Hudson Valley

The Hudson Valley or Hudson River Valley comprises the valley of the Hudson River and its adjacent communities in the U.S. state of New York. The region stretches from the Capital District including Albany and Troy south to Yonkers in Westchester County, bordering New York City.

History

Pre-Columbian era

The Hudson Valley was inhabited by indigenous peoples long before European settlers arrived. The Lenape, Wappinger, and Mahican branches of the Algonquins lived along the river, mostly in peace with the other groups. The lower Hudson River was inhabited by the Lenape. The Lenape people waited for the explorer Giovanni da Verrazzano onshore, traded with Henry Hudson, and sold the island of Manhattan. Further north, the Wappingers lived from Manhattan Island up to Poughkeepsie. They lived a similar lifestyle to the Lenape, residing in various villages along the river. They traded with both the Lenape to the south and the Mahicans to the north. The Mahicans lived in the northern valley from present-day Kingston to Lake Champlain, with their capital located near present-day Albany. The Algonquins in the region lived mainly in small clans and villages throughout the area. One major fortress was called Navish, which was located at Croton Point, overlooking the Hudson River. Other fortresses were located in various locations throughout the Hudson Highlands.

Hudson River exploration

In 1497, John Cabot traveled along the coast and claimed the entire country for England; he is credited with the Old World's discovery of continental North America. Between then and about 1609, exploration took place around New York Bay, but not into the Hudson Valley. In 1609, the Dutch East India Company financed English navigator Henry Hudson in his attempt to search for the Northwest Passage. During this attempt, Henry Hudson decided to sail his ship up the river that would later be named after him. As he continued up the river, its width expanded, into Haverstraw Bay, leading him to believe he had successfully reached the Northwest Passage. He also proceeded upstream as far as present-day Troy before concluding that no such strait existed there.

Colonization

After Henry Hudson realized that the Hudson River was not the Northwest Passage, the Dutch began to examine the region for potential trading opportunities. Dutch explorer and merchant Adriaen Block led voyages there between 1611 and 1614, which led the Dutch to determine that fur trade would be profitable in the region. As such, the Dutch established the colony of New Netherland. The Dutch settled three major fur-trading outposts in the colony, along the river, south to north: New Amsterdam, Wiltwyck, and Fort Orange. New Amsterdam later became known as New York City, Wiltwyck became Kingston, and Fort Orange became Albany. In 1664, the British invaded New Netherland via the port of New Amsterdam. New Amsterdam and New Netherland as a whole were surrendered to the British and renamed New York.
Under British colonial rule, the Hudson Valley became an agricultural hub, with manors being developed on the east side of the river. At these manors, landlords rented out land to their tenants, letting them take a share of the crops grown while keeping and selling the rest of the crops. Tenants were often kept at a subsistence level so that the landlord could minimize his costs. Landlords held immense political power in the colony due to driving such a large proportion of the agricultural output. Meanwhile, land west of Hudson River contained smaller landholdings with many small farmers living off the land. A large crop grown in the region was grain, which was largely shipped downriver to New York City, the colony's main seaport, for export back to Great Britain. In order to export the grain, colonial merchants were given monopolies to grind the grain into flour and export it. Grain production was also at high levels in the Mohawk River Valley.

Revolutionary War

The Hudson River was a key river during the Revolutionary War. The Hudson's connection to the Mohawk River allowed travelers to get to the Great Lakes and the Mississippi River eventually. In addition, the river's close proximity to Lake George and Lake Champlain would allow the British navy to control the water route from Montreal to New York City. In doing so, the British, under General John Burgoyne's strategy, would be able to cut off the patriot hub of New England and focus on rallying the support of loyalists in the South and Mid-Atlantic regions. The British knew that total occupation of the colonies would be unfeasible, which is why this strategy was chosen. As a result of the strategy, numerous battles were fought along the river, including several in the Hudson Valley.

Industrial Revolution

In the early 19th century, popularized by the stories of Washington Irving, the Hudson Valley gained a reputation as a somewhat gothic region characterized by remnants of the early days of the Dutch colonization of New York. The area is also associated with the Hudson River School, a group of American Romantic painters who worked from about 1830 to 1870.
Following the building of the Erie Canal, the area became an important industrial center. The canal opened the Hudson Valley and New York City to commerce with the Midwest and Great Lakes regions. However, in the mid 20th century, many of the industrial towns went into decline.
The first railroad in New York, the Mohawk and Hudson Railroad, opened in 1831 between Albany and Schenectady on the Mohawk River, enabling passengers to bypass the slowest part of the Erie Canal. The Hudson Valley proved attractive for railroads once technology progressed to the point where it was feasible to construct the required bridges over tributaries. The Troy and Greenbush Railroad was chartered in 1845 and opened that same year, running a short distance on the east side between Troy and Greenbush, now known as East Greenbush. The Hudson River Railroad was chartered the next year as a continuation of the Troy and Greenbush south to New York City, and was completed in 1851. In 1866, the Hudson River Bridge opened over the river between Greenbush and Albany, enabling through traffic between the Hudson River Railroad and the New York Central Railroad west to Buffalo. When the Poughkeepsie Bridge opened in 1889, it became the longest single-span bridge in the world.
The New York, West Shore and Buffalo Railway began at Weehawken Terminal and ran up the west shore of the Hudson as a competitor to the merged New York Central and Hudson River Railroad. Construction was slow and was finally completed in 1884; the New York Central purchased the line the next year.
During the Industrial Revolution, the Hudson River Valley became a major location for production. The river allowed for fast and easy transport of goods from the interior of the Northeast to the coast. Hundreds of factories were built around the Hudson, in towns including Poughkeepsie, Newburgh, Kingston, and Hudson. The North Tarrytown Assembly, on the river in Sleepy Hollow, was a large and notable example. The river links to the Erie Canal and the Great Lakes, which allowed manufacturers in the Midwest, including automobile factories in Detroit, to use the river for transport. With industrialization came new technologies, such as streamboats, for faster transport. In 1807, the North River Steamboat, became the first commercially successful steamboat. It carried passengers between New York City and Albany along the Hudson River. At the end of the 19th century, the Hudson River region of New York State would become the world's largest brick manufacturing region, with 130 brickyards lining the shores of the Hudson River from Mechanicsville to Haverstraw and employing 8,000 people. At its peak, about 1 billion bricks a year were produced, with many being sent to New York City for use in its construction industry.
Tourism became a major industry as early as 1810. With convenient steamboat connections in New York City and numerous attractive hotels in romantic settings, tourism became an important industry. Early guidebooks provided suggestions for travel itineraries. Middle-class people who read James Fenimore Cooper's novels or saw the paintings of the Hudson River School were especially attracted to the region.

Geology and physiography

The Hudson River valley runs primarily north to south down the eastern edge of New York State, cutting through a series of rock types including Triassic sandstones and redbeds in the south and much more ancient Precambrian gneiss in the north. In the Hudson Highlands, the river enters a fjord cut during previous ice ages. To the west lie the extensive Appalachian Highlands. In the Tappan Zee region, the west side of the river has high cliffs produced by an erosion-resistant diabase; the cliffs range from in height.
The Hudson Valley is one physiographic section of the larger Ridge-and-Valley province, which in turn is part of the larger Appalachian physiographic division. The northern portions of the Hudson Valley fall within the Eastern Great Lakes and Hudson Lowlands Ecoregion.
During the last ice age, the valley was filled by a large glacier that pushed south as far as Long Island. Near the end of the last ice age, the Great Lakes drained south down the Hudson River, from a large glacial lake called Lake Iroquois. Lake Ontario is the remnant of that lake. Large sand deposits remain from where Lake Iroquois drained into the Hudson; these are now part of the Rome Sand Plains.
Due to its resemblance, the Hudson River often has been described as "America's Rhine". In 1939, the magazine Life described the river as such, comparing it to the stretch of the Rhine in Central and Western Europe.

Major industries

Agriculture

The Hudson Valley has a long agricultural history and agriculture was its main industry when the region was first settled. Around the 1700s, tenant farming was highly practiced. The farms' main products were grains, though hops, maple syrup, vegetables, dairy products, honey, wool, livestock, and tobacco were produced there. The region became the breadbasket of colonial America, given that the surrounding New England and Catskills areas were more mountainous and had rockier soils. In the late 1800s, most farms transitioned from tenant farming to being family-owned, with more incentive to improve the land. Grain production moved west to the Genesee Valley, and so Hudson Valley farms specialized, especially in viticulture, berries, and orchard cultivation. Agriculture began to decline in the 19th century, and rapidly declined in the 20th century.
By the 1970s, the United States' culinary revolution began, and the Hudson Valley began to lead the farm-to-table movement, the local food movement, and sustainable agricultural practices. The fertile Black Dirt Region of the Wallkill and Schoharie valleys also began to be farmed. Dairy farms are predominant, though fruit, vegetable, poultry, meat, and maple syrup production are also common. Orchard cultivation is common in Orange, Ulster, Dutchess, and Columbia counties.