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Conanicut Island

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41°31′00″N 71°23′00″W  /  41.5167°N 71.3833°W  / 41.5167; -71.3833

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46-830: Conanicut Island ( / k ə ˈ n æ n ə k ʌ t / kə- NAN -ə-kut ) is an island in Narragansett Bay in the American state of Rhode Island . The second-largest in the Bay, it is connected on the east to Newport on Aquidneck Island by the Claiborne Pell Bridge , commonly known as the Newport Bridge, and on the west to North Kingstown on the mainland via the Jamestown-Verrazano Bridge . The town of Jamestown comprises

92-629: A consortium of about 100 buyers purchased Conanicut, Dutch, and Gould Islands. They divided Conanicut into roughly a dozen large plots and reserved Dutch Island and parts of Conanicut for common use. Benedict Arnold (great-grandfather of the Revolutionary War traitor , who became governor of the Colony of Rhode Island the same year) and William Case were among the purchasers. The Indians and colonists lived side-by-side in relative peace for almost four decades. Conflicts eventually occurred in

138-645: A family of Indigenous languages of the Americas and most of the languages in the Algic language family are included in the group. The name of the Algonquian language family is distinguished from the orthographically similar Algonquin dialect of the Indigenous Ojibwe language (Chippewa), which is a senior member of the Algonquian language family. The term Algonquin has been suggested to derive from

184-482: A large army". Dutch navigator Adriaen Block explored and mapped the bay in 1614, and nearby Block Island is named in his honor. The first permanent Colonial settlement was established in 1636 by Roger Williams , a former member of the Massachusetts Bay Colony . He was friends with Narragansett sachem Canonicus , who provided him with land on which to build Providence Plantations . Around

230-515: A major United States Navy training center. The city of Fall River, Massachusetts is located at the confluence of the Taunton River and Mount Hope Bay , which form the northeasternmost part of Narragansett Bay. The southwest side of the bay includes the seaside tourist towns of Narragansett and Wickford . Quonset Point , south of Warwick, gives its name to the Quonset hut . Tides in

276-547: A new treatment that involves removal of nitrogen Narragansett Bay is the site of one of the world's longest-running plankton surveys, extending from 1957 through the present. Researchers at the University of Rhode Island ’s Graduate School of Oceanography collect samples weekly and the dataset contains 246 different species. Algonquian languages The Algonquian languages ( / æ l ˈ ɡ ɒ ŋ k ( w ) i ə n / al- GONG -k(w)ee-ən ; also Algonkian ) are

322-449: A noun, that it must be a purely linguistic characterization. Anthropological linguists have conversely argued the strong connection between animacy and items viewed as having spiritual importance. Another important distinction involves the contrast between nouns marked as proximate and those marked as obviative . Proximate nouns are those deemed most central or important to the discourse, while obviative nouns are those less important to

368-417: A number of places in southern New England, leading to what is known as King Philip's War . Life in the region was dominated by the colonists after 1676, although Conanicut Island remained a haven for many Indians. In 1725, a ferry was established between the island and Newport. Another ferry was established to South Kingstown in 1748. Narragansett Bay Narragansett Bay is a bay and estuary on

414-459: A single word. Ex: ( Menominee ) paehtāwāēwesew "He is heard by higher powers" ( paeht - 'hear', - āwāē - 'spirit', - wese - passivizer, - w third-person subject) or ( Plains Cree ) kāstāhikoyahk "it frightens us". These languages have been extensively studied by Leonard Bloomfield , Ives Goddard , and others. Algonquian nouns have an animate/inanimate contrast: some nouns are classed as animate , while all other nouns are inanimate . There

460-539: A site near the elementary school. The island is named for Chief Canonicus of the Narragansetts, who maintained his royal residence on the island. In 1636 or 1637, Dutch fur traders paid to use the island of Quentenis (today’s Dutch Island, located just west of Conanicut) as a base for their activities. In 1638, the English colonists made arrangements to use Conanicut Island for grazing sheep, and Canonicus

506-408: Is 10–40 days, with an average of 26 days. Tidal mixing is the dominant driver of circulation patterns in the bay, where currents can reach up to 2.5 feet per second. Non-tidal currents such as the flow of low salinity water at the surface out of the bay and high salinity deep water into the bay contribute to a current of about 0.33 feet per second. Winds also drive circulation patterns in the bay. In

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552-472: Is highest in winter and lowest in summer, while CSOs increase dramatically following heavy rain. Water from these freshwater inputs mixes with sea water to form a salinity gradient ranging from 24 ppt at the mouth of the Providence River to 32 ppt at the mouth of the bay. Water temperatures range between -0.5 °C and 24 °C over the year. Salinity and temperature patterns measured throughout

598-500: Is incorrect, and that Central Algonquian (in which he includes the Plains Algonquian languages) is a genetic subgroup, with Eastern Algonquian consisting of several different subgroups. However, this classification scheme has failed to gain acceptance from other specialists in the Algonquian languages. Instead, the commonly accepted subgrouping scheme is that proposed by Ives Goddard (1994). The essence of this proposal

644-405: Is ongoing debate over whether there is a semantic significance to the categorization of nouns as animate or inanimate, with scholars arguing for it as either a clearly semantic issue, or a purely syntactic issue, along with a variety of arguments in between. More structurally inclined linguistic scholars have argued that since there is no consistent semantic system for determining the animacy of

690-605: Is slowly subsiding between a shifting fault system. Providence is Rhode Island 's capital and largest city and sits at the northernmost arm of the bay. Many of Providence's suburbs are also on the bay, including East Providence , Warwick and Cranston . Newport is located at the south end of Aquidneck Island on the ocean, and is the home of the United States Naval War College , the Naval Undersea Warfare Center , and

736-624: Is sometimes said to have included the extinct Beothuk language of Newfoundland , whose speakers were both in geographic proximity to Algonquian speakers and who share DNA in common with the Algonquian-speaking Miꞌkmaq . However, linguistic evidence is scarce and poorly recorded, and it is unlikely that reliable evidence of a connection can be found. The Algonquian language family is known for its complex polysynthetic morphology and sophisticated verb system. Statements that take many words to say in English can be expressed with

782-448: Is that Proto-Algonquian originated with people to the west who then moved east, although Goddard did not attempt to identify a specific western urheimat for Proto-Algonquian in his 1994 paper. By this scenario, Blackfoot was the first language to branch off, which coincides well with its being the most divergent language of Algonquian. In west-to-east order, the subsequent branchings were: This historical reconstruction accords best with

828-547: The Maliseet word elakómkwik ( pronounced [ɛlæˈɡomoɡwik] ), "they are our relatives/allies". Speakers of Algonquian languages stretch from the east coast of North America to the Rocky Mountains . The proto-language from which all of the languages of the family descend, Proto-Algonquian , was spoken around 2,500 to 3,000 years ago. There is no scholarly consensus about where this language

874-584: The Plateau region of Idaho and Oregon or the Rocky Mountain-Great Plains boundary of Montana , dropping off subgroups as people migrated. Goddard also points out that there is clear evidence for pre-historical contact between Eastern Algonquian and Cree-Montagnais, as well as between Cheyenne and Arapaho–Gros Ventre. There has long been especially extensive back-and-forth influence between Cree and Ojibwe. It has been suggested that

920-582: The Sakonnet River , Mount Hope Bay , and the southern, tidal part of the Taunton River . The bay opens on Rhode Island Sound and the Atlantic Ocean; Block Island lies less than 20 miles (32 km) southwest of its opening. "Narragansett" is derived from the southern New England Algonquian word Naiaganset meaning "(people) of the small point of land". The watershed of Narragansett Bay has seven river sub-drainage basins , including

966-542: The Taunton , Pawtuxet , and Blackstone Rivers , and they provide freshwater input at approximately 2.1 million U.S. gallons (7.9 × 10 ^  L) per day. River water inflow has a seasonal variability, with the highest flow in the spring and the minimum flow in early fall. The bay is a ria estuary (a drowned river valley) which is composed of the Sakonnet River valley, the East Passage river valley, and

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1012-430: The "Eastern Great Lakes" languages – what Goddard has called "Core Central", e.g., Ojibwe–Potawatomi, Shawnee, Sauk–Fox–Kickapoo, and Miami-Illinois (but not Cree–Montagnais or Menominee) – may also constitute their own genetic grouping within Algonquian. They share certain intriguing lexical and phonological innovations. However, this theory has not yet been fully fleshed out and is still considered conjectural. Algonquian

1058-710: The Algonquian languages is their direct-inverse (also known as hierarchical ) morphosyntactic alignment , distinguishing between an unmarked voice where the subject outranks the object in a person hierarchy and a marked voice where the opposite relation obtains. Because Algonquian languages were some of the first with which Europeans came into contact in North America, the language family has given many words to English . Many eastern and midwestern U.S. states have names of Algonquian origin ( Massachusetts , Connecticut , Illinois , Michigan , Wisconsin , etc.), as do many cities: Milwaukee , Chicago , et al. Ottawa ,

1104-567: The North to South nutrient concentration gradient in the bay (24). Near the Providence River, biomass levels are highest in the summer and lowest in the winter. In the east and west passages there are peaks in the spring and fall. Annual blooms have shrunk over the last decade (2006 onward) as the amount of nitrogen (an important nutrient) supply to the bay has decreased by more than 50% due to wastewater treatment facilities switching to

1150-408: The Providence River does show some vertical stratification. Narragansett Bay circulation is made up of forces provided by the winds, tides, and changes in water density within the watershed. Its circulation is the result of the flow of fresh water at the head interacting with salt water at the point where the bay meets the open ocean. Residence time of water due to the circulation of Narragansett Bay

1196-511: The West Passage river valley. The bathymetry varies greatly among the three passages, with the average depths of the East, West, and Sakonnet River passages being 121 feet (37 m), 33 feet (10 m), and 25 feet (7.6 m) respectively. Narragansett Bay is a ria that consists of a series of flooded river valleys formed of dropped crustal blocks in a horst and graben system that

1242-440: The bay in his ship La Dauphine in 1524 after visiting New York Bay . Verrazzano called the bay Refugio , the "Refuge". It has several entrances, however, and historians can only speculate as to the exact route of his voyage and the location where he laid anchor, along with a corresponding uncertainty over which tribe made contact with him. Verrazzano reported that he found clearings and open forests suitable for travel "even by

1288-529: The bay indicate a range of mixed to stratified conditions and the amount of time it takes for the total volume of fresh water in the bay to be equaled by the fresh water input (flushing time) varies from 40 days to 10 days, depending on freshwater input. Dissolved oxygen levels in Narragansett Bay are seasonal with lower levels in the summer and higher levels in the winter. This is due to warmer temperatures and higher biological demand for oxygen in

1334-532: The bay was probably in the early 16th century. At the time, the area surrounding the bay was inhabited by two different Indian tribes: the Narragansetts occupied the west side of the bay, and the Wampanoags lived on the east side, occupying the land east to Cape Cod . It is accepted by most historians that first contact by Europeans was made by Giovanni da Verrazzano , an Italian explorer who entered

1380-831: The capture and burning of the British customs schooner Gaspee . The American victory contributed to the eventual start of the war at the Battles of Lexington and Concord in Massachusetts three years later. The event is celebrated in Pawtuxet Village as the Gaspee Days Celebration in June which includes burning the ship in effigy. Roger Williams and other early colonists named the islands Prudence , Patience , Hope , Despair , and Hog . To remember

1426-491: The discourse. There are personal pronouns which distinguish three persons, two numbers (singular and plural), inclusive and exclusive first person plural , and proximate and obviative third persons. Verbs are divided into four classes: transitive verbs with an animate object (abbreviated "TA"), transitive verbs with an inanimate object ("TI"), intransitive verbs with an animate subject ("AI"), and intransitive verbs with an inanimate subject ("II"). A very notable feature of

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1472-555: The entire island. The U.S. Census Bureau reported a land area of 24.46 km (9.44 sq mi) and a population of 5,622 in 2000. A tombolo connects the southern part of Conanicut to an extension of the island to the southwest. Conanicut Island was a seasonal home to the Narragansett tribe of American Indians. The largest Indian cemetery in New England is located on the island, and artifacts have been recovered from

1518-400: The many rivers that feed into the watershed, and human-made sources such as water treatment plants. Fresh and saltwater mixing results in a salinity range in the bay of 24 parts per thousand (ppt) in the upper Providence River area to 32 ppt at the mouth of the bay. The bay's currents and circulation patterns greatly influence the sediment deposits within the region. The majority of

1564-651: The names, colonial school children often recited the poem: "Patience, Prudence, Hope, and Despair. And the little Hog over there." Narragansett Bay is divided by Conanicut Island into east and west passages. Its depth averages approximately 9.0 meters throughout the bay, but it is shallower in the west passage and deeper in the east. Narragansett Bay receives freshwater input from several sources, including rivers (approximately 80%), direct precipitation (13%), wastewater treatment facilities (9%), and unknown amounts from ground-water and combined sewer overflows (CSOs). The freshwater input varies greatly from season to season as it

1610-581: The north side of Rhode Island Sound covering 147 square miles (380 km ), 120.5 square miles (312 km ) of which is in Rhode Island . The bay forms New England 's largest estuary, which functions as an expansive natural harbor and includes a small archipelago. Small parts of the bay extend into Massachusetts . There are more than 30 islands in the bay; the three largest ones are Aquidneck Island , Conanicut Island , and Prudence Island . Bodies of water that are part of Narragansett Bay include

1656-440: The observed levels of divergence within the family, whereby the most divergent languages are found furthest west (since they constitute the earliest branchings during eastern migration), and the shallowest subgroupings are found furthest to the east (Eastern Algonquian, and arguably Core Central). This general west-to-east order is compatible with the proposal from J.P. Denny (1991) that Proto-Algonquian people may have moved east from

1702-459: The region experiences two high and low tides daily. The tides range in height from 3.6 feet (1.1 m) at the bay's mouth and 4.6 feet (1.4 m) at its head. Water depth varies about 4 feet (1.2 m) between high and low tide. The lunar, semi-diurnal M2 tide occurs at a period of 12.42 hours, with two tides occurring in the watershed every 24 hours and 50 minutes. The watershed's neap and spring tides occur every 14.8 days. In Narragansett bay,

1748-720: The same time, the Dutch established a trading post approximately 12 miles (20 km) to the southwest which was under the authority of New Amsterdam in New York Bay. In 1643, Williams traveled to England and was granted a charter for the Colony of Rhode Island and Providence Plantations . The Gaspee Affair was an important naval event which moved the Thirteen Colonies toward the American Revolution . It occurred in Narragansett Bay in 1772 and involved

1794-467: The sediments within the bay are fine-grained material such as detritus, clay-silt, and sand-silt-clay. Scientists have been able to identify 11 types of sediment that range from coarse gravels to fine silts. the bay's currents deposit fine materials through the harbors of the lower and middle sections of the bay, and the coarse, heavy materials are deposited in the lower areas of the bay where the water velocities are higher. The first visit by Europeans to

1840-478: The separate main articles for each of the three divisions. Eastern Algonquian is a true genetic subgrouping. The Plains Algonquian and the Central Algonquian groups are not genetic groupings but rather areal groupings. Although these areal groups often do share linguistic features, these commonalities are usually attributed to language contact . Paul Proulx has argued that this traditional view

1886-572: The summer and the opposite in the winter. Narragansett Bay is also subject to periodic summer hypoxic events in the Northern half of the bay, nearing anoxic conditions in some parts. Phytoplankton forms the base of the food chain for many of the bay's marine animals. General trends in phytoplankton biomass across the bay are characterized by highest levels in the Providence River and lowest levels in Rhode Island Sound , correlating with

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1932-406: The tides show a distinct double-peak flood during high tide and single peak ebb during low tide. The movement of water within a system is its circulation . Estuaries are given a classification depending on the pattern of their circulations. The circulation classification can be well-mixed, partially mixed, salt wedge, or Fjord-type. For Narragansett, the circulation is mostly well-mixed; however,

1978-402: The watershed are measured at Providence, Fall River, Quonset Point, Conimicut Light , Prudence Island, and Newport. In shallow water, sound waves are used to measure water height by precisely measuring their travel time. In deeper water, tides are measured with pressure-sensing tide gauges that are placed on the ocean floor to measure water height. The bay's tides are semi-diurnal, meaning that

2024-419: The winter, winds come from the northwest, helping move water towards the bay's mouth; in the summer, they are out of the southwest and move water towards the head of the bay. Wind-driven waves of over 4.25 feet (1.30 m) also help mix surface waters. Density-driven forces are the third factor affecting circulation. Fresh water inflow comes from natural sources such as atmospheric precipitation and inflow from

2070-598: Was one of the Narragansett sachems who gave consent. They referred to the island in his honor, and the Jamestown seal today includes the figure of a sheep. Conanicut Island was a part of the island territory included in a commission which the Council of State of England granted to William Coddington in 1651 separating them from the mainland and making him indefinite governor of the islands (later revoked). In 1657,

2116-444: Was spoken. This subfamily of around 30 languages is divided into three groups according to geography: Plains , Central , and Eastern Algonquian . Of the three, only Eastern Algonquian constitutes a true genetic subgroup. The languages are listed following the classifications of Goddard (1996) and Mithun (1999). Extinct languages are marked with †, and endangered languages are noted as such. For dialects and subdialects, consult

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