Coventry Centre, Rhode Island
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Coventry Centre, Rhode Island
Coventry Centre is a historic village in Coventry, Rhode Island. The village was founded in 1809 and was originally called "Shoethread." The village was renamed Coventry Centre because it is the geographic center of the town. In the 18th century Bog iron was mined in Maroon Swamp (named after the color of the iron deposits), an area now known as Stump Pond. The area also contains Foster Ledge Quarry from which granite Granite () is a coarse-grained ( phaneritic) intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies under ... was transported by the Hartford Fishkill Railroad and used in various buildings across the state.Andrew D. Boisvert, Coventry Roots: Coventry Centre, Coventry Patch, May 3, 2011, http://coventry.patch.com/articles/coventry-roots-coventry-centre References Villages in Kent County, Rhode Island Coventry, Rhod ...
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Coventry, Rhode Island
Coventry is a town in Kent County, Rhode Island, United States. The population was 35,688 at the 2020 census and is part of the . Geography According to the United States Census Bureau, the town has a total area of . of it is land and of it (4.49%) is water. The town is bordered by West Warwick to the east, Foster, Scituate, and Cranston to the north, West Greenwich and East Greenwich to the south, and Sterling, Connecticut, to the west. It is the largest town in land area in Rhode Island, being surpassed in total area only by South Kingstown, Rhode Island, with water and land area of . Climate According to the Köppen Climate Classification system, Coventry has an oceanic climate, abbreviated "Cfb" on climate maps. History Coventry was first settled by English colonists in the early 18th century, when the town was part of Warwick. Since the area was so far away from the center of Warwick, the section that became Coventry grew very slowly. However, by 1741, enou ...
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Bog Iron
Bog iron is a form of impure iron deposit that develops in bogs or swamps by the chemical or biochemical oxidation Redox (reduction–oxidation, , ) is a type of chemical reaction in which the oxidation states of substrate change. Oxidation is the loss of electrons or an increase in the oxidation state, while reduction is the gain of electrons or ... of iron carried in solution. In general, bog ores consist primarily of iron oxyhydroxides, commonly goethite (FeO(OH)). Iron-bearing groundwater typically emerges as a Spring (hydrology), spring and the iron in it forms ferric hydroxide upon encountering the oxidizing environment of the surface. Bog ore often combines goethite, magnetite, and vugs or stained quartz. Oxidation may occur through enzyme catalysis by iron bacteria. It is not clear whether the magnetite precipitates upon the first contact with oxygen, then oxidizes to ferric compounds, or whether the ferric compounds are reduced when exposed to Anoxic ...
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Granite
Granite () is a coarse-grained ( phaneritic) intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground. It is common in the continental crust of Earth, where it is found in igneous intrusions. These range in size from dikes only a few centimeters across to batholiths exposed over hundreds of square kilometers. Granite is typical of a larger family of ''granitic rocks'', or '' granitoids'', that are composed mostly of coarse-grained quartz and feldspars in varying proportions. These rocks are classified by the relative percentages of quartz, alkali feldspar, and plagioclase (the QAPF classification), with true granite representing granitic rocks rich in quartz and alkali feldspar. Most granitic rocks also contain mica or amphibole minerals, though a few (known as leucogranites) contain almost no dark minerals. Granite is near ...
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New York And New England Railroad
The New York and New England Railroad (NY&NE) was a railroad connecting southern New York State with Hartford, Connecticut; Providence, Rhode Island; and Boston, Massachusetts. It operated under that name from 1873 to 1893. Prior to 1873 it was known as the Boston, Hartford and Erie Railroad, which had been formed from several smaller railroads that dated back to 1846. After a bankruptcy in 1893, the NY&NE was reorganized and briefly operated as the New England Railroad before being leased to the competing New York, New Haven and Hartford Railroad in 1898. Today, most of the original New York and New England lines have been abandoned. A segment in Massachusetts is now part of the MBTA's Franklin Line providing commuter rail service to South Station in Boston, and another segment near East Hartford and Manchester, Connecticut, is used for freight service on the Connecticut Southern Railroad. Other portions in Connecticut and Rhode Island have been converted to rail trails. Histo ...
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Villages In Kent County, Rhode Island
A village is a clustered human settlement or community, larger than a hamlet but smaller than a town (although the word is often used to describe both hamlets and smaller towns), with a population typically ranging from a few hundred to a few thousand. Though villages are often located in rural areas, the term urban village is also applied to certain urban neighborhoods. Villages are normally permanent, with fixed dwellings; however, transient villages can occur. Further, the dwellings of a village are fairly close to one another, not scattered broadly over the landscape, as a dispersed settlement. In the past, villages were a usual form of community for societies that practice subsistence agriculture, and also for some non-agricultural societies. In Great Britain, a hamlet earned the right to be called a village when it built a church.
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Providence Metropolitan Area
The Providence metropolitan area is a region extending into eight counties in two states, and is the 38th largest metropolitan area in the United States. Anchored by the city of Providence, Rhode Island, it has an estimated population of 1,622,520, exceeding that of Rhode Island by slightly over 60%. The area covers almost all of Rhode Island. Thirty-eight of the 39 municipalities in the state are included; only Westerly is not. The Providence Metropolitan Statistical Area also extends into southern Massachusetts with an average population density of 2300 per mi2 (888 per km2). Its Gross Metropolitan Product is the country's 42nd largest at $64.7 billion, just above the Gross State Product of the entire state of Hawaii. Since 2006, the Providence metropolitan area has been officially included in the Greater Boston Combined Statistical Area (CSA), the sixth-largest CSA in the country, with over eight million residents. Boundaries The Providence metropolitan area contains towns ...
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Villages In Rhode Island
A village is a clustered human settlement or community, larger than a hamlet but smaller than a town (although the word is often used to describe both hamlets and smaller towns), with a population typically ranging from a few hundred to a few thousand. Though villages are often located in rural areas, the term urban village is also applied to certain urban neighborhoods. Villages are normally permanent, with fixed dwellings; however, transient villages can occur. Further, the dwellings of a village are fairly close to one another, not scattered broadly over the landscape, as a dispersed settlement. In the past, villages were a usual form of community for societies that practice subsistence agriculture, and also for some non-agricultural societies. In Great Britain, a hamlet earned the right to be called a village when it built a church.
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