Vote for your favorite mineral in #MinCup26! - Sphalerite vs. Anorthite
Both zinc ore Sphalerite and calcium plagioclase feldspar Anorthite have perfect cleavage that will split cleanly if you hit them with a hammer, but only one can claim a larger split of your votes!
Log InRegister
Quick Links : The Mindat ManualThe Rock H. Currier Digital LibraryMindat Newsletter [Free Download]
Home PageAbout MindatThe Mindat ManualHistory of MindatCopyright StatusWho We AreContact UsAdvertise on Mindat
Donate to MindatCorporate SponsorshipSponsor a PageSponsored PagesMindat AdvertisersAdvertise on Mindat
Learning CenterWhat is a mineral?The most common minerals on earthInformation for EducatorsMindat ArticlesThe ElementsThe Rock H. Currier Digital LibraryGeologic TimeExplore Fossils
Minerals by PropertiesMinerals by ChemistryMineral Visual ExplorerAdvanced Locality SearchRandom MineralRandom LocalitySearch by minIDLocalities Near MeSearch ArticlesSearch GlossaryMore Search Options
Search For:
Mineral Name:
Locality Name:
Keyword(s):
 
The Mindat ManualAdd a New PhotoRate PhotosLocality Edit ReportCoordinate Completion ReportAdd Glossary Item
Mining CompaniesStatisticsUsersMineral MuseumsClubs & OrganizationsMineral Shows & EventsThe Mindat DirectoryDevice SettingsThe Mineral QuizTime Machine
Photo SearchPhoto GalleriesSearch by ColorPhoto Colour ExplorerNew Photos TodayNew Photos YesterdayMembers' Photo GalleriesPast Photo of the Day GalleryPhotography
This page is currently not sponsored. Click here to sponsor this page.
PhotosMapsSearch
Latitude & Longitude (WGS84):
30° 9' 21'' South , 139° 20' 47'' East
Latitude & Longitude (decimal):
Type:
Mine (Abandoned) - last checked 2025
Mindat Locality ID:
16756
Long-form identifier:
mindat:1:2:16756:6
GUID (UUID V4):
0
Other/historical names associated with this locality:
Sir Dominic Mine; Sir Domonic Mine


Copley: H54-9/Umberatana SH5409
Record of mines - Summary Card No: 277

"Name: Sir Dominick Mine"
"Alternative names: No: 8 Yudnamutana Group"

"Location: On western bank of Daly Creek, 3/4 mile southeast of the Daly Mine."

"History: It was opened up in 1862 by the Northern Minerals Association and from 1866 to 1868 was one of the properties of the Daly-Stanley Mining Company. At a later date it was held by the Tasmanian Copper Company, and subsequently by tributors.
Further exploration was carried out about 1910 and in 1914 the mine was taken over by the Flinders Copper Mining Company, being known as the No: 8 Workings. (Jones 1910, p.24) A small amount of ore was produced in 1918, and work finally ceased in 1920 then the field was abandoned. W.C. 5174 (M.R. 573) of about 40 acres round the mine was taken up on October 9th, 1967 by Kennecott Explorations (Aust.) Pty. Ltd."

Above is an excerpt from the Record of Mines - Mines Summary Card
(Spelling and grammar may differ from present standards.)

05184810017272029466269.jpg
Sir Dominick Daly


The Daly Mine, the Sir Dominick Mine, and the nearby Daly Bore were all named after Sir Dominick Daly - the former governor of South Australia (1862–1868). He also served as governor of Prince Edward Island, Canada (1854-1859). Born on 11 August 1798 at Ardfry, Ireland; Died 19 February 1868, Adelaide, South Australia, Australia. His nephew (and namesake) Dominick Daly became a government surveyor for the state of South Australia with G. G. McLachlan's No. 6 Party with Goyder's Expedition of 1869.

The alternative mine names would appear to be simply misspelled names and not official names for the mine. It is believed people often, while looking for the Sir Dominick Mine, come across the Daly first without realizing that there are in fact two mines in close proximity. It is interesting to note that there is quite a marked difference in the matrix and geology of the two mines. This was even noted by H.Y.L. Brown in 'The Record of Mines of South Australia - 1908'. To add to the confusion, there is only ¾ mile or 1.2 km (1.7 km by track) between these mines, and the official northern boundary of Sir Dominick is the southern boundary of Daly.

The Sir Dominick mine is reached by following the track past the Daly mine and continuing along the creek another 1.7 km; the last 500 m is cut into the side of the hill and is not recommended due to steep washouts. Heavy rains in January 2011 washed away whole sections of the access track along the creek from the Daly mine onward.

The mine is best known for specimens of malachite pseudomorphs after azurite, with some clusters found up to 10 cm across and single crystals 2-3 cm across. These have formed in a kaolinized matrix, which is often found in various earthy shades, and show no points of attachment. A small arsenate zone has been identified in the uppermost adit, producing specimens of olivenite with malachite, cornwallite, and cornubite.

There are a number of other mines in the vicinity that also contain copper arsenate minerals, so care should be taken when recording locality information.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Commodity List

This is a list of exploitable or exploited mineral commodities recorded at this locality.


Mineral List


12 valid minerals.

Rock Types Recorded


Select Rock List Type

Alphabetical List Tree Diagram

Detailed Mineral List:

'Agardite'
References:
Peter ElliottIdentification: SEM-EDS
Azurite
Formula: Cu3(CO3)2(OH)2
Description: England (1980): "Isolated pockets of unaltered azurite crystals occur throughout the workings but these crystals rarely exceed 1/2 inch in diameter. An interesting occurrence in the walls of the open cut above No. 2 adit is the presence of azurite crystals with malachite-replaced centers. This would indicate an apparent additional short period of azurite growth after replacement of the original azurite crystals. Perhaps this was favored by a recent lack of groundwater movement in some sections of the deposit. The azurite usually occurs as single isolated crystals or small groups. In the open cut above No. 2 adit, exceptionally fine chain-like groups of prismatic crystals were found in a soft claystone in a small and apparently unique pocket. Cleaning of these specimens required several hours painstaking work and in many cases careful repair was essential to preserve these unusual groups intact."
Chrysocolla
Formula: Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Conichalcite
Formula: CaCu(AsO4)(OH)
Cornubite
Formula: Cu5(AsO4)2(OH)4
Cornwallite
Formula: Cu5(AsO4)2(OH)4
Cuprite
Formula: Cu2O
Hematite
Formula: Fe2O3
Kaolinite
Formula: Al2(Si2O5)(OH)4
Malachite
Formula: Cu2(CO3)(OH)2
Habit: England (1980, on malachite pseudomorphs): "There are three major morphological types, showing sharply defined crystal faces. All have an internal radiating fibrous structure. (a) single crystals The single crystals from the Sir Dominick mine show distinct monoclinic symmetry and vary in habit from thin tabular to prismatic barrel-shaped crystals, both types consisting of simple combinations of hemi-prism and basal pinacoid faces. The convex appearance of the prismatic crystals is due to the presence of quite prominent hemi-pyramid faces (h). Most single crystals actually comprise a number of individuals in parallel growth, made evident by the presence of multiple termination faces. Many of the tabular crystals show unaltered azurite centers. (b) rosette groups Tabular crystals commonly occur in sub-parallel to divergent groups, giving the appearance of malachite rosettes, ranging from 1/4 inch to almost 2 inches in diameter. (c) spherical aggregates These are probably the most common of the pseudomorph types. Specimens comprise irregular to spherical aggregates of prismatic to tabular crystals occasionally exceeding 4 inches in diameter. Individual crystals in the aggregates range up to 3/4 inch in diameter."
Description: England (1980): "Isolated, small, vuggy dark gray quartz pods in the kaolinitic crush zones, particularly in the open cut above No. 2 adit, contain tufted groups of acicular malachite crystals to 1/4 inch long. These provide exceptional micromounts."
Olivenite
Formula: Cu2(AsO4)(OH)
Quartz
Formula: SiO2
Colour: white; dark gray
Tremolite
Formula: ◻Ca2Mg5(Si8O22)(OH)2

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 4 - Oxides and Hydroxides
Cuprite4.AA.10Cu2O
Hematite4.CB.05Fe2O3
Quartz4.DA.05SiO2
Group 5 - Nitrates and Carbonates
Azurite5.BA.05Cu3(CO3)2(OH)2
Malachite5.BA.10Cu2(CO3)(OH)2
Group 8 - Phosphates, Arsenates and Vanadates
Olivenite8.BB.30Cu2(AsO4)(OH)
Cornwallite8.BD.05Cu5(AsO4)2(OH)4
Cornubite8.BD.30Cu5(AsO4)2(OH)4
Conichalcite8.BH.35CaCu(AsO4)(OH)
Group 9 - Silicates
Tremolite9.DE.10◻Ca2Mg5(Si8O22)(OH)2
Kaolinite9.ED.05Al2(Si2O5)(OH)4
Chrysocolla9.ED.20Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Unclassified
'Agardite'-

List of minerals for each chemical element

HHydrogen
H AzuriteCu3(CO3)2(OH)2
H ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
H ConichalciteCaCu(AsO4)(OH)
H CornubiteCu5(AsO4)2(OH)4
H CornwalliteCu5(AsO4)2(OH)4
H KaoliniteAl2(Si2O5)(OH)4
H MalachiteCu2(CO3)(OH)2
H OliveniteCu2(AsO4)(OH)
H Tremolite◻Ca2Mg5(Si8O22)(OH)2
CCarbon
C AzuriteCu3(CO3)2(OH)2
C MalachiteCu2(CO3)(OH)2
OOxygen
O AzuriteCu3(CO3)2(OH)2
O ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
O ConichalciteCaCu(AsO4)(OH)
O CornubiteCu5(AsO4)2(OH)4
O CornwalliteCu5(AsO4)2(OH)4
O CupriteCu2O
O HematiteFe2O3
O KaoliniteAl2(Si2O5)(OH)4
O MalachiteCu2(CO3)(OH)2
O OliveniteCu2(AsO4)(OH)
O QuartzSiO2
O Tremolite◻Ca2Mg5(Si8O22)(OH)2
MgMagnesium
Mg Tremolite◻Ca2Mg5(Si8O22)(OH)2
AlAluminium
Al ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Al KaoliniteAl2(Si2O5)(OH)4
SiSilicon
Si ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Si KaoliniteAl2(Si2O5)(OH)4
Si QuartzSiO2
Si Tremolite◻Ca2Mg5(Si8O22)(OH)2
CaCalcium
Ca ConichalciteCaCu(AsO4)(OH)
Ca Tremolite◻Ca2Mg5(Si8O22)(OH)2
FeIron
Fe HematiteFe2O3
CuCopper
Cu AzuriteCu3(CO3)2(OH)2
Cu ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Cu ConichalciteCaCu(AsO4)(OH)
Cu CornubiteCu5(AsO4)2(OH)4
Cu CornwalliteCu5(AsO4)2(OH)4
Cu CupriteCu2O
Cu MalachiteCu2(CO3)(OH)2
Cu OliveniteCu2(AsO4)(OH)
AsArsenic
As ConichalciteCaCu(AsO4)(OH)
As CornubiteCu5(AsO4)2(OH)4
As CornwalliteCu5(AsO4)2(OH)4
As OliveniteCu2(AsO4)(OH)

Other Regions, Features and Areas containing this locality

Australia
Australian PlateTectonic Plate

This page contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders for access and that you are aware of all safety precautions necessary.

References

 
and/or  
Mindat.org® is an outreach project of the Hudson Institute of Mineralogy, a 501(c)(3) not-for-profit organization. Mindat® and mindat.org® are registered trademarks of the Hudson Institute of Mineralogy.
Copyright © mindat.org and the Hudson Institute of Mineralogy 1993-2026, except where stated. Most political location boundaries are © OpenStreetMap contributors. Mindat.org relies on the contributions of thousands of members and supporters. Founded in 2000 by Jolyon Ralph and Ida Chau.
Content on this site may not be used to train, fine-tune, or otherwise develop artificial intelligence or machine learning models without prior written permission - see our Terms & Conditions.
To cite: Ralph, J., Von Bargen, D., Martynov, P., Zhang, J., Que, X., Prabhu, A., Morrison, S. M., Li, W., Chen, W., & Ma, X. (2025). Mindat.org: The open access mineralogy database to accelerate data-intensive geoscience research. American Mineralogist, 110(6), 833–844. doi:10.2138/am-2024-9486.
Privacy Policy - Terms & Conditions - Contact Us / DMCA issues - Report a bug/vulnerability Current server date and time: September 3, 2026 02:34:22 Page updated: April 6, 2026 18:28:10
Go to top of page