The Great Black Swamp (also known simply as the Black Swamp) was a glacially fed wetland in northwest Ohio and northeast Indiana, United States, that existed from the end of the Wisconsin glaciation until the late 19th century. Comprising extensive swamps and marshes, with some higher, drier ground interspersed, it occupied what was formerly the southwestern part of proglacial Lake Maumee, a Holocene precursor to Lake Erie. The area was about 25 miles (40 km) wide (north to south) and 100 miles (160 km) long, covering an estimated 1,500 square miles (4,000 km2). [3] Gradually drained and settled in the second half of the 19th century, it is now highly productive farmland. However, this development has been detrimental to the ecosystem as a result of agricultural runoff. [4] This runoff, in turn, has contributed to frequent toxic algal blooms in Lake Erie. [5]
The land once covered by the swamp lies primarily within the Maumee River and Portage River watersheds in northwest Ohio and northeast Indiana. The boundary was determined primarily by ancient sandy beach ridges formed on the shores of Lakes Maumee and Whittlesey, after glacial retreat several thousand years ago. It stretched roughly from Fort Wayne, Indiana, eastward to the Ottawa National Wildlife Refuge near Port Clinton along the Lake Erie shore, and from (roughly) US 6 south to Findlay [6] and North Star, Ohio in Darke County. [7] Near its southern edge at the southwestern corner of present-day Auglaize County, wheeled transportation was impossible during most of the year, and local residents thought the rigors of travel to be unsuitable for anyone except adult men. [8]
The vast swamp was a network of forests, wetlands, and grasslands. In the lowest, flattest areas, prone to permanent inundation, deciduous swamp forests predominated, characterized especially by species of ash, elm, cottonwood and sycamore. In slightly higher areas with some topographic relief and better drainage, beech, maples, basswood, tuliptree and other more mesic species were dominant. On elevated beach ridges and moraines with good to excessive drainage, more xeric species, especially oak and hickory, were dominant. The area contained non-forested wetlands, particularly marsh and wet prairies, with marshes being particularly extensive along the Lake Erie shoreline east of Toledo.
Although much of the area to the east, south, and north was settled in the early 19th century, the dense habitat and difficulty of travel through the swamp delayed its development by several decades. A corduroy road (from modern-day Fremont, Ohio, to Perrysburg, Ohio) was constructed through the Maumee Road Lands in 1825, and was overlaid with gravel in 1838. Travel in the wet season could still take days or even weeks. The impassibility of the swamp was an obstacle during the so-called Toledo War (1835–36); unable to traverse the swamp, the Michigan and Ohio militias never came to battle. Settlement of the region was also inhibited by endemic malaria. The disease was a chronic problem for residents of the region until the area was drained and former mosquito-breeding grounds were dried up.
In the 1850s, the states began an organized attempt to drain the swamp for agricultural use and ease of travel. Various projects were undertaken over a 40-year period. Bowling Green, Ohio resident James B. Hill expedited the draining of swampy areas with his Buckeye Traction Ditcher. [9] Hill's ditching machine laid drainage tiles at a record pace. The area was largely drained and settled over the next three decades. The development of railroads and a local drainage tile industry are thought to have contributed greatly to drainage and settlement. [10]
During the second half of the 20th century, efforts were undertaken to preserve and restore portions of the swamp to its pre-settlement state (e.g. Limberlost Swamp) [11] After the excessive spread of harmful algal blooms in nearby western Lake Erie returned in 2011 and every year since then, there has been renewed interest in restoring wetlands in the drained Black Swamp area. [12] William J. Mitsch (2017) [13] called for the restoration and creation of 150 sq mi (400 km2) of treatment wetlands in the former Black Swamp or 10% of the former wetland, as needed to significantly reduce phosphorus inflow by 40% from the polluted Maumee River to Lake Erie.
The Black Swamp Conservancy, founded in 1993, has also been involved in preserving former swamplands. They currently protect 17,600 acres (7,100 ha) spread throughout the Northwest Ohio region. [14]
Metroparks Toledo is another regional leader in wetland restoration, most notably through the creation of Howard Marsh Metropark. This restored wetland converted nearly 1,000 acres (400 ha) of historical agricultural land into a prosperous wetland that now boasts over half of the bird species found throughout Ohio. Pearson Metropark is another example of both a historic, old growth wet forest, paired with sections of restored wetlands.[ citation needed ]
Toledo is a city in and the county seat of Lucas County, Ohio, United States. At the 2020 census, it had a population of 270,871, making Toledo the fourth-most populous city in Ohio, after Columbus, Cleveland, and Cincinnati. Toledo is the 85th-most populous city in the United States. It is the principal city of the Toledo metropolitan area, which had 606,240 residents in 2020. Toledo also serves as a major trade center for the Midwest; its port is the fifth-busiest on the Great Lakes.
The Toledo War (1835–1836), also known as the Michigan–Ohio War or Ohio–Michigan War, was a boundary dispute between the U.S. state of Ohio and the adjoining territory of Michigan over what is now known as the Toledo Strip. Control of the mouth of the Maumee River and the inland shipping opportunities it represented, and the good farmland to the west were seen by both parties as valuable economic assets.
A swamp is a forested wetland. Swamps are considered to be transition zones because both land and water play a role in creating this environment. Swamps vary in size and are located all around the world. The water of a swamp may be fresh water, brackish water, or seawater. Freshwater swamps form along large rivers or lakes where they are critically dependent upon rainwater and seasonal flooding to maintain natural water level fluctuations. Saltwater swamps are found along tropical and subtropical coastlines. Some swamps have hammocks, or dry-land protrusions, covered by aquatic vegetation, or vegetation that tolerates periodic inundation or soil saturation. The two main types of swamp are "true" or swamp forests and "transitional" or shrub swamps. In the boreal regions of Canada, the word swamp is colloquially used for what is more formally termed a bog, fen, or muskeg. Some of the world's largest swamps are found along major rivers such as the Amazon, the Mississippi, and the Congo.
Oregon is a city in Lucas County, Ohio, United States. Located on Lake Erie, it is a suburb of Toledo lying east of the city and is home to Maumee Bay State Park. The population was 19,950 at the 2020 census.
The Maumee River is a river running in the United States Midwest from northeastern Indiana into northwestern Ohio and Lake Erie. It is formed at the confluence of the St. Joseph and St. Marys rivers, where Fort Wayne, Indiana has developed, and meanders northeastwardly for 137 miles (220 km) through an agricultural region of glacial moraines before flowing into the Maumee Bay of Lake Erie. The city of Toledo is located at the mouth of the Maumee. The Maumee was designated an Ohio State Scenic River on July 18, 1974. The Maumee watershed is Ohio's breadbasket; it is two-thirds farmland, mostly corn and soybeans. It is the largest watershed of any of the rivers feeding the Great Lakes, and supplies five percent of Lake Erie's water.
Maumee Bay on Lake Erie is located in the U.S. state of Ohio, just east of the city of Toledo. The bay and the surrounding wetlands form most of the Maumee River basin, and in 1975 part of the area was incorporated into Maumee Bay State Park. The park is not huge, covering 1,450 acres (5.9 km2), but its wetlands feature some of the best bird watching in the United States. The Maumee Bay area is a popular vacation spot in the Midwest, featuring several resorts and a golf course.
The Limberlost Swamp in the eastern part of the present-day U.S. state of Indiana was a large, nationally known wetlands region with streams that flowed into the Wabash River. It originally covered 13,000 acres (53 km2) of present-day Adams and Jay counties. Parts of it were known as the Loblolly Marsh, based on a word by local Miami Native Americans for the sulphur smell of the marsh gas. The wetlands had mixed vegetation and supported a rich biodiversity, significant for local and migrating birds and insects, as well as other animals and life.
The Auglaize River is a 113-mile-long (182 km) tributary of the Maumee River in northwestern Ohio in the United States. It drains a primarily rural farming area in the watershed of Lake Erie. The name of the river was derived from the French term for it. The French called it "rivière à la Grande Glaize", referring to the soil in the area.
The Miami and Erie Canal was a 274-mile (441 km) canal that ran from Cincinnati to Toledo, Ohio, creating a water route between the Ohio River and Lake Erie. Construction on the canal began in 1825 and was completed in 1845 at a cost to the state government of $8 million. At its peak, it included 19 aqueducts, three guard locks, 103 canal locks, multiple feeder canals, and a few man-made water reservoirs. The canal climbed 395 feet (120 m) above Lake Erie and 513 feet (156 m) above the Ohio River to reach a topographical peak called the Loramie Summit, which extended 19 miles (31 km) between New Bremen, Ohio to lock 1-S in Lockington, north of Piqua, Ohio. Boats up to 80 feet long were towed along the canal by mules, horses, or oxen walking on a prepared towpath along the bank, at a rate of four to five miles per hour.
Maumee may refer to:
Lake Maumee was a proglacial lake and an ancestor of present-day Lake Erie. It formed about 17,500 calendar years, or 14,000 Radiocarbon Years Before Present (RCYBP) as the Huron-Erie Lobe of the Laurentide Ice Sheet retreated at the end of the Wisconsin glaciation. As water levels continued to rise the lake evolved into Lake Arkona and then Lake Whittlesey.
Metroparks Toledo, officially the Metropolitan Park District of the Toledo Area, is a public park district consisting of parks, nature preserves, a botanical garden, trail network and historic battlefield in Lucas County, Ohio.
Providence is a ghost town on the north side of the Maumee River in southern Providence Township, Lucas County, Ohio, United States, about 24 miles (39 km) southwest of Toledo. After suffering a destructive fire and a cholera epidemic in mid-19th century, the village was abandoned. In this period, canal traffic had also fallen off.
Lake Erie Basin consists of Lake Erie and surrounding watersheds, which are typically named after the river, creek, or stream that provides drainage into the lake. The watersheds are located in the states of Indiana, Michigan, New York, Ohio, and Pennsylvania in the United States, and in the province of Ontario in Canada. The basin is part of the Great Lakes Basin and Saint Lawrence River Watershed, which feeds into the Atlantic Ocean. 80% of the lake's water flows in from the Detroit River, with only 9% coming from all of the remaining watersheds combined. A littoral zone serves as the interface between land and lake, being that portion of the basin where the lake is less than 15 feet (4.6 m) in depth.
The Wilma H. Schiermeier Olentangy River Wetland Research Park is an experimental wetland complex located adjacent to the campus of Ohio State University in Columbus, Ohio, United States and is part of the School of Environment and Natural Resources at the university. Begun in 1992, the park has developed into a multitude of different habitats and setups which are used by OSU faculty and students for research. Additionally, the general public is welcome to enjoy independent tours of the area during daylight hours. Guided tours are also available upon request.
Mary Jane Thurston State Park is a 105-acre (42 ha) public recreation area one mile west of Grand Rapids in Wood and Henry counties, Ohio, United States. The state park lies along the south bank of the Maumee River near remains of the historic Miami and Erie Canal. It is named for Mary Jane Thurston, a schoolteacher from Grand Rapids who bequeathed land for the establishment of a park. The park's year-round recreation includes hunting, fishing, boating, picnicking, and camping.
William Mitsch is an ecosystem ecologist and ecological engineer who was co-laureate of the 2004 Stockholm Water Prize in August 2004 as a result of a career in wetland ecology and restoration, ecological engineering, and ecological modelling.
The Oak Openings Region is a globally rare ecosystem composed of over 1,300 square miles (3,400 km2) of Michigan and Ohio. The land consists largely of oak savanna and grassland prairie. It is considered by The Nature Conservancy as having a similar ecological importance as the Florida Everglades and is one of the 200 "Last Great Places on Earth".
The North Maumee Bay Archeological District is a historic district containing archeological sites located in the southeasternmost corner of Erie Township in Monroe County, Michigan. It was added to the National Register of Historic Places on December 5, 1980.
The story of the first European settlement in 1833 in the Great Black Swamp at Lauber Hill is told in "Out of the Wilderness, History of the Central Mennonite Church," 1835-1960. O. Grieser and E. Beck, The Dean Hicks Company, Grand Rapids Michigan, 1960.