Cascade Falls (Osceola)
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Cascade Falls (Osceola)
Cascade Falls is a waterfall in the small town of Osceola, Wisconsin. The water source for Cascade Falls is the Osceola Creek which runs through the Osceola Mill Pond and then flows into the St. Croix River (Wisconsin-Minnesota). Characteristics The structure of the Cascade Falls has an undercutting knickpoint. The knick point is created by the flow and splash of water, which will eventually cause the base of the water fall to erode and eventually become unstable enough to collapse. Geology The Cascade Falls were carved out by the St. Croix River which is much larger. The St. Croix River created a canyon A canyon (from ; archaic British English spelling: ''cañon''), or gorge, is a deep cleft between escarpments or cliffs resulting from weathering and the erosion, erosive activity of a river over geologic time scales. Rivers have a natural tenden ... which developed the Osceola Creek and the smaller Geiger Falls in the same area. History William Kent discovered the Cascade Fa ...
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Osceola, Wisconsin
Osceola is a village in Polk County, Wisconsin, United States. The population was 2,568 at the 2010 census. Located mostly within the Town of Osceola, the village sits on the border with Minnesota, separated by the St. Croix River. It is along Wisconsin Highway 35. History The village was named after Osceola, chief of the Seminoles. Geography Osceola is located at (45.322365, -92.698534). Cascade Falls, a waterfall with a crest on Osceola Creek, is located in downtown Osceola. According to the United States Census Bureau, the village has a total area of , of which, of it is land and is water. Demographics 2010 census As of the census of 2010, there were 2,568 people, 1,142 households, and 660 families living in the village. The population density was . There were 1,289 housing units at an average density of . The racial makeup of the village was 96.0% White, 0.3% African American, 0.3% Native American, 1.0% Asian, 0.9% from other races, and 1.6% from two or more races ...
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Waterfall
A waterfall is a point in a river or stream where water flows over a vertical drop or a series of steep drops. Waterfalls also occur where meltwater drops over the edge of a tabular iceberg or ice shelf. Waterfalls can be formed in several ways, but the most common method of formation is that a river courses over a top layer of resistant bedrock before falling on to softer rock, which Erosion, erodes faster, leading to an increasingly high fall. Waterfalls have been studied for their impact on species living in and around them. Humans have had a distinct relationship with waterfalls for years, travelling to see them, exploring and naming them. They can present formidable barriers to navigation along rivers. Waterfalls are religious sites in many cultures. Since the 18th century they have received increased attention as tourist destinations, sources of hydropower, andparticularly since the mid-20th centuryas subjects of research. Definition and terminology A waterfall is gen ...
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Knickpoint
In geomorphology, a knickpoint or nickpoint is part of a river or channel where there is a sharp change in channel slope, such as a waterfall or lake. Knickpoints reflect different conditions and processes on the river, often caused by previous erosion due to glaciation or variance in lithology. In the cycle of erosion model, knickpoints advance one cycle upstream, or inland, replacing an older cycle. A knickpoint that occurs at the head (furthest upstream extent) of a channel is called a headcut. Headcuts resulting in headward erosion are hallmarks of unstable expanding drainage features such as actively eroding gullies. Knickpoints also occur on other planetary bodies that previously had or currently have surface liquids, namely Mars and Titan. On Mars, the knickpoints have a common elevation that suggest a common sea level for a former Martian ocean. On Titan, mountain valleys adjacent to the present-day hydrocarbon seas show evidence of knickpoints and recent sea-level ...
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Canyon
A canyon (from ; archaic British English spelling: ''cañon''), or gorge, is a deep cleft between escarpments or cliffs resulting from weathering and the erosion, erosive activity of a river over geologic time scales. Rivers have a natural tendency to cut through underlying surfaces, eventually wearing away rock layers as sediments are removed downstream. A river bed will gradually reach a baseline elevation, which is the same elevation as the body of water into which the river drains. The processes of weathering and erosion will form canyons when the river's River source, headwaters and estuary are at significantly different elevations, particularly through regions where softer rock layers are intermingled with harder layers more resistant to weathering. A canyon may also refer to a rift between two mountain peaks, such as those in ranges including the Rocky Mountains, the Alps, the Himalayas or the Andes. Usually, a river or stream carves out such splits between mountains. Examp ...
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Waterfalls Of Wisconsin
A waterfall is a point in a river or stream where water flows over a vertical drop or a series of steep drops. Waterfalls also occur where meltwater drops over the edge of a tabular iceberg or ice shelf. Waterfalls can be formed in several ways, but the most common method of formation is that a river courses over a top layer of resistant bedrock before falling on to softer rock, which erodes faster, leading to an increasingly high fall. Waterfalls have been studied for their impact on species living in and around them. Humans have had a distinct relationship with waterfalls for years, travelling to see them, exploring and naming them. They can present formidable barriers to navigation along rivers. Waterfalls are religious sites in many cultures. Since the 18th century they have received increased attention as tourist destinations, sources of hydropower, andparticularly since the mid-20th centuryas subjects of research. Definition and terminology A waterfall is generally d ...
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