Today, Bettowynd Creek is a topic that generates great interest and debate in society. For decades now, Bettowynd Creek has been a constant topic of conversation, capturing the attention of people of all ages and interests. Whether due to its impact on our daily lives, in politics, in science or in popular culture, Bettowynd Creek has managed to position itself as a relevant element in people's lives. In this article, we will explore different aspects of Bettowynd Creek, from its history to its impact on the world today, in order to understand its importance and the role it plays in our lives.
Bettowynd Creek | |
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Etymology | Aboriginal: a place where water lilies abound[1] |
Location | |
Country | Australia |
State | New South Wales |
Region | South East Corner (IBRA), Southern Tablelands |
Local government area | Queanbeyan–Palerang |
Physical characteristics | |
Source | below Benmanang Range, Great Dividing Range |
• location | near Majors Creek |
• elevation | 430 m (1,410 ft) |
Mouth | confluence with the Deua River |
• location | south of Monga National Park |
• elevation | 104 m (341 ft) |
Length | 16 km (9.9 mi) |
Basin features | |
River system | Moruya River catchment |
National park | Monga NP |
[2][3] |
Bettowynd Creek, a partly perennial stream of the Moruya River catchment, is located in the Southern Tablelands and South Coast regions of New South Wales, Australia.
Bettowynd Creek rises below Benmanang Range, about 14 kilometres (8.7 mi) south southwest of the village of Majors Creek, on the eastern slopes of the Great Dividing Range. The river flows generally northeast and then southeast before reaching its confluence with the Deua River in remote country south of the Monga National Park.[2] The river descends 311 metres (1,020 ft) over its 16 kilometres (9.9 mi) course.[3]
35°42′S 149°48′E / 35.700°S 149.800°E