Devil's Lake State Park | |
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Location | Sauk County, Wisconsin, United States |
Coordinates | 43°24′53″N89°42′47″W / 43.41472°N 89.71306°W |
Area | 9,217 acres (37.30 km2) |
Elevation | 1,329 ft (405 m) [1] |
Established | 1911 |
Governing body | Wisconsin Department of Natural Resources |
Devil's Lake State Park is a state park located in the Baraboo Range in eastern Sauk County, just south of Baraboo, Wisconsin. It is around thirty-five miles northwest of Madison, and is on the western edge of the last ice-sheet deposited during the Wisconsin glaciation. [2] The state park encompasses 9,217 acres (3,730 ha), [3] making it the largest in Wisconsin. [4] The state park is known for its 500-foot-high (150 m) quartzite bluffs along the 360-acre (150 ha) Devil's Lake, which was created by a glacier depositing terminal moraines that plugged the north and south ends of the gap in the bluffs during the last ice age approximately 12,000 years ago. The sand at the bottom of Devil's Lake is thought to be deposited by glaciers.
There are many quartzite rock formations, such as Balanced Rock and Devil's Doorway, throughout the park. Effigy mounds are also located throughout the park. The park contains approximately eleven miles of the 1,200-mile (1,900 km) Ice Age Trail. [5] Its scenery, along with its proximity to the Wisconsin Dells, has made it one of the most visited of Wisconsin's state parks for both day use and overnight camping; the park receives over three million visitors annually. [6] During the fall, the park's brilliant foliage makes it a popular attraction. Parfrey's Glen, Wisconsin's first state natural area, is managed by Devil's Lake State Park and located just east of the park.
The original inhabitants of the area around the lake date back much further than when the European settlers first discovered the land. There is proof that humans occupied the land between 12,000 to 16,000 years ago, but Ho-Chunk historians speak of people living there longer than 300,000 years ago. [7] The area may have been inhabited originally between 12,000 to 16,000 years ago due to the fact that this was the time the last of the glaciers had receded from the area. Many Native tribes throughout Wisconsin inhabited the lands. They called the lake various different names, such as Tewakakak or Minnewaukan, which translate to spirit lake in various Native American Languages. [7]
The area where the park now stands was first settled by pioneers in the mid-1800s. By the start of the 20th century, the area had become a popular vacation destination for wealthy families from Chicago and Madison. The first hotel was established in 1866, 50 years before the park was founded. [8]
The park was founded in 1911. [9] It was home to five resorts, two of which were perched on the west bluff. Few traces of these structures remain, though footings and foundational structures can be found along the South shore and near Prospect Point on the West Bluff. There were also many private residences in the west and south shores of the lake, only four of which remain. [10] At various times the lakeshore hosted water slides, lodges, ferry boat launches and golf courses. The clubhouse of one course sat on the current location of the Park's nature center. By the 1940s, the hotels were all closed, and the Park was retreating to its former natural self.
From 1934 to 1941, approximately two hundred members of the Civilian Conservation Corps resided in a work camp. These young men built many of the trails, buildings, and benches still in use today. [9]
In 1974, the National Park Service declared the Southern portion of the Baraboo Hills a National Natural Landmark. The Nature Conservancy also designated it as one of the "Last Great Places," one of only 77 such designations in the world. [4]
In 2020, a man was stabbed to death along the Grottos Trail. [11] Several witnesses reported seeing a man running from the scene of the murder, but he remains unidentified. As of 2024, the case remains unsolved. [12]
Loess covers most of the hills and forms the parent material of a brown silt loam soil. The lake is surrounded by a mixed conifer-deciduous forest and the Baraboo Hills are also home to one of the largest contiguous hardwood forests in the Midwest. [4]
Several moraines are featured in the park, another side effect of glaciation. The North Glacial Moraine is well covered by the north shore developments. The parking lots, concession building and the picnic shelter all sit atop the moraine. This moraine forms the northern border of Devil's Lake. [13] This moraine is approximately 80 feet (24 m) thick. [14] The Southeast Glacial Moraine is located between the East Bluff-South Face and the South Bluff. The Group Camp is located atop the moraine. It is best seen from the Roznos Meadow parking area along State Route 113. [13] The moraine is approximately 130 feet (40 m) thick. [14]
Due to the long geological history of Devil's Lake and the Baraboo Range, the area has been used in geological research for years. The lake itself is rectangular in shape and is a little over a mile long from north to south and a half mile from east to west. It has many cliffs, unique rock formations and a variety of animal and plant species. [15] One of the most notable features of the park is the presence of large talus slopes on three sides of the lake. [16]
The state park includes many buildings on its land. The exhibits at the park's nature center focus on the geology and natural history of the area. Public nature programs are offered in the summer, as well as evening programs on Saturday nights in the Northern Lights Amphitheater. The nature center also has many historical photographs that come from as far back as the 1800s. They also have many displays of examples of the flora and fauna that can be found throughout the park. [4]
The park has several American Indian mounds. Across the parking lot from the nature center are effigy mounds built in stylized animal shapes, such as a lynx and a sparrow. In front of the concession building is a linear mound, one of several geometric mounds in the park. These mounds were used as ancient burial sites by early North Americans. The nature center offers courses on the history of the effigy mounds. [17] [18]
There are 29 miles (47 km) of hiking trails in Devil's Lake State Park. There are trails ranging from handicapped-accessible paved trails, to steep, difficult hiking trails, to rigorous, off-trail routes. The highest point is at Prospect Point, on the West Bluff, 500 feet (150 m) above Devil's Lake. [19]
Devil's Lake State Park has four miles of off-road - the Upland Trail Loop. There are no official paved road-bike trails in the park, although many people enjoy riding several miles on all the paved campground roads.
There are four popular campgrounds at the park containing 407 campsites all together:[ citation needed ]
Northern Lights Campground features a decent sledding hill. [4]
The geology of the Baraboo Hills surrounding Devil's Lake makes it one of the premier rock climbing areas in the Midwest, with climbs of varying difficulty. The Baraboo Hills are primarily quartzite, which is solid enough to climb. Most outcroppings in the region, especially in the Driftless Area, are composed of sandstone or limestone, which are too brittle to climb safely.
Devil's Lake has enjoyed a history of rock climbing since early ascents in the 20th century. Climbers such as the Stettner Brothers, and members of the hard-climbing group "DLFA" [20] have frequented the park extensively. Guidebooks cover more than a lifetime's worth of unique "routes" and sub-areas of the park. [21] For climbers, unique names for each major bluff formation is important in finding specific climbs and areas. The climbing style and protection system at Devil's Lake is known for its difficult, glassy rock and traditional fall-protection methods and anchors. [21]
There have been occasional deaths, injuries, and emergency rescues among the rock climbers at Devil's Lake. [22] [23]
The "East Bluff" refers to the Eastern outcroppings in the park, and includes many sub-areas for climbers, including "Doorway Mass" which are climbs surrounding the famous Devil's Doorway formation, "Balanced Rock Wall" near the famous Balanced rock, and an area off of the CCC trail known as the "East Ramparts" which is the most popular due to the high concentration of sheer, unbroken cliff faces to climb. [24]
The west side of the park features climbing areas such as "Stettner Rocks", The Cleo Amphitheatre, and the "Lost Face". The Cleo Amphitheatre features the classic climb of a 25 ft freestanding spire known as "Cleopatra's Needle" [21] [25]
Wildlife abounds at Devil’s Lake State Park. Among the flora and fauna [26] at Devil’s Lake are:
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Wood County is a county located in the U.S. state of Wisconsin. As of the 2020 census, the population was 74,207. Its county seat is Wisconsin Rapids. The county is named after Joseph Wood, a member of the Wisconsin State Assembly. Wood County comprises the Wisconsin Rapids-Marshfield, WI Micropolitan Statistical Area and is included in the Wausau-Stevens Point-Wisconsin Rapids, WI Combined Statistical Area.
The Ice Age Trail is a National Scenic Trail stretching 1,200 miles (1,900 km) in the state of Wisconsin in the United States. The trail is administered by the National Park Service, and is constructed and maintained by private and public agencies including the Ice Age Trail Alliance, a non-profit and member-volunteer based organization with local chapters. It became an official unit of the National Park System in 2023.
The Wisconsin glaciation, also called the Wisconsin glacial episode, was the most recent glacial period of the North American ice sheet complex, peaking more than 20,000 years ago. This advance included the Cordilleran Ice Sheet, which nucleated in the northern North American Cordillera; the Innuitian ice sheet, which extended across the Canadian Arctic Archipelago; the Greenland ice sheet; and the massive Laurentide Ice Sheet, which covered the high latitudes of central and eastern North America. This advance was synchronous with global glaciation during the last glacial period, including the North American alpine glacier advance, known as the Pinedale glaciation. The Wisconsin glaciation extended from about 75,000 to 11,000 years ago, between the Sangamonian Stage and the current interglacial, the Holocene. The maximum ice extent occurred about 25,000–21,000 years ago during the last glacial maximum, also known as the Late Wisconsin in North America.
Glacial Lake Wisconsin was a prehistoric proglacial lake that existed from approximately 18,000 to 14,000 years ago, at the end of the last ice age, in the central part of present-day Wisconsin in the United States.
The Driftless Area, also known as Bluff Country and the Paleozoic Plateau, is a topographical and cultural region in the Midwestern United States that comprises southwestern Wisconsin, southeastern Minnesota, northeastern Iowa, and the extreme northwestern corner of Illinois. The Driftless Area is a USDA Level III Ecoregion: Ecoregion 52. The Driftless Area takes up a large portion of the Upper Midwest forest–savanna transition. The eastern section of the Driftless Area in Minnesota is called the Blufflands, due to the steep bluffs and cliffs around the river valleys. The western half is known as the Rochester Plateau, which is flatter than the Blufflands. The Coulee Region is the southwestern part of the Driftless Area in Wisconsin. It is named for its numerous ravines.
Interstate Park comprises two adjacent state parks on the Minnesota–Wisconsin border, both named Interstate State Park. They straddle the Dalles of the St. Croix River, a deep basalt gorge with glacial potholes and other rock formations. The Wisconsin park is 1,330 acres (538 ha) and the Minnesota park is 298 acres (121 ha). The towns of Taylors Falls, Minnesota and St. Croix Falls, Wisconsin are adjacent to the park. Interstate Park is within the Saint Croix National Scenic Riverway and the Ice Age National Scientific Reserve. The western terminus of the Ice Age National Scenic Trail is on the Wisconsin side. On the Minnesota side, two areas contain National Park Service rustic style buildings and structures that are listed on the National Register of Historic Places.
Devil's Lake is a lake in the South Range of the Baraboo Range, about two miles south of Baraboo, Wisconsin, in Sauk County, Wisconsin, United States. It has no surface outlets, so by some definitions, it is endorheic; however, it possibly drains by underground channels into the Baraboo River, which would make the lake cryptorheic. The lake is one of the primary attractions of Devil's Lake State Park. It is also a popular recreation destination for watercraft, fishing, hiking, and climbing.
Sakatah Lake State Park is an 842-acre (341 ha) state park of Minnesota, USA, on a natural widening of the Cannon River near the town of Waterville. The Dakota native to the area called it "Sakatah" which means "singing hills". To honor this native heritage, some of the trails in the park have been given Dakota names. The Sakatah Singing Hills State Trail, which connects Faribault and Mankato, runs through this park.
The Pike Lake Unit of the Kettle Moraine State Forest is a 825-acre (334 ha) unit of the Wisconsin state park system. The unit is located just east of Hartford, Wisconsin on State Highway 60, on the east shore of the 446-acre (180 ha) Pike Lake. It was dedicated by Wisconsin governor Patrick J. Lucey in June 1971.
Willow River State Park is a 2,891-acre (1,170 ha) Wisconsin state park located five miles (8 km) north of Hudson. The centerpiece of the park is Willow Falls, a powerful cascade in a 200-foot (61 m) deep gorge. Another popular feature is Little Falls Lake, a shallow reservoir on the Willow River. Because of its proximity to Minneapolis-St. Paul it is one of the most visited state parks in Wisconsin. Trilobite fossils found in the lower layers of the gorge indicate the rock is around 600 million years old.
Mill Bluff State Park is a state park in west-central Wisconsin, United States. It is located in eastern Monroe and western Juneau counties, near the village of Camp Douglas. A unit of the Ice Age National Scientific Reserve, the park protects several prominent sandstone bluffs 80 feet (24 m) to 200 feet (61 m) high that formed as sea stacks 12,000 years ago in Glacial Lake Wisconsin. As a result, these bluffs are steep and angular, dissimilar to the rounded terrain more typical of the eastern half of the United States. The bluffs served as landmarks to both early pioneers and travelers today on Interstate 90/94, which passes through the park.
The Baraboo Range is a mountain range in Columbia County and Sauk County, Wisconsin. Geologically, it is a syncline fold consisting of highly eroded Precambrian metamorphic rock. It is about 25 miles (40 km) long and varies from 5 to 10 miles (16 km) in width. The Wisconsin River, previously traveling in a north to south direction, turns to the east just north of the range before making its turn to the west towards the Upper Mississippi River. The eastern end of the range was glaciated during the Wisconsinian glaciation, while the western half was not, and consequently, marks the eastern boundary of Wisconsin's Driftless Area.
Wisconsin, a state in the Midwestern United States, has a vast and diverse geography famous for its landforms created by glaciers during the Wisconsin glaciation 17,000 years ago. The state can be generally divided into five geographic regions—Lake Superior Lowland, Northern Highland, Central Plain, Eastern Ridges & Lowlands, and Western Upland. The southwestern part of the state, which was not covered by glaciers during the most recent ice age, is known as the Driftless Area. The Wisconsin glaciation formed the Wisconsin Dells, Devil's Lake, and the Baraboo Range. A number of areas are protected in the state, including Devil's Lake State Park, the Apostle Islands National Lakeshore, and the Chequamegon–Nicolet National Forest.
Pewit's Nest State Natural Area is a nature reserve in Wisconsin, USA, that includes a deep gorge formed during the retreat of the last glacier. Pewit's Nest is outside Baraboo in Sauk County. At one time a waterwheel and mill were located on the site and an individual lived in the solid sandstone. The name of the site was a result of early settlers calling it "Peewit's Nest" after the abode, ten feet above a deep pool of water, resembling the nest of a phoebe. The water-wheel once turned lathes for repairing or manufacturing equipment, but no evidence of it remains. Pewit's Nest is owned by the Wisconsin Department of Natural Resources and was designated a State Natural Area in 1985.
Parfrey's Glen, located within Devil's Lake State Park, is a Wisconsin Department of Natural Resources-designated State Natural Area. The glen is a deep gorge cut through the sandstone of the south flank of the Baraboo Hills. It was the first State Natural Area to be designated in Wisconsin. The valley was named for Robert Parfrey.
Baraboo Quartzite is a Precambrian geological formation of quartzite, found in the region of Baraboo, Wisconsin. While pure quartzite is usually white or gray, Baraboo Quartzite is typically dark purple to maroon in color, due to the presence of iron (hematite) and other impurities. Baraboo Quartzite may display strata created by progressive deposition of layers of sand in the original sandstone from which the quartzite was formed. Specimens of Baraboo quartzite may also display ripple marks that appear visually similar to the patterns one might see in the sand at a beach. Ripples indicate that the sandstone from which the quartzite was metamorphosed was originally water-laid sediment.
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The geology of Wisconsin includes Precambrian crystalline basement rock over three billion years old. A widespread marine environment during the Paleozoic flooded the region, depositing sedimentary rocks which cover most of the center and south of the state.
Kiser Lake Wetlands State Nature Preserve, or simply Kiser Lake Wetlands, is a 51 acres (21 ha) nature reserve located in Johnson Township, Champaign County, Ohio, United States. It is located wholly within the Kiser Lake State Park, and operated by the Ohio Department of Natural Resources.
Devil's Doorway is a rock formation in Devil's Lake State Park. The signature feature of the park, it is a popular spot for climbing and photographs. The quartzite rocks that make up Devil's Doorway form a doorway-shaped natural rock arch.
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