Albany Pine Bush

Albany Pine Bush Preserve
IUCN Category Ib (Wilderness Area)
Location of the Albany Pine Bush
in the US state of New York
Location Albany County, New York, USA
(NYSDEC Region 4)[1]
Nearest city Albany, New York
Area 3,010 acres (1,220 ha)[2]
Established 1988[2]
Governing body Albany Pine Bush
Preserve Commission

The Albany Pine Bush, referred to locally as the Pine Bush, is one of the largest of the 20 inland pine barrens in the world,[3] and is centrally located in New York's Capital District within Albany and Schenectady counties, between the cities of Albany and Schenectady.[4][5] The Albany Pine Bush was formed thousands of years ago, following the drainage of Glacial Lake Albany.[6][7]

The Albany Pine Bush is the sole remaining undeveloped portion of a pine barrens that once covered over 40 square miles (100 km2), [8] and is "one of the best remaining examples of an inland pine barrens ecosystem in the world."[4] Today it includes all parcels of the Albany Pine Bush Preserve (a state nature preserve spanning 3,010 acres (1,220 ha)), the properties that connect these protected parcels, and some of the surrounding areas that abut the preserve.[2][8] The 135-acre (55 ha) Woodlawn Preserve and surrounding areas in Schenectady County are the western sections of the Pine Bush and are separated from the Albany Pine Bush Preserve in Albany County.[9]

The Pine Bush has been a historical, cultural, and environmental asset to the Capital District and Hudson Valley regions of New York. Pioneers moving west passed through the pine barrens, which later became the site of the first passenger railroad in the United States.[10][11] The Pine Bush is also home to the Karner Blue butterfly, an endangered species first identified by Vladimir Nabokov in 1944 using a type specimen from the Pine Bush.[12]

Contents

History

European colonization

Around 10,000 years ago Native Americans moved into the Pine Bush area. When Europeans arrived in the early 17th century, two groups lived in the immediate area: the Mohawk nation of the Iroquois to the west, and the Mahicans to the east, along the Hudson River.[13] The Dutch traded with both native groups from their trading outpost at Fort Orange (present day Albany), which was established in 1624. For the natives the Pine Bush was an important source of firewood and animal pelts to trade with the Dutch, but by 1640 the natives were having trouble finding enough animals in the Pine Bush to supply the growing European demand.[13] Schenectady was a name given by the Iroquois to the settlement at Fort Orange, meaning "beyond the pine plains" referring to the Pine Bush; and the Dutch granted a patent under the name of Schenectady to a settlement opposite the Pine Bush from Fort Orange in 1661.[14] To the settlers at Fort Orange, the settlement on the Mohawk River started by Arent van Curler was "beyond the pine plains", and therefore the name Schenectady (in various spelling connotations) became associated with the village at that site.[15] In 1664, the Dutch surrendered their entire colony of New Netherland, including Albany and Schenectady, to the English.[16]

The King's Highway originated during Dutch times as a series of foot paths the natives took through the Pine Bush to trade with Fort Orange, but after the founding of Schenectady it referred to a major route between the two settlements. Until the mid-18th century, the King's Highway was no more developed than those foot paths.[17] During the French and Indian Wars, the British military improved the road significantly, and after the war it was used by a large number of settlers moving west.[17] Also during the war from 1699 to 1707 Albany residents collected firewood from the Pine Bush for the large army that was camped at Fort Frederick.[13] In 1710, Germans immigrated from Palatine to the Albany area to live and work in the Pine Bush in order to harvest pines for pitch and rosin for the construction of naval vessels.[13] These immigrants would later go on to discover and name the Helderberg Escarpment and settle Schoharie County.[18]

During the late-18th century, taverns and the occasional homesteader began to dot the Pine Bush along the King's Highway while development began to encroach on the Pine Bush at the Albany and Schenectady edges as those settlements began to grow out towards each other.[17] The highway and the Pine Bush was a frontier wilderness and extremely dangerous, so starting in 1765 militiamen began taking turns escorting travelers through to protect them from outlaws, bandits, smugglers, and other dangers. During the American Revolutionary War it was home to Loyalists of the British Crown.[13] One of the taverns established in the 1760s catering to Pine Bush travelers on the King's Highway was the Truax Tavern owned by Isaac Truax, who was a Tory sympathizer during the Revolution, but in his own words "not a Tory, but a man for the King". Rumors circulated of several murders/robberies being carried out at the tavern.[13] Travel became a bit safer in 1793 when a stage coach began taking passengers through the Pine Bush for three cents per mile.[13] Herman Melville, a native of Albany and nearby Troy, described the Pine Bush in his 1851 novel, Moby-Dick.[19]

19th century

The 19th century saw great improvements in modes of transportation for traveling through the Pine Bush with better roads and soon thereafter railroads. Beginning in 1799 the Great Western Turnpike (today's US Route 20) and the Albany-Schenectady Turnpike (New York Route 5) were built through the Pine Bush. The Western Turnpike connected Albany west across the state to the US Midwest, while the Albany-Schenectady Turnpike replaced the King's Highway to Schenectady.[13] In 1826, in order to reduce travel time between Schenectady and Albany along the Erie Canal, the Mohawk and Hudson Railroad was chartered; it was the first railroad in the state of New York, and the fourth in the United States. On July 2, 1830, the DeWitt Clinton became the first passenger train in the United States, traveling over the 16-mile (26 km) route through the heart of the Pine Bush.[10][11]

Over time, the turnpikes and railroad opened up parts of the Pine Bush to settlement, farming, and even land speculation. One of the earliest residents was Theophillus Roessle, who owned a large farm and manor in what is now the hamlet of Roessleville, just outside of Albany in the town of Colonie. He claimed that the sandy soil of the Pine Bush was "the best land for fruits in the world."[13] Further west part of the Pine Bush was carved up in 1858 into 860 plots as part of what is now known as the "Great Land Swindle" and sold to buyers outside the region. When they came to inspect their land, they felt it to be useless barrens devoid of any good use; they would then try to recoup their money by selling the land to other unsuspecting outsiders.[13]

Pressures through direct settlement and roads for passersby were not the only disturbance the Pine Bush felt during the 19th century. As in the colonial period, the Pine Bush continued to be tapped for its natural resources; whereas in earlier centuries its primary resources were firewood and wildlife, it was now water.[13] The Patroon Creek, roughly where three feeder streams joined in the heart of the Pine Bush along Albany's northern border, was dammed in 1850 to form Rensselaer Lake.[13]

In 1871, the northwestern portion of Albany, west from Magazine Street, consisting of mostly undeveloped Pine Bush, was annexed to the neighboring town of Guilderland[20] after the town of Watervliet refused annexation of said territory.[21][22] Portions of this territory would be ceded back to Albany in 1910, setting up, more-or-less, the current border.[23] The law (Chapter 375 of the Laws of New York, 1910) described the Pine Bush as "being a territory lying to the west of the present boundary line of the city and which is in large part waste and unoccupied land, the ownership of which is uncertain."[24] This law authorized Albany to lay out the newly annexed territory into lots and to acquire land for a park system to connect the Rensselaer Lake waterworks property to the old city border.[24]

20th century

The Reverend Louis W. Parson and his wife migrated in 1927 from Mississippi to Albany, where he founded the First Church of God in Christ. In four trips to Mississippi, Parson encouraged friends and family to move to Albany and join the church and many did during the 1930s and 1940s. The reverend felt that the mores of Albany's South End, where they originally settled, was not conducive to religious life and therefore he started a community in the Pine Bush along Rapp Road. Two 14-acre (5.7 ha) undeveloped properties were purchased by Reverend Parson in 1930 and 1933 and the community grew by "haphazard" splitting of the properties, a narrow land which is today the Rapp Road Community Historic District, a state and national historic place.[25]

In 1912, the city of Albany commissioned a study by notable architect Arnold W. Brunner and landscape architect Charles Downing Lay regarding beautification of the city, and this report was later published under the name Stvdies for Albany.[26][27] In this study, Brunner and Lay proposed using the Rensselaer Lake waterworks property as the core of a new 1,000-acre (400 ha) natural park, preferably with little done to improve it – "In fact the less done to it the better."[28] Instead of adding land to create a park, portions of the original waterworks property were sold off piecemeal and developed over the following century.[29] In the 1950s, the New York State Thruway (Interstate 90) was built through the Pine Bush.[30] Further development would be seen in the 1950s and 60s with the construction of the W. Averell Harriman State Office Building Campus and the SUNY Albany uptown campus.[31] The Pine Bush today is about 90% smaller than it was prior to 1950.[32]

Mayor Erastus Corning 2nd in the 1960s pushed forward the Washington Avenue Extension, a four-lane divided highway extending Washington Avenue westward from Fuller Road through the Pine Bush to New Karner Road (NY Route 155). This opened the heart of the Pine Bush and the western section of the city to development and was called "a knife through the heart of the Pine Bush".[33] Soon afterward, Neil Hellman, a race horse magnate and major developer in the city, proposed a huge "city within a city" on 390 acres (160 ha) that would have apartments, stores, an office park, one or two schools, and fire and police stations. Mayor Corning estimated between 10,000 and 15,000 individuals would live there. Environmentalists and neighborhood groups fought and ultimately defeated this proposal.[34]

The history of the Pine Bush received notoriety when Mayor Corning gave archaeologist Don Rittner a $500 donation in 1972 to excavate the Truax Tavern along the King's Highway. Rittner disproved the prevailing historical beliefs concerning the sophistication and structure of the tavern, and possibly confirmed rumors about murder at the tavern with the discovery of several skeletons under the tavern's floor.[13] This discovery led to Rittner becoming Albany's first municipal archaeologist and possibly the first in the nation.[35]

While Mayor Corning was responsible for the largest purchases of Pine Bush land as a preserve, he was also responsible for placing the Albany landfill in the Pine Bush, the construction of the Washington Avenue Extension, and authorizing much of the development that occurred during his 42 years in office as mayor.[36] In 1967, a portion of Albany's waterworks/Pine Bush property in the town of Colonie along Central Avenue was sold to developers who built an enclosed mall, the Northway Mall. Two years later the city moved its dump to the Pine Bush,[37] and the Dunes, a single family housing development in the middle of the Pine Bush off the Washington Avenue Extension, was built in the mid-1970s.[38] In response to these developments of sensitive Pine Bush lands, concerned citizens formed Save the Pine Bush in 1978. The organization filed lawsuits for the next several decades to stop further developments.[39]

Among those developments Save the Pine Bush fought was the construction of Crossgates Mall in the town of Guilderland. First proposed in 1978, it was finished in 1984, then expanded to double the original size in 1994 to become the third largest mall in New York at 1.5 million square feet.[40] Plans in the late 1990s to increase the size of the Crossgates Mall with over 2 million additional square feet of retail space on two new stories, a 12-story hotel, and activities such as bowling, ice skating, miniature golf and soccer, were dropped in 1999 against widespread opposition.[41]

In 1985, a bill to establish a state controlled preserve to protect Pine Bush lands never made it out of committee. The bill was proposed the following year by Assemblyman Robert Connor (D)-New City. Among the local politicians who opposed the bill was Albany Mayor Thomas Whalen III, who sparred with Assemblyman Connors in a series of letters in which Connors stated, "if the mayor allows the final destruction of the Pine Bush, the city of Albany will be an ancient archaeological ruin before the pine barren is replaced." Assemblyman Arnold Proskin (R)-Colonie, whose district included portions of the proposed preserve, opposed on the grounds that the bill was creating another state agency like the Adirondack Park Agency that would wrest control from local communities over their own development.[42]

The Albany Pine Bush Preserve Commission was finally created in 1988 and consists of the New York State Department of Environmental Conservation, the New York State Office of Parks, Recreation and Historic Preservation, The Nature Conservancy, the towns of Colonie and Guilderland, the city of Albany, Albany County, and four private citizens appointed by the governor.[3] In 2001, the State Employees Federal Credit Union (SEFCU) bank branch on New Karner Road was taken by the state for the Albany Pine Bush Discovery Center.[4]

The Albany landfill has been in the Pine Bush since 1969 and has had numerous expansions, the latest of which occurred in 2010. As of 2010, the landfill is expected to have seven years of operating life remaining with the latest expansion of 15 acres (6.1 ha). The landfill contributes $4–5 million to the Albany budget and allows the residents of the city to have free trash collection.[43] The city will spend $18 million to restore Pine Bush habitat in exchange for this expansion.[44]

The same year Albany opened its landfill, the city of Schenectady set aside its only patch of Pine Bush as the Woodlawn Preserve. A 135-acre (55 ha) forever wild preserve, the city has been approached numerous times since 1969 by developers wishing to build on the land.[45] 24 acres (9.7 ha) in the neighboring town of Niskayuna, a part of the Woodlawn Pine Barrens–Wetlands Complex in Schenectady County which borders the Woodlawn Preserve, was protected as parkland in 2009 by the county and deeded to the town. This complimented larger plans to connect the Complex to the larger Pine Bush Preserve in Albany County[46]

Geography

The Pine Bush is within the Hudson Valley section of the Appalachian Valley and Ridge Province in the state of New York, and occupies parts of the city of Albany and the towns of Colonie and Guilderland within Albany County. The Pine Bush includes not only pine barrens, but also grasslands of prairie grasses, northern and southern successional forests, and numerous ravines with some wetlands. The Pine Bush ranges in elevation from 260 feet (79 m) to 360 feet (110 m) above sea level.[8]

Geology

Underlying the Albany Pine Bush is a bedrock consisting of shale and siltstone, laid down 450 million years ago during the Middle Ordovician. The bedrock is covered by glaciolacustrine deposits which make up the sandy topsoils of the barrens.[8]

As the glaciers of the Wisconsin glaciation began to recede from the Hudson Valley area, a glacial lake known today as Lake Albany extended across the mid and upper Hudson Valley and a large delta formed west of Albany where the predecessor of the Mohawk River flowed into the lake.[8][13] Along the shoreline of the lake, lacustrine sands were deposited between the present-day cities of Hudson and Glens Falls; this became the Hudson Valley sandplain.[8] Relieved from the weight of the glacier, the land began to rebound, and the lake receded by draining into the Hudson River, the deposits of sand in the delta area were then sculpted by wind into sand dunes. Plants later colonized the land and stabilized the dunes.[8][13] The Pine Bush originally occupied 40 square miles (100 km2), at which point it was the largest inland pine barrens in North America[8]

Ecology

Flora

Less than half of the protected areas of the Albany Pine Bush (42%, or 952 acres (385 ha)) are currently pitch pine-scrub oak barrens, with an additional 680 acres (280 ha) of disturbed areas with invasive plant growth that are now under protection and can be restored to their pristine barren status. The remaining pine barrens are dominated by pitch pine (Pinus rigida), a tall shrub layer consisting of bear oak and dwarf chestnut oak (Quercus ilicifolia and Q. prinoides), and a low shrub layer composed of lowbush blueberries (Vaccinium angustifolium and V. pallidum), black huckleberry (Gaylussacia baccata), and sweet fern (Comptonia peregrina). Between areas of pitch pine-scrub oak barrens are small patches of grassland dominated by prairie grasses including big bluestem (Andropogon gerardii), little bluestem (Schizachyrium scoparium), Indiangrass (Sorghastrum nutans), as well as small trees like the shrubby willows (Salix humilis and S. tristis). Characteristic flowering plants include bush clover (Lespedeza capitata), goat's-rue (Tephrosia virginiana), and wild lupine (Lupinus perennis).[8]

Due to prolonged periods of natural fire suppression, much of the Pine Bush has evolved into northern or southern hardwood forests. These forests, often dominated by invasive species that are foreign to the area, occupy roughly 500 acres (200 ha) of the Albany Pine Bush Preserve. The southern hardwood forests are dominated by black locust (Robinia pseudoacacia), which is exotic, and black cherry (Prunus serotina); with lesser numbers of native oaks (Quercus) and maples (Acer), and the exotic tree of heaven (Ailanthus altissima). The shrub layer is dominated by black raspberry (Rubus occidentalis) and other brambles (Rubus sp.). In contrast the northern hardwood forests are dominated by Aspen (Populus), black cherry, red maple (Acer rubrum), white pine (Pinus strobus), gray birch (Betula populifolia), green ash (Fraxinus pennsylvanica), and oaks.[8]

Ravines within the Pine Bush contain mixed forests of pine-northern hardwoods and Appalachian oak-pine. The pine-hardwood forests are dominated by species such as white pine and yellow birch (Betula alleghaniensis), mixed with scattered red maple, a shrub layer dominated by witch-hazel (Hamamelis virginiana), and a herbaceous layer composed of a variety of herbs, mosses, and lichens. The Appalachian oak-pine forest has a tree canopy of one or more oak species, primarily black oak, white oak, and red oak (Quercus velutina, Q. alba, and Q rubra); these are mixed with pitch pine and some white pine, and a shrub layer dominated by heath shrubs, typically blueberries and black huckleberry. Marshes and wetlands occur along the northern boundary of the Pine Bush and along the bottoms of ravines. Roughly 35 acres (14 ha) of vernal pools have been mapped, these are ground-water fed ponds that are dominated by grasses, sedges, herbs, and low shrubs.[8]

The Pine Bush is home to bog bluegrass (Poa paludigena), a Federal Species of Concern, as well as the rare red-rooted flatsedge (Cyperus erythrorhizos), Houghton's umbrella-sedge (Cyperus houghtonii), and Schweinitz's flatsedge (Cyperus schweinitzii). Bog bluegrass occurs at the bottom of a ravine in the Pine Bush and is the only place in the New York Bight watershed where this plant appears. Bayard's malaxis (Malaxis bayardii) is a rare orchid that occurs in the Pine Bush as well.[8]

Fauna

The Albany Pine Bush is home to hundreds of species of Lepidoptera (moths), including over 40 Noctuidae considered to be pine barrens specialists, but the most well-known species in the area is the Karner Blue (Lycaeides melissa samuelis), a butterfly on the Endangered Species List. Once found in large numbers throughout the grassy openings of the pine barrens, it is today extremely rare and found in only a handful of sites. Attempts to reintroduce the butterfly focus on the food and host plant for its larvae – the wild blue lupine, which needs frequent forest fires to maintain its habitat. Other regionally-rare butterflies include the dusted skipper (Atrytonopsis hianna), Henry's Elfin (Incisalia henrici), Frosted Elfin (Incisalia irus), and Edward's Hairstreak (Satyrium edwardsii). The inland barrens buck moth (Hemileuca maia) is a state-listed special concern animal; and other rare moths include the broad-lined catopyrrha (Catopyrrha coloraria), several noctuid moths (Apharetra purpurea, Chaetaglaea cerata, Chytonix sensilis, Macrochilo bivittata, and Zanclognatha martha), bird dropping moth (Cerma cora), and a geometrid moth (Itame). The Albarufan dagger moth was last seen in the Pine Bush in 1983 and is presumed locally extinct.[8]

The Pine Bush is also home to 30 of the 44 species of amphibians and reptiles that are indigenous to Albany County, and seven of these species are generally not seen so far north in the state of New York.[49] Three species of salamander, the Jefferson salamander (Ambystoma jeffersonium), blue-spotted salamander (Ambystoma laterale), and spotted salamander (Ambystoma maculatum), are state-listed special concern animals. Two species of turtle, the spotted turtle (Clemmys guttata) and wood turtle (Clemmys insculpta), are also special concern animals. About 45 species of birds breed in the Albany Pine Bush (according to the 1985 New York State Breeding Bird Atlas) and are fairly common species for the area; and about 32 species of common small mammals have been found in and adjacent to the Pine Bush.[8]

See also

Capital District portal
Hudson Valley portal
New York portal
Other notable pine barrens

References

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  33. ^ Grondahl 2007, p. 382
  34. ^ Grondahl 2007, p. 381
  35. ^ Grondahl 2007, p. 386
  36. ^ Grondahl 2007, p. 379
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Bibliography

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