478:. Before the deposition of the Valley Heads Moraine, glaciers had deepened the many north-south oriented valleys that characterize the region. These valleys originally were streams that flowed to the south. The moraine formed a series of lakes in the valleys. Drainage was still to the south over the moraine until the glacier retreated far enough to the north to allow escape of the waters along the southern edge of the glacier. At an elevation of about 900 feet, the glacial lakes filling the finger lakes valleys joined to form an interlocking system of lakes to the west (glacial Lake Warren ). At first Lake Warren continued to drain to the west, but as the ice retreated west of Rome, New York, flow shifted to the east into the Mohawk-Hudson River system. As the ice continued to retreat, a series of east-west channels were cut by the easterly flowing glacial meltwater. According to Fairchild, the westernmost of these was the gully that runs from near Mud Pond about 4 miles north-northeast of Skaneateles and 4 miles north-northwest of Marcellus and empties into Nine Mile Creek 2 miles south of the Village of Marcellus. The water was impounded in the Otisco Valley (glacial Lake Marcellus), and the delta formed where debris carried by this meltwater stream was deposited as it entered the lake can be easily seen on topographic maps. The meltwater soon continued draining to the east, carving the channel now known as Pumpkin Hollow that leads east from the Village of Marcellus. With the continuing northward retreat of the glacier, meltwater deepened the Nine Mile Creek Valley and cut the Camillus Valley that runs east from Martisco to the Village of Camillus. For a time this channel discharged to the east towards Syracuse at an elevation of about 500 feet. Eventually the glacier receded far enough north to open the channel near Rome New York that resulted in the formation of
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comparison, most free flowing drainages in the northeast only support from 6 to 20 species. In the town of
Marcellus, Nine Mile Creek comprises two distinct fisheries. Otisco Lake outlet to the old Crown Mill (adjacent to Marcellus Falls) contains species more tolerant of warm water and low dissolved oxygen levels. This section of creek averages thirteen species, with more species found closer to the Otisco Lake outlet. While trout numbers are low in this upper section, other stream fishes are very abundant, including an estimated 6000+ fish per acre near the Lawrence Rd. Crossing (DEC 1996). Fish diversity is much lower in this section with only an average of 7 fish species. Trout presence is quite impressive with typically more than 500 trout per acre (DEC 1996). Most of the trout captured by NYSDEC biologists in August 1996 were of wild strain indicating successful reproduction and growth in the stream.
775:, which use the creek for various class outings and field laboratories. Students involved in the educational opportunities facilitated by these institutions see many plants, birds and other organisms that they do not see elsewhere. In the article "ESF Puts Environment in High School", cooperation between the SUNY College of Environmental Science and Forestry and Marcellus High School in performing studies at Nine Mile Creek was headlined in the November 13, 2001, issue of the Post Standard. It is notable that much of the biological, hydrological and geological information gathered for this article was found in graduate theses that were written by students at Syracuse University and SUNY ESF.
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368:, Otisco Lake's ferryboat, made transportation of people and goods relatively easier. The M&OL Railway was abandoned on July 15, 1937, after roads for motorcars were constructed in the region. The short-line railroad was a unique chapter in the town's history with only an empty railroad grade and an old station building remaining. The grade and arches nevertheless are still a prominent feature of the lower reaches of the creek within Marcellus.
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established along Nine Mile Creek. Deacon Samuel Rice and Judge Dan
Bradley built the first mill on the creek between 1795 and 1796. While the mill is no longer standing it was reportedly built south of the village. The Crown Mill, which is located in the village on State Route 174, is one of the few old mills still standing. The mill was demolished in 2016. Robert and Thomas Dyer built it in 1812. The mill has since changed hands many times.
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through such cavernous networks to allow pollutants to be removed from the system. In particular, White noted that nitrates are not broken down as they flow through karst drainages. Thus nitrate inputs into the groundwater system at
Pleasant Valley may be expected to be similar to the outputs into Nine Mile Creek at Marcellus Falls. From this perspective, sources of
547:, which by nature are easily eroded and deemed unsuitable for development. From just north of Sevier Road to just south of the village line, the creek takes on a stained color due to natural siltation from the silt loam soils that comprise its bank. Obviously, extensive and chronic sources of siltation in the area could cause sediment overload that would smother
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Public access and some docks exist along Nine Mile Creek, but the Creek is generally only deep enough to boat in from Munro Park in the
Village of Camillus downstream to the mouth at Onondaga Lake. While some sections of fast moving water exist, as well as hazards such as low dams (at Warners Rd) and
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Fishing is the main form of recreation along Nine Mile Creek. The Creek is notable as an outdoor classroom for the seasoned angler as well as for the parent and child. From Crown Mill downstream to the
Marcellus town boundary, cooler and highly oxygenated water supports a healthy trout fishery, which
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A distinct difference in the creeks character occurs north versus south of the
Village of Marcellus. South of the Village, one finds a meandering shallow stream with dense bank vegetation and the occasional beaver impoundment. The dam at the north end of Otisco Lake controls the flow of the creek and
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Interest in rail transportation peaked in the late 19th century. After railroad fever took hold in the 1870s, a short-line railroad was constructed that connected Otisco Lake to
Marcellus. Through incorporation of the Marcellus & Otisco Lake Railway Company, the rail line was eventually completed
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The Nine Mile Creek corridor supports a high diversity of plants due to a temperate climate, wide range of wetland and terrestrial habitats, nutritious limestone bedrock, and floodplain soils. In total, some 142 different species of plants have been documented in the Nine Mile Creek corridor and its
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A clean-up program is currently being conducted by
Honeywell (the successor to Allied Signal) along the lower part of Nine Mile Creek and for Onondaga Lake under terms of a consent order with the New York State Department of Environmental Conservation. Documents concerning the clean-up can be found
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The beds along Nine Mile Creek near the lakeshore were abandoned after 1944 when a waste bed dike failed, causing flooding of portions of the
Village of Solvay by the waste. A series of additional waste beds (beds 9–15) were then constructed along Nine Mile Creek upstream of the lake. A portion of
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exist, thousands of 1-year and 2-year browns and 1-year brookies are stocked from
Onondaga County's Carpenters Brook Fish Hatchery every year. However, NYSDEC electrofishers have found that wild brown trout are predominant after the heavy spring fishing pressure, from Marcellus Falls downstream.
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In terms of variation in plant communities along the creek, there is a rather uniform floral composition from the outlet of Otisco Lake to Masters Road. Dense herbivorous vegetation and numerous layers of forest canopy typify it. A mix of herbaceous and woody vegetation provides robust riparian
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creates a diverse fishery, thereby making it the most popular trout stream in Onondaga County. State and private stocking projects along with migration from Otisco and Onondaga Lakes have contributed to the creek’s impressive diversity of fishes, which totals some thirty species (DEC 1996). By
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at Marcellus Falls have been observed to be active as late as October. These groundwater flows serve as a significant input of cold, nutrient-rich waters during summer months. It is notable that water flowing through karst systems is sensitive to change. This is because water flows too quickly
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geology, which is typified by a cavernous underground landscape. Through the use of water tracer dyes, Proett (1978) identified a distinct hydrologic connection between Disappearing Lake and its eventual outlet into Nine Mile Creek at Marcellus Falls. Although Disappearing Lake is a springtime
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Nine Mile Creek transforms itself several times throughout its approximately 10-mile (16 km)-long course through the Town of Marcellus. Nine Mile Creek drops in elevation between the Otisco Lake outlet and the Camillus-Marcellus town line by 360 feet (110 m) making the average stream
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was built around Nine Mile Creek and an appreciation of the Creek is necessary for understanding the Town's history. The Nine Mile Creek valley was known for its very productive agricultural soils and its "deep picturesque valley" of eastern hemlocks. Since the late 1700s some 25 mills were
390:) began production in 1886. Initially wastes from the process were deposited along the shore of Onondaga Lake. Starting in 1916, waste beds 1–6 were constructed on the shore of the lake in the vicinity of Nine Mile Creek, and the creek was diverted to the north around beds 5 and 6.
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near the creek and Onondaga Lake from the late 19th century to the late 20th century. Recent reclamation has significantly restored quality in the final stretch of the creek. Farther to the south and upstream, the state of New York maintains fishing access sites.
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fish such as trout. In this reach, however, a diverse fishery is maintained, with a wide variety of fish more closely associated with warm waters. North of the Village the stream cuts through the Alps region (a steep sided valley cut through the
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documented the flora north of the town center by walking down the old Martisco Railroad bed. Aside from documenting all of the 92 commonly seen species in the creek corridor, the club noted the presence of the following state protected plants:
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Due east of the DEC parking area at Marcellus Falls and along the Nine Mile Creek corridor are steep slopes and a group of important springs which drain into the creek. The area is of considerable botanical interest. In 1983, the
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at an elevation of about 440 feet. Lake Iroquois had a relatively long existence, but 13,400 years ago the collapse of an ice dam led to the rapid draining of Lake Iroquois, and Nine Mile Creek started to assume its present form.
609:, both of which are occasionally seen in the area. This section includes the only regulated wetland in the town of Marcellus, MAR-11, that is located within the flood plain of Nine Mile Creek. The flora of this wetland includes
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Nine Mile Creek receives a variety of recreational usage, both on the water and off. In addition to fishing and boating, there are many publicly and privately held green spaces such as at Marcellus Falls and Baltimore Woods.
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The lower part of Nine Mile Creek (from Route 173 to Onondaga Lake) has been significantly affected by the construction and operation of waste beds containing byproducts from the production of sodium carbonate by the
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A similar phenomenon occurs in the watershed of Geddes Brook, the largest tributary of Ninemile Creek. The headwaters of Geddes Brook disappear into channels in the limestone at Lost Lake, at the top of the Onondaga
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requiring clear water. Although showing a much different character, the soils bordering the creek north of the Village of Marcellus are not free from erosion hazards. The steep valley walls in this section create
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Blasland & Bouck. 1989. Hydrogeologic Assessment of the Allied Waste Beds in the Syracuse area. Volume 1 of 2. Prepared for AlliedSignal, Syracuse, NY. Blasland & Bouck Engineers, P.C., Syracuse,
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Nine Mile Creek is subject to Onondaga County's special fishing regulation for trout of a daily limit of 5, with no more than 2 larger than 12" (the 5/2 rule). The trout season is open from 4/1 to 10/15.
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between one million and ten thousand years ago. The last glacier to recede (starting about 19,000 years ago and leaving New York entirely approximately 11,000 years ago) deposited the Valley Heads
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students, they estimate that Nine Mile Creek supports 90 species of breeding birds and many more during migration periods. During field visits to the Creek in the fall of 2002, large flocks of
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buffers. This area is home to many of the 92 commonly seen plant species observed in the Nine Mile Creek area, and is also home to protected ferns and such protected or rarely seen plants as
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Sources and Sinks of Phosphorus in Ninemile Creek and the Effects of Mineral Deposits"Anthony Prestigiacomo, Steven Effler, David Matthews, and Feng Peng. Upstate Freshwater Institute, 2010.
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695:(scuds) are extremely abundant in this area indicating both favored water quality and a quality food base for trout growth. Recent (2004–2005) Trout habitat has improved trout density.
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Hewlett, John, D., 1956. The Development of Vegetation on the Solvay Waste Beds. State University of New York College of Environmental Science and Forestry, Syracuse, New York., Thesis
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associated wetlands. Ninety-two of these species are commonly occurring throughout the Nine Mile Creek corridor, whereas the other 49 occur in specific locations along the creek.
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strongly influences the first several kilometers of the stream. Warm surface water from the lake feeds Nine Mile Creek in summer months making it intolerable for
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on May 25, 1905. The project was more difficult than anticipated, with 46 curves constructed in just 9.05 miles (14.56 km) of track. Connection with the
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of the Nine Mile Creek corridor provides a relatively narrow belt of habitat suitable for many forms of wildlife. Based on data being collected under the
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low overhangs (at Route 5 Culvert and Erie Canal Aqueduct), paddling in Nine Mile Creek is accessible to both experienced and inexperienced paddlers.
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The Disappearing Lake area in Pleasant valley area is a geologically significant feature of the area. This lake is located on an area of
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From Masters Road to the Village center, there is vegetation similar to that in the upper sections. However, additional species include
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Allenson, Sherman (1952). "Stratigraphy and Structure of the Southern Part of the Camillus Quadrangle, Onondaga County, New York".
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velocity about 0.8 ft/s. The maximum depth is 5.5 feet (1.7 m) and average depth is 1.0 feet. (Update for entire creek )
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Storey, Mike (1977), "Heartland: A natural history of Onondaga County, N. Y.", Syracuse, New York: Onondaga Audubon Society, Inc.
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The creek in this section shows an increase in pH and a decrease in phosphate concentration, due to the high alkalinity of
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Overall, the Nine Mile Creek watershed covers 115 square miles (300 km) and includes portions of ten towns within
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are all concerns for upland areas associated with Disappearing Lake area. This is because they may eventually alter
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has worked to create an officially designated water trail, and conducts an annual fish-stocking event by canoe.
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owns a large parcel along Nine Mile Creek south of the Village of Camillus and allows public fishing access
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monitors the water quality of Nine Mile Creek through their volunteer-led Red Flag Monitoring Program.
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A number of educational institutions directly benefit from Nine Mile Creek. These include SUNY ESF,
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utilizes two locations on Nine Mile Creek in the Town of Marcellus to collect water quality data.
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The predominant soil types associated with the Nine Mile Creek corridor are Teel and Wayland
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Many grassroot and national groups do work on behalf of Nine Mile Creek. A partial list:
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migrants were observed, which suggests that the corridor serves as a migration pathway.
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has done stream stabilization and riparian ecosystem improvement projects.
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Proett, Brian, ed. (1978), "Hydrology of Marcellus Disappearing Lake",
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receives the most fishing hours. While a self-sustaining population of
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the creek was rerouted to allow construction of beds 9, 10, and 11.
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Fairchild, H. L. "Pleistocene Features in the Syracuse Region",
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386:. The Solvay Process Company (later acquired by
975:Unpublished Masters Thesis, Syracuse University
328:. Nine Mile Creek is a scenic stream noted for
1046:"Onondaga County Special Fishing Regulations"
1008:"Ninemile Creek Electrofishing Survey (2007)"
993:Geomorphology and Hydrology of Karst Terrains
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446:. Nine Mile Creek is the major tributary of
1119:NYSDEC Nine Mile Creek Fishing Access Sites
1093:: CS1 maint: numeric names: authors list (
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519:in Nine Mile Creek below Marcellus Falls.
995:. New York City: Oxford University Press.
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962:, Syracuse, New York: Syracuse University
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933:The Geological History of New York State
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304:in the United States. Its source is at
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788:Nine Mile Creek Conservation Council
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1069:DEC Region 7 Bureau of Fisheries.
1006:DEC Region 7 Bureau of Fisheries.
713:New York State Breeding Bird Atlas
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715:as well as field observations by
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16:River in New York, United States
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808:conducts stream cleanup events.
644:stinking Benjamin or wake-robin
458:The contemporary landscape of
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824:Community Science Institute
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1134:Rivers of New York (state)
960:Unpublished Masters Thesis
837:List of rivers in New York
635:Adirondack Wildflower Club
652:fancy (toothed) wood fern
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779:NGO / nonprofit activity
543:environments. These are
412:Physical Characteristics
268:375 ft (114 m)
191:785 ft (239 m)
991:White, William (1988).
812:Onondaga Soil and Water
640:large-flowered trillium
556:potential due to rapid
946:The American Geologist
935:, Kennikat Press, 1914
472:St. Lawrence watershed
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773:Marcellus High School
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476:Susquehanna watershed
407:Onondaga Lake Cleanup
247:43.08911°N 76.22952°W
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562:stormwater retention
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170:42.90442°N 76.3131°W
931:Miller, William J,
800:Izaak Walton League
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913:Missing or empty
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842:Otisco Lake
747:brook trout
743:brown trout
721:Neotropical
603:Scotch pine
588:button bush
554:flash flood
541:flood plain
306:Otisco Lake
250: /
173: /
128:Otisco Lake
1128:Categories
1080:2011-01-15
1055:2011-01-15
1017:2011-01-15
853:References
727:Recreation
525:escarpment
377:Waste Beds
342:deposited
278:Waterfalls
238:76°13′46″W
235:43°05′21″N
161:76°18′47″W
158:42°54′16″N
763:Education
693:Amphipods
648:bloodroot
611:blue flag
607:butternut
537:silt loam
503:road salt
474:from the
434:Watershed
357:Marcellus
314:Marcellus
97:Marcellus
1089:cite web
1026:cite web
906:citation
831:See also
754:Paddling
717:SUNY ESF
703:Wildlife
399:leachate
318:Camillus
218:Lakeland
141:Marietta
109:Syracuse
101:Camillus
93:Marietta
61:New York
42:Location
35:Camillus
736:Fishing
682:Fishery
568:Ecology
512:E. Coli
468:Moraine
454:Geology
366:Fontney
351:History
333:fishing
308:in the
296:, is a
47:Country
1075:NYSDEC
1050:NYSDEC
1012:NYSDEC
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771:, and
629:sp.).
627:Cornus
594:, and
558:runoff
509:, and
405:here:
326:Geddes
298:stream
124:Source
105:Solvay
89:Cities
78:County
67:Region
623:Carex
573:Flora
531:Soils
493:karst
330:trout
201:Mouth
57:State
1095:link
1032:link
919:help
745:and
707:The
674:and
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