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The Lane Cove National Park is a protected national park that is located within metropolitan Sydney, in New South Wales, Australia.The 670-hectare (1,700-acre) national park is situated about 10 kilometres (6.2 mi) north-west of the Sydney central business district and features various vegetation types, such as, wet and dry sclerophyll forest, heathland, mangroves and tidal flats.
Location of Davis County in Utah. This is a list of the National Register of Historic Places listings in Davis County, Utah. This is intended to be a complete list of the properties and districts on the National Register of Historic Places in Davis County, Utah, United States. Latitude and longitude coordinates are provided for many National ...
Listings for Salt Lake City can be found here. This is intended to be a complete list of the properties and districts on the National Register of Historic Places in Salt Lake County, Utah, United States. Latitude and longitude coordinates are provided for many National Register properties and districts; these locations may be seen together in a ...
The area surrounding the river, no more than 1 kilometre (0.62 mi) wide, is called Lane Cove National Park, and is a site of ecological importance, listed on the Australian Register of the National Estate. It contains an endangered community of fungi, some species of which have still not been classified.
Commandment Rock is a large rock located in the Lane Cove National Park, Sydney, New South Wales, Australia. The site is home to rock engravings, both Aboriginal and European. An engraving of the Fifth Commandment on the rock gives it its name. It is reputed to have been carved in the late 19th century by a nearby resident, Thomas Tunbridge, as ...
(1994) "Duchesne County" article in the Utah History Encyclopedia. The article was written by Craig Fuller and the Encyclopedia was published by the University of Utah Press. ISBN 9780874804256. Archived from the original on February 7, 2024, and retrieved on April 18, 2024.
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Lake Bonneville was the largest Late Pleistocene paleolake in the Great Basin of western North America. It was a pluvial lake that formed in response to an increase in precipitation and a decrease in evaporation as a result of cooler temperatures.