Forty-eighth Congress
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Forty-eighth Congress
The 48th United States Congress was a meeting of the legislative branch of the United States federal government, consisting of the United States Senate and the United States House of Representatives. It met in Washington, D.C. from March 4, 1883, to March 4, 1885, during the last two years of the administration of U.S. President Chester A. Arthur. The apportionment of seats in the House of Representatives was based on the Tenth Census of the United States in 1880. The Senate had a Republican majority, and the House had a Democratic majority. Major events * September 5, 1883: Mary F. Hoyt became the first woman appointed to the U.S. federal civil service (and the second person appointed by examination (in which she came top) instituted under the Pendleton Civil Service Reform Act) when she became a clerk in the Bank Redemption Agency of the Department of the Treasury. * October 15, 1883: The Supreme Court of the United States declared part of the Civil Rights Act of 1875 u ...
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United States Capitol
The United States Capitol, often called The Capitol or the Capitol Building, is the seat of the legislative branch of the United States federal government, which is formally known as the United States Congress. It is located on Capitol Hill at the eastern end of the National Mall in Washington, D.C. Though no longer at the geographic center of the federal district, the Capitol forms the origin point for the street-numbering system of the district as well as its four quadrants. Central sections of the present building were completed in 1800. These were partly destroyed in the 1814 Burning of Washington, then were fully restored within five years. The building was later enlarged by extending the wings for the chambers for the bicameral legislature, the House of Representatives in the south wing and the Senate in the north wing. The massive dome was completed around 1866 just after the American Civil War. Like the principal buildings of the executive and judicial branches ...
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Civil Rights Act Of 1875
The Civil Rights Act of 1875, sometimes called the Enforcement Act or the Force Act, was a United States federal law enacted during the Reconstruction era in response to civil rights violations against African Americans. The bill was passed by the 43rd United States Congress and signed into law by United States President Ulysses S. Grant on March 1, 1875. The act was designed to "protect all citizens in their civil and legal rights", providing for equal treatment in public accommodations and public transportation and prohibiting exclusion from jury service. It was originally drafted by Senator Charles Sumner in 1870, but was not passed until shortly after Sumner's death in 1875. The law was not effectively enforced, partly because President Grant had favored different measures to help him suppress election-related violence against blacks and Republicans in the Southern United States. The Reconstruction era ended with the resolution of the 1876 presidential election, and the Civil ...
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1884 United States Presidential Election
The 1884 United States presidential election was the 25th quadrennial presidential election, held on Tuesday, November 4, 1884. It saw the first Democrat elected President of the United States since James Buchanan in 1856, and the first Democratic president to hold office since Andrew Johnson, who assumed the presidency after the assassination of Abraham Lincoln. Governor Grover Cleveland of New York defeated Republican James G. Blaine of Maine. The election was set apart by unpleasant mudslinging and shameful personal allegations that eclipsed substantive issues, for example, civil administration change. It was a historically significant election, as Cleveland was the only Democratic president between Andrew Johnson, who left office in 1869, and Woodrow Wilson, who began his first term in 1913, representing a disruption of the period of Republican domination of the presidency between Reconstruction and the Great Depression. Cleveland won the presidential nomination on the seco ...
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Greenwich Meridian
The historic prime meridian or Greenwich meridian is a geographical reference line that passes through the Royal Observatory, Greenwich, Royal Observatory, Greenwich, in London, England. The modern IERS Reference Meridian widely used today is based on the Greenwich meridian, but differs slightly from it. This prime meridian (at the time, one of prime meridian, many) was first established by George Biddell Airy, Sir George Airy in 1851, and by 1884, over two-thirds of all ships and tonnage used it as the reference Meridian (geography), meridian on their Nautical chart, charts and maps. In October of that year, at the behest of President of the United States, US President Chester A. Arthur, 41 delegates from 25 nations met in Washington, D.C., United States, for the International Meridian Conference. This conference selected the meridian passing through Greenwich as the world standard prime meridian due to its popularity. However, France abstained from the vote, and French maps ...
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International Meridian Conference
The International Meridian Conference was a conference held in October 1884 in Washington, D.C., in the United States, to determine a prime meridian for international use. The conference was held at the request of U.S. President Chester A. Arthur. The subject to discuss was the choice of "a meridian to be employed as a common zero of longitude and standard of time reckoning throughout the world". It resulted in the recommendation of the Greenwich Meridian as the international standard for zero degrees longitude. Background By the 1870s there was pressure both to establish a prime meridian for worldwide navigation purposes and to unify local times for railway timetables. The first International Geographical Congress, held in Antwerp in 1871, passed a motion in favour of the use of the Greenwich Meridian for (smaller scale) passage charts, suggesting that it should become mandatory within 15years. In Britain, the Great Western Railway had standardised time by 1840 and in 1847 t ...
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Newport, Rhode Island
Newport is an American seaside city on Aquidneck Island in Newport County, Rhode Island. It is located in Narragansett Bay, approximately southeast of Providence, Rhode Island, Providence, south of Fall River, Massachusetts, south of Boston, and northeast of New York City. It is known as a New England summer resort and is famous for its historic Newport Mansions, mansions and its rich sailing history. It was the location of the first U.S. Open tournaments in both US Open (tennis), tennis and US Open (golf), golf, as well as every challenge to the America's Cup between 1930 and 1983. It is also the home of Salve Regina University and Naval Station Newport, which houses the United States Naval War College, the Naval Undersea Warfare Center, and an important Navy training center. It was a major 18th-century port city and boasts many buildings from the Colonial history of the United States, Colonial era. The city is the county seat of Newport County, Rhode Island, Newport County ...
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United States Naval War College
The Naval War College (NWC or NAVWARCOL) is the staff college and "Home of Thought" for the United States Navy at Naval Station Newport in Newport, Rhode Island. The NWC educates and develops leaders, supports defining the future Navy and associated roles and missions, supports combat readiness, and strengthens global maritime partnerships. The Naval War College is one of the senior service colleges including the Army War College, the Marine Corps War College, and the USAF Air War College. Additionally, the U.S. Department of Defense operates the National War College. History The college was established on October 6, 1884; its first president, Commodore Stephen B. Luce, was given the old building of the Newport Asylum for the Poor to house it on Coasters Harbor Island in Narragansett Bay. Among the first four faculty members were Tasker H. Bliss, a future Army Chief of Staff, James R. Soley, the first civilian faculty member and a future Assistant Secretary of the Navy, and, ...
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Amityville, New York
Amityville () is a Political subdivisions of New York State#Village, village near the Babylon (town), New York, Town of Babylon in Suffolk County, New York, Suffolk County, on the South Shore (Long Island), South Shore of Long Island, in New York (state), New York. The population was 9,523 at the 2010 United States census, 2010 census. History Huntington (CDP), New York, Huntington settlers first visited the Amityville area in 1653 due to its location to a source of salt hay for use as animal fodder. Wyandanch (sachem), Chief Wyandanch granted the first deed to land in Amityville in 1658. The area was originally called ''Huntington West Neck South'' (it is on the Great South Bay and Suffolk County, New York border in the southwest corner of what once called Huntington South), but is now the Town of Babylon. According to village lore, the name was changed in 1846 when residents were working to establish its new post office. The meeting turned into bedlam and one participant was t ...
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Jamaica, Queens
Jamaica is a neighborhood in the New York City borough of Queens. It is mainly composed of a large commercial and retail area, though part of the neighborhood is also residential. Jamaica is bordered by Hollis to the east; St. Albans, Springfield Gardens, Rochdale Village to the southeast; South Jamaica to the south; Richmond Hill and South Ozone Park to the west; Briarwood to the northwest; and Kew Gardens Hills, Jamaica Hills, and Jamaica Estates to the north. Jamaica, originally a designation for an area greater than the current neighborhood, was settled under Dutch rule in 1656. It was originally called ' before it took its current name. Subsequently, under English rule Jamaica became the center of the "Town of Jamaica". It was the first county seat of Queens County, holding that title from 1683 to 1788, and was also the first incorporated village on Long Island. When Queens was incorporated into the City of Greater New York in 1898, both the Town of Jamaica and the Vil ...
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Mercalli Intensity Scale
The Modified Mercalli intensity scale (MM, MMI, or MCS), developed from Giuseppe Mercalli's Mercalli intensity scale of 1902, is a seismic intensity scale used for measuring the intensity of shaking produced by an earthquake. It measures the effects of an earthquake at a given location, distinguished from the earthquake's inherent force or strength as measured by seismic magnitude scales (such as the "" magnitude usually reported for an earthquake). While shaking is caused by the seismic energy released by an earthquake, earthquakes differ in how much of their energy is radiated as seismic waves. Deeper earthquakes also have less interaction with the surface, and their energy is spread out across a larger volume. Shaking intensity is localized, generally diminishing with distance from the earthquake's epicenter, but can be amplified in sedimentary basins and certain kinds of unconsolidated soils. Intensity scales empirically categorize the intensity of shaking based on the effect ...
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Earthquake
An earthquake (also known as a quake, tremor or temblor) is the shaking of the surface of the Earth resulting from a sudden release of energy in the Earth's lithosphere that creates seismic waves. Earthquakes can range in intensity, from those that are so weak that they cannot be felt, to those violent enough to propel objects and people into the air, damage critical infrastructure, and wreak destruction across entire cities. The seismic activity of an area is the frequency, type, and size of earthquakes experienced over a particular time period. The seismicity at a particular location in the Earth is the average rate of seismic energy release per unit volume. The word ''tremor'' is also used for Episodic tremor and slip, non-earthquake seismic rumbling. At the Earth's surface, earthquakes manifest themselves by shaking and displacing or disrupting the ground. When the epicenter of a large earthquake is located offshore, the seabed may be displaced sufficiently to cause ...
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Time Zone
A time zone is an area which observes a uniform standard time for legal, Commerce, commercial and social purposes. Time zones tend to follow the boundaries between Country, countries and their Administrative division, subdivisions instead of strictly following longitude, because it is convenient for areas in frequent communication to keep the same time. All time zones are defined as offsets from Coordinated Universal Time (UTC), ranging from UTC−12:00 to UTC+14:00. The UTC offset, offsets are usually a whole number of hours, but a few zones are offset by an additional 30 or 45 minutes, such as in Indian Standard Time, India, Time in Australia, South Australia and Nepal Time, Nepal. Some areas of higher latitude use daylight saving time for about half of the year, typically by adding one hour to local time during spring (season), spring and summer. List of UTC offsets In the table below, the locations that use daylight saving time (DST) are listed in their UTC offse ...
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