In this article we are going to delve into the exciting world of Tidbinbilla River, a topic that has captured the attention of millions of people around the world. From its origins to its impact on today's society, Tidbinbilla River has been the subject of debate, analysis and reflection. Throughout the next few lines, we will explore its multiple facets, unraveling its mysteries and discovering its possible implications in different areas. Whatever your interest in Tidbinbilla River, we are sure that this article will provide you with rich insight and new perspectives on this fascinating topic.
| Tidbinbilla | |
|---|---|
| Location | |
| Country | Australia |
| Territory | Australian Capital Territory |
| Region | South Eastern Highlands (IBRA), Capital Country |
| Physical characteristics | |
| Source | Brindabella Ranges |
| • location | Billy Billy Rocks in Tidbinbilla Nature Reserve |
| • coordinates | 35°26′35″S 148°55′31″E / 35.44306°S 148.92528°E |
| • elevation | 1,330 m (4,360 ft) |
| Mouth | confluence with Paddys River |
• coordinates | 35°25′28″S 148°57′31″E / 35.42444°S 148.95861°E |
• elevation | 618 m (2,028 ft) |
| Length | 13 km (8.1 mi) |
| Basin features | |
| River system | Murrumbidgee catchment, Murray–Darling basin |
| National park | Namadgi NP |
| [1] | |
The Tidbinbilla River is a perennial stream that is part of the Murrumbidgee catchment within the Murray–Darling basin, and is located in the Australian Capital Territory, Australia.
Tidbinbilla River rises on the eastern slopes of the Brindabella Ranges in the south-west of the Australian Capital Territory (ACT), below Billy Billy Rocks in Tidbinbilla Nature Reserve, within Namadgi National Park. The creek flows generally north-east before reaching its confluence with Paddys River, south-west of Tuggeranong Town Centre. The creek descends 708 metres (2,323 ft) over its 13-kilometre (8.1 mi) course.[1]
In the years after the 2003 Canberra Bushfires, an existing weir on the river has been used to maintain large downstream ponds as part of conservation efforts.[2]
In 2012, heavy downpours caused damage to the existing river system with erosion damaging the river's ability to hold water. In coordination with local landowners and stakeholders, the Mulloon Institute is currently undertaking rehydration works in order to primarily reduce erosion amongst other benefits.[3][4]