In the modern world, Congewai Creek has caught the attention of millions of people around the world. Whether due to its impact on society, its relevance in the political sphere, its influence on popular culture, or its meaning in history, Congewai Creek has become a topic of constant interest and debate. From its origins to its current evolution, Congewai Creek has marked a before and after in the way we live, think and relate to the world around us. In this article, we will explore different aspects of Congewai Creek, from its origins to its impact on everyday life, seeking to understand its true meaning and relevance in our society.
Congewai Creek North Arm of Wollombi Brook, Coongewai Creek, Coongeewa Creek[1] | |
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![]() View down Congewai Creek valley | |
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Location | |
Country | Australia |
State | New South Wales |
Region | Sydney Basin (IBRA), Upper Hunter |
Local government area | Cessnock |
Physical characteristics | |
Source | Myall Range |
• location | Watagans National Park |
• elevation | 199 m (653 ft) |
Mouth | confluence with Wollombi Brook |
• location | near Wollombi |
• elevation | 93 m (305 ft) |
Length | 45 km (28 mi) |
Basin features | |
River system | Hunter River catchment |
National park | Watagans NP |
[1][2] |
Congewai Creek, a watercourse of the Hunter River catchment, is located in the Hunter district of New South Wales, Australia.
The Congewai Creek rises below Myall Range, about 3 kilometres (1.9 mi) southeast of Quorrobolong trig station within the Watagans National Park. The river flows generally west by south, then north by west, then northwest by north, then west by north, then west southwest, and then south,[1] joined by four tributaries including the Cedar Creek, before reaching its confluence with the Wollombi Brook near Wollombi. The river descends 106 metres (348 ft) over its 45 kilometres (28 mi) course.[2]
32°52′S 151°12′E / 32.867°S 151.200°E