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Ku-Ring-Gai Chase is a suburb of Sydney, New South Wales, Australia approximately located 25 kilometers north of the Sydney central business district, located 51 km north to Sydney International Airport.

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Ku-ring-gai Chase National Park is a national park on the northern side of Sydney in New South Wales, Australia. The 14,977-hectare (37,010-acre) park is 25 kilometres (16 mi) north of the Sydney central business district and generally comprises the land east of the M1 Pacific Motorway, south of the Hawkesbury River, west of Pittwater and north of Mona Vale Road. It includes Barrenjoey Headland on the eastern side of Pittwater.

Ku-ring-gai Chase is a popular tourist destination, known for its scenic setting on the Hawkesbury River and Pittwater, significant plant and animal communities, Aboriginal sites and European historic places. Picnic, boating, and fishing facilities can be found throughout the park. There are many walking tracks in Ku-ring-gai Chase. The villages of Cottage Point, Appletree Bay, Elvina Bay, Lovett Bay, Coasters Retreat, Great Mackerel Beach and Bobbin Head are located within the park boundaries.

The park was declared in 1894, and is the third oldest national park in Australia. The park is managed by the NSW National Parks & Wildlife Service and was added to the Australian National Heritage List in December 2006.

The park gets its name from the Guringai Aboriginal people who were long thought to be the traditional owners of the area. However, more contemporary research suggests that this was not the case.

Ku-ring-gai Chase is part of the Hornsby Plateau, a massive block of sandstone tilting upwards to the north. The park comprises a plateau with an elevation of generally 150–200 m above sea level. The plateau is divided into separate sections by the steep valleys of Cowan Creek, Coal and Candle Creek, and Smiths Creek. These “flooded” or “drowned” valleys, knowns as rias, were eroded into the sandstone much deeper than the current sea level during the glacial phases of the Pleistocene ice age. When the ice caps melted about 10,000 years ago, the sea levels rose and flooded the valleys of the park.

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