Central gold district
The discovery of alluvial gold in gullies south of Clermont in 1861 triggered one of Queensland's major gold rushes. Today, the old gold mining district surrounding Clermont attracts interest from fossickers and metal detector enthusiasts.
Fossickers require a fossicking licence in all areas and must comply with the special conditions of access (see below).
Access
There are 12 separate general permission areas in the Clermont area where landholders have given general permission for fossicking. View the map of 8 of these general permission areas in the Clermont area 357.1 KB).
Maps
- Bathampton fossicking map 664.4 KB)
- Birimgan East fossicking map 937.1 KB)
- Birimgan West fossicking map 733.3 KB)
- Black Ridge fossicking map 742.8 KB)
- Brigalow fossicking map 811.9 KB)
- Flat Diggings fossicking map 639.4 KB)
- Four Mile East fossicking map 702.3 KB)
- Four Mile West fossicking map 767.6 KB)
- McDonald Flat fossicking map 712.4 KB)
- McMasters fossicking map 803.2 KB)
- Museum Reserve fossicking map 782.6 KB)
- Town Reserve fossicking map 784.9 KB)
Facilities
Camping is not permitted. There is a range of accommodation facilities in Clermont.
Fossicking notes
Gold occurs in a range of settings in the district. The primary source is numerous lode gold deposits, mostly quartz reefs, in the Anakie Metamorphic Group. Only a small number of these were economic to work.
More important were deep leads in old conglomerates (gravels) of Permian age, which overlie the metamorphics. These have usually been interpreted as ancient buried streams in which alluvial gold shed from the lodes has accumulated. Nuggets in excess of 15g were common and some specimen gold occurred in quartz-rich clasts. Other deep leads were located in late Tertiary alluvial deposits, in linear belts cutting across the present drainage pattern.
Finally there were the alluvial deposits of modern-day streams, derived from gold shed from older deposits.
The deep leads produced the most gold.
The gold of interest to modern fossickers is primarily from the young alluvial material, as well as eluvial deposits formed when gold or gold-bearing rock fragments have been transported short distances from their sources, and concentrated within the soil horizon.
Some older Tertiary wash on the edges and tops of interfluves may also be of interest. Some nuggets may have formed in these environments by chemical accretion of small gold particles into larger fragments or through the chemical action of host soils or sediments on a gold solution.
Panning is the simplest recovery method for the finer alluvial gold. However, the scarcity of water may preclude panning during dry periods. Dry blowing methods may be employed.
Special conditions
- Special conditions to fossick in general permission areas within the Clermont area 110.6 KB)
- Special conditions to fossick in Flat Diggings Reserve general permission area 92.2 KB)
- Fossicking is not permitted on Mining claims, Mining leases and Mining Lease applications in these areas without the permission of the holders or applicants. See maps for details.