General Information
Secondary Commodities: silver, gold
Aliases: Dome Lode
Deposit Type(s): Vein Au-Quartz
Location(s): 63.863060 N, -138.910560 W
NTS Mapsheet(s): 115O15
Location Comments: .5 Kilometres
Hand Samples Available at YGS: No
Capsule
Work History
The earliest staking was probably Pride of the Mountain cl (4218) by H.N. Coleman in June, 1900. Re-staked as a forty claim property by Aaron Knorr, commencing with Discovery, etc (6926) in May, 1904 and optioned to Dome Lode Development Company Ltd., which traced four veins on surface for 460 m with 4 shafts (4.3 to 24 m deep) and a number of trenches. In 1909-1910, a 792 m crosscut was driven at a cost of $70,000. About 25 claims were taken to lease, including some up to 3.2 km northeast. Sam Thurber blasted an open cut on the Hunker claim, adjoining to the east, in 1912. Near the road, 1.6 km to the north, W.D. MacKay put in a 15 m shaft and an open cut on the Jennie claim and J. Cameron did some trenching on the Summit claim, all prior to 1912.
Re-staked as Eleventh Hour cl (15037) in June, 1924 and Bridge, etc cl (39010) in September, 1937 by A.J. Matheson, who explored with hand pits until 1940-1942, when he cleaned out and resampled the crosscut and drifted 37 m.
Re-staked as Dominion cl 1-4 (86971) and King Solomon cl 1-7 (86975) in August, 1965 by Orekon Ltd., which bulldozer trenched in 1966 and 1972. The adit was re-staked in November, 1980 as Dominion cl 1-4 (YA55110) and King Solomon cl 1-36 (YA55114) by Lindex Exploration Ltd. and transferred to Orekon Ltd. in 1982.
Cominco added KSD cl 1-140 (YA49490) to the west in January, 1980 and carried out mapping, geochemistry and IP surveys later in the year. I. Mahoney staked a single Junker cl (YA55283) 2.5 km to the east in May, 1981 and drilled two holes (11.3 m) in 1982.
Dawson Eldorado Gold Explorations Ltd. re-staked the KSD group as Klook cl 1-48 (YA65751) in June, 1983 and explored with mapping and geochemical sampling later in the year. A joint venture between United Keno Hill Mines Ltd. (UKHM) and Falconbridge Ltd. added Dom cl 1-149 (YA80272) to the southwest in June, 1984, re-staked the old workings as Kin cl 1-82 (YA89442) in July, 1987 and performed mapping, geochemical sampling, VLF-EM surveys and bulldozer trenching in 1987 and 1988.
Barramundi Gold Ltd. staked LP cl 1-13 (YB68565) to the east in March, 1996. In March, 1999 Barramundi completed 3,850 line km of detailed airborne magnetometer and VLF-EM surveying that covered a 16 km x 24 km area centered about King Solomon Dome and included this occurrence. In 1999, Barramundi optioned the majority of Klondike claims, excluding those under option from UKHM and JAE resources, to KSL Exploration (Yukon) Ltd.
Klondike Gold Corp. (formerly Arbor Resources Inc.) staked the nearby GRE claims in 2003 and performed soil sampling and prospecting in 2004. Klondike Gold Corp. optioned a 50% interest of the claims to Klondike Star Mineral Corp. (KSMC), which became a 50/50 joint venture in 2005. Klondike Star Mineral Corp held a 55% interest in the claims by 2005 and staked the GATA and GOTTA claims. Trenching was performed by KSMC near the Hunker Dome prospect on the GATA claims in 2006 in the vicinity of historical UKHM trenches. Several lines of a Mobile Metal Ion (MMI) soil survey were also taken along the Hunker Dome prospect in 2006. The SHE and TIE claims were also staked by Klondike Gold in 2006 and the claim group (GATA, GOTTA, SHE, GRE and TIE) became known as the Dominion property.
Klondike Gold Corp. resumed work in 2011 and purchased Klondike Star Mineral Corp. in 2015 to restore a 100% interest. Klondike Gold Corp. performed soil sampling and chip sampling in a series of trenches dug with a backhoe in 2012 on the GRE claims. In 2013 and 2014, Klondike Gold performed small prospecting and rock sampling programs on these claims. Regional orthophoto and ground magnetic surveys were performed over the Dominion claims in 2015 by Klondike Gold. Prospecting in the Hunker Dome area was also performed in 2015. In 2016, Klondike Gold drilled 10 NQ holes along a 900 m strike length in the Hunker Dome area as a follow-up to the 2015 exploration program.
Regional & Property Geology
The Hunker Dome area is located within the Klondike region, which is underlain by the Permian Klondike Schist Assemblage of the Yukon-Tanana terrane (YTT). The Klondike Schist represents a transition from plutonism to arc volcanism that has undergone greenschist facies metamorphism and consists of metaplutonic Sulphur Creek orthogneiss in the west that transitions eastward to a package of metavolcanic and metasedimentary units including: felsic to mafic (quartz-mica ± chlorite) schist, graphitic schist, and quartz augen schist (PKf and PKs). Evidence of five deformation events (D1 to D5) are present in within the Klondike Schist Assemblage as a result of obduction and regional thrusting and faulting related to uplift, which have produced a visible S2 and S3 foliation fabric in the schist units.
The Dominion group of claims owned by Klondike Gold Corp., including the Hunker Dome area on the GATA claims, straddles a north-south trending thrust fault within the Klondike Schist (Mortensen, 1996). The area is underlain by medium to dark green chlorite-quartz-actinolite schist (unit Psc) and minor metagabbro (unit Pg) in the gangingwall, which has been thrust on top of a package of micaceous quartzite and quartz-muscovite schist (unit Psq) forming the footwall.
The lithological units of the Klondike region, including the Hunker Dome, commonly contain both large, foliaform quartz veins associated with D3 folding and thrusting and discordant quartz veins possibly associated with D4 brittle faulting. Mineralization is generally hosted in the discordant quartz veins, however, the exact mineralization age and timing in the Klondike region is currently unknown. The white to locally oxidized, discordant veins are generally mineralized with sulphides (pyrite, rare galena, chalcopyrite), as well as visible gold, and are rarely more than 2-3 metres thick. Where present, visible gold is commonly noted along the selvages of both fresh and oxidized pyrite grains and can also occur as free grains within the quartz veins.
The Mitchell and Orekon veins, which lie north and northwest of King Solomon Dome and the veins on the ridge between Upper Dominion and Lombard Creeks form a large-scale en-echelon sheeted vein system. Individual veins strike north-south and dip steeply east. Some veins in the Orekon system have faulted margins, but generally the veins appear to be simple fillings of tension fractures.
Mineralization & Results
Mineralization at the Hunker Dome is commonly noted within discordant vein sets. The vein material consists mainly of white, coarsely crystalline quartz with minor ferroan carbonate and pyrite. Concentrations of galena with traces of chalcopyrite and sphalerite are present locally. Traces of tetrahedrite and arsenopyrite have also been reported from the nearby Mitchell vein (MINFILE occurrence 115O 068). Free gold occurs sporadically in the veins, generally associated with sulphides. Wallrock alteration adjacent to the veins consists of widespread introduction of brown weathering ferroan carbonate and more restricted zones of pyritization. Assay values from veins in the vicinity of King Solomon Dome vary widely. Values of up to 48.0 g/t Au and 10,457 g/t Ag have been obtained from samples of the Mitchell and Orekon veins, although most samples contain only trace amounts.
The veins on the ridge between Upper Dominion and Lombard Creeks have received the most development work of any in the Klondike District. Four veins were uncovered on surface and were explored in the early 1900's by trenches and a shallow shaft. MacLean (1914, p. 112-114) examined the property in 1912 and sampled some of the surface showings. Three samples from trenches and shafts averaged 2.7 g/t Au and 3.4 g/t Ag. The 790 m tunnel was collared approximately 150 m vertically below these showings. Between 250 m and 600 m from the portal, the tunnel intersected six veins ranging from 0.6 to 1.8 m in thickness. Very little information is available on the results of this work, but newspaper accounts report assays of up to 857 g/t Au and 125 g/t Ag.
Quartz veins containing traces of galena and pyrite are also present in old trenches and shafts on the ridge immediately west of Hunker Summit (MacKay and Summit occurrences). MacLean (1914) sampled quartz from both of these showings, but the highest assay was only 1.4 g/t Au. In 1987, United Keno Hill Mines Ltd. uncovered a system of en-echelon quartz veins which were traced in bulldozer trenches 3.5 km north from the Hunker Dome grid onto the Mackay grid. The veins are discontinuous, less than 1 m wide and carry traces of disseminated pyrite and galena. Gold values were generally low, but one sample from the Hunker Dome grid assayed 15.3 g/t Au over 3.0 m.
Hoymann and Friedrich (1992) analysed gold with pyrite inclusions from the Hunker Dome vein and found an average silver content of 12.74 wt% and an average tellurium content of 0.08 wt%. Gold intergrown with galena from the same location had an average silver content of 22.07 wt%. Three stages of mineralization were identified: (1) quartz-carbonate-gold-arsenopyrite-pyrite-pyrrhotite-chalcopyrite-galena; (2) quartz-carbonate-chalcopyrite-sphalerite-tetrahedrite-freibergite-polybasite-polyargyrite-argentite-pyrostilbnite-galena; (3) quartz-gold. Fluid inclusions contain CO2 and have salinities ranging from 0 to 7.2 wt% NaCl equivalent. Homogenization temperatures range from 390°C down to 120°C, and show a systematic decrease from Stage 1 to Stage 3.
Trenching on the Hunker Dome by Klondike Gold in 2006 returned anomalous gold values from oxidized quartz veins in two of the four trenches, with up to 1.284 g/t Au over 2.2 m and 1.5 g/t Au over 2.0 m in trench KS06-02 and 24.72 g/t Au over 0.65 m, including 1% galena and 1-2% pyrite, in trench KS06-03.
Prospecting and sampling programs performed by Klondike Gold Corp. in 2013 on the GATA claims hosting the Hunker Dome occurrence returned anomalous gold values in grab samples with up to 81.3 g/t Au near a historical shaft and 27.78 g/t Au in a quartz vein sample with galena and chalcopyrite. The follow-up 2014 and 2015 programs also yielded anomalous Au values in grab samples up to 42.6 g/t Au. Quartz veins exposed in the 2006 trenches were also resampled and returned gold values between 1 g/t Au and 371 g/t Au with up to 930 g/t Ag.
In 2016, Klondike Gold Corp. drilled 10 NQ holes on the Dominion claims, including the GATA claim, targeting outcropping gold-mineralized quartz veins that returned two significant intersects beneath historic shafts on the property of: 15.4 g/t Au over 0.34 m in DM16-01 and 1.7 g/t Au with 162 g/t Ag over 1.5 m in DM16-08.
The earliest staking was probably Pride of the Mountain cl (4218) by H.N. Coleman in June, 1900. Re-staked as a forty claim property by Aaron Knorr, commencing with Discovery, etc (6926) in May, 1904 and optioned to Dome Lode Development Company Ltd., which traced four veins on surface for 460 m with 4 shafts (4.3 to 24 m deep) and a number of trenches. In 1909-1910, a 792 m crosscut was driven at a cost of $70,000. About 25 claims were taken to lease, including some up to 3.2 km northeast. Sam Thurber blasted an open cut on the Hunker claim, adjoining to the east, in 1912. Near the road, 1.6 km to the north, W.D. MacKay put in a 15 m shaft and an open cut on the Jennie claim and J. Cameron did some trenching on the Summit claim, all prior to 1912.
Re-staked as Eleventh Hour cl (15037) in June, 1924 and Bridge, etc cl (39010) in September, 1937 by A.J. Matheson, who explored with hand pits until 1940-1942, when he cleaned out and resampled the crosscut and drifted 37 m.
Re-staked as Dominion cl 1-4 (86971) and King Solomon cl 1-7 (86975) in August, 1965 by Orekon Ltd., which bulldozer trenched in 1966 and 1972. The adit was re-staked in November, 1980 as Dominion cl 1-4 (YA55110) and King Solomon cl 1-36 (YA55114) by Lindex Exploration Ltd. and transferred to Orekon Ltd. in 1982.
Cominco added KSD cl 1-140 (YA49490) to the west in January, 1980 and carried out mapping, geochemistry and IP surveys later in the year. I. Mahoney staked a single Junker cl (YA55283) 2.5 km to the east in May, 1981 and drilled two holes (11.3 m) in 1982.
Dawson Eldorado Gold Explorations Ltd. re-staked the KSD group as Klook cl 1-48 (YA65751) in June, 1983 and explored with mapping and geochemical sampling later in the year. A joint venture between United Keno Hill Mines Ltd. (UKHM) and Falconbridge Ltd. added Dom cl 1-149 (YA80272) to the southwest in June, 1984, re-staked the old workings as Kin cl 1-82 (YA89442) in July, 1987 and performed mapping, geochemical sampling, VLF-EM surveys and bulldozer trenching in 1987 and 1988.
Barramundi Gold Ltd. staked LP cl 1-13 (YB68565) to the east in March, 1996. In March, 1999 Barramundi completed 3,850 line km of detailed airborne magnetometer and VLF-EM surveying that covered a 16 km x 24 km area centered about King Solomon Dome and included this occurrence. In 1999, Barramundi optioned the majority of Klondike claims, excluding those under option from UKHM and JAE resources, to KSL Exploration (Yukon) Ltd.
Klondike Gold Corp. (formerly Arbor Resources Inc.) staked the nearby GRE claims in 2003 and performed soil sampling and prospecting in 2004. Klondike Gold Corp. optioned a 50% interest of the claims to Klondike Star Mineral Corp. (KSMC), which became a 50/50 joint venture in 2005. Klondike Star Mineral Corp held a 55% interest in the claims by 2005 and staked the GATA and GOTTA claims. Trenching was performed by KSMC near the Hunker Dome prospect on the GATA claims in 2006 in the vicinity of historical UKHM trenches. Several lines of a Mobile Metal Ion (MMI) soil survey were also taken along the Hunker Dome prospect in 2006. The SHE and TIE claims were also staked by Klondike Gold in 2006 and the claim group (GATA, GOTTA, SHE, GRE and TIE) became known as the Dominion property.
Klondike Gold Corp. resumed work in 2011 and purchased Klondike Star Mineral Corp. in 2015 to restore a 100% interest. Klondike Gold Corp. performed soil sampling and chip sampling in a series of trenches dug with a backhoe in 2012 on the GRE claims. In 2013 and 2014, Klondike Gold performed small prospecting and rock sampling programs on these claims. Regional orthophoto and ground magnetic surveys were performed over the Dominion claims in 2015 by Klondike Gold. Prospecting in the Hunker Dome area was also performed in 2015. In 2016, Klondike Gold drilled 10 NQ holes along a 900 m strike length in the Hunker Dome area as a follow-up to the 2015 exploration program.
Regional & Property Geology
The Hunker Dome area is located within the Klondike region, which is underlain by the Permian Klondike Schist Assemblage of the Yukon-Tanana terrane (YTT). The Klondike Schist represents a transition from plutonism to arc volcanism that has undergone greenschist facies metamorphism and consists of metaplutonic Sulphur Creek orthogneiss in the west that transitions eastward to a package of metavolcanic and metasedimentary units including: felsic to mafic (quartz-mica ± chlorite) schist, graphitic schist, and quartz augen schist (PKf and PKs). Evidence of five deformation events (D1 to D5) are present in within the Klondike Schist Assemblage as a result of obduction and regional thrusting and faulting related to uplift, which have produced a visible S2 and S3 foliation fabric in the schist units.
The Dominion group of claims owned by Klondike Gold Corp., including the Hunker Dome area on the GATA claims, straddles a north-south trending thrust fault within the Klondike Schist (Mortensen, 1996). The area is underlain by medium to dark green chlorite-quartz-actinolite schist (unit Psc) and minor metagabbro (unit Pg) in the gangingwall, which has been thrust on top of a package of micaceous quartzite and quartz-muscovite schist (unit Psq) forming the footwall.
The lithological units of the Klondike region, including the Hunker Dome, commonly contain both large, foliaform quartz veins associated with D3 folding and thrusting and discordant quartz veins possibly associated with D4 brittle faulting. Mineralization is generally hosted in the discordant quartz veins, however, the exact mineralization age and timing in the Klondike region is currently unknown. The white to locally oxidized, discordant veins are generally mineralized with sulphides (pyrite, rare galena, chalcopyrite), as well as visible gold, and are rarely more than 2-3 metres thick. Where present, visible gold is commonly noted along the selvages of both fresh and oxidized pyrite grains and can also occur as free grains within the quartz veins.
The Mitchell and Orekon veins, which lie north and northwest of King Solomon Dome and the veins on the ridge between Upper Dominion and Lombard Creeks form a large-scale en-echelon sheeted vein system. Individual veins strike north-south and dip steeply east. Some veins in the Orekon system have faulted margins, but generally the veins appear to be simple fillings of tension fractures.
Mineralization & Results
Mineralization at the Hunker Dome is commonly noted within discordant vein sets. The vein material consists mainly of white, coarsely crystalline quartz with minor ferroan carbonate and pyrite. Concentrations of galena with traces of chalcopyrite and sphalerite are present locally. Traces of tetrahedrite and arsenopyrite have also been reported from the nearby Mitchell vein (MINFILE occurrence 115O 068). Free gold occurs sporadically in the veins, generally associated with sulphides. Wallrock alteration adjacent to the veins consists of widespread introduction of brown weathering ferroan carbonate and more restricted zones of pyritization. Assay values from veins in the vicinity of King Solomon Dome vary widely. Values of up to 48.0 g/t Au and 10,457 g/t Ag have been obtained from samples of the Mitchell and Orekon veins, although most samples contain only trace amounts.
The veins on the ridge between Upper Dominion and Lombard Creeks have received the most development work of any in the Klondike District. Four veins were uncovered on surface and were explored in the early 1900's by trenches and a shallow shaft. MacLean (1914, p. 112-114) examined the property in 1912 and sampled some of the surface showings. Three samples from trenches and shafts averaged 2.7 g/t Au and 3.4 g/t Ag. The 790 m tunnel was collared approximately 150 m vertically below these showings. Between 250 m and 600 m from the portal, the tunnel intersected six veins ranging from 0.6 to 1.8 m in thickness. Very little information is available on the results of this work, but newspaper accounts report assays of up to 857 g/t Au and 125 g/t Ag.
Quartz veins containing traces of galena and pyrite are also present in old trenches and shafts on the ridge immediately west of Hunker Summit (MacKay and Summit occurrences). MacLean (1914) sampled quartz from both of these showings, but the highest assay was only 1.4 g/t Au. In 1987, United Keno Hill Mines Ltd. uncovered a system of en-echelon quartz veins which were traced in bulldozer trenches 3.5 km north from the Hunker Dome grid onto the Mackay grid. The veins are discontinuous, less than 1 m wide and carry traces of disseminated pyrite and galena. Gold values were generally low, but one sample from the Hunker Dome grid assayed 15.3 g/t Au over 3.0 m.
Hoymann and Friedrich (1992) analysed gold with pyrite inclusions from the Hunker Dome vein and found an average silver content of 12.74 wt% and an average tellurium content of 0.08 wt%. Gold intergrown with galena from the same location had an average silver content of 22.07 wt%. Three stages of mineralization were identified: (1) quartz-carbonate-gold-arsenopyrite-pyrite-pyrrhotite-chalcopyrite-galena; (2) quartz-carbonate-chalcopyrite-sphalerite-tetrahedrite-freibergite-polybasite-polyargyrite-argentite-pyrostilbnite-galena; (3) quartz-gold. Fluid inclusions contain CO2 and have salinities ranging from 0 to 7.2 wt% NaCl equivalent. Homogenization temperatures range from 390°C down to 120°C, and show a systematic decrease from Stage 1 to Stage 3.
Trenching on the Hunker Dome by Klondike Gold in 2006 returned anomalous gold values from oxidized quartz veins in two of the four trenches, with up to 1.284 g/t Au over 2.2 m and 1.5 g/t Au over 2.0 m in trench KS06-02 and 24.72 g/t Au over 0.65 m, including 1% galena and 1-2% pyrite, in trench KS06-03.
Prospecting and sampling programs performed by Klondike Gold Corp. in 2013 on the GATA claims hosting the Hunker Dome occurrence returned anomalous gold values in grab samples with up to 81.3 g/t Au near a historical shaft and 27.78 g/t Au in a quartz vein sample with galena and chalcopyrite. The follow-up 2014 and 2015 programs also yielded anomalous Au values in grab samples up to 42.6 g/t Au. Quartz veins exposed in the 2006 trenches were also resampled and returned gold values between 1 g/t Au and 371 g/t Au with up to 930 g/t Ag.
In 2016, Klondike Gold Corp. drilled 10 NQ holes on the Dominion claims, including the GATA claim, targeting outcropping gold-mineralized quartz veins that returned two significant intersects beneath historic shafts on the property of: 15.4 g/t Au over 0.34 m in DM16-01 and 1.7 g/t Au with 162 g/t Ag over 1.5 m in DM16-08.
Location Map
Last Updated: Dec 4, 2019
Work History
| Year | Work Type | Comment |
|---|---|---|
| 2016 | Drilling: Diamond | A total of 10 NQ holes were drilled near the Hunker Dome area. |
| 2015 | Airphotography: Orthophoto | |
| 2015 | Ground Geophysics: Magnetics | |
| 2015 | Other: Prospecting | |
| 2014 | Geochemistry: Rock | |
| 2014 | Other: Prospecting | |
| 2013 | Geochemistry: Rock | Rock and chip sampling from 2006 trenches. |
| 2013 | Other: Prospecting | |
| 2006 | Geochemistry: Soil | Mobile Metal Ion (MMI) survey. |
| 2006 | Trenching: Mechanical | Trenching performed in the vicinity of historical UKHM trenches. |
| 1999 | Airborne Geophysics: Magnetic | Also VLF-EM survey. |
| 1988 | Geochemistry: Soil | |
| 1988 | Geology: Bedrock Mapping | |
| 1988 | Ground Geophysics: EM | Also VLF survey. |
| 1988 | Trenching: Mechanical | |
| 1987 | Geochemistry: Soil | |
| 1987 | Geology: Bedrock Mapping | |
| 1987 | Ground Geophysics: EM | Also VLF survey. |
| 1987 | Trenching: Mechanical | |
| 1983 | Geochemistry: Soil | |
| 1983 | Geology: Bedrock Mapping | |
| 1982 | Drilling: Diamond | Two holes, 11.3 m. |
| 1980 | Geochemistry: Rock | |
| 1980 | Geochemistry: Soil | |
| 1980 | Geology: Bedrock Mapping | |
| 1980 | Ground Geophysics: IP | |
| 1972 | Trenching: Mechanical | |
| 1966 | Trenching: Mechanical | |
| 1942 | Development, Underground: Rehabilitation | Also minor drifting. |
| 1942 | Geochemistry: Rock | |
| 1942 | Trenching: Hand | |
| 1941 | Trenching: Hand | |
| 1940 | Trenching: Hand | |
| 1912 | Development, Underground: Shaft Development | Sunk a 15.24 m shaft. |
| 1912 | Trenching: Hand | Blasted on open cut. |
| 1910 | Development, Underground: Drifting/Raising | |
| 1904 | Development, Underground: Shaft Development | Sunk 4 shafts (4.27 to 24.38 m deep). |
| 1904 | Trenching: Hand |
Regional Geology - Terrane
Group: Intermontane
Affinity: W Laurentia
Name: Yukon-Tanana
Realm: peri-Laurentian
Regional Geology - Bedrock
Supergroup:
Group/Suite: Klondike
Formation:
Member:
Terrane: Yukon-Tanana
Period Max: Permian
Age Max: 271 MA
Period Min: Permian
Age Min: 251 MA
Rock Major: quartzite/qt-ms-cl schist/gneiss/amphibolite
Rock Minor:
Reference: Mortensen (1996) - YGS OF 1996-1(G)
Geological Unit (1M): PK
Geological Unit (250K): PK2
Assessment Reports that overlap occurrence
| Report Number | Year | Title | Worktypes | Holes Drilled | Meters Drilled |
|---|---|---|---|---|---|
| 096818 | 2014 | Prospecting Report on the Dominion Project | Rock - Geochemistry, Prospecting - Other | ||
| 096879 | 2014 | Ground Magnetics, Orthophoto and Prospecting Report on the Dominion Project | Orthophoto - Airphotography, Magnetics - Ground Geophysics, Prospecting - Other | ||
| 096563 | 2013 | 2013 Geochemical Assessment Report on the Dominion Project | Rock - Geochemistry, Rock - Geochemistry, Prospecting - Other, Prospecting - Other | ||
| 094783 | 2006 | Geological Mapping, Trenching, Rock, and Soil Geochemical Sampling on the Dominion Property | Soil - Geochemistry, Bedrock Mapping - Geology, Backhoe - Trenching | ||
| 094021 | 1999 | Detailed Airborne Magnetics and VLF-EM over the Klondike District, Dawson City - 1999 | Electromagnetic - Airborne Geophysics, Magnetic - Airborne Geophysics | ||
| 093711 | 1996 | JAE Mapping Report 1996 A Geological and Geochemical Report for the Hunker Dome Project | Rock - Geochemistry, Soil - Geochemistry, Bedrock Mapping - Geology | ||
| 092743 | 1988 | Geological Mapping and Trenching of the 1987 Soil Geochemical Anomalies on the Mackay, Dominion, Hunker, Dome, and King Solomon Dome Grids | Rock - Geochemistry, Soil - Geochemistry, Bedrock Mapping - Geology, Mechanical - Trenching | ||
| 092600 | 1987 | Geological and Geochemical Exploration of the Mackay, Dominion, King Solomon Dome, Hunker Dome, Lombard, Lloyd, Lloyd II, Lloyd III, Green Gulch, and Dominion Mountain Grids - Hunker Summit Area | Rock - Geochemistry, Soil - Geochemistry, Bedrock Mapping - Geology, Prospecting - Other, Mechanical - Trenching | ||
| 091634 | 1984 | Report on the 1984 Exploration Program in Klondike Gold Fields | Electromagnetic - Airborne Geophysics, Percussion - Drilling, Drill Cuttings - Geochemistry, EM - Ground Geophysics | 95 | 6900.67 |
| 091561 | 1983 | Assessment Report on Klook 1-48 Claims | Soil - Geochemistry, Regional Bedrock Mapping - Geology | ||
| 090769 | 1980 | Geochemical Assessment Report on the KSD Claim Group | Rock - Geochemistry, Soil - Geochemistry, Bedrock Mapping - Geology, IP - Ground Geophysics, Line Cutting - Other, Prospecting - Other | ||
| 060149 | 1972 | Geological and Geochemical Report Yukon Quartz Mineral Claims | Silt - Geochemistry, Soil - Geochemistry |
Related References
| Number | Title | Page(s) | Document Type |
|---|---|---|---|
| 1992GeolVol3_18 | Gold and sulphide mineralization in the Hunker Creek area, Yukon Territory, Canada | Annual Report Paper | |
| 1992GeolVol3_15 | Preliminary observations on the geology and geochemistry of quartz veins in the Klondike District, west-central Yukon | Annual Report Paper | |
| 1996-1(G) | Geological Compilation Maps of the Northern Stewart River Area, Klondike and Sixtymile Districts (115N/15, 16, 115O/13, 14 and Parts of 115O/15, 16) | Open File (Geological - Bedrock) | |
| 1991Rushton | A fluid inclusion and stable isotope study of mesothermal gold-quartz veins in the Klondike Schists, Yukon Territory | MSc Thesis |
| Citations |
|---|
| Department of the Interior, 1916. The Yukon Territory - Its History and Resources, p. 116-120. |
| Klondike Gold Corp. and Klondike Star Mineral Corp., 2013. Assessment Report #096563 by I. Mitchell, W. Mann and K. Dodd. |
| Klondike Gold Corp., 2014. Assessment Report #096818 by P. Tallman. |
| Klondike Gold Corp., 2015. Assessment Report #096879 by P. Tallman. |
| Klondike Gold Corp., Management Discussion & Analysis: 30 Nov/2015 and 30 Nov/2016. |
| Klondike Gold Corp., News Releases: 16 Jul/2015, 24 Sept/2015, 14 Jul/2016, 10 Aug/2016, and 28 Sep/2016. |
| MacLean, T.A., 1914. Lode Mining in Yukon. Mines Branch Publication 222, p. 106, 112-114. |
