Burgess Mine, Carlow Township, Hastings County, Ontario, Canadai
| Regional Level Types | |
|---|---|
| Burgess Mine | Mine (Inactive) |
| Carlow Township | Township |
| Hastings County | County |
| Ontario | Province |
| Canada | Country |
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Latitude & Longitude (WGS84):
45° 15' 55'' North , 77° 42' 3'' West
Latitude & Longitude (decimal):
Type:
Mine (Inactive) - last checked 2024
Köppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| Bancroft | 3,838 (2008) | 26.1km |
Nearest Clubs:
Local clubs are the best way to get access to collecting localities
Local clubs are the best way to get access to collecting localities
| Club | Location | Distance |
|---|---|---|
| Bancroft Gem and Mineral Club and Museum | Bancroft, Ontario | 26km |
This mine is made up of a large adit driven into the west side of Burgess Ridge and a large dump located beside a pond about 35 meters from the adit.
The mine is within a northeasterly trending body of syenitic gneisses & pink & white leucosyenite pegmatite. These syenites, along with granitic rock, form the Burgess Ridge.
(Eardley-Wilmot, 1927, description as follows)
Mining was started in July 1902, on concession XIV, lot 14, by the Ontario Corundum Company. Operations were continued until 1905, when the property was taken over by the Ashland Emery and Corundum Company. Shipments were at first small and irregular, mainly owing to the depletion of the ore at the original location. Mining activities were transferred to a deposit on concession XVI, lots 15 and 16, north of Grady Lake, about 2 miles (3.22 km) to the north, from which a considerable tonnage was obtained for the next two years. In 1907 these deposits were also abandoned, and ore was taken first from concession XII, lot 10, a haulage of 3 miles (ca. 5 km) to the mill, and later from the deposit on John Armstrong's hill, concession XV, lot 10, about 1.5 miles (2.41 km) to the west.
Early in 1910, the Armstrong Corundum Company, Limited, secured a lease on the Burgess plant, but after operating only two months, it was taken over by the Manufacturers Corundum Company, which was already operating the Craig mill and mine about 4 miles (6.44 km) to the east. The crude concentrates from the Burgess mine were finished at the Craig mill.
In the main workings in the steep hillside just to the north of the old mill, the quarry is about 200 feet (ca. 61 m) in length with a 50-foot face. The corundum, which is very pockety, occurs as large, brown, or bronze crystals in coarse, micaceous, red pegmatite syenite. There is very little to be seen in place except at the north end of the workings near the contact of the syenite and banded gneiss.
The nearest railway is at Barry's Bay station, 32 miles (ca. 51 km) to the north. The ore and concentrates during the summer were hauled to a wharf on the York River and shipped by barge to the station.
In the main Burgess workings, the interbanded layers of grey and pink syenite lie almost horizontally. Corundum occurs in both types of syenite, sometimes in association with magnetite.
The mine buildings have long been removed, but the road through the property is passable for automobiles; the Burgess property is now PRIVATELY OWNED, and collecting is not permitted. NO TRESPASSING!
The mine is within a northeasterly trending body of syenitic gneisses & pink & white leucosyenite pegmatite. These syenites, along with granitic rock, form the Burgess Ridge.
(Eardley-Wilmot, 1927, description as follows)
Mining was started in July 1902, on concession XIV, lot 14, by the Ontario Corundum Company. Operations were continued until 1905, when the property was taken over by the Ashland Emery and Corundum Company. Shipments were at first small and irregular, mainly owing to the depletion of the ore at the original location. Mining activities were transferred to a deposit on concession XVI, lots 15 and 16, north of Grady Lake, about 2 miles (3.22 km) to the north, from which a considerable tonnage was obtained for the next two years. In 1907 these deposits were also abandoned, and ore was taken first from concession XII, lot 10, a haulage of 3 miles (ca. 5 km) to the mill, and later from the deposit on John Armstrong's hill, concession XV, lot 10, about 1.5 miles (2.41 km) to the west.
Early in 1910, the Armstrong Corundum Company, Limited, secured a lease on the Burgess plant, but after operating only two months, it was taken over by the Manufacturers Corundum Company, which was already operating the Craig mill and mine about 4 miles (6.44 km) to the east. The crude concentrates from the Burgess mine were finished at the Craig mill.
In the main workings in the steep hillside just to the north of the old mill, the quarry is about 200 feet (ca. 61 m) in length with a 50-foot face. The corundum, which is very pockety, occurs as large, brown, or bronze crystals in coarse, micaceous, red pegmatite syenite. There is very little to be seen in place except at the north end of the workings near the contact of the syenite and banded gneiss.
The nearest railway is at Barry's Bay station, 32 miles (ca. 51 km) to the north. The ore and concentrates during the summer were hauled to a wharf on the York River and shipped by barge to the station.
In the main Burgess workings, the interbanded layers of grey and pink syenite lie almost horizontally. Corundum occurs in both types of syenite, sometimes in association with magnetite.
The mine buildings have long been removed, but the road through the property is passable for automobiles; the Burgess property is now PRIVATELY OWNED, and collecting is not permitted. NO TRESPASSING!
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsDetailed Mineral List:
| ⓘ 'Allanite Group' Formula: (A12+REE3+)(M13+M23+M32+)O[Si2O7][SiO4](OH) Habit: Platy crystals in cavities and found loose in dumps. Description: Collected by and in collections of Matthew Neuzil and Michal Adamowicz References: |
| ⓘ 'Biotite' Formula: K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 Description: Radioactive minerals have been reported |
| ⓘ Calcite Formula: CaCO3 Description: Dont visit during hunting season
References: |
| ⓘ 'Calcium Amphibole Subgroup' Formula: AnCa2(C2+5-mC3+m)(Si8-(n+m)Al(n+m))W2 References: Cyrille Daoud CollectionIdentified by Cyrille Daoud: Visual Identification |
| ⓘ 'Chlorite Group' Description: Radioactive minerals have been reported |
| ⓘ Corundum Formula: Al2O3 Colour: grey, bronze, black, red Description: Radioactive minerals have been reported |
| ⓘ Epidote Formula: (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) Description: Radioactive minerals have been reported |
| ⓘ 'Hornblende Root Name Group' Formula: ◻Ca2(C2+4C3+)(AlSi7O22)W2 Description: Radioactive minerals have been reported |
| ⓘ Magnetite Formula: Fe2+Fe3+2O4 Colour: grey -metalic Fluorescence: none Description: Radioactive minerals have been reported |
| ⓘ Muscovite Formula: KAl2(AlSi3O10)(OH)2 Description: Radioactive minerals have been reported |
| ⓘ Pyrite Formula: FeS2 Description: Radioactive minerals have been reported |
| ⓘ 'Pyroxene Group' Formula: ADSi2O6 References: Cyrille Daoud CollectionIdentified by Cyrille Daoud: Visual Identification, Optical Analysis |
| ⓘ Rutile Formula: TiO2 Description: Radioactive minerals have been reported |
| ⓘ 'Scapolite' |
| ⓘ Schorl ? Formula: NaFe2+3Al6(Si6O18)(BO3)3(OH)3(OH) |
| ⓘ Titanite Formula: CaTi(SiO4)O Description: Radioactive minerals have been reported |
| ⓘ 'Tourmaline' ? Formula: AD3G6(T6O18)(BO3)3X3Z |
| ⓘ Uraninite Formula: UO2 |
| ⓘ Zircon Formula: Zr(SiO4) Description: Radioactive minerals have been reported |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 2 - Sulphides and Sulfosalts | |||
|---|---|---|---|
| ⓘ | Pyrite | 2.EB.05a | FeS2 |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Magnetite | 4.BB.05 | Fe2+Fe3+2O4 |
| ⓘ | Corundum | 4.CB.05 | Al2O3 |
| ⓘ | Rutile | 4.DB.05 | TiO2 |
| ⓘ | Uraninite | 4.DL.05 | UO2 |
| Group 5 - Nitrates and Carbonates | |||
| ⓘ | Calcite | 5.AB.05 | CaCO3 |
| Group 9 - Silicates | |||
| ⓘ | Zircon | 9.AD.30 | Zr(SiO4) |
| ⓘ | Titanite | 9.AG.15 | CaTi(SiO4)O |
| ⓘ | Epidote | 9.BG.05a | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| ⓘ | Schorl ? | 9.CK.05 | NaFe2+3Al6(Si6O18)(BO3)3(OH)3(OH) |
| ⓘ | Muscovite | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
| Unclassified | |||
| ⓘ | 'Biotite' | - | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| ⓘ | 'Chlorite Group' | - | |
| ⓘ | 'Tourmaline' ? | - | AD3G6(T6O18)(BO3)3X3Z |
| ⓘ | 'Scapolite' | - | |
| ⓘ | 'Hornblende Root Name Group' | - | ◻Ca2(C2+4C3+)(AlSi7O22)W2 |
| ⓘ | 'Pyroxene Group' | - | ADSi2O6 |
| ⓘ | 'Calcium Amphibole Subgroup' | - | AnCa2(C2+5-mC3+m)(Si8-(n+m)Al(n+m))W2 |
| ⓘ | 'Allanite Group' | - | (A12+REE3+)(M13+M23+M32+)O[Si2O7][SiO4](OH) |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| H | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| H | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| H | ⓘ Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
| H | ⓘ Allanite Group | (A12+REE3+)(M13+M23+M32+)O[Si2O7][SiO4](OH) |
| B | Boron | |
| B | ⓘ Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
| B | ⓘ Tourmaline | AD3G6(T6O18)(BO3)3X3Z |
| C | Carbon | |
| C | ⓘ Calcite | CaCO3 |
| O | Oxygen | |
| O | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| O | ⓘ Calcite | CaCO3 |
| O | ⓘ Corundum | Al2O3 |
| O | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| O | ⓘ Magnetite | Fe2+Fe23+O4 |
| O | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| O | ⓘ Rutile | TiO2 |
| O | ⓘ Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
| O | ⓘ Titanite | CaTi(SiO4)O |
| O | ⓘ Tourmaline | AD3G6(T6O18)(BO3)3X3Z |
| O | ⓘ Uraninite | UO2 |
| O | ⓘ Zircon | Zr(SiO4) |
| O | ⓘ Hornblende Root Name Group | ◻Ca2(C42+C3+)(AlSi7O22)W2 |
| O | ⓘ Pyroxene Group | ADSi2O6 |
| O | ⓘ Allanite Group | (A12+REE3+)(M13+M23+M32+)O[Si2O7][SiO4](OH) |
| F | Fluorine | |
| F | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Na | Sodium | |
| Na | ⓘ Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
| Mg | Magnesium | |
| Mg | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Al | Aluminium | |
| Al | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Al | ⓘ Corundum | Al2O3 |
| Al | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| Al | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Al | ⓘ Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
| Al | ⓘ Hornblende Root Name Group | ◻Ca2(C42+C3+)(AlSi7O22)W2 |
| Al | ⓘ Calcium Amphibole Subgroup | AnCa2(C2+5-mCm3+)(Si8-(n+m)Al(n+m))W2 |
| Si | Silicon | |
| Si | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Si | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| Si | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Si | ⓘ Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
| Si | ⓘ Titanite | CaTi(SiO4)O |
| Si | ⓘ Zircon | Zr(SiO4) |
| Si | ⓘ Hornblende Root Name Group | ◻Ca2(C42+C3+)(AlSi7O22)W2 |
| Si | ⓘ Pyroxene Group | ADSi2O6 |
| Si | ⓘ Calcium Amphibole Subgroup | AnCa2(C2+5-mCm3+)(Si8-(n+m)Al(n+m))W2 |
| Si | ⓘ Allanite Group | (A12+REE3+)(M13+M23+M32+)O[Si2O7][SiO4](OH) |
| S | Sulfur | |
| S | ⓘ Pyrite | FeS2 |
| K | Potassium | |
| K | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| K | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Ca | Calcium | |
| Ca | ⓘ Calcite | CaCO3 |
| Ca | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| Ca | ⓘ Titanite | CaTi(SiO4)O |
| Ca | ⓘ Hornblende Root Name Group | ◻Ca2(C42+C3+)(AlSi7O22)W2 |
| Ca | ⓘ Calcium Amphibole Subgroup | AnCa2(C2+5-mCm3+)(Si8-(n+m)Al(n+m))W2 |
| Ti | Titanium | |
| Ti | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Ti | ⓘ Rutile | TiO2 |
| Ti | ⓘ Titanite | CaTi(SiO4)O |
| Fe | Iron | |
| Fe | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Fe | ⓘ Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) |
| Fe | ⓘ Magnetite | Fe2+Fe23+O4 |
| Fe | ⓘ Pyrite | FeS2 |
| Fe | ⓘ Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
| Zr | Zirconium | |
| Zr | ⓘ Zircon | Zr(SiO4) |
| U | Uranium | |
| U | ⓘ Uraninite | UO2 |
Mindat Articles
Hunting for Corundum & other minerals at the Burgess Mine, Ontario by Michael AdamowiczOther Regions, Features and Areas containing this locality
Canada
- Ontario
- Bancroft areaMineral Occurrence Area
North AmericaContinent
North America PlateTectonic Plate
- Granite-Rhyolite ProvinceMagmatic Province
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Burgess Mine, Carlow Township, Hastings County, Ontario, Canada