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Bedrock Geology Map of the Wolfville-Windsor Area, NTS Sheet

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Bedrock Geology Map of the Wolfville-Windsor Area, NTS Sheet Nova Scotia Department of Natural Resources Mineral Resources Branch 64°30' 3 Open File Map ME 2000-3, Version 2 83000mE 84 85 86 87 88 89 390 91 92 93 94 45°15' 95 96 97 98 99 400 01 02 E*Fs 03 04 05 06 07 08 09 410 64°00' 11 12 13 14 15 16 17 18 19 420 4 000m S c o t s 21 E N A - N - Bedrock Geology Map of - 45°15' B a 2 y 1 10 1 - 0 5 0 000m 5 5 000m 0 Mn,Ba L^Fw 0 0 0 11 0 Geology Legend 6 0 0 0 10 11 H01-009 0 0 18 0 50 the Wolfville-Windsor Area, 50 m m m m m 7 m 7 Fundy Basin E#Hcv C Shubenacadie Kennetcook Musquodoboit 75 NTS Sheet 21H/01 and E#Wm part of 21A/16, Basin 50 . (Windsor) Basin Basin 12 10 m m 49 CENOZOIC F 35 50 F 10 Rawdon Block y in ic 8 a a zo Kennetcook B nt so E#Hh/m ts ou e Hants and Kings Counties, o M y Thrust Fault Rawdon Fault 8 6 18 c M d t S e i 55 R QUATERNARY not differentiated but widely distributed on this bedrock geology map, includes: h t c m Chaswood Fm. 15 r rt je or 11 w e o o f a N Pr on Chaswood Formation 31 E#Hh/u H p 10 i c 60 i 8 n 8 16 8 ! t n U r h o 8 S y e 8 . 5 RECENT: swamp, stream, tidal deposits and muds with associated rootlet beds, peat and parts of fossil trees r s t 48 o m 6 10 60 t r F C n L^Fw e Nova Scotia n o o Scotch Village Fm. v i u o t 8 8 id a n C o n e m c m r h D 09 lo o e n E#Hcv t 16 v PLEISTOCENE: glacial till and ablation till including gravelly tills with a high stone content, loca Sha /C u r a w h rchill Mine F v Watering Brook Fm. t B New r io 12 a e e G t ll r k Watering Brook Fm. n t Gays 10 09 u i M e i a t lly distributed, and may rest on the earlier glacial units; glaciofluvial deposits including eskers, kames, kame e o u v Q i C Mn, Ba 82 ? f u terraces, deltas and outwash; ground moraine deposits including sandy, silty, clayey till, unsorted i l r t m 77 r F 10 E#Hh/m o p a r r u o o 65 r U 52 Canaan h s r m o River e W p a y r o and unstratified with a stone content in a great size range. In the Bay of Fundy this unit is called Scotian p m r R o F n 6 c n e r o F Shelf drift. Thickness of these units in the region ranges from nil to >30 m. a a s t 20 L^Fb r y P d u t k i F a e H i e or n Fm. h Fm. o O n s m n W n F a ation Gree a 64 6 p o r - q d R.G. Moore, S.A. Ferguson, r a u e pre-Quaternary regional unconformity R.C. Boehner and C.M. Kennedy t u id G 78 45 Mn,Ba o Series of northeast t h m n l L s a t a i r f ke H01-011 h i e Mn,Ba s B Z F r 8 t orm h trending fold axis at 85 o a e o 86 e e tio a lu n n g E#Hh/u a l MacDonald H01-012 s Kentville a R t f e e 5 -1 0 t d 0 0 m in ervals 85 f f h i M MESOZOIC F o E*Fn Wentworth Station Formation Road Formation 40 c o o Ba,Fe o 75 Fm. M 50 c r 65 50 l w k m 8 i d Stephens 40 08 d a Carrolls Coldstream 15 57 Ba,Mn H01-010 F d 8 Scale 1:50 000 t e m l i 75 Mine 08 n . e o Miller Creek Formation 62 H01-014 d Formation Ì n 8 H Corner CRETACEOUS (Early) s o 22 a 10123km r Ì c to Salem-Admiral Fm. Gays River E#Wws n 60 15 Mn h n 42 B 65 L^Fw 50 Ba d Rock Thrust 30 e Ì 42 7 Halifax L Formation 88 l 58 Î H01-013 CHASWOOD FORMATION u m o 40 H01-044 (E"c): zeolite w ff 50 f silica sand, grey and red kaolinitic clay, minor lignite; fluvial sediments near coastal floodplain deposits near the Mesozoic 50 a e F Stewiacke Formation E#Wwq r 37 a E"c localities are known in the gypsum quarry at Miller Creek and McKay Settlement areas, also suspecte continent/Atlantic Ocean coastal margin. Outcrop Halifax, Nova Scotia Formation o 37 55 E#Hcv u H01-050 H r 25 t d presence in the recent exploration by Metall Mining in the Goshen area near Walton. Thickness of these m l zeolite 20 i o L^Fw 82 in the region ranges from nil to >60 m. t c units Fe 70 2009 r a t t e H01-052 o io Halifax 55 E#Wm E#Wmr a n 40 H01-006 d pre-Cretaceous regional unconformity Series of northea t l B n W s l 07 hi Fe Ì t m L^Fw ? Meguma Group lu e Q on a trending fold axis at y f uarry Formati re Formation E#Hh/m 60 50 07 IN f st n H01-005 45 A . d o Ì 25 1 T F Fm l ti - 00 m intervals UN m Macumber Co a 50 30 Mn JURASSIC (Early) O South m 45 M . or Goldenville 78 55 GL-6-1 TH F H01-015 20 E#Hh/m FUNDY GROUP OR Musquodoboit 27 GL-6-3 Walton Mine N Formation TS Mountain Cheverie Formation A 53 40 60 L 28 35 68 Cu Zn Mn Ba Pb Ag BC-83-10 E#Hh/m F 35 54 Halifax Batholith E 35 45 GL-6-4 17 Batholith G 45 GL-6-2 SCOTS BAY FORMATION (E*Fs): light coloured interbedded sandstone, limestone and claystone, variably calcareous, with chert and jasperoid replacements of D Ì AV-J-2 I BC-83-9 Formation R B 68 E*Fs post-volcanic fluvial-lacustrine (thermal spring altered) sediments. Thickness ranges from 8 m in t limestone near the base (thermal spring activity), Crown Copyright © 2009, Province of Nova Scotia, all rights reserved. M 74 53 Î 80 85 BC-83-11 06 A 58 73 gypsum TZ-136-1 ype section up to 369 m in Bay of Fundy (including correlative McCoy Brook Formation in Chinampas N-37 well) C 23 disconformity 35 BC-83-8 06 H01-037 E#Hh/l Goldenville Î Î NaCl Ì Walton Mine Area: 46 20 Î Feuchtwagner Formation 88 65 S-67-7 H01-048 Î 28 Ì 35 83 Multiple Drillholes E#Hh/u Meguma Group Î TRIASSIC - JURASSIC South 85 Mine Ì 57 80 80 Î 75 Ì 35 Î 50 35 60 71 4 48 ND-12 Mountain 40 57 H 10 30 E#Hh/u 25 50 Mn,Ba,Fe BC-83-12 NORTH MOUNTAIN FORMATION 25 (E*Fn): tholeiitic basalt, massive, columnar and amygdaloidal flows with variable zeolite and silica minerals, rare thin (< 1 m) inte Ì 25 Mn,Ba,Fe 65 Meguma Group H01-016, 80 flow units typically thick single flows of massive columnar jointed, coarse-grained basalt (up to Batholith 35 rflow siliciclastic interbeds, lower and upper Regional Key Map 25 50 H01-017 E*Fn 55 H01-039 ? 190 m) with a middle unit comprising multiple thin amygdaloidal flows. Regionally distributed tholeiitic plateau Ì 35 Sturgis basalt (Fundy Rift). Thickness is approximately 274 m in the map area, and may exceed 400 m near Di 05 45 E#Hh/m 20 55 32 47 gby and in the Bay of Fundy. Mine 05 Î 75 paraconformity 80 zeolite Î 63 20 11 22 65 66°W 64°W 30 H01-051 62°W 60°W 17 15 30 23 25 42 32 27 40 NSDM6174 Highly simplified diagrammatic representation of the geological map units in the Wolfville and Windsor area. 50 Ì TRIASSIC (Late) 25 46 31 40 Series of northeast Ì E#Wwq AV-J-1 WS-6 35 32 NSDM6173 trending fold axis at 25 50 25 20 Mn WS-5 45 BLOMIDON FORMATION 25-75 m intervals (L^Fb) 36 WS-4 : interbedded mudrocks including laminated and cross-bedded red shale, siltstone, fine sandstone. Distal (intra)continental ri 48 Ì H01-018 WS-7 E#Wmr 20 mudflat (locally gypsiferous) and minor aeolian sediments. Thickness up to 370 m in the type area n NSDM6177 25 IP-1 L^Fb fluvial-deltaic, ft basin (arid-aeolian) lacustrine, playa, 65 04 30 40 E#Hh/m Fe,Mn 70 E#Wws 04 conformable gradational contact ear Cape Blomidon and 1100 m in the Bay of Fundy (Chinampas 10 N-37 well).
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