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Staten Island is one of the five boroughs of New York
City. Situated on an island of the same name that is the
most geographically separate of the city's boroughs,
Staten Island is the least populated of the five
boroughs.
The Borough of Staten Island is coterminous with
Richmond County, the southernmost county in the state of
New York. Until 1975 the borough was officially named
the Borough of Richmond.
With a population of just over 460,000, Staten Island is
often called "the forgotten borough," as it is much less
well-known than its four sisters, The Bronx, Queens,
Manhattan, and Brooklyn.
By far the least populated, most ethnically homogeneous
and most remote borough of New York City, Staten Island
is primarily suburban. Much of the central and southern
sections of the island were once dominated by dairy and
poultry farms, some of which were still in existence as
recently as the early 1960s. Some areas have an urban
feel comparable to the areas of Eastern Queens and
Northern Bronx. The borough's steady rise in population
since the opening of the Verrazano-Narrows Bridge has
added to a sharp increase in traffic that plagues the
island and is a cause of frequent road repairs and
accidents.
Staten Island is also known for the Fresh Kills
Landfill, the repository of garbage from all of New York
City for 53 years. The landfill was closed in 2001, and
there is an ongoing attempt to decontaminate the land
and rehabilitate it for recreational uses.
History of
Staten Island
Staaten Eylandt
Richmond County
Consolidation with New York City
History of Staten
Island
The bedrock of the island is a diabase sill formed
during the volcanic eruptions that created much of the
bedrock of northern New Jersey, including the New Jersey
Palisades, approximately 200 million years ago. As an
island, Staten Island was formed in the wake of the last
ice age. In the late Pleistocene between 20,000 and
14,000 years ago, the ice sheet that covered
northeastern North America reached to as far south as
present day New York City, to a depth of approximately
the same height as the Empire State Building. At one
point, during its maximum reach, the ice sheet precisely
ended at the center of present day Staten Island,
forming a terminal moraine on the existing diabase sill.
The central moraine of the island is sometimes called
the Serpentine ridge because it contains large amounts
of that particular mineral.
At the retreat of the ice sheet, Staten Island and Long
Island were not yet separated by The Narrows, which had
not yet formed. Geologists reckoning of the course of
the Hudson River have placed it alternatively through
the present course of the Raritan River, south of the
island, as well through present-day Flushing Bay and
Jamaica Bay.
As in much of North America, human habitation appeared
in the island fairly rapidly after the retreat of the
ice sheet. Archaeologists have recovered tool evidence
of Clovis culture activity dating from approximately
14,000 years ago. The island was probably abandoned
later, possibly because of the extinction of large
mammals on the island. Evidence of the first permanent
aboriginal American settlements and agriculture date
from about 5,000 years ago (Jackson, 1995).
In the Sixteenth Century, the island was part of a
larger area known as Lenapehoking that was inhabited by
the Lenape, an Algonquian aboriginal American people
also called the "Delaware". The band that occupied the
southern part of the island was called the Raritans. To
the Lenape, the island was called "Aquehonga Manacknong"
and "Eghquaons" (Jackson, 1995). The island was laced
with foot trails, one of which followed the south side
of the ridge near the course of present day Richmond
Road and Amboy Road. The Lenape did not live in fixed
encampments, but moved seasonally, using slash and burn
agriculture. The staples of their diet included
shellfish, including the oysters that are native to both
Upper New York Bay and Lower New York Bay.

Staaten Eylandt
The first recorded European contact with the island was
in 1524 by Giovanni da Verrazzano who sailed through the
Narrows. In 1609, Henry Hudson established Dutch trade
in the area and named the island Staaten Eylandt after
the Staten-Generaal, the Dutch parliament.
Although the first Dutch settlement of the New
Netherlands colony was made on Manhattan in 1620,
Staaten Eylandt remained uncolonized by the Dutch for
many decades. From 1639 to 1655, the Dutch made three
separate attempts to establish a permanent settlement on
the island, but each time the settlement was destroyed
in the conflicts between the Dutch and the local tribes.
In 1661, the first permanent Dutch settlement was
established at Oude Dorp (Dutch for "Old Village"), just
south of the Narrows near South Beach, by a small group
of Dutch Walloon and Huguenot families.

Richmond County
At the end of the Second Anglo-Dutch War in 1667, the
New Netherlands colony was ceded to England in the
Treaty of Breda, and what was now anglicized as Staten
Island became part of the new English colony of New
York.
In 1670, the Native Americans ceded all claims to Staten
Island to the English in a deed to Gov. Francis
Lovelace. In 1671, in order to encourage an expansion of
the Dutch settlements, the English resurveyed Oude Dorp
(which became known as Old Town) and expanded the lots
along the shore to the south. These lots were settled
primarily by Dutch and became known as Nieuwe Dorp
(meaning "New Village"), which later became anglicized
as New Dorp.
In 1683, the colony of New York was divided into ten
counties. As part of this process, Staten Island, as
well as several minor neighboring islands, were
designated as Richmond County. The name derives from the
title of an illegitimate son of King Charles II.
In 1687-1688, the English divided the island into four
administrative divisions based on natural features,
called the North, South, and West divisions, as well as
the 5100 acre (21 kmē) manorial estate of colonial
governor Thomas Dongan in the central hills known as the
"Lordship or Manner of Cassiltown." These divisions
would later evolve into the four townships Northfield,
Southfield, Westfield and Castleton.
Land patents in rectangular blocks of eighty acres
(320,000 mē) were granted, with the most desirable lands
being along the coastline and inland waterways. By 1708,
the entire island had been divided up through this
fashion into 166 small farms and two large manorial
estates, the Dongan estate as well as a 1600 acre (6.5
kmē) parcel on the southwestern tip of the island
belonging to Christopher Billop (Jackson, 1995).
In 1729, a county seat was established at the village of
Richmond Town, located at the headwaters of the Fresh
Kills near the center of the island.
The island played a significant role in the American
Revolutionary War. In the summer of 1776, the British
forces under William Howe evacuated Boston and prepared
to attack New York City. Howe used the strategic
location of Staten Island as a staging ground for the
attack. Howe established his headquarters in New Dorp at
the Rose and Crown tavern near the junction of present
New Dorp Lane and Amboy Road. It is here that the
representatives of the British government reportedly
received their first notification of the Declaration of
Independence.
The following month, in August 1776, the British forces
crossed the Narrows to Brooklyn and routed the American
forces under George Washington at the Battle of Long
Island, resulting in the British capture of New York.
Three weeks later, on September 11, 1776, the British
received a delegation of Americans consisting of
Benjamin Franklin, Edward Rutledge, and John Adams at
the Conference House on the southwestern tip of the
island (known today as Tottenville) on the former estate
of Christopher Billop. The Americans refused the peace
offer from the British in exchange for the withdrawal of
the Declaration of Independence, however, and the
conference ended without an agreement.
British forces remained on Staten Island throughout the
war. Although local sentiment was predominantly
Loyalist, the islanders found the demands of supporting
the troops to be onerous. Many buildings and churches
were destroyed, and the military demand for resources
resulted in an extensive deforestation of the island by
the end of the war. The British again used the island as
a staging ground for their final evacuation of New York
City on December 5, 1783. After the war, the largest
Loyalist landowners fled to Canada and their estates
were subdivided and sold.
On July 4, 1827, the end of slavery in New York state
was celebrated at Swan Hotel, West Brighton. Rooms at
the hotel were reserved months in advance as local
abolitionists and prominent free blacks prepared for the
festivities. Speeches, pageants, picnics, and fireworks
marked the celebration, which lasted for two days.
In 1860, parts of Castleton and Southfield were made
into a new town, Middletown. The Village of New Brighton
in the town of Castleton was incorporated in 1866, and
in 1872 the Village of New Brighton annexed all the
remainder of the Town of Castleton and became
coterminous with the town.

Consolidation with New York City
All these towns and the villages within them were
abolished in 1898 when the City of Greater New York was
consolidated, with Richmond as one of its five boroughs.
Except for the areas along the harbor, however, the
borough remained relatively underdeveloped until the
building of the Verrazano Narrows Bridge in 1964, which
is considered the watershed event in the history of the
borough, since it opened up the island to explosive
suburban development by giving it direct road access to
Brooklyn. The Verrazano, along with the other three
major Staten Island bridges, created a new way for
commuters and travelers to reach Brooklyn, Manhattan and
areas further east on Long Island, by car from New
Jersey, and the network of highways running between the
bridges has effectively carved up many of the borough's
old neighborhoods. This road expansion was planned
initially by Robert Moses.
Some of the island's open space and historic areas were
incorporated in 1972 into Gateway National Recreation
Area, part of the National Park System. The Staten
Island Unit of Gateway NRA is joined by the Jamaica Bay
Unit in Brooklyn and Queens and the Sandy Hook Unit in
New Jersey. The Staten Island Unit is comprised of Great
Kills Park, Miller Field, Fort Wadsworth, as well as
Hoffman Island and Swinburne Island.
For the last half of the 20th Century, Staten Island was
arguably best known as the site of the Fresh Kills
Landfill, the primary destination for garbage from the
five boroughs of New York City and the largest single
source of methane pollution in the world. The landfill
was closed in early 2001 but was temporarily reopened
later that year to receive the ruins of the World Trade
Center after the September 11, 2001 terrorist attacks.
Staten Island bore much of the loss of life in September
11, 2001 attacks, nearly 300 residents, with a large
numbers of firemen and World Trade Center workers living
on Staten Island. The Fresh Kills landfill is chosen to
hold the debris from the towers and serves as a crime
lab for police investigators searching for human
remains.
Throughout the 1980s, a movement which had as its goal
the secession of Staten Island from the city steadily
grew in popularity, reaching its peak during the mayoral
term of David Dinkins. The movement largely evaporated
with Rudolph Giuliani's election as mayor in 1993,
although some pro-secession sentiment remains.
In the 1980s, the United States Navy had a base on
Staten Island, Naval Station New York. Composed of two
sections, a home port in Stapleton, and a larger section
around Ft. Wadsworth, where the Verrazano Narrows Bridge
enters the island. A few frigates, destroyers, and at
least one cruiser were based there. It was closed in
1994 through the BRAC process. A hostile political
climate and the expense of basing personnel there led to
closure.

(Article Source:
Wikipedia, the free encyclopedia)
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