JEWISH FAMILY PHOTO LONG ISLAND NEW YORK 1950

JEWISH FAMILY PHOTO LONG ISLAND NEW YORK 1950. Size:13x8.5 cm.

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Long Island is a largely urbanized and densely populated island in the southeastern geographical area of the U.S. state of New York, part of the New York metropolitan area. It begins at New York Harbor approximately 0.35 miles (0.56 km) east of Manhattan Island and extends eastward over 100 miles (160 km) into the Atlantic Ocean. The island comprises four counties; Kings and Queens counties (the New York City boroughs of Brooklyn and Queens, respectively) and Nassau County share the western third of the island, while Suffolk County occupies the eastern two thirds. More than half of New York City's residents live on Long Island, in Brooklyn and in Queens.[2] However, people in the New York metropolitan area colloquially use the term Long Island (or the Island) to refer exclusively to Nassau and Suffolk counties,[3] and conversely, employ the term the City to mean Manhattan alone.[4] While the Nassau-plus-Suffolk definition of Long Island does not have any legal existence, it is recognized as a "region" by the state of New York.[5] Although geographically an island, the Supreme Court of the United States has held that given the island's extensive ties to the mainland, it should be treated like a peninsula, allowing the state to have jurisdiction within its maritime boundaries.[6] Broadly speaking, "Long Island" may refer both to the main island and the surrounding outer barrier islands. To its west, Long Island is separated from Manhattan and the Bronx by the East River tidal estuary. North of the island is Long Island Sound, across which lie Westchester County, New York and the state of Connecticut. Across the Block Island Sound to the northeast is the state of Rhode Island. Block Island—which is part of Rhode Island—and numerous smaller islands extend further into the Atlantic. To the extreme southwest, Long Island is separated from Staten Island and the state of New Jersey by Upper New York Bay, the Narrows, and Lower New York Bay. The longest and the largest island in the contiguous United States,[7] Long Island extends 118 miles (190 km) eastward from New York Harbor to Montauk Point, with a maximum north-to-south distance of 23 miles (37 km) between Long Island Sound and the Atlantic coast.[8] With a land area of 1,401 square miles (3,630 km2), Long Island is the 11th-largest island in the United States and the 149th-largest island in the world—larger than the 1,214 square miles (3,140 km2) of the smallest U.S. state, Rhode Island.[9] With an enumerated population of 8,063,232 residents as of the 2020 U.S. Census, constituting 40% of New York State's population,[10][11][12][13][14] Long Island is the most populated island in any U.S. state or territory, the third-most populous island in the Americas (after only Hispaniola and Cuba), and the 18th-most populous island in the world (ahead of Ireland, Jamaica, and Hokkaidō). Its population density is 5,859.5 inhabitants per square mile (2,262.4/km2). If Long Island geographically constituted an independent metropolitan statistical area, it would rank fourth most populous in the United States; while if it were a U.S. state, Long Island would rank thirteenth in population and first in population density. Long Island is culturally and ethnically diverse, featuring some of the wealthiest and most expensive neighborhoods in the world near the shorelines as well as working-class areas in all four counties. As a hub of commercial aviation, Long Island is home to two of the New York City metropolitan area's three busiest airports, JFK International Airport and LaGuardia Airport,[a] in addition to Islip MacArthur Airport; as well as two major air traffic control radar facilities, the New York TRACON and the New York ARTCC. Nine bridges and thirteen navigable tunnels (road and railroad tunnels but not metropolitan water tunnels) connect Brooklyn and Queens to the three other boroughs of New York City. Ferries connect Suffolk County northward across Long Island Sound to the state of Connecticut. The Long Island Rail Road is the busiest commuter railroad in North America and operates continually.[15] Nassau County high school students often feature prominently as winners of the Intel International Science and Engineering Fair and similar STEM-based academic awards.[16] Biotechnology companies and scientific research play a significant role in Long Island's economy,[17] including research facilities at Brookhaven National Laboratory, Cold Spring Harbor Laboratory, Stony Brook University, New York Institute of Technology, Plum Island Animal Disease Center, the New York University Tandon School of Engineering, the City University of New York, and Hofstra Northwell School of Medicine. Contents 1 History 1.1 Early history 1.2 18th and 19th centuries 1.3 20th century 1.4 21st century 2 Geography 2.1 Geology 2.2 Countyscapes 2.3 Climate 2.4 Additional islands 3 Demographics 4 Economy 5 Government and politics 5.1 Law enforcement 5.2 Statehood proposals 6 Education 6.1 Primary and secondary education 6.2 Colleges and universities 7 Culture 7.1 Music 7.2 Cuisine 7.3 Sports 7.3.1 Major league sports 7.3.2 Minor league and college sports 7.3.3 Other sports 7.3.4 Notable sportspeople and teams 8 Transportation 8.1 Public transportation 8.1.1 Rail 8.1.2 Bus 8.2 Roads 8.2.1 Ground transportation 9 See also 10 Notes 11 References 12 External links History Main article: History of Long Island Early history By the year 1643, there were 14 indigenous tribes living on Long Island: Canarsee, Rockaway, Matinecock, Merrick, Massapequa, Nissequoge, Secatoag, Seatauket, Patchoag, Unquechogue, has Corchaug, Shinnecock, Manhasset and Montaukett. Long Island Native American settlements The tribes used canoes as a source of transportation, and since they lived by the shores, they went fishing.[18][better source needed] The fishermen used bows, arrows, and hooks to catch seafood such as crabs, scallops, and lobster.[19][better source needed] The farmers used fish for fertilizer and planted vegetables such as corn, beans, and squash, which were popular among the indigenous people. They were exceptional farmers; they had a great understanding of how the weather and soil affected the crops.[20][better source needed] Many of them hunted animals, such as deer, raccoon, and turkey in the forest. Three Lenapes The government that they set up was a participatory democracy and there was an alliance between the tribes. Each tribe had their own territory and chief that was respected by other tribes.[21] Prior to European contact, the Lenape people (named the Delaware by Europeans) inhabited the western end of Long Island, and spoke the Munsee dialect of Lenape, part of the Algonquian language family. The Lenape (who were part of the Shinnecock Tribe) practiced record keeping and used wooden tablets, trees, and stones to keep record. They also used wampum belts to write down important messages.[22] They also used their wampum to trade with the Europeans.[19] The Lenape people, in specific, were seen as peacemakers by other indigenous tribes, although they would defend themselves if necessary. The Europeans admired their friendliness and their skills in mediation.[23] Giovanni da Verrazzano was the first European to record an encounter with the Lenapes, after entering what is now New York Bay in 1524. The island's eastern portion was inhabited by speakers of the Mohegan-Montauk-Narragansett language group of Algonquian languages; they were part of the Pequot and Narragansett peoples inhabiting the area that now includes Connecticut and Rhode Island. In 1609, the English navigator Henry Hudson explored the harbor and purportedly landed at Coney Island. Dutch explorer Adriaen Block followed in 1615, and is credited as the first European to determine that both Manhattan and Long Island are islands. In 1636, Charles I of England, a Stuart, rewarded Scottish courtier, diplomat, and colonial governor William Alexander's service to the Crown by creating him Lord Alexander of Tullibody and Viscount of Stirling. On 22 April of that year Charles told the Plymouth Colony, which had laid claim to Long Island but had not settled it, to cede it to Alexander. When his agent James Farret arrived in New Amsterdam in 1637 to present his claim of English sovereignty he was arrested and sent to prison in Holland (but escaped). In 1639, Lion Gardiner purchased an islet off of today's East Hampton, Gardiners Island, from the Montaukett, received Farret's approval of the transaction on behalf of Alexander (by then the 1st Earl of Stirling and Viscount Canada), and subsequently received a royal patent establishing him as Lord of the Manor over it. In 1640, English colonists attempted to settle at Cow Bay at what today is Port Washington. After an alert by Native leader Penhawitz, the colonists were arrested by the Dutch but released after saying they were mistaken about the title.[24] Through Farret (who personally received Shelter Island and Robins Island), Alexander in turn sold most of the eastern island to the New Haven Colony and Connecticut Colony.[25] In spite of these shifting claims to title and absentee land sales, European settlers continued to purchase land directly from the Indigenous people. In 1655 they split the acquired land amongst themselves and continued to search the island for more land for settlement. Other parts of indigenous land were bought, areas that are now known as Brookhaven, Bellport, and South haven. These purchases occurred on June 10, 1664, the exchange was four coats and what is now[when?] $16.25.[18] The white settlers and the indigenous people lived amicably together for a while. During King Philip's War in 1675, the English governor of New York ordered all canoes that were east of Hell Gate to be confiscated. This was done to prevent the Indigenous people from helping their native allies on the mainland, who were attacking settlers there.[26] After the Dutch began to move into Manhattan many of the indigenous people moved to Pennsylvania and Delaware. Many of them who stayed behind died from smallpox as North Americans had never been exposed to the disease before, resulting in large scale deaths due to lack of antibodies and natural resistance which Eurasian peoples gained.[27] Native American land deeds recorded by the Dutch from 1636 state that the Indians referred to Long Island as Sewanhaka (Sewanhacky and Sewanhacking were other spellings in the transliteration of Lenape).[28] Sewan was one of the terms for wampum (commemorative stringed shell beads, for a while also used as currency by colonists in trades with the Lenape), and is also translated as "loose" or "scattered", which may refer either to the wampum or to Long Island.[28] The name "'t Lange Eylandt alias Matouwacs" appears in Dutch maps from the 1650s.[29][30] Later, the English referred to the land as "Nassau Island",[31] after the Dutch Prince William of Nassau, Prince of Orange (who later also ruled as King William III of England). It is unclear when the name "Nassau Island" was discontinued. Another indigenous name from colonial time, Paumanok, comes from the Native American name for Long Island and means "the island that pays tribute."[32] The very first European settlements on Long Island were by settlers from England and its colonies in present-day New England. Lion Gardiner settled nearby Gardiners Island. The first settlement on the geographic Long Island itself was on October 21, 1640, when Southold was established by the Rev. John Youngs and settlers from New Haven, Connecticut. Peter Hallock, one of the settlers, drew the long straw and was granted the honor to step ashore first. He is considered the first New World settler on Long Island. Southampton was settled in the same year. Hempstead followed in 1644, East Hampton in 1648, Huntington in 1653, Brookhaven in 1655, and Smithtown in 1665. The Old House in Cutchogue, built 1699. While the eastern region of Long Island was first settled by the English, the western portion of Long Island was settled by the Dutch; until 1664, the jurisdiction of Long Island was split between the Dutch and English, roughly at the present border between Nassau County and Suffolk County. The Dutch founded six towns in present-day Brooklyn beginning in 1645. These included: Brooklyn, Gravesend, Flatlands, Flatbush, New Utrecht, and Bushwick. The Dutch had granted an English settlement in Hempstead, New York (now in Nassau County) in 1644, but after a boundary dispute they drove out English settlers from the Oyster Bay area. However, in 1664, the English returned to take over the Dutch colony of New Netherland, including Long Island. The 1664 land patent granted to the Duke of York included all islands in Long Island Sound. The Duke of York held a grudge against Connecticut, as New Haven had hidden three of the judges (John Dixwell, Edward Whalley and William Goffe[33]) who sentenced the Duke's father, King Charles I, to death in 1649. Settlers throughout Suffolk County pressed to stay part of Connecticut, but Governor Sir Edmund Andros threatened to eliminate the settlers' rights to land if they did not yield, which they did by 1676.[34] All of Long Island (as well as the islands between it and Connecticut) became part of the Province of New York within the Shire of York. Present-day Suffolk County was designated as the East Riding (of Yorkshire), present-day Brooklyn was part of the West Riding, and present-day Queens and Nassau were part of the larger North Riding. In 1683, Yorkshire was dissolved and the three original counties on Long Island were established: Kings, Queens, and Suffolk. 18th and 19th centuries Early in the American Revolutionary War, the island was captured by the British from General George Washington in the Battle of Long Island, a decisive battle after which Washington narrowly evacuated his troops from Brooklyn Heights under a dense fog. After the British victory on Long Island, many Patriots fled, leaving mostly Loyalists behind. The island was a British stronghold until the end of the war in 1783.[35] General Washington based his espionage activities on Long Island, due to the western part of the island's proximity to the British military headquarters in New York City. The Culper Spy Ring included agents operating between Setauket and Manhattan. This ring alerted Washington to valuable British secrets, including the treason of Benedict Arnold and a plan to use counterfeiting to induce economic sabotage.[citation needed] Long Island's colonists served both Loyalist and Patriot causes, with many prominent families divided among both sides. During the occupation British troops used a number of civilian structures for defense and demanded to be quartered in the homes of civilians. A number of structures from this era remain. Among these are Raynham Hall, the Oyster Bay home of patriot spy Robert Townsend, and the Caroline Church in Setauket, which contains bullet holes from a skirmish known as the Battle of Setauket. Also in existence is a reconstruction of Brooklyn's Old Stone House, on the site of the Maryland 400's celebrated last stand during the Battle of Long Island.[36] The Brooklyn Bridge, the first of multiple crossings constructed across the East River, connects Long Island with Manhattan Island (background). Oheka Castle, a Gold Coast estate, is the second-largest private residence in the country In the 19th century, Long Island was still mainly rural and devoted to agriculture. The predecessor to the Long Island Rail Road (LIRR) began service in 1836 from the South Ferry in Brooklyn, through the remainder of Brooklyn, to Jamaica in Queens. The line was completed to the east end of Long Island in 1844 (as part of a plan for transportation to Boston). Competing railroads (soon absorbed by the LIRR) were built along the south shore to accommodate travellers from those more populated areas. For the century from 1830 until 1930, total population roughly doubled every twenty years, with more dense development in areas near Manhattan. Several cities were incorporated, such as the 'City of Brooklyn' in Kings County, and Long Island City in Queens.[citation needed] Until the 1883 completion of the Brooklyn Bridge, the only means of travel between Long Island and the rest of the United States was by boat or ship. As other bridges and tunnels were constructed, areas of the island began to be developed as residential suburbs, first around the railroads that offered commuting into the city. On January 1, 1898, Kings County and portions of Queens were consolidated into the 'City of Greater New York', abolishing all cities and towns within them. The easternmost 280 square miles (730 km2) of Queens County, which were not part of the consolidation plan,[37][38][39][40][41][42] separated from Queens in 1899 to form Nassau County. At the close of the 19th century, wealthy industrialists who made vast fortunes during the Gilded Age began to construct large "baronial" country estates in Nassau County communities along the North Shore of Long Island, favoring the many properties with water views. Proximity to Manhattan attracted such men as J. P. Morgan, William K. Vanderbilt, and Charles Pratt, whose estates led to this area being nicknamed the Gold Coast. This period and the area was immortalized in fiction, such as F. Scott Fitzgerald's The Great Gatsby, which has also been adapted in films. 20th century Charles Lindbergh lifted off from Roosevelt Field with his Spirit of Saint Louis for his historic 1927 solo flight to Europe, one of the events that helped to establish Long Island as an early center of aviation during the 20th century. Other famous aviators such as Wiley Post originated notable flights from Floyd Bennett Field in Brooklyn, which became the first major airport serving New York City before it was superseded by the opening of La Guardia Airport in 1939. Long Island was also the site of Mitchel Air Force Base and was a major center of military aircraft production by companies such as Grumman and Fairchild Aircraft during World War II and for some decades afterward. Aircraft production on Long Island extended all the way into the Space Age – Grumman was one of the major contractors that helped to build the early lunar flight and space shuttle vehicles. Although the aircraft companies eventually ended their Long Island operations and the early airports were all later closed – Roosevelt Field, for instance, became the site of a major shopping mall – the Cradle of Aviation Museum on the site of the former Mitchel Field documents the Island's key role in the history of aviation. From the 1920s to the 1940s, Long Island began the transformation from backwoods and farms as developers created numerous suburbs. Numerous branches of the LIRR already enabled commuting from the suburbs to Manhattan. Robert Moses engineered various automobile parkway projects to span the island, and developed beaches and state parks for the enjoyment of residents and visitors from the city. Gradually, development also followed these parkways, with various communities springing up along the more traveled routes. After World War II, suburban development increased with incentives under the G.I. Bill, and Long Island's population skyrocketed, mostly in Nassau County and western Suffolk County. Second and third-generation children of immigrants moved out to eastern Long Island to settle in new housing developments built during the post-war boom. Levittown became noted as a suburb, where housing construction was simplified to be produced on a large scale. These provided opportunities for white World War II military veterans returning home to buy houses and start a family. In his 1966 book, My Private America (Moja prywatna Ameryka), Kazimierz Wierzyński, a Polish poet who could not go back to Poland after World War II, describes Polish farmers living there, as "walking novels".[43] 21st century By the start of the 21st century, a number of Long Island communities had converted their assets from industrial uses to post-industrial roles. Brooklyn reversed decades of population decline and factory closings to resurface as a globally renowned cultural and intellectual hotbed. Gentrification has affected much of Brooklyn and a portion of Queens, relocating a sizeable swath of New York City's population. On eastern Long Island, such villages as Port Jefferson, Patchogue, and Riverhead have been changed from inactive shipbuilding and mill towns into tourist-centric commercial centers with cultural attractions. The descendants of late 19th- and early 20th-century immigrants from southern and eastern Europe, and black migrants from the South, have been followed by more recent immigrants from Asia and Latin America. Long Island has many ethnic Irish, Jews, and Italians, as well as an increasing numbers of Asians and Hispanics, reflecting later migrations. Geography Main article: Geography of Long Island Montauk Point is at Long Island's rural eastern tip The four counties of Long Island include two independent counties (Nassau and Suffolk) and two New York City boroughs (Brooklyn and Queens) Satellite imagery showing the New York metropolitan area at night. Long Island is highly developed and densely populated, extending approximately 120 miles (190 km) eastward from the central core of Manhattan The westernmost end of Long Island contains the New York City boroughs of Brooklyn (Kings County) and Queens (Queens County). The central and eastern portions contain the suburban Nassau and Suffolk counties. However, colloquial usage of the term "Long Island" usually refers only to Nassau and Suffolk counties. For example, the Federal Reserve Bank of New York has a district named "Long Island (Nassau-Suffolk Metro Division)."[44] At least as late as 1911, locations in Queens were still commonly referred to as being on Long Island.[45] Some institutions in the New York City section of the island use the island's names, like Long Island University and Long Island Jewish Medical Center. In 1985, the United States Supreme Court ruled in United States v. Maine that Long Island is integrally related to the mainland enough that Long Island Sound and the western part of Block Island Sound constitute a "juridicial bay" for the purpose of determining maritime state boundaries.[46] In the popular media this has been often misinterpreted as a ruling that Long Island is legally not an island.[47][48][49] The United States Board on Geographic Names still considers Long Island an island, because it is surrounded by water.[50] There are few tall buildings on Long Island. Nassau County is more densely developed than Suffolk County. While affluent overall, Nassau County has pockets of more pronounced wealth with estates covering greater acreage within the Gold Coast of the North Shore and the Five Towns area on the South Shore. South Shore communities are built along protected wetlands of the island and contain white sandy beaches of Outer Barrier Islands fronting on the Atlantic Ocean. Dutch and English settlers from the time before the American Revolutionary War, as well as communities of Native Americans, populated the island. The 19th century saw the infusion of the wealthiest Americans in the so-called Gold Coast of the North Shore, where wealthy Americans and Europeans in the Gilded Age built lavish country homes. In its easternmost sections, Suffolk County remains semi-rural, as in Greenport on the North Fork and some of the periphery of the area prominently known as The Hamptons, although summer tourism swells the population in those areas. The North Fork peninsula of Suffolk County's East End has developed a burgeoning wine region.[51] In addition, the South Fork peninsula is known for beach communities, including the Hamptons, and for the Montauk Point Lighthouse at the eastern tip of the island. The Pine Barrens is a preserved pine forest encompassing much of eastern Suffolk County. The intersection of Long Island, Manhattan, and the continental mainland The bluffs of the North Shore Geology A detailed geomorphological study of Long Island provides evidence of glacial history of the kame and terminal moraines of the island which were formed by the advance and retreat of two ice sheets.[52] Long Island, as part of the Outer Lands region, is formed largely of two spines of glacial moraine, with a large, sandy outwash plain beyond. These moraines consist of gravel and loose rock left behind during the two most recent pulses of Wisconsin glaciation during the ice ages some 21,000 years ago (19,000 BC). The northern moraine, which directly abuts the North Shore of Long Island at points, is known as the Harbor Hill moraine. The more southerly moraine, known as the Ronkonkoma moraine, forms the "backbone" of Long Island; it runs primarily through the very center of Long Island, roughly coinciding with the length of the Long Island Expressway. The land to the south of this moraine to the South Shore is the outwash plain of the last glacier. One part of the outwash plain was known as the Hempstead Plains, and this land contained one of the few natural prairies to exist east of the Appalachian Mountains.[53] The glaciers melted and receded to the north, resulting in the difference between the topography of the North Shore beaches and the South Shore beaches. The North Shore beaches are rocky from the remaining glacial debris, while the South Shore's are crisp, clear, outwash sand. Jayne's Hill, at 401 feet (122 m), within Suffolk County near its border with Nassau County, is the highest hill along either moraine; another well-known summit is Bald Hill in Brookhaven Town, not far from its geographical center at Middle Island. The glaciers also formed Lake Ronkonkoma in Suffolk County and Lake Success in Nassau County, each a deep kettle lake. Countyscapes The Downtown Brooklyn skyline at the western end of Long Island. The Manhattan Bridge (far left) and the Brooklyn Bridge (near left) are seen across the East River from Lower Manhattan at sunset in 2013. The expanding skyline of Long Island City, Queens, one of New York City's fastest-growing neighborhoods,[54] seen facing the East River at blue hour in 2015. At left is the Queensboro Bridge, connecting Queens to Manhattan. The Village of Freeport on Baldwin Bay in Nassau County A beach in The Hamptons of Suffolk County   Climate Under the Köppen climate classification, Long Island lies in a transition zone between a humid subtropical climate (Cfa) and a hot-summer humid continental climate (Dfa).[55] The climate features hot, usually humid summers with occasional thunderstorms, mild spring and fall weather, and cold winters with a mix of snow and rain and stormier conditions. Spring can be cool due to the relatively cooler temperatures of the Atlantic Ocean and occasional blocking. Thunderstorms rarely form directly over Long Island, but can form over inland areas and then move eastward. Some storms may weaken as they approach Long Island due to the moderating effects of the Atlantic Ocean. The ocean also brings afternoon sea breezes to the immediate South Shore areas (within 1 mile (1.6 km)) that temper the heat in the warmer months. The temperatures south of Sunrise Highway (NY Route 27) tend to be significantly cooler than the rest of Long Island in the spring and summer months because of the relatively cooler temperatures of the Atlantic Ocean. Long Island has a moderately sunny climate, averaging 2,400 to 2,800 hours of sunshine annually.[56] Cumulus congestus clouds over Long Island on a summer afternoon Clear skies in autumn over the Great Peconic Bay, with the Atlantic Ocean as its primary inflow, separating the North Fork and South Fork at the East End of Long Island Due to its coastal location, Long Island winter temperatures are milder than most of the state. The coldest month is January, when average temperatures range from 25 to 45 °F (−4 to 7 °C), and the warmest month is July, when average temperatures range from 74 to 85 °F (23 to 29 °C).[57] Temperatures seldom fall below −5 °F (−21 °C) or rise above 100 °F (38 °C). Coldest temp ever recorded on Long Island was −23 °F (−31 °C) on January 22, 1961. Long Island temperatures vary from west to east, with the western part (Nassau County, Queens, and Brooklyn) generally 2 to 3 degrees F (1 to 2 degrees C) warmer than the east (Suffolk County). This is due to several factors: the western part is closer to the mainland and more densely developed, causing the "urban heat island" effect, and Long Island's land mass veers northward as one travels east. Also, daytime high temperatures on the eastern part of Long Island are cooler on most occasions, due to the moderating effect of the Atlantic Ocean and Long Island Sound. On dry nights with no clouds or wind, the Central Part of Suffolk County and Pine Barrens forest of eastern Suffolk County can be almost 5 to 10 F (3 to 5 C) cooler than the rest of the island, due to radiational cooling. Average dew points, a measure of atmospheric moisture, typically lie in the 60–70 °F (16–21 °C) range during July and August. Stripped Rockaway Beach Boardwalk after Hurricane Sandy in 2012 Precipitation is distributed uniformly throughout the year, with approximately 3–4 inches (76–102 mm) on average during each month. Average yearly snowfall totals range from approximately 20 to 35 inches (51 to 89 cm), with the north shore and western parts averaging more than the immediate south shore (South of Sunrise Hwy) and the east end. In any given winter, however, some parts of the island can see up to 50 inches (130 cm) of snow or more. There are also milder winters, in which much of the island see less than 10 inches (25 cm) of snow. On August 13, 2014, flash flooding occurred in western-central Suffolk County after a record-setting rainfall deposited more than three months' worth of precipitation on the area within a few hours.[58] Long Island is somewhat vulnerable to tropical cyclones.[59] While it lies north of where most tropical cyclones turn eastward and out to sea (most landfalls on the East Coast of the US occur from North Carolina southward), several tropical cyclones have struck Long Island, including a devastating Category 3, the 1938 New England Hurricane (also known as the "Long Island Express"), and another Category 3, Hurricane Carol in 1954. Other 20th-century storms that made landfall on Long Island at hurricane intensity include the Great Atlantic Hurricane of 1944, Hurricane Donna in 1960, Hurricane Belle in 1976, and Hurricane Gloria in 1985. Also, the eyewall of Hurricane Bob in 1991 brushed the eastern tip. In August 2011, portions of Long Island were evacuated in preparation for Hurricane Irene, a Category 1 hurricane which weakened to a tropical storm before it reached Long Island.[60] On October 29, 2012, Hurricane Sandy caused extensive damage to low-lying coastal areas of Nassau and Suffolk counties, Brooklyn, and Queens, destroying or severely damaging thousands of area homes and other structures by ocean and bay storm surges. Hundreds of thousands of residents were left without electric power for periods of time ranging up to several weeks while the damage was being repaired. The slow-moving "Superstorm Sandy" (so-nicknamed because it merged with a nor'easter before it made landfall) caused 90% of Long Island households to lose power and an estimated $18 billion in damages in Nassau and Suffolk counties alone.[61][62] The storm also had a devastating impact on coastal communities in the Brooklyn and Queens portions of the island, including Coney Island in Brooklyn and the Rockaway Peninsula in Queens, although estimates of monetary damages there are usually calculated as part of the overall losses suffered in New York City as a whole. When allowance is made for inflation, the extent of Sandy's damages is second only to that of those caused by the 1938 Long Island Express. Although a lower central pressure was recorded in Sandy, the National Hurricane Center estimates that the 1938 hurricane had a lower pressure at landfall.[63][64][full citation needed] Hurricane Sandy and its profound impacts have prompted the discussion of constructing seawalls and other coastal barriers around the shorelines of Long Island and New York City to minimize the risk of destructive consequences from another such event in the fu