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.
ID | Name | NTS | Lat.(N) Long.(W) Deg. Min. Sec. | Commodities | Geological description | Reserves, resources or development work | Reference(s) |
---|---|---|---|---|---|---|---|
M1 | Thornhill | 62G | 49 13 19 98 12 14 | Bentonite | Cretaceous Vermillion River Fm. | M.I. 62G/1 BNT 1 | |
S4 | Tuax-Avonlea | 72H | 49 55 24 104 57 06 | Bentonite (Swelling) | Late Cretaceous Bearpaw Fm. | Estimated reserves in excess of 10 million tons | Monea (1984); Guliov and Buller (1987); S.E.M. Assessment Files 73H15-0001 to 73H15-0008, Truax Area; Brady (1962) |
A5 | Drumheller | 82P | 51 28 54 112 42 40 | Bentonite | Upper 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) | |
A7 | Rosalind | 83A | 52 39 34 112 26 20 | Bentonite | Bentonite 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 since | Scafe (1975); Babet (1966); ARC Econ. Mins. Files; Ross (1964); Anderson and Plein (1962) |
A8 | McLeod River | 83F | 53 27 40 116 38 35 | Bentonite | Paleocene/U. Cretaceous Saunders Gp. bentonite, 2-2.7m thick, almost pure white; 7m thick overburden | Small quantity was mined for cosmetic use in the 1930's | Scafe (1975); Babet (1966); ARC Econ. Mins. Files; Ross (1964); Byrne (1955); Allan (1931) |
A9 | Onoway | 83G | 53 49 29 114 17 09 | Bentonite | Upper Cretaceous Horseshoe Canyon Fm. bentonite, in scattered lenses up to 1.7m thick, greenish cream, thin overburden; fair discontinuity of beds | Estimated reserves more than 300,000 tons. Production low, intermittent, started in 1960 | Scafe (1975); Babet (1966); Ross (1964) |
M2 | Kildonan | 62I | 50 00 00 97 14 00 | Clay - expandable | Stratified blue clay deposit | Bamburak (pers. comm., 1990) | |
M3 | Ste. Rose du Lac | 62J | 50 59 38 99 29 57 | Clay - brick | Lower Cretaceous Swan River Fm. | M.I. 62J/13 SNL 2 | |
A12 | Cypress Hills | 72E | 49 32 44 110 10 25 | Clay - stoneware/refractory | Quarry 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) | |
A14 | Cypress Hills, Eagle Butte | 72E | 49 37 58 110 29 23 | Clay - stoneware | Quarry 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) | |
A16 | Cypress Hills, Fly Lake | 72E | 49 39 43 110 22 36 | Clay - stoneware | Quarry 34 (IXL). Kaolinitic sand unit, 2-3m thick, in Upper Cretaceous Whitemud Fm. | Crockford (1951); Hamilton, Scafe and Laidler (1988) | |
A19 | Dunmore | 72E | 49 58 04 110 36 25 | Clay - brick | Clay 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 lenticular | Production started by Alberta Clay Products Company in 1911 | Ries and Keele (1912); Ries and Keele (1913); Scafe (1991) |
S12 | Ravenscrag Butte | 72F | 49 28 48 109 01 56 | Clay - stoneware | Upper Cretaceous Whitemud Formation | Unknown | Worcester (1950) |
S13 | Ravenscrag | 72F | 49 28 48 109 10 00 | Clay - stoneware | Upper Cretaceous Whitemud Formation | Unknown | Worcester (1950) |
S14 | Eastend | 72F | 49 31 19 108 54 02 and 49 34 02 108 46 58 | Clay - stoneware, refractory; kaolin | Upper Cretaceous Whitemud Formation | Unknown | Worcester (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) |
S15 | Rockglen | 72G | 49 13 05 106 12 24 | Clay - stoneware | Tertiary (Paleocene) Ravenscrag Formation (Willow Bunch Member) | Unknown | Worcester (1950); Field and Hudson (1979) |
S16 | Gollier Creek | 72G | 49 23 34 106 12 24 | Clay - kaolin, ball, stoneware | Upper Cretaceous Whitemud Formation | Estimated geological reserves of kaolinized sediments 375 million tons | Worcester (1950); Crawford and Carlson (1953); McLearn and McMahon (1933); Albon (1957); master (1987); Spyker et al. (1954) |
S17 | Wood Mountain | 72G | 49 23 34 106 20 28 | Clay - kaolin, ball, stoneware | Upper Cretaceous Whitemud Formation | Estimated geological reserves of kaolinized sediments 375 million tons | Worcester (1950); Crawford and Carlson (1953); McLearn and McMahon (1933); Albon (1957); master (1987); Spyker et al. (1954) |
ID | Name | NTS | Lat.(N) Long.(W) Deg. Min. Sec. | Commodities | Geological description | Reserves, resources or development work | Reference(s) |
---|---|---|---|---|---|---|---|
S18 | Fir Mountain Area | 72G | 49 23 34 106 28 33 | Clay - kaolin, ball, stoneware | Upper Cretaceous Whitemud Formation | Estimated geological reserves of kaolinized sediments 375 million tons | Worcester (1950); Crawford and Carlson (1953); McLearn and McMahon (1933); Albon (1957); Master (1987); Spyker et al. (1954) |
S29 | Dirt Hills | 72I | 50 00 13 105 12 49 | Clay - refractory | Upper Cretaceous Whitemud Formation, kaolinized sands and associated plastic kaolinitic clay | Unknown | Worcester (1950); Davis (1918); Ries and Keele (1913); Byers (1969) |
S30 | Cactus Hills | 72I | 50 05 27 105 29 11 | Clay - refractory | Upper Cretaceous Whitemud Formation, kaolinized sands and associated plastic kaolinitic clay | Unknown | Worcester (1950); Davis (1918); Ries and Keele (1913); Byers (1969) |
S31 | Regina | 72I | 50 26 26 104 41 13 | Clay - expandable | Glacial Lake clays | Reserves reported as abundant | Sacuta (1956); Davis (1918); Ries and Keele (1913) |
A20 | Redcliff | 72L | 50 04 10 110 47 20 | Clay - brick | Upper 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) | |
S37 | Saskatoon - Sutherlane | 73B | 52 10 55 106 34 18 | Clay - expandable | Glacial lake clay deposits | Not available | Sacuta (1956); Carlson and Babey (1955) |
A31 | Blairmore | 82G | 49 36 14 114 26 27 | Clay - brick | Jurassic Fernie Fm. shales: dark grey shale, marine, fossiliferous; dark brown shale, very calcareous, formerly used in making cement | Crockford (1951); Scafe (1991) | |
A35 | Taber | 82H | 49 49 20 112 08 18 | Clay - brick | Shale 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* | Sandstone | 82J | 50 45 14 114 02 08 | Clay - brick | Shales 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) | |
A44 | DeWinston | 82J | 50 49 36 114 00 44 | Clay - expandable | Mudstones, light olive gray to olive gray, 0.30-3m, massive, minor silt, noncalcerous Tertiary Paskapoo and Porcupine Hills fms. | Scafe (1980); Scafe (1991) | |
A46* | Brickburn | 82O | 51 03 34 114 09 07 | Clay - brick | Approximately 5.4 m of Paleocene Porcupine Hills Fm. shale, gray green, sandy, interbedded sandstone | Ries and Keele (1912) | |
A47 | Calgary - Bow River A | 82O | 51 03 34 114 10 30 | Clay - brick | Paleocene 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 B | 82O | 51 04 27 114 10 30 | Clay - brick | Approximately 5.5m of Paleocene Porcupine Hills Fm. shale buff to greenish brown, gritty; 2-4m overburden | Worcester (1932) | |
A49* | Lac des Arcs | 82O | 51 04 27 115 10 31 | Clay - shale | Impure shaly limestone and shale, in places dolomitic, in Mississippian Banff Fm. | Holter (1976); goudge (1945); Fox (1981) | |
A50 | Exshaw (Seebe) | 82O | 51 05 19 115 04 56 | Clay - shale | Quarry 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) | |
A51 | Cochrane | 82O | 51 11 26 114 28 39 | Clay - brick | Dark gray calcareous clay in Paleocene Porcupine Hills Fm; very plastic | Ries and Keele (1912); Ries (1915); ARC Econ. Mins. Files (1948); Scafe (1991) | |
A53* | Innisfail | 83A | 52 01 09 113 56 36 | Clay - brick | Pleistocene clay comprising alternate bands of sand, silty clay and stiff clay, in horizontal layers 15-30cms thick | Keele (1915) | |
A55 | Red Deer | 83A | 52 16 00 113 27 52 | Clay - brick | Pleistocene clay, sandy, laminated, calcareous, less than 2m thick; overlies less than 1m of yellowish, jointed, silty clay | Ries and Keele (1912) | |
A65 | Vegreville | 83H | 53 29 23 112 03 25 | Clay - brick | Pleistocene clay, brownish, noncalcareous, very sandy | Keele (1915) | |
A67 | South Edmonton | 83H | 53 31 08 113 31 54 | Clay - brick | Pleistocene glacial clay of considerable extent | Ries and Keele (1912) | |
A69* | North Edmonton | 83H | 53 35 30 113 37 48 | Clay - brick | Pleistocene clay, yellow, very sandy, dense, some gypsum, approx. 4.5m thick | Used for common brick | Ries and Keele (1913) |
A71 | Edmonton NW (St. Albert) | 83H | 53 38 59 113 40 45 | Clay - expandable | Clay, Pleistocene glacial lacustrine, olive gray, slightly silty, calcareous | Scafe (1978); Scafe (1991) |
ID | Name | NTS | Lat.(N) Long.(W) Deg. Min. Sec. | Commodities | Geological description | Reserves, resources or development work | Reference(s) |
---|---|---|---|---|---|---|---|
A72 | Namao | 83H | 53 45 05 113 32 10 | Clay - expandable | Upper 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) | |
A73 | Smoky Lake | 83I | 54 07 46 112 27 58 | Clay - brick | Upper Cretaceous Belly River (?) clay, yellowish, sandy; 1.2m thick bed | Used for making stiff-mud brick | Allan (1921); Hamilton and Babet (1975) |
A74 | Athabasca | 83I | 54 41 49 113 16 07 | Clay - brick | Pleistocene glacial lacustrine clay, brownish gray, very calcareous | Blended with other local clays for brick | ARC Econ. Mins. Files; Scafe (1991) |
A76 | Grande Prairie | 83M | 55 08 56 118 48 25 | Clay - brick | Pleistocene clay, yellowish, silty calcareous | Used for sand mould brick | Allan and Carr (1946); Scafe (1991) |
M5 | Poplarfield | 62I | 50 54 20 97 40 17 | Dolomite | Silurian Interlake Group | M.I. 62I/13 DOL 2 | |
M6 | Rosehill | 62O | 51 04 57 98 39 22 | Dolomite | Devonian Winnipegosis Fm. | M.I. 62O/2 DOL 1 | |
M7 | Grand Rapids | 63G | 53 08 51 99 17 25 | Dolomite | Silurian Atikameg and Moose Lake fms. | M.I 63G/3 DOL 1 | |
M8 | Paterson | 63J | 54 27 25 99 57 27 | Dolomite - dimension stone | Ordovician Stony Mountain Fm. | M.I. 63K/8 STN 1 | |
M9 | Cormorant Lake | 63K | 54 11 43 100 32 10 | Dolomite - dimension stone | Ordovician Stony Mountain Fm. | M.I. 63K/2 STN 1 | |
S41 | Deschambault - Limestone Lakes | 63L | 54 39 30 103 25 00 | Dolomite - dimension stone | Ordovician Red River Formation high density dolomite | Extensive resource, limited quarrying for building stone | Kupsch (1952); Mysyk (1985); Guliov (1989) |
A80 | Crowsnest Lake | 82G | 49 37 40 114 38 08 | Dolomite | Upper part of Devonian-Fairholme Group. Gray dolomite outcrop on small knoll south of highway; 30m thickness exposed | Size of deposit: medium | Holter (1976) |
A82 | Castle Mountain | 82O | 51 15 48 115 53 47 | Dolomite | Cambrian Eldon Fm. dolomite, dark blue-gray, fine grained, pure dolomite | Small quarry. 55.48% CaCo3; 44.17% MgCo3 | Goudge (1945) |
A88 | Brooks | 72L | 50 33 00 111 53 40 | Formation brine - calcium chloride | Formation water from Upper Devonian Beaverhill Lake Fm, is the brine source; consists of about 3 parts Ca to 1 part Na | Formation reservoir properties unknown; size of deposit: large; production not reported | Hamilton (1969); Holter (1970) |
S44 | PCS Cory | 73B | 52 06 00 106 47 21 (Mine shaft Location) | Formation brine - calcium chloride | Middle Devonian, Prairie Formation sylvite mineralization in marine evaporite | Not available | Holter (1969); Furzesy (1982); Buchinski (1988) |
A89 | Drumheller | 82P | 51 23 39 112 34 14 | Formation brine - calcium chloride | Formation water from Upper Devonian Beaverhill Lake Fm.; well depth 1,666.7m | Size of deposit: large; operation began in mid-1981 | Pers. comm. (General Chemicals) |
A90 | Slave Lake | 83O | 55 15 54 114 17 45 | Formation brine - calcium chloride | Formation brine field in M. Devonian Keg River Fm. Producing zone 1685-1693m; well depth 1736m | Products are: 77% CaCl2 flake; 90% CaCl2 flake; 35% CaCl2 brine | Pers. comm. (Tiger Chemicals) |
A91 | Calling Lake | 83P | 55 10 38 113 13 23 | Formation brine - calcium chloride | M. Devonian Keg River Fm.; depth of well about 1,500m; top of Keg River Fm. 1363m | Variable production; plant capacity 800cu.m/day; one well producing | Pers. comm (Ward Chemicals) |
A92 | St. Mary River | 82H | 49 30 07 112 57 11 | Gemstone | Ammonites 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 moisture | Estimated over 1 billion ammonites to be found under Alberta Plains; Korite Limited is only currently active mine | Vandervelde (1992); Wilson (1984) |
M11 | Silver Plains | 62H | 49 27 30 97 15 00 | Gypsum | Subsurface deposit, in Jurassic Amaranth Fm., underground mining to 100m depth from 1964-75 | M.I 62H/6 GYP 1 | |
M12 | Amaranth | 62J | 50 33 03 98 46 28 | Gypsum | Jurassic Amaranth Fm. | Combined production 100,000 tpa | M.I. 62J/10 GYP 1, GYP2 |
M13 | Gypsumville | 62O | 51 47 51 98 31 40 | Gypsum | Jurassic Amaranth Fm., infills Lake St. Martin crater, 10m or more in thickness, overburden <2m | M.I. 62O/15 GYP 1, GYP 4 | |
B11 | Lussier River - Coyote Creek | 82J/4 | 50 09 00 115 38 00 | Gypsum | Isolated occurrences of gypsum have been traced along both limbs of syncline between Lussier River and coyote Creek; anhydrite begins at 20-25m from surface | Potential estimate 20-40 million tonnes (SB); Production1990: 135,000 tonnes; total reserves calculated in 1984: 7 million tonnes of gypsum | Butrenchuk (1989b) |
B13 | Elkhorn | 82J/5 | 50 28 00 115 52 00 | Gypsum | Southern extension of Burnais Fm. Beds exploited by Windermere quarries | 10-20 million tonnes estimate (SB) | Butrenchuk (1989b) |
B14 | Windermere | 82J/12 | 50 30 00 115 53 00 | Gypsum | Gypsum 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 tonnes | Butrenchuk (1989b) |
ID | Name | NTS | Lat.(N) Long.(W) Deg. Min. Sec. | Commodities | Geological description | Reserves, resources or development work | Reference(s) |
---|---|---|---|---|---|---|---|
A103 | Paintearth Mine (Tannathin) | 83A/8 | 52 25 36 112 11 57 | Leonardite | U.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 |
M14 | Tyndall - Garson | 62I | 50 05 00 96 42 00 | Leonardite, dimension stone | Ordovician Red River Fm., dolomitic limestone in lower half Selkirk Member, 6.5-9m quarriable section, 2-4m overburden | Not available | M.I 62I/2 STN |
M15 | Lily Bay Cement | 62J | 50 43 43 98 13 45 | Limestone | Devonian Elm Point Fm. | M.I. 62J/16 LST 1 | |
M16 | Spearhill | 62O | 51 19 09 98 22 34 | Limestone | Devonian Elm Point Fm. | M.I. 62O/8 LST 1 | |
M17 | Faulkner | 62O | 51 24 23 98 47 53 | Limestone | Devonian Elm Point Fm. | 300,000 tpa | M.I. 62O/7 LST 2 |
M18 | Steep Rock | 62O | 51 26 53 98 48 03 | Limestone | Devonian Elm Point Fm., grades 95-99% CaCO3 | Not available | M.I. 62O/7 LST 1 |
M19 | Paradise Beach | 62O | 51 34 52 99 46 57 | Limestone | Devonian Dawson Bay Fm. | M.I. 62O/12 LST 2 | |
M20 | Mafeking | 63C | 52 48 13 101 09 44 | Limestone | Devonian Souris River Fm., grades 95-98% CaCO3 | M.I. 63C/14 LST 1 | |
A107 | Blairmore | 82G | 49 36 14 114 25 05 | Limestone | Mississippian Banff Fm. limestone; 120m exposed; includes dark gray, medium crystalline dolomitic limestones with shale interbeds and abundant chart lenses | Avg. CaCO3 67.39%; Avg. MgCO3 14.24%; Si02 17.09% | Holter (1976) |
A108 | Crowsnest Lake | 82G | 49 37 59 114 40 00 | Limestone | Limestone quarry in Mississippian Livingstone Fm. Consists of 37m thick high-grade limestone units, separated by 11m thick dolomitic limestone unit | Estimated to contain 1.2 million tonnes of high purity limestone; at 1981 production levels, the quarry will be exhausted by 1994 | Macdonald and Hamilton (1981); Holter (1976); Goudge (1945) |
A111 | Exshaw | 82O | 51 03 34 115 10 31 | Limestone | The 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 dolomite | Size of deposit: large | Holter (1976); Goudge (1945) |
A112 | Canmore | 82O | 51 03 34 115 16 06 | Limestone | Mississipian Livingstone Fm., limestone; very fine-grained, dark bluish gray, in massive, indistinct beds flecked with tiny crystals of black calcite | Large operation started by Alberta Portland Cement Co. in 1906-1914 | Holter (1976); Goudge (1945) |
A113 | Kananaskis QB | 82O | 51 04 47 115 07 33 | Limestone | Cambrian 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 bedding | Size of deposit: medium | Goudge (1945), p.108 Hamilton (1987), p. 17-23; 34, 36,47,48. N.M.I. Record 115062 |
A114 | Corkscrew Mountain | 82O | 51 57 44 115 17 16 | Limestone | Limestone quarry in Shunda/Pekisko fms., Mississipian | Size of deposit: medium | Holter and Hamilton (1989) |
A116 | Nordegg | 83C | 52 28 20 116 03 07 | Limestone | Limestone 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 zone | Size of deposit: medium; quarry opened for ballast before 1944; presently worked for rip rap | Holter (1976); Matthews (1961); Goudge (1945) |
A117 | Henry House | 83D | 52 56 13 118 02 07 | Limestone | 43m 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 face | Quarry operated 1917 to 1930 for production of Portland Cement | Goudge (1945) |
A121 | Cadomin | 83F | 53 00 38 117 19 33 | Limestone | Limestone 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 range | Size of deposit: large; proven reserves 22 million tonnes | Holter (1976); Goudge (1945) |
A122 | Roche Miette | 83F | 53 10 14 117 57 44 | Limestone | Devono-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 thick | Quarry formerly worked for lime production | Goudge (1945) |
A123 | Jasper Gate | 83F | 53 13 43 117 48 57 | Limestone | Quarry 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 thickness | 97% CaCO3; 3% MgCO3 | Holter (1976) |
ID | Name | NTS | Lat.(N) Long.(W) Deg. Min. Sec. | Commodities | Geological description | Reserves, resources or development work | Reference(s) |
---|---|---|---|---|---|---|---|
B18 | Baker Creek - Sukunka R. | 93P/4 | 55 09 09 121 55 02 | Limestone | Light gray limestone of the Mississippian Rundle Group, minimum width of 45m | A short lived production in 1984/1985 for agriculture and highway construction - poor market conditions; reserves 40 million tonnes of chemical lime grade | Fischl (1992) |
B19 | Mount Brussilof | 82J/13E | 50 47 20 115 40 40 | Magnetite | Sparry 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-escarpment | 9.5 million tonnes 95% Mg0; 13.6 million tonnes 93-95% MgO; 17.6 million tonnes 92% MgO; in calcined product; production 1990: 170,000 tonnes | Grant (1987); MacLean (1988); Simandl and Hancock (1991) |
A134 | Marlboro | 83F | 53 32 54 116 47 25 | Marl | Fluvial 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) | |
A136 | Duffield | 83G | 53 25 55 114 17 00 | Marl | Abandoned 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 wet | Poor-quality deposit | Macdonald (1982) |
A142 | Halfway Lake | 83I | 54 09 31 113 30 57 | Marl | Marl 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 cement | Macdonald (1982); Holter (1972) |
A143 | McGregor | 83J | 54 06 05 115 23 16 | Marl | Hillside 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 0.3m | Moderate size deposit, fair-good quality | Macdonald (1982) |
A148 | Grimshaw | 84C | 56 06 31 117 38 33 | Marl | Deposit 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 surface | Moderately large deposit; good quality; in 1976 some production and local sale as agricultural lime | Macdonald (1982) |
B34 | Crow | 82G/10 | 49 39 45 114 42 30 | Phosphate | A one metre thick phosphate of Fernie Formation repeated tectonically four times has 26.20% P205 and 757 ppm Y | Consistent 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) |
S56 | Rocanville | 62K | 50 27 45 101 32 33 | Potash | Middle Devonian Prairie Formation, sylvite mineralization in marine evaporite | Not Available | Holter (!969); Fuzesy (1982) |
S57 | Esterhazy | 62K | 50 38 25 101 51 18 | Potash | Middle Devonian Prairie Formation, sylvite mineralization and by-product salt from marine evaporite | Not Available | Holter (!969); Fuzesy (1982) |
S58 | Esterhazy | 62K | 50 43 43 101 59 40 | Potash | Middle Devonian Prairie Formation, sylvite mineralization and by-product salt from marine evaporite | Not Available | Holter (!969); Fuzesy (1982) |
S60 | Belle Plaine | 72I | 50 26 26 105 14 13 | Potash | Middle Devonian Prairie Formation, sylvite mineralization with halite | Not Available | Holter (!969); Fuzesy (1982) |
S61 | Allan | 72O | 51 55 32 106 04 28 | Potash | Middle Devonian Prairie Formation, sylvite mineralization and by-product salt from marine evaporite | Not Available | Holter (!969); Fuzesy (1982) |
S64 | Lanigan | 72P | 51 50 18 105 11 40 | Potash | Middle Devonian Prairie Formation, sylvite mineralization | Not Available | Holter (!969); Fuzesy (1982) |
S65 | Colonsay | 72P | 51 55 32 105 45 40 | Potash | Middle Devonian Prairie Formation, sylvite mineralization and by-product salt from marine evaporite | Not Available | Holter (!969); Fuzesy (1982) |
S66 | Cominco (Vanscoy) | 73B | 52 00 46 107 04 29 | Potash | Middle Devonian Prairie Formation, sylvite mineralization and by-product salt from marine evaporite | Not Available | Holter (!969); Fuzesy (1982) |
S67 | Patience Lake (Potash Company of America) | 73B | 52 06 00 106 21 39 | Potash | Middle Devonian Prairie Formation, sylvite mineralization and by-product salt from marine evaporite | Not Available | Holter (!969); Fuzesy (1982) |
S68 | PCS Cory | 73B | 52 06 00 106 47 21 (Mine Shaft Location) | Potash | Middle Devonian Prairie Formation, sylvite mineralization and by-product salt from marine evaporite | Not Available | Holter (!969); Fuzesy (1982) |
S73 | Waldeck | 72J | 50 21 13 107 35 07 | Pumicite | Probably Eocene-Oligocene | Unknown | Worcester (1950); Crawford (1955) |
ID | Name | NTS | Lat.(N) Long.(W) Deg. Min. Sec. | Commodities | Geological description | Reserves, resources or development work | Reference(s) |
---|---|---|---|---|---|---|---|
A166 | Willow Creek | 82J/1 | 50 07 36 114 08 25 | Pumicite | Recent (?) 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 mesh | Small deposit, est. 1,000-1200 m3; excavated on small scale for use in cleansing compounds 1942-51 | ARC Econ. Mins. Files |
B44 | Nicholson | 82N/2W | 51 12 40 116 51 33 | Quartzite | Massive quartzite of the Ordovician Mount Wilson Formation, SiO2 99.85%; lump silica producer | 3 million tonnes (1985); Production 1990: 36,000 tonnes | Foye (1987) |
S74 | Esterhazy | 62K | 50 38 25 101 51 18 and 50 43 43 101 59 40 | Salt | Middle Devonian Prairie Formation, sylvite mineralization and by-product salt from marine evaporite | Not available | Holter (1969); Fuzesy (1982) |
S75 | Belle Plaine | 72I | 50 26 26 105 14 13 | Salt | Middle Devonian Prairie Formation, sylvite mineralization with halite | Not available | Holter (1969); Fuzesy (1982) |
S76 | Saskatoon Chemicals (Weyerhaeuser) | 73B | 52 11 14 106 38 47 | Salt (NaCl) | Middle Devonian, Prairie Formation salt beds | Not available | Holter (1969) |
S77 | Unity | 73C | 52 26 57 109 05 54 | Salt | Middle Devonian Prairie Formation | Extensive reserves | Holter (1969) |
A168 | Hughenden | 73D | 52 29 06 110 57 06 | Salt (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 products | Hamilton (1971); ERCB Well Files |
A169 | Hardisty | 73D | 52 38 42 111 17 15 | Salt (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 products | Hamilton (1971); ERCB Well Files |
A170 | Duvernay | 73E | 53 46 49 111 42 08 | Salt | Mid-Devonian Lower Elk Point Fm. Upper Lotsberg Salt. Salt interval: 4395'-4740'; cored 4403'-4736' | Hamilton (1971); ERCB Well Files | |
A171 | Lindberg | 73E | 53 52 04 110 38 12 | Salt | Mid-Devonian Prairie Evaporite salt interval: 2631'-3073' T.D.; cored: 2631'-3073' | Hamilton (1971) | |
A172 | Fort McMurray | 74D | 56 42 16 111 20 51 | Salt | Mid-Devonian Upper Elk Point Fm. Prairie Evaporite salt; salt interval: 723'-934'; cored 623'-934' | Hamilton (1971); ERCB Well Files; Allan (1943) | |
A173 | Fort Saskatchewan | 83H | 53 44 12 113 11 21 | Salt | Mid-Devonian Lower Elk Point Fm.; salt interval: 6091' n.p.; cored: 6125'-27' | Hamilton (1971) | |
A174* | Fort Saskatchewan | 83H | 53 45 05 113 09 52 | Salt (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 products | Hamilton (1971); ERCB Well Files; Allan (1943) |
A175 | Bruderheim A | 83H | 53 47 35 112 52 57 | Salt | Mid-Devonian Lower Elk Point Subgroup - Upper Lotsberg salt; salt interval 1751-1841 m; cored 1745-1769.5m | Salt bringing operation for NaCLO3 manufacture; salt production capacity 50 Ktpa | ARC Econ. Mins. Files |
A176 | Bruderheim B | 83H | 53 48 01 112 53 41 | Salt | Mid-Devonian Lower Elk Point Subgroup - Upper Lotsberg salt; salt interval 1750-1840m | Salt bringing operation for NaCLO3 manufacture; salt production capacity 50 Ktpa | ARC Econ. Mins. Files |
A177* | Fort Saskatchewan | 83H | 53 48 34 113 08 22 | Salt (storage) | Mid-Devonian Lower Elk Point Fm.; Upper Lotsberg salt; salt interval: 5985'-6232' | Salt cavern for underground storage of petroleum products | Hamilton (1971); ERCB Well Files; Allan (1943) |
A178 | Redwater | 83H | 53 50 19 113 05 24 | Salt (storage) | Mid-Devonian Lower Elk Point Fm. Upper Lotsberg salt; salt interval: 5804'-6062'; cored 5846'-6062' | Salt cavern for underground storage of petroleum products | Hamilton (1971); ERCB Well Files; Allan (1943) |
A179 | Brocket | 82H | 49 32 44 113 48 35 | Sandstone - building stone | Tertiary Paskapoo Fm. heavy sandstone, 7m thick; fine to medium gray with slightly brownish cast and with clean "peppery" appearance | Parks (1916) | |
A180 | Porcupine Hills | 82H | 49 44 05 113 37 45 | Sandstone - building stone | Tertiary Paskapoo Fm. sandstone, 4m thick; stone of external weathered zone uniform grayish colour, blue cores show in lower layers | Small amount quarried | Parks (1916) |
A181 | Monarch | 82H | 49 49 20 113 13 21 | Sandstone - building stone | Tertiary 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) | |
A182 | High River B | 82I | 50 30 23 113 47 48 | Sandstone - building stone | Tertiary Paskapoo Fm. sandstone on banks of Little Bow river; stone medium grained, uniform grayish with yellowish green cast; little evidence of reediness | Small amount quarried | Parks (1916) |
ID | Name | NTS | Lat.(N) Long.(W) Deg. Min. Sec. | Commodities | Geological description | Reserves, resources or development work | Reference(s) |
---|---|---|---|---|---|---|---|
A183 | High River A | 82I | 50 34 45 113 53 39 | Sandstone - building stone | 15m 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 reediness | Small amount quarried | Parks (1916) |
A184* | High River C | 82I | 50 36 30 113 50 53 | Sandstone - building stone | Tertiary Paskapoo Fm. sandstone | Inconsiderable output used for foundation | Parks (1916) |
A185 | Sandstone | 82J | 50 46 06 114 02 08 | Sandstone - building stone | Section 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) | |
A186 | Pigeon Creek | 82O | 51 01 50 115 14 42 | Sandstone - dimension stone | Dolomitic 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 1m | Thunderstone Quarries opened in 1961; Rundle Rock sold as flagstone, dry pack sheets and landscaping stone | Edwards (1991) (Guidebook); Fox (1981) |
A187* | Calgary | 82O | 51 02 42 114 06 19 | Sandstone - building stone | Tertiary 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 bed | Quarry originally opened in 1902. Operations later prohibited by conditions under which land was sold for building lots | Parks (1916) |
A188* | Brickburn | 82O | 51 03 34 114 09 07 | Sandstone - building stone | Section 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 section | Quarry in operation 1910-1914 | Parks (1916) |
A189 | Canmore | 82O | 51 07 57 115 23 05 | Sandstone - building stone | Dolomitic 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 1m | Production of Rundle Rock building stone seasonal over past 35yrs. | Fox (1981); Edwards (1991) |
A190 | Rocky View | 82O | 51 08 49 114 04 56 | Sandstone - building stone | Tertiary 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 reediness | Quarries not worked since 1910 | Parks (1916) |
A191* | Glenbow | 82O | 51 09 41 114 23 04 | Sandstone - building stone | Tertiary 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 structure | Extensive quarrying till 1909; cessation in operation due to increase in blue hardhead and considerable overburden | Parks (1916) |
A192 | Cochrane | 82O | 51 12 18 114 28 39 | Sandstone - building stone | Tertiary 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 quarried | Parks (1916) |
A193 | Didsbury | 82O | 51 38 32 114 07 50 | Sandstone - building stone | Tertiary 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, gray | Quarried on small scale | Parks (1916) |
A194 | Innisfail A | 82P | 51 58 32 113 43 45 | Sandstone - building stone | Tertiary Paskapoo Fm. sandstone; upper 1.5m thin-bedded, lower part heavy bedded with irregular planes of parting; uniform bluish gray colour | Quarried on small scale | Parks (1916) |
A195 | Innisfail B | 83A | 52 02 02 113 55 10 | Sandstone - building stone | Tertiary 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) | |
A196 | Red Deer | 83A | 52 16 00 113 49 27 | Sandstone - building stone | Tertiary 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) |
ID | Name | NTS | Lat.(N)Long.(W) Deg. Min. Sec. | Commodities | Geological description | Reserves, resources or development work | Reference(s) |
---|---|---|---|---|---|---|---|
A197 | Entwistle | 83G | 53 35 31 114 59 46 | Sandstone - building stone | Tertiary 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) | |
M32 | Black Island | 62P | 51 15 00 96 23 00 | Silica sand | Ordovician Winnepeg River Fm., high purity silica sand | Estimated reserves 20 million t, quarry capacity 180,000 tpa | M.I. 62P/1 SIA 1 |
S78 | Red Deer River | 63C | 52 58 42 101 44 34 | Silica sand | Early Cretaceous Mannville Formation | Estimated 14 million tonnes reserve locally; production to date is minor | Beck (1974); Babey (1955); Wickenden (1945); Collings and Andrews (1986, 1989); Northern Silica Limited (1968); Red Deer Silica Inc. (1986) |
B46 | Mount Moberly | 82N/7W | 51 22 18 116 57 49 | Silica sand | A friable phase of the Ordovician Mount Wilson Formation; at the mine site up to 200m thick, 99.5% SiO2, less than 0.1% Fe2-O2 | Geological reserves estimated at 10 million tonnes; production 1990: 90,000 tonnes | Foye (1987) |
A203 | Bruderheim | 83H | 53 51 11 112 55 00 | Silica sand | Upper Pleistocene glacial outwash sand; post depositional modification has resulted in presence of thin film of iron oxide on sand grains, giving deposit a yellow colour | 88.79% of natural sand retained on 100-mesh sieve | Carrigy (1970) |
S83 | Sybouts Lake East | 72H | 49 02 14 104 24 29 | Sodium sulphate | Saline lake deposit; permanent and intermittent crystal beds and brine | Original reserve estimated at 3.5 million tons Na2SO4 | Cole (1926); Tomkins (1954); Last (1984) |
S86 | Frederick Lake | 72H | 49 44 27 105 19 34 | Sodium sulphate | Saline lake deposit; permanent crystal bed and brine | Original reserve estimated at 3.7 million tons Na2SO4 | Cole (1926); Tomkins (1954); Last (1984) |
S87 | Bishopric (Fredrick Lake) | 72I | 50 00 13 105 45 34 | Sodium sulphate | Saline Lake; brine, intermittent and permanent crystal beds and brine | Original reserve estimated at 2.4 million tons Na2SO4 | Cole (1926); Tomkins (1954); Last (1984) |
S88 | Chaplin Lake | 72J | 50 21 13 106 37 23 | Sodium sulphate | Saline Lake; brine with intermittent and permanent crystal beds | Original reserve estimated at 3 million tons Na2SO4 | Tomkins (1954); Last (1984) |
S91 | Verlo | 72K | 5021 13 108 24 37 | Sodium sulphate | Saline Lake deposit; permanent and intermittent crystal beds and brine | Original reserve estimated at 950,000 tons Na2SO4 | Tomkins (1954); Worsley (1975) |
S92 | Ingebright South | 72K | 5021 13 109 22 22 | Sodium sulphate | Saline lake deposit; permanent crystal bed | Original reserve estimated at 9 million tons Na2SO4 | Cole (1926); Tomkins (1954); Last (1984) |
S94 | Snakehole Lake | 72K | 50 34 12 108 24 47 | Sodium sulphate | Saline Lake deposit; permanent and intermittent crystal beds and brine | Original reserve estimated at 1.7 million tons Na2SO4 | Cole (1926); Tomkins (1954); Last (1984) |
S95 | Alsask | 72N | 51 18 52 109 52 15 | Sodium sulphate | Saline lake brine and intermittent and permanent crystal beds | Original reserve estimated at 2.6 million tons Na2SO4 | Cole (1926); Tomkins (1954); Last (1984) |
S98 | Berry Lake | 73A | 52 00 27 105 34 24 | Sodium sulphate | Saline Lake deposit, crystal beds with intermittent brine | Estimate reserves 800,000 tons | Cole (1926); Tomkins (1954); Last (1984) |
S102 | Whiteshore Lake | 73C | 52 06 06 108 17 07 | Sodium sulphate | Saline lake deposit as brine and intermittent and permanent crystal beds | Estimated initial reserves of 6.5 million tons anhydrous salt | Cole (1926); Tomkins (1954) |
A211 | Metiskow | 73D | 52 21 14 110 44 9 | Sodium sulphate | Lake 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 thick | The 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 tpa | Broughton (1976); Govett (1958); Cole (1926) |
S104 | Steelman | 62E | 49 18 42 102 37 21 | Sulphur | Sour gas field | Production 7 | Oilweek Jan. 21, 1991 |
S105 | Regina | 72I | 50 31 40 104 32 58 | Sulphur (by-product) | By-products of heavy oil upgrader | Production 250 tonnes per day | |
A214 | Fort McMurray | 74E | 57 00 33 111 29 39 | Sulphur | Sulphur in crude bitumen extracted from Athabaska Oil Sands; Cret. McMurray Fm.; S content 5% by wieght of bitumen | Sulphur extraction plant; recovery capacity 441 tpd; reserves: 5.8 M t | Oilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18 |
A215 | Mildred Lake | 74E | 57 02 18 111 34 29 | Sulphur | Sulphur in crude bitumen extracted from Athabaska Oil Sands; Cret. McMurray Fm.; S content 5% by wieght of bitumen | Sulphur extraction plant; recovery capacity 1255 tpd; reserves: 10.8 M t | Oilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18 |
A216 | Coleman (Savannah Creek) | 82G | 49 37 59 114 00 35 | Sulphur | Sour gas field; producing zones: Miss. Rundle and Dev. Wabamun; H2S content 24% | Sulphur extraction plant; recovery capacity 389 tpd; reserves: 2.5 M t | Oilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18 |
A217 | Waterton | 82G | 49 18 13 114 00 35 | Sulphur | Sour gas field; producing zones: Miss. Rundle and Dev. Wabamun; H2S content 19% | Sulphur extraction plant; recovery capacity 3,107 tpd; reserves: 7.3 M t | Oilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18 |
A218 | Mazeppa (Okotoks) | 82I | 50 38 34 113 46 54 | Sulphur | Sour gas field; producing zones: Miss. Rundle and Dev. Wabamun; H2S content 36% | Sulphur extraction plant; recovery capacity 577 tpd | Oilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18 |
A219 | Okotoks | 82I | 50 43 29 113 56 25 | Sulphur | Sour gas field; producing zones: Miss. Rundle and Dev. Wabamun; H2S content 36% | Sulphur extraction plant; recovery capacity 431 tpd; reserves : 2.1 M t | Oilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18 |
ID | Name | NTS | Lat.(N)Long.(W) Deg. Min. Sec. | Commodities | Geological description | Reserves, resources or development work | Reference(s) |
---|---|---|---|---|---|---|---|
A220 | Turner Valley (Diamond) | 82J | 50 35 37 114 09 03 | Sulphur | Sour gas field; producing zone: Miss. Rundle; H2S content 2.5% | Sulphur extraction plant; recovery capacity 10.7 tpd; reserves not stated | Oilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18 |
A221 | Quirk Creek | 82J | 50 45 14 114 29 50 | Sulphur | Sour gas field; producing zone: Miss. Rundle; H2S content 9% | Sulphur extraction plant; recovery capactiy 299 tpd; reserves not stated | Oilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18 |
A222 | Jumping Pound | 82O | 51 07 57 114 34 14 | Sulphur | Sour gas field; producing zone: Miss. Rundle; H2S content 6% | Sulphur extraction plant; recovery capactiy 597 tpd; reserves: 2.8 M t | Oilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18 |
A223 | Wildcat Hills | 82O | 51 13 11 114 38 25 | Sulphur | Sour gas field; producing zone: Miss. Rundle; H2S content 4% | Sulphur extraction plant; recovery capactiy 177 tpd; reserves not stated | Oilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18 |
A224 | Crossfield E. | 82O | 51 23 41 114 02 09 | Sulphur | Sour gas field; producing zone: Dev. Wabamun; H2S content 34% | Sulphur extraction plant; recovery capactiy 1,797 tpd; reserves:2.2 M t | Oilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18 |
A225 | Carstairs - Crossfield | 82O | 51 32 25 114 12 00 | Sulphur | Sour gas field; producing zone: Miss. Elkton; H2S content 0.5% | Sulphur extraction plant; recovery capacity 65 tpd | Oilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18 |
A227 | Burnt Timber | 82O | 51 34 09 114 51 22 | Sulphur | Sour gas field; producing zone: Miss. Rundle and Dev. Wabamun; H2S content 13% | Sulphur extraction plant; recovery capacity 489 tpd reserves: 1.2 M t | Oilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18 |
A228 | Harmattan | 82O | 51 41 09 114 29 06 | Sulphur | Sour gas field; producing zone: Miss. Rundle; H2S content 46% | Sulphur extraction plant; recovery capacity 490 tpd. Reserves not stated | Oilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18 |
A229 | Olds | 82O | 51 44 39 114 07 50 | Sulphur | Sour gas field; producing zone not stated; H2S content 15% | Sulphur extraction plant; recovery capacity 389 tpd; reserves not stated | Oilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18 |
A230 | Bearberry | 82O | 51 53 23 114 48 56 | Sulphur | Devonian 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 t | Kitzan and Auger (1992) |
A231 | Caroline | 82O | 51 56 00 114 31 56 | Sulphur | Sour 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 t | Oilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18 |
A232 | Caroline - Swan Hills | 82O | 51 58 04 114 45 00 | Sulphur | Devonian Beaverhill Lake Fm., sour gas reservoir; H2S content 30-35% | Plant design capacity 4000 tpd 1.4 M tpy | Oilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18 |
A233 | Innisfail | 82O | 51 58 37 114 03 37 | Sulphur | Sour gas field; producing zone: Dev. Leduc; H2S content 16% | Sulphur extraction plant, recovery capacity 163 tpd; reserves not stated | Oilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18 |
A234 | Caroline (Garrington) | 82O | 51 59 29 114 45 02 | Sulphur | Sour gas field; producing zones -Miss. Rundle and Dev. Beaverhill Lake | Sulphur extraction plant; recovery capacity 10.4 tpd | Oilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18 |
A235 | Crossfield (Balzac) | 82P | 51 11 45 113 55 35 | Sulphur | Sour 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 t | Oilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18 |
A236 | Lone Pine Creek | 82P | 51 30 38 115 51 34 | Sulphur | Sour gas field; producing zones: Dev. Wabamun and Leduc; H2S content 10% | Sulphur extraction plant: recovery capacity 157 tpd; reserves not stated | Oilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18 |
A237 | Lone Pine Creek | 82P | 51 35 00 113 50 10 | Sulphur | Sour gas field; producing zones; Dev. Wabamun and Leduc; H2S content 10% | Sulphur extraction plant: recovery capacity 283 tpd; reserves not stated | Oilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18 |
A238 | Wimborne | 82P | 51 54 13 113 33 30 | Sulphur | Sour gas field; producing zone: Dev. Leduc; H2S content 13% | Sulphur extraction plant: recovery capacity 182 tpd; reserves not stated | Oilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18 |
A239 | Nevis | 83A | 52 18 37 113 05 11 | Sulphur | Sour gas field; producing zone: Devonian; H2S content 4% | Sulphur extraction plant; recovery capacity 197tpd | Oilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18 |
A240 | Joffre | 83A | 52 21 14 113 42 38 | Sulphur | Sour gas field; producing zones; Cret. Mannville and Dev. Nisku; H2S content 3.4% | Sulphur extraction plant: recovery capacity 25 tpd; reserves not stated | Oilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18 |
A242 | Ram River (Strachan) | 83B | 52 09 06 115 19 18 | Sulphur | Sour gas field; producing zone: Dev. Leduc; H2S content 19% | Sulphur extraction plant: recovery capacity 4,572 tpd | Oilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18 |
A243 | Strachan | 83B | 52 13 28 115 10 44 | Sulphur | Sour gas field; producing zone: Dev. Leduc; H2S content 9% | Sulphur extraction plant; recovery capacity 953 tpd; reserves: 0.8 M t | Oilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18 |
A244 | Homeglen Rimbey | 83B | 52 45 48 114 06 34 | Sulphur | Sour gas field; producing zone: Dev. Leduc; H2S content 1% | Sulphur extraction plant; recovery capacity 128 tpd; reserves not stated | Oilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18 |
A245 | Brazeau River (Nordegg) | 83B | 52 46 40 115 39 26 | Sulphur | Sour 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 t | Oilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18 |
A246 | Minnehik-Buck Lake | 83B | 52 56 17 114 50 06 | Sulphur | Sour gas field; producing zone: Miss. Pekisko; H2S content 0.1% | Sulphur extraction plant; recovery capacity 45 tpd; reserves not stated | Oilweek, Jan. 21, 1991; Prud'homme (1989); ERCB ST 91-18 |
ID | Name | NTS | Lat.(N) Long.(W) Deg. Min. Sec. | Commodities | Geological description | Reserves, resources or development work | Reference(s) |
---|---|---|---|---|---|---|---|
A247 | Brazeau River | 83B | 52 56 36 115 54 07 | Sulphur | Sour gas field; producing zones: Miss. Elkton-Shunda, and Dev. Nisku; H2S content 0.8% | Sulphur extraction plant; recovery capacity 110 tpd | Oilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18 |
A248 | Hanlan-Robb | 83F | 53 12 57 116 48 27 | Sulphur | Sour gas field; producing zones: Dev. Nisku and Beaverhill Lake; H2S content 9% | Sulphur extraction plant; recovery capacity 1,092 tpd; reserves: 2.9 M t | Oilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18 |
A249 | Medicine Lodge | 83F | 53 28 32 117 02 10 | Sulphur | Sour gas field; producing zone: Dev. Wabamun; H2S content ? | Sulphur extraction plant; recovery capacity 45 tpd; reserves not stated | Oilweek, Jan. 21 1991;ERCB ST 91-18 |
A250 | Edson | 83F | 53 33 46 116 32 41 | Sulphur | Sour gas field; producing zone: Miss. Elkton-Shunda; H2S content 1.4% | Sulphur extraction plant; recovery capacity 288 tpd; reserves not stated | Oilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18 |
A251 | Rosevear | 83F | 53 39 00 116 06 08 | Sulphur | Sour gas field; producing zone: Dev. Beaverhill Lake; H2S content 8% | Sulphur extraction plant; recovery capacity 171 tpd; reserves not stated | Oilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18 |
A252 | Rosevear | 83F | 53 42 30 116 09 05 | Sulphur | Sour gas field; producing zone: Dev. Beaverhill lake; H2S content 8% | Sulphur extraction plant; recovery capacity 110 tpd; reserves not stated | Oilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18 |
A253 | West Pembina (Brazeau) | 83G | 53 02 22 115 57 48 | Sulphur | Sour 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 |
A254 | Brazeau River | 83G | 53 11 06 115 44 38 | Sulphur | Sour gas field; producing zones: Miss. Elkton-Shunda, and Dev. Nisku; H2S content 7% | Sulphur extraction plant; recovery capacity 447 tpd | Oilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18 |
A255 | Bonnie Glen | 83H | 53 03 09 113 55 02 | Sulphur | Sour gas field; producing zone:Dev. Leduc; H2S content 0.4% | Sulphur extraction plant; recovery capacity 12.5 tpd; reserves not stated | Oilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18 |
A256 | Redwater | 83H | 53 57 18 113 05 24 | Sulphur | Sour gas field; producing zone: Dev. Leduc; H2S content 2.6% | Sulphur extraction plant; recovery capacity 11 tpd; reserves not stated | Oilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18 |
A257 | Kaybob S. III | 83K | 54 06 05 116 36 45 | Sulphur | Sour 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 t | Oilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18 |
A258 | Windfall-Whitecourt | 83K | 54 11 19 116 12 45 | Sulphur | Sour 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 t | Oilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18 |
A259 | Bigstone | 83K | 54 15 40 117 12 44 | Sulphur | Sour gas field; producing zone: Dev. Wabamun; H2S content 1.6% | Sulphur extraction plant; recovery capacity 385 tpd; reserves not stated | Oilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18 |
A260 | Kaybob S. | 83K | 54 20 55 116 51 44 | Sulphur | Sour 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 stated | Oilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18 |
A261 | Simonette | 83K | 54 25 17 117 46 08 | Sulphur | Sour gas field; producing zones: Cret. Mannville, and Dev. Wabamun and Leduc; H2S content 16% | Sulphur extraction plant; recovery capacity 95 tpd; reserves not stated | Oilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18 |
A262 | Sturgeon Lake | 83K | 54 56 42 117 14 32 | Sulphur | Sour gas field; producing zone: Dev. Leduc; H2S content 9% | Sulphur extraction plant; recovery capacity 98 tpd; reserves not stated | Oilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18 |
A263 | Gold Creek | 83L | 54 49 44 118 38 50 | Sulphur | Sour gas field; producing zones: Cret. Mannville and Dev. Wabamun; H2S content 3% | Sulphur extraction plant; recovery capacity 43 tpd; reserves not stated | Oilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18 |
A264 | Teepee Creek | 83M | 55 22 53 118 29 57 | Sulphur | Sour gas field; producing zones: Trias. Doig, and Dev. Wabamun; H2S content 3% | Sulphur extraction plant; recovery capacity 30 tpd; reserves not stated | Oilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18 |
A265 | Sinclair-Hythe | 83M | 55 24 38 119 49 57 | Sulphur | Sour gas field; producing zones: Trias. Doig; H2S content 8% | Sulphur extraction plant; recovery capacity 30 tpd; reserves not stated | Oilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18 |
A266 | Progress | 83M | 55 43 50 119 24 33 | Sulphur | Sour gas field; producing zone: Trias. Halfway; H2S content 0.7% | Sulphur extraction plant; recovery capacity 14 tpd; reserves not stated | Oilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18 |
A267 | Rainbow | 84L | 58 26 56 119 14 25 | Sulphur | Sour gas field; producing zones: Dev. Slave Point and Keg River; H2S content 2% | Sulphur extraction plant; recovery capacity 139 tpd; reserves not stated | Oilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18 |
A268 | Zama | 84M | 59 03 34 118 52 01 | Sulphur | Sour gas field; producing zone: Dev. Elk Point; H2S content 8% | Sulphur extraction plant; recovery capacity 74 tpd; reserves not stated | Oilweek, Jan. 21 1991; Prud'homme (1989); ERCB ST 91-18 |
B47 | Pine River | 93P/5 | 55 17 00 121 38 00 | Sulphur | Sour gas field | 1055 tpd | Oilweek, Jan. 21, 1991 |
B48 | Taylor Flats | 94A/2 | 56 06 58 120 53 50 | Sulphur | Sour gas field, H2S content 3% | 460 tpd | Oilweek, Jan. 21, 1991 |
B49 | Cypress | 94B/16 | 56 47 00 122 21 00 | Sulphur | Sour gas field | 15 tpd | Oilweek, Jan. 21, 1991 |
B56 | Fort Nelson | 94J/10 | 58 40 00 122 38 00 | Sulphur | Sour gas field; H2S content 0.5-7% | 1100 tpd | Oilweek, Jan. 21, 1991 |