Indiana Dunes National Park

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Indiana Dunes National Park
Indiana Dunes National Lakeshore, Michigan City, Indiana, Estados Unidos, 2012-10-20, DD 03.jpg
Indiana Dunes National Park
Location Porter County, Lake County and LaPorte County, Indiana, United States
Nearest city Beverly Shores, Indiana
Porter, Indiana
Coordinates 41°38′53″N87°06′29″W / 41.64806°N 87.10806°W / 41.64806; -87.10806
Area15,349 acres (62.12 km2)
EstablishedNovember 5, 1966 (national lakeshore)
February 15, 2019 (national park)
Visitors2,834,180(in 2022 [1] )
Governing body National Park Service
Website Indiana Dunes National Park

Indiana Dunes National Park is a United States national park located in northwestern Indiana managed by the National Park Service. It was authorized by Congress in 1966 as the Indiana Dunes National Lakeshore and was redesignated as the nation's 61st national park on February 15, 2019. [2] The park runs for about 20 miles (32 km) along the southern shore of Lake Michigan and covers 15,349 acres (6,212 ha). Along the lakefront, the eastern area is roughly the lake shore south to U.S. 12 or U.S. 20 between Michigan City, Indiana, on the east and the Cleveland-Cliffs steel plant on the west. This area's conservation scheme is enhanced by the older Indiana Dunes State Park. To the west of the steel plant lies West Beach and a small extension south of the steel mill continues west along Salt Creek to Indiana 249. The western area is roughly the shoreline south to U.S. 12 between the Burns Ditch west to Broadway in downtown Gary, Indiana. In addition, there are several outlying areas, including Pinhook Bog, in LaPorte County to the east; the Heron Rookery in Porter County, the center of the park; and the Calumet Prairie State Nature Preserve and the Hobart Prairie Grove, both in Lake County, the western end of the park.

Contents

History

West side of the national park Indiana Dunes parkmap west.jpg
West side of the national park
East side of the national park Indiana Dunes NL parkmap east.jpg
East side of the national park

There is little evidence of permanent Native American communities forming during the earlier years; rather, the evidence suggests that seasonal hunting camps were the norm. The earliest evidence for permanent camps was the occupation of the Ohio valley by the Hopewell culture. Five groups of mounds have been documented in the dunes area. These mounds are consistent with the period of 200 BCE (Goodall Focus) to 800 CE (early Mississippian), [3] though even that was a short lived permanency. Beginning in the 1500s, European exploration and trade introduced more changes to the human environment. Tribal animosities and traditional European competition affected tribal relations[ not specific enough to verify ]. Entire populations began moving westward, while others sought to dominate large geographic trading areas. Once again, the dunes became a middle point on a journey from the east or the west. It continued to remain a key hunting ground for villages over a wide area. [4]

It wasn't until the 19th century that native villages once again were scattered through the area, but this was soon followed by European settlement. [5] Joseph Bailly was the earliest recorded settler in the dunes. He moved here from trading villages around Niles, Michigan. Settling along the Calumet River. [5] Soon he was joined by a series of other settlers and the communities in the dunes began to develop. They included Chesterton, Porter, Tremont, and the Town of the Pines. These pioneer communities grew and expanded.

City West was one of several "ghost towns" situated in the dunes. Planned as a rival to Chicago, [6] it was partly built in 1837 but failed that summer, during a national economic panic. The remains of the town, partly carted off to be used as lumber, were located near where the pavilion in the state park now stands, until a forest fire in the 1850s destroyed whatever was left. [6] Today, most of the coastline has been settled for use as homes, factories, and businesses, with some areas reserved for public parks.

Preserving the dunes and National Lakeshore

Steven Mather visits the Indiana Dunes. Steven Mather Visit to Indiana Dune (cropped).jpg
Steven Mather visits the Indiana Dunes.

Triggered by a publication on the unique flora of the dunes in the 1899 Botanical Gazette by University of Chicago botanist Henry Chandler Cowles, [7] a movement began to preserve the dunes habitat. [8] In 1916, the visionary National Parks Director Stephen Mather held hearings in Chicago on a "Sand Dunes National Park". [9] Another factor leading to the desire to preserve the dunes was the disappearance of the Hoosier Slide, a particularly large dune along this shore. The sand from this dune was found to be ideal for glass manufacture, and much of this sand was transported to the Ball Brothers and Hemingray Glass Co. plants in Muncie, producing the well-known 'Ball Blue' canning jars and 'Hemingray Blue' insulators. The Hoosier Slide was completely consumed by 1920, and a power plant sits on the site today. [10] In 1926, the Indiana Dunes State Park opened. In the 1950s, a desire to maximize economic development through a "Port of Indiana" spurred interest in preservation. The Save the Dunes Council, including its president Dorothy Richardson Buell and activist Hazel Hannell, began a nationwide campaign to buy the land. Their first success was the purchase of 56 acres (23 ha) in Porter County, the Cowles Tamarack Bog. [9] The Kennedy Compromise entailed the creation of a national lakeshore and a port. [8] Illinois Senator Paul H. Douglas led the Congressional effort to save the dunes. In late 1966, the bill passed and the Indiana Dunes National Lakeshore became a reality. Four subsequent expansion bills for the park (1976, 1980, 1986, and 1992) have increased the size of the park to more than 15,000 acres (61 km2). [9]

Redesignation as National Park

A bill to reclassify Indiana Dunes National Lakeshore as Indiana Dunes National Park was sponsored by Representative Pete Visclosky and Senators Todd Young and Mike Braun and previously by Senator Joe Donnelly, who wanted to bring the site more recognition. [11] [12] Deputy Director of the National Park Service Paul Daniel Smith testified that the Service opposed the redesignation because it would be inconsistent with the Service's naming conventions and the Indiana Dunes have more in common with other national lakeshores and seashores than national parks, which are typically much larger. [11] [13]

H.R. 1488 originally passed in the House of Representatives on November 1, 2017, but it did not receive a vote in the Senate during the 115th Congress. The Consolidated Appropriations Act of 2019 included the bill as a provision and was signed by President Donald Trump on February 15, creating the country's 61st National Park and the first in Indiana. [14] [15]

Geography

The creeks and rivers of the national park include:

Climate

According to the Köppen climate classification system, Indiana Dunes National Park has a hot summer Humid continental climate (Dfa). According to the United States Department of Agriculture, the plant hardiness zone at Indiana Dunes National Park at 614 ft (187 m) is 6a with an average annual extreme minimum temperature of −9.4 °F (−23.0 °C). [21]

The primary feature of Indiana Dunes National Park is Lake Michigan. The lake brings with it several weather-related conditions that can create threats to the enjoyment of the area.

Climate data for Indiana Dunes National Lakeshore, Indiana, 1991–2020 normals, extremes 1989–present
MonthJanFebMarAprMayJunJulAugSepOctNovDecYear
Record high °F (°C)66
(19)
72
(22)
85
(29)
88
(31)
95
(35)
98
(37)
102
(39)
98
(37)
96
(36)
89
(32)
77
(25)
69
(21)
102
(39)
Mean maximum °F (°C)52.5
(11.4)
56.6
(13.7)
70.0
(21.1)
79.4
(26.3)
86.9
(30.5)
91.3
(32.9)
92.7
(33.7)
91.4
(33.0)
88.9
(31.6)
81.8
(27.7)
68.1
(20.1)
56.7
(13.7)
94.4
(34.7)
Mean daily maximum °F (°C)32.1
(0.1)
35.5
(1.9)
45.6
(7.6)
57.2
(14.0)
68.4
(20.2)
77.5
(25.3)
81.6
(27.6)
80.0
(26.7)
74.3
(23.5)
62.3
(16.8)
48.7
(9.3)
37.4
(3.0)
58.4
(14.7)
Daily mean °F (°C)24.9
(−3.9)
28.3
(−2.1)
37.7
(3.2)
48.4
(9.1)
59.0
(15.0)
68.5
(20.3)
73.0
(22.8)
71.6
(22.0)
65.3
(18.5)
53.5
(11.9)
41.5
(5.3)
30.8
(−0.7)
50.2
(10.1)
Mean daily minimum °F (°C)17.8
(−7.9)
21.1
(−6.1)
29.8
(−1.2)
39.5
(4.2)
49.6
(9.8)
59.5
(15.3)
64.3
(17.9)
63.1
(17.3)
56.3
(13.5)
44.7
(7.1)
34.2
(1.2)
24.1
(−4.4)
42.0
(5.6)
Mean minimum °F (°C)−3.7
(−19.8)
2.0
(−16.7)
12.6
(−10.8)
26.0
(−3.3)
35.5
(1.9)
44.5
(6.9)
52.8
(11.6)
52.6
(11.4)
42.5
(5.8)
31.5
(−0.3)
20.2
(−6.6)
5.2
(−14.9)
−7.3
(−21.8)
Record low °F (°C)−22
(−30)
−15
(−26)
−4
(−20)
18
(−8)
31
(−1)
37
(3)
45
(7)
46
(8)
35
(2)
23
(−5)
7
(−14)
−19
(−28)
−22
(−30)
Average precipitation inches (mm)2.21
(56)
1.97
(50)
2.34
(59)
3.55
(90)
4.27
(108)
4.31
(109)
3.98
(101)
4.08
(104)
3.65
(93)
3.75
(95)
2.76
(70)
2.29
(58)
39.16
(995)
Average snowfall inches (cm)16.0
(41)
9.7
(25)
6.0
(15)
0.6
(1.5)
0.0
(0.0)
0.0
(0.0)
0.0
(0.0)
0.0
(0.0)
0.0
(0.0)
0.0
(0.0)
0.7
(1.8)
7.3
(19)
40.3
(102)
Average precipitation days (≥ 0.01 in)12.69.010.911.312.311.79.79.99.611.510.611.9131.0
Average snowy days (≥ 0.1 in)8.45.63.40.60.00.00.00.00.00.01.05.724.7
Source: NOAA [23] [24]

Geology

Glacial Lake Chicago, 14,000 years before present. In this map, the present dunes park area is covered by the lake at left. Formation of the dunes is in part due to action of the advancing and receding melt water. Glacial Lake Chicago (14,000 YBP) 7a.jpg
Glacial Lake Chicago, 14,000 years before present. In this map, the present dunes park area is covered by the lake at left. Formation of the dunes is in part due to action of the advancing and receding melt water.

The Lake Michigan Basin was formed during the Wisconsin Glacial Period. The Michigan Lobe of the continental glacier began its retreat northward over 20,000 years before present (YBP) [25] forming the southern shore of the Lake Michigan Basin.

The Valparaiso Moraine is the dominant geologic form that created the various landscape forms of the Indiana Dunes about 40,000 YBP. [25] Within the arc created by the Valparaiso Moraine are the two younger recessional moraines of the Tinley Moraine and the Lake Border Moraine. Each moraine created an dam across the southern outflow of the melt waters of the receding glaciers. As each glacial lake breached a low spot in the moraines, water levels receded, leaving a series of shorelines and dune ridges. [25]

The Calumet Shoreline is the oldest visible shoreline of Lake Michigan. It is a visible sand ridge along Ridge Road through Lake and Porter Counties, Indiana. Two older shorelines, the Tolleston and the Glenwood Shoreline are much harder to identify and further south in those counties. [26]

During the periods of glacial retreat, there were periods of stability. During these times, glacial lakes formed along the southern borders of the glaciers, bound into the Lake Michigan Basin by the recessional moraines. Four major glacial lake periods created the Indiana Dunes. They are the glacial Lake Chicago (14,000 YBP), glacial Lake Algonquin (9,000 YBP), glacial Lake Chippewa (7,000 YBP), and the Nipissing Great Lakes stage (4,000 YBP). Once the glaciers had fully retreated from the Lake Michigan basin, after the Lake Nipissing stage, the same factors that created the dunes south of the current shoreline, expanded the existing shoreline. [25] The littoral currents or Longshore drift transport sand southward along the eastern shore of Lake Michigan. As they encounter streams bringing water from inland, sandbars are created, pointing down current, either southward if the shore is north to south or westward along the southern shore itself. [26] If the currents were strong enough, as they were when the Glenwood Shoreline was created, shallow inland bays would be formed with a wide sand spit between each bay and the open lake. [26] Over time, the sand spits would merge with the far shoreline, forming interdunal ponds. [26] Each sand spit would become a dune ridge. As the ponds filled in and wind built the outer sand ridges higher, the ponds would dry up and only a stream would remain, as with the Little Calumet River today, just south of the state and national parks. As the shoreline moved northward, new ridges formed along with additional streams, now slower and less powerful, and the process duplicated itself. To the west of the Indiana Dunes, Wolf Lake in Hammond, Indiana, forms a western border to the dunes. Here the same process is at work, only the littoral drift is again south, but along the western shore, pushing the sand and sand spits eastward. [26] Today, it is the remnants of the marsh lands and inter-dunal or inter-sand spit lakes that have formed this region over 40,000 years. [26]

Flora and fauna

The park is in the central forest-grasslands transition ecoregion.

According to the A. W. Kuchler U.S. Potential natural vegetation Types, Indiana Dunes National Park has an Oak/Hickory (100) potential vegetation type and an Eastern Hardwood forest, aka Temperate broadleaf and mixed forest (26) potential vegetation form. [27]

Rare, threatened, and endangered species

The park includes habitats for several rare plants and animals. The park has more than 1,400 species of vascular plants, ranking it 8th in total plant species among all units of the National Park System. At least two plant species are on the Federal list of Threatened and Endangered Species:

Several others are on the list of state T&E species. [28] Populations of each plant group are estimated to be around 100–120 individual plants. The species included are: [28]

Among the federally threatened and endangered wildlife are: [28]

In addition, the park has habitat suitable for the bald eagle (Haliaeetus leucocephalus). [28]

Species count

GroupNumber of speciesExtirpated speciesMain article
Chordates or Animals with Backbones
Mammals or Mammalia
41
11 [29]
Mammals of the Indiana Dunes
Birds or Aves
352 [30]
2
Birds of the Indiana Dunes
Reptiles or Reptilia
23 [30]
List of reptiles of the Indiana Dunes
Amphibians or Amphibia
18
List of amphibians of the Indiana Dunes
Fish
71 [30]
List of fish of the Indiana Dunes
Invertebrate or Animals without Backbones
Arthropoda (Crustacea)-Crustacean
15
List of crustaceans of the Indiana Dunes
Arthropoda (Chelicerata)-Arachnida
12
List of arachnids of the Indiana Dunes
Arthropoda (Chelicerata)-Insects
296
Arthropoda (Myriapoda)- Other invertebrates
2
Invertebrates of Indiana Dunes
Annelida-segmented worms
Mollusca
66
List of non-marine mollusks of the Indiana Dunes
Plants or Plantae
Vascular plantferns. [31]
26
Vascular plant-clubmosses
Vascular plant-flowering plants
1,130 [32]
Vascular plant-conifers
Fungi
64
Bryophytes  Bryophyta (mosses), Marchantiophyta (liverworts), and Anthocerotophyta (hornworts).
41
Algae  – especially the green algae.
Lichens algae and fungi in a symbiotic arrangement [33]
62
92
Change in the number of species between 1896 (Calkins) and 1986 (Wetmore) [33]
Invasive Plants
54
List of invasive plant species in the Indiana Dunes
Plankton and other microscopic life forms
Plankton [34]
33
Total to date
2,336
105

Wildlife

Indiana Dunes National Park is host to wide variety of wildlife, including white-tailed deer, red fox, raccoons, opossums, cottontail rabbits, various rodents, Canada geese, gulls, squirrels, hawks, turkey vultures, mallards, great blue herons, songbirds, and garter snakes. Recent records, documented photographically, indicate that North American river otter (Lontra canadensis) and bobcat (Lynx rufus) began returning to the area in 2011 and 2018, respectively. As of 2023, the Indiana Audubon have observed nearly 370 bird species living in or migrating through the Indiana Dunes.

Flowering plants

Indiana Dunes has over 369 species of flowering plants. Of these, thirteen are considered threatened or in danger of extinction. Additionally, there four invasive flowering plants on the list. Some of the most common spring flowers include the May apple, buttercups (six varieties), and violets (14 varieties). Summer brings out the orchids (five varieties) and much goldenrod (11 varieties). [35]

Invasive plants

Invasive plants are those introduced species that dominate a landscape pushing out traditionally native species and others species by their ability to multiply rapidly. There are 54 such species in the dunes. [36]

Unusual sightings

In October 1920, a rare Arctic three-toed woodpecker was captured a mile west of Dune Park Station. Later that month another male was captured east of Dune Park Station. One was busy digging out grubs and the other was nervously flying from tree to tree. [37]

In May 1919, a clay-colored sparrow was found near Dune Park. It was a part of a larger flock of Harris's sparrow migrating along the western shore of Lake Michigan. [37]

Extirpated species

Several species of plants and animals have disappeared from the dunes. Few can be clearly identified. Among those species thought to be gone are listed below:

SpeciesLatin NameLast Seen [29]
Eastern cougar [38] Puma concolor couguar
1830
American bison Bison bison
1731
Elk/WapitiCervus canadensis canadensis
1830
Canada lynx Lynx canadensis
1880
Bobcat Lynx rufus [29]
1880
Gray wolf Canis lupus [29]
1908
Red wolf Canis rufus [29]
1832
American black bear Ursus americanus [29]
1850
Fisher Pekania pennanti
1855
River otter Lontra canadensis
1900
Porcupine Erethizon dorsatum [29]
1918
Passenger pigeon Ectopistes migratorius
1900, extinct
Piping plover Charadrius melodus

Exotic and invasive species

Alien or exotic species are plants and animals which are not native to the area. These plants can be classified as Invasive if they rapidly replace other plants and animals in the ecosystem, creating a monoculture and threatening the extinction of the traditional plants and animals. Among plants found in the park, the following are considered to be exotic. Those marked with an '*' are listed as invasive.

BioBlitz

On May 15 and 16, 2009, the park hosted an All Taxa Biological Diversity survey. In a 24-hour period, as part of the BioBlitx 2,000 students and thousands of additional volunteers surveyed the park for every available living species. John Francis, vice president of research, conservation and exploration for the National Geographic Society, stated that 890 species had been inventoried. [39] The tally at the close of the 24 hours was 890 species, including 26 amphibians and reptiles, 101 birds, 18 fish, 27 fungi, 11 mammals, 410 plants, and 178 insects. [40] The tally had risen to 1,200 unique species by June 1. [41]

Natural areas

Calumet Prairie

Calumet Prairie Calumet Priarie P7150033.jpg
Calumet Prairie

Calumet Prairie is a joint venture between the National Park Service and the Indiana Department of Natural Resources. The Calumet Prairie State Nature Preserve in the northern portion of the land between Interstate 90 to the north and the Little Calumet River on the south. The National Park owns the southern half of this plot.

Cowles Bog

Cowles Bog, a National Natural Landmark, is a wetland complex containing bog, fen, marsh, swamp, wet meadow, and pond habitats; named in honor of biologist and ecologist Henry Chandler Cowles. Located south and west of Dune Acres, Indiana, Cowles Bog is the sole remnant of the "Central Dunes" where Cowles performed his pioneering field studies of ecological succession and species diversity. The complex is drained by Dunes Creek, which flows to Lake Michigan at the Indiana Dunes State Park swimming beach. A National Park trail runs from Mineral Springs Road into Cowles Bog. [42]

Great Marsh

The Great Marsh is an interdunal wetland just south of the dune ridge overlooking Lake Michigan. It stretches from steel plants in Burns Harbor, 12 miles (19 km) east to County Line Road on the edge of Michigan City. A century ago, it was the nesting and migratory layover for many birds which depended on its variety of plants. [43] In the late 19th century, the marsh was drained through a series of ditches, creating three watersheds and reducing the water table. As the water levels changed, new plants and trees moved in, creating a new habitat and displacing the wildlife that was dependent on the pre-existing wetlands. [43]

Beginning in 1998, the national lakeshore began restoration of the marsh by closing Derby Ditch and restoring 500 acres (200 ha). The work consists of: [43]

Heron Rookery

Yellow trout-lily Erythronium americanum - Heron Rookery65.jpg
Yellow trout-lily

The heron rookery is located along the East Arm Little Calumet River in the northeast corner of Porter County. The rookery is physically separated from the main part of the park. It is accessible from County Road 600 East, south of County Road 1400 North. The rookery is a hardwood forest. The great blue heron nests for which the site is named are no longer a feature of the area. Spring brings out a variety of wildflowers. [44]

Hobart Prairie Grove

Hobart Prairie Grove is an area of forested ravines along the west shore of Lake George. The Hobart Prairie Grove preserves several habitats including wetlands, prairie remnants, white oak flatlands, and a rare bur oak savanna. At about 300 acres (120 ha), the grove contains 343 native plants and a variety of birds and animals. The unique soil is at least 70 percent silt and clay with some sand. The soil supports a diversity of life. The Hobart Woodland trail is a .05-mile (0.080 km) walk to an overlook on Lake George from the Oak Savannah rail trail. The Oak Savannah rail trail runs from North Hobart Road, Hobart to South Colfax Street, Griffith. Of the trails 9-mile (14 km) length, 2 miles (3.2 km) are through the Hobart Prairie Grove. The trail follows the old Elgin, Joliet and Eastern Railroad route and connects with the Prairie Duneland rail trail, continuing east to Chesterton. [45]

Hoosier Prairie

Hoosier Prairie, a National Natural Landmark, is a 430-acre (170 ha) tallgrass prairie adjacent to Griffith, Indiana. It is a geographically isolated unit of the park, owned and maintained by the Indiana Department of Natural Resources as a state nature preserve. Some 574 species of plants have been observed growing in this patch of prairie.

Miller Woods

Miller Woods is located in Miller Beach, Indiana. It is accessed through the Paul H. Douglas Center for Environmental Education on Lake Street. The area is dominated by ridge and swale topography. the ridges or swells are beach and dune sand. They date from the post Glacial Lake Nipissing period some 3000 years before present. The swales are the depressions between the ridges. They are generally either ponds or marshes. [46]

Mnoké Prairie

Mnoké Prairie is an active prairie restoration along Beam Street in the central portion of the park. The prairie's name was suggested by Potawatomi elders; "mno" means good, "ké" means earth. It is pronounced "mno-ca" (the second syllable is like the word "cat" without the "t".) The Little Calumet River Trail provides access through the prairie. It is accessible from the Mnoké Prairie parking lot on Beam Street.

Mount Baldy

Typical wildflowers near Mount Baldy. Plants such as these help hold the dune together. INDunesFlower.JPG
Typical wildflowers near Mount Baldy. Plants such as these help hold the dune together.

Mount Baldy is a sand dune located at the east end of the park. At 123 feet (37 m) tall, it is one of the tallest sand dunes on the southern shore of Lake Michigan. It is a wandering dune that moves an average of 4 feet (1.2 m) every year, and so is called a "living dune". Mount Baldy is accessible from U.S. Route 12 (also known as Dunes Highway) between the Town of Pines and the western border of Michigan City. Visitors were formerly allowed to hike 0.7 miles (1.1 km) up the dune. As of July 2018, much of the dune itself, including the summit, was closed to allow beach grasses and other native plants to regenerate, and prevent injuries to visitors. An alternative trail leading to the beach takes visitors directly past the dune, cresting just slightly lower than the summit itself. On a clear day, there are views of Lake Michigan, Chicago's skyline, and south shore, from this point.[ citation needed ]

Pinhook Bog

Pinhook Bog, a National Natural Landmark, is a geographically isolated unit of the national park. The quaking peat bog is located near U.S. Route 421 approximately 9 miles (14 km) south of Michigan City. The bog formed from a postglacial kettle moraine left behind about 14,000 years before the present by the melting of the ice sheet during the end of the last glacial period. The acidic bog is noted for pitcher plants and other wetland species. Access to the bog is restricted to ranger-led guided tours. [47]

Historic areas

Bailly Homestead

This is the location of the pioneer trading post established in 1822 by fur trade pioneer Joseph Bailly. Bailly settled here and his last home, adapted from his 1830s retirement house, survives. [48] The Homestead was designated a U.S. National Historic Landmark in 1962.

Chellberg Farm

The real estate became the home of the Chellberg family, who built a farm on its sandy soil. As of 2008, the park maintains a heritage farm on the Chellberg land, with the Bailly family cemetery on the northern edge of the property. [49]

Bailly Cemetery

Bailly Cem Bailly plaque 2004 39.jpg

The Bailly Cemetery is located half a mile north of the homestead. Its location is a sandy bluff, which once looked out across the dunes to Lake Michigan. [50] Today, the forest covers the dunes and the lake is not visible. Numerous changes have occurred since the first burial in 1827. [51]

Joseph Bailly buried his only son by Marie in the fall of 1827 on a sandy knoll. He erected an oak cross on the site and a three-sided shelter. After 1866, the Bailly area was no longer the quiet place that it had been. Other families now lived in the area and some had been using the cemetery for their families as well. However, late in 1866, Rose Howe (granddaughter of Joseph Bailly) had the family plots fenced and requested that those other families remove their deceased to other cemeteries. In 1879, she had the entire cemetery walled in and an iron gate installed to the north. [51]

Finally in 1914, Rose Howe took one further step to protect the cemetery of her family. She had the area inside the wall filled with sand. Stone steps replaced the gate to a contemplative walk atop the cemetery. An oaken cross was raised atop this new ground, continuing the tradition started by her grandfather. Rose Howe died in 1916, while in California. She was returned to Indiana in 1917 and was the last burial in the family cemetery. [52]

Century of Progress Architectural District

The Florida Tropical House, back elevation taken from the beach Florida Tropical House back elevation.JPG
The Florida Tropical House, back elevation taken from the beach

The Century of Progress Architectural District is listed on the National Register of Historic Places and is located in the east portion of the park. The district consists of a total of five buildings, all from the Homes of Tomorrow Exhibition during the 1933 Century of Progress World's Fair which took place in Chicago. [53]

Good Fellow Club Youth Camp

Created by the Good Fellow Club of U.S. Steel in 1941, the camp served the children of Gary, until 1977. It provided outdoor recreation and a chance to leave the city behind for a week or more. [54] The camp used tent cabins with a central restroom and shower house. Atop a rise was the main lodge where meals were provided and a trading post with a bowling alley were maintained.

Lustron Homes

Lustron House on Drake Avenue Lustron Home P7150043.jpg
Lustron House on Drake Avenue

The national park acquired three Lustron houses during its land acquisition process. The Jacob Klien House was located in an endangered habitat. It was moved to the east side of Drake Avenue in Beverly Shores and placed atop a dune overlooking the lake. The Schulof house located on Lakefront Drive was transferred to the Historic Landmarks Foundation of Indiana for preservation and was moved to Stephens Street in Porter. The Powell house remains inaccessible within the park on Lakefront Drive. [55]

Swedish Farmsteads Historic District (pending)

The Swedish Farmsteads of Porter County, Indiana, are representative of the numerous rural communities settled by a significant ethnic population. They influenced the religious community and social community. Swedish immigration was at its highest from 1840 until 1920. At its height in 1910, it was estimated that 1 out of every 5 Swedes was living in the United States. [56]

Recreation

Richard Lieber (front right) with NPS Director Stephen Mather at what would become Indiana Dunes State Park in 1916 Lieber-dunes-1916.jpg
Richard Lieber (front right) with NPS Director Stephen Mather at what would become Indiana Dunes State Park in 1916

The park contains 15 miles (24 km) of beaches, as well as sand dunes, bogs, marshes, swamps, fens, prairies, rivers, oak savannas, and woodland forests. The park is also noted for its singing sands. More than 350 species of birds have been observed in the park. It has one of the most diverse plant communities of any unit in the U.S. National Park System [ citation needed ] with 1418 vascular plant species including 90 threatened or endangered ones. The Indiana Dunes area is unique in that it contains both Arctic and boreal plants (such as the bearberry) alongside desert plants (such as the prickly pear cactus).

First-time visitors to the park often go to the Dorothy Buell Memorial Visitor Center at U.S. Route 20 and Indiana Route 49, near Porter. This center offers standard visitor-center amenities, including a video, brochures, hands-on exhibits, and a gift shop. It is free to the general public. [57]

Indiana Dunes State Park Bathhouse and Pavilion - Chesterton, Indiana IndianaDunesBathHouse.jpg
Indiana Dunes State Park Bathhouse and Pavilion – Chesterton, Indiana

Camping is available at the Dunewood Campground on U.S. Route 12. The campground includes an RV dump station and two loops of trailer accessible sites (some with pull-through drives). All sites have grills, a picnic table, and access to restrooms with running water and showers. There are a limited number of walk-in sites in the Douglas Loop.

The park provides opportunities for bird watching, camping, 45 miles (72 km) of hiking, fishing, swimming, horseback riding, and cross-country skiing. Cycling is available on the Calumet Trail, a crushed limestone multiuse trail which runs through the eastern section of the park, providing access to Indiana Dunes State Park, as well as to the communities of Beverly Shores; the Town of Pines; and Mount Baldy on the edge of Michigan City, Indiana. The Great Marsh Trail opened in 2010 with an accessible, paved section usable by wheelchairs opening in fall 2012. The trail is off Broadway in the east end of the park. The park has about 2 million visits a year. Rules state not to feed any of the wildlife, including seagulls, deer, or raccoons. Collecting crinoid fossils on the beach is strictly prohibited. Possession or use of a metal detector is also prohibited – as in all national parks.

Rangers provide free walks and talks throughout the park on a regular basis. The Singing Sands, the official newspaper of the national park is published semi-annually with a listing of Ranger lead activities. [58] Events in 2013, showed that on large dunes unexpected sink holes may develop. Scientists concluded these are caused by buried trees that eventually decay causing cavities. [59]

Trails

Indiana Dunes has numerous short hike trails and a few longer distance trails:

Map of the Paul H. Douglas Trail Miller Woods Trail Map.JPG
Map of the Paul H. Douglas Trail
Indiana Dunes National Lakeshore-1.JPG
Succession Trail arriving at the beach
Contours of the Cowles Bog Trail from the trailhead to Lake Michigan. Distances shown in yards/meters. Cowles Bog Trail.PNG
Contours of the Cowles Bog Trail from the trailhead to Lake Michigan. Distances shown in yards/meters.

Burnham Plan trails

The Marquette Plan, a Lakeshore Investment Strategy for Indiana, is composed of two key elements. A 50-mile (80 km) trail is planned to cross Indiana to link Illinois, Indiana, and Michigan communities along the Lake Michigan shore. There are planned both land trails for bicycles and hikers and a blue water trail for kayakers. [62]

Water Trail

The Lake Michigan Water Trail, was designated a National Recreation Trail in 2011 and currently extends 45 miles (72 km) from Chicago's Northerly Island to Michigan City's Millennium Plaza. [63]

Long Distance Hike/Bike Trail

There will be links to major parks and a wide variety of cultural and natural sites. The 9-mile (14 km) Calumet Trail will eventually connect the eastern and western segments of Indiana Dunes National Park. The 3-mile (4.8 km) Porter Brickyard Trail opened in 2012 as part of the Burnham Plan Centennial. It will link several community hike/bike trails to the Calumet Hike/Bike trail creating a link between the Lake County communities and Michigan City. Northwestern Indiana Regional Planning Commission is guiding the work with assistance from local governments, the National Park Service, private landowners, and the American Planning Association. [62]

Lake Michigan

Chicago visible across Lake Michigan from West Beach, Indiana Dunes National Park Indiana Dunes National Lakeshore West Beach view Chicago.jpg
Chicago visible across Lake Michigan from West Beach, Indiana Dunes National Park

West Beach, located adjacent to U.S. Route 12 and County Line Road, lies on the border of Gary and Portage, Indiana. It is a geographically separated section of the park that is preserved as a piece of public beach access and an example of the same theme of plant succession as is found in Cowles Bog. This section of the park displays most of the successive stages of Indiana Dunes biotic progression, from open beach sands to mature Eastern Black Oak forest. The 0.7-mile (1.1 km) West Beach Succession Trail opened in 2007 and features different stages of plant succession in the beach and inland dunes.

The Portage Lakefront and Riverwalk was completed in 2009 as a project of the National Park Service, Northwest Indiana Regional Development Authority, and the City of Portage. The National Park Service owns the site and all facilities. The site is operated by the City of Portage through a cooperative agreement.

Porter Beach, located north of U.S. Route 12, is a small, public sand beach within Indiana Dunes National Park. The surrounding area is residential and is governed by the town of Porter.

Education

Public programs

Rail programs

Indiana Dunes National Park partners with the non-profit 501(c)(3) American Passenger Rail Heritage Foundation to provide on-board educational programs for train passengers on the South Shore Line. On select Saturdays, interpretive guides with the APRHF Rail Rangers ride roundtrip between Millennium Station and South Bend Airport station to provide narration about the park and the other sites passengers see outside their window. [65] [66] [67] [68]

Professional development

During the academic year, Indiana Dunes National Park and the Dunes Learning Center (DLC) provide professional development opportunities for teachers in the K–12 setting. Workshops feature experts in various fields of study, hands-on activities, and adventures within the national park. Illinois and Indiana teachers can receive continuing education units (CEUs) or continuing recertification units (CRUs) for each workshops. Those teachers wishing to earn graduate credit can do so through Indiana University Northwest and Chicago State University. Workshops are held at the DLC. [69]

Sister park

The park has a sister park relationship with Poland's Kampinos National Park. [70]

Accessibility

The park can be accessed by car from U.S. Route 12. Access by rail is provided by the South Shore Line at Dune Park station. [71]

Indiana Dunes is working to provide access to beach areas. Access to the waters of Lake Michigan is a challenging problem. Presently, two beach access areas are considered accessible: West Beach, Portage Lakefront and Riverwalk, [72]

Accessible parking and restroom services are available throughout the park. A standard wheelchair is available for loan at the Paul H. Douglas Center. [72]

Facilities

Dunes National Park Association

In 2012, the Dunes National Park Association (DNPA) was established as a nonprofit organization dedicated to supporting the Indiana Dunes National Lakeshore. The DNPA is endorsed by the Indiana Dunes National Lakeshore. The primary purpose of the DNPA is to solicit funds for the direct benefit or support of the lakeshore and related activities, advocate on behalf of the park and educate the community on the abundant resources available in the national park. [80]

See also

Geological forms (North to South)

People associated with the Dunes

Related Research Articles

<span class="mw-page-title-main">Porter County, Indiana</span> County in Indiana, United States

Porter County is a county in the U.S. state of Indiana. As of 2020, the population was 173,215, making it the 10th most populous county in Indiana. The county seat is Valparaiso. The county is part of Northwest Indiana, as well as the Chicago metropolitan area. Porter County is the site of much of the Indiana Dunes, an area of ecological significance. The Hour Glass Museum in Ogden Dunes documents the region's ecological significance.

<span class="mw-page-title-main">Pictured Rocks National Lakeshore</span> U.S. National Lakeshore on Lake Superior

Pictured Rocks National Lakeshore is a U.S. National Lakeshore in the Upper Peninsula of Michigan, United States. It extends for 42 mi (68 km) along the shore of Lake Superior and covers 73,236 acres. The park has extensive views of the hilly shoreline between Munising and Grand Marais in Alger County, with picturesque rock formations, waterfalls, and sand dunes.

<span class="mw-page-title-main">Indiana Dunes State Park</span> State park in Indiana, United States

Indiana Dunes State Park is an Indiana State Park located in Porter County, Indiana, United States, 47 miles (75.6 km) east of Chicago. The park is bounded by Lake Michigan to the northwest and is surrounded by as well as within the authorized boundaries of Indiana Dunes National Park, a unit of the National Park Service; the NPS owns the water from the ordinary high water mark to 300 feet (91 m) offshore. The 1,530-acre (619.2 ha) Dunes Nature Preserve makes up the bulk of eastern part of the park, and includes most of the park's hiking trails and dune landscape. This was one of the first places Richard Lieber considered when establishing the Indiana State Park system. Like all Indiana state parks, there is a fee for entrance. Indiana Dunes State Park was established in 1925 and designated a National Natural Landmark in 1974.

Northwest Indiana, nicknamed The Region after the Calumet Region, comprises Lake, Porter, LaPorte, and Newton counties in Indiana. This region neighbors Lake Michigan and is part of the Chicago metropolitan area. According to the 2020 Census, Northwest Indiana has a population of 831,080 and is the state's second largest urban area after the Indianapolis Metropolitan Area. It is also the home of the Indiana Dunes, parts of which have been preserved through conservation efforts. The town of Ogden Dunes houses the Hour Glass, a museum showcasing the ecological and conservation efforts of O. D. Frank.

<span class="mw-page-title-main">Lake Chicago</span> Prehistoric lake from the Wisconsin Glacial Period

Lake Chicago was a prehistoric proglacial lake that is the ancestor of what is now known as Lake Michigan, one of North America's five Great Lakes. Formed about 13,000 years ago and fed by retreating glaciers, it drained south through the Chicago Outlet River.

<span class="mw-page-title-main">Cowles Bog</span> Wetland complex in Indiana, US

Cowles Bog is a 4,000-year-old wetland complex in Indiana Dunes National Park, near Chesterton, Indiana. It is named for Henry Chandler Cowles who did his pioneering work in ecology and ecological succession here. His work brought international attention to the area which led to efforts to preserve the Indiana Dunes. It was designated a National Natural Landmark in 1965. It contains bog, fen, marsh, wet meadow, swamp, and pond habitats.

<span class="mw-page-title-main">Calumet Trail</span> Trail in Indiana, United States

The Calumet Trail is an east-west bicycle and multiuse recreational trail in the Calumet region of northwestern Indiana, United States. It runs roughly parallel to U.S. Route 12 and the right-of-way of the South Shore line, along the NIPSCO easement.

<span class="mw-page-title-main">Westchester Township, Porter County, Indiana</span> Township in Indiana, United States

Westchester Township is one of twelve townships in Porter County, Indiana. It is included in the Calumet, Northwest Indiana, and Great Lakes regions. It is located on the southern shore of Lake Michigan, about 50 miles (80 km) southeast of Chicago. It stretches from the famous Indiana Dunes on its northern border, south to the Valparaiso Moraine, a ridge of rolling hills left by the last glacier to pass through the area. As of the 2010 census, its population was 19,396.

<span class="mw-page-title-main">Kankakee Outwash Plain</span>

The Kankakee Outwash Plain is a flat plain interspersed with sand dunes in the Kankakee River valley in northwestern Indiana and northeastern Illinois of the United States. It is just south of the Valparaiso Moraine and was formed during the Wisconsin Glaciation. As the glacier stopped at the Valparaiso Moraine, its meltwater was carried away to the outwash plain. On the south side of the moraine, where the elevation drops, the meltwaters eroded away valleys, carrying sand and mud with them. As the muddy meltwater reached the valley where the slope lessened, the water slowed, depositing the sand on the outwash plain. This created a smooth, flat, and sandy plain. Before its draining, the Kankakee Marsh, located on the outwash plain, was one of the largest freshwater marshes in the United States.

<span class="mw-page-title-main">Miller Beach</span> Neighborhood in Lake County, Indiana, United States

Miller Beach is a neighborhood of Gary, Indiana on the southernmost shore of Lake Michigan. First settled in 1851, Miller Beach was originally an independent town. However, the "Town of Miller" was eventually annexed by the then flourishing city of Gary in 1918. Located in the northeastern corner of Lake County, Indiana, the former town is now known as "The Miller Beach Community." Miller Beach borders Lake Michigan to the north, Porter County to the east, and is largely surrounded by protected lands, including Indiana Dunes National Park. Miller Beach is also the closest beach/resort community to Chicago, and has been a popular vacation spot since the early 20th century. As of the 2000 US census, it had a population of 9,900.

<span class="mw-page-title-main">Calumet Shoreline</span>

The Calumet Shoreline is an ancient shoreline of Lake Michigan located in the Lake Michigan Basin. It can be clearly seen as a sand ridge along Ridge Road south of Chicago. Closer to the lake from the Calumet Shoreline, there are the Tolleston shorelines and farther from the lake are the Glenwood Shoreline, the Tinley Moraine, and the Valparaiso Moraine. The shoreline is named after the Calumet Region of Northern Indiana.

<span class="mw-page-title-main">Glenwood Shoreline</span>

The Glenwood Shoreline is an ancient shoreline of the precursor to Lake Michigan, Lake Chicago. It is named after the town of Glenwood, Illinois. The shoreline was formed when the lake was higher during the last ice age, while ice blocked the Straits of Mackinac. After the straits were freed, the lake receded and left behind a sand ridge at an elevation of about 640 feet (200 m) where the shore resided. This ridge can be seen clearly in Glenwood, Illinois, Dyer, Indiana, and Schererville, Indiana, all south of Chicago.

<span class="mw-page-title-main">Tremont, Indiana</span> Ghost town in Indiana, United States

Tremont, Indiana, is a ghost town formerly located in what is now the Indiana Dunes State Park and Indiana Dunes National Park in Westchester Township in northern Porter County, Indiana. It was first established in 1833. It was located at the intersection of U.S. Highway 12 and County Road 100 East, near Indiana 49. The community is named for three massive sand dunes that are now contained within the State park. They are Mount Tom, Mount Holden 170 feet (52 m), and Mount Green 160 feet (49 m).

The Indiana Dunes are natural sand dunes occurring at the southern end of Lake Michigan in the American State of Indiana. They are known for their ecological significance. Many conservationists have played a role in preserving parts of the Indiana Dunes. The Hour Glass, a museum in Ogden Dunes, showcases some of the ecological import of the Dunes.

<span class="mw-page-title-main">Habitats of the Indiana Dunes</span> Set of habitats in the United States

The Indiana Dunes comprise ten different habitats. Each provides for a unique combination of plants and animals. The range of the Indiana Dunes varies depending your source. The Indiana Lake Michigan Coastal Program uses the river drainage systems along the shoreline. This expands the area from the areas of lakeshore southward to the edges of the Valparaiso Moraine. This entire region has been dune landscapes since over 114,000 years before present (YBP). Traditionally, the Indiana Dunes area thought of as a narrow area along the shores of Lake Michigan, including the areas of Marquette Park in Gary, Indiana (1920), Indiana Dunes State Park (1926) and Indiana Dunes National Park,. The identified ten habitats can be found in these parks, where they have been preserved, but are also visible throughout the three counties of Northwest Indiana.

<span class="mw-page-title-main">East Arm Little Calumet River</span> River in Indiana, United States

The East Arm Little Calumet River, also known as the Little Calumet River East Branch, is a 22.1-mile-long (35.6 km) portion of the Little Calumet River that begins just east of Holmesville, Indiana in New Durham Township in LaPorte County and flows west to Porter County and the Port of Indiana-Burns Waterway.

<span class="mw-page-title-main">Salt Creek (Little Calumet River tributary)</span> River in Indiana, United States

Salt Creek is a 24.0-mile-long (38.6 km) tributary of the East Arm Little Calumet River that begins south of Valparaiso in Porter County, Indiana and flows north until it joins the East Arm Little Calumet River just before it exits to Lake Michigan via the Port of Indiana-Burns Waterway.

The Toleston Shoreline is the third ancient shoreline of the precursor to Lake Michigan, Lake Chicago. It takes its name from the village of Tolleston, now a portion of Gary, Indiana. The shoreline formed when Lake Chicago was high enough to drain through the Chicago outlet into the Des Plaines River. The beach is 18 to 25 feet above the level of Lake Michigan. The Indiana segment and the Illinois segment, north to Evanston are still visible. North of Evanston and Michigan City, Indiana, the beach has been eroded by later ice movement or shoreline wave action.

<span class="mw-page-title-main">Dunes Creek</span> River in Indiana, United States

Dunes Creek is a northwards-flowing 4.3-mile-long (6.9 km) stream which drains the Great Marsh of Indiana Dunes State Park and Indiana Dunes National Park in Porter County, Indiana, United States. Dunes Creek passes through the coastal sand dunes to empty into Lake Michigan.

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Further reading