
Thundereggs, also known as thunder eggs, are colourful rocks formed by the crystallisation of siliceous liquids containing minerals and impurities. They are found throughout Australia, with one of the country's largest deposits located at Mt Hay in Queensland. This site is particularly popular for fossicking, or rock searching, with visitors able to dig for their own thundereggs in a designated area. Other notable sites in Queensland include Agate Creek and Hummock Creek in Bundaberg. In New South Wales, thundereggs can be found in the Tweed Valley, Couchy Creek, and Mt. Jerusalem, among other locations.
| Characteristics | Values |
|---|---|
| Location | Queensland, New South Wales |
| Specific Sites | Mt. Hay, Agate Creek, Black Rock Waterhole, Black Soil Area, Campsite, Cave Creek, Spring Creek, Mt. Tambourine, Canungra, Cedar Creek, Couchy Creek, Mt. Jerusalem, Doon Doon, Perch Creek, Pine Log, Mt. Nardi, Bundaberg, Boggabri, Narrabri, Jowlet Hill, Tweed Valley |
| Age | 120 million years old |
| Composition | Rhyolite shell with trapped gas bubbles, which cracked and allowed siliceous liquids with minerals and impurities to enter and crystallize, forming colourful centres of agate, chalcedony, jasper, quartz crystal, amethyst, or a combination |
| Appearance | Knobbly exterior with intricate patterns in colours like maroon and dark blue |
| Size | Thumbnail-sized to extremely large |
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What You'll Learn

Queensland's Mount Hay
Mount Hay holds a special significance as it is the remnant of an ancient volcano, dormant for approximately 120 million years. During its active past, the volcano hosted millions of gas bubbles within its molten rhyolite lava. These gas "pockets" laid the foundation for the Thundereggs that captivate collectors and enthusiasts alike.
The formation of Thundereggs at Mount Hay is a captivating geological process. As the lava cooled, a rhyolite shell enveloped the trapped gas bubbles, only to crack later and release the gases, leaving behind hollow cavities. Siliceous liquids, enriched with minerals and impurities, then permeated these cavities, crystallizing and sealing the cracks. This transformation resulted in the creation of the Thundereggs' enigmatic centres, often composed of agate, chalcedony, jasper, quartz crystal, or a harmonious blend of these minerals.
The Mount Hay Gemstone Tourist Park stands as a testament to the allure of Thundereggs. Visitors are invited to embark on a fossicking journey, guided by friendly and knowledgeable experts who provide essential tools for the exploration. The park offers a comprehensive experience, allowing visitors to uncover Thundereggs at their own pace and even providing on-site professional cutting services to reveal the hidden treasures within their finds.
The park caters to individuals, families, and even groups, with reasonable entry fees and the option to stay longer at the caravan and motorhome sites. The on-site gift shop further enhances the experience, presenting a diverse range of gemstone products and gifts for visitors to cherish as mementos of their Thunderegg adventure at Queensland's Mount Hay.
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Agate Creek
Thundereggs are colourful centres usually made up of agate, chalcedony, jasper, quartz crystal, or a combination of these minerals. They are volcanic marvels that are very rare and found only in a few countries. In Australia, they can be found in Queensland, New South Wales, and the Tweed Valley.
Queensland is home to some of the best-known sources of thundereggs, including Agate Creek and Mt. Hay. Agate Creek, located near Forsayth in northern Queensland, is a fossicking area that is known for its multi-coloured agate with straight, curved, or irregular banding. The thunder eggs in the rhyolite at Agate Creek may contain infillings of red-brown jasper. Black Soil Creek, Crystal Hill, Bald Hill, Simpsons, Blue Hills, and Flanagans are some of the main areas of interest within the Agate Creek locality.
The Agate Creek fossicking area is characterised by a basin-shaped region called Agate Pocket, which is underlain by volcanic rocks. This volcanic sequence dates back to the early Permian age and consists of three distinct formations: the Big Surprise Tuff, Black Soil Andesite, and Thunder Egg Rhyolite. The Black Soil Andesite is a type of basaltic andesite lava flow in which agate occurs as amygdales, or filled gas bubbles. The Thunder Egg Rhyolite, on the other hand, forms the north-eastern rim of the pocket, where thunder eggs are found as spherulites in rhyolitic lava.
The volcanic nature of Agate Creek is further highlighted by its connection to the Agate Creek Volcanic Group. This group of rocks serves as a reminder of the region's volcanic past, with the volcanics covered by sandstones and conglomerates from the Jurassic period. While most of these deposits have been stripped away, remnants can still be found as hill cappings in specific locations, such as the south-western escarpment bordering the pocket and the head of Spring and Agate creeks.
Overall, Agate Creek in Queensland, Australia, is a notable location for fossicking and exploring the geological wonders of thundereggs. Its volcanic history, unique rock formations, and the presence of colourful agate and thunder eggs make it a fascinating destination for those interested in the natural wonders of the country.
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Mount Tamborine
The Thunderegg Mine is open every day except Christmas Day and Good Friday, from 9:30 am to 2:30 pm. Visitors can discover hidden treasures from prehistoric volcanic lava in the world's largest Thunderegg Mine. Staff at the rock shop suggest that because Thundereggs tend to run in "seams", you are more likely to find them where others have been found before.
The activity is suitable for the whole family, and the park also offers other attractions, such as a high ropes course, mini-golf, and bird feeding. There is an onsite restaurant, as well as shower and toilet facilities.
One visitor to the park noted that there is minimal shade, so it is important to bring your own water. Another visitor mentioned that booking in advance is easy, and the staff at the front desk are friendly and helpful.
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New South Wales' Couchy Creek
Thundereggs are colourful, hollow rocks formed from volcanic gas bubbles. They are considered very rare and are found only in a few countries. In Australia, they are mostly sourced from a band of rhyolite that runs from Mt Tamborine in Queensland to Mt Nardi in Northern New South Wales. This band, formed during the late Triassic period, is approximately 225 million years old.
New South Wales Couchy Creek thundereggs are found in the Tweed Valley. They are known for their unsilicified rhyolite shells and "Waterline/Horizontal Banding" types of agate. The agates are often colourless with greenish to bluish tints. The Couchy Creek site is now part of the Australia National Park, and collecting thundereggs is not permitted.
Thundereggs are also found at other sites in New South Wales, including Mt. Jerusalem, Doon Doon, Perch Creek, and Pine Log. These sites are all located within the band of rhyolite that runs through the state. The Mt. Jerusalem site is particularly notable for its unique specimens, which often occur as bizarre cores.
The best-known sources of thundereggs in Queensland are Agate Creek and Mt. Hay. Agate Creek is known for its nice colours and level banding, while Mt. Hay offers a variety of sub-sources for thundereggs. Other sources of thundereggs in Australia include Canungra, Numinbah, and Mt. Tambourine "Cedar Creek". These sites offer a range of thundereggs with different structures and fillings.
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Perch Creek
Thundereggs are mostly found in New South Wales, Australia, in a band of rhyolite that resulted from Mt Warning's eruption in the late Triassic period, around 225 million years ago. This band runs from Mt Tamborine in Queensland to Mt Nardi in Northern NSW. Perch Creek, located within this band, is one of several sites where thundereggs can be found.
The thundereggs found at Perch Creek vary in size and appearance. Some may be quite large, while others are smaller and attached to larger teggs, indicating their origin from this specific region. The thundereggs from this location often exhibit interesting and distinctive features, such as water lines or unusual core structures.
Collectors and enthusiasts often share their experiences and findings from Perch Creek. Some describe the thundereggs they have acquired from the site, noting their aesthetic appeal, such as the presence of beautiful colours and level banding. Others may share tips on the best locations within Perch Creek to find these specimens or provide insights into the preparation processes required after discovery, such as cutting and polishing.
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Frequently asked questions
Thundereggs can be found throughout Australia, but some of the country's largest deposits are at Mt Hay in Queensland. Queensland had the right volcanic conditions for thundereggs to form hundreds of millions of years ago.
Agate Creek and Mt Tambourine are also known for their thundereggs.
Yes, thundereggs can also be found in New South Wales, specifically in the Tweed Valley and at Mt. Jerusalem.


