Chagrin River | |
---|---|
Location | |
Country | United States |
State | Ohio |
Physical characteristics | |
Source | Bass Lake, Ohio |
• location | Munson Township, Northeast Ohio |
Mouth | Chagrin Harbor |
• location | Eastlake, Lake County, OH |
• coordinates | 41°40′36″N81°26′13″W / 41.67667°N 81.43694°W |
Discharge | |
• location | Eastlake, OH |
The Chagrin River is located in Northeast Ohio. [1] The river has two branches, the Aurora Branch and East Branch. Of three hypotheses as to the origin of the name, the most probable is that it is a corruption of the name of a Frenchman, Sieur de Seguin, who established a trading post on the river ca. 1742. [2] [3] [4] The Chagrin River runs through suburban areas of Greater Cleveland in Cuyahoga, Geauga, and Portage counties, transects two Cleveland Metroparks reservations, and then meanders into nearby Lake County before emptying into Lake Erie.
The East Branch begins in Geauga County, flows north then west through Lake County, largely in Kirtland, and Kirtland Hills. In these communities the East Branch transects the Holden Arboretum, before intersecting the main in Willoughby. [5]
The Aurora Branch begins in northwest Portage County, flowing northwest through Aurora and portions of Geauga and Cuyahoga Counties, intersecting the main branch west of Chagrin Falls. [6]
The Chagrin River was designated as a state scenic river in 1979.
Along its banks and tributaries, Berea sandstone, Bedford shale, Cleveland Shale, and Chagrin Shale bedrock are exposed in layers. The river itself was cut through the Allegheny Plateau as glaciers receded in the area at the end of the Wisconsin glaciation.
The lowest visible bedrock is Chagrin shale. Named for the river and easily found in the river valley. Chagrin shale is blue gray in color, an offshore alluvial, silt shale of the Devonian period. This layer is found below about 800 feet (240 m) msl.
The next layer is Cleveland shale. This is a black shale that is an important source of local fossils. Cleveland Shale is found in the Chagrin River valley between 800 and 900 feet (270 m) msl.
Bedford Shale is found above the Cleveland Shale layer. This material marks the uncertain transition between the Devonian and Pennsylvanian periods in the region and is also an important source of local fossils. This layer is found in the ravines that carry tributaries of the Chagrin River. Bedford shale is a sand shale and is characterized by its roughly 90° cleavage pattern. Pieces of Bedford shale can look as if they were cut by human hands and are found up to about 950 feet (290 m) msl.
Berea sandstone is found from around 950 feet (290 m) msl to roughly 1,070 feet (330 m) msl. Berea sandstone is an important local building material. In the nineteenth century it was quarried from the base of Gildersleeve Mountain (in the East Branch watershed). This material was used to build Kirtland Temple and other local structures. Berea sandstone is still used as a local building material
According to the Ohio Department of Natural Resources, more than 49 species of fish and 90 bird species live in the Chagrin River watershed, including the American brook lamprey, which is relatively rare in Ohio.
Hiking is popular in many areas along the Chagrin River. [7] Some areas are also popular for fishing: ESPN Outdoors recommends the Chagrin River for fishing, [8] especially for finding steelhead. The Daniels Park Dam, a small lowhead dam, was their favorite spot. On December 31, 2004, the Daniels Park Dam failed due to excess pressure from ice and water. [9]
The Aurora branch of the Chagrin River is a class III-IV of whitewater, according to the American Whitewater Association. [10] On the other hand, the Daniels Park section is rated a class I.
In 2007, the Ohio Environmental Protection Agency were notified that, in violation of both state law and Federal Regulations, 8,700 feet (2,700 m) of the East Branch of the river was channelized and diked to prevent flooding on agricultural land owned by the Village of Kirtland Hills. [11] This activity was conducted by local developer Jerome T. Osborne Sr., who leased the land from the village. Both the village and Osborne were cited for the activity, which threatened the riparian floodplains and increased the likelihood and severity of downstream flooding in the communities of Willoughby and Eastlake. In 2012, the Ohio Attorney General's Office under Mike DeWine sued Osborne's company for failing to obtain the proper permits. [12] In 2016, Lake County Commons Pleas Judge Richard L. Collins Jr. ordered the now-late Osborne estate to pay a civil penalty of $404,240 plus interest to the Ohio State treasury. [13] The Ohio Department of Natural Resources later dedicated $2.2 million to the restoration of the East Branch, which is ongoing as of 2024. [14]
Lake County is a county in the U.S. state of Ohio. As of the 2020 census, the population was 232,603. Its county seat is Painesville, and its largest city is Mentor.
Geauga County is a county in the U.S. state of Ohio. As of the 2020 census, the population was 95,397. The county seat and largest city is Chardon.
Berea is a city in Cuyahoga County, Ohio, United States. The population was 18,545 at the 2020 census. A western suburb of Cleveland, it is a part of the Cleveland metropolitan area. Berea is home to Baldwin Wallace University, as well as the training facility for the Cleveland Browns and the Cuyahoga County Fairgrounds.
Willoughby is a city in Lake County, Ohio, United States, along the Chagrin River. The population was 23,959 at the time of the 2020 census. A suburb of Cleveland, it is part of the Cleveland metropolitan area.
Aurora is a city in northwestern Portage County, Ohio, United States. A suburb in between Akron and Cleveland, the population was 17,239 at the 2020 census. It is part of the Akron metropolitan area.
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Cleveland Metroparks is an extensive system of nature preserves in Greater Cleveland, Ohio. Eighteen reservations, which largely encircle the city of Cleveland, follow along the shore of Lake Erie and the rivers and creeks that flow through the region. Referred to unofficially as the 'Emerald Necklace', the network of parks spans over 25,000 acres (10,000 ha) and includes over 300 miles (480 km) of walking, bicycle, and horse trails as well as numerous picnic areas, nature education centers, golf courses, and countless fishing spots. In addition, the district includes the zoo in Cleveland. Four of the reservations are adjacent to Cuyahoga Valley National Park.
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Brandywine Creek is a tributary of the Cuyahoga River that is partly contained in Cuyahoga Valley National Park in Ohio.
Gildersleeve Mountain is a summit located in Kirtland, Ohio, United States.
The Bedford Shale is a shale geologic formation in the states of Ohio, Michigan, Pennsylvania, Kentucky, West Virginia, and Virginia in the United States.
Berea Sandstone, also known as Berea Grit, is a sandstone formation in the U.S. states of Michigan, Ohio, Pennsylvania, West Virginia, and Kentucky. It is named after Berea, Ohio. The sandstone has been used as a building stone and is a source of oil and gas.
Abram Creek, in Cuyahoga County, Ohio, is a tributary of the Rocky River, draining 10.6 square miles in parts of Berea, Brook Park (31.3%), Cleveland (13.1%), Middleburg Heights (48.8%), and a very small portion of Parma Heights(0.2%).
The Cleveland Shale, also referred to as the Cleveland Member, is a shale geologic formation in the eastern United States.
The Chagrin Shale is a shale geologic formation in the eastern United States that is approximately 365 million years old. The Chagrin Shale is a gray shale that begins thin and deep underground in north-central Ohio. As it proceeds east, the formation thickens, rises to the surface, and contains greater amounts of siltstone.
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Big Creek is a 15.6-mile-long (25.1 km) tributary of the Grand River and flows through Lake and Geauga counties in Ohio. It rises in glacial till near Chardon, Ohio, and cuts through the Defiance Moraine on its way north and exposes rock formations from the Paleozoic Era, including the fossiliferous Chagrin Shale. It joins the Grand River in Painesville Township in Helen Hazen Wyman Park.
Euclid Creek is a 43-mile (69 km) long stream located in Cuyahoga and Lake counties in the state of Ohio in the United States. The 11.5-mile (18.5 km) long main branch runs from the Euclid Creek Reservation of the Cleveland Metroparks to Lake Erie. The west branch is usually considered part of the main branch, and extends another 16 miles (26 km) to the creek's headwaters in Beachwood, Ohio. The east branch runs for 19 miles (31 km) and has headwaters in Willoughby Hills, Ohio.