Cabin Creek Raised Bog | |
---|---|
Location | Randolph County, Indiana |
Nearest city | Winchester, IN |
Coordinates | 40°08′15″N85°07′30″W / 40.13750°N 85.12500°W |
Area | 40 acres (16 ha) |
Designated | 1975 |
Governing body | National Park Service |
The Cabin Creek Raised Bog is a 40-acre raised bog located in Randolph County, Indiana, near Farmland. Identified as one of the few post-glacial raised bogs remaining in the Eastern Deciduous Forest Province of the central United States, [1] it was designated as a National Natural Landmark in 1975.
The Cabin Creek Raised Bog is an elevated fen, a peat-forming wetland characterized by alkaline water and soil. Its hydrology comes from artesian seeping water, rather than running water. It is rich in the living species adapted to fen life, many of which are rare or even endangered species because most of the fenlands of the United States have been altered or drained. [2] When surveyed by the United States Fish and Wildlife Service (USFWS) in 1973–1974, the Cabin Creek Raised Bog contained elevations that were elevated as much as 10 feet above the surrounding floodplain. Local groundwater movements created an artesian flow that caused water to seep into the fen and its saturated peatland. The water is alkaline, having flowed through calcium-rich layers of gravel or stone. [1]
The USFWS performed a biological inventory of the Cabin Creek Raised Bog, finding over 200 species of plant life within the 40-acre parcel. Key species were quaking aspen and prickly ash. [1]
The United States Fish and Wildlife Service is an agency within the United States Department of the Interior dedicated to the management of fish, wildlife, and natural habitats. The mission of the agency is "working with others to conserve, protect, and enhance fish, wildlife, plants and their habitats for the continuing benefit of the American people."
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.
A fen is a type of peat-accumulating wetland fed by mineral-rich ground or surface water. It is one of the main types of wetlands along with marshes, swamps, and bogs. Bogs and fens, both peat-forming ecosystems, are also known as mires. The unique water chemistry of fens is a result of the ground or surface water input. Typically, this input results in higher mineral concentrations and a more basic pH than found in bogs. As peat accumulates in a fen, groundwater input can be reduced or cut off, making the fen ombrotrophic rather than minerotrophic. In this way, fens can become more acidic and transition to bogs over time.
A bog or bogland is a wetland that accumulates peat as a deposit of dead plant materials – often mosses, typically sphagnum moss. It is one of the four main types of wetlands. Other names for bogs include mire, mosses, quagmire, and muskeg; alkaline mires are called fens. A bayhead is another type of bog found in the forest of the Gulf Coast states in the United States. They are often covered in heath or heather shrubs rooted in the sphagnum moss and peat. The gradual accumulation of decayed plant material in a bog functions as a carbon sink.
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Minerotrophic refers to environments that receive nutrients primarily through groundwater that flows through mineral-rich soils or rock, or surface water flowing over land. Minerotrophic, “minerogenous”, and “geogenous” are now often used interchangeably, although the latter two terms refer primarily to hydrological systems, while the former refers to nutrient dynamics. The hydrologic process behind minerotrophic wetlands results in water that has acquired dissolved chemicals which raise the nutrient levels and reduce the acidity. This in turn affects vegetation assemblages and diversity in the wetland in question. If dissolved chemicals include chemical bases such as calcium or magnesium ions, the water is referred to as base-rich and is neutral or alkaline. In contrast to minerotrophic environments, ombrotrophic environments get their water mainly from precipitation, and so are very low in nutrients and more acidic. Of the various wetland types, fens and rich fens are often minerotrophic while poor fens and bogs are often ombrotrophic. Marshes and swamps may also be fed through groundwater sources to a degree.
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