Information about Finger Lakes
The Finger Lakes, a major tourist destination in the west-central section of Upstate New York, are actually eleven in number, but only seven of the largest are commonly identified as such. The lakes mainly are linear in shape, each lake oriented on a north-south axis. The longest, Cayuga Lake and Seneca Lake, are among the deepest in America. Both are close to 40 miles (64 km) from end to end, but never more than 3.5 miles (5,600 m) wide. Cayuga is actually the longest (38.1 miles (61.3 km)), but Seneca the largest in total area. Seneca is the deepest (618 feet, 188.4 m), followed by Cayuga (435 feet, 132.6 m), with the bottoms well below sea level. These largest lakes resemble the others in shape, which collectively reminded early map-makers of the fingers of a hand.
Cazenovia Lake to the east, although smaller, is sometimes called "the eighth Finger Lake," because it is similar in shape, located in Appalachian hill terrain, with a historic village linked to other Finger Lakes by US Route 20. It may have been formed in the same manner as the Finger Lakes, as satellite photos show three valleys similar in character and spacing to the Finger Lakes east of Otisco Lake. The first is the Tully Valley, which includes a chain of small lakes at the south end that could be a "Finger Lake" that never formed because of a terminal moraine. The moraine caused the Tioughnioga River to flow south instead of north, the opposite of the other waters of the Finger Lakes. The next two valleys to the east contain Butternut Creek, which flows north, and the East Branch of the Tioughnioga River, which flows south. The next valley contains Limestone Creek, which flows north. The next valley after that contains Cazenovia Lake.
Oneida Lake, to the northeast of Syracuse, New York, is sometimes included as the "thumb," although it is shallow and somewhat different in character from the rest. Onondaga Lake, though located just north of the Finger Lakes region, is not considered one of the Finger Lakes. Conesus, Hemlock, Canadice, Honeoye, and Otisco are considered the minor Finger Lakes. Other, smaller lakes, including Silver, Waneta, and Lamoka lakes, dot this region. However, Waneta and Lamoka lakes are part of the Susquehanna River watershed as they drain into a tributary of the Chemung River.
East of Oneida and Cazenovia Lakes are the headwaters of the Susquehanna River and Hudson River watersheds (the latter through the Mohawk Valley).
The Finger Lakes are situated on the northern edge of the Appalachian Upland. They now drain northward to Lake Ontario. The southern ends of the lakes are characterized by steeper hills etched by streams running toward the lakes below. Glacial hanging valleys, terraces in the descent toward the lakes, often end with waterfalls. Taughannock Falls, with a drop of 214 ft (65 m), is one of the highest waterfalls east of the Rocky Mountains. Taughannock Falls State Park, Fillmore Glen, Treman State Park, and Watkins Glen are especially scenic examples of glens and waterfalls that have been incorporated into public parks. The glens of this region are unique worldwide. They are the narrow, rocky valleys carved by rainfall's relatively quick (10,000 years) erosion of the loose shale and siltstone of this plateau of nearly level sedimentary rock. The eroded sediment ends up, e.g., along or in Cayuga Lake (Taughannock and Treman) and Seneca Lake (Watkins Glen).
Most of the area was originally forested with oak, hickory, maple, chestnut, ash, hemlock, and beech trees, but the Iroquois maintained, by annual burning, the land between Cayuga and Seneca Lakes as prairie, with herds of bison, normally thought of as a western animal. Today the Finger Lakes area is still known for fishing and hunting. Winter sports are also popular, with skiing, snowmobling and ice fishing available.
The Finger Lakes region is an important agricultural sector of New York. The rolling land between the lakes is occupied notably by vineyards (discussed below) but more commonly with other farms, mostly dairy operations, a number owned by Amish and Mennonite families in the twentieth centuries. Many Quakers settled in the nineteenth century. Farms raise corn, hay, wheat, oats, barley, and soybeans. Cabbages, sweetcorn, and potatoes are major vegetable crops. Maple syrup and honey are also local products. Cornell University (below) maintains the New York State Agricultural Experiment Station and horticultural gene bank at Geneva on the north end of Seneca Lake.
Finger Lakes cities and larger villages are situated at the head and foot of most major lakes: Skaneateles, Auburn, Ithaca, Geneva, Watkins Glen, Penn Yan, Hammondsport and Canandaigua. These historic communities with scenic situations all are tourist destinations, as is the village of Aurora, which is situated on the east shore of Cayuga Lake, and Naples, located about five miles south of Canandaigua Lake. Although not on one of the lakes, the nearby city of Corning is also a major destination for visitors, because of its famous glass museum and demonstrations. Similarly, the villages of Seneca Falls and Waterloo, although not on lakes, attract many to the several sites of the Women's Rights National Historical Park and the National Women's Hall of Fame. Likewise not on a lake but attracting many visitors is the Genesee Country Village and Museum at Mumford. Similarly, Letchworth State Park, with its famous gorge and waterfalls, draws visitors to the western end of the Finger Lakes region. The Montezuma National Wildlife Refuge at the foot of Cayuga Lake is also a major feature of the region, as is the Sonnenberg Gardens and Mansion State Historic Park at Canandaigua.
Tourism has become a major growth industry of the Finger Lakes Region. According to the New York State Department of Economic Development, taxable sales derived from tourism in one county alone exceeded ninety million dollars in a recent year (2001). Visitors spent an estimated 200 million dollars in the central Finger Lakes region, where the industry employed about fifteen thousand people.
Water quality becomes an increasing concern as population expands, with waterfront property increasingly in demand. Skaneateles Lake is the purest of the Finger Lakes, in large part because of controls imposed by the City of Syracuse, which in 2006 spent 2.3 million dollars to protect its water supply. Skaneateles Lake is deep and also has a relatively small watershed compared to other Finger Lakes. Smaller and shallower Owasco Lake, to the west, has a watershed nearly four times larger, while receiving discharge from two municipal sewage plants, but with far less pollution control.
The Finger Lakes area is New York's largest wine producing region, and the second largest in the United States behind the Napa Valley in California. Numerous wineries and vineyards are centered around Seneca, Cayuga, Canandaigua, and Keuka Lakes. Because of the lakes' great depth, they provide a lake effect to the lush vineyards that flank their shores. Retaining residual summer warmth in the winter, and winter's cold in the spring, the grapes are protected from disastrous spring frost during grape formation, and early frost before the harvest. With the passage of the Farm Winery Act in 1978, countless numbers of wineries have opened their doors to visitors from all over the world. Wineries are a major growth industry of the region, not merely contributing to the economy through production, but increasingly because they attract large numbers of visitors who support other components of tourism.
As one of the most powerful Indian nations during colonial times, the Iroquois were able to prevent European colonization of the Finger Lakes region for nearly two centuries after first contact. By the late 18th century Iroquois power had weakened, relative to the European-Americans, and internal strife eroded the political unity of the Iroquois League. During the American Revolutionary War some of the Iroquois sided with the British and some with the Americans, resulting in civil war among the Iroquois. In the late 1770s, British-allied Iroquois attacks various American frontier settlements, prompting counter-attacks, culminating in the Sullivan Expedition of 1779, which destroyed most of the Iroquois towns and effectively broke Iroquois power.
After the Revolutionary War, the Iroquois and other Indians of the region were assigned reservations. Most of their land, including the Finger Lakes region, was opened up to purchase and settlement.
Roughly the western half of the Finger Lakes region comprised the Phelps and Gorham Purchase of 1790. The region was rapidly settled at the turn of the nineteenth century, largely by a westward migration from New England, but to a lesser degree by northward influx from Pennsylvania. The regional architecture reflects these area traditions of the Federal and Greek Revival periods.
The Finger Lakes region, together with the Genesee Country of Western New York, has been referred to as the Burned-Over District, where, in the 19th century, the Second Great Awakening was a revival of Christianity, and some new religions were also formed. The region was active in reform and utopian movements. Many Underground Railroad sites have been documented. The Harriet Tubman Home at Auburn recalls the life and work of the African-American "Moses of her people."
On the northern end of the Finger Lakes is also Seneca Falls, the birthplace of the Women's suffrage movement, Waterloo, the birthplace of Memorial Day, and Palmyra, the birthplace of The Church of Jesus Christ of Latter-day Saints, also known as the Mormon Church. An annual outdoor drama, The Hill Cumorah Pageant, produced by the Mormons draws thousands of visitors each year.
Hammondsport was the home of aviation pioneer Glenn Curtiss, and the favorable air currents make the area a popular spot for glider pilots. Elmira, just to the south, was the home of Mark Twain in his later life, and the site of an infamous Civil War prison. Corning is most noted as the home of Corning Glass Works. Hornell, just southwest of the Finger Lakes was a major railroad center. Locomotives were repaired there until recently.

Notable among the historic buildings of the region (most linked below) is the Granger Homestead (1816), a large village house in Federal Style at Canandaigua, New York. Another example of the Federal Style is the Prouty-Chew House (1829) at Geneva, portions of which were altered at various times in new fashions. Three Greek Revival mansions are situated near three lakes: The Richard DeZeng House, Skaneateles (1839), Rose Hill, Geneva (1839), and Esperanza, Penn Yan (1838). The latter two are open to the public. The Seward House in Auburn, a National Historic Landmark, is a mansion more characteristic of the Civil War era, virtually unchanged from the nineteenth century. Belhurst Castle, Geneva, a stone mansion in the Romanesque Revival style, now serves as an inn. Sonnenberg mansion at Canandaigua is later nineteenth-century residence in the Queen Anne style, known for its restored period gardens. Geneva on the Lake is a villa (1910-14) that recalls those on Italian lakes. Now an inn, it has exceptional gardens in the European manner. Many buildings and historic districts of the Finger Lakes region are notable, other than these historic houses.
3365 mi[1] (0 km)
1926[1]
US 101 in Newport, OR
I-5 at Albany, OR
I-15 at Idaho Falls, ID
I-25 at Casper, WY
I-29 at Sioux City, IA
I-35 near Williams, IA
I-55 near Chicago, IL
I-75 near Toledo, OH
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Lakes
The Finger Lakes from east to west (the first seven being commonly identified as Finger Lakes):- Otisco Lake
- Skaneateles Lake
- Owasco Lake
- Cayuga Lake
- Seneca Lake
- Keuka Lake
- Canandaigua Lake
- Honeoye Lake
- Canadice Lake
- Hemlock Lake
- Conesus Lake
Cazenovia Lake to the east, although smaller, is sometimes called "the eighth Finger Lake," because it is similar in shape, located in Appalachian hill terrain, with a historic village linked to other Finger Lakes by US Route 20. It may have been formed in the same manner as the Finger Lakes, as satellite photos show three valleys similar in character and spacing to the Finger Lakes east of Otisco Lake. The first is the Tully Valley, which includes a chain of small lakes at the south end that could be a "Finger Lake" that never formed because of a terminal moraine. The moraine caused the Tioughnioga River to flow south instead of north, the opposite of the other waters of the Finger Lakes. The next two valleys to the east contain Butternut Creek, which flows north, and the East Branch of the Tioughnioga River, which flows south. The next valley contains Limestone Creek, which flows north. The next valley after that contains Cazenovia Lake.
Oneida Lake, to the northeast of Syracuse, New York, is sometimes included as the "thumb," although it is shallow and somewhat different in character from the rest. Onondaga Lake, though located just north of the Finger Lakes region, is not considered one of the Finger Lakes. Conesus, Hemlock, Canadice, Honeoye, and Otisco are considered the minor Finger Lakes. Other, smaller lakes, including Silver, Waneta, and Lamoka lakes, dot this region. However, Waneta and Lamoka lakes are part of the Susquehanna River watershed as they drain into a tributary of the Chemung River.
East of Oneida and Cazenovia Lakes are the headwaters of the Susquehanna River and Hudson River watersheds (the latter through the Mohawk Valley).
Region
The Finger Lakes were modified by glaciers, but were not simply gouged out by glacial action, as often asserted. The present lakes were preglacial stream valleys or earlier lakes. Glaciers modified the terrain somewhat, but more critically: when the ice retreated, deposits left behind dammed the valleys, impounding water. The deep valley south of Syracuse, seen from Interstate 81, might have been another Finger Lake, had the glacier's recessional moraine been deposited farther north rather than at Tully, New York.The Finger Lakes are situated on the northern edge of the Appalachian Upland. They now drain northward to Lake Ontario. The southern ends of the lakes are characterized by steeper hills etched by streams running toward the lakes below. Glacial hanging valleys, terraces in the descent toward the lakes, often end with waterfalls. Taughannock Falls, with a drop of 214 ft (65 m), is one of the highest waterfalls east of the Rocky Mountains. Taughannock Falls State Park, Fillmore Glen, Treman State Park, and Watkins Glen are especially scenic examples of glens and waterfalls that have been incorporated into public parks. The glens of this region are unique worldwide. They are the narrow, rocky valleys carved by rainfall's relatively quick (10,000 years) erosion of the loose shale and siltstone of this plateau of nearly level sedimentary rock. The eroded sediment ends up, e.g., along or in Cayuga Lake (Taughannock and Treman) and Seneca Lake (Watkins Glen).
Most of the area was originally forested with oak, hickory, maple, chestnut, ash, hemlock, and beech trees, but the Iroquois maintained, by annual burning, the land between Cayuga and Seneca Lakes as prairie, with herds of bison, normally thought of as a western animal. Today the Finger Lakes area is still known for fishing and hunting. Winter sports are also popular, with skiing, snowmobling and ice fishing available.
The Finger Lakes region is an important agricultural sector of New York. The rolling land between the lakes is occupied notably by vineyards (discussed below) but more commonly with other farms, mostly dairy operations, a number owned by Amish and Mennonite families in the twentieth centuries. Many Quakers settled in the nineteenth century. Farms raise corn, hay, wheat, oats, barley, and soybeans. Cabbages, sweetcorn, and potatoes are major vegetable crops. Maple syrup and honey are also local products. Cornell University (below) maintains the New York State Agricultural Experiment Station and horticultural gene bank at Geneva on the north end of Seneca Lake.
Finger Lakes cities and larger villages are situated at the head and foot of most major lakes: Skaneateles, Auburn, Ithaca, Geneva, Watkins Glen, Penn Yan, Hammondsport and Canandaigua. These historic communities with scenic situations all are tourist destinations, as is the village of Aurora, which is situated on the east shore of Cayuga Lake, and Naples, located about five miles south of Canandaigua Lake. Although not on one of the lakes, the nearby city of Corning is also a major destination for visitors, because of its famous glass museum and demonstrations. Similarly, the villages of Seneca Falls and Waterloo, although not on lakes, attract many to the several sites of the Women's Rights National Historical Park and the National Women's Hall of Fame. Likewise not on a lake but attracting many visitors is the Genesee Country Village and Museum at Mumford. Similarly, Letchworth State Park, with its famous gorge and waterfalls, draws visitors to the western end of the Finger Lakes region. The Montezuma National Wildlife Refuge at the foot of Cayuga Lake is also a major feature of the region, as is the Sonnenberg Gardens and Mansion State Historic Park at Canandaigua.
Tourism has become a major growth industry of the Finger Lakes Region. According to the New York State Department of Economic Development, taxable sales derived from tourism in one county alone exceeded ninety million dollars in a recent year (2001). Visitors spent an estimated 200 million dollars in the central Finger Lakes region, where the industry employed about fifteen thousand people.
Water quality becomes an increasing concern as population expands, with waterfront property increasingly in demand. Skaneateles Lake is the purest of the Finger Lakes, in large part because of controls imposed by the City of Syracuse, which in 2006 spent 2.3 million dollars to protect its water supply. Skaneateles Lake is deep and also has a relatively small watershed compared to other Finger Lakes. Smaller and shallower Owasco Lake, to the west, has a watershed nearly four times larger, while receiving discharge from two municipal sewage plants, but with far less pollution control.
Wine
Vineyard overlooking Canandaigua Lake, from Route 21
History
The Finger Lakes region is a central part of the Iroquois homeland. The Iroquois tribes include the Seneca and Cayuga tribes, for which the two largest Finger Lakes are named. The Tuscarora tribe lived in the Finger Lakes region as well. The Onondaga and Oneida tribes lived at the eastern edge of the region, closer to their namesake lakes, Lake Oneida and Onondaga Lake. The sixth Iroquois tribe, the Mohawk, lived farther east. During colonial times, many other tribes moved to the Finger Lakes region, seeking the protection of the Iroquois. For example, remnants of several tribes of North Carolina, collectively called the Tutelo, moved to the town of Coreorgonel at the south end of Cayuga Lake near present-day Ithaca. Major Iroquois towns in the Finger Lakes region included the Seneca town of Gen-nis-he-yo (present-day Geneseo), Kanadaseaga (Seneca Castle, near present-day Geneva), Goiogouen (Cayuga Castle, east of Cayuga Lake), Chonodote (Cayuga town, present-day Aurora), and Catherine's Town (near present-day Watkins Glen).As one of the most powerful Indian nations during colonial times, the Iroquois were able to prevent European colonization of the Finger Lakes region for nearly two centuries after first contact. By the late 18th century Iroquois power had weakened, relative to the European-Americans, and internal strife eroded the political unity of the Iroquois League. During the American Revolutionary War some of the Iroquois sided with the British and some with the Americans, resulting in civil war among the Iroquois. In the late 1770s, British-allied Iroquois attacks various American frontier settlements, prompting counter-attacks, culminating in the Sullivan Expedition of 1779, which destroyed most of the Iroquois towns and effectively broke Iroquois power.
After the Revolutionary War, the Iroquois and other Indians of the region were assigned reservations. Most of their land, including the Finger Lakes region, was opened up to purchase and settlement.
Roughly the western half of the Finger Lakes region comprised the Phelps and Gorham Purchase of 1790. The region was rapidly settled at the turn of the nineteenth century, largely by a westward migration from New England, but to a lesser degree by northward influx from Pennsylvania. The regional architecture reflects these area traditions of the Federal and Greek Revival periods.
The Finger Lakes region, together with the Genesee Country of Western New York, has been referred to as the Burned-Over District, where, in the 19th century, the Second Great Awakening was a revival of Christianity, and some new religions were also formed. The region was active in reform and utopian movements. Many Underground Railroad sites have been documented. The Harriet Tubman Home at Auburn recalls the life and work of the African-American "Moses of her people."
On the northern end of the Finger Lakes is also Seneca Falls, the birthplace of the Women's suffrage movement, Waterloo, the birthplace of Memorial Day, and Palmyra, the birthplace of The Church of Jesus Christ of Latter-day Saints, also known as the Mormon Church. An annual outdoor drama, The Hill Cumorah Pageant, produced by the Mormons draws thousands of visitors each year.
Hammondsport was the home of aviation pioneer Glenn Curtiss, and the favorable air currents make the area a popular spot for glider pilots. Elmira, just to the south, was the home of Mark Twain in his later life, and the site of an infamous Civil War prison. Corning is most noted as the home of Corning Glass Works. Hornell, just southwest of the Finger Lakes was a major railroad center. Locomotives were repaired there until recently.
Granger Homestead, 1816, Canandaigua
Notable among the historic buildings of the region (most linked below) is the Granger Homestead (1816), a large village house in Federal Style at Canandaigua, New York. Another example of the Federal Style is the Prouty-Chew House (1829) at Geneva, portions of which were altered at various times in new fashions. Three Greek Revival mansions are situated near three lakes: The Richard DeZeng House, Skaneateles (1839), Rose Hill, Geneva (1839), and Esperanza, Penn Yan (1838). The latter two are open to the public. The Seward House in Auburn, a National Historic Landmark, is a mansion more characteristic of the Civil War era, virtually unchanged from the nineteenth century. Belhurst Castle, Geneva, a stone mansion in the Romanesque Revival style, now serves as an inn. Sonnenberg mansion at Canandaigua is later nineteenth-century residence in the Queen Anne style, known for its restored period gardens. Geneva on the Lake is a villa (1910-14) that recalls those on Italian lakes. Now an inn, it has exceptional gardens in the European manner. Many buildings and historic districts of the Finger Lakes region are notable, other than these historic houses.
Educational institutions
The area is also known for education, with the largest institution being Cornell University in Ithaca, the state land grant institution. Its alma mater begins "Far Above Cayuga's Waters", because it is on the hills overlooking the city of Ithaca and the southern end of Cayuga Lake. There are also the State Universities of New York at Geneseo and Cortland, Ithaca College in Ithaca, Hobart and William Smith Colleges in Geneva, Wells College in Aurora, also on Cayuga Lake, Keuka College, New York Chiropractic College in Seneca Falls, and several community colleges.References
- Thompson, John H., ed. Geography of New York State (Syracuse: Syracuse University Press, 1977)
- Engeln, O. D., von. ''The Finger Lakes Region: Its Origin and Nature (Ithaca: Cornell University Press, 1961, 1988)
- Finger Lakes Tourism Statistics http://www.visitfingerlakes.com/media_room/statistics.asp
External links
- Formation of the Finger Lakes
- Woman's Rights National Park, Seneca Falls
- National Women's Hall of Fame, Seneca Falls
- New York State Parks, Finger Lakes Region
- Harriet Tubman Home, Auburn
- Granger Homestead, Canandaigua
- Rose Hill Mansion, Geneva
- Seward House, Auburn
- Sonnenberg Gardens, Canandaigua
- Genesee Country Village Museum, Mumford
- Plant Genetics Resource Unit at Geneva
- Finger Lakes State Parks
- * Maps and aerial photos for Coordinates:
- Maps from , Google Maps, Live Search Maps, Yahoo! Maps, or MapQuest
- Topographic maps from TopoZone or TerraServer-USA
Upstate New York is the region of New York State north of the core of the New York metropolitan area. It has a population of 7,121,911 out of New York State's total 18,976,457. Were it an independent state, it would be ranked 13th by population.
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Coordinates
Lake type glacial
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Lake type glacial
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Coordinates
Lake type glacial
Primary sources
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Lake type glacial
Primary sources
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Location New York
Coordinates
Lake type glacial
Primary outflows
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Coordinates
Lake type glacial
Primary outflows
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Coordinates
Lake type glacial
Basin countries USA
Max length 16 miles (25.
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Lake type glacial
Basin countries USA
Max length 16 miles (25.
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Location New York
Coordinates
Lake type glacial
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Coordinates
Lake type glacial
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Coordinates
Lake type glacial
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Lake type glacial
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Coordinates
Lake type glacial
Primary sources
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Lake type glacial
Primary sources
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Coordinates
Lake type glacial
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Lake type glacial
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Coordinates
Lake type glacial
Basin countries USA
Max length 16 miles (25 km)
Max width 1.5 miles (2.
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Lake type glacial
Basin countries USA
Max length 16 miles (25 km)
Max width 1.5 miles (2.
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Location Ontario County, New York
Coordinates
Lake type Glacial
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Coordinates
Lake type Glacial
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Coordinates
Lake type glacial
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Lake type glacial
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Location Livingston County, New York
Coordinates
Lake type glacial
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Coordinates
Lake type glacial
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Coordinates
Lake type glacial
Basin countries USA
Max width 8 miles (13 km)
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Lake type glacial
Basin countries USA
Max width 8 miles (13 km)
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Location New York
Primary sources Swamplands to the north
Primary outflows Chittenango Creek
Basin countries United States
Max length
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Primary sources Swamplands to the north
Primary outflows Chittenango Creek
Basin countries United States
Max length
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3365 mi[1] (0 km)
1926[1]
US 101 in Newport, OR
I-5 at Albany, OR
I-15 at Idaho Falls, ID
I-25 at Casper, WY
I-29 at Sioux City, IA
I-35 near Williams, IA
I-55 near Chicago, IL
I-75 near Toledo, OH
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Tully, New York may refer to:
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- Tully, New York (town)
- Tully, New York (village)
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Moraine refers to any glacially formed accumulation of unconsolidated debris which can occur in currently glaciated and formerly glaciated regions, such as those areas acted upon by a past ice age.
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The Tioughnioga River (tei-uhf-nee-O-guh) is a tributary of the Chenango River, approximately 70 miles (113 km) long, in central New York in the United States. It drains a dissected plateau area east of the Finger Lakes at the northernmost edge of the watershed of the
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Location New York
Primary sources Oneida Creek
Primary outflows Oneida River
Basin countries United States
Max length 21 mi (33 km)
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Primary sources Oneida Creek
Primary outflows Oneida River
Basin countries United States
Max length 21 mi (33 km)
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City of Syracuse
A view of the Downtown Syracuse skyline
Seal
Nickname: The Salt City
Location of Syracuse within the state of New York
Coordinates:
Country
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A view of the Downtown Syracuse skyline
Seal
Nickname: The Salt City
Location of Syracuse within the state of New York
Coordinates:
Country
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Location Syracuse,New York
Basin countries United States
Max length 5 mi (8 km)
Max width 1 mi (1.5 km)
Surface area 4.6 sq mi (11.
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Basin countries United States
Max length 5 mi (8 km)
Max width 1 mi (1.5 km)
Surface area 4.6 sq mi (11.
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Location western New York
Coordinates
Lake type alkaline
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Coordinates
Lake type alkaline
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Susquehanna River
Country | USA
States | Maryland,Pennsylvania,New York
Major cities |
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Susquehanna River near Chesapeake Bay
Country | USA
States | Maryland,Pennsylvania,New York
Major cities |
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Chemung River
Country | United States
States | New York,Pennsylvania
Counties |
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The Chemung River at Elmira, New York
Country | United States
States | New York,Pennsylvania
Counties |
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Headstream is the origin of water flow that initiates the subject watercourse. It is the start of the river or stream.
The source of a river or stream may be a lake, a marsh, a spring, glacier, or a collection of headwaters.
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The source of a river or stream may be a lake, a marsh, a spring, glacier, or a collection of headwaters.
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Susquehanna River
Country | USA
States | Maryland,Pennsylvania,New York
Major cities |
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Susquehanna River near Chesapeake Bay
Country | USA
States | Maryland,Pennsylvania,New York
Major cities |
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Hudson River (Muh-he-kun-ne-tuk or Muhheakantuck)
Country | USA
States |
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Looking upriver from the Bear Mountain Bridge
Country | USA
States |
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The Mohawk Valley region of the U.S. state of New York is a suburban and rural area surrounding the industrialized cities of Utica and Rome, along with other smaller commercial centers.
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glacier is a large, slow moving river of ice, formed from compacted layers of snow, that slowly deforms and flows in response to gravity. Glacier ice is the largest reservoir of fresh water on Earth, and second only to oceans as the largest reservoir of total water.
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Herod_Archelaus