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Crystal Kingdom was established in 1974 and later expanded in 2004 to make room for more specimens that had never been on display before. This display included crystals, minerals and fossils from the local Warrumbungle Range. This was the first collection in Australia to display minerals and fossils from one local area only.

The Warrumbungle Range includes two extinct volcanoes, the Warrumbungle Volcano at 17-14 million years of age and the Garrawilla Volcanics which was active 24-200 million years ago.

This exhibit contains some of the world's rarest and most colourful zeolite crystals and rare fossils that are found nowhere else in the world.

We are open daily from 8 am to 5 pm. Closed Christmas day.

Entry is a donation to help support the museum.

OUR VOLCANOES

 

The Warrumbungle Range is a spur of the Great Dividing Range and forms a large semi-circle to the west. This area contains two ancient extinct volcanoes. The oldest one is known as the Garrawilla Volcanics and is located about 40 km to the east of the town of Coonabarabran. It consists of a basement of the Permian Black Jack Formation (coal), overlain by the sedimentary Triassic Digby and Napperby Beds. After these beds were laid down, the area was subjected to a period of intense volcanic activity. Eruptions of flows and pyroclastics, from numerous centres, produced a thick volcanic pile, the Garrawilla Volcanics.

This Volcano was active from about 200 million years ago until it stopped about 45 million years ago. Sedimentary rocks of the Purlewaugh and Pilliga Beds overlay these flows in the south and west, suggesting that much of the Garrawilla Volcano remained as an island or peninsula in the Jurassic Sea, about 120 million years ago.

An area in this volcanic complex, about 40 km long and 7 km wide, produced the rare and colourful Zeolite Crystals on display in the Crystal Kingdom.

The Warrumbungle Mountains, to the west of Coonabarabran, is a much younger volcano. This one started about 17 million years ago and finished about 13 million years ago. At that time, the landscape was very much like it is today.

The early eruptions consisted mainly of trachyte, a very viscous type of lava. These formed the spectacular spires and domes you see today.

The later eruptions were of the more fluid basalt type, which flowed over the top of these and created a large Shield Volcano. Most of this basalt is eroded away and the older trachyte vents are now dominating the landscape.

The Warrumbungle volcano is Australia's most spectacular shield volcano and is the most westerly volcano in eastern Australia. It encompasses a wide variety of microclimates where species from completely different environments can be found near each other. For example, on some high ridges there are grass trees growing in the same area as snow gums. There are many different timbers, wildflowers and habitats for birds and wildlife. Being a nature lover’s paradise with over 360 species of birds being counted in our local area. Many species of wildlife are also found here including possums, sugar gliders, wombats, kangaroos, wallaroos, koalas, and wallabies.

Unfortunately for us the Warrumbungles have not worn down enough yet to allow us to discover its interesting minerals. Underneath this lies the much older Garrawilla volcano. This volcanic system stretches from Dubbo, to Narrabri, Gunnedah and at least as far west as Coonamble. At approximately 170 million years of age, it has been worn down to its early history and that is where the rare zeolite crystals have been discovered and the whole area is rich in fossils.

Have you ever wanted to know?

What is a Zeolite?;

Why do crystals have different shapes?;

How are crystals formed?:

How is a mineral identified?;

Can crystals generate electricity?;

What is the difference between an intrusive and an extrusive volcano?;

What is a fossil?;

What permian plant was responsible for the coal deposits of the “Gunnedah Basin”?

You will find the answer to these and other questions at the CRYSTAL KINGDOM, the home of the “ Minerals of the Warrumbungles”.

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Gallery

Amberat

Amberrat comes from the nest of the extinct Sticknest Rat. These small mammals build their nests in a fissure in a sandstone cliff. As rats do, they made a mess of their nest, but kept building more nests on top of each other. Over time this mess compacted into a black substance.

It is believed that 1 mm thickness contains the residue of 3 years. The depth of this nest is approx. 3 m. This substance is made up of rat droppings, some bones and plant material.

By testing for age and analysing this material,

scientists can establish what the local climate was in the past.

These animals were widespread throughout the area, but were wiped out by foxes and cats