Meetings are currently being held online via Zoom - see below

Monthly meetings

The society meets on the first Friday of each month (excluding January), unless that Friday is a public holiday or before a long weekend, in which case the meeting is on the second Friday.

Meetings start at 7.30pm. Visitors are very welcome.

All members attending the meeting should be double vaccinated. Masks can be worn but are optional and social distancing should be maintained. Everyone should sign the Attendance Register although registering by QR code is not required. Anyone who feels unwell or has had recent contact with an infected person should not attend the Meeting.


Meetings are held in the clubrooms of the Parramatta Holroyd Lapidary Club at 73 Fullagar Rd, Wentworthville.

Upcoming program


01jul7:00 pm9:00 pmJuly MeetingThe program will include a lecture to be given by Luis Martins on : – ‘A Mineral Collecting Trip to the Faroe Islands’.  There will also be a mini-talk to be given by John Chapman and David Colchester on : – ‘Iridescence – Now And Then’.  Members are invited to bring in any specimens showing iridescence to display to the Meeting. 


05aug7:00 pm9:00 pmAugust MeetingThe Society Annual General Meeting and the Mayne-Walker Memorial Lecture to be given this year by Dr Ken McQueen on “The Paddy’s River Skarns, ACT: Their Origin and Mineralogy”  The following details about the speaker and the subject of his lecture have been provided by John Chapman:  ‘We are honoured to have Dr McQueen present the Mayne-Walkers Memorial Lecture this year. Ken is Adjunct Professor (Geochemistry and Landscape Evolution), at the University of Canberra. He is also an old friend of the Society having given us a number of presentations over the years. The work on the skarn deposits of Paddys River was recently published in the Australian Journal of Mineralogy  Several areas of skarn mineralization occur along the Paddy’s River valley in the ACT. The deposits are zoned, magnetite- and silicate-rich metasomatic replacement skarns containing complex assemblages of prograde and retrograde primary minerals and an association of base metal sulfides, scheelite, minor silver, gold and bismuth. The skarn mineralogies indicate medium-high temperature, oxidising conditions during their formation. Sulfides and scheelite were introduced during hydrous retrograde alteration. Weathering of the skarns has resulted in a great variety of secondary minerals and oxidation products. More than 90 different primary and secondary mineral species have been identified in the skarns.’