filename;drill_core;outcrop;hand_sample;structure;misc;caption
Figure 2 Anvil_range_from_trench.jpg;no;no;no;no;yes;Looking northeast from Robert Campbell Highway in 1995. Tintina Trench is in foreground. The south edge of the town of Faro is visible on left edge of photograph. The central area is Vangorda Plateau. Rock waste dumps from mining of Grum deposit are in the centre of the Vangorda Plateau. The Anvil Range forms mountains in background.
TitlePhoto2 Faro Blast 1979.jpg;no;no;no;no;yes;Faro blast; 1979.
Figure 5 3G0_core.jpg;yes;no;no;no;no;Mount Mye formation phyllite. BQ-size core. Core breaks on finely spaced crenulation cleavage which forms the dominant foliation. Note minor colour variations are transposed subparallel to dominant foliation. Drill hole CNR76-01; 426 ft - 449 ft (130 m - 137 m).
Figure 7 1CD_core.jpg;yes;no;no;no;no;Mount Mye formation. NQ-size core. Biotite-andalusite clots and clusters within matrix of biotite-muscovite phyllite transitional to schist. Dominant foliation is closely spaced crenulation cleavage. Drill hole 84F-28.
Figure 12 Mt_Mye_3d_79F_01.jpg;yes;no;no;no;no;Calc-silicate rock in Mount Mye formation. Drill hole 79F-01; 258 feet - 264 feet (78.6 m to 80.5 m). NQ-size core. Dark bands are biotite-rich pelite and light bands are calc-silicate rock.
Figure 15 Vangorda_phyllite_core.jpg;yes;no;no;no;no;Vangorda formation phyllite. NQ-size core. Pelitic bands are silvery grey. Siltstone interbands are pale cream and have a grainy texture. Dominant cleavage going across core is S2 axial planar crenulation cleavage. Note microfolds between S2 cleavages. Smallest division on scale is 1 mm.
Figure 18 Vangorda_cs_core.jpg;yes;no;no;no;no;Vanagorda formation. NQ-sized core. Calc-silicate rock from diamond drill hole 84F-09; 89 m - 95 m.
Figure 20 5A_typo_core.jpg;yes;no;no;no;no;Basal carbonaceous phyllite member of Vangorda formation. BQ-sized drill core from diamond drill hole CNR76-02; 304 m to 312 m. Disseminated pyrite cubes form rusty splotches in core.
Figure 50 5C_foliated_CNR76_04_67f_90f.jpg;yes;no;no;no;no;Ordovician-Silurian gabbro sill in Vangorda formation. Margin of sill is located immediately to right of flagging in the second row from the top. The sill margin is strongly foliated. Lower rows are less foliated and display relict igneous texture. Drill Hole CNR76-04. Depth 67 feet to 90 feet (20 to 27 m). BQ-size core.
Figure 51 5C4_fuchsite_FAGU189_18m_25m.jpg;yes;no;no;no;no;Strongly quartz-carbonate altered Ordovician-Silurian gabbro sill in Grum deposit. Sill is strongly foliated and is located in middle row of core. Drill hole FAGU189; 17.9-25 m. BQ-size core.
Figure 60 D1_fold_core.jpg;no;no;no;yes;no;D1 minor fold defined by siltstone bed in Vangorda formation. Drill hole 76X-11; 72 ft (22 m). Drill hole located in Dy/Grizzly deposit area. NQ-size core.
Figure 64 D2_fold_core.jpg;no;no;no;yes;no;D2 minor fold in Vangorda formation. S2 axial plane crenulation cleavage dips steeply to right in picture. NQ-size core. Drill hole 72X-23; 84 ft (26 m).
Figure 66 fault_rock.jpg;no;no;no;yes;no;Extensional fault rock; Vangorda Plateau. Clasts of quartz vein and highly altered mafic gabbro dyke in sheared and gouged carbonaceous phyllite fault rock matrix. NQ size core. Drill hole 81VX-01; 395-400 m.
Figure 4 98LP149-1.jpg;no;no;yes;no;no;Mount Mye formation phyllite. Weathering consists of a brownish coating. Bedding is visible progressing from top to bottom of photo near the centre. Canadian penny is 1.9 cm across.
Figure 8 98LP138_1CDstaur.jpg;no;no;yes;no;no;Mount Mye formation. Staurolite-garnet-biotite-muscovite-quartz schist. Dominant foliation is a closely spaced crenulation cleavage. Major division of scale is 1 cm. Field station 98LP138.
Figure 9 98LP171_3A.jpg;no;no;yes;no;no;Carbonaceous phyllite within Mount Mye formation. Penny is 1.9 cm across. Field station 98LP171.
Figure 21 98LP026_5Dfield.JPG;no;no;yes;no;no;Contact hornfelsed Vangorda formation phyllite adjacent to massive greenstone lens. Light bands are quartzcalcite siltstone and dark bands are greenish muscovite-quartz-chlorite phyllite. Field station 98LP026 on Swim Lake road.
Figure 32 Duo_Lake_hornfels_99LP280.jpg;no;no;yes;no;no;Black argillite of Duo Lake Formation. Field station 98LP099.
Figure 54 84_50_Anvil_suite_3.jpg;no;no;yes;no;no;Anvil plutonic suite. Slightly foliated biotite-muscovite granite. Stained for K-feldspar. Penny is 1.9 cm across. Field station 84-50.
Figure 56 10E-2xx_NWdyke.JPG;no;no;yes;no;no;Tay River plutonic suite. Equigranular biotite-plagioclase-K-feldspar-quartz granite. Sample from northwest wall of Faro open pit.
Figure 57 Tertiary_plug_2.jpg;no;no;yes;no;no;Eocene quartz-feldspar porphyry. Flow-banded with scattered clear and grey quartz phenocrysts. Field station 99LP228. Penny is 1.9 cm across.
Figure 58 10F_Mine_dumps.jpg;no;no;yes;no;no;Eocene quartz-feldspar porphyry. Smokey quartz and small white feldspar phenocrysts. Sample from northeast wall of Faro open pit. Penny is 1.9 cm across.
Figure 6 1CD_andalusite_LP98_3_24.jpg;no;yes;no;no;no;Mount Mye formation phyllite transitional to schist with andalusite prisms pseudomorphed by dark green chlorite. Pencil is 14 cm long. Southwest wall of Faro open pit.
Figure 10 3F0_outcrop_stn87_24.jpg;no;yes;no;no;no;Marble interval in Mount Mye formation. Banding delineated by schist and calc-silicate bands and boudins in marble. Clipboard is 25.5 cm wide. Field station 87LP024.
Figure 11 3F0_98LP015.jpg;no;yes;no;no;no;Closeup view of marble interval in Mount Mye formation. Abundant siliceous bands and boudins in a marble matrix. Pencil is 14 cm long. Siliceous bands parallel dominant foliation. Foliation is locally cross-cut by later shear bands. Field station 98LP015; in immediate hanging wall of extensional Tie fault.
Figure 13 3D_mt_mye_outcrop.jpg;no;yes;no;no;no;Calc-silicate rock in Mount Mye formation. Thinly interbedded pale greenish calc-silicate rock and dark brown biotite schist. Outcrop strongly folded. Axial planar foliation is crenulation cleavage which forms dominant foliation in the outcrop. Field station 98LP142.
Figure 14 Vangorda_phyllite_1.jpg;no;yes;no;no;no;Vangorda formation phyllite. Light grey to white quartz-calcite siltstone interbeds in silvery grey; noncalcareous to slightly calcareous muscovite-chlorite phyllite. Coin is 2.7 cm wide.
Figure 16 Vangorda_fm_LP99_302a.jpg;no;yes;no;no;no;Vangorda formation phyllite. Thin limestone interbeds in phyllite. Slaty cleavage is subhorizontal. Field station 99LP302. Solid division on scale is 1 cm.
Figure 17 Vangorda_cs_faro_pit.jpg;no;yes;no;no;no;Vangorda formation. Calc-silicate rock outcrop in southwest wall of Faro deposit open pit. Pale green calc-silicate rock bands and lenses; interbedded with dark purplish brown to grey biotite-rich bands and lenses. Pencil on right side of photo is 14.5 cm long.
Figure 19 5A_98LP024.jpg;no;yes;no;no;no;Basal carbonaceous phyllite member of Vangorda formation. Outcrop located on the edge of the Swim Lake road; field station 98LP024. Fractures have orange weathering surface coating.
Figure 22 99LP258A_Menzie_pillows.jpg;no;yes;no;no;no;Menzie Creek formation. Pillow basalt flow. Field station 99LP258A.
Figure 23 99LP209_Menzie_isolated_pillows.jpg;no;yes;no;no;no;Menzie Creek formation. Isolated pillows in chloritic matrix; pillow basalt flow. Field station 99LP209.
Figure 24 99LP214_Menzie_pillow_in_breccia.jpg;no;yes;no;no;no;Menzie Creek formation. Isolated pillow in monolithic basalt breccia. Pencil magnet is 12.5 cm long. Field station 99LP214.
Figure 25 99LP220_Menzie_breccia.jpg;no;yes;no;no;no;Menzie Creek formation; clast supported; monolithic; basalt breccia. Field station 99LP220.
Figure 26 98LP181_Menzie_breccia_2.jpg;no;yes;no;no;no;Menzie Creek formation; matrix supported; monolithic; basalt breccia. Field station 98LP181.
Figure 27 99LP218_Menzie_epiclastic.jpg;no;yes;no;no;no;Menzie Creek formation. Epiclastic volcanic sandstone. Field station 99LP218.
Figure 30 99LP284_Menzie_overlies_Road_River.jpg;no;yes;no;no;no;Altered and hornfelsed Duo Lake Formation carbonaceous phyllite. Field station 99LP280.
Figure 31 Duo_Lake_98LP099.jpg;no;yes;no;no;no;Carbonaceous shale of Duo Lake Formation conformably overlain by pillow basalt of Menzie Creek formation. Primary bedding dips gently to the left. Slaty cleavage dips about 45 degrees to the left. Field station 99LP238.
Figure 37 98LP057_green_arg.jpg;no;yes;no;no;no;Mount Aho formation; pale green argillite. Field station 98LP057.
Figure 38 98LP049_maroon_cht.jpg;no;yes;no;no;no;Maroon chert and siliceous argillite; Mount Aho formation - lower member DCMAgr. Maroon chert and argillite is intimately interbedded with green chert and argillite. Field station 98LP049.
Figure 39 98LP044_congl_arg.jpg;no;yes;no;no;no;Mount Aho formation - lower member DCMAgr. Chert-pebble conglomerate interval within argillite. Bedding is nearly horizontal. Conglomerate is in centre of picture. Slaty cleavage is oriented parallel to the pencil magnet; going from lower left to upper right across the picture. Pencil magnet is 12.5 cm long. Field station 98LP044.
Figure 40 98LP114_bedded_lmst.jpg;no;yes;no;no;no;Mount Aho formation - upper member DCMAbl. Black silty chert interbedded with dark grey; fine-grained; silty limestone. A 35-cm-thick limestone bed occurs under the rock hammer. Bedding dips steeply to the right side of the picture. Field station 98LP114.
Figure 41 98LP055_blk_congl.jpg;no;yes;no;no;no;Mount Aho formation - upper member DCMAbl. Black chert-pebble conglomerate. Field station 98LP055.
Figure 42 99LP131_barite_chert.jpg;no;yes;no;no;no;Mount Aho formation. Interbedded grey barite and pale tan chert. Field station 99LP131.
Figure 43 99LP131_barite.jpg;no;yes;no;no;no;Mount Aho formation; bedded barite. Slaty cleavage oriented horizontally in this picture. Field station 99LP131.
Figure 44 98LP107_bedded_cht.jpg;no;yes;no;no;no;Rose Mountain formation; pale cream; phyllitic; bedded chert. Field station 98LP107.
Figure 45 99LP068_Rose_Mtn_red_cht.jpg;no;yes;no;no;no;Rose Mountain formation red chert. Bedding is near vertical. Spaced fracture cleavage dips steeply left. Field station 99LP068.
Figure 46 PCR_basalt.jpg;no;yes;no;no;no;Campbell Range formation. Autobrecciated texture with epidote well developed in matrix. Pencil magnet is 12.5 cm long. Late cross-cutting quartz vein. Field station 99LP207.
Figure 47 PCR_chert_and_basalt_P99LP051.jpg;no;yes;no;no;no;Campbell Range formation green chert interbedded with basalt. Field station 99LP048. Bedding contact is near-vertical in centre of photo with chert being on the left.
Figure 55 99LP014_granite_contact.jpg;no;yes;no;no;no;Anvil plutonic suite. Granite contact with overlying Vangorda formation calc-silicate rock. Contact proceeds from upper left to lower right across photograph. Left end of pencil is approximately on the contact. Pencil is 14.5 cm long. Field station 99LP014.
Figure 59 D1_fold_outcrop.jpg;no;no;no;yes;no;Small D1 fold in Vangorda formation adjacent to Ordovician-Silurian gabbro sill. Outcrop located in Dy/Grizzly deposit area. D1 axial plane is near vertical. Re-folded by near-horizontal D2 minor fold. Pencil (14 cm long) is oriented parallel to the S2 axial planar crenulation cleavage.
Figure 61 98LP164_d1_fold_NE_District_2.jpg;no;no;no;yes;no;D1 minor fold in silty limestone beds; Vangorda formation. Fold closure visible on left side of photo. Field station 98LP164.
Figure 62 99LP164_D1_rose_mtn.jpg;no;no;no;yes;no;Macroscopic northeast-verging; D1 minor fold on northeast slope of Rose Mountain. Looking north; person is standing in steep limb. Beds in upper left and lower right parts of picture are structurally upright. Field station 99LP164.
Figure 65 99LP149_d2_fold_YTT.jpg;no;no;no;yes;no;D2 minor fold with incipiently developed S2 axial-planar crenulation cleavage; micaceous quartzite in Yukon-Tanana Terrane. Field station 99LP149. S2 fabric parallel to handle of rock hammer.
Figure 67 84_4_S_C_banding_in_Anvil_Batholith.jpg;no;no;no;yes;no;S-C banding in Anvil Batholith in immediate footwall of Tie fault. S-foliation dips gently to west. C-bands are parallel to edge of scale card. Field station 84-4.
Figure 70 Discovery_showing_Vangorda_1980.jpg;no;yes;no;no;no;Discovery showing on Vangorda Creek. Exposed outcrop consists of highly weathered quartzose mineralization. Staked in 1953 by Al Kulan. Camera lens on left side of photograph is 49 mm across.
Figure 71 JRV_sulphide_float.jpg;no;yes;no;no;no;Float boulder of sulphide mineral breccia in Anvil plutonic suite granite. JRV property; Ace High Creek; north of Mount Mye.