Commune with nature and explore Burnt-Down Scrub Nature Reserve located 4.7 mi (7.5 km) from central Coombadjha. If you like Burnt-Down Scrub Nature Reserve, you'll love Washpool National Park, just a short drive away.
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Frequently asked questions
Can I book refundable accommodations in Coombadjha?
If you need the flexibility to change your plans to Coombadjha, most hotels provide refundable* rates you can book. You can find these properties by searching our site and using the "fully refundable" filter to narrow down the results.
What will the weather in Coombadjha be like during my visit?
January and December are typically the warmest months in Coombadjha when the average temp is 72°F. July and August are the coldest months when the average temperature is 56°F. March and February are the months with the most rain.
Why should I book my Coombadjha accommodation with Hotels.com?
There are lots of reasons to book your Coombadjha trip with us: our free cancellations on selected hotels gives you flexibility, and with One Key™, our rewards program, you will be able to earn and use OneKeyCash™* on all eligible bookings such as hotels, car rentals, flights, vacation rentals and more on Hotels.com, Expedia and Vrbo.
![Hanging Rock is a mamelon, created 6.25 million years ago by stiff magma pouring from a vent and congealing in place. Often thought to be a volcanic plug, it is not. Two other mamelons exist nearby, created in the same period: Camels Hump, to the south on Mount Macedon and, to the east, Crozier's Rocks.[citation needed] All three mamelons are made of solvsbergite, a form of trachyte only found in two or three other places in the world. As Hanging Rock's magma cooled and contracted it split into rough columns. These weathered over time into the many pinnacles that can be seen today
Hanging Rock contains numerous distinctive rock formations, including the "Hanging Rock" itself (a boulder suspended between other boulders, under which is the main entrance path), the Colonnade, the Eagle and the UFO. The highest point on Hanging Rock is 718 metres above sea level and 105 metres above the plain below.](https://images.trvl-media.com/place/553248634374820821/f1ded2d1-03db-409a-bf64-42f6835b4be8.jpg?impolicy=resizecrop&rw=1920&ra=fit&ch=480)
![Hanging Rock is a mamelon, created 6.25 million years ago by stiff magma pouring from a vent and congealing in place. Often thought to be a volcanic plug, it is not. Two other mamelons exist nearby, created in the same period: Camels Hump, to the south on Mount Macedon and, to the east, Crozier's Rocks.[citation needed] All three mamelons are made of solvsbergite, a form of trachyte only found in two or three other places in the world. As Hanging Rock's magma cooled and contracted it split into rough columns. These weathered over time into the many pinnacles that can be seen today
Hanging Rock contains numerous distinctive rock formations, including the "Hanging Rock" itself (a boulder suspended between other boulders, under which is the main entrance path), the Colonnade, the Eagle and the UFO. The highest point on Hanging Rock is 718 metres above sea level and 105 metres above the plain below.](https://mediaim.expedia.com/destination/2/eba90ca5de6b9f10afd87dd5b6c6b649.jpg?impolicy=fcrop&w=900&h=675&p=1&q=high)