Question: what is the 3112 acre Pennsylvania state park that took over 11,000 to make due to the wave action of lake Erie called?

full_context: Document 1: Presque Isle State Park: Presque Isle State Park is a 3112 acre Pennsylvania state park on an arching, sandy peninsula that juts into Lake Erie, 4 mi west of the city of Erie, in Millcreek Township, Erie County, Pennsylvania, in the United States. The peninsula sweeps northeastward, surrounding Presque Isle Bay along the park's southern coast. It has 13 mi of roads, 21 mi of recreational trails, 13 beaches for swimming, and a marina. Popular activities at the park include swimming, boating, hiking, biking, and birdwatching.
Document 2: Kelleys Island State Park: Kelleys Island State Park is a 676 acre Ohio, United States, state park established in 1956 that makes up almost all of the northern third of Kelleys Island in Lake Erie. The park offers 6 mi of hiking, ruins of lime kilns and quarrying operations, a sand beach and a campground. The park cooperates with other agencies to manage the adjoining Glacial Grooves State Memorial, a set of rare glacial grooves, North Shore Alvar State Natural Area, a rare alvar habitat, and the North Pond Nature Preserve, a lake embayment usually separated from the lake by a sand bar.
Document 3: History of Presque Isle: The History of Presque Isle Pennsylvania began when Presque Isle was created by the wave action of Lake Erie over the course of the 11,000 years that have passed since the last ice age.
Document 4: Erie Bluffs State Park: Erie Bluffs State Park is a 587 acre Pennsylvania state park in Girard and Springfield Townships, Erie County, Pennsylvania in the United States. The park is the largest undeveloped stretch of land overlooking Lake Erie in Pennsylvania. Erie Bluffs State Park is just north of Pennsylvania Route 5 near Lake City and 12 mi west of Erie. It is one of Pennsylvania's newest state parks.
Document 5: Indigenous people of the Everglades region: The indigenous people of the Everglades region arrived in the Florida peninsula of what is now the United States approximately 14,000 to 15,000 years ago, probably following large game. The Paleo-Indians found an arid landscape that supported plants and animals adapted to prairie and xeric scrub conditions. Large animals became extinct in Florida around 11,000 years ago. Climate changes 6,500 years ago brought a wetter landscape. The Paleo-Indians slowly adapted to the new conditions. Archaeologists call the cultures that resulted from the adaptations Archaic peoples. They were better suited for environmental changes than their ancestors, and created many tools with the resources they had. Approximately 5,000 years ago, the climate shifted again to cause the regular flooding from Lake Okeechobee that gave rise to the Everglades ecosystems.
Document 6: Lake Connecticut: Glacial Lake Connecticut formed over what is now Long Island Sound and coastal Connecticut at the fore edge of the ice sheet of the Wisconsin glaciation, as the lobe of the Laurentide ice sheet began to retreat, some 18 to 20,000 years before present. It was dammed by the terminal moraine that now forms the spine of Long Island and Fishers Island. About 15,000 BP, the moraine dam that impounded Lake Connecticut failed; the outlet, known as The Race for its tidal rip currents, lies between the North Fork of Long Island and Fishers Island. For a time, much of the lake bed was exposed to wind-driven erosion: the cue is found in soundings that reveal regional unconformities in the sediment bed of Long Island Sound.
Document 7: Allegheny Islands State Park: Allegheny Islands State Park is a 43 acre Pennsylvania state park in Harmar Township, Allegheny County, Pennsylvania in the United States. The undeveloped park is composed of three alluvial islands located in the middle of the Allegheny River northeast of Pittsburgh. The islands are just north of the boroughs of Oakmont and Plum, and southwest of Cheswick. Bridges for the Pennsylvania Turnpike (Interstate 76) and the Bessemer and Lake Erie Railroad Branch of the Canadian National Railway cross the Allegheny River at the middle island.
Document 8: Presque Isle Bay: Presque Isle Bay is a natural bay located off the coast of Erie, Pennsylvania, United States. Its 5.8 sqmi embayment is about 4.6 mi in length, about 1.8 mi across at its widest point, and an average depth of about 20 ft . The bay is at an elevation of 571 ft (174 m) above sea level. It is bounded on the north and west by a recurved peninsula that makes up Presque Isle State Park. On the south, the bay is edged by the urban Erie shoreline, which hosts the Port of Erie Marine Terminal, as well as an assortment of parks, tourist attractions and marinas such as the Erie Yacht Club. Fishing, water skiing, swimming, and boating, are a few examples of common activities among visitors who come to appreciate this natural bay for its sheltered waters and captivating views of Erie’s historic neighborhoods and landmarks. A small channel on the east provides a shipping lane into and out of Lake Erie. Cascade Creek, Garrison Run, Mill Creek, and surface runoff drain the lands of the Presque Isle Bay Watershed into the bay.
Document 9: USRC Erie: The USRC "Erie" was a United States Revenue Cutter stationed at Presque Isle in Erie, Pennsylvania. It replaced the USRC "Benjamin Rush" on the Great Lakes. Daniel Dobbins supervised the construction of and was in command of the USRC "Erie" from 1833 to 1841. Dobbins was placed back in command of the USRC "Erie" in 1845. USRC "Erie" was active in the prevention of the violation of United States neutrality during the Canadian Rebellions of 1837 and was placed under the control of the United States War Department in April 1839.
Document 10: Lake Wayne: Lake Wayne formed in the Lake Erie and Lake St. Clair basins around 12,500 years before present (YBP) when Lake Arkona dropped in eleveation. About 20 ft below the Lake Warren beaches it was early described as a lower Lake Warren level. Based on work in Wayne County, near the village of Wayne evidence was found that Lake Wayne succeeded Lake Whittlesey and preceded Lake Warren. From the Saginaw Basin the lake did not discharge water through Grand River but eastward along the edge of the ice sheet to Syracuse, New York, thence into the Mohawk valley. This shift in outlets warranted a separate from Lake Warren. The Wayne beach lies but a short distance inside the limits of the Warren beach. Its character is not greatly different when taken throughout its length in Michigan, Ohio, Pennsylvania and New York. At the type locality in Wayne County, Michigan, it is a sandy ridge, but farther north, and to the east through Ohio it is gravel. The results of the isostatic rebound area similar to the Lake Warren beaches.
Document 11: Point Pelee National Park: Point Pelee National Park ( ; French "Parc national de la Pointe-Pelée") is a national park in Essex County in southwestern Ontario, Canada where it extends into Lake Erie. The word "pelée" is French for 'bald'. Point Pelee consists of a peninsula of land, mainly of marsh and woodland habitats, that tapers to a sharp point as it extends into Lake Erie. Middle Island, also part of Point Pelee National Park, was acquired in 2000 and is just north of the Canada–United States border in Lake Erie. Point Pelee is the southernmost point of mainland Canada, and is located on a foundation of glacial sand, silt and gravel that bites into Lake Erie. This spit of land is slightly more than seven kilometres long by 4.5 km wide at its northern base. Established in 1918, Point Pelee was the first national park in Canada to be established for conservation. It was designated as a Ramsar site on 27 May 1987.
Document 12: History of the Duwamish tribe: The region now known as Seattle has been inhabited since the end of the last glacial period (c. 8,000 BCE.: 10,000 years ago). Archaeological excavations at West Point in Discovery Park, Magnolia confirm that the Seattle area has been inhabited by humans for at least 4,000 years and probably much longer. West Point was called "Oka-dz-elt-cu", "Per-co-dus-chule", or "Pka-dzEltcu". The village of "tohl-AHL-too" ("herring house") had been inhabited at least since the 6th century CE, as had "hah-AH-poos"—"where there are horse clams"—at the then-mouth of the Duwamish River in what is now the Industrial District. The Lushootseed (Skagit-Nisqually)-speaking Salish "Dkh'Duw'Absh" ("People of the Inside") and "Xacuabš" ("People of the Large Lake")—ancestors of today's Duwamish Tribe—occupied at least 17 villages in the mid-1850s and lived in some 93 permanent longhouses ("khwaac'ál'al") along the lower Duwamish River, Elliott Bay, Salmon Bay, Portage Bay, Lake Washington, Lake Sammamish, and the Duwamish River tributaries, the Black and Cedar Rivers.
Document 13: Pymatuning State Park (Pennsylvania): Pymatuning State Park is a Pennsylvania state park covering 21122 acre in Conneaut, North Shenango, Pine, Sadsbury, South Shenango, West Fallowfield and West Shenango Townships, Crawford County, Pennsylvania, in the United States. Pymatuning State Park is the largest state park in Pennsylvania and contains the 17088 acre of Pymatuning Lake, three-quarters of which is in Pennsylvania and one-quarter of which is in Ohio. A three-mile (5 km) causeway extends between Pennsylvania and Ohio near the center of the lake. The lake provides fishing and boating year round. There are two natural areas, Clark Island (161 acre ) and Blackjack (725 acre ) in the park. The park is also home to the University of Pittsburgh's Pymatuning Laboratory of Ecology. Like all Pennsylvania state parks, admission to the Pymatuning State Park is free. The northern access for Pymatuning State Park can be reached from U.S. Route 6 and the southern access is reached from U.S. Route 322.
Document 14: Lake Hitchcock: Lake Hitchcock was a glacial lake that formed approximately 15,000 years ago in the late Pleistocene epoch. After the Laurentide ice sheet retreated, glacial ice melt accumulated at the terminal moraine and blocked up the Connecticut River, creating the long, narrow lake. The lake existed for approximately 3,000 years, after which a combination of erosion and continuing geological changes likely caused it to drain. At its longest, Lake Hitchcock stretched from the moraine dam at present-day Rocky Hill, Connecticut, to St. Johnsbury, Vermont (about 320 km ). Although the rift valley through which the river flows above Rocky Hill actually continues south to New Haven, on Long Island Sound, the obstructing moraine at Rocky Hill diverted the river southeast to its present mouth at Old Saybrook.
Document 15: Lake Erie Metropark: Lake Erie Metropark is a park in the Huron-Clinton system of metro parks. The park is a 1607 acre recreational facility located at the mouth of the Huron River on Lake Erie and consists of meadows, a marsh and lagoons. It has a three-mile (5 km) shoreline along the lake and is a popular bird-watching site. The Park has a wave action swimming pool, an 18-hole regulation golf course, the Marshlands Museum and Nature Center, boat launches and a marina. The children's play area, previously featuring a child-size town, is now under construction as a newer, more modern, playscape area is being built.
ground_truth: Presque Isle