Mount Royal | |
---|---|
basalt outcrop on Mount Royal
|
|
Highest point | |
Elevation | 1,185 m (3,888 ft) |
Coordinates | 32°10.454′S 151°19.571′E / 32.174233°S 151.326183°ECoordinates: 32°10.454′S 151°19.571′E / 32.174233°S 151.326183°E |
Geography | |
Location | Hunter Region, Australia |
Country | Australia |
Parent range | Mount Royal Range |
Geology | |
Age of rock | Late Paleocene |
Mountain type | basalt cap |
Mount Royal is situated at the southern end of the Mount Royal Range in the Barrington Tops region of eastern Australia. It is part of the World Heritage Gondwana Rainforests of Australia.
The lower sections of the mountain are made up of sedimentary rocks such as mudstones. A residual basalt cap appears at 1,100 metres (3,600 ft) above sea level. It originated from the flow of the nearby Barrington Volcano. The mountain is partially in Mount Royal National Park and Barrington Tops National Park.
The high altitude rainforest growing on the red/brown soils lacks the Antarctic beech despite apparently ideal conditions. Their place the upper canopy is taken by the golden sassafras. The elevated narrow rainforest features hanging moss, often covered in mist.
The mountain's summit is covered in a low rainforest thicket, composed mostly of the hill water gum. Other noteworthy plants on the mountain include New England blackbutt, chainfruit, prickly ash, grass tree and the . Another interesting feature of Mount Royal is the grassy balds, surrounded by temperate rainforest. Fire caused by lightning is one speculative theory of their origin.
The lower south east slopes of Mount Royal support a well developed sub-tropical rainforest. Significant species include the Australian red cedar, citronella, rosewood and the giant stinging tree.