Lake Shore

Location: Teck Township
Years of Operation: 1918 – 1965, 1982 – 1987, 1997 – 1998
Tons Milled: 17,208,323
Ounces of Gold Produced: 8,602,791






Lake Shore Gold MineCopyright: G. Hamden

Lake Shore Gold Mine
Copyright: G. Hamden


Reproduced with permission of Kirkland Lake Gold Inc.

Lake Shore

The Lake Shore mine is located in the center of the Kirkland Lake camp bounded to the west by the Teck-Hughes mine and to the east by the Wright-Hargreaves mine. Lake Shore may be thought of as the “crown jewel” of the Kirkland Lake camp, for it was by far the largest gold producer, producing 8,499,199 ounces at a grade of 0.51 oz/T from continuous production from 1918 unti1 1965.

This is almost twice the total number of ounces produced from the neighboring second highest producer, Wright-Hargreaves, and represents 36% of the total ounces produced from the entire camp. Additional amounts were recovered from pillars in later years.

Harry Oakes discovered gold on claim L1557, in 1911. In 1913 Harry Oakes purchased the adjoining claim to the west (Ll6635). From 1914-1918 the No.1 Shaft was developed to 400 feet on the South (No.1) Vein Zone and 7,464 feet of underground development on levels at 100, 200, 300, and 400 feet was carried out. A 65-ton mill was installed and milling began in 1918. All work was carried out by Lake Shore Gold Mines Limited.

From 1919-1965 the mine was eventually serviced by four surface shafts and three internal shafts. The original No.1 Shaft and its extension were both inactive during the latter years of operations. The No.4 Shaft, collared at 4,325-foot level, took the workings to a depth of 8,150 feet. Underground development was carried out on 57 levels and, during the life of the mine, totaled 279,238 feet of drifting, 108,317 feet of crosscutting, and 154,547 feet of raising. Milling capacity was gradually increased to a maximum of 2,400 tons per day and production was continuous until the mine closed in July 1965. Ore from the Wright-Hargreaves Mine was treated at the Lake Shore mill from 1957 until the closure of that mine in March 1965.

High-grade ore material, on the bottom levels, was still being mined when the mine closed. Diamond drilling below these levels indicated that the ore continues and that the Main Break shows no signs of weakening at depth. Relatively low tonnage of ore at deeper levels and difficulties in mining at these extreme depths proved deepening of the mine workings to be uneconomical with the fixed gold prices of the day.

The Main Break and related sub-parallel structures strike continuously across the Lake Shore property but are offset by significant post-ore faulting along the Lake Shore fault at the east end of the property. Near surface, offset on this fault is 600-750 feet horizontally and about 325 feet vertically, with the east side moving down, and north, relative to the west side. The fault strikes about 012° and dips sub-vertically to the southeast. At deeper levels the fault appears as a strike fault and merges with the No.5 fault between the 6325 and 6825 foot levels. At the bottom levels of the mine, the strike of the fault follows the North vein.

The North, or No.2 vein is the most productive and extensive structure at Lake Shore. This structure is continuous from surface down to the 8075 foot level and has been traced by diamond drilling for 800 feet below this level. Between the 1200 and 4000 foot levels the Main Break branches into several faults. The North vein is the continuation of the Main Break at the west end of the property. At the east end of the property the Main Break is represented by the South, or No.1, vein which continues as the South vein on the Wright-Hargreaves property.

Mining on the North (No.2) vein was extensive throughout the mine. Of these zones, the area containing mixed syenite porphyry and augite syenite west of the shaft area from surface to the 5450 foot level was most productive. Occasionally sub-parallel veins were mined separately from this vein, but in places the veins are closely spaced and have been stoped together across widths up to 70 feet. Stoping was nearly continuous on the North vein from surface to the 5400 foot level where veining weakened considerably and stopped at the 6325 foot level. Another ore shoot continues below this from the 7575 foot level to the 8075 foot level, the bottom level of the mine. This ore shoot was traced by diamond drilling down to 8,500’ and showed no signs of weakening. The North vein on the 8075’ level was mined over an 807’ strike length at an average stoping width of 7.6’ and an average grade of 0.677 oz/T.

The South (No. I) vein was second in importance only to the North vein. This structure contains numerous branches and splays and related veining and is far less continuous than the North vein . The ore also was not as extensive with lower average stoping widths varying from 3 to 35 feet. Above the 1000 foot level, the South vein is regular and is sub-parallel to the North vein which is some 400 to 500 feet to the north. Below the 1000 foot level, the south vein is much less regular and less continuous until finally the ore bottoms out on the 6075 foot level.

Several subsidiary veins have also been mined in the ground adjacent to these main structures. Most of these veins occurred between the North and South veins, where they formed along tensional fractures related to fault movements.

Another significant structure, sub-parallel to the North vein, occurs some 1,200 to 1,600 feet to the north. It is referred to as the Narrows break, or No.3 vein zone, and has been drilled and explored on various levels down to the 5450 foot levels. While some high-grade intersections have been reported, no significant amounts of ore have been mined form this zone. This structure likely continues to the west and east and is called the ’05 break at the Macassa mine.

Mining at Lake Shore was almost entirely within intrusive rocks except in the upper levels of the mine to the 800 foot level, where ore was found in conglomerate on the north side of the North (No.2) vein. Most of the ore is hosted in syenite porphyry with augite syenite hosting some ore at the west end of the property. Syenite porphyry is the only rock type reported in the lower levels of the mine.

The above summary of the history of the Lake Shore Mine is taken from: STILL, A.C. 2001 Structural setting and controls of gold mineralization at the Macassa Mine, Kirkland Lake, Ontario. Unpublished Masters of Science Thesis, Queens University 151p.


Lake Shore Gold Mine

Lake Shore Gold Mine



Lake Shore Mine (Past Producer)

Partial history as of 1979


LOCATION:  Immediately  west  of  Kirkland  Lake,  in west-central  Teck  Township.  Patented  claims L1557,  L2606,  L2645,  L16633-L16635,  and L16726  and  patented  fractional  claims  L2242, L2243,  and  L2605.  No.1  Shaft  in  patented  claim L1557  and  No.3  Shaft  in  patented  claim  L2606. Latitude 48.150,  Longitude 80.050 . Map  reference:  ODM  1945-1,  Township  of Teck.

GEOLOGY: Shafts No.1  and No.3 were sunk at the west end of the main stock of Algoman syenite porphyry in  the  Kirkland  Lake  camp.  This  intrusive  body trends N650E, or approximately parallel to the vein system,  and  dips  steeply  south.  Because  the south contact has a shallower dip than the north boundary, the body widens with depth. West of the shaft sec tion,  it  interfingers with augite syenite and syenite and has an almost vertical plunge. This  area of complexly  intermingled  intrusives has been highly productive ground. The syenite porphy ry  is the predominant host rock of the veins in the mine  and  has  replaced  all  other  rock  types  in  the eastern  half  of  the  mine  and  on  the  lower  levels. Quartz-feldspar porphyry  is found as small irregular bodies within the syenite porphyry. A diabase dike occurs near the west boundary of the property and cuts  all  other  rock  types,  as  well  as veins and ore- bodies. This dike is nearly vertical and strikes rough ly  normal  to the veins. The main syenite porphyry intrusive and the interf ingered intrusives to the west are flanked by Timiskaming metasediments and tuffs. The  North  (No.2)  Vein  Zone, which  lies along the 176 main Kirkland  Lake Fault, is the strongest and most productive  structure  in the mine. The fracture pattern  associated  with it includes the less continuous South  (No.1)  Vein  Zone  and various diagonal vein fractures  lying  between  them.  This  broad  zone  of fracturing,  located  largely  on  the  Lake  Shore  pro perty,  is the result of the transfer of the main fault ing  movement from the North Vein  in the western part of the  camp  to the South Vein  in the eastern part.  The productive veins occur along the fracture system  described  above  and  are  found  in  all  rock types within the fractured zone except the diabase. The  veins  range  in  size  from  narrow  high-grade quartz  stringers  to  quartz  stockworks  and  quartz breccia bodies having widths up to 70 feet. Post-ore faults are well-defined planes of movement and may  be classified as strike faults, oblique faults, and cross faults. The most important post-ore fault is  a  steeply dipping cross fault, known  as the Lake Shore Fault, occurring near the east end of the mine. At  a  depth  of 3,000 feet, this fault splits into two branches.  The  effect  of  movement  along  these  is that the South (No.1) Vein, which was faulted from Lake  Shore ground into the Wright-Hargreaves pro perty  east of the  Lake  Shore  Fault,  is,  below the junction with  the  L  Fault, retained on  Lake Shore property several hundred feet farther east.

ECONOMIC FEATURES: An estimated 330,000 tons of ore  averaging 0.42 ounce  of Au  per ton remain  in the  old workings  above the 4,000-foot  level  (Nor thern  Miner,  July  11,  1974).  Diamond-drilling indicates  ore  grade  values  to  a  depth  of 400-feet below  the  8,075-foot  level  (bottom  level  of  the mine), but economic considerations have precluded further development.  There  are  3,302,460 tons of tailings slimes averaging 0.072 ounce of Au  per ton (Northern Miner, May 10, 1973).

OWNERSHIP: Lakeshore Mines Limited.

HISTORY:  1911:  Gold  discovered  in  claim  L1557  by Harry Oakes. 1913:  The  adjoining  claim  to  the west  (L16635) purchased by Harry Oakes. 1914-1918:  No.1  Shaft to 400 feet on  the South (No.1)  Vein  Zone  and  7,464 feet of underground development  on  levels  at  100,  200,  300,  and  400 feet.  A  65-ton mill was installed and milling begun in  1918.  All  work  by  Lake  Shore  Gold  Mines Limited. 1919-1965:  The  mine  was  eventually  serviced  by four  surface  shafts  and  three  internal  shafts.  The original  No.1  Shaft  and  its  extension  were  both inactive during  the  latter  years  of  operations.  The No.4  Shaft,  collared  at 4,325-foot  level,  took the workings  to  a  depth  of  8,150  feet.  Underground development  was  carried  out  on  57  levels  and, during  the  life of the  mine, totalled:  279,238 feet of drifting, 108,317 feet of crosscutting, and 154,547 feet  of  raising.  Milling  capacity  was  gradually  in creased  to  a  maximum of 2,400 tons  per day and production  was  continuous  until  the  mine  closed in  July  1965.  Ore  from  the  Wright-Hargreaves Mine was treated at the  Lake Shore mill from 1957 until the closure of that mine in March 1965. 1965-1968:  A small  amount of gold was produced through  mill  cleanup  in  1965.  A feasibility  study, carried out during the summer of  1965,  indicated that reprocessing of the mine tailings would be fea sible  at  a  rate of 1,500 to 2,000 tons per day.  Re processing was carried out during a  5-month period from  1966 to  1968,  when  it was decided that the price  of  gold  could  not  justify  the  cost  of  the operation.


Year Gold Silver Ore Milled Recovered Grade
(ounces) (ounces)  (tons) (ounce of Au per ton)
1918-1965 8,499,199 1,955,132 16,620,903 0.51


CIMM  1948,  Structural  Geology  of Canadian Ore Deposits, Vol.1, p.644-653.
Northern Miner, May 10, 1973; July 11, 1974.
ODM 1920, Vol.29, pt.4, p.33-36.
ODM 1928, Vol.37, pt.2, p.112-125.
ODM 1948, Vol.57, pt.5, p. 150-160.
ODM 1964, GC11, p.33-41.
ODM 1964, MRC3, p.47-49.
ODM 1965, Vol.75, p.35-37.
ODM 1968, Vol.78, p.21.
Resident  Geologist’s  Files, Ontario Ministry of Na tural Resources, Kirkland Lake

Gordon, J.B., Lovell, H.L., de Grijs, Jan, and Davie, R.F.
1979:  Gold  Deposits of Ontario,  Part  2:  Part of District of Cochrane,  Districts of Muskoka,  Nipissing,  Parry  Sound,  Sudbury,  Timiskaming,  and  Counties  of Southern  Ontario;  Ontario  Geological  Survey,  Mineral  Deposits  Circular  18,  253p.


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