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Where's the butter? EarthCache

Hidden : 11/4/2009
Difficulty:
1.5 out of 5
Terrain:
4 out of 5

Size: Size:   not chosen (not chosen)

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Geocache Description:

This Earthcache is located in the Warrumbungle National Park in North Western New South Wales. The National Park contains many interesting geological features. The specific feature examined in this Earthcache however is The Breadknife.


The name Warrumbungle is of Aboriginal origin and is believed to either mean ‘small mountains’ or ‘crooked mountains’. The Warrumbungle National Park is around 500 kilometres north-west of Sydney, with the nearby town of Coonabarabran being the most common way to access the park.

The Breadknife itself is a fantastic example of an igneous dyke which has been left exposed following erosion. It was formed as part of the eruption of the Warrumbungle volcano. It is estimated that the Warrumbungle volcano first erupted around 17 million years ago and then stopped around 13 million years ago. Most of the volcano has been eroded away, leaving the many geological features that are contained within the park.

This Warrumbungle volcano was a shield volcano which indicates that the magma, or molten rock, was very hot and runny. This meant that eruptions were not as violent as some volcanoes and resulted in a large amount of magma flowing to the surface.

In order to reach The Breadknife itself a bushwalk is required. Starting at the Pincham carpark the return walk is around 12km and you should allow around 4-6 hours return. The Breadknife is found along the route towards the Grand High Tops. Take plenty of water and sun protection and note that there is some gain in altitude. If you continue past The Breadknife to the Grand High Tops you will be able to observe it at another angle. Note that climbing is prohibited on The Breadknife.

Along the way there are other interesting geological features to observe including Belougery Spire which is another feature formed by the extinct volcano.

In the case of The Breadknife, some magma was extruded through ash and cinders from the volcano. The magma then cooled and hardened. As the ash and cinders eroded over time the thin band of rock reaching up from the surrounding landscape is all that remains. The ‘blade’ of The Breadknife is quite high in places and is many hundreds of metres long.

To log your visit at the site you need to email the answers to the following questions:

1. Estimate how high The Breadknife is at the given co-ordinates (it might help by having someone stand beside the rock and taking them as 1.5-2m high).

2. Look at the fault lines (cracks) in the rock. Estimate how wide a ‘block’ (or square) of rock that comprises The Breadknife is.

You also need to take a photo of you/ your party standing beside The Breadknife and upload this with your log.

Logs without corresponding answers and picture may be deleted.

Additional Hints (No hints available.)