Vv

CHAPTER II]—Concluded
Stratigraphy—Concluded

Upper Cretaceous—Concluded 5 Pacn

iKotaneeleeiformationsy ape prey ce hacer taser ee eae neers. 103
Liard River Valley, p. 103; age and correlation, p. 105.

Wapiti group setae enn teen tba ASM pas teh Ege WA aha naity cle 3H: 106

BedshwiteH quesevumianciycum sea aey eee eee een essen ne 109

FD enti ary eercssts myeper toe top ere icici aie etSie AS cLe OTS lke eo Sache ere ie 110
Rhy Oltet scree ciety tal hey ener sce eonlaes Sea renaie alot pets i chal, AVE STEN es wisi eseie § 110
CoaltRiven Tertiary jest orn eee nee Ocoee nts ddeatins 110

CHAPTER IV

Structuraligeolowy sess clacts cree ye eaters ties ele erase ete Pea vtec 111
Generaliistatemen tsi) rspsvscioresisterctotele erste ase ae cherie ouiooeetrhien earn bisee 111
JOTI Ey tune nad soda no Ab USOUUUCHORG IO Gon CHOCO CROSH ESE mere an 111
Pine and Peace River Valleys............00..ccccccesccevccccecccece 111
Harrell @reekesyoictayeisssieyara.syots) cist ais(ejsiciab nasi leteia)s isis «:dislsia overs ero th esse eheats 112
Halfway River to Steamboat Mountain..............00.cceeecesecees 113
ike NUE ees eqrapsboomedo non 6b AB OUCoo UC DHEA GUSH E AAAS SEC UM tno eee aa 113
Pineyandebeacershiverstootnillssnerereeee heer n ieee neni aanioe 113

Portage-Butler structural zone, p. 113; Dunlevy syncline, p. 114;
Gething-Stott structural zone, p. 114; Beattie Hill structure, p.
115; Branham Ridge syncline, p. 115; Horseshoe Hill structure,
p. 116; Schooler Creek syncline, p. 116; Folded Hill structure, p.
116; Brown Hill structure, p. 116; Pardonet anticline, p. 117;
Carbon Creek basin, p. 117; Fisher Creek structural zone, p. 117;
Pine River anticline, p. 118; Pine River syncline, p. 118; Commo-
tion-Hulcross structural zone, p. 118; comments, p. 119.
Halfway River to Prophet River. ...........-. cece eeecescereceecs So Alri)
Pink Mountain structure, p. 120; Halfway River Valley, p. 120; struc-
tures in Sikanni Chief Valley, p. 120; Buckinghorse River Valley
structures, p. 121; Pocketknife anticline, p. 121.
TetsaRiversHoothillamew recite ol rie tilttclantre rs Lecpeisretteleereieicrciece 121
Eastern Triassic belt, p. 121; Paleozoic fault block, p. 122; Western
Triassic belt, p. 122.
Foothills!andwaiard Plateau ceejcttiesvelcte co crorcier teil olel ef deteve:cleiciers’cie sicielstern store 122
Tei ard SRVELs DASLM Heresy aarsieer otek evel erotetatatelelotoin sich rowstarer stat arets ga000Dg908 poo WP
Liard syncline, p. 122; Toad anticline, p. 123; Scatter River monocline,
p. 123; Beaver River anticline, p. 123; structures recorded on air
photographs, p. 123; La Biche anticline, p. 124; Liard Range
structure, p. 124; Petitot River syncline, p. 124.

RockyzMountainsteecer-erieeeereieer einer ilpterrrir terre siti 124
iPinesRiverstorMuskwashiver nce) -titekrcrtrcy rte rleiesicier 124
Summit Lake to Muncho Lake....................2 220s eeeecrccceees 125
Muncho Lake to Liard River bridge. ............... eee eee cence eee 126
OB H Oe ferirosn JEEVES 6G Aa dceooocbeouK nb obouDecosouOouneODoodooOoOnIE 126

IbrEhyel dH bins An a Uwe Aine cr moo Ete GOO oR a GA OF CORES Cc adoninc Soy mene 126

RockyaMountaimebrenchuraea vrei toe atte a aererdet sole ietsietciore silicic a = 126

Eastern part of Omineca and Cassiar Mountains...............0-eeseee eee 126