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Organ Pipes National Park

Organ Pipes National Park
Victoria
Organ Pipes Geological Feature Melbourne Australia.JPG
Organ Pipes geological feature.
Organ Pipes National Park is located in Victoria
Organ Pipes National Park
Organ Pipes National Park
Nearest town or city Melbourne
Coordinates 37°40′07″S 144°46′02″E / 37.66861°S 144.76722°E / -37.66861; 144.76722Coordinates: 37°40′07″S 144°46′02″E / 37.66861°S 144.76722°E / -37.66861; 144.76722
Established 12 March 1972 (1972-03-12)
Area 1.21 km2 (0.5 sq mi)
Visitation 50,000 (in 1996–7)
Managing authorities Parks Victoria
Website Organ Pipes National Park
See also Protected areas of Victoria

The Organ Pipes National Park, abbreviated as OPNP, is a national park located in the Central region of Victoria, Australia. The 121-hectare (300-acre) protected area was established with the focus on conservation of the native flora and fauna, and preservation of the geological features in the Jacksons Creek, a part of the Maribyrnong valley, north-west of Melbourne. It is situated in a deep gorge in the grassy, basalt Keilor plains.

Within Organ Pipes National Park, the valley walls of Jacksons Creek expose Pleistocene volcanic rocks of the New Volcanic Group. These 2.5 to 2.8 million year-old basalt lavas, commonly known as "trap rock," fractured during cooling into vertically standing, hexagonal basalt columns. These columns are locally known as the "organ pipes" for which this park is named. Over the last one to two million years, the slow cutting by Jackson Creek of its valley down into the basaltic plains and through the underlying trap rock exposed these geological structures. The bottom of the valley of Jackson Creek also exposes a prehistoric buried creek valley, which is cut into 400 million year-old (Silurian) mudstones and sandstones. The bottom of this buried valley contains ancient creek gravel. Both the ancient river valley and the Silurian sedimentary rock lies buried beneath the basaltic volcanic rocks of the New Volcanic Group. Marine fossils that are found in the Silurian sedimentary rocks demonstrate that they accumulated beneath a prehistoric ocean.


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