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The Stone Forest or Shilin (Chinese: 石 林; pinyin: Shílín) is a notable set of limestone formations about 500 km 2 located in Shilin Yi Autonomous County, Yunnan Province, People's Republic of China, near Shilin approximately 90 km (56 mi) from the provincial capital Kunming.
The original source for lithographic limestone was the Solnhofen Limestone, named after the quarries of Solnhofen where it was first found. This is a late Jurassic deposit, part of a deposit of plattenkalk (a very fine-grained limestone that splits into thin plates, usually micrite) that extends through the Swabian Alb and Franconian Alb in Southern Germany. [5]
The Gardens of Stone National Park is a protected national park that is located in the Central Tablelands region of New South Wales in eastern Australia. The 15,080-hectare (37,300-acre) national park is situated 125 kilometres (78 mi) northwest of Sydney , and 30 kilometres (19 mi) northwest of Lithgow .
In John Cary's New and Correct English Atlas published in 1793 The Great Stone of Four Stones is shown on the map [5] In 1822 Joseph Ashton of Manchester wrote The Lancashire Gazette The Second Edition in it The Great Stone of Four Stones is listed as being "a boundary stone between the counties of York and Lancaster. 2 miles S. of Bentham." [6]
The forest property types are defined as follows according to 3 of the Federal Forest Act (BWaldG): [8] State forest: forest in sole ownership of the federal government, a state or an institution or a foundation under public law as well as forest in co-ownership of a country, insofar as it is regarded as state forest according to state regulations.
Pobiti Kamani occupies an area 8 km (5.0 mi) long and 3 km (1.9 mi) wide, running from north to south. There are seven groups of stone pillars. For example, "Dikilitash", the main group, includes over 350 stones. "Strashimirovo" features four rows of stones that are distinctive for their "bulging" middle segments. [4]
Tamala Limestone of the Henderson Cliffs in Beeliar Regional Park. Tamala Limestone is the geological name given to the widely occurring eolianite limestone deposits on the western coastline of Western Australia, between Shark Bay in the north and nearly to Albany in the south.
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