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Home > Documents > Geologic Map of the Bonners Ferry 30' x 60' Quadrangle ...Kpsp Kpdc Kphc _l Zsc Ybq Ys Ym Ycq Ywcu...

Geologic Map of the Bonners Ferry 30' x 60' Quadrangle ...Kpsp Kpdc Kphc _l Zsc Ybq Ys Ym Ycq Ywcu...

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Ql Qag Qls Tcb Ttp Ktmc Kg _l Zsc Ybq Ys Ym Ycq Ywcu Yt Ysr Yr Ybk Ymsu Ymsl Yhm Ysh Yss Yw Ye Deer Trail Group Belt Supergroup Windermere Group Eocene TERTIARY CRETACEOUS JURASSIC CAMBRIAN LATE PROTEROZOIC MIDDLE PROTEROZOIC CENOZOIC MESOZOIC PALEOZOIC QUATERNARY Glacial and alluvial deposits (Quaternary) Landslide deposits (Quaternary) Glacial-lacustrine deposits (Quaternary) Chlorite breccia and cataclastic rocks associated with the Newport Fault zone (Eocene) Quartz monzonite of Trapper Peak (Eocene) Priest River complex Granodiorite of Trapper Creek (Cretaceous) Mixed granitic and metamorphic rocks of Lookout Mountain (Cretaceous) Garnet-bearing granodiorite (Cretaceous) Granodiorite of Caribou Creek (Cretaceous) Mafic granodiorite of Marsh Lake (Cretaceous) Granodiorite of Search Lake (Cretaceous) Mafic granodiorite of Lucky Creek (Cretaceous) Monzogranite of Klootch Mountain (Cretaceous) Two-mica granitic rocks of Horton Creek (Cretaceous) Mafic granodiorite of Cavanaugh Bay (Cretaceous) Mixed granitic rocks of Camels Prairie (Cretaceous) Mixed granitic and metamorphic rocks of Soldier Creek (Cretaceous) Monzogranite of Shorty Peak (Cretaceous) Mixed two-mica rocks of Ball Creek (Cretaceous) Granodiorite of Falls Creek (Cretaceous) Tonalite of Snow Peak (Cretaceous) Granitic and metamorphic rocks, undivided (Cretaceous) Monzogranite of Hunt Creek (Cretaceous) Monzonite of Long Canyon (Mesozoic) Prichard Formation, metamorphosed (Middle Proterozoic) Monzogranite of Granite Pass (Cretaceous) Two-mica monzogranite or granodiorite of Twenty Mile Creek (Cretaceous) Monzogranite of Tango Creek (Cretaceous) Monzogranite of Hungry Mountain (Cretaceous) Monzogranite of Gleason Mountain (Cretaceous) Granitic rocks, undivided (Cretaceous) Monzonite of Wall Mountain (Mesozoic) Granodiorite of Bonners Ferry (Cretaceous) Granodiorite of Hall Mountain (Cretaceous) Boulder Mountain pluton Granodiorite of Reeder Creek (Cretaceous) Porphyritic, muscovite-bearing, biotite granodiorite Galena Point Granodiorite (Cretaceous) Granodiorite of Ruby Creek (Cretaceous) Granodiorite of Copeland (Cretaceous) Granodiorite of Priest Lake (Cretaceous) Granodiorite of Kelly Pass (Cretaceous) Granodiorite of Road V-78 (Cretaceous) Tonalite of Continental Mountain (Jurassic) Trondhjemite of Continental Mountain (Jurassic) Dolomite (Cambrian) Windermere Group (Late Proterozoic) Shedroof Conglomerate Mafic intrusive rocks (Late or Middle Proterozoic) Deer Trail Group (Middle Proterozoic) Buffalo Hump Formation Stensgar Dolomite McHale Slate Wabash Detroit Formation and Chamokane Creek Formation, undivided Quartzite unit Togo Formation Belt Supergroup (Middle Proterozoic) Mount Shields Formation Upper part Lower part CORRELATION OF MAP UNITS LIST OF MAP UNITS Qls Tcb Yppm Kgp Ktc Kh Kgm Kbf Khbm Krc Krcp Kcu Kco Kru Kv Kkp Kgpl Kptc Kplm Kpgb Kpcc Kpml Kplc Kpkm Kpcb Kpcp Kpms Kpsh Kpbc Kpfc Kpsp Kpdc Kph Kphc Jcmt Jcm }w ZYmi }pl Pleistocene Ttp Classification after Streckeisen (1976) 5 Quartz Quartz Alkali Feldspar Plagioclase Tonalite Granodiorite Quartz Monzonite Monzonite Monzodiorite Quartz Monzodiorite Quartz Syenite Quartz Syenite 20 90 65 35 10 Monzogranite Syenogranite Diorite Monzogranite of Granite Pass Monzogranite of Hungry Mountain Monzogranite of Tango Creek Galena Point Granodiorite Granodiorite of Hall Mountain Granodiorite of Reeder Creek Monzogranite of Gleason Mountain Kg Kgp Kco Kru Kv Kkp Kgpl Ktmc Ktc Kh Kbf Khbm Krcp Krc Kptc Kplm Kpgb Kpcc Kpml Kplc Kpkm Kph Kpcb Kpcp Kpms Kpsh }pl Jcmt Jcm }w Granodiorite of Ruby Creek Granodiorite of Priest Lake Granodiorite of Caribou Creek Granodiorite of Search Lake Mafic granodiorite of Lucky Creek Monzogranite of Shorty Peak Mixed two-mica rocks of Ball Creek Monzogranite of Klootch Mountain Monzogranite of Hunt Creek Tonalite of Continental Mountain Trondhjemite of Continental Mountain Monzonite of Long Canyon Kcu Kgm Kpsl Kpsl Yp Ymi Yp Ypf Granitic and metamorphic rocks of the Priest River complex* * The Priest River complex in the Bonners Ferry quadrangle is an Eocene structure made up of at least 19 lithodemes that range in age from Cretaceous to Triassic(?) and includes one highly metamorphosed Proterozoic unit. All of the units yield Eocene conventional potassium-argon biotite ages. The units shown in the connected boxes are probably not distinct sequentially emplaced plutons but rather represent one or more, inhomogeneous, composite intrusive masses that are variably intermixed with metamorphic rocks. All of the granitic units are probably Mesozoic in age, and the intermixed metamorphic rocks are derived from the Belt Supergroup or from sills that intrude it. The arrangement of the boxes, either by column or row, has little petrogenetic significance, but corresponds to the sequence in List of Map Units, proceeding by row from left to right. The disconnected boxes are positioned in the Correlation of Map Units to reflect the known or presumed age of their respective protoliths, and are described in the order of their position. Qag Ql Figure 3. Modal compositions for selected granitic units in Bonners Ferry quadrangle. ? ? ? ? Kpbc Kpfc Kpsp Kpdc Kphc _l Zsc Ybq Ys Ym Ycq Ywcu Yt ZYmi Ymsu Ymsl Ysr Yr Ybk Yss Yw Ye Ymi Yp Ypf Contact—Generally located within ±25 m, except within Priest River complex where many contacts are highly gradational and subject to interpretive placement Faults High-angle—Includes normal, reverse, and multiply reactivated faults. Solid where located within ±25 m; dashed where located within ±50 m; dotted where concealed; queried where location uncertain. Bar and ball on downthrown side. Low-angle normal (detachment)—Solid where located within ±25 m; dashed where located within ±50 m; dotted where concealed Folds Anticline—Arrow indicates direction of plunge Syncline—Arrow indicates direction of plunge Strike and dip of bedding* Inclined Vertical Overturned Strike and dip of primary igneous features* Foliation Inclined Vertical Strike and dip of secondary foliation, igneous rocks Strike and dip of foliation, metamorphic* Inclined Vertical Bearing and plunge of lineations* Stretching Primary igneous Minor fold axes *Symbols may be used in combination ? 48 30' Figure 2. Index map of Bonners Ferry 30' x 60' quadrangle showing geographic and cultural features referred to in the text. Also shown are the approximate areas predominently underlain by (1) Deer Trail Group and Windermere Group, tan; (2) eastern Priest River complex, gray; and (3) Belt Supergroup, green. Town. Mountain peak. Specific feature. COPELAND EASTPORT BONNERS MORAVIA NAPLES LEONIA Wall Mtn Kelly Pass Lookout Mtn Snow Peak Camels Prairie NORDMAN Crossport Shorty Pk IDAHO MONTANA Ta ngo Cr e e k R e e d e r C re e k R u b y C r e e k T r a p p e r C r e e k C ari b o u C r e e k Priest Lake H o r t o n C reek H u nt Creek So l d i er Cr e e k L u cky C r ee k T w e n t y m i l e C r e e k F a ll C r e e k K o ot e n a i R i v e r DEEP CREEK M o y i e R i v e r C A B I N E T MO U N T A INS B a ll Creek L o n g C a n y o n C r e e k V-78 Road U p p e r P r i e s t R iv e r CAVANAUGH BAY Upper Priest Lake Continental Mtn Marsh Lake Trapper Pk Search Lake Boulder Mtn Klootch Mtn MOYIE SPRINGS FERRY Approximate Purcell Trench boundary of 117 00' 48 30' 116 00' 116 00' KILOMETERS 0 10 20 25 49 00' 49 00' 117 00' Slate Ridge McGinty Ridge Dodge Pk 49 48 118 ? ? ? S T. M A R Y F A U L T ? ? ? ? ? ? ? K O O T E N A Y A R C P U R C E L L T R E N C H F A U L T P U R C E L L T R E N C H N E W P O R T F A U L T J U M P O F F J O E F A U L T JOJ HOPE FAULT MOYIE NEWPORT(?) ID AH O FAULT UNITED STATES CANADA BRITISH COLUMBIA WASHINGTON ? P R I E S T R I V E R C OM P L E X P R I E S T R I V E R C O M P L E X 116 H U C K L E B E R R Y R AN G E F A U L T HRF Q u e s n e llia 0 20 40 Kilometers Granitic rocks (Cretaceous and Jurassic) Priest River complex (Cretaceous to Middle Proterozic) Rocks of Quesnellia Terrane (Jurassic to Carboniferous) Rocks west of Huckleberry Range Fault Deer Trail Group, Windermere Group, and Paleozoic rocks (Ordovician to Middle Proterozoic) Belt Supergroup and Paleozoic rocks (Mississip- pian to Middle Proterozoic) Mylonitized rocks C N 48 30' 117 Granitic rocks (Tertiary) Figure 1. Simplified geologic map showing relations of major structures in Bonners Ferry quadrangle to other major structures in the region. Bonners Ferry quadrangle outlined in green. HRF, Huckleberry Range Fault; JOJ, Jumpoff Joe Fault; N, Newport; C, Chewelah. Town. JOJ(?) AND FAULTS ID A H O M ON TA N A û û û û û û C l a r k F o r k - E a s t p o r t S e q ue n c e of B e lt S u p e rgro u p N e w p o r t S e q u e n c e o f B e l t S u p e r g r o up NEWPORT(?) FAULT JOJ FAULT Argillite of Half Moon Lake Shepard Formation Snowslip Formation Wallace Formation Empire Formation St Regis Formation Revett Formation Burke Formation Mafic sills Prichard Formation U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY MISCELLANEOUS FIELD STUDIES MAP MF-2426 Pamphlet accompanies map Geologic Map of the Bonners Ferry 30' x 60' Quadrangle, Idaho and Montana By Fred K. Miller and Russell F. Burmester Digital preparation by Pamela M. Cossette and Pamela D. Derkey 2003 0 1 1 2 3 4 5 6 7 8 9 10 11 KILOMETERS 0 1 1 2 3 4 5 6 7 MILES CONTOUR INTERVAL 50 METERS SCALE 1:100,000 N MN 17° Declination at center of map, 2003 Base from U.S. Geological Survey Bonners Ferry 1:100,000 scale map, 1983; U.S. Geological Survey Bonners Ferry East and West digital line graphs (DLG), 1983 Universal Transverse Mercator projection, zone 11 Geology mapped by Fred K. Miller, 1977-1993; Russell F. Burmester, 1980-1988 Edited by Jane S. Ciener and Jan L. Zigler Manuscript approved for publication November 12, 2003 IDAHO LOCATION MAP Any use of trade, firm, or product names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government. This map was printed on an electronic plotter directly from digital files. Dimensional calibration may vary between electronic plotters and between X and Y directions on the same plotter, and paper may change size due to atmospheric conditions; therefore, scale and proportions may not be true on plots of this map. For sale by U.S. Geological Survey, Information Services, Box 25286, Federal Center, Denver, CO 80225, 1-888-ASK-USGS Digital files available on World Wide Web at http://geopubs.wr.usgs.gov/map-mf/mf2426 Granitic and metamorphic rocks of the Priest River complex End of granitic and metamorphic rocks of the Priest River complex Yppm Yhm Ysh
Transcript
  • QlQagQls

    Tcb

    Ttp

    KtmcKg

    _l

    Zsc

    Ybq

    Ys

    Ym

    Ycq

    Ywcu

    Yt

    Ysr

    Yr

    Ybk

    Ymsu

    Ymsl

    Yhm

    Ysh

    Yss

    Yw

    Ye

    DeerTrail

    Group

    BeltSupergroup

    WindermereGroup

    Eocene TERTIARY

    CRETACEOUS

    JURASSIC

    CAMBRIAN

    LATEPROTEROZOIC

    MIDDLEPROTEROZOIC

    CENOZOIC

    MESOZOIC

    PALEOZOIC

    QUATERNARY

    Glacial and alluvial deposits (Quaternary)

    Landslide deposits (Quaternary)

    Glacial-lacustrine deposits (Quaternary)

    Chlorite breccia and cataclastic rocks associated with the Newport Fault zone (Eocene)

    Quartz monzonite of Trapper Peak (Eocene)

    Priest River complex

    Granodiorite of Trapper Creek (Cretaceous)

    Mixed granitic and metamorphic rocks of Lookout Mountain (Cretaceous)

    Garnet-bearing granodiorite (Cretaceous)

    Granodiorite of Caribou Creek (Cretaceous)

    Mafic granodiorite of Marsh Lake (Cretaceous)

    Granodiorite of Search Lake (Cretaceous)

    Mafic granodiorite of Lucky Creek (Cretaceous)

    Monzogranite of Klootch Mountain (Cretaceous)

    Two-mica granitic rocks of Horton Creek (Cretaceous)

    Mafic granodiorite of Cavanaugh Bay (Cretaceous)

    Mixed granitic rocks of Camels Prairie (Cretaceous)

    Mixed granitic and metamorphic rocks of Soldier Creek (Cretaceous)

    Monzogranite of Shorty Peak (Cretaceous)

    Mixed two-mica rocks of Ball Creek (Cretaceous)

    Granodiorite of Falls Creek (Cretaceous)

    Tonalite of Snow Peak (Cretaceous)

    Granitic and metamorphic rocks, undivided (Cretaceous)

    Monzogranite of Hunt Creek (Cretaceous)

    Monzonite of Long Canyon (Mesozoic)

    Prichard Formation, metamorphosed (Middle Proterozoic)

    Monzogranite of Granite Pass (Cretaceous)

    Two-mica monzogranite or granodiorite of Twenty Mile Creek (Cretaceous)

    Monzogranite of Tango Creek (Cretaceous)

    Monzogranite of Hungry Mountain (Cretaceous)

    Monzogranite of Gleason Mountain (Cretaceous)

    Granitic rocks, undivided (Cretaceous)

    Monzonite of Wall Mountain (Mesozoic)

    Granodiorite of Bonners Ferry (Cretaceous)

    Granodiorite of Hall Mountain (Cretaceous)

    Boulder Mountain pluton

    Granodiorite of Reeder Creek (Cretaceous)

    Porphyritic, muscovite-bearing, biotite granodiorite

    Galena Point Granodiorite (Cretaceous)

    Granodiorite of Ruby Creek (Cretaceous)

    Granodiorite of Copeland (Cretaceous)

    Granodiorite of Priest Lake (Cretaceous)

    Granodiorite of Kelly Pass (Cretaceous)

    Granodiorite of Road V-78 (Cretaceous)

    Tonalite of Continental Mountain (Jurassic)

    Trondhjemite of Continental Mountain (Jurassic)

    Dolomite (Cambrian)

    Windermere Group (Late Proterozoic)

    Shedroof Conglomerate

    Mafic intrusive rocks (Late or Middle Proterozoic)

    Deer Trail Group (Middle Proterozoic)

    Buffalo Hump Formation

    Stensgar Dolomite

    McHale Slate

    Wabash Detroit Formation and Chamokane Creek Formation, undivided

    Quartzite unit

    Togo Formation

    Belt Supergroup (Middle Proterozoic)

    Mount Shields Formation

    Upper part

    Lower part

    CORRELATION OF MAP UNITSLIST OF MAP UNITS

    Qls

    Tcb

    Yppm

    Kgp

    Ktc Kh Kgm

    Kbf Khbm Krc KrcpKcu

    KcoKru

    Kv

    KkpKgpl

    Kptc Kplm Kpgb Kpcc Kpml

    Kpsl Kplc Kpkm

    Kpcb Kpcp Kpms Kpsh

    Kpbc Kpfc Kpsp Kpdc

    Kph

    Kphc

    JcmtJcm

    }w

    ZYmi

    }pl

    Pleistocene

    Ttp Classification after Streckeisen (1976)

    5

    Quartz Quartz

    Alkali Feldspar Plagioclase

    Tonalite

    Granodiorite

    QuartzMonzonite

    Monzonite Monzodiorite

    QuartzMonzodiorite

    Quartz

    Syenite

    QuartzSyenite

    20

    90 65 35 10

    Mon

    zogr

    anit

    e

    Syen

    ogra

    nite

    Diorite

    Monzogranite of Granite Pass

    Monzogranite of Hungry MountainMonzogranite of Tango Creek

    Galena Point Granodiorite

    Granodiorite of Hall Mountain

    Granodiorite of Reeder Creek

    Monzogranite of Gleason Mountain

    Kg

    Kgp

    Kco

    Kru

    Kv

    Kkp

    Kgpl

    Ktmc

    Ktc

    Kh

    Kbf

    Khbm

    Krcp

    Krc

    Kptc

    Kplm

    Kpgb

    Kpcc

    Kpml

    Kplc

    Kpkm

    Kph

    Kpcb

    Kpcp

    Kpms

    Kpsh

    }pl

    Jcmt

    Jcm

    }w

    Granodiorite of Ruby Creek Granodiorite of Priest Lake

    Granodiorite of Caribou Creek Granodiorite of Search Lake

    Mafic granodiorite of Lucky Creek

    Monzogranite of Shorty Peak Mixed two-mica rocks of Ball Creek

    Monzogranite of Klootch Mountain

    Monzogranite of Hunt Creek Tonalite of Continental Mountain

    Trondhjemite of Continental Mountain Monzonite of Long Canyon

    Kcu

    Kgm

    Kpsl

    Kpsl

    Yp

    Ymi

    Yp

    Ypf

    Granitic and metamorphic rocks of the Priest River complex*

    * The Priest River complex in the Bonners Ferry quadrangle is an Eocene structure made up of at least 19 lithodemes that range in age from Cretaceous to Triassic(?) and includes one highly metamorphosed Proterozoic unit. All of the units yield Eocene conventional potassium-argon biotite ages. The units shown in the connected boxes are probably not distinct sequentially emplaced plutons but rather represent one or more, inhomogeneous, composite intrusive masses that are variably intermixed with metamorphic rocks. All of the granitic units are probably Mesozoic in age, and the intermixed metamorphic rocks are derived from the Belt Supergroup or from sills that intrude it. The arrangement of the boxes, either by column or row, has little petrogenetic significance, but corresponds to the sequence in List of Map Units, proceeding by row from left to right. The disconnected boxes are positioned in the Correlation of Map Units to reflect the known or presumed age of their respective protoliths, and are described in the order of their position.

    Qag

    Ql

    Figure 3. Modal compositions for selected granitic units in Bonners Ferry quadrangle.

    ?

    ??

    ?

    Kpbc

    Kpfc

    Kpsp

    Kpdc

    Kphc

    _l

    Zsc

    Ybq

    Ys

    Ym

    Ycq

    Ywcu

    Yt

    ZYmi

    Ymsu

    Ymsl

    Ysr

    Yr

    Ybk

    Yss

    Yw

    Ye

    Ymi

    YpYpf

    Contact—Generally located within ±25 m, except within Priest River complex where many contacts are highly gradational and subject to interpretive placement

    Faults

    High-angle—Includes normal, reverse, and multiply reactivated faults. Solid where located within ±25 m; dashed where located within ±50 m; dotted where concealed; queried where location uncertain. Bar and ball on downthrown side.

    Low-angle normal (detachment)—Solid where located within ±25 m; dashed where located within ±50 m; dotted where concealed

    Folds

    Anticline—Arrow indicates direction of plunge

    Syncline—Arrow indicates direction of plunge

    Strike and dip of bedding*

    Inclined

    Vertical

    Overturned

    Strike and dip of primary igneous features*

    Foliation

    Inclined

    Vertical

    Strike and dip of secondary foliation, igneous rocks

    Strike and dip of foliation, metamorphic*

    Inclined

    Vertical

    Bearing and plunge of lineations*

    Stretching

    Primary igneous

    Minor fold axes

    *Symbols may be used in combination

    ?

    48 30'

    Figure 2. Index map of Bonners Ferry 30' x 60' quadrangle showing geographic and cultural features referred to in the text. Also shown are the approximate areas predominently underlain by (1) Deer Trail Group and Windermere Group, tan; (2) eastern Priest River complex, gray; and (3) Belt Supergroup, green. Town. Mountain peak. Specific feature.

    COPELAND

    EASTPORT

    BONNERS

    MORAVIA

    NAPLES

    LEONIA

    Wall Mtn

    Kelly Pass

    Lookout Mtn

    Snow Peak

    Camels Prairie

    NORDMAN

    Crossport

    Shorty Pk

    IDA

    HO

    MO

    NT

    AN

    A

    Tango Creek

    R

    ee de r Creek

    Ruby

    Cre

    ek

    Trap

    per

    Cre

    ekC

    arib

    ou

    C r

    eek

    Priest Lake

    Horton Creek

    Hunt Cree

    k

    Soldie

    r Creek

    Luck

    yC

    reek

    Twe ntymile Creek

    F all Cree k

    K ootenai

    River

    DEEP CREEK

    Mo

    yieR

    iver

    CA

    BIN

    ETM

    OU

    NTAINS

    Ball

    Creek

    Lon

    g

    C any

    on

    Cree

    k

    V-78 Road

    U

    pperP

    riestR

    iver

    CAVANAUGHBAY

    UpperPriest Lake

    Continental Mtn

    MarshLake

    Trapper Pk

    Search Lake

    BoulderMtn

    KlootchMtn

    MOYIESPRINGS

    FERRY

    Approximate

    Purcell Trenchboundary of

    117 00'48 30'

    116 00'

    116 00'

    KILOMETERS

    0 10 20 25

    49 00' 49 00'117 00'

    Slate Ridge

    McGinty Ridge

    Dodge Pk

    49

    48 118

    ??

    ?

    ST.

    MA

    R YF A

    U LT

    ??

    ?

    ??

    ??

    KO

    O

    T

    E

    N

    A

    Y

    A

    R

    C

    PU

    RC

    EL

    L

    TR

    EN

    CH

    FA

    UL

    T

    P

    U

    R

    C

    EL

    LT

    RE

    NC

    H

    N

    E W P O R T F

    AU

    LT

    JUM

    PO

    FF

    JOE

    FAU

    LT

    JOJ

    HOPE FAULT

    MO

    YIE

    NEWPORT(?)

    IDA

    HO

    FAULT

    UNITED STATESCANADABRITISH COLUMBIA

    WASHINGTON

    ?

    PR

    IES

    TR

    IVE

    RC

    OM

    PLE

    X

    PR

    IES

    TR

    IVE

    RC

    OM

    PLE

    X

    116

    HU

    CK

    LEB

    ER

    RY

    RANG

    EFA

    ULT

    HRF

    Que

    snell

    ia

    0 20 40Kilometers

    Granitic rocks (Cretaceous and Jurassic)

    Priest River complex (Cretaceous to Middle Proterozic)

    Rocks of Quesnellia Terrane (Jurassic to Carboniferous)

    Rocks west of Huckleberry Range Fault

    Deer Trail Group, Windermere Group, and Paleozoic rocks (Ordovician to Middle Proterozoic)

    Belt Supergroup and Paleozoic rocks (Mississip-pian to Middle Proterozoic)

    Mylonitized rocks

    C

    N

    48 30'

    117

    Granitic rocks (Tertiary)

    Figure 1. Simplified geologic map showing relations of major structures in Bonners Ferry quadrangle to other major structures in the region. Bonners Ferry quadrangle outlined in green. HRF, Huckleberry Range Fault; JOJ, Jumpoff Joe Fault; N, Newport; C, Chewelah. Town.

    JOJ(?) AND

    FAULTS

    IDA

    HO

    MO

    NT

    AN

    A

    ûûû

    û

    û

    û

    Cl

    ark

    Fork

    -E

    astp

    ort

    Seq

    uenc

    eof

    Bel

    tS

    uper

    grou

    p

    New

    port Sequence

    ofB

    eltS

    upergroup

    NEWPORT(?) FAULT

    JOJ FAULT

    Argillite of Half Moon Lake

    Shepard Formation

    Snowslip Formation

    Wallace Formation

    Empire Formation

    St Regis Formation

    Revett Formation

    Burke Formation

    Mafic sills

    Prichard Formation

    U.S. DEPARTMENT OF THE INTERIORU.S. GEOLOGICAL SURVEY MISCELLANEOUS FIELD STUDIES MAP MF-2426

    Pamphlet accompanies map

    Geologic Map of the Bonners Ferry 30' x 60' Quadrangle, Idaho and MontanaBy

    Fred K. Miller and Russell F. Burmester

    Digital preparation by Pamela M. Cossette and Pamela D. Derkey2003

    0 11 2 3 4 5 6 7 8 9 10 11 KILOMETERS

    0 11 2 3 4 5 6 7 MILES

    CONTOUR INTERVAL 50 METERS

    SCALE 1:100,000N MN

    17°

    Declination at

    center of map, 2003

    Base from U.S. Geological Survey Bonners Ferry 1:100,000 scale map, 1983; U.S. Geological Survey Bonners Ferry East and West digital line graphs (DLG), 1983

    Universal Transverse Mercator projection, zone 11

    Geology mapped by Fred K. Miller, 1977-1993; Russell F. Burmester, 1980-1988

    Edited by Jane S. Ciener and Jan L. Zigler

    Manuscript approved for publication November 12, 2003

    IDAHO

    LOCATION MAP

    Any use of trade, firm, or product names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government.

    This map was printed on an electronic plotter directly from digital files. Dimensional calibration may vary between electronic plotters and between X and Y directions on the same plotter, and paper may change size due to atmospheric conditions; therefore, scale and proportions may not be true on plots of this map.

    For sale by U.S. Geological Survey, Information Services, Box 25286, Federal Center, Denver, CO 80225, 1-888-ASK-USGS

    Digital files available on World Wide Web at http://geopubs.wr.usgs.gov/map-mf/mf2426

    Granitic and metamorphic rocks of the Priest River complex

    End of granitic and metamorphic rocks of the Priest River complex

    Yppm

    Yhm

    Ysh


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