Monday, May 29, 2017  
 
News & Updates
VISITING MOUNT BUFFALO IN MAY
13-04-2017 
Our Mountain is amazing in the Autumn, but it is getting colder so make sure that you bring some warm clothes as the alps are normally 10 degrees cooler than Bright and the Alpine valleys. There are still enough warm days for rock climbing and abseiling in the gorge, bushwalking or a bike ride.
Spoil yourself and "Visit Mount Buffalo" this Autumn.

LAKE CATANI CAMPING GROUND CLOSED
13-04-2017 
Note that Parks Victoria have now closed the Lake Catani camping ground for general camping (There are limited snow camping sites available during winter). Camping reopens again in November.


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ABOUT OUR MOUNTAIN

GEOLOGY
Formed well below the earths surface millions of years ago, wind, water and ice have eroded away the granite leaving behind the mountain's amazing rock formations.  The sedimentary rocks that originally covered the area (and some of the metamorphic rocks of the contact zones) can still be seen at places on the road to the mountain top.
Pegmatites and Dykes will be found in the granites of mount Buffalo by the observant person (although not crystal rich as are the pegmatites of the Beechworth Granites). Xenoliths are also interesting and quite common.

ABOUT XENOLITHS
www.umanitoba.ca/geoscience/faculty/arc/xenolith.html

MORE ABOUT GRANITE
geology.about.com/od/more_igrocks/a/granite.ht


Explorers Hume and Hovell named Mount Buffalo in 1824 as they passed through the area on their way from Sydney to Port Phillip Bay traveling through what is now the Wangaratta / Glenrowan ares. They likened the mountain to a sleeping buffalo in the distance. This explains the names for the granite tors such as the Horn and the Hump.

MORE ABOUT HUME AND HOVELL
www.australianhistory.org/hume-hovell.php
www.kidcyber.com.au/topics/humenhovell.htm

The Horn (at the South End of the Mountain), rises to 1723 metres and is the highest point on the plateau.

SEE THE DROP DOWN MENU FOR MORE INFORMATION