24.11.2014 Views

Part 1: Campus Profile - SUNY Cobleskill

Part 1: Campus Profile - SUNY Cobleskill

Part 1: Campus Profile - SUNY Cobleskill

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

<strong>SUNY</strong> <strong>Cobleskill</strong> Facilities Master Plan – Phase 1 Report<br />

November 2011<br />

PHYSICAL ENVIRONMENT<br />

G<br />

G – PHYSICAL ENVIRONMENT<br />

<strong>SUNY</strong> <strong>Cobleskill</strong> is located in the Village of <strong>Cobleskill</strong> in New York’s<br />

Schoharie County, a picturesque and historic area approximately 160<br />

miles northwest of New York City and midway between Albany and<br />

Oneonta. NYS Route 7 runs through the middle of the campus at the<br />

western edge of the Village of <strong>Cobleskill</strong>, directly off of I-88.<br />

Schoharie County offers a rare combination of rural life and direct access<br />

to the services and activities of a metropolitan area, New York’s Capital<br />

Region. Albany is only a 40-minute drive east of the College. The county<br />

lies in close proximity to such natural splendors as the Adirondack Park,<br />

the Catskill Mountains, the historic Helderberg Mountains, and the<br />

Mohawk Valley. State and private parks, streams, lakes, mountain trails<br />

and ski areas provide an abundance of outdoor activities.<br />

PHYSICAL CONTEXT<br />

era, when a vast slurry of limestone coursed through the region. This<br />

has given rise to areas of irregular limestone known as “Karst,” in which<br />

caves, fissures, joints, sinkholes, depressions, springs (“resurgences”), and<br />

sinking streams (“insurgences”) are found, including the nearby tourist<br />

attraction known as the Howe Caverns. In these areas, water passes<br />

quickly through solutional passages, but does not purify itself in doing so<br />

as it would through more consolidated and organic strata. These areas<br />

are therefore vulnerable to pollution from agricultural and development<br />

uses of land (cattle pastures, trash dumps, septic tanks, etc). The Town<br />

of <strong>Cobleskill</strong> has concluded that the best environmental solution lies in<br />

preserving farmland, which in turn raises issues of entrepreneurship that<br />

are central to <strong>SUNY</strong> <strong>Cobleskill</strong>’s focus on agribusiness. The Protection<br />

Plan identifies several key strengths and weaknesses which appear to be<br />

areas in which <strong>SUNY</strong> <strong>Cobleskill</strong> could both assist and benefit the region.<br />

Cambrian<br />

Middle Proterozoic<br />

Ordovician<br />

Silurian<br />

Devonian<br />

Graphic G1<br />

Bedrock Geology of New York<br />

State<br />

The Village of <strong>Cobleskill</strong>, with approximately 5,300 residents, is a typical<br />

small college town with convenient access to shopping, dining, houses of<br />

worship, recreational facilities, and medical services. With a history that<br />

dates to 1711 (when the first pioneer settlers arrived), the <strong>Cobleskill</strong> area<br />

is a treasure trove of historic sites and museums.<br />

Late Proterozoic<br />

Cambrian - Late Ordivician<br />

Middle Proterozoic<br />

Triassic<br />

Cretaceous<br />

The Village of <strong>Cobleskill</strong> was founded in 1752, while the Town was<br />

established in 1797. Key historic structures such as the Bulls Head Inn<br />

(1802), the oldest building in the Village, remain. Over the course of<br />

the 19th century, the Village evolved from a small village on a stream to<br />

a prosperous and bustling town with the arrival of the railroad. Historic<br />

images on postcards illustrate tree-lined streets with an urban, small-town<br />

presence and a major railroad station as early as 1900. The Village’s<br />

Main Street continues through the center of the campus (renamed as<br />

Albany Street).<br />

Given <strong>SUNY</strong> <strong>Cobleskill</strong>’s distinctive focus on land, agriculture, and<br />

natural resources, and its commitment to environmental issues and to<br />

partnerships with local and regional interests, it is interesting to note that<br />

<strong>Cobleskill</strong> lies in a unique geological area with significant implications for<br />

farming and the environmental health of its region. According to the Town<br />

of <strong>Cobleskill</strong> Agricultural and Farmland Protection Plan, <strong>Cobleskill</strong> lies on<br />

the edge of a large region to the south that is geologically composed of<br />

Marcellus Shale, a marine sedimentary rock that is a potential source of<br />

natural gas obtained through the controversial process of “fracking.”<br />

To the north, extending in a broad arc from the Hudson west to Michigan,<br />

is an area of unusual geological formations created during the Devonian<br />

St. Lawrence-Champlain Lowlands<br />

Adirondack Mountains<br />

Tug Hill Plateau<br />

Ontario Lowlands<br />

Allegheny Plateau<br />

Catskill Mountains<br />

Hudson Highlands<br />

Newark Lowlands<br />

Atlantic Coastal Plain<br />

Mohawk Valley<br />

Taconic<br />

Mountains<br />

Hudson Valley<br />

Manhattan<br />

Prong<br />

Graphic G2<br />

Physiographic Provinces of New<br />

York State<br />

29

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!