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Coordinates: 43°15′30″N 77°36′08″W / 43.25833°N 77.60222°W / 43.25833; -77.60222
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{{Short description|River in New York and Pennsylvania}}
{{Infobox river
{{Infobox river
| name = Genesee River
| name = Genesee River
| name_native = Čunehstí•yu•<ref>{{Cite book |title=History of Rochester and Monroe county, New York |last=Peck |first=William |year=1908 |page=[https://archive.org/details/bub_gb_IvssAAAAYAAJ/page/n23 15] |url=https://archive.org/details/bub_gb_IvssAAAAYAAJ |accessdate=April 4, 2009 |publisher=The Pioneer publishing company}}<br>'''NOTE''': Čunehstí•yu• is from the [[Seneca tribe]] name ''Chin-u-shio'' ([[Tuscarora language]]) meaning ''a beautiful open valley''.</ref>
| name_native = {{native name|tus|Čunehstí•yu•}}<ref>{{Cite book |title=History of Rochester and Monroe county, New York |last=Peck |first=William |year=1908 |page=[https://archive.org/details/bub_gb_IvssAAAAYAAJ/page/n23 15] |url=https://archive.org/details/bub_gb_IvssAAAAYAAJ |access-date=April 4, 2009 |publisher=The Pioneer publishing company}}<br>'''NOTE''': Čunehstí•yu• is from the [[Seneca tribe]] name ''Chin-u-shio'' ([[Tuscarora language]]) meaning ''a beautiful open valley''.</ref>
| name_native_lang =
| name_native_lang =
| name_other =
| name_other =
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| image = Genesee river 9044.jpg
| image = Genesee river 9044.jpg
| image_caption = Genesee River near [[Belmont, New York|Belmont]]
| image_caption = Genesee River near [[Belmont, New York|Belmont]]
| map = Genesee map large.jpg
| map = Genesee River Watershed.png
| map_size = 300
| map_size = 300
| map_caption = Map of Genesee River
| map_caption = Genesee River watershed ([https://mghydro.com/watersheds/shared/F15986.html Interactive map])
| pushpin_map =
| pushpin_map =
| pushpin_map_size = 300
| pushpin_map_size = 300
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| subdivision_type2 = State
| subdivision_type2 = State
| subdivision_name2 = [[New York (state)|New York]], [[Pennsylvania]]
| subdivision_name2 = [[New York (state)|New York]], [[Pennsylvania]]
| subdivision_type3 = [[County (United States)|Counties]] &<br>Tributaries
| subdivision_type3 = [[County (United States)|Counties]]
| subdivision_name3 = (see [[Genesee River#References|Navbox, below]])
| subdivision_name3 = (see [[Genesee River#References|Navbox, below]])
| subdivision_type4 =
| subdivision_type4 =
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<!---------------------- BASIN FEATURES -->
<!---------------------- BASIN FEATURES -->
| source1 =
| source1 =
| source1_location = [[Ulysses Township, Potter County, Pennsylvania|Ulysses Township]], [[Potter County, Pennsylvania|Potter County]], [[Pennsylvania]]
| source1_location = [[Ulysses Township, Pennsylvania|Ulysses Township]], [[Potter County, Pennsylvania|Potter County]], [[Pennsylvania]]
| source1_coordinates= {{coord|41|53|33|N|77|43|54|W|display=inline}}<ref name=gnis/>
| source1_coordinates= {{coord|41|53|33|N|77|43|54|W|display=inline}}<ref name=gnis/>
| source1_elevation = {{convert|2275|ft|abbr=on}}<ref>''Harrison Valley, PA,'' 7.5 Minute Topographic Quadrangle, USGS, 1957 (1971 rev)</ref>
| source1_elevation = {{convert|2275|ft|abbr=on}}<ref>''Harrison Valley, PA,'' 7.5 Minute Topographic Quadrangle, USGS, 1957 (1971 rev)</ref>
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| extra =
| extra =
}}
}}
The '''Genesee River''' is a [[tributary]] of [[Lake Ontario]] flowing northward through the [[Twin Tiers]] of [[Pennsylvania]] and [[New York (state)|New York]] in the United States.
The '''Genesee River''' ({{IPAc-en|ˌ|dʒ|ɛ|n|ɪ|ˈ|s|iː}} {{respell|JEN|iss|EE}}) is a [[tributary]] of [[Lake Ontario]] flowing northward through the [[Twin Tiers]] of [[Pennsylvania]] and [[New York (state)|New York]] in the United States. The river contains several waterfalls in New York at [[Letchworth State Park]] and [[Rochester, New York|Rochester]].


The river provided the original power for the Rochester area's 19th century mills and still provides hydroelectric power for downtown Rochester.
The river was historically used as a border between the lands of the [[Seneca people|Seneca]] to the east and the [[Erie people|Erie]] and [[Wenrohronon|Wenro]] to the west. Later, the river provided the original power for the Rochester area's 19th century mills, and still provides hydroelectric power for downtown Rochester. Flooding occurred periodically in the river valley before construction of the [[Mount Morris Dam]] in the 1950s.


==Geology==
==Geology==
[[File:Letchworth State Park Upper Falls and Genesee Arch Bridge July 2022.jpeg|thumb|left|[[Portage Viaduct]] below Upper Falls in Letchworth State Park]]
The Genesee is the remaining western branch of [[Glacial geology of the Genesee River|a preglacial system]], with rock layers tilted an average of 40 feet (12 m) per mile, so the river flows across progressively older bedrock as it flows northward. It begins in exposing the [[Allegheny Plateau]]'s characteristic [[conglomerate (geology)|conglomerates]]: [[sandstone]]s and [[shale]]s in the {{nowrap|[[rock (geology)|rock]] [[geologic record|column]]s}} of the [[Mississippian age|Mississippian]] and [[Pennsylvanian (geology)|Pennsylvanian]] subperiods. Thereafter, further downstream as it traverses the area known as ''The Grand Canyon of the East'',<ref name=StParkBlurb>[http://www.letchworthpark.com/ Letchworth State Park], accessdate=2016-06-05</ref> where it falls (three times) through over 600 feet (180 m)<ref name=StParkBlurb/> as to passes through the gorges in New York's [[Letchworth State Park]], the river also often exposes older rocks such as [[shale]]s (some rich in hydrocarbons<ref>Such layers often allow carbon-14 dating to synchronize subdisciplines of stratigraphy</ref>), [[siltstone]]s and some [[limestone]]s of the [[Devonian]] period at Letchworth and, at other canyons with three more waterfalls<ref name=upper>[http://www.cityofrochester.gov/article.aspx?id=8589936495 High falls & Browns race area], City of Rochester, accessdate=2016-06-05</ref><ref name=center>[http://www.cityofrochester.gov/lowergorge/ downtown falls area], City of Rochester, accessdate=2016-06-05</ref><ref name=lowerfalls>[http://www.lowerfalls.org/ MAPLEWOOD/LOWER FALLS - Rochester, NY], accessdate=2016-06-05</ref> at Rochester cuts through the [[Niagara Escarpment]] exposing limestones and shales of [[Silurian]] age in the rock column. With cuttings in the geologic record showing so many early ages, the river area has a great variety of [[fossil]]s for paleobiological and [[stratigraphic]] analysis.
The Genesee is the remaining western branch of [[Glacial geology of the Genesee River|a preglacial system]], with rock layers tilted an average of 40 feet (12 m) per mile, so the river flows across progressively older bedrock as it flows northward. It begins in exposing the [[Allegheny Plateau]]'s characteristic [[conglomerate (geology)|conglomerates]]: [[sandstone]]s and [[shale]]s in the {{nowrap|[[rock (geology)|rock]] [[geologic record|column]]s}} of the [[Mississippian age|Mississippian]] and [[Pennsylvanian (geology)|Pennsylvanian]] subperiods. Thereafter, farther downstream as it traverses the area known as ''The Grand Canyon of the East'',<ref name=StParkBlurb>[http://www.letchworthpark.com/ Letchworth State Park], accessdate=2016-06-05</ref> where it falls (three times) through over 600 feet (180 m)<ref name=StParkBlurb/>. As it passes through the gorges in New York's [[Letchworth State Park]], the river also often exposes older rocks such as [[shale]]s (some rich in hydrocarbons<ref>Such layers often allow carbon-14 dating to synchronize subdisciplines of stratigraphy</ref>), [[siltstone]]s and some [[limestone]]s of the [[Devonian]] period at Letchworth and, at other canyons with three more waterfalls<ref name=upper>[http://www.cityofrochester.gov/article.aspx?id=8589936495 High falls & Browns race area], City of Rochester, accessdate=2016-06-05</ref><ref name=center>[http://www.cityofrochester.gov/lowergorge/ downtown falls area], City of Rochester, accessdate=2016-06-05</ref><ref name=lowerfalls>[http://www.lowerfalls.org/ MAPLEWOOD/LOWER FALLS - Rochester, NY], accessdate=2016-06-05</ref> at Rochester cuts through the [[Niagara Escarpment]], exposing limestones and shales of [[Silurian]] age in the rock column. With cuttings in the geologic record showing so many early ages, the river area has a great variety of [[fossil]]s for paleobiological and [[stratigraphic]] analysis.


During the past million years, [[Glacier|four glacial ages]] covered the [[Rochester, New York|Rochester]] area. The southern edges of the [[Laurentide Ice Sheet]] and those advances impacted the formation geology and geography of the area. The most recent glacier that left evidence here was about 10,000 years ago and it caused compression of the earth by as much as 2,500 feet (760 m).<ref name="Glacial 100K">{{cite web |title=Geology: 100,000 years ago |url=http://www.vintageviews.org/vv-tl/timeline/geology.html#100,000 |url-status=dead |archive-url=https://web.archive.org/web/20080603092054/http://www.vintageviews.org/vv-tl/timeline/geology.html#100,000#100,000 |archive-date=2008-06-03 |access-date=July 11, 2008 |work=Rochester's History: An Illustrated Timeline}}</ref> About 12,000 years ago, the area underwent massive changes, which included the rerouting of the Genesee and other water bodies. The pre-[[ice age]] eastern branch of the Genesee runs south of Mount Morris and was completely diverted by extensive terminal [[moraine]]s in [[Livingston County, New York|Livingston County]] with a key blocking dam just south of [[Dansville, Livingston County, New York|Dansville]], so most of the upper section of the ancient river was diverted instead to fall the off [[Appalachian Plateau]] toward the [[Susquehanna River]] system (to an eventual destination well to the southeast).
==History==
During the past million years there were [[Glacier|four glacial ages]] that covered the [[Rochester, New York|Rochester]] area with the southern edges of the [[Laurentide Ice Sheet]] and those advances were major impactors in the formation geology and geography of the area. The most recent glacier that left evidence here was about 10,000 years ago and it caused compression of the earth by as much as 2,500 feet (760 m).<ref name="Glacial 100K">{{cite web|url=http://www.vintageviews.org/vv-tl/timeline/geology.html#100,000|title=Geology: 100,000 years ago|work=Rochester's History: An Illustrated Timeline|accessdate=July 11, 2008|archive-url=https://web.archive.org/web/20080603092054/http://www.vintageviews.org/vv-tl/timeline/geology.html#100,000#100,000|archive-date=2008-06-03|url-status=dead}}</ref> About 12,000 years ago, the area underwent massive changes, which included the rerouting of the Genesee and other water bodies. The pre-[[ice age]] eastern branch of the Genesee runs south of Mount Morris and was completely diverted by extensive terminal [[moraine]]s in [[Livingston County, New York|Livingston County]] with a key blocking dam just south of [[Dansville, Livingston County, New York|Dansville]], so most of the upper section of the ancient river was diverted instead to fall the off [[Appalachian Plateau]] toward the [[Susquehanna River]] system (to an eventual destination well to the southeast).


Currently only a small creek flows in what is left of this large paleogeologic valley. The area of the lower river was also affected. Since the earth rebounded from the melting glaciers more rapidly in Canada than in New York, water from Lake Ontario was spilled over New York due to its lower elevation. During this time, the original outlet of the Genesee River, Irondequoit Bay, was flooded out, creating the current bay. As these waters later retreated, glacial debris caused the river to be rerouted to the west along its current path.<ref name="Glacial 12K">{{cite web|url=http://www.vintageviews.org/vv-tl/timeline/geology.html#12,000|title=Geology: 12,000 years ago|work=Rochester's History: An Illustrated Timeline|accessdate=July 11, 2008|archive-url=https://web.archive.org/web/20080603092054/http://www.vintageviews.org/vv-tl/timeline/geology.html#12,000#12,000|archive-date=2008-06-03|url-status=dead}}</ref>
Only a small creek ([[Irondequoit Creek]]) flows in what is left of this large paleogeologic valley. The area of the lower river was also affected. Since the earth rebounded from the melting glaciers more rapidly in Canada than in New York, water from Lake Ontario was spilled over New York due to its lower elevation. During this time, the original outlet of the Genesee River, [[Irondequoit Bay]], was flooded out, creating the current bay. As these waters later retreated, glacial debris caused the river to be rerouted to the west along its current path.<ref name="Glacial 12K">{{cite web |title=Geology: 12,000 years ago |url=http://www.vintageviews.org/vv-tl/timeline/geology.html#12,000 |url-status=dead |archive-url=https://web.archive.org/web/20080603092054/http://www.vintageviews.org/vv-tl/timeline/geology.html#12,000#12,000 |archive-date=2008-06-03 |access-date=July 11, 2008 |work=Rochester's History: An Illustrated Timeline}}</ref><ref>{{Cite journal |last=Rogers |first=Brownell |date=1893 |title=The Genesee River |url=https://zenodo.org/record/1448335 |journal=Science |volume=21 |issue=526 |pages=121 |doi=10.1126/science.ns-21.526.121|pmid=17814804 }}</ref>


==History==
The [[Seneca nation]] traditionally lived between the Genesee River and [[Canandaigua Lake]].<!--SOURCE: Seneca nation WIKIARTICLE--> The region was surveyed by [[Thomas Davies (British Army officer)|Thomas Davies]] in 1766. The High Falls was then also known as the Great Seneca Falls, and the Genesee River was also spelled Zinochsaa by early writers.<ref>Supplement to [[Dobson's Encyclopedia]] volume 3, which cites [[Jedidiah Morse]] as its source, probably the American Gazetteer, 1795</ref>
The [[Seneca nation]] traditionally lived between the Genesee River and [[Canandaigua Lake]].<!--SOURCE: Seneca nation WIKIARTICLE--> The region was surveyed by [[Thomas Davies (British Army officer)|Thomas Davies]] in 1766. The High Falls was then also known as the Great Seneca Falls, and the Genesee River was also spelled Zinochsaa by early writers.<ref>Supplement to [[Dobson's Encyclopedia]] volume 3, which cites [[Jedidiah Morse]] as its source, probably the American Gazetteer, 1795</ref>


Historically, the river's gorge formed a clearly demarcated border between the lands of the [[Five Nations of the Iroquois]], whose range extended east and the related tribes of the [[Erie people]] and [[Wenrohronon|Wenro]] along the west side of the gorge. By the end of the [[Beaver Wars]] and the American Revolution, the lands in all of upstate New York into the [[Ohio Country]] were controlled by the Iroquois Confederation, but were also effectively depopulated, the tribes weakened in the Revolution. In 1779, on the orders of [[George Washington]], the [[Sullivan Expedition]] destroyed over 40 Haudenosaunee villages in and around the watershed to force the Seneca and allied nations out of the newly formed United States. Subsequently, with most Iroquois having fled to Canada, the remnant tribal groups were in no position to further impede white settlers, so most of New York state west of the Genesee River became part of the [[Holland Purchase]] after the [[American Revolution]].<!--THIS IS ABOUT THE LAND, NOT THE RIVER: So, and yep (put back) --> From 1801 to 1846 the entire region was sold to individual owners from the Holland Land office in [[Batavia, New York]]. In the 1797 [[Treaty of Big Tree]], the Seneca tribes were granted six reservations along the river, among them [[Canawaugus]], [[Little Beard's Town]], Geneseo, Caneadea, Deyuitgau and Gardeau. In August 1826, the [[David A. Ogden|Ogden Land Company]] purchased the six Genesee River reservations from the Seneca, allegedly under duress;<ref name="Sagoyewatha2006">{{cite book|last1=Red Jacket (Seneca chief)|title=The Collected Speeches of Sagoyewatha, Or Red Jacket|date=2006|publisher=[[Syracuse University Press]]|isbn=9780815630968|url=https://books.google.com/books?id=JP27XEqTNycC&pg=PA285|accessdate=May 8, 2017|language=en}}</ref> the modern [[Seneca Nation of Indians]] does not recognize the 1826 sale as valid and moved to reclaim Canawaugus in December 2022.<ref name=canawaugus-repurchase>{{Cite web |last=Quigley |first=Kellen |date=December 31, 2022 |title=Seneca Nation purchases ancestral Genesee Valley land |url=https://www.salamancapress.com/news/seneca-nation-purchases-ancestral-genesee-valley-land/article_7fcb785a-885b-11ed-9c26-87556795cadf.html |access-date=2022-12-31 |website=The [[Salamanca Press]] |language=en}}</ref>
If "not for hydropower, the flour mills, clothing mills, and tool fabricators would not have located in Rochester",<ref name="RochesterPower">{{cite journal |last=Baily |first=Rod |date=October 1984|title=Sources of Energy in Rochester's History|journal=Rochester History |volume=XLVI |issue=3-4 | publisher=Rochester Public Library | issn =0035-7413 |url=http://www.rochester.lib.ny.us/~rochhist/v46_1984/v46i3-4.pdf |accessdate=December 29, 2009 |quote=''Hydropower has never contributed more than two and a half percent of the total energy supply of Rochester''}}</ref> and the 1825 [[Erie Canal]] allowed the mills to ship products to [[New York City]]. A few hundred feet north of the center of the village of Rochester, the Erie Canal crossed the Genesee River via an 1823 stone aqueduct (802 feet (244 m) long, 17 feet (5.2 m) wide), which was replaced by the [[Erie Canal: Second Genesee Aqueduct|Second Genesee Aqueduct in 1842]].

Historically, the river's gorge formed a clearly demarcated border between the lands of the [[Five Nations of the Iroquois]], whose range extended east and the related tribes of the [[Erie people]] along the west side of the gorge. By the end of the [[Beaver Wars]] and the American Revolution, the lands in all of upstate New York into the [[Ohio Country]] were controlled by the Iroquois Confederation, but were also effectively depopulated, the tribes weakened in the Revolution. In 1779, on the orders of [[George Washington]], the [[Sullivan Expedition]] destroyed over 40 Haudenosaunee villages in and around the watershed, committing clear acts of [[genocide]] to force the Seneca and allied nations out of the newly formed United States. Subsequently, with most Iroquois having fled to Canada, the remnant tribal groups were in no position to further impede white settlers, so most of New York state west of the Genesee River became part of the [[Holland Purchase]] after the [[American Revolution]].<!--THIS IS ABOUT THE LAND, NOT THE RIVER: So, and yep (put back) --> From 1801 to 1846 the entire region was sold to individual owners from the Holland Land office in [[Batavia, New York]]. The river demarcates the "Genesee Country" of New York to the west<!-- But it follows the history well, so no cite needed. Check history first in etymology! {{Citation needed|reason=Even the Holland Purchase wikiarticle doesn't have a source for this name|date=December 2008}}---> and the [[Finger Lakes]] geographic region, and heartland of the Iroquois to the east.


On Friday, November 13, 1829 (Friday the 13th), the daredevil [[Sam Patch]] jumped to his death before 8,000 spectators at the [[:File:Upper fallspost.jpg|Upper Falls in Rochester]].
On Friday, November 13, 1829 (Friday the 13th), the daredevil [[Sam Patch]] jumped to his death before 8,000 spectators at the [[:File:Upper fallspost.jpg|Upper Falls in Rochester]].


If "not for hydropower, the flour mills, clothing mills, and tool fabricators would not have located in Rochester",<ref name="RochesterPower">{{cite journal |last=Baily |first=Rod |date=October 1984 |title=Sources of Energy in Rochester's History |url=http://www.rochester.lib.ny.us/~rochhist/v46_1984/v46i3-4.pdf |journal=Rochester History |publisher=Rochester Public Library |volume=XLVI |issue=3–4 |issn=0035-7413 |access-date=December 29, 2009 |quote=''Hydropower has never contributed more than two and a half percent of the total energy supply of Rochester'' |archive-date=March 27, 2009 |archive-url=https://web.archive.org/web/20090327043430/http://www.rochester.lib.ny.us/~rochhist/v46_1984/v46i3-4.pdf |url-status=dead }}</ref> and the 1825 [[Erie Canal]] allowed the mills to ship products to [[New York City]]. A few hundred feet north of the center of the village of Rochester, the Erie Canal crossed the Genesee River via an 1823 stone aqueduct (802 feet (244 m) long, 17 feet (5.2 m) wide), which was replaced by the [[Erie Canal: Second Genesee Aqueduct|Second Genesee Aqueduct in 1842]].
In 1836 the [[Genesee Valley Canal]] was begun to build a new canal from the [[Erie Canal]] near Rochester, up the Genesee Valley, across to the [[Allegheny River]] at [[Olean, New York|Olean]]. Construction of new sections extended upriver (southward) until 1880. Although an important commercial route, the canal was plagued by frequent flood damage and the final leg down the Allegany River was never completed. The most difficult section to build was the bypass around the gorge and falls at present day Letchworth Park. The canal followed the old [[Native Americans of the United States|Native American]] [[portage]] route, which necessitated many locks. These old locks can still be seen near Nunda. The project was abandoned and the right of way was sold in 1880. The property became the roadbed for the [[Genesee Valley Canal Railroad]], which eventually merged with the [[Pennsylvania Railroad]]. Much of the canal and railroad right-of-way is open to the public today as the [[Genesee Valley Greenway]], which was started in 1991.

In 1836 the [[Genesee Valley Canal]] was begun to build a new canal from the [[Erie Canal]] near Rochester, up the Genesee Valley, across to the [[Allegheny River]] at [[Olean, New York|Olean]]. Construction of new sections extended upriver (southward) until 1880. Although an important commercial route, the canal was plagued by frequent flood damage and the final leg down the Allegany River was never completed. The most difficult section to build was the bypass around the gorge and falls at present day Letchworth Park. The canal followed the old [[Native Americans of the United States|Native American]] [[portage]] route, which necessitated many locks. These old locks can still be seen near Nunda. The project was abandoned, and the right of way was sold in 1880. The property became the roadbed for the [[Genesee Valley Canal Railroad]], which eventually merged with the [[Pennsylvania Railroad]]. Much of the canal and railroad right-of-way is open to the public today as the [[Genesee Valley Greenway]], which was started in 1991.


In 1852 a wooden railroad bridge was built over the Upper Falls at [[Portageville, New York|Portageville]]. It was the largest of all wooden bridges built at the time.{{Citation needed|date=April 2009}} The wood from 300&nbsp;acres (1.2&nbsp;km²) of trees was required for its timber. In the "summer of 1943", [[Arch Merrill]] walked the length of the Genesee River.<ref name=Genesee>{{cite web
In 1852 a wooden railroad bridge was built over the Upper Falls at [[Portageville, New York|Portageville]]. It was the largest of all wooden bridges built at the time.{{Citation needed|date=April 2009}} The wood from 300&nbsp;acres (1.2&nbsp;km²) of trees was required for its timber. In the "summer of 1943", [[Arch Merrill]] walked the length of the Genesee River.<ref name=Genesee>{{cite web
|last=Merrill
|last=Merrill
|first=Arch
|first=Arch
|authorlink=Arch Merrill
|author-link=Arch Merrill
|year=1943
|year=1943
|title=A River Ramble: Saga of the Genesee Valley
|title=A River Ramble: Saga of the Genesee Valley
|url=http://mcnygenealogy.com/book/river-ramble-1.htm
|url=http://mcnygenealogy.com/book/river-ramble-1.htm
|publisher= GenWeb, Monroe County, NY
|publisher= GenWeb, Monroe County, NY
|accessdate=November 26, 2009
|access-date=November 26, 2009
}}
}}
::(see also: {{cite web
::(see also: {{cite web
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|publisher=Democrat and Chronicle
|publisher=Democrat and Chronicle
}}{{dead link|date=January 2017 |bot=InternetArchiveBot |fix-attempted=yes }})</ref>
}}{{dead link|date=January 2017 |bot=InternetArchiveBot |fix-attempted=yes }})</ref>

Serial killer [[Arthur Shawcross]] dumped most of his victims in or near the river, leading to him being nicknamed "The Genesee River Killer".<ref>{{cite web | url=https://thoughtcatalog.com/brie-calvert/2018/03/27-gruesome-facts-about-the-real-life-killer-known-as-the-monster-of-the-rivers/ | title=27 Gruesome Facts About 'The Monster of the Rivers' (AKA Arthur John Shawcross) | date=18 March 2018 }}</ref>


=== Crossings ===
=== Crossings ===
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| publisher = [[National Weather Service|NWS Eastern Region Headquarters]]
| publisher = [[National Weather Service|NWS Eastern Region Headquarters]]
| url = http://www.erh.noaa.gov/nerfc/historical/jun1972.htm
| url = http://www.erh.noaa.gov/nerfc/historical/jun1972.htm
| accessdate = December 18, 2009}}</ref><ref
| access-date = December 18, 2009}}</ref><ref
name=flood>{{Cite news | title = The great flood of 1972 |newspaper=[[Star-Gazette]] |location=[[Elmira, New York]] |publisher=Gannett | page=63 |year=1972 }}</ref> The water from Hurricane Agnes caused the only instance where the river's flow exceeded the storage capacity of the reservoir of the [[Mount Morris Dam]], the largest flood control dam east of the [[Mississippi River|Mississippi]], and water had to be released from the dam to prevent overtopping of the spillway.
name=flood>{{Cite news | title = The great flood of 1972 |newspaper=[[Star-Gazette]] |location=[[Elmira, New York]] |publisher=Gannett | page=63 |year=1972 }}</ref> The water from Hurricane Agnes caused the only instance where the river's flow exceeded the storage capacity of the reservoir of the [[Mount Morris Dam]], the largest flood control dam east of the [[Mississippi River|Mississippi]], and water had to be released from the dam to prevent overtopping of the spillway.


<gallery widths="200px" heights="145px">
<gallery class="center" widths="250px" heights="187px">
File:A View of the Casconchiagon or Great Seneca Falls - Thomas Davies.jpg|''A View of the Casconchiagon or Great Seneca Falls, Lake Ontario, taken 1766'' by [[Thomas Davies (British Army officer)|Thomas Davies]]
File:A View of the Casconchiagon or Great Seneca Falls - Thomas Davies.jpg|''A View of the Casconchiagon or Great Seneca Falls, Lake Ontario, taken 1766'' by [[Thomas Davies (British Army officer)|Thomas Davies]]
File:HighFallsGenesee.jpg|The [[High Falls, Rochester New York|High Falls]] in downtown [[Rochester, New York|Rochester]]
File:HighFallsGenesee.jpg|The [[High Falls, Rochester New York|High Falls]] in downtown [[Rochester, New York|Rochester]]
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==Literature==
==Literature==
The Genesee has been the subject of books and poetry.
The Genesee has been the subject of books and poetry:
* ''By the Genesee: Rhymes and Verses'' by [[Thomas Thackeray Swinburne]] (1900)
* ''A River Ramble: Saga of the Genesee Valley'' by [[Arch Merrill]] (1943). A walk along the Genesee from its source to its mouth
* ''Genesee Fever'' by [[Carl Carmer]]. Novel about the early settlement of the Genesee Valley (1941)
* ''The Genesee'' by [[Henry W. Clune]], part of the [[Rivers of America Series]] (1963)
* ''Valley of the Genesee: A Poem'' by Charles Edwin Furman (1879)
* ''Valley of the Genesee: A Poem'' by Charles Edwin Furman (1879)
* ''By the Genesee: Rhymes and Verses'' by [[Thomas Thackeray Swinburne]] (1900)
* ''Genesee Fever'' by [[Carl Carmer]] (1941); a novel about the early settlement of the Genesee Valley.
* ''A River Ramble: Saga of the Genesee Valley'' by [[Arch Merrill]] (1943); a walk along the Genesee from its source to its mouth.
* ''The Genesee'' by [[Henry W. Clune]] (1963); part of the [[Rivers of America Series]]

==See also==
==See also==
* [[List of rivers of New York]]
* [[List of rivers of New York]]
* [[List of rivers of Pennsylvania]]
* [[List of rivers of Pennsylvania]]
* [[Glacial geology of the Genesee River]]


==References==
==References==

Latest revision as of 22:42, 2 November 2024

Genesee River
Genesee River near Belmont
Genesee River watershed (Interactive map)
Native nameČunehstí•yu• (Tuscarora)[1]
Location
CountryUnited States
StateNew York, Pennsylvania
Counties(see Navbox, below)
CityRochester, NY
Physical characteristics
Source 
 • locationUlysses Township, Potter County, Pennsylvania
 • coordinates41°53′33″N 77°43′54″W / 41.89250°N 77.73167°W / 41.89250; -77.73167[2]
 • elevation2,275 ft (693 m)[3]
MouthLake Ontario
 • location
Charlotte, Rochester, Monroe County, New York
 • coordinates
43°15′30″N 77°36′08″W / 43.25833°N 77.60222°W / 43.25833; -77.60222[2]
 • elevation
243 ft (74 m)[2]
Length157 mi (253 km)
Basin size2,500 sq mi (6,500 km2)
Discharge 
 • locationLake Ontario
Discharge 
 • locationPortageville, NY

The Genesee River (/ˌɛnɪˈs/ JEN-iss-EE) is a tributary of Lake Ontario flowing northward through the Twin Tiers of Pennsylvania and New York in the United States. The river contains several waterfalls in New York at Letchworth State Park and Rochester.

The river was historically used as a border between the lands of the Seneca to the east and the Erie and Wenro to the west. Later, the river provided the original power for the Rochester area's 19th century mills, and still provides hydroelectric power for downtown Rochester. Flooding occurred periodically in the river valley before construction of the Mount Morris Dam in the 1950s.

Geology

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Portage Viaduct below Upper Falls in Letchworth State Park

The Genesee is the remaining western branch of a preglacial system, with rock layers tilted an average of 40 feet (12 m) per mile, so the river flows across progressively older bedrock as it flows northward. It begins in exposing the Allegheny Plateau's characteristic conglomerates: sandstones and shales in the rock columns of the Mississippian and Pennsylvanian subperiods. Thereafter, farther downstream as it traverses the area known as The Grand Canyon of the East,[4] where it falls (three times) through over 600 feet (180 m)[4]. As it passes through the gorges in New York's Letchworth State Park, the river also often exposes older rocks such as shales (some rich in hydrocarbons[5]), siltstones and some limestones of the Devonian period at Letchworth and, at other canyons with three more waterfalls[6][7][8] at Rochester cuts through the Niagara Escarpment, exposing limestones and shales of Silurian age in the rock column. With cuttings in the geologic record showing so many early ages, the river area has a great variety of fossils for paleobiological and stratigraphic analysis.

During the past million years, four glacial ages covered the Rochester area. The southern edges of the Laurentide Ice Sheet and those advances impacted the formation geology and geography of the area. The most recent glacier that left evidence here was about 10,000 years ago and it caused compression of the earth by as much as 2,500 feet (760 m).[9] About 12,000 years ago, the area underwent massive changes, which included the rerouting of the Genesee and other water bodies. The pre-ice age eastern branch of the Genesee runs south of Mount Morris and was completely diverted by extensive terminal moraines in Livingston County with a key blocking dam just south of Dansville, so most of the upper section of the ancient river was diverted instead to fall the off Appalachian Plateau toward the Susquehanna River system (to an eventual destination well to the southeast).

Only a small creek (Irondequoit Creek) flows in what is left of this large paleogeologic valley. The area of the lower river was also affected. Since the earth rebounded from the melting glaciers more rapidly in Canada than in New York, water from Lake Ontario was spilled over New York due to its lower elevation. During this time, the original outlet of the Genesee River, Irondequoit Bay, was flooded out, creating the current bay. As these waters later retreated, glacial debris caused the river to be rerouted to the west along its current path.[10][11]

History

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The Seneca nation traditionally lived between the Genesee River and Canandaigua Lake. The region was surveyed by Thomas Davies in 1766. The High Falls was then also known as the Great Seneca Falls, and the Genesee River was also spelled Zinochsaa by early writers.[12]

Historically, the river's gorge formed a clearly demarcated border between the lands of the Five Nations of the Iroquois, whose range extended east and the related tribes of the Erie people and Wenro along the west side of the gorge. By the end of the Beaver Wars and the American Revolution, the lands in all of upstate New York into the Ohio Country were controlled by the Iroquois Confederation, but were also effectively depopulated, the tribes weakened in the Revolution. In 1779, on the orders of George Washington, the Sullivan Expedition destroyed over 40 Haudenosaunee villages in and around the watershed to force the Seneca and allied nations out of the newly formed United States. Subsequently, with most Iroquois having fled to Canada, the remnant tribal groups were in no position to further impede white settlers, so most of New York state west of the Genesee River became part of the Holland Purchase after the American Revolution. From 1801 to 1846 the entire region was sold to individual owners from the Holland Land office in Batavia, New York. In the 1797 Treaty of Big Tree, the Seneca tribes were granted six reservations along the river, among them Canawaugus, Little Beard's Town, Geneseo, Caneadea, Deyuitgau and Gardeau. In August 1826, the Ogden Land Company purchased the six Genesee River reservations from the Seneca, allegedly under duress;[13] the modern Seneca Nation of Indians does not recognize the 1826 sale as valid and moved to reclaim Canawaugus in December 2022.[14]

On Friday, November 13, 1829 (Friday the 13th), the daredevil Sam Patch jumped to his death before 8,000 spectators at the Upper Falls in Rochester.

If "not for hydropower, the flour mills, clothing mills, and tool fabricators would not have located in Rochester",[15] and the 1825 Erie Canal allowed the mills to ship products to New York City. A few hundred feet north of the center of the village of Rochester, the Erie Canal crossed the Genesee River via an 1823 stone aqueduct (802 feet (244 m) long, 17 feet (5.2 m) wide), which was replaced by the Second Genesee Aqueduct in 1842.

In 1836 the Genesee Valley Canal was begun to build a new canal from the Erie Canal near Rochester, up the Genesee Valley, across to the Allegheny River at Olean. Construction of new sections extended upriver (southward) until 1880. Although an important commercial route, the canal was plagued by frequent flood damage and the final leg down the Allegany River was never completed. The most difficult section to build was the bypass around the gorge and falls at present day Letchworth Park. The canal followed the old Native American portage route, which necessitated many locks. These old locks can still be seen near Nunda. The project was abandoned, and the right of way was sold in 1880. The property became the roadbed for the Genesee Valley Canal Railroad, which eventually merged with the Pennsylvania Railroad. Much of the canal and railroad right-of-way is open to the public today as the Genesee Valley Greenway, which was started in 1991.

In 1852 a wooden railroad bridge was built over the Upper Falls at Portageville. It was the largest of all wooden bridges built at the time.[citation needed] The wood from 300 acres (1.2 km²) of trees was required for its timber. In the "summer of 1943", Arch Merrill walked the length of the Genesee River.[16]

Serial killer Arthur Shawcross dumped most of his victims in or near the river, leading to him being nicknamed "The Genesee River Killer".[17]

Crossings

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Floods

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A March 1865 thaw was the worst Genesee flood in Rochester history, and a similar 1913 flood motivated the excavation of the Genesee's rock bed in Downtown Rochester. The 1972 Hurricane Agnes flood broke all county historical records, with the most concentrated damage in the Wellsville area.[18][19] The water from Hurricane Agnes caused the only instance where the river's flow exceeded the storage capacity of the reservoir of the Mount Morris Dam, the largest flood control dam east of the Mississippi, and water had to be released from the dam to prevent overtopping of the spillway.

Literature

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The Genesee has been the subject of books and poetry:

See also

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References

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  1. ^ Peck, William (1908). History of Rochester and Monroe county, New York. The Pioneer publishing company. p. 15. Retrieved April 4, 2009.
    NOTE: Čunehstí•yu• is from the Seneca tribe name Chin-u-shio (Tuscarora language) meaning a beautiful open valley.
  2. ^ a b c U.S. Geological Survey Geographic Names Information System: Genesee River
  3. ^ Harrison Valley, PA, 7.5 Minute Topographic Quadrangle, USGS, 1957 (1971 rev)
  4. ^ a b Letchworth State Park, accessdate=2016-06-05
  5. ^ Such layers often allow carbon-14 dating to synchronize subdisciplines of stratigraphy
  6. ^ High falls & Browns race area, City of Rochester, accessdate=2016-06-05
  7. ^ downtown falls area, City of Rochester, accessdate=2016-06-05
  8. ^ MAPLEWOOD/LOWER FALLS - Rochester, NY, accessdate=2016-06-05
  9. ^ "Geology: 100,000 years ago". Rochester's History: An Illustrated Timeline. Archived from the original on 2008-06-03. Retrieved July 11, 2008.
  10. ^ "Geology: 12,000 years ago". Rochester's History: An Illustrated Timeline. Archived from the original on 2008-06-03. Retrieved July 11, 2008.
  11. ^ Rogers, Brownell (1893). "The Genesee River". Science. 21 (526): 121. doi:10.1126/science.ns-21.526.121. PMID 17814804.
  12. ^ Supplement to Dobson's Encyclopedia volume 3, which cites Jedidiah Morse as its source, probably the American Gazetteer, 1795
  13. ^ Red Jacket (Seneca chief) (2006). The Collected Speeches of Sagoyewatha, Or Red Jacket. Syracuse University Press. ISBN 9780815630968. Retrieved May 8, 2017.
  14. ^ Quigley, Kellen (December 31, 2022). "Seneca Nation purchases ancestral Genesee Valley land". The Salamanca Press. Retrieved 2022-12-31.
  15. ^ Baily, Rod (October 1984). "Sources of Energy in Rochester's History" (PDF). Rochester History. XLVI (3–4). Rochester Public Library. ISSN 0035-7413. Archived from the original (PDF) on March 27, 2009. Retrieved December 29, 2009. Hydropower has never contributed more than two and a half percent of the total energy supply of Rochester
  16. ^ Merrill, Arch (1943). "A River Ramble: Saga of the Genesee Valley". GenWeb, Monroe County, NY. Retrieved November 26, 2009.
    (see also: "Rediscovering the Rambling River". Democrat and Chronicle.[permanent dead link])
  17. ^ "27 Gruesome Facts About 'The Monster of the Rivers' (AKA Arthur John Shawcross)". 18 March 2018.
  18. ^ "HURRICANE AGNES and the GENESEE RIVER FLOODING". NWS Eastern Region Headquarters. Retrieved December 18, 2009.
  19. ^ "The great flood of 1972". Star-Gazette. Elmira, New York: Gannett. 1972. p. 63.
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