Appendix 34.1

Appendix 34.1 Summary of Available Data for Selected Industrial (Nonmetallic) Mineral Deposits in the Western Canada Sedimentary Basin

Note: Deposits in this table are listed in alphabetical order by major commodity; and second (i.e., within commodities), sequentially in order of NTS grid number and latitude-longitude location, which results in a geographic arrangement generally from southeast to northwest. ID numbers with an asterisk (*) indicate deposits or occurrences that have not been plotted on Figure 34.5 because of overcrowding of deposit symbols.

 

IDNameNTSLat.(N) Long.(W) Deg. Min. Sec.CommoditiesGeological descriptionReserves, resources or development workReference(s)
M1Thornhill62G49 13 19 98 12 14BentoniteCretaceous Vermillion River Fm. M.I. 62G/1 BNT 1
S4Tuax-Avonlea72H49 55 24 104 57 06Bentonite (Swelling)Late Cretaceous Bearpaw Fm.Estimated reserves in excess of 10 million tonsMonea (1984); Guliov and Buller (1987); S.E.M. Assessment Files 73H15-0001 to 73H15-0008, Truax Area; Brady (1962)
A5Drumheller82P51 28 54 112 42 40BentoniteUpper Cretaceous Horseshoe Canyon bentonite, light olive gray through olive gray to dusky brown, massive, waxy, slightly silty, breaks into pieces <25cm square, thick overburden. Scafe (1975); Babet (1966); Byrne (1955)
A7Rosalind83A52 39 34 112 26 20BentoniteBentonite deposit in Upper Cretaceous Horseshoe Canyon Fm., 2.7-3.3m thick, main zone 166m wide and 1.2km long, individual seams up to 0.33m thick, thin overburdens; the bentonites exhibit good to excellent yields, low grit content.Estimated reserves more than 1 million tons. Production started in 1959, has continued sinceScafe (1975); Babet (1966); ARC Econ. Mins. Files; Ross (1964); Anderson and Plein (1962)
A8McLeod River83F53 27 40 116 38 35BentonitePaleocene/U. Cretaceous Saunders Gp. bentonite, 2-2.7m thick, almost pure white; 7m thick overburdenSmall quantity was mined for cosmetic use in the 1930'sScafe (1975); Babet (1966); ARC Econ. Mins. Files; Ross (1964); Byrne (1955); Allan (1931)
A9Onoway83G53 49 29 114 17 09BentoniteUpper Cretaceous Horseshoe Canyon Fm. bentonite, in scattered lenses up to 1.7m thick, greenish cream, thin overburden; fair discontinuity of bedsEstimated reserves more than 300,000 tons. Production low, intermittent, started in 1960Scafe (1975); Babet (1966); Ross (1964)
M2Kildonan62I50 00 00 97 14 00Clay - expandableStratified blue clay deposit Bamburak (pers. comm., 1990)
M3Ste. Rose du Lac62J50 59 38 99 29 57Clay - brickLower Cretaceous Swan River Fm. M.I. 62J/13 SNL 2
A12Cypress Hills72E49 32 44 110 10 25Clay - stoneware/refractoryQuarry 66 (IXL). Upper Cretaceous Whitemud Fm. 3.6m light-med. grayy clay with 0.6m kaolinitic sand at base of Whitemud Hamilton, Scafe and Laidler (1988)
A14Cypress Hills, Eagle Butte72E49 37 58 110 29 23Clay - stonewareQuarry 45 (IXL). Upper Cretaceous Whitemud Fm.; light gray and dark brown shale with 2ft. of pale gray sandstone at top; total thickness 20ft. section Crockford (1951); Hamilton, Scafe and Laidler (1988)
A16Cypress Hills, Fly Lake72E49 39 43 110 22 36Clay - stonewareQuarry 34 (IXL). Kaolinitic sand unit, 2-3m thick, in Upper Cretaceous Whitemud Fm. Crockford (1951); Hamilton, Scafe and Laidler (1988)
A19Dunmore72E49 58 04 110 36 25Clay - brickClay deposit in Upper Cretaceous Judith River Fm.; 2m of black clay with numerous plant remains overlain by gray, sandy clay and underlain by buff clay; clay beds lenticularProduction started by Alberta Clay Products Company in 1911Ries and Keele (1912); Ries and Keele (1913); Scafe (1991)
S12Ravenscrag Butte72F49 28 48 109 01 56Clay - stonewareUpper Cretaceous Whitemud FormationUnknownWorcester (1950)
S13Ravenscrag72F49 28 48 109 10 00Clay - stonewareUpper Cretaceous Whitemud FormationUnknownWorcester (1950)
S14Eastend72F49 31 19 108 54 02
and
49 34 02 108 46 58
Clay - stoneware, refractory; kaolinUpper Cretaceous Whitemud FormationUnknownWorcester (1950); Crawford and Carlson (1953); Davis (1918); Carlson and Babey (1955); McLearn and McMahon (1933); Alcan International Ltd. (1977); Brady (1962); Pruett (1988); S.E.M. Assessment Files for NTS 72F,G,H for kaolin, clay; Lindoe (1965)
S15Rockglen72G49 13 05 106 12 24Clay - stonewareTertiary (Paleocene) Ravenscrag Formation (Willow Bunch Member)UnknownWorcester (1950); Field and Hudson (1979)
S16Gollier Creek72G49 23 34 106 12 24Clay - kaolin, ball, stonewareUpper Cretaceous Whitemud FormationEstimated geological reserves of kaolinized sediments 375 million tonsWorcester (1950); Crawford and Carlson (1953); McLearn and McMahon (1933); Albon (1957); master (1987); Spyker et al. (1954)
S17Wood Mountain72G49 23 34 106 20 28Clay - kaolin, ball, stonewareUpper Cretaceous Whitemud FormationEstimated geological reserves of kaolinized sediments 375 million tonsWorcester (1950); Crawford and Carlson (1953); McLearn and McMahon (1933); Albon (1957); master (1987); Spyker et al. (1954)
IDNameNTSLat.(N) Long.(W) Deg. Min. Sec.CommoditiesGeological descriptionReserves, resources or development workReference(s)
S18Fir Mountain Area72G49 23 34 106 28 33Clay - kaolin, ball, stonewareUpper Cretaceous Whitemud FormationEstimated geological reserves of kaolinized sediments 375 million tonsWorcester (1950); Crawford and Carlson (1953); McLearn and McMahon (1933); Albon (1957); Master (1987); Spyker et al. (1954)
S29Dirt Hills72I50 00 13 105 12 49Clay - refractoryUpper Cretaceous Whitemud Formation, kaolinized sands and associated plastic kaolinitic clayUnknownWorcester (1950); Davis (1918); Ries and Keele (1913); Byers (1969)
S30Cactus Hills72I50 05 27 105 29 11Clay - refractoryUpper Cretaceous Whitemud Formation, kaolinized sands and associated plastic kaolinitic clayUnknownWorcester (1950); Davis (1918); Ries and Keele (1913); Byers (1969)
S31Regina72I50 26 26 104 41 13Clay - expandableGlacial Lake claysReserves reported as abundantSacuta (1956); Davis (1918); Ries and Keele (1913)
A20Redcliff72L50 04 10 110 47 20Clay - brickUpper Cretaceous Oldman (?) Fm. shales; 1) yellow 3-4 m bed; 2) dark gray 2m bed; 3)light buff, sandy 1.5m bed Ries and Keele (1912); Scafe (1991)
S37Saskatoon - Sutherlane73B52 10 55 106 34 18Clay - expandableGlacial lake clay depositsNot availableSacuta (1956); Carlson and Babey (1955)
A31Blairmore82G49 36 14 114 26 27Clay - brickJurassic Fernie Fm. shales: dark grey shale, marine, fossiliferous; dark brown shale, very calcareous, formerly used in making cement Crockford (1951); Scafe (1991)
A35Taber82H49 49 20 112 08 18Clay - brickShale in Upper Cretaceous Judith River Fm. dark and somewhat gypsiferous, about 1m thick, underlies lignite seam, very plastic, smooth Ries and Keele (1913); Scafe (1991)
A43*Sandstone82J50 45 14 114 02 08Clay - brickShales in Paleocene Porcupine Hills Fm: gray and blue shale mixture as used for brick making, calcerous; black through yellowish green shales, some carbonate and sand, ~6m greenish gray shales with sandstone interbeds to 0.6m thick, some carbonate Ries and Keele (1913); Scafe (1991)
A44DeWinston82J50 49 36 114 00 44Clay - expandableMudstones, light olive gray to olive gray, 0.30-3m, massive, minor silt, noncalcerous Tertiary Paskapoo and Porcupine Hills fms. Scafe (1980); Scafe (1991)
A46*Brickburn82O51 03 34 114 09 07Clay - brickApproximately 5.4 m of Paleocene Porcupine Hills Fm. shale, gray green, sandy, interbedded sandstone Ries and Keele (1912)
A47Calgary - Bow River A82O51 03 34 114 10 30Clay - brickPaleocene Porcupine Hills Fm. shale, buff to greenish brown, some grit, 7 m thick, with two major sandstone interbeds, some calcareous bands Worcester (1932
A48*Calgary - Bow River B82O51 04 27 114 10 30Clay - brickApproximately 5.5m of Paleocene Porcupine Hills Fm. shale buff to greenish brown, gritty; 2-4m overburden Worcester (1932)
A49*Lac des Arcs82O51 04 27 115 10 31Clay - shaleImpure shaly limestone and shale, in places dolomitic, in Mississippian Banff Fm. Holter (1976); goudge (1945); Fox (1981)
A50Exshaw (Seebe)82O51 05 19 115 04 56Clay - shaleQuarry in section of Upper Cretaceous Wapiabi Fm. dark gray silty shale, lower part of Wapiti Fm; about 15m exposed in pit Scafe (1978); Fox (1981); Scafe (1991)
A51Cochrane82O51 11 26 114 28 39Clay - brickDark gray calcareous clay in Paleocene Porcupine Hills Fm; very plastic Ries and Keele (1912); Ries (1915); ARC Econ. Mins. Files (1948); Scafe (1991)
A53*Innisfail83A52 01 09 113 56 36Clay - brickPleistocene clay comprising alternate bands of sand, silty clay and stiff clay, in horizontal layers 15-30cms thick Keele (1915)
A55Red Deer83A52 16 00 113 27 52Clay - brickPleistocene clay, sandy, laminated, calcareous, less than 2m thick; overlies less than 1m of yellowish, jointed, silty clay Ries and Keele (1912)
A65Vegreville83H53 29 23 112 03 25Clay - brickPleistocene clay, brownish, noncalcareous, very sandy Keele (1915)
A67South Edmonton83H53 31 08 113 31 54Clay - brickPleistocene glacial clay of considerable extent Ries and Keele (1912)
A69*North Edmonton83H53 35 30 113 37 48Clay - brickPleistocene clay, yellow, very sandy, dense, some gypsum, approx. 4.5m thickUsed for common brickRies and Keele (1913)
A71Edmonton NW (St. Albert)83H53 38 59 113 40 45Clay - expandableClay, Pleistocene glacial lacustrine, olive gray, slightly silty, calcareous Scafe (1978); Scafe (1991)
IDNameNTSLat.(N) Long.(W) Deg. Min. Sec.CommoditiesGeological descriptionReserves, resources or development workReference(s)
A72Namao83H53 45 05 113 32 10Clay - expandableUpper Cretaceous Wapiti shale, olive gray, slightly silty, noncalcareous, gradational lower contact, about 0.25m; over shale, dusky yellowish brown, noncalcareous, ironstone nodules at contact with a siltstone above Scafe (1991)
A73Smoky Lake83I54 07 46 112 27 58Clay - brickUpper Cretaceous Belly River (?) clay, yellowish, sandy; 1.2m thick bedUsed for making stiff-mud brickAllan (1921); Hamilton and Babet (1975)
A74Athabasca83I54 41 49 113 16 07Clay - brickPleistocene glacial lacustrine clay, brownish gray, very calcareousBlended with other local clays for brickARC Econ. Mins. Files; Scafe (1991)
A76Grande Prairie83M55 08 56 118 48 25Clay - brickPleistocene clay, yellowish, silty calcareousUsed for sand mould brickAllan and Carr (1946); Scafe (1991)
M5Poplarfield62I50 54 20 97 40 17DolomiteSilurian Interlake Group M.I. 62I/13 DOL 2
M6Rosehill62O51 04 57 98 39 22DolomiteDevonian Winnipegosis Fm. M.I. 62O/2 DOL 1
M7Grand Rapids63G53 08 51 99 17 25DolomiteSilurian Atikameg and Moose Lake fms. M.I 63G/3 DOL 1
M8Paterson63J54 27 25 99 57 27Dolomite - dimension stoneOrdovician Stony Mountain Fm. M.I. 63K/8 STN 1
M9Cormorant Lake63K54 11 43 100 32 10Dolomite - dimension stoneOrdovician Stony Mountain Fm. M.I. 63K/2 STN 1
S41Deschambault - Limestone Lakes63L54 39 30 103 25 00Dolomite - dimension stoneOrdovician Red River Formation high density dolomiteExtensive resource, limited quarrying for building stoneKupsch (1952); Mysyk (1985); Guliov (1989)
A80Crowsnest Lake82G49 37 40 114 38 08DolomiteUpper part of Devonian-Fairholme Group. Gray dolomite outcrop on small knoll south of highway; 30m thickness exposedSize of deposit: mediumHolter (1976)
A82Castle Mountain82O51 15 48 115 53 47DolomiteCambrian Eldon Fm. dolomite, dark blue-gray, fine grained, pure dolomiteSmall quarry. 55.48% CaCo3; 44.17% MgCo3Goudge (1945)
A88Brooks72L50 33 00 111 53 40Formation brine - calcium chlorideFormation water from Upper Devonian Beaverhill Lake Fm, is the brine source; consists of about 3 parts Ca to 1 part NaFormation reservoir properties unknown; size of deposit: large; production not reportedHamilton (1969); Holter (1970)
S44PCS Cory73B52 06 00 106 47 21 (Mine shaft Location)Formation brine - calcium chlorideMiddle Devonian, Prairie Formation sylvite mineralization in marine evaporiteNot availableHolter (1969); Furzesy (1982); Buchinski (1988)
A89Drumheller82P51 23 39 112 34 14Formation brine - calcium chlorideFormation water from Upper Devonian Beaverhill Lake Fm.; well depth 1,666.7mSize of deposit: large; operation began in mid-1981Pers. comm. (General Chemicals)
A90Slave Lake83O55 15 54 114 17 45Formation brine - calcium chlorideFormation brine field in M. Devonian Keg River Fm. Producing zone 1685-1693m; well depth 1736mProducts are: 77% CaCl2 flake; 90% CaCl2 flake; 35% CaCl2 brinePers. comm. (Tiger Chemicals)
A91Calling Lake83P55 10 38 113 13 23Formation brine - calcium chlorideM. Devonian Keg River Fm.; depth of well about 1,500m; top of Keg River Fm. 1363mVariable production; plant capacity 800cu.m/day; one well producingPers. comm (Ward Chemicals)
A92St. Mary River82H49 30 07 112 57 11GemstoneAmmonites in Upper Cretaceous Bearspaw Fm.; have undergone unique metamorphosis resulting in brilliantly coloured gemstones known as Ammolite; ammonites found in ironstone occurrences in tight shale beds impervious to moistureEstimated over 1 billion ammonites to be found under Alberta Plains; Korite Limited is only currently active mineVandervelde (1992); Wilson (1984)
M11Silver Plains62H49 27 30 97 15 00GypsumSubsurface deposit, in Jurassic Amaranth Fm., underground mining to 100m depth from 1964-75 M.I 62H/6 GYP 1
M12Amaranth62J50 33 03 98 46 28GypsumJurassic Amaranth Fm.Combined production 100,000 tpaM.I. 62J/10 GYP 1, GYP2
M13Gypsumville62O51 47 51 98 31 40GypsumJurassic Amaranth Fm., infills Lake St. Martin crater, 10m or more in thickness, overburden <2m M.I. 62O/15 GYP 1, GYP 4
B11Lussier River - Coyote Creek82J/450 09 00 115 38 00GypsumIsolated occurrences of gypsum have been traced along both limbs of syncline between Lussier River and coyote Creek; anhydrite begins at 20-25m from surfacePotential estimate 20-40 million tonnes (SB); Production1990: 135,000 tonnes; total reserves calculated in 1984: 7 million tonnes of gypsumButrenchuk (1989b)
B13Elkhorn82J/550 28 00 115 52 00GypsumSouthern extension of Burnais Fm. Beds exploited by Windermere quarries10-20 million tonnes estimate (SB)Butrenchuk (1989b)
B14Windermere82J/1250 30 00 115 53 00GypsumGypsum occurs in a northwesterly trend along a strike; length of 5 km north and south of Windermere Creek; it is part of Devonian Burnais Formation; at depth of 20-40m from surface the gypsum turns into anhydrite.Production 1990: 410,000 tonnes; total production since 1950 is over 6.8 million tonnesButrenchuk (1989b)
IDNameNTSLat.(N) Long.(W) Deg. Min. Sec.CommoditiesGeological descriptionReserves, resources or development workReference(s)
A103Paintearth Mine (Tannathin)83A/852 25 36 112 11 57LeonarditeU.K. Horseshoe Canyon Fm., coal measures 45-70m above base; leonardite mined from bed 1.1m thick; carbonaceous humic-rich shale, used in drilling fluids.Mined from 1959-80; reported production 2.6Kt (mined as "coal")ARC Econ. Mins. Files; ERCB 88-45
M14Tyndall - Garson62I50 05 00 96 42 00Leonardite, dimension stoneOrdovician Red River Fm., dolomitic limestone in lower half Selkirk Member, 6.5-9m quarriable section, 2-4m overburdenNot availableM.I 62I/2 STN
M15Lily Bay Cement62J50 43 43 98 13 45LimestoneDevonian Elm Point Fm. M.I. 62J/16 LST 1
M16Spearhill62O51 19 09 98 22 34LimestoneDevonian Elm Point Fm. M.I. 62O/8 LST 1
M17Faulkner62O51 24 23 98 47 53LimestoneDevonian Elm Point Fm.300,000 tpaM.I. 62O/7 LST 2
M18Steep Rock62O51 26 53 98 48 03LimestoneDevonian Elm Point Fm., grades 95-99% CaCO3Not availableM.I. 62O/7 LST 1
M19Paradise Beach62O51 34 52 99 46 57LimestoneDevonian Dawson Bay Fm. M.I. 62O/12 LST 2
M20Mafeking63C52 48 13 101 09 44LimestoneDevonian Souris River Fm., grades 95-98% CaCO3 M.I. 63C/14 LST 1
A107Blairmore82G49 36 14 114 25 05LimestoneMississippian Banff Fm. limestone; 120m exposed; includes dark gray, medium crystalline dolomitic limestones with shale interbeds and abundant chart lensesAvg. CaCO3 67.39%; Avg. MgCO3 14.24%; Si02 17.09%Holter (1976)
A108Crowsnest Lake82G49 37 59 114 40 00LimestoneLimestone quarry in Mississippian Livingstone Fm. Consists of 37m thick high-grade limestone units, separated by 11m thick dolomitic limestone unitEstimated to contain 1.2 million tonnes of high purity limestone; at 1981 production levels, the quarry will be exhausted by 1994Macdonald and Hamilton (1981); Holter (1976); Goudge (1945)
A111Exshaw82O51 03 34 115 10 31LimestoneThe 33m of Devonian Palliser Fm. strata being quarried are relatively low in Mg and consist mainly of fine, brittle, fine grained dark gray, high Ca limestone together with minor beds that are mottled with dolomiteSize of deposit: largeHolter (1976); Goudge (1945)
A112Canmore82O51 03 34 115 16 06LimestoneMississipian Livingstone Fm., limestone; very fine-grained, dark bluish gray, in massive, indistinct beds flecked with tiny crystals of black calciteLarge operation started by Alberta Portland Cement Co. in 1906-1914Holter (1976); Goudge (1945)
A113Kananaskis QB82O51 04 47 115 07 33LimestoneCambrian Eldon Fm., composed of dark gray, finely crystalline variegated and mottled limestone and interbedded dolomite; the quarry is in steeply dipping bands of very light coloured limestone, which appear to run oblique to the beddingSize of deposit: mediumGoudge (1945), p.108 Hamilton (1987), p. 17-23; 34, 36,47,48. N.M.I. Record 115062
A114Corkscrew Mountain82O51 57 44 115 17 16LimestoneLimestone quarry in Shunda/Pekisko fms., MississipianSize of deposit: mediumHolter and Hamilton (1989)
A116Nordegg83C52 28 20 116 03 07LimestoneLimestone quarry in Mississipian Pekisko Fm.; three major units; 10m gray-weathering, dark gray to black, massive, coarse-grained, high-calcium limestone; underlain by 15-18m of magnesian limestone, over high-calcium limestone zoneSize of deposit: medium; quarry opened for ballast before 1944; presently worked for rip rapHolter (1976); Matthews (1961); Goudge (1945)
A117Henry House83D52 56 13 118 02 07Limestone43m of Devonian Palliser Fm. limestone in quarry; very fine grained, nearly black, in beds up to 2m thick; a few minor beds of mottled magnesian limestone observed, particularly in upper part of faceQuarry operated 1917 to 1930 for production of Portland CementGoudge (1945)
A121Cadomin83F53 00 38 117 19 33LimestoneLimestone deposit in Upper Devonian Palliser Fm,; thick-bedded, gray and blue, fine-grained, high-calcium limestone intercalated with beds containing magnesium carbonate in 10-20% MgCO3 rangeSize of deposit: large; proven reserves 22 million tonnesHolter (1976); Goudge (1945)
A122Roche Miette83F53 10 14 117 57 44LimestoneDevono-Carboniferous Mount Hawk Fm.(?) limestones; beds of high-calcium limestone, up to 12m thick, interbedded with beds of impure magnesian limestone, up to 13.7m thickQuarry formerly worked for lime productionGoudge (1945)
A123Jasper Gate83F53 13 43 117 48 57LimestoneQuarry in steeply dipping beds of Devonian Palliser Fm. limestones; high calcium rock, typically dark gray, massively bedded, finely crystalline, mottled and dolomitic in part; formation varies between 180 to 240m in thickness97% CaCO3; 3% MgCO3Holter (1976)
IDNameNTSLat.(N) Long.(W) Deg. Min. Sec.CommoditiesGeological descriptionReserves, resources or development workReference(s)
B18Baker Creek - Sukunka R.93P/455 09 09 121 55 02LimestoneLight gray limestone of the Mississippian Rundle Group, minimum width of 45mA short lived production in 1984/1985 for agriculture and highway construction - poor market conditions; reserves 40 million tonnes of chemical lime gradeFischl (1992)
B19Mount Brussilof82J/13E50 47 20 115 40 40MagnetiteSparry magnetite replacing dolomite of Middle Cambrian Cathedral Formation; deposit is part of the 15km long magnetite belt located adjacent and cast of the Cathedral paleo-escarpment9.5 million tonnes 95% Mg0; 13.6 million tonnes 93-95% MgO; 17.6 million tonnes 92% MgO; in calcined product; production 1990: 170,000 tonnesGrant (1987); MacLean (1988); Simandl and Hancock (1991)
A134Marlboro83F53 32 54 116 47 25MarlFluvial and lacustrine marl deposit, deposition since last deglaciation; the marl ranges from 1-2.75m thick with all C.E.E. values 74% and most 85%; generally the marl lies below the water table Govett and Byrne (1958); Holter (1970); Macdonald (1982)
A136Duffield83G53 25 55 114 17 00MarlAbandoned channel oxbow lake marl deposit, 0.5-3m thick; overburden 0.3m; lies 30m below surrounding upland and 3m above current river level; some sections of deposit well drained, while others are wetPoor-quality depositMacdonald (1982)
A142Halfway Lake83I54 09 31 113 30 57MarlMarl deposits in Recent glaciofluvial and glaciolacustrine sediments, found north of, in, and south of Halfway Lake; lake shallow with carbonate bottom; average C.C.E. 73-75% (1m thick)Large deposit; plant established in 1973 to produce cementMacdonald (1982); Holter (1972)
A143McGregor83J54 06 05 115 23 16MarlHillside seepage marl deposit; thickness ranges from 3.6m at center to 0.3m at margin; layers of peat interbedded with the non-tufaceous marl; C.C.E. values quite variable with most from 80-85%, with organic rich layers 40-60%; overburden 0.3mModerate size deposit, fair-good qualityMacdonald (1982)
A148Grimshaw84C56 06 31 117 38 33MarlDeposit is a mound of marl 13m high with numerous tufa fragments up to 30cm long; lensoidal in shape, max. thickness at center 4m, diameter 360m; samples up to 96.8% C.C.E., avg. 85%; avg. moisture content 20%, water table 3.5m below surfaceModerately large deposit; good quality; in 1976 some production and local sale as agricultural limeMacdonald (1982)
B34Crow82G/1049 39 45 114 42 30PhosphateA one metre thick phosphate of Fernie Formation repeated tectonically four times has 26.20% P205 and 757 ppm YConsistent bed, 1-2m thick (locally 2-3m), between 11% and 29% P205, averaging 17% P205; can be traced along strike for approx. 300km, the Y values on average are 650-700 ppm (occasionally may reach 1300 ppm in sample)Butrenchuk (in press); Macdonald (1987)
S56Rocanville62K50 27 45 101 32 33PotashMiddle Devonian Prairie Formation, sylvite mineralization in marine evaporiteNot AvailableHolter (!969); Fuzesy (1982)
S57Esterhazy62K50 38 25 101 51 18PotashMiddle Devonian Prairie Formation, sylvite mineralization and by-product salt from marine evaporiteNot AvailableHolter (!969); Fuzesy (1982)
S58Esterhazy62K50 43 43 101 59 40PotashMiddle Devonian Prairie Formation, sylvite mineralization and by-product salt from marine evaporiteNot AvailableHolter (!969); Fuzesy (1982)
S60Belle Plaine72I50 26 26 105 14 13PotashMiddle Devonian Prairie Formation, sylvite mineralization with haliteNot AvailableHolter (!969); Fuzesy (1982)
S61Allan72O51 55 32 106 04 28PotashMiddle Devonian Prairie Formation, sylvite mineralization and by-product salt from marine evaporiteNot AvailableHolter (!969); Fuzesy (1982)
S64Lanigan72P51 50 18 105 11 40PotashMiddle Devonian Prairie Formation, sylvite mineralizationNot AvailableHolter (!969); Fuzesy (1982)
S65Colonsay72P51 55 32 105 45 40PotashMiddle Devonian Prairie Formation, sylvite mineralization and by-product salt from marine evaporiteNot AvailableHolter (!969); Fuzesy (1982)
S66Cominco (Vanscoy)73B52 00 46 107 04 29PotashMiddle Devonian Prairie Formation, sylvite mineralization and by-product salt from marine evaporiteNot AvailableHolter (!969); Fuzesy (1982)
S67Patience Lake (Potash Company of America)73B52 06 00 106 21 39PotashMiddle Devonian Prairie Formation, sylvite mineralization and by-product salt from marine evaporiteNot AvailableHolter (!969); Fuzesy (1982)
S68PCS Cory73B52 06 00 106 47 21 (Mine Shaft Location)PotashMiddle Devonian Prairie Formation, sylvite mineralization and by-product salt from marine evaporiteNot AvailableHolter (!969); Fuzesy (1982)
S73Waldeck72J50 21 13 107 35 07PumiciteProbably Eocene-OligoceneUnknownWorcester (1950); Crawford (1955)
IDNameNTSLat.(N) Long.(W) Deg. Min. Sec.CommoditiesGeological descriptionReserves, resources or development workReference(s)
A166Willow Creek82J/150 07 36 114 08 25PumiciteRecent (?) age, filling surface depression along with organic muds and marks; ash bed about 0.4m thick, covered by 0.7m of black mud, 80% - 2000 meshSmall deposit, est. 1,000-1200 m3; excavated on small scale for use in cleansing compounds 1942-51ARC Econ. Mins. Files
B44Nicholson82N/2W51 12 40 116 51 33QuartziteMassive quartzite of the Ordovician Mount Wilson Formation, SiO2 99.85%; lump silica producer3 million tonnes (1985); Production 1990: 36,000 tonnesFoye (1987)
S74Esterhazy62K50 38 25 101 51 18
and
50 43 43 101 59 40
SaltMiddle Devonian Prairie Formation, sylvite mineralization and by-product salt from marine evaporiteNot availableHolter (1969); Fuzesy (1982)
S75Belle Plaine72I50 26 26 105 14 13SaltMiddle Devonian Prairie Formation, sylvite mineralization with haliteNot availableHolter (1969); Fuzesy (1982)
S76Saskatoon Chemicals (Weyerhaeuser)73B52 11 14 106 38 47Salt (NaCl)Middle Devonian, Prairie Formation salt bedsNot availableHolter (1969)
S77Unity73C52 26 57 109 05 54SaltMiddle Devonian Prairie FormationExtensive reservesHolter (1969)
A168Hughenden73D52 29 06 110 57 06Salt (storage)Mid-Devonian Upper Elk Point Fm. Prairie Evaporite. Salt interval: 4500'-4825' T.D.; cored: 4493'-4851'Salt cavern for underground storage of petroleum productsHamilton (1971); ERCB Well Files
A169Hardisty73D52 38 42 111 17 15Salt (storage)Mid-Devonian Upper Elk Point Fm. Prairie Evaporite. Salt interval: 4464'-4865' T.D., 4446'=4816' T.D., 4435'-4811' T.D., 4458'-4826' T.D.Salt cavern for underground storage of petroleum productsHamilton (1971); ERCB Well Files
A170Duvernay73E53 46 49 111 42 08SaltMid-Devonian Lower Elk Point Fm. Upper Lotsberg Salt. Salt interval: 4395'-4740'; cored 4403'-4736' Hamilton (1971); ERCB Well Files
A171Lindberg73E53 52 04 110 38 12SaltMid-Devonian Prairie Evaporite salt interval: 2631'-3073' T.D.; cored: 2631'-3073' Hamilton (1971)
A172Fort McMurray74D56 42 16 111 20 51SaltMid-Devonian Upper Elk Point Fm. Prairie Evaporite salt; salt interval: 723'-934'; cored 623'-934' Hamilton (1971); ERCB Well Files; Allan (1943)
A173Fort Saskatchewan83H53 44 12 113 11 21SaltMid-Devonian Lower Elk Point Fm.; salt interval: 6091' n.p.; cored: 6125'-27' Hamilton (1971)
A174*Fort Saskatchewan83H53 45 05 113 09 52Salt (storage)Mid-Devonian Lower Elk Point Fm. Upper Lotsberg salt, interval: 6080'-6332', cored 6214'-6304'; 6110'-6343', cored 6110'-6327'; 6091'-6326', cored 6122'-6326'; 6072'-6318', cored 6072'-6318'Salt cavern for underground storage of petroleum productsHamilton (1971); ERCB Well Files; Allan (1943)
A175Bruderheim A83H53 47 35 112 52 57SaltMid-Devonian Lower Elk Point Subgroup - Upper Lotsberg salt; salt interval 1751-1841 m; cored 1745-1769.5mSalt bringing operation for NaCLO3 manufacture; salt production capacity 50 KtpaARC Econ. Mins. Files
A176Bruderheim B83H53 48 01 112 53 41SaltMid-Devonian Lower Elk Point Subgroup - Upper Lotsberg salt; salt interval 1750-1840mSalt bringing operation for NaCLO3 manufacture; salt production capacity 50 KtpaARC Econ. Mins. Files
A177*Fort Saskatchewan83H53 48 34 113 08 22Salt (storage)Mid-Devonian Lower Elk Point Fm.; Upper Lotsberg salt; salt interval: 5985'-6232'Salt cavern for underground storage of petroleum productsHamilton (1971); ERCB Well Files; Allan (1943)
A178Redwater83H53 50 19 113 05 24Salt (storage)Mid-Devonian Lower Elk Point Fm. Upper Lotsberg salt; salt interval: 5804'-6062'; cored 5846'-6062'Salt cavern for underground storage of petroleum productsHamilton (1971); ERCB Well Files; Allan (1943)
A179Brocket82H49 32 44 113 48 35Sandstone - building stoneTertiary Paskapoo Fm. heavy sandstone, 7m thick; fine to medium gray with slightly brownish cast and with clean "peppery" appearance Parks (1916)
A180Porcupine Hills82H49 44 05 113 37 45Sandstone - building stoneTertiary Paskapoo Fm. sandstone, 4m thick; stone of external weathered zone uniform grayish colour, blue cores show in lower layersSmall amount quarriedParks (1916)
A181Monarch82H49 49 20 113 13 21Sandstone - building stoneTertiary Paskapoo Fm. sandstones, medium to fine grained, with distinctly blue colour; little reediness seen in specimen and stone is almost devoid of speckled appearance Parks (1916)
A182High River B82I50 30 23 113 47 48Sandstone - building stoneTertiary Paskapoo Fm. sandstone on banks of Little Bow river; stone medium grained, uniform grayish with yellowish green cast; little evidence of reedinessSmall amount quarriedParks (1916)
IDNameNTSLat.(N) Long.(W) Deg. Min. Sec.CommoditiesGeological descriptionReserves, resources or development workReference(s)
A183High River A82I50 34 45 113 53 39Sandstone - building stone15m bank of heavy sandstone in Tertiary Paskapoo Fm., covered with variable amount of drift; lenticular beds with pronounced crossbedding; medium-grained, uniform grayish sandstone with slightly yellowish green cast and little evidence of reedinessSmall amount quarriedParks (1916)
A184*High River C82I50 36 30 113 50 53Sandstone - building stoneTertiary Paskapoo Fm. sandstoneInconsiderable output used for foundationParks (1916)
A185Sandstone82J50 46 06 114 02 08Sandstone - building stoneSection of sandstone and shale beds in Tertiary Paskapoo Fm.; sandstone beds up to 1m thick; fine grained, light grayish colour with cast of yellow; some beds badly shattered with considerable amount of hardhead Parks (1916)
A186Pigeon Creek82O51 01 50 115 14 42Sandstone - dimension stoneDolomitic siltstone from Triassic Spray River Fm.; hard, flaggy, medium gray material known as "Rundle Rock"; contains lamination and beds ranging in thickness from 0.5cm to over 1mThunderstone Quarries opened in 1961; Rundle Rock sold as flagstone, dry pack sheets and landscaping stoneEdwards (1991) (Guidebook); Fox (1981)
A187*Calgary82O51 02 42 114 06 19Sandstone - building stoneTertiary Paskapoo Fm. sandstone; formation practically horizontal but beds lenticular; 1.8m sandstone in two variable beds (poor colour, used for rubble); 8.5m sandstone in beds up to 1.2m thick (avg. 6m good buff stone); 3m solid sandstone bedQuarry originally opened in 1902. Operations later prohibited by conditions under which land was sold for building lotsParks (1916)
A188*Brickburn82O51 03 34 114 09 07Sandstone - building stoneSection in Tertiary Paskapoo Fm. in river bank; 7.6m heavy bedded sandstone, pronounced lenticular character and irregular jointing; stone is fine grained and buff coloured toward top of sectionQuarry in operation 1910-1914Parks (1916)
A189Canmore82O51 07 57 115 23 05Sandstone - building stoneDolomitic siltstone from Triassic Spray River Fm; hard, flaggy, medium gray material known as "Rundle Rock"; contains lamination and beds ranging in thickness from 0.5cm to over 1mProduction of Rundle Rock building stone seasonal over past 35yrs.Fox (1981); Edwards (1991)
A190Rocky View82O51 08 49 114 04 56Sandstone - building stoneTertiary Paskapoo Fm. sandstone; section at greatest height of dome-shaped quarry face (10.5m): 6m tall soil, thin stone and shale; 3m buff sandstone; 1.2m hard blue sandstone; buff sandstone; formation is broken; differences in grain, in reedinessQuarries not worked since 1910Parks (1916)
A191*Glenbow82O51 09 41 114 23 04Sandstone - building stoneTertiary Paskapoo Fm. sandstone; 7.6m drift, thin stone and shale; 3m sandstone, partly in heavy beds; 0.6-1.5m shale; 6m sandstone, mostly heavy beds; stone essentially buff type but shows considerable variation in grain, colour, scaly structureExtensive quarrying till 1909; cessation in operation due to increase in blue hardhead and considerable overburdenParks (1916)
A192Cochrane82O51 12 18 114 28 39Sandstone - building stoneTertiary Paskapoo Fm. sandstone; quarry section: 3m soil, shale and thin sandstone; 2 m sandstone (mostly thin, with some good stone toward bottom); 6.4m sandstone in heavy beds with irregular partings.Large amount quarriedParks (1916)
A193Didsbury82O51 38 32 114 07 50Sandstone - building stoneTertiary Paskapoo Fm. sandstone; quarry section: 1.4m drift; 2m thin bedded stone; 1.2m heavy bedded stone; lower heavy bedded stone is divided by curved parting planes into lenticular beds; main joints 1.5m apart; medium to fine grained, grayQuarried on small scaleParks (1916)
A194Innisfail A82P51 58 32 113 43 45Sandstone - building stoneTertiary Paskapoo Fm. sandstone; upper 1.5m thin-bedded, lower part heavy bedded with irregular planes of parting; uniform bluish gray colourQuarried on small scaleParks (1916)
A195Innisfail B83A52 02 02 113 55 10Sandstone - building stoneTertiary Paskapoo Fm. sandstone exposure; upper 1.8m of stone thin bedded and shattered; lower stone in variable beds with lenticular planes of parting; fresh stone gray, weathers yellow; stone is fine grained, grayish with distinctly reedy structure Parks (1916)
A196Red Deer83A52 16 00 113 49 27Sandstone - building stoneTertiary Paskapoo Fm. sandstone; 4.5m drift over 2.4m exposed sandstone; beds horizontal but bedding planes not regular; avg. thickness about 25cm; weathered stone uniform gray with some evidence of reediness and false bedding Parks (1916)
IDNameNTSLat.(N)Long.(W) Deg. Min. Sec.CommoditiesGeological descriptionReserves, resources or development workReference(s)
A197Entwistle83G53 35 31 114 59 46Sandstone - building stoneTertiary Paskapoo and Edmonton Fm. sandstone; section: 6m drift; 8.5m blue and buff sandstone in fairly heavy, irregular beds, some hard, flinty bands; 9m gray sandstone, beds 25cm - 1m thick; stone coarse grained, uniform colour, little reediness Parks (1916)
M32Black Island62P51 15 00 96 23 00Silica sandOrdovician Winnepeg River Fm., high purity silica sandEstimated reserves 20 million t, quarry capacity 180,000 tpaM.I. 62P/1 SIA 1
S78Red Deer River63C52 58 42 101 44 34Silica sandEarly Cretaceous Mannville FormationEstimated 14 million tonnes reserve locally; production to date is minorBeck (1974); Babey (1955); Wickenden (1945); Collings and Andrews (1986, 1989); Northern Silica Limited (1968); Red Deer Silica Inc. (1986)
B46Mount Moberly82N/7W51 22 18 116 57 49Silica sandA friable phase of the Ordovician Mount Wilson Formation; at the mine site up to 200m thick, 99.5% SiO2, less than 0.1% Fe2-O2Geological reserves estimated at 10 million tonnes; production 1990: 90,000 tonnesFoye (1987)
A203Bruderheim83H53 51 11 112 55 00Silica sandUpper Pleistocene glacial outwash sand; post depositional modification has resulted in presence of thin film of iron oxide on sand grains, giving deposit a yellow colour88.79% of natural sand retained on 100-mesh sieveCarrigy (1970)
S83Sybouts Lake East72H49 02 14 104 24 29Sodium sulphateSaline lake deposit; permanent and intermittent crystal beds and brineOriginal reserve estimated at 3.5 million tons Na2SO4Cole (1926); Tomkins (1954); Last (1984)
S86Frederick Lake72H49 44 27 105 19 34Sodium sulphateSaline lake deposit; permanent crystal bed and brineOriginal reserve estimated at 3.7 million tons Na2SO4Cole (1926); Tomkins (1954); Last (1984)
S87Bishopric (Fredrick Lake)72I50 00 13 105 45 34Sodium sulphateSaline Lake; brine, intermittent and permanent crystal beds and brineOriginal reserve estimated at 2.4 million tons Na2SO4Cole (1926); Tomkins (1954); Last (1984)
S88Chaplin Lake72J50 21 13 106 37 23Sodium sulphateSaline Lake; brine with intermittent and permanent crystal bedsOriginal reserve estimated at 3 million tons Na2SO4Tomkins (1954); Last (1984)
S91Verlo72K5021 13 108 24 37Sodium sulphateSaline Lake deposit; permanent and intermittent crystal beds and brineOriginal reserve estimated at 950,000 tons Na2SO4Tomkins (1954); Worsley (1975)
S92Ingebright South72K5021 13 109 22 22Sodium sulphateSaline lake deposit; permanent crystal bedOriginal reserve estimated at 9 million tons Na2SO4Cole (1926); Tomkins (1954); Last (1984)
S94Snakehole Lake72K50 34 12 108 24 47Sodium sulphateSaline Lake deposit; permanent and intermittent crystal beds and brineOriginal reserve estimated at 1.7 million tons Na2SO4Cole (1926); Tomkins (1954); Last (1984)
S95Alsask72N51 18 52 109 52 15Sodium sulphateSaline lake brine and intermittent and permanent crystal bedsOriginal reserve estimated at 2.6 million tons Na2SO4Cole (1926); Tomkins (1954); Last (1984)
S98Berry Lake73A52 00 27 105 34 24Sodium sulphateSaline Lake deposit, crystal beds with intermittent brineEstimate reserves 800,000 tonsCole (1926); Tomkins (1954); Last (1984)
S102Whiteshore Lake73C52 06 06 108 17 07Sodium sulphateSaline lake deposit as brine and intermittent and permanent crystal bedsEstimated initial reserves of 6.5 million tons anhydrous saltCole (1926); Tomkins (1954)
A211Metiskow73D52 21 14 110 44 9Sodium sulphateLake Brine, contains about 11% sodium sulphate and about 12% sodium carbonate; permanent crystal bed, 6-10m thick over most of deposit, but over southern part of like is over 15m thickThe only Alberta deposit of commercial value; reserves about 3 million t; production began in mid-1969 for high purity sodium sulphate for use in detergents; production about 65,000 tpaBroughton (1976); Govett (1958); Cole (1926)
S104Steelman62E49 18 42 102 37 21SulphurSour gas fieldProduction 7Oilweek Jan. 21, 1991
S105Regina72I50 31 40 104 32 58Sulphur (by-product)By-products of heavy oil upgraderProduction 250 tonnes per day 
A214Fort McMurray74E57 00 33 111 29 39SulphurSulphur in crude bitumen extracted from Athabaska Oil Sands; Cret. McMurray Fm.; S content 5% by wieght of bitumenSulphur extraction plant; recovery capacity 441 tpd; reserves: 5.8 M tOilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18
A215Mildred Lake74E57 02 18 111 34 29SulphurSulphur in crude bitumen extracted from Athabaska Oil Sands; Cret. McMurray Fm.; S content 5% by wieght of bitumenSulphur extraction plant; recovery capacity 1255 tpd; reserves: 10.8 M tOilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18
A216Coleman (Savannah Creek)82G49 37 59 114 00 35SulphurSour gas field; producing zones: Miss. Rundle and Dev. Wabamun; H2S content 24%Sulphur extraction plant; recovery capacity 389 tpd; reserves: 2.5 M tOilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18
A217Waterton82G49 18 13 114 00 35SulphurSour gas field; producing zones: Miss. Rundle and Dev. Wabamun; H2S content 19%Sulphur extraction plant; recovery capacity 3,107 tpd; reserves: 7.3 M tOilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18
A218Mazeppa (Okotoks)82I50 38 34 113 46 54SulphurSour gas field; producing zones: Miss. Rundle and Dev. Wabamun; H2S content 36%Sulphur extraction plant; recovery capacity 577 tpdOilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18
A219Okotoks82I50 43 29 113 56 25SulphurSour gas field; producing zones: Miss. Rundle and Dev. Wabamun; H2S content 36%Sulphur extraction plant; recovery capacity 431 tpd; reserves : 2.1 M tOilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18
IDNameNTSLat.(N)Long.(W) Deg. Min. Sec.CommoditiesGeological descriptionReserves, resources or development workReference(s)
A220Turner Valley (Diamond)82J50 35 37 114 09 03SulphurSour gas field; producing zone: Miss. Rundle; H2S content 2.5%Sulphur extraction plant; recovery capacity 10.7 tpd; reserves not statedOilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18
A221Quirk Creek82J50 45 14 114 29 50SulphurSour gas field; producing zone: Miss. Rundle; H2S content 9%Sulphur extraction plant; recovery capactiy 299 tpd; reserves not statedOilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18
A222Jumping Pound82O51 07 57 114 34 14SulphurSour gas field; producing zone: Miss. Rundle; H2S content 6%Sulphur extraction plant; recovery capactiy 597 tpd; reserves: 2.8 M tOilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18
A223Wildcat Hills82O51 13 11 114 38 25SulphurSour gas field; producing zone: Miss. Rundle; H2S content 4%Sulphur extraction plant; recovery capactiy 177 tpd; reserves not statedOilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18
A224Crossfield E.82O51 23 41 114 02 09SulphurSour gas field; producing zone: Dev. Wabamun; H2S content 34%Sulphur extraction plant; recovery capactiy 1,797 tpd; reserves:2.2 M tOilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18
A225Carstairs - Crossfield82O51 32 25 114 12 00SulphurSour gas field; producing zone: Miss. Elkton; H2S content 0.5%Sulphur extraction plant; recovery capacity 65 tpdOilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18
A227Burnt Timber82O51 34 09 114 51 22SulphurSour gas field; producing zone: Miss. Rundle and Dev. Wabamun; H2S content 13%Sulphur extraction plant; recovery capacity 489 tpd reserves: 1.2 M tOilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18
A228Harmattan82O51 41 09 114 29 06SulphurSour gas field; producing zone: Miss. Rundle; H2S content 46%Sulphur extraction plant; recovery capacity 490 tpd. Reserves not statedOilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18
A229Olds82O51 44 39 114 07 50SulphurSour gas field; producing zone not stated; H2S content 15%Sulphur extraction plant; recovery capacity 389 tpd; reserves not statedOilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18
A230Bearberry82O51 53 23 114 48 56SulphurDevonian Leduc Fm., porous reef dolomite @4000m depth; "ultra sour" natural gas reservoir; H2S content 90%Demo plant, 204 tpd capacity; reserves 70 M -100 M tKitzan and Auger (1992)
A231Caroline82O51 56 00 114 31 56SulphurSour gas field; producing zones: Miss. Rundle and Dev. Beaverhill Lake; H2S content 0.8%Sulphur extraction plant; recovery capacity 8.3 tpd; reserves: 25 M tOilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18
A232Caroline - Swan Hills82O51 58 04 114 45 00SulphurDevonian Beaverhill Lake Fm., sour gas reservoir; H2S content 30-35%Plant design capacity 4000 tpd 1.4 M tpyOilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18
A233Innisfail82O51 58 37 114 03 37SulphurSour gas field; producing zone: Dev. Leduc; H2S content 16%Sulphur extraction plant, recovery capacity 163 tpd; reserves not statedOilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18
A234Caroline (Garrington)82O51 59 29 114 45 02SulphurSour gas field; producing zones -Miss. Rundle and Dev. Beaverhill LakeSulphur extraction plant; recovery capacity 10.4 tpdOilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18
A235Crossfield (Balzac)82P51 11 45 113 55 35SulphurSour gas field; producing zones: Cret. Mannville. Miss. Rundle and Dev. Wabamun ; H2S content 17%Sulphur extraction plant; recovery capacity 1696 tpd; reserves: 2.1 M tOilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18
A236Lone Pine Creek82P51 30 38 115 51 34SulphurSour gas field; producing zones: Dev. Wabamun and Leduc; H2S content 10%Sulphur extraction plant: recovery capacity 157 tpd; reserves not statedOilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18
A237Lone Pine Creek82P51 35 00 113 50 10SulphurSour gas field; producing zones; Dev. Wabamun and Leduc; H2S content 10%Sulphur extraction plant: recovery capacity 283 tpd; reserves not statedOilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18
A238Wimborne82P51 54 13 113 33 30SulphurSour gas field; producing zone: Dev. Leduc; H2S content 13%Sulphur extraction plant: recovery capacity 182 tpd; reserves not statedOilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18
A239Nevis83A52 18 37 113 05 11SulphurSour gas field; producing zone: Devonian; H2S content 4%Sulphur extraction plant; recovery capacity 197tpdOilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18
A240Joffre83A52 21 14 113 42 38SulphurSour gas field; producing zones; Cret. Mannville and Dev. Nisku; H2S content 3.4%Sulphur extraction plant: recovery capacity 25 tpd; reserves not statedOilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18
A242Ram River (Strachan)83B52 09 06 115 19 18SulphurSour gas field; producing zone: Dev. Leduc; H2S content 19%Sulphur extraction plant: recovery capacity 4,572 tpdOilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18
A243Strachan83B52 13 28 115 10 44SulphurSour gas field; producing zone: Dev. Leduc; H2S content 9%Sulphur extraction plant; recovery capacity 953 tpd; reserves: 0.8 M tOilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18
A244Homeglen Rimbey83B52 45 48 114 06 34SulphurSour gas field; producing zone: Dev. Leduc; H2S content 1%Sulphur extraction plant; recovery capacity 128 tpd; reserves not statedOilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18
A245Brazeau River (Nordegg)83B52 46 40 115 39 26SulphurSour gas field; producing zones: Miss. Elkton-Shunda, and Dev. Nisku; H2S content 1.3%Sulphur extraction plant; recovery capacity 42 tpd; reserves: 2.9 M tOilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18
A246Minnehik-Buck Lake83B52 56 17 114 50 06SulphurSour gas field; producing zone: Miss. Pekisko; H2S content 0.1%Sulphur extraction plant; recovery capacity 45 tpd; reserves not statedOilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18
IDNameNTSLat.(N) Long.(W) Deg. Min. Sec.CommoditiesGeological descriptionReserves, resources or development workReference(s)
A247Brazeau River83B52 56 36 115 54 07SulphurSour gas field; producing zones: Miss. Elkton-Shunda, and Dev. Nisku; H2S content 0.8%Sulphur extraction plant; recovery capacity 110 tpdOilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18
A248Hanlan-Robb83F53 12 57 116 48 27SulphurSour gas field; producing zones: Dev. Nisku and Beaverhill Lake; H2S content 9%Sulphur extraction plant; recovery capacity 1,092 tpd; reserves: 2.9 M tOilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18
A249Medicine Lodge83F53 28 32 117 02 10SulphurSour gas field; producing zone: Dev. Wabamun; H2S content ?Sulphur extraction plant; recovery capacity 45 tpd; reserves not statedOilweek, Jan. 21 1991;ERCB ST 91-18
A250Edson83F53 33 46 116 32 41SulphurSour gas field; producing zone: Miss. Elkton-Shunda; H2S content 1.4%Sulphur extraction plant; recovery capacity 288 tpd; reserves not statedOilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18
A251Rosevear83F53 39 00 116 06 08SulphurSour gas field; producing zone: Dev. Beaverhill Lake; H2S content 8%Sulphur extraction plant; recovery capacity 171 tpd; reserves not statedOilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18
A252Rosevear83F53 42 30 116 09 05SulphurSour gas field; producing zone: Dev. Beaverhill lake; H2S content 8%Sulphur extraction plant; recovery capacity 110 tpd; reserves not statedOilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18
A253West Pembina (Brazeau)83G53 02 22 115 57 48SulphurSour gas field; producing zones: Miss. Elkton-Shunda, and Dev. Nisku; H2S content ?Sulphur extraction plant; recovery capacity 520 tpd;Oilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18
A254Brazeau River83G53 11 06 115 44 38SulphurSour gas field; producing zones: Miss. Elkton-Shunda, and Dev. Nisku; H2S content 7%Sulphur extraction plant; recovery capacity 447 tpdOilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18
A255Bonnie Glen83H53 03 09 113 55 02SulphurSour gas field; producing zone:Dev. Leduc; H2S content 0.4%Sulphur extraction plant; recovery capacity 12.5 tpd; reserves not statedOilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18
A256Redwater83H53 57 18 113 05 24SulphurSour gas field; producing zone: Dev. Leduc; H2S content 2.6%Sulphur extraction plant; recovery capacity 11 tpd; reserves not statedOilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18
A257Kaybob S. III83K54 06 05 116 36 45SulphurSour gas field; producing zones: Trias., and Dev. Nisku and Beaverhill Lake; H2S content 16%Sulphur extraction plant; recovery capacity 3,557 tpd; reserves: 1.0 M tOilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18
A258Windfall-Whitecourt83K54 11 19 116 12 45SulphurSour gas field; producing zones: Cret. Mannville, Miss. Rundle, and Dev. Nisku and Leduc; H2S content 21%Sulphur extraction plant; recovery capacity 1m330 tpd; reserves: 3.2 M tOilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18
A259Bigstone83K54 15 40 117 12 44SulphurSour gas field; producing zone: Dev. Wabamun; H2S content 1.6%Sulphur extraction plant; recovery capacity 385 tpd; reserves not statedOilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18
A260Kaybob S.83K54 20 55 116 51 44SulphurSour gas field; producing zones: Cret. Mannville, Miss. Rundle, and Dev. Nisku and Leduc; H2S content 16%Sulphur extraction plant; recovery capacity 1,086 tpd; reserves not statedOilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18
A261Simonette83K54 25 17 117 46 08SulphurSour gas field; producing zones: Cret. Mannville, and Dev. Wabamun and Leduc; H2S content 16%Sulphur extraction plant; recovery capacity 95 tpd; reserves not statedOilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18
A262Sturgeon Lake83K54 56 42 117 14 32SulphurSour gas field; producing zone: Dev. Leduc; H2S content 9%Sulphur extraction plant; recovery capacity 98 tpd; reserves not statedOilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18
A263Gold Creek83L54 49 44 118 38 50SulphurSour gas field; producing zones: Cret. Mannville and Dev. Wabamun; H2S content 3%Sulphur extraction plant; recovery capacity 43 tpd; reserves not statedOilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18
A264Teepee Creek83M55 22 53 118 29 57SulphurSour gas field; producing zones: Trias. Doig, and Dev. Wabamun; H2S content 3%Sulphur extraction plant; recovery capacity 30 tpd; reserves not statedOilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18
A265Sinclair-Hythe83M55 24 38 119 49 57SulphurSour gas field; producing zones: Trias. Doig; H2S content 8%Sulphur extraction plant; recovery capacity 30 tpd; reserves not statedOilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18
A266Progress83M55 43 50 119 24 33SulphurSour gas field; producing zone: Trias. Halfway; H2S content 0.7%Sulphur extraction plant; recovery capacity 14 tpd; reserves not statedOilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18
A267Rainbow84L58 26 56 119 14 25SulphurSour gas field; producing zones: Dev. Slave Point and Keg River; H2S content 2%Sulphur extraction plant; recovery capacity 139 tpd; reserves not statedOilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18
A268Zama84M59 03 34 118 52 01SulphurSour gas field; producing zone: Dev. Elk Point; H2S content 8%Sulphur extraction plant; recovery capacity 74 tpd; reserves not statedOilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18
B47Pine River93P/555 17 00 121 38 00SulphurSour gas field1055 tpdOilweek, Jan. 21, 1991
B48Taylor Flats94A/256 06 58 120 53 50SulphurSour gas field, H2S content 3%460 tpdOilweek, Jan. 21, 1991
B49Cypress94B/1656 47 00 122 21 00SulphurSour gas field15 tpdOilweek, Jan. 21, 1991
B56Fort Nelson94J/1058 40 00 122 38 00SulphurSour gas field; H2S content 0.5-7%1100 tpdOilweek, Jan. 21, 1991