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VSWCB PLANN�NU BULL,LlM dit),
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<br />ny _srifl �!Lm UlAami, DESCI
<br />Predorninsint consohdated ra
<br />Cambrian Light grey ta greenish-grey phyllite interbedded and wippabihty and increasii
<br />with layers of f ine-grained quartzite, locally upper-case letiers, Leaseerzai
<br />(4Z h Hampton calcareous, some graywachy and medium to thick- fallfied uxh; at nmaive ro
<br />(Harpers), bedded, coarse, -grained ivartz sandstone.
<br />Formation b SHANC
<br />Otis,
<br />Cambrian Light grey-to-white, Ane-grained, finely- =1
<br />I ami nated- to bonded cium-tzite. Some quartz- sffly
<br />Wevertort pebble conglomerate, pebbly quartz sandstone, ado
<br />Formation and very sericitic sarielstorn, phyllite and sandy ify a
<br />phyllite, thin
<br />b SANDS1
<br />Upper Pre- Interbedded, reddish- "role, tuffaceous 12:1
<br />Cambrian phyl I i te; dark-green metabasa 1 +, white. pink and to g
<br />d f stzd q ze cal,.. tan rhislitic metatuf, iV rs
<br />CT-a o t i.' n meta-sediments; metabasalt, basaltic flow
<br />Forlte n
<br />ion breccias, epidosite and purple amygdaJoidal
<br />slate. sarat
<br />Willi
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<br />Upper Pre- Heterisgentsus unit of metagraywacke, irieta arkose, schi
<br />Cambrian and phyllites. Ov"alll textwe ranges froin Am
<br />gneissic boulder beds Wward through cobble beds bhd
<br />Kp,cs) Swift Run and arkoses to (yoss-beked, meThm-grained WM QUAR11
<br />Formation arkose and platy-bedded sandstone. 12:1 dorl,
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<br />gIon
<br />bed,
<br />Pre-Cambrian Light- to -dark gray, meTurn-grained granitic Li r
<br />rock, including quartz monzonite syenitic ano
<br />(Pfm) flaashal I granite and augen gneiss. Felsic and mafic dike dw
<br />1019) Formation intrusions.
<br />rate
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<br />IYLAND, LJSGS Ml SC, INV, SER ES MAP 1-1313-C
<br />ROCK INPES
<br />rchar W d"newmg eme W excavatton
<br />atenn rock nairw and inap symbol an
<br />are rock stmicaue Is, bedded rmlin 1,
<br />IT] M
<br />BAMLT-- nAva haws inunnevialed WIM st"Uhed SeNme
<br />oacks. Gray-green I,.,) blaCk, Owtljo` harc, Iriled,j),
<br />purphsh brown, fsjyjjuij�ncals, mirace-
<br />mosaic of equigranuiw, subhedri fekkpar
<br />idspathic siltsteole, locaflie ferssiidercnm
<br />pyroxene Orlit jn pan porphy/rific
<br />wk red (h) places _.,t". it to Tyl hWA5
<br />'elck � � . e
<br />, par phenocrysts, in pan. diabajs�c i�l �'(X L,`
<br />or beds of HgN Way to reddish-brown
<br />37ton1y weadeered to ye'.-Hossisn C rioidnh,tjrleeeenfo
<br />Rocks of dos unit am johmed and read
<br />Mym& resmium an ;Wk as 10 mnoammml; J"i
<br />is entl rolling lbris. M"ed bw ,
<br />day weaMemd cars smnm. lhin Has Me Wan
<br />cListrey Sclam soil cxcvp kehewe fiesh
<br />Thicker iess bwo
<br />road or snearn cuts
<br />jitmn,,'(A mas mvenstey jolmed
<br />well deve5ped cc'u PT, nar pins. Tops of Bows arc
<br />eavern pwt A the baAw red to brown
<br />jnionly vesicuiar ter amygdaloida amy,duies m=
<br />nicacersus sandstone, con Imcnily with
<br />-oroan-j calc�ee ann zerdites.Fornes, ne rrotk r ,, --,
<br />a iag_�s III
<br />imbedded v0d; puqQh1rown sandy
<br />reguhr upland topography
<br />ludes nQuor arrorm"s of By sand
<br />,tlTj
<br />1=2:
<br />(3REENSTONE CCMCR=RATn-`vu9 rt=y j
<br />lostible congIrnmenate In Hte ecief
<br />ills, gray, canaireclus, and inhoiltedded
<br />gpreennif)-gray r,-) reddisin-iereals, oubi antJ
<br />I c
<br />fOSSiNUPOUS ShclwS sTld SffljA(_J'3_1ta, and
<br />nomy"eval having a copc SWAY see SMY it
<br />iandy cemented hy shica. Clams mAnN mviuciunel
<br />r composed of basW Eyeenswirte, and
<br />angular, �,,;rcjjmsorne woh nninor subjroundcd qua
<br />it is jonited bw mostly tesistant �0 eres,
<br />aly adling urelands and ImAy Meep
<br />an(3 quaitz, Commonil, forms swein bedrocs, e)
<br />DUI I011H 1t 1 Lipjand swfaces may be mantled by rn,
<br />and soil are ON and sandy
<br />alely fificx, saloomfic 3,sjocluurn c<1 M?., sca"Herell,
<br />ERME—Red to pqhh bmwn wjd
<br />siones, `Soo is thin sdi ana cl,
<br />,,, pebble, CdAir am! baA&r con�
<br />wait',
<br />i poody sorted, siltt sand mailirt, Her-
<br />b
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<br />TBERMALLY sn[ETAMORPHOSED ROCUS--Ther
<br />l rcvven arkosicsandsione and purp4ish-
<br />rnecamect pho co selfimen'tary rocks surrorli
<br />loeri Clains are mitonly subyounded m
<br />afisibase intnisive bodres, Red-bresesen stlistoric
<br />=art, lte, and sc la; A K the stanem pad of
<br />hoj,10els are bleaciieo, to vanous sfta64
<br />m&d Teenswene, basadt, hmewonti,
<br />nmuve, bul or greenTay, commonly sW%cd
<br />Zne tJasls in, the wesi con�fknrierate is,
<br />, ,s naee ocen baked () g�cai awghrless,
<br />nec�
<br />wemliwred and �Oose in Hie el"d celu-
<br />mjncoaiization �s corcirnor, toorig pcdms or fraciur
<br />re deupo onalemd un We %Tv. Re`
<br />blabs tvl�hm the rocks, o, within ciasui ut met,
<br />td
<br />sapoiHic WW wif 6 ow MW T"elly,
<br />phoseo cotjgjewnera�o Tylacvl rrietatnet"Phic aw
<br />r
<br />mrse No ginavel as Me surface,
<br />m the una inch-ide sdeidoitt, coycliejriia nietaUic n
<br />M1. ERATE. -- Dom6eiaraly pvb1ii1v
<br />AS, pIermew, w gw"L Be"mg a aw&nWit,
<br />rnnenme with a rMdmWbmwn to gmy
<br />amwned, Runiumi N geal,alts thir, itet�j� �er,
<br />m i w Iit
<br />e s 1cv
<br />g ; my urjn colly
<br />tan alacent Wabasc
<br />isne, Clasts we gno'afly sultrwon ed 10
<br />linnesj�one
<br />DIABASE-- ire..rvs dIss, moat aw 01% UoU
<br />n woh rnmor schisi, I)Zh e,
<br />deme, Ima donv%"o W-K nwortyawme ui
<br />extreinaiiesusfaeplible In, aclution, pau
<br />ock having a merhurn -grained s,toure airei an eqw,�
<br />ed fiices am i otong pjr,fj, or fractujes,
<br />jar fabru of mtedockng sulcheoral IeWsPxi
<br />,rown, non-ccocareout 171 ajv! stridy
<br />pyriettene laegular nods and pcgrnalaw act
<br />residuun-t is h i's thirt
<br />gMICAM"M dW WMMOWn ramer diabase botlics
<br />awar suke rLdges of nmssive conyono
<br />;Mn or, rAdow to y6huesh0mven and gmy :n,t
<br />L' very thick in. eeayal�ei orades where
<br />itenseN pAnved md Inolmd m where
<br />XC!Si&Wol cS MUCf1 Soi D-1 ni tnick, cornrl-tonjiy conc
<br />tpfiejokidlly ceeatnCred core 5�icrlrjs, of iahly fresn
<br />iihstone, The bedieick surfaca bensojith
<br />',)Ili[
<br />coiliTnoniy onnis uregijiar uniana etposii`an)rj:
<br />Ulcr, el,111h pilk, teidev and lennack,,es of
<br />LcaHlj unoer ies i,.esemnds and v.Lffleys
<br />YChkA (0 6 frt (,)Y MOrC on Om bedroa
<br />mQ
<br />PRBTRIASSdC ROCKSUrj iivined scnijo, pri
<br />quarizue, greensione, iirrjesjorc_,, or nee,,-asilnitone
<br />--n0niy belated and cleatled
<br />opwhy: cave.., except ham and Anh where expo
<br />stiffs o, sirearit cuss. Soii✓ cconrnoniy Ukk Of ictat
<br />:cie on upIands undeflam we quarizite (,sarldy sc
<br />gricenseiie? 16ayey
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