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・ Flint Indians
・ Flinders Island (disambiguation)
・ Flinders Island (Queensland)
・ Flinders Island (South Australia)
・ Flinders Island Airport
・ Flinders Island Chronicle
・ Flinders Island spotted fever
・ Flinders Lane, Melbourne
・ Flinders Medical Centre
・ Flinders Park, South Australia
・ Flinders Peak
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・ Flinders Ranges
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Flinders Ranges National Park
・ Flinders Ranges Way
・ Flinders Ranges worm-lizard
・ Flinders Reef
・ Flinders River
・ Flinders Street
・ Flinders Street railway station
・ Flinders Street Viaduct
・ Flinders Street, Adelaide
・ Flinders Street, Melbourne
・ Flinders University
・ Flinders University Art Museum
・ Flinders University Hall
・ Flinders university hockey club
・ Flinders View, Queensland


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Flinders Ranges National Park : ウィキペディア英語版
Flinders Ranges National Park

The Flinders Ranges National Park is situated approximately 400 km north of Adelaide in the northern central part of South Australia's largest mountain range, the Flinders Ranges. The park covers an area of 912 km², northeast of the small town of Hawker. The Heysen Trail and Mawson Trails pass through the park.
The park's most characteristic landmark is Wilpena Pound, a large, sickle-shaped, natural amphitheatre covering nearly 80 km², containing the range's highest peak, St Mary Peak (1,170 metres).
The park centre at Wilpena Pound is accessible by sealed road from Hawker. Other areas in the park can be reached by un-sealed roads, which are mostly accessible by two-wheel drive vehicles except in bad weather or after heavy rain. There are many lookouts, scenic vistas, small canyons and unusual rock formations located in the park. These include Wilpena Pound, Wilkawillina Gorge, Hucks Lookout, Brachina Gorge, Bunyeroo Gorge and Arkaroo Rock. The park has some stone ruins from early European settlement and Aboriginal rock art sites. An amazing rock formation called the Great Wall of China is located just outside the park. Camping is permitted at many locations in the park.〔
==Geology==
The Flinders Ranges are largely composed of folded and faulted sediments of the Adelaide Geosyncline. This very thick sequence of sediments were deposited in a large basin during the Neoproterozoic on the passive margin of the ancient continent of Rodinia. During the Cambrian, approximately 540 million years ago, the area underwent the Delamerian orogeny where the geosynclinal sequence was folded and faulted into a large mountain range. Since this time the area has undergone erosion resulting in the relatively low ranges today.
Most of the high ground and ridgetops in the Flinders are sequences of quartzites that outcrop along strike. The high walls of Wilpena Pound are formed by the outcropping beds of the eponymous Pound Quartzite in a synclinal structure. The same formation forms many of the other high parts of the Flinders, including the high plateau of the Gammon Ranges and the Heysen Range. Cuesta forms are also very common in the Flinders.

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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