoic since the Ordovician Period. However, other groups, such as calcifying algae, especially members of the red algae Rhodophyta
18.
Southern Hemisphere
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The Southern Hemisphere is the half sphere of Earth which is south of the equator. It contains all or parts of five continents, four oceans and its surface is 80. 9% water, compared with 60. 7% water in the case of the Northern Hemisphere, and it contains 32. 7% of Earths land. Due to the tilt of Earths rotation relative to the Sun, September 22 or 23 is the vernal equinox and March 20 or 21 is the autumnal equinox. The South Pole is in the middle of the southern hemispherical region, Southern Hemisphere climates tend to be slightly milder than those at similar latitudes in the Northern Hemisphere, except in the Antarctic which is colder than the Arctic. This is because the Southern Hemisphere has significantly more ocean and much land, water heats up. In the Southern Hemisphere the sun passes from east to west through the north, sun-cast shadows turn anticlockwise throughout the day and sundials have the hours increasing in the anticlockwise direction. Cyclones and tropical storms spin clockwise in the Southern Hemisphere due to the Coriolis effect, the southern temperate zone, a subsection of the Southern Hemisphere, is nearly all oceanic. Forests in the Southern Hemisphere have special features which set apart from those in the Northern Hemisphere. Both Chile and Australia share, for example, unique species or Nothofagus. The eucalyptus is native to Australia but is now planted in Southern Africa and Latin America for pulp production and, increasingly. Approximately 800,000,000 humans live in the Southern Hemisphere and this is due to the fact that there is significantly less land in the Southern Hemisphere than in the Northern Hemisphere. Africa Antarctica Asia Australia South America Zealandia Media related to Southern Hemisphere at Wikimedia Commons
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American Samoa
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American Samoa is an unincorporated territory of the United States located in the South Pacific Ocean, southeast of Samoa. American Samoa consists of five islands and two coral atolls. The largest and most populous island is Tutuila, with the Manuʻa Islands, Rose Atoll, All islands except for Swains Island are part of the Samoan Islands, located west of the Cook Islands, north of Tonga, and some 300 miles south of Tokelau. To the west are the islands of the Wallis and Futuna group, the 2010 census showed a total population of 55,519 people. The total land area is 199 square kilometers, slightly more than Washington, American Samoa is the southernmost territory of the U. S. and one of two U. S. territories south of the Equator, along with the uninhabited Jarvis Island. Tuna products are the exports, and the main trading partner is the United States. American Samoa is noted for having the highest rate of enlistment of any U. S. state or territory. Most American Samoans are bilingual and can speak English and Samoan fluently, Samoan is the same language spoken in neighboring independent Samoa. Contact with Europeans began in the early 18th century, dutchman Jacob Roggeveen was the first known European to sight the Samoan Islands in 1722. This visit was followed by French explorer Louis-Antoine de Bougainville who named them the Navigator Islands in 1768, contact was limited before the 1830s, when English missionaries and traders began arriving. The site of battle is called Massacre Bay. Mission work in the Samoas had begun in late 1830 when John Williams of the London Missionary Society arrived from the Cook Islands, by that time, the Samoans had gained a reputation for being savage and warlike, as violent altercations had occurred between natives and European visitors. In March 1889, an Imperial German naval force entered a village on Samoa, three American warships then entered the Apia harbor and prepared to engage the three German warships found there. Before any shots were fired, a typhoon wrecked both the American and German ships, a compulsory armistice was then called because of the lack of any warships. Forerunners to the Tripartite Convention of 1899 were the Washington Conference of 1887, the Treaty of Berlin of 1889, the following year, the USA formally occupied its portion, a smaller group of eastern islands, one of which contains the noted harbor of Pago Pago. The Navy secured a Deed of Cession of Tutuila in 1900, the territory became known as the US Naval Station Tutuila. On July 17,1911, the US Naval Station Tutuila, in 1918 during the final stages of World War I, the flu pandemic had taken its toll, spreading rapidly from country to country. The result of Poyers quick actions earned him the Navy Cross from the US Navy, with this distinction, American Samoans regarded Poyer as their hero for what he had done to prevent the deadly disease
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Equator
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The Equator usually refers to an imaginary line on the Earths surface equidistant from the North Pole and South Pole, dividing the Earth into the Northern Hemisphere and Southern Hemisphere. The Equator is about 40,075 kilometres long, some 78. 7% lies across water and 21. 3% over land, other planets and astronomical bodies have equators similarly defined. Generally, an equator is the intersection of the surface of a sphere with the plane that is perpendicular to the spheres axis of rotation. The latitude of the Earths equator is by definition 0° of arc, the equator is the only line of latitude which is also a great circle — that is, one whose plane passes through the center of the globe. The plane of Earths equator when projected outwards to the celestial sphere defines the celestial equator, in the cycle of Earths seasons, the plane of the equator passes through the Sun twice per year, at the March and September equinoxes. To an observer on the Earth, the Sun appears to travel North or South over the equator at these times, light rays from the center of the Sun are perpendicular to the surface of the Earth at the point of solar noon on the Equator. Locations on the Equator experience the quickest sunrises and sunsets because the sun moves nearly perpendicular to the horizon for most of the year. The Earth bulges slightly at the Equator, the diameter of the Earth is 12,750 kilometres. Because the Earth spins to the east, spacecraft must also launch to the east to take advantage of this Earth-boost of speed, seasons result from the yearly revolution of the Earth around the Sun and the tilt of the Earths axis relative to the plane of revolution. During the year the northern and southern hemispheres are inclined toward or away from the sun according to Earths position in its orbit, the hemisphere inclined toward the sun receives more sunlight and is in summer, while the other hemisphere receives less sun and is in winter. At the equinoxes, the Earths axis is not tilted toward the sun, instead it is perpendicular to the sun meaning that the day is about 12 hours long, as is the night, across the whole of the Earth. Near the Equator there is distinction between summer, winter, autumn, or spring. The temperatures are usually high year-round—with the exception of high mountains in South America, the temperature at the Equator can plummet during rainstorms. In many tropical regions people identify two seasons, the wet season and the dry season, but many places close to the Equator are on the oceans or rainy throughout the year, the seasons can vary depending on elevation and proximity to an ocean. The Equator lies mostly on the three largest oceans, the Pacific Ocean, the Atlantic Ocean, and the Indian Ocean. The highest point on the Equator is at the elevation of 4,690 metres, at 0°0′0″N 77°59′31″W and this is slightly above the snow line, and is the only place on the Equator where snow lies on the ground. At the Equator the snow line is around 1,000 metres lower than on Mount Everest, the Equator traverses the land of 11 countries, it also passes through two island nations, though without making a landfall in either. Starting at the Prime Meridian and heading eastwards, the Equator passes through, Despite its name, however, its island of Annobón is 155 km south of the Equator, and the rest of the country lies to the north
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Rain
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Rain is liquid water in the form of droplets that have condensed from atmospheric water vapor and then precipitated—that is, become heavy enough to fall under gravity. Rain is a component of the water cycle and is responsible for depositing most of the fresh water on the Earth. It provides suitable conditions for many types of ecosystems, as well as water for power plants. The major cause of production is moisture moving along three-dimensional zones of temperature and moisture contrasts known as weather fronts. If enough moisture and upward motion is present, precipitation falls from convective clouds such as cumulonimbus which can organize into narrow rainbands. On the leeward side of mountains, desert climates can exist due to the dry air caused by downslope flow which causes heating and drying of the air mass, the movement of the monsoon trough, or intertropical convergence zone, brings rainy seasons to savannah climes. The urban heat island effect leads to increased rainfall, both in amounts and intensity, downwind of cities, global warming is also causing changes in the precipitation pattern globally, including wetter conditions across eastern North America and drier conditions in the tropics. The globally averaged annual precipitation over land is 715 mm, climate classification systems such as the Köppen climate classification system use average annual rainfall to help differentiate between differing climate regimes. Rainfall is measured using rain gauges, rainfall amounts can be estimated by weather radar. Rain is also known or suspected on other planets, where it may be composed of methane, neon, sulfuric acid, or even iron rather than water. Air contains water vapor, and the amount of water in a mass of dry air. The amount of moisture in air is commonly reported as relative humidity. How much water vapor a parcel of air can contain before it becomes saturated, warmer air can contain more water vapor than cooler air before becoming saturated. Therefore, one way to saturate a parcel of air is to cool it, the dew point is the temperature to which a parcel must be cooled in order to become saturated. There are four mechanisms for cooling the air to its dew point, adiabatic cooling, conductive cooling, radiational cooling. Adiabatic cooling occurs when air rises and expands, the air can rise due to convection, large-scale atmospheric motions, or a physical barrier such as a mountain. Conductive cooling occurs when the air comes into contact with a surface, usually by being blown from one surface to another. Radiational cooling occurs due to the emission of infrared radiation, either by the air or by the surface underneath, evaporative cooling occurs when moisture is added to the air through evaporation, which forces the air temperature to cool to its wet-bulb temperature, or until it reaches saturation
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Tussock (grass)
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Tussock grasses or bunch grasses are found as native plants in natural ecosystems, as forage in pastures, and as ornamental grasses in gardens. As perennial plants usually, they more than one season. Many species have long roots that may reach 2 meters or more into the soil, which can aid slope stabilization, erosion control, also, their roots can reach moisture more deeply than other grasses and annual plants during seasonal or climatic droughts. The plants provide habitat and food for insects, birds, small animals and larger herbivores, the leaves supply material, such as for basket weaving, for indigenous peoples and contemporary artists. In western North American wildfires, bunch grasses tend to smolder and not ignite into flames, flavescens Festuca novaezelandiae Poa caespitosa P. colensoi P. http, //www. landcareresearch. co. nz/resources/identification/plants/grass-key
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Vine
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A vine in the narrowest sense is the grapevine, but more generally it can refer to any plant with a growth habit of trailing or scandent stems, lianas or runners. The word also can refer to such stems or runners themselves, in the United Kingdom, the term vine applies almost exclusively to the grapevine. The term climber is used for all climbing plants, certain plants always grow as vines, while a few grow as vines only part of the time. For instance, poison ivy and bittersweet can grow as low shrubs when support is not available, a vine displays a growth form based on long stems. This has been a successful growth form for plants such as kudzu and Japanese honeysuckle. There are some tropical vines that develop skototropism, and grow away from the light, growth away from light allows the vine to reach a tree trunk, which it can then climb to brighter regions. The vine growth form may also enable plants to large areas quickly. This is the case with periwinkle and ground ivy and it is also an adaptation to life in areas where small patches of fertile soil are adjacent to exposed areas with more sunlight but little or no soil. A vine can root in the soil but have most of its leaves in the brighter, exposed area, the evolution of a climbing habit has been implicated as a key innovation associated with the evolutionary success and diversification of a number of taxonomic groups of plants. It has evolved independently in several plant families, using many different climbing methods such as and it directs its stem into a crevice in the bark of fibrous barked trees where the stem adopts a flattened profile and grows up the tree underneath the host trees outer bark. The fetterbush then sends out branches that emerge near the top of the tree and these may be divided into woody vines or lianas, such as wisteria, kiwifruit, and common ivy, and herbaceous vines, such as morning glory. One odd group of vining plants is the fern genus Lygodium, the stem does not climb, but rather the fronds do. The fronds unroll from the tip, and theoretically never stop growing, they can form thickets as they unroll over other plants, rockfaces, gardeners can use the tendency of climbing plants to grow quickly. If a plant display is wanted quickly, a climber can achieve this, climbers can be trained over walls, pergolas, fences, etc. Climbers can be grown over other plants to provide additional attraction, artificial support can also be provided. Some climbers climb by themselves, others need work, such as tying them in, vines widely differ in size, form and evolutionary origin. Darwin classified climbing groups based on their climbing method and he classified five classes of vines including twining plants, leaf climbers, tendril bearers, root climbers and hook climbers. Vines are unique in that they have multiple origins and a wide range of phenotypic plasticity
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Habitat
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A habitat is an ecological or environmental area that is inhabited by a particular species of animal, plant, or other type of organism. The term typically refers to the zone in which the organism lives and it is the natural environment in which an organism lives, or the physical environment that surrounds a species population. Every organism has certain habitat needs for the conditions in which it will thrive, habitat types include polar, temperate, subtropical and tropical. The terrestrial vegetation type may be forest, steppe, grassland, the word habitat has been in use since about 1755 and derives from the Latin third-person singular present indicative of habitāre, to inhabit, from habēre, to have or to hold. Habitat can be defined as the environment of an organism. It is similar in meaning to a biotope, an area of environmental conditions associated with a particular community of plants. Generally speaking, animal communities are reliant on specific types of plant communities, some plants and animals are generalists, and their habitat requirements are met in a wide range of locations. The small white butterfly for example is found on all the continents of the world apart from Antarctica and its larvae feed on a wide range of Brassicas and various other plant species, and it thrives in any open location with diverse plant associations. Disturbance is important in the creation of biodiverse habitats, in the absence of disturbance, a climax vegetation cover develops that prevents the establishment of other species. Lightning strikes and toppled trees in tropical forests allow species richness to be maintained as pioneering species move in to fill the gaps created. Similarly coastal habitats can become dominated by kelp until the seabed is disturbed by a storm, another cause of disturbance is when an area may be overwhelmed by an invasive introduced species which is not kept under control by natural enemies in its new habitat. Terrestrial habitat types include forests, grasslands, wetlands and deserts, within these broad biomes are more specific habitats with varying climate types, temperature regimes, soils, altitudes and vegetation types. Many of these habitats grade into each other and each one has its own communities of plants. A habitat may suit a particular species well, but its presence or absence at any particular location depends to some extent on chance, on its dispersal abilities, freshwater habitats include rivers, streams, lakes, ponds, marshes and bogs. Although some organisms are found across most of these habitats, the majority have more specific requirements, similarly, aquatic plants can be floating, semi-submerged, submerged or grow in permanently or temporarily saturated soils besides bodies of water. Marine habitats include brackish water, estuaries, bays, the sea, the intertidal zone. Further variations include rock pools, sand banks, mudflats, brackish lagoons, sandy and pebbly beaches, the benthic zone or seabed provides a home for both static organisms, anchored to the substrate, and for a large range of organisms crawling on or burrowing into the surface. A desert is not the kind of habitat that favours the presence of amphibians, with their requirement for water to keep their skins moist, nevertheless, some frogs live in deserts, creating moist habitats underground and hibernating while conditions are adverse
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Kingman Reef
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It is the northernmost of the Northern Line Islands and lies 36 nautical miles northwest of the next closest island, and 930 nautical miles south of Honolulu. The reef encloses a lagoon up to 270 feet deep in its western part, the total area within the outer rim of the reef is 29 sq mi. There are two strips of dry land composed of coral rubble and giant clamshells on the eastern rim with areas of 2 and 1 acre having a coastline of 2 miles. The highest point on the reef is less than 5 feet above sea level and it has no natural resources and supports no economic activity. Kingman Reef has the status of a territory of the United States, administered from Washington. The atoll is closed to the public, for statistical purposes, Kingman Reef is grouped as part of the United States Minor Outlying Islands. In January 2009, Kingman Reef was designated a national monument. The Island also has a flag, the pre-20th century names Danger Reef, Caldew Reef, Maria Shoal and Crane Shoal refer to this atoll, which by then was entirely submerged at high tide. Thomas Hale Streets described its state in the 1870s, when it had, hardly, as yet, assumed the distinctive features of an island. It is entirely under water at high tide, and but a few coral heads project here and there above the surface at low water, in the course of time, however, it will undoubtedly be added to the. Kingman Reef was discovered by the American Captain Edmund Fanning of the ship Betsey on June 14,1798, Captain W. E. Kingman described it on November 29,1853. Kingman Reef was claimed in 1860 by the United States Guano Company and this claim was made under by the Guano Islands Act of 1856 although there is no evidence that guano existed or was ever mined on Kingman Reef. On December 29,1934, the US Navy assumed jurisdiction over Kingman Reef, the lagoon was used in 1937 and 1938 as a halfway station between Hawaii and American Samoa by Pan American Airways flying boats. Pan Am wanted to expand flights into the Pacific and include Australia, in 1935 it was decided that the lagoon at Kingman Reef was suitable for overnight stops en route from the U. S. to New Zealand via Samoa. Kingman Reef became the stopover to and from Pago Pago, American Samoa, a supply ship, the North Wind, was stationed at Kingman Reef to provide fuel, lodging, and meals. The S42B Pan American Clipper II, piloted by Captain Edwin Musick, several successful flights followed, but the flight on January 11,1938 ended in tragedy. Shortly after the early morning take off from Pago Pago, bound for New Zealand, the right outboard engine had developed an oil leak and the plane burst into flames while dumping fuel, there were no survivors. As a result of the tragedy, Pan Am ended flights to New Zealand via Kingman Reef, a new route was established in July 1940 by way of Canton Island and New Caledonia
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Midway Atoll
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Midway Atoll is a 2. 4-square-mile atoll in the North Pacific Ocean at 28°12′N 177°21′W. As its name suggests, Midway is roughly equidistant between North America and Asia, Midway Atoll is an unorganized, unincorporated territory of the United States. Midway continues to be the island in the Hawaiian archipelago that is not part of the state of Hawaii. Unlike the other Hawaiian islands, Midway observes Samoa Time, which is one hour behind the time in the state of Hawaii, for statistical purposes, Midway is grouped as one of the United States Minor Outlying Islands. The Midway Atoll National Wildlife Refuge, encompassing 590,991.50 acres of land and water in the area, is administered by the United States Fish. The refuge and most of its area are part of the larger Papahānaumokuākea Marine National Monument. Until 1993, the atoll was the home of the Naval Air Facility Midway, the Battle of Midway, which was fought between June 4 and 6,1942, was one of the most important battles of the Pacific campaign of World War II. The United States Navy defeated a Japanese battle group marking a point in the war in the Pacific Theater. USAAF aircraft based at the original Henderson Field on Eastern Island joined the attack against the Japanese fleet, approximately 40 to 60 people live on the atoll, which includes staff of the US Fish and Wildlife Service and contract workers. At present, visitation to the atoll is only for business reasons as the tourism program has been suspended due to budget cutbacks. In 2012, the last year that the program was in operation,332 people made the trip to Midway. Tours focused on both the ecology of Midway as well as its military history. The economy is derived solely from governmental sources and tourist fees, nearly all supplies must be brought to the island by ship or plane, though a hydroponic greenhouse and garden supply some fresh fruits and vegetables. As its name suggests, Midway is roughly equidistant between North America and Asia, and lies almost halfway around the world longitudinally from Greenwich and it is near the northwestern end of the Hawaiian archipelago, about one-third of the way from Honolulu, Hawaii, to Tokyo, Japan. Midway Atoll is less than 140 nautical miles east of the International Date Line, about 2,800 nautical miles west of San Francisco, and 2,200 nautical miles east of Tokyo. Midway Atoll is part of a chain of islands, atolls. It consists of a barrier reef and several sand islets. The two significant pieces of land, Sand Island and Eastern Island, provide a habitat for millions of seabirds
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Palmyra Atoll
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Palmyra Atoll is one of the Northern Line Islands, located almost due south of the Hawaiian Islands, roughly one-third of the way between Hawaii and American Samoa. The nearest continent is almost 5,400 kilometres to the northeast, the atoll is 4.6 sq mi, and it is located in the equatorial Northern Pacific Ocean. Its 9 mi of coastline has one known as West Lagoon. It is an unoccupied equatorial Northern Pacific atoll administered as an incorporated territory by the United States federal government. The atoll consists of a reef, two shallow lagoons, and some 50 sand and reef-rock islets and bars covered with vegetation—mostly Coconut palms, Scaevola. The islets of the atoll are mostly connected, sand Island and the two Home Islets in the west and Barren Island in the east are not. The largest island is Cooper Island in the north, followed by Kaula Island in the south, average annual rainfall is approximately 175 in per year. Daytime temperatures average 85 °F year round, Palmyra is an incorporated territory of the United States, meaning that it is subject to all provisions of the U. S. Constitution and is permanently under American sovereignty, however, since Palmyra is also an unorganized territory, there is no Act of Congress specifying how Palmyra should be governed. Palmyra has no permanent residents, however, in 2004 accommodations were built to support a number of temporary inhabitants. The only relevant federal law simply gives the President the authority to administer Palmyra as directed, the issue of the governing of Palmyra is generally a moot point, since there is no permanent population remaining there, nor any reason to think that there will be in the future. Palmyra is the only unorganized incorporated territory of the United States, Cooper Island and ten other land parcels in this atoll are owned by The Nature Conservancy, Inc. which manages them as a nature reserve. The southwesternmost islets, including Home, are owned by descendants of former Palmyra owner Henry Ernest Cooper, the rest of Palmyra is federal land and waters under the jurisdiction of the U. S. Fish and Wildlife Service. For all other purposes, Palmyra is counted as one of the U. S, there is no current economic activity on Palmyra other than paid ecotourism visits and sport fishing by Nature Conservancy donors. Most of the roads and causeways there were built during World War II, All of these are now unserviceable and overgrown with bushes and grass, and most have washed-away gaps. There is a 2, 000-yard -long, unpaved, airstrip on Cooper Island that was built for the Palmyra Island Naval Air Station before, a construction program in 2004 erected several two-person bungalows and showers for the temporary residents. Fresh water is collected from the roof of a building in this area. The communal buildings of the area on the western coast of Cooper Island consist of about half a dozen buildings next to the only sea dock
28.
United Kingdom of Great Britain and Ireland
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The United Kingdom of Great Britain and Ireland was established as a sovereign state on 1 January 1801 by the Acts of Union 1800, which merged the kingdoms of Great Britain and Ireland. The growing desire for an Irish Republic led to the Irish War of Independence, Northern Ireland remained part of the United Kingdom, and the state was consequently renamed the United Kingdom of Great Britain and Northern Ireland. Britain financed the European coalition that defeated France in 1815 in the Napoleonic Wars, the British Empire thereby became the foremost world power for the next century. The Crimean War with Russia and the Boer wars were relatively small operations in a largely peaceful century, rapid industrialisation that began in the decades prior to the states formation continued up until the mid-19th century. A devastating famine, exacerbated by government inaction in the century, led to demographic collapse in much of Ireland. It was an era of economic modernization and growth of industry, trade and finance. Outward migration was heavy to the colonies and to the United States. Britain also built up a large British Empire in Africa and Asia, India, by far the most important possession, saw a short-lived revolt in 1857. In foreign policy Britain favoured free trade, which enabled its financiers and merchants to operate successfully in many otherwise independent countries, as in South America. Britain formed no permanent military alliances until the early 20th century, when it began to cooperate with Japan, France and Russia, and moved closer to the United States. A brief period of limited independence for Ireland came to an end following the Irish Rebellion of 1798, the British governments fear of an independent Ireland siding against them with the French resulted in the decision to unite the two countries. This was brought about by legislation in the parliaments of both kingdoms and came into effect on 1 January 1801, however, King George III was bitterly opposed to any such Emancipation and succeeded in defeating his governments attempts to introduce it. When the Treaty of Amiens ended the war, Britain agreed to return most of the territories it had seized, in May 1803, war was declared again. In 1806, Napoleon issued the series of Berlin Decrees, which brought into effect the Continental System and this policy aimed to eliminate the threat from the British by closing French-controlled territory to foreign trade. Frances population and agricultural capacity far outstripped that of the British Isles, Napoleon expected that cutting Britain off from the European mainland would end its economic hegemony. The Spanish uprising in 1808 at last permitted Britain to gain a foothold on the Continent, after Napoleons surrender and exile to the island of Elba, peace appeared to have returned. The Allies united and the armies of Wellington and Blucher defeated Napoleon once, simultaneous with the Napoleonic Wars, trade disputes, arming hostile Indians and British impressment of American sailors led to the War of 1812 with the United States. The war was little noticed in Britain, which could devote few resources to the conflict until the fall of Napoleon in 1814, American frigates inflicted a series of defeats on the Royal Navy, which was short on manpower due to the conflict in Europe
29.
United States Exploring Expedition
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The United States Exploring Expedition was an exploring and surveying expedition of the Pacific Ocean and surrounding lands conducted by the United States from 1838 to 1842. The original appointed commanding officer was Commodore Thomas ap Catesby Jones, funding for the original expedition was requested by President John Quincy Adams in 1828, however, Congress would not implement funding until eight years later. In May 1836, the oceanic exploration voyage was finally authorized by Congress, the expedition is sometimes called the U. S. Ex. Ex. for short, or the Wilkes Expedition in honor of its next appointed commanding officer, the expedition was of major importance to the growth of science in the United States, in particular the then-young field of oceanography. During the event, armed conflict between Pacific islanders and the expedition was common and dozens of natives were killed in action and it was to promote commerce and to offer protection to the heavy investment in the whaling and seal hunting industries, chiefly in the Pacific Ocean. Congress also agreed that a ship or ships should be used. At the time, the ships owned by the government capable of such a circumnavigation were those of the navy. So, in fact, Congress had decided that an expedition be authorized. The veteran US Sloop-of-war Peacock was decommissioned and broken down in 1827 to be rebuilt as USS Peacock, intended as an exploration ship. There were to be many unforeseen impediments and it was not until May 18,1836, that an act was passed, which authorized funding, and approved by President Andrew Jackson, Adams political rival. Even with the burden of finance lifted, there were two years of alteration of formation and command before six oddly assorted ships moved down from Norfolk to Hampton Roads on August 9,1838. On August 17, they were joined by the tenders Sea Gull and Flying-Fish, due to light breezes, the expedition did not discharge their pilots until 09,00 August 19, when they passed Cape Henry Light. By 11,00, the fleet was standing to open seas. Originally, the expedition was organized under Commodore Jones, however, several more senior officers had either resigned from or indicated their unwillingness to accept command of the expedition. Command was finally vested in Lieutenant Wilkes, the three duties laid down were daunting to officers trained only in fighting ships. As well, a scientific corps was to be included as an additional command responsibility. There were few officers in the American navy at that time with any surveying experience, the United States Coast Survey, where most of the surveyors were employed and learned their trade, was a civilian organization. Wilkes, who had trained himself in surveying work, cut the excessively large number of scientists down to nine
30.
Guano Islands Act
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The Guano Islands Act is a United States federal law passed by the U. S. Congress that enables citizens of the United States to take possession of unclaimed islands containing guano deposits. The islands can be located anywhere, so long as they are not occupied and it also empowers the President of the United States to use the military to protect such interests and establishes the criminal jurisdiction of the United States in these territories. The Act continues to be part of the law of the United States, the most recent Guano Islands Act claim was made to Navassa Island, however, the claim was discarded because a court ruled the island was already under American jurisdiction. In the 1840s, guano came to be prized as a source of saltpeter for gunpowder as well as an agricultural fertilizer, the United States began importing it in 1843 through New York. By the early 1850s, the U. K. imported over 200,000 tons a year, and U. S. imports totaled about 760,000 tons. The Act enables U. S. citizens to take possession of unclaimed islands containing guano for the U. S. and this encouraged American entrepreneurs to search and exploit new deposits on tiny islands and reefs in the Caribbean and in the Pacific. This is the beginning of the concept of insular areas in U. S. territories, with insular areas, land could be held by the federal government without the prospect of its ever becoming a state in the Union. The provision was considered and ruled constitutional by the U. S. Supreme Court in Jones v. United States,137 U. S.202. More than 100 islands have been claimed for the United States under the Guano Islands Act, but most claims have been withdrawn. The Act specifically allows the islands to be considered possessions of the U. S. on the other hand, it also does not say that the U. S. cannot retain possession though the guano is exhausted. The Act does not specify what the status of the territory is after it is abandoned by private U. S. interests, the implication is that it reverts to its former status as terra nullius. In most cases, the stems from attempts by a state to expand its exclusive economic zone over the surrounding seas. To cement the U. S. claim to Navassa Island against Haiti, control of Navassa Island was transferred by the Department of the Interior to the Director of the Office of Insular Affairs under Order No.3205 on January 16,1997. Both the Department of the Interior and Insular Affairs would later grant administration responsibilities to the United States Fish, Order No 3210 also established a 12-nautical-mile territorial sea boundary for the United States around Navassa Island. Multiple countries have claimed ownership of Serranilla Bank and the Bajo Nuevo Bank, Bajo Nuevo Bank is the subject of conflicting claims made by a number of sovereign states. In 1899, a claim was made on Fox Island, Quebec, neither the US nor Jamaica recognized his claim before the raft was destroyed in a storm in 1966
31.
Baker Island
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Baker Island /ˈbeɪkər/ is an uninhabited atoll located just north of the equator in the central Pacific Ocean about 3,090 km southwest of Honolulu. The island lies almost halfway between Hawaii and Australia, the island covers 2.1 km2, with 4.8 km of coastline. The climate is equatorial, with rainfall, constant wind. The terrain is low-lying and sandy, an island surrounded by a narrow fringing reef with a depressed central area devoid of a lagoon with its highest point being 8 m above sea level. The island now forms the Baker Island National Wildlife Refuge and is an unincorporated and unorganized territory of the U. S. which vouches for its defense and it is visited annually by the U. S. Fish and Wildlife Service. For statistical purposes, Baker is grouped with the United States Minor Outlying Islands, Baker Island is also the last piece of land that experiences the New Year. A cemetery and rubble from earlier settlements are located near the middle of the west coast, there are no ports or harbors, with anchorage available only offshore. The narrow fringing reef surrounding the island can be a maritime hazard, bakers abandoned World War II runway,5,463 ft long, is completely covered with vegetation and is unserviceable. The United States claims an Exclusive Economic Zone of 200 nautical miles, during a 1935–1942 colonization attempt, the island was most likely on Hawaii time, which was then 10.5 hours behind UTC. Since it is uninhabited the islands time zone is unspecified, Baker was discovered in 1818 by Captain Elisha Folger of the Nantucket whaling ship Equator, who called the island New Nantucket. In August 1825 Baker was sighted by Captain Obed Starbuck of the Loper, the island is named for Michael Baker, who visited the island in 1834. Other references state that he visited in 1832, and again on August 14,1839, in the whaler Gideon Howland, Captain Baker claimed the island in 1855, then he sold his interest to a group who later formed the American Guano Company. The United States took possession of the island in 1857, claiming it under the Guano Islands Act of 1856 and its guano deposits were mined by the American Guano Company from 1859 to 1878. On 7 December 1886, it all its rights to the British firm John T. Arundel and Company. Arundel applied in 1897 to the British Colonial Office for a licence to work the island on the presumption that the USA had abandoned their claim, the United Kingdom then considered Baker Island as a British territory, while never formally annexing it. This short-lived attempt at colonization begun when American colonists arrived aboard the USCGC Itasca and they built a lighthouse and substantial dwellings, and they attempted to grow various plants. The settlement was named Meyerton, after Captain H. A, meyer of the United States Army, who helped establish the camps in 1935. One sad-looking clump of coconut palms was jokingly called King-Doyle Park after two well-known citizens of Hawaii who visited on the Taney in 1938, King-Doyle Park was later adopted as a geographic name by the USGS
32.
Cupola
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In architecture, a cupola /ˈkjuːpələ/ is a small, most often dome-like, structure on top of a building. Often used to provide a lookout or to light and air. The word derives, via Italian, from the lower Latin cupula small cup indicating a vault resembling an upside down cup. The cupola is a development during the Renaissance of the oculus, an ancient device found in Roman architecture, the chhatri, seen in Indian architecture, fits the definition of a cupola when it is used atop a larger structure. Cupolas often appear as small buildings in their own right and they often serve as a belfry, belvedere, or roof lantern above a main roof. In other cases they may crown a spire, tower, or turret, barns often have cupolas for ventilation. The square, dome-like segment of a North American railroad train caboose that contains the second-level or angel seats is called a cupola. Some armored fighting vehicles have cupolas, called commanders cupola, which is a dome or cylinder with armored glass to provide 360-degree vision around the vehicle
33.
Veranda
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A veranda or verandah is a roofed, open-air gallery or porch. A veranda is often enclosed by a railing and frequently extends across the front. Although the form verandah is correct and very common, some prefer the version without an h. The veranda has featured prominently in Australian vernacular architecture and first became widespread in colonial buildings during the 1850s. The Victorian Filigree architecture style is used by residential and commercial buildings across Australia and features decorative screens of wrought iron, the Queenslander is a style of residential construction in Queensland, Australia, which is adapted to subtropical climates and characterized by its large verandas. The bandeirista style house from Brazil typically has a veranda positioned to face the sunrise, the Creole townhouse in New Orleans, Louisiana, is also noted for its prominent use of verandas. In fact, most houses constructed in the Southern United States before the advent of air conditioning were built with a front porch or veranda. Spanish Colonial architecture commonly incorporates verandas, both on the exterior of buildings and, in cases of buildings with courtyards, along the walls of courtyards. In some cases, homes were constructed with every room opening into a courtyard veranda, rather than interior corridors or direct connections to other rooms
34.
Shore
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A shore or a shoreline is the fringe of land at the edge of a large body of water, such as an ocean, sea, or lake. Shores are influenced by the topography of the landscape, as well as by water induced erosion. The geological composition of rock and soil dictates the type of shore which is created, Riviera is an Italian word for shoreline, ultimately derived from Latin ripa. It came to be applied as a name to the coast of the Ligurian Sea, in the form riviera ligure. Historically, the Ligurian Riviera extended from Capo Corvo south of Genoa, north and west into what is now French territory past Monoco, now it is divided into the Italian Riviera and the French Riviera. Although the French use the term Riviera to refer to the Italian Riviera, as a result of the fame of the Ligurian rivieras, the term came into English to refer to any shoreline, especially one that is sunny, topographically diverse and popular with tourists. Such places using the term include the Australian Riviera in Queensland, offshore or Intertidal zone Ballantine Scale Coastal path Shorezone Anders, F. J. and Byrnes, M. R. Accuracy of shoreline change rates as determined from maps and aerial photographs Shore and Beach, v.59, processes influencing the transport and fate of contaminated sediments in the coastal ocean—Boston Harbor and Massachusetts Bay, U. S. Geological Survey Circular 1302, pp. 1–89. Equilibrium beach profiles—characteristics and applications Journal of Coastal Research, v.7, the Budget of Littoral Sediments—Concepts and Applications Shore and Beach, v.64, pp. 18–26. Meade, R. H. Sources, sinks and storage of river sediments in the Atlantic drainage of the United States Journal of Geology, v.90, an Assessment of the Nations Shorelines, USA Shore and Beach v.71, no. Stockdon, H. F. Sallenger, A. H. List, J. H. and Holman, estimation of shoreline position and change using airborne topographic lidar data Journal of Coastal Research, v.18, no. The use of models to predict beach behavior for U. S. coastal engineering—A critical review Journal of Coastal Research, v.16. Media related to Shores at Wikimedia Commons shore, the American Heritage Dictionary of the English Language
35.
Samuel Gardner Wilder
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Samuel Gardner Wilder was an American shipping magnate and politician who developed a major transportation company in the Kingdom of Hawaii. Samuel Gardner Wilder was born June 20,1831 in Leominster and his father was William Chauncey Wilder and mother was Harriet Waters. They moved to Canada for a few years, and then to New York in 1840, part of the California Gold Rush, the family moved west in 1852. He worked for the Adams Express Company which allowed him to travel to and his first visit to the Hawaiian Islands was in 1856. He married Elizabeth Kinaʻu Judd, daughter of doctor and politician Gerrit P. Judd September 29,1857 in Honolulu. She was namesake of the native Hawaiian civil leader Elizabeth Kīnaʻu and he took a load of guano from Jarvis Island to New York City, which served as the couples honeymoon voyage. He then started a plantation with his father-in-law in 1864. He sent for his brother, William Chauncey Wilder who had served in the cavalry in the American Civil War, the plantation failed by 1868 and William returned to Geneva, Illinois. In 1870 other sugar planters had Wilder sent to China to bring back low-cost workers and he encountered resistance from the British administration in Hong Kong, and only 188 Chinese came as a result. In 1871 he took over the business of James I. He also became agent for the government-owned steamship Kilauea, named for Kīlauea volcano, in 1872 with C. H. Lewers, he established Wilder & Company for the shipping and related businesses. In 1873 his brother William brought out his wife and family to help in the shipping business, in 1877 the government ordered a second steamer Likelike from San Francisco. After one voyage, the government promptly sold it to Wilder, the Likelike was about 50% larger than the aged Kilauea, which needed frequent repairs. Part of his agreement was to carry the mail on his ships, over time more ships were added to his fleet, and railroads built to meet the ports. The Hawaiian Railroad was constructed from 1881 to 1883 and it ran from plantations in the Kohala district of the island of Hawaiʻi to a harbor he built at Māhukona. The company was incorporated as Wilder Steamship Company in 1883, in 1868, Wilder was elected to the House of Representatives of the legislature of the Hawaiian Kingdom. In 1874, King Lunalilo appointed him to the upper House of Nobles of the legislature, Lunalilo died after reigning only one year, so the first job of the 1874 legislature was to elect a new king, Wilder was selected to count and announce the votes. Wilder used his steamer to campaign for David Kalākaua, who won the election in the Legislative Assembly, in 1878, Wilder established the first telephone line on Oahu, from his government office to his lumber business
36.
Fertilizer
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A fertilizer or fertiliser is any material of natural or synthetic origin that is applied to soils or to plant tissues to supply one or more plant nutrients essential to the growth of plants. Fertilizers enhance the growth of plants and this goal is met in two ways, the traditional one being additives that provide nutrients. The second mode by which some fertilizers act is to enhance the effectiveness of the soil by modifying its water retention and aeration and this article, like many on fertilizers, emphasises the nutritional aspect. The nutrients required for plant life are classified according to the elements. Instead compounds containing these elements are the basis of fertilizers, the macronutrients are consumed in larger quantities and are present in plant tissue in quantities from 0. 15% to 6. 0% on a dry matter basis. Plants are made up of four elements, hydrogen, oxygen, carbon. Carbon, hydrogen and oxygen are widely available as water and carbon dioxide, although nitrogen makes up most of the atmosphere, it is in a form that is unavailable to plants. Nitrogen is the most important fertilizer since nitrogen is present in proteins, DNA, to be nutritious to plants, nitrogen must be made available in a fixed form. Only some bacteria and their host plants can fix atmospheric nitrogen by converting it to ammonia, phosphate is required for the production of DNA and ATP, the main energy carrier in cells, as well as certain lipids. Micronutrients are consumed in quantities and are present in plant tissue on the order of parts-per-million, ranging from 0.15 to 400 ppm DM. These elements are present at the active sites of enzymes that carry out the plants metabolism. Because these elements enable catalysts their impact far exceeds their weight percentage, Fertilizers are classified in several ways. They are classified according to whether they provide a single nutrient, multinutrient fertilizers provide two or more nutrients, for example N and P. Fertilizers are also sometimes classified as inorganic versus organic. Inorganic fertilizers exclude carbon-containing materials except ureas, organic fertilizers are usually plant- or animal-derived matter. Inorganic are sometimes called synthetic fertilizers since various chemical treatments are required for their manufacture, the main nitrogen-based straight fertilizer is ammonia or its solutions. Ammonium nitrate is widely used. Urea is another source of nitrogen, having the advantage that it is solid and non-explosive, unlike ammonia and ammonium nitrate. A few percent of the fertilizer market has been met by calcium ammonium nitrate
37.
Entrepreneurship
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What appears as a real opportunity ex ante might actually be a non-opportunity or one that cannot be actualized by entrepreneurs lacking the necessary business skills, financial or social capital. Traditionally, an entrepreneur has been defined as a person who starts, organizes and manages any enterprise, especially a business, usually with considerable initiative and risk. Rather than working as an employee, an entrepreneur runs a business and assumes all the risk and reward of a given business venture, idea. The entrepreneur is commonly seen as a leader and innovator of new ideas. They act as the manager and oversee the launch and growth of an enterprise, Entrepreneurship is the process by which an individual identifies a business opportunity and acquires and deploys the necessary resources required for its exploitation. For Schumpeter, the changes and dynamic disequilibrium brought on by the innovating entrepreneur, the ‘norm’ of a healthy economy. Entrepreneurial spirit is characterized by innovation and risk-taking, for example, in the 2000s, the field of social entrepreneurship has been identified, in which entrepreneurs combine business activities with humanitarian, environmental or community goals. In the 2010s, entrepreneurship can be studied in college or university as part of the disciplines of management or business administration, Entrepreneur, is a loanword from French. First used in 1723, today the term entrepreneur implies qualities of leadership, initiative, economist Robert Reich has called team-building, leadership, and management ability essential qualities for the entrepreneur. Historically the study of entrepreneurship reaches back to the work in the late 17th and early 18th centuries of Richard Cantillon and Adam Smith, which was foundational to classical economics. In the 20th century, entrepreneurship was studied by Joseph Schumpeter in the 1930s and other Austrian economists such as Carl Menger, Ludwig von Mises, the term entrepreneurship was coined around the 1920s, while the loan from French of the word entrepreneur dates to the 1850s. According to Schumpeter, an entrepreneur is willing and able to convert a new idea or invention into a successful innovation, thus, creative destruction is largely responsible for long-term economic growth. The idea that leads to economic growth is an interpretation of the residual in endogenous growth theory. For Schumpeter, entrepreneurship resulted in new industries and in new combinations of currently existing inputs, Schumpeters initial example of this was the combination of a steam engine and then current wagon making technologies to produce the horseless carriage. In this case the innovation, the car, was transformational and it did not immediately replace the horse-drawn carriage, but in time, incremental improvements reduced the cost and improved the technology, leading to the modern auto industry. Despite Schumpeters early 20th-century contributions, traditional microeconomic theory did not formally consider the entrepreneur in its theoretical frameworks, in this treatment, the entrepreneur was an implied but unspecified actor, consistent with the concept of the entrepreneur being the agent of x-efficiency. For Schumpeter, the entrepreneur did not bear risk, the capitalist did, Schumpeter was of the opinion that entrepreneurs shift the Production Possibility Curve to a higher level using innovations. Cantillon emphasized the willingness of the entrepreneur to assume risk and to deal with uncertainty, thus, he draws attention to the function of the entrepreneur, and distinguishes clearly between the function of the entrepreneur and the owner who provides the money
38.
Henry Winkelmann
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Henry Winkelmann was a notable New Zealand photographer. Winkelmanns photographs covered a range of topics, but he is best known for his yachting photographs. Henry Winkelmann was born in Bradford, Yorkshire, England on 26 September 1860, one of eight children of Peter Winkelmann a stuff and yarn merchant and he spent parts of his childhood in nearby Gomersal, Bramley and Manningham. His older brother, Charles, immigrated to New Zealand in 1875, in Henry Winkelmann immigrated to New Zealand arriving at Port Chalmers in October 1878 on the sailing ship Calypso. As his father had died in 1877 his mother, Louise, by 1881 he was living in Auckland and unemployed. Henderson would provide passage and provisions plus a salary, payable upon return of £2 10s for every month spent on the island and they were to stay a minimum of three months, a maximum of five, and they were to resist any attempts at dispossession. They left Auckland aboard the schooner Sunbeam on 8 June 1881, in order to prevent other Auckland business rivals knowing what they were doing, their advertised destination was given as the Kingsmill Islands. The schooner reached Jarvis Island on 2 August 1881 which dropped them off in August 1881, the island was small, consisted mostly of white coral and guano, had no trees and was home to three graves and a number of rundown buildings built by the American Guano Company. They explored the island and removed a foreign flag, finding evidence of a recent caretaker who had left the island because of sickness, a notice stated he would return. Winkelmann and Hudson made their own declaration, signed it and hoisted the British flag, however, when the ship failed to return, the men struggled to survive. They built a still, caught turtles and preserved and ate birds eggs and they were finally rescued on 23 March 1882 by a ship sent by Henderson, nearly eight months after their arrival on the island. Before leaving the island, the tried to load up with guano. A man named Squire Flockton was left behind to retain ownership, several months later, deranged and full of gin, he shot and killed himself. Upon their return to Auckland, Henderson paid them their wages, in 1882 Winkelmann joined the Bank of New Zealand. He worked in branches in New Zealand and Fiji, supplementing his income by teaching the zither, in 1889 he was transferred to the banks Sydney branch, returning to Auckland in 1891. In April 1892 Winkelmann purchased a Lancaster Instantograph camera and soon recognising its commercial potential began to supplement his earnings as bank clerk with photography and he created a darkroon in his mothers house in Dock Street, Devonport. He continued to work at the Bank of New Zealand, which by 1896 had relocated him to Blenheim and he remained there until 1897 when after his mothers death he left the bank and returned to Auckland. Back in Auckland he began a customs and indent agency on Queen Street wharf and he also sold insurance for the Magdeburg Insurance Company, acted as a debt collector
39.
Gin
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Gin is a spirit which derives its predominant flavour from juniper berries. From its earliest origins in the Middle Ages, gin has evolved from use in medicine to an object of commerce in the spirits industry. Gin is one of the broadest categories of spirits, represented by products of various origins, styles, Gin emerged in England in varying forms as of the early 17th century, and at the time of the Restoration, enjoyed a brief resurgence. Gin drinking in England rose significantly after the Government allowed unlicensed gin production and this created a market for poor-quality grain that was unfit for brewing beer, and thousands of gin-shops sprang up throughout England, a period known as the Gin Craze. Because of the price of gin, when compared with other drinks available at the same time and in the same geographic location. Of the 15,000 drinking establishments in London, not including coffee shops and drinking chocolate shops, Beer maintained a healthy reputation as it was often safer to drink the brewed ale than unclean plain water. Gin, though, was blamed for various problems. The reputation of the two drinks was illustrated by William Hogarth in his engravings Beer Street and Gin Lane, described by the BBC as arguably the most potent anti-drug poster ever conceived. The negative reputation of gin survives today in the English language, in terms like gin mills or the American phrase gin joints to describe disreputable bars, the epithet mothers ruin is a common British name for gin, the origin of which is the subject of ongoing debate. The Gin Act 1736 imposed high taxes on retailers and led to riots in the streets, the prohibitive duty was gradually reduced and finally abolished in 1742. The Gin Act 1751 was more successful, however, it forced distillers to sell only to licensed retailers, Gin in the 18th century was produced in pot stills, and was somewhat sweeter than the London gin known today. In London in the early 18th century, much gin was distilled legally in residential houses and was often flavoured with turpentine to generate resinous woody notes in addition to the juniper. As late as 1913, Websters Dictionary states without further comment, another common variation was to distill in the presence of sulphuric acid. Although the acid itself does not distil, it imparts the aroma of diethyl ether to the resulting gin. Sulphuric acid subtracts one water molecule from two molecules to create diethyl ether, which also forms an azeotrope with ethanol. The result is a spirit, and one that may have possessed additional analgesic or even intoxicating effects – see Paracelsus. Dutch or Belgian gin, also known as jenever or genever, evolved from malt wine spirits, Schiedam, a city in the province of South Holland, is famous for its jenever-producing history. The oude style of jenever remained very popular throughout the 19th century, the 19th century gave rise to a style of gin referred to as Old Tom Gin, which is a softer, sweeter style of gin, often containing sugar
40.
Headstone
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A headstone, tombstone, or gravestone is a stele or marker, usually stone, that is placed over a grave. They are traditional for burials in the Christian, Jewish and Muslim religions, in many parts of Europe insetting a photograph of the deceased in a frame is very common. The stele, as it is called in a context, is one of the oldest forms of funerary art. Originally, a tombstone was the lid of a stone coffin, or the coffin itself. Now all three terms are used for markers placed at the head of the grave. Some graves in the 18th century also contained footstones to demarcate the end of the grave. This sometimes developed into full kerb sets that marked the perimeter of the grave. Footstones were rarely annotated with more than the initials and year of death. Many cemeteries and churchyards have removed those extra stones to ease grass cutting by machine mower, note that in some UK cemeteries the principal, and indeed only, marker is placed at the foot of the grave. Owing to soil movement and Downhill creep on gentle slopes, older headstones and footstones can often be tilted at an angle. Over time, this movement can result in the stones being sited several metres away from their original location, graves, and any related memorials are a focus for mourning and remembrance. The names of relatives are often added to a gravestone over the years, since gravestones and a plot in a cemetery or churchyard cost money, they are also a symbol of wealth or prominence in a community. Some gravestones were even commissioned and erected to their own memory by people who were living, as a testament to their wealth. In a Christian context, the wealthy often erected elaborate memorials within churches rather than having simply external gravestones. Crematoria frequently offer similar alternatives to families who do not have a grave to mark, carved or cast commemorative plaques inside the crematorium for example may serve this purpose. A cemetery may follow national codes of practice or independently prescribe the size and use of certain materials, some may limit the placing of a wooden memorial to six months after burial, after which a more permanent memorial must be placed. Others may require stones of a shape or position to facilitate grass-cutting. Headstones of granite, marble and other kinds of stone are usually created, installed, restoration is a specialized job for a monumental mason
41.
Cemetery
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A cemetery or graveyard is a place where the remains of dead people are buried or otherwise interred. The word cemetery implies that the land is designated as a burial ground. The term graveyard is used interchangeably with cemetery, but primarily referred to a burial ground within a churchyard. The intact or cremated remains of people may be interred in a grave, commonly referred to as burial, or in a tomb, an above-ground grave, in Western cultures, funeral ceremonies are often observed in cemeteries. These ceremonies or rites of passage according to cultural practices. Modern cemeteries often include crematoria, and some previously used for both, continue as crematoria as a principal use long after the interment areas have been filled. The Oxford English Dictionary defines a cemetery as a burial-ground generally, a large public park or ground laid out expressly for the interment of the dead, and not being the ‘yard’ of any church. Prehistoric cemeteries are referred to by the term grave field. From about the 7th century, European burial was under the control of the Church, practices varied, but in continental Europe, bodies were usually buried in a mass grave until they had decomposed. The bones were exhumed and stored in ossuaries, either along the arcaded bounding walls of the cemetery, or within the church under floor slabs. In Europe this was accompanied with a depiction of their coat of arms. Most others were buried in graveyards again divided by social status, mourners who could afford the work of a stonemason had a headstone engraved with a name, dates of birth and death and sometimes other biographical data, and set up over the place of burial. Usually, the writing and symbols carved on the headstone. Some families hired a blacksmith and had large crosses made from various metals put on the place of burial, in many European states, burial in graveyards was eventually outlawed altogether through government legislation. Instead of graveyards, completely new places of burial were established away from populated areas and outside of old towns. Many new cemeteries became municipally owned or were run by their own corporations, in some cases, skeletons were exhumed from graveyards and moved into ossuaries or catacombs. A large action of this occurred in 18th century Paris when human remains were transferred from graveyards all over the city to the Catacombs of Paris. The bones of an estimated 6 million people are to be found there, an early example of a landscape-style cemetery is Père Lachaise in Paris
42.
John T. Arundel
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John T. Arundel was an English entrepreneur who was instrumental in the development of the mining of phosphate rock on the Pacific islands of Nauru and Banaba. Williams & Macdonald described J. T. Arundel as a example of that mid-Victorian phenomenon. His father owned a gentlemans outfitter in the City of London, the family were active in the Congregational Church, and through a church connection he joined Houlder Brothers & Co. a firm that provided ships for migration to New Zealand and Australia. In 1860, J. T. Arundel travelled on a Houlder Brothers & Co ship into the Pacific, calling at the Chincha Islands, on which guano was mined for refining into superphosphate. J. T. Arundel took an interest in the potential of the fertiliser business, when J. T. J. T. Arundel and Lillie Whibley were not to marry until 1881. Following their marriage Lillie Arundel would travel into the central Pacific with J. T. Arundel when he would visit the islands on which his company has operations. Lillie Arundel gave birth in 1884 to their daughter while on Manra, then known as Sydney Island. In 1898 Fred Whibley, Lillies younger brother, arrived in Sydney, after 10 years in the United States, J. T. Arundel offered Fred Whibley a position with John T. Arundel & Co. Fred Whibley declined and chose to become a trader on Niutao in what is now Tuvalu. A harmonious working relationship would have been given the pious Christian attitudes of J. T. Arundel. In 1871 with financial support from Houlder Brothers and Co. he established John T. Arundel & Co, the initial activities were carried out by the two companies. Houlder Brothers and Co leased Flint Island from the British government, in 1872, Caroline Island was leased by the Houlder Brothers. In 1881, the lease was taken over by Arundel. John T. Arundel & Co went on to engage in mining guano on other Pacific islands and also established coconut plantations and traded in copra and other commodities. The company operated from Sydney, Australia with business interests in the Pacific that included, Mining guano on, the guano mining, which began in 1874, supplied a total of about 10,000 tons of phosphate until supplies were exhausted around 1895. Baker Island from 1886 to 1899, which is now claimed as a territory of the United States. Howland Island from 1886 to 1899, which is part of the Phoenix Islands. Jarvis Island from 1886 to 1899, which is part of the Line Islands
