Qa

Qoa

?

?

?

?

QTa

Qc Qac Ql

!@s !@sc

?

?

?

?

!@f

Kev

Keva

Keva

Kevm

Kevl

Kevu

Ks

!@ts

@s2

@s3

@s1

~!s

?

!@s2

!@s1

af dt

Qt

@b

QTb

QTp QTp1 QTp2

@r

Kal

Kg Kqm

Kwqm

Kmo

Kgd

Kqd Ksd

Kad Kb Kd Km

Tl

?

Ki Kl

Kbqm

Kbqmf

Kbqmm

#ql

Qp Qpw

? ?

Qbg

QTg

?

?

Qog Qgt

Qgto Qgtc

Qgty Qag

Zd

Kk

Jm

*a

P*pq

Pp

*q

Mb

*Mab

Mmu

Mm

Ml

MDt

Du

Dj

D_m

_pi

_pp

_wf

_p

_m

_w

_f

Ye

Ys

Ygm

Ygu

Ygl

Yg

Yn

Ynu

Ynl

Yl

Je

Jme

Kcm

Kcu

Ktc

Ke

Kma

Kmb

Kmc

Kmd

Kme

Kmg

Kmf

Kmh

Kc

Kcl

Disconformities

Unconformity

Unconformity

Unconformity

Unconformity

Unconformity

Unconformity

Unconformity

Unconformity

Unconformity

Western part

of quadrangle

Southeastern part

of quadrangle

Units of Sedimentary and Volcanic Origin Units of Igneous Intrusive Origin

Unconformity

Unconformity

Intrusive contacts

Intrusive contacts

CORRELATION OF MAP UNITS

Qa

Qac

Qbg

Qc

dt

af

Ql

Qoa

Ygu

Ygm

Ygl

Ye

Ys

Yg

Yn

Ynu

Ynl

Yl

Ktc

Kc

Kcu

Kcm

Kcl

Kwqm

Kg

Kbqm

Kbqmf

Kqm

Kd

Kmo

Kad

Kb

Ksd

Kk

Kal

Jme

Jm

Je

Km

P*pq

Pp

*a

*Mab

Mb

Mmu

Mm

Ml

MDt

Du

Dj

D_m

_pp

_pi

_p

_m

_w

_wf

_f 

Zd

*q

Ki

Kqd

Kgd

Qog

Qp

Qpw

Qt

Qgt

Qgtc

Qgty

Qgto

QTg

QTp

QTp1

QTp2

QTb

~!s

!@s2

!@s1

!@s

@b

#ql

@r

!@ts

@s3

@s2

@s1

Tl

Kmh

Kmf

Kme

Kmd

Kmc

Kmb

Kma

Kmg

Kev

Kevu

Kevm

Kevl

Keva

QTa

Qag

Kbqmm

Kl

!@f

!@sc

Ks

Ke

Alluvium (Holocene)

Alluvium and colluvium, undivided (Holocene)

Boulder gravel (Holocene or Pleistocene)

Colluvium (Holocene)

Dredge tailings (Holocene)

Artificial fill (Holocene)

Landslide deposit (Holocene and Pleistocene)

Old alluvium (Holocene or Pleistocene)

Greyson Formation, upper member

Greyson Formation, middle member

Greyson Formation, lower member

Empire Formation

Belt Supergroup (Mesoproterozoic)

Spokane Formation

Greyson Formation, undivided

Newland Formation, undivided

Newland Formation, limestone-bearing upper part

Newland Formation, lower part

Lahood Formation

Telegraph Creek Formation (Upper Cretaceous)

Colorado Group sedimentary rocks, undivided (Upper and Lower Cretaceous)

Upper part (Upper and Lower Cretaceous)

Middle part (Lower Cretaceous)

Lower part (Lower Cretaceous)

Quartz monzonite of the Wilson Park pluton (Late Cretaceous)

Granite (Late Cretaceous)

Butte quartz monzonite (Late Cretaceous)

Alaskite and related felsic rocks within the Butte quartz monzonite

Butte quartz monzonite, medium grained

Quartz monzonite (Late Cretaceous)

Diorite porphyry (Late Cretaceous)

Monzonite (Late Cretaceous)

Andesite and diorite intrusive rocks (Late Cretaceous)

Basalt (Late Cretaceous)

Syenodiorite (Late Cretaceous)

Kootenai Formation (Lower Cretaceous)

Alaskite and related felsic rocks (Late Cretaceous)

Morrison Formation and Ellis Group, undivided (Jurassic)

Morrison Formation (Jurassic)

Ellis Group, undivided (Jurassic)

Mafic igneous rocks, undivided (Late Cretaceous)

Phosphoria Group (Permian) and Quadrant Formation (Pennsylvanian), undivided

Phosphoria Group (Permian)

Amsden Formation (Pennsylvanian)

Amsden Formation (Pennsylvanian) and Big Snowy Group (Upper Mississippian), undivided

Big Snowy Group, undivided (Upper Mississippian)

Mission Canyon and Lodgepole Limestones, undivided (Upper and Lower Mississippian)

Mission Canyon Limestone (Upper and Lower Mississippian)

Lodgepole Limestone (Lower Mississippian)

Three Forks Formation (Lower Mississippian and Upper Devonian)

Upper and Middle Devonian rocks, undivided

Jefferson Formation (Upper Devonian)

Maywood Formation (Upper and Middle Devonian), locally includes some Cambrian rocks

Pilgrim Formation (Upper Cambrian) and Park Shale (Upper and Middle Cambrian), undivided

Pilgrim Formation (Upper Cambrian)

Park Shale (Upper and Middle Cambrian)

Meagher Limestone (Middle Cambrian)

Wolsey Formation (Middle Cambrian)

Wolsey Formation and Flathead Sandstone, undivided (Middle Cambrian)

Flathead Sandstone (Middle Cambrian)

Diorite (Neoproterozoic)

Quadrant Formation (Pennsylvanian)

Andesitic intrusive rocks related to Elkhorn Mountains Volcanics (Late Cretaceous)

Quartz diorite (Late Cretaceous)

Granodiorite (Late Cretaceous)

Old gravel (Holocene or Pleistocene)

Pediment gravel (Holocene? and Pleistocene)

Pediment gravel with windblown silt and sand (Holocene? and Pleistocene)

Terrace gravel (Holocene and Pleistocene)

Glacial till, undifferentiated (Pleistocene)

Older glacial till and associated colluvium (Pleistocene)

Glacial till, younger till where more than one age of till is recognized (Pleistocene)

Glacial till, older till where more than one age of till is recognized (Pleistocene)

Older gravel (Pleistocene or Pliocene)

Older pediment gravel, undivided (Pleistocene and Pliocene)

Older pediment gravel, lower level where two levels of gravel are adjacent 

 across the underlying bedrock surface (Pleistocene and Pliocene) 

Older pediment gravel, higher level where two levels of gravel are adjacent

 across the underlying bedrock surface (Pleistocene and Pliocene) 

Basalt (Pleistocene? or Pliocene?)

Sedimentary rocks, undivided (Pliocene and Miocene)

Sandstone and conglomerate tongue

Orange-red conglomerate and sandstone tongue

Sedimentary rocks, undivided (Miocene and Oligocene)

Basalt (Oligocene)

Quartz latite (Eocene)

Rhyolite shallow intrusive bodies and flows (Oligocene)

Sedimentary rocks, undivided, covered with discontinuous

 veneer of gravel, loess, sand (Miocene and Oligocene)

Vitric tuff and tuffaceous sedimentary rocks (Miocene and Oligocene)

Dunbar Creek Formation (Oligocene)

Upper part (Oligocene)

Climbing Arrow Formation (Oligocene and Eocene?)

Lower part (Oligocene and Eocene?)

Lamprophyre (Tertiary?) 

Maudlow Formation (Upper Cretaceous)

Maudlow Formation, unit h

Maudlow Formation, unit f

Maudlow Formation, unit e

Maudlow Formation, unit d

Maudlow Formation, unit c

Maudlow Formation, unit b

Maudlow Formation, unit a

Maudlow Formation, unit g

Elkhorn Mountains Volcanics, undivided (Upper Cretaceous)

Upper member

Middle member

Lower member

Ashflow tuff (present in Kevm and locally in Kevl)

Older alluvium (Pleistocene or Pliocene)

Alluvium and glacial till, undivided (Holocene? and Pleistocene)

Fort Logan Formation (Miocene and Oligocene)

Lamprophyre (Late Cretaceous)

LIST OF MAP UNITS

Eagle Sandstone (Upper Cretaceous)

Slim Sam Formation (Upper Cretaceous)

Ynl

Qa

Kbqm

Ygl

!@sc

Ys

Ki

Ygm

Kevl

Mm

Yn

Qa

Yn

Yg

Ys

Kevl

Water

QTp

QTa

Qa

Qpw

Mm

Ygl

Kbqm

!@sc

Ygm

Yg

Qoa

Ml

QTp

Dj

Kqm

Ys

Yn

Kevl

Qoa

Kgd

Ys

Qa

Ygu

Ygu

Qp

Yg

Dj

Yg

Qa

Ki

Water

Kk

Qp

Yg

Yg

Qoa

Ygu

!@s

Ynu

Qgt

Ki

Ygl

Qoa

Qgt

!@s

Ys

Yg

Ynl

Yg

Mm

!@sc

!@sc

Kcu

Mm

Dj

Qp

Qp

Ynu

Ynu

Ml

Zd

Qa

Qoa

QTp

Ys

Ml

Kevl

Ki

!@s

Kk

Dj

_pi

QTp

Qoa

Qp

Ki

QTp

Qp

!@s

Mm

Yl

Dj

Qp

!@s

Keva

Ygm

QTp

QTa

Ynu

Ygl

Qp

Kevm

Kevm

Ys

Mm

Yn

Kk

Qp

Qgt

Yn

Qoa

Mm

Kmg

Kevm

Yg

Qac

Qp

Kd

Kcl

*Mab

Ml

!@s

Kbqm

Qc

Kk

Qp

Ys

Qp

Ys

~!s

Qoa

Mm

Kevl

Kev

QTp1

Ki

Kk

Jme

P*pq

!@sc

Ks

Zd

Ys

Kcl

Jme

Ynu

QTa

Yg

Qpw

QTa

Kcu

Qc

_pi

Kcm

Yg

!@s

*q

Kcm

QTp1

Kd

Qp

!@s

Ml

Kmc

Kcm

Yg

Mm

Ys

_pp

Ml

Qt

Qpw

Kgd

*q

Kevl

Kmf

Kqm

Ys

Kevl

Dj

Qp

Ml

Ygm

Kmf

Qpw

~!s

Qoa

Kcl

Mm

Qp

!@f

Kev

Ql

QTp

Qoa

Kk

QTp

Qoa

Kcm

QTp

!@sc

Ygl

P*pq

Qbg

Kev

Dj

Kk

Ml

!@sc

Qgt

Ygl

Qp

Ys

Qgt

Dj

*q

Ql

Qp

Qp

!@s

Ks

Ml

!@s

Kevl

Qp

Qoa

Yg

Ks

Kcl

Ks

Dj

Mm

Ks

Qgt

Kk

Kevl

Kal

Jme

Kbqm

Du

Ys

Kk

Qc

Qp

Dj

QTp2

Ml

_m

Kcu

Qgty

Qa

!@f

Kmf

Ksd

Kqm

QTp1

Qp

Ks

Kk

QTg

_pp

Qa

_m

Mm

Qp

Ygu

Qa

Qp

QTg

Kk

Ki

Kevm

Ks

Ys

Kevl

Kme

Ki

Qa

Qpw

!@s

Qa

!@sc

Ml

Qag

QTp1

Yg

MDt

Ktc

Kd

Kcl

Ynu

Qa

Kwqm

Kcm

QTg

!@s

Qp

!@s

Kcl

*q

Yn

Ys

Dj

Qp

_m

Ks

Qp

!@s

Kevm

_m

Qpw

Qpw

@s3

Kcl

Qa

QTa

Ys

_m

Kk

Kmg

!@s

Qa

Kcu

Ks

Dj

Kevl

_m

Ml

MDt

Kcm

Kk

_w

Kbqm

Ks

Qp

Ys

_pi

Qc

Kcu

Qgty

Ml

Kcl

Qp

Qgty

Qp

~!s

Qp

Kcm

Kevu

Ys

_pi

Kgd

Kev

!@s

Ys

Qgty

@r

Jme

Kevl

Km

Qa

_pi

Dj

QTp

QTa

Qa

Kk

!@f

_w

Kk

Kk

_f

Kev

Dj

!@f

Qc

Qp

Ml

Qp

Dj

Kcm

Qpw

Kevm

Ml

Dj

Kcl

Qp

Kad

!@f

*Mab

~!s2

Ys

QTp

Kevl

Water

!@f

Mb

*q

Kd

@s1

_pi

Kcm

Ki

Ml

Ml

Qa

!@sc

Qa

!@s

Kbqm

!@s

!@s

Dj

_pi

Ki

Yn

Ks

Qp

Qa

Qgt

Qa

Ml

Kevm

Qp

Kevu

_pi

Ygl

Kcm

Kk

Qp

Jme

Kc

Dj

_pi

*Mab

Qpw

Ki

*q

_m

Kevl

_m

Kqm

Kevm

Ks

_m

Ys

Qp

Kwqm

!@sc

Ktc

Kmd

Qpw

Kcm

Ks

Dj

Dj

!@s

Ki

Ks

Pp

Water

Keva

Qa

Kk

Mm

_pi

Qgty

Qc

Dj

Dj

QTa

Ys

Qgty

Ml

Qa

Dj

Kgd Qa

Kd

Ml

Qoa

Ml

QTp

Qgt

Qc

!@s

Ki

Qpw

Qoa

Dj

Kk

Jm

Water

Qgt

_w

Mm

Kd

_pi

Qp

Kevl

QTp

Kevl

Dj

Dj

Kcm

QTp

Qc

Kqm

_m

QTp1

Kd

QTp

Mm

Mm

Kmh

QTg

Qc

!@s

Qgto

Qp Qc

Kbqm

Kd

Kevm

@s2

Zd

_pi

Qc

_f

!@s

!@s

Ks

Kk

Mm

Ml

Qoa

Qa

Qc

Qgt

QTg

Kevl

Qgty

Qoa

Qp

Kcl

Kqm

*q

Kcm

Qc

_w

Kevu

Kcm

Kevl

!@s

Ynu

Mm

Kevl

Kme

Qa

!@s

Kgd

Kbqm

Ml

Qac

Kk

!@s

Kmf

Jme

Kevl

Ys

_w

Qac

!@f

Ygm

Ksd

Yg

Ki

Qc

Qc

Dj

#ql

Kevm Qoa

Qpw

!@ts

_pi

*q

Kk

Kevl

Dj

_m

@s2

QTg

Zd

Dj

!@s

Kmb

Pp

Qt

Qp

Kcl

QTp1

_f

Ki

Ml

_m

Qp

Kmc

Kk

Kmf

Qp

Ki

Ki

Qa

!@s

Qa

Ki

Ml

Qoa

_m

_p

P*pq

QTp2

Mm

Qp

Kevl

Qa

Mm

Kcm

@s1

QTp

Qp

@s3

Qoa

!@s

_pi

Kcl

Kk

@s3

Qc

Mm

Kevl

_pp

Ql

QTp

Ki

QTg

Ki

Kevu

Kad

!@s

Kcm

Qc

Kcm

!@sc

!@s

Qpw

Kgd

Mm

Mm

Kwqm

_pi

Qc

Dj

Kcm

Ml

Kmd

Keva

Ki

!@s

Kmc

@s3

Ks

*a

Qa

Kad

!@s

Kcm

Kevm

Ktc

Qa

_pi

Qp

Kcm

QTp

Kcl

Qpw

Kcm

Qc

Qog

*q

Kqm

@s1

Water

Kevu

QTp

Jme

Qa

Ki

Qc

Qgt

Qgtc

Kk

_w

Kqm

Kqm

Kk

!@f

Qc

Kevl

Ys

Ql

Ki

Qa

Qa

Kevu

Qa

Qa

Qgtc

Kmc

Kevl

Jme

Qc

Kcm

@s3

Qp

Zd

Qp

Kmc

Kd

Dj

Ktc

_pi

@r

QTp

_m

Kmc

Qoa

Yg

QTp

Ys

Kmc

Qc

!@s1

Qgty

Qp

Kcu

Kmf

!@s

Kcm

Ygl

Ki

Kmc

Dj

Ki

Je

Dj

dt

Qc

_f

Qpw

Kev

_pi

Ml

Qc

Kal

Mm

Kgd

Qoa

Kevu

Qpw

Kd

Kevl

Jme

Qa

QTp

_m

Kmc

Kgd

_w

_m

Qc

Kgd

Qc

Kg

_f

Ks

Qa

@s2

Kcl

Dj

Ys

Qc

Ys

Qog

Qoa

Ql

Kevl

Qt

Km

Kgd

#ql

*q

Kevl

Kgd

Qa

Qa

QTp

QTg

Qt

Ks

QTg

Kmc

Ynl

Ml

@r

Mmu

Ml

Yg

Ks

Mm

Kcl

!@ts

Qa

Kk

Qc

!@s

@r

Kmd

Ki

Qgtc

Mm

Qpw

Ml

_m

Qa

Kcu

Qa

Qc

QTp

Ks

Kgd

_f

Qc

Kevl

Qp

Qpw

QTp

!@s

Kgd

Ys

Kgd

Kcl

_m

Kcu

@s3

Dj

Qc

_pi

Qgt

Kcu

Kevl

Qc

QTp

Qac

Qc

Kevm

QTp

Ki

@s3

Kbqm

QTp

Qc

Kevm

Kevm

Ki

Kevm

Ks

Qgtc

Qa

Kk

Ki

Kcu

Qac

Kma

Keva

Dj

Qp

_w

Kbqmm

Dj

Ql

Pp

Yn

Ki

Dj

!@s

Kme

Qc

Jme

Kad

Qc

Dj

@s3

Dj

Kcu

Ql

Kmd

Qp

Ygl

Kgd

Kme

Qac

Kmg

Kqm

Qgto

Dj

Qt

Kd

Qpw

Kcm

Ki

Ki

QTp

Dj

Kwqm

Ks

Qc

Kal

Qbg

Kevl

Qoa

Ks

*q

Qoa

Qt

Ks

Qac

Mm

Qc

Ki

Qgt

Qc

_w

Kmd

_f

Qp

Kevu

Kbqm

Qac

Keva

Yg

!@s

Ml

Yg

Ys

Qc

Qc

Dj

@r

Qa

Ys

@s1

Kk

Ynu

_f

Dj

Qpw

_pi

Qp

Kcl

Dj

!@s

Kgd

Qc

Kcm

Kd

Kevl

Kgd

Kevm

Qa

Qc

Ql

Qp

Ys

Qp

QTp2

Qa

Qbg

Ql

Kk

_pi

Qp

Kk

Kk

!@s

Kcu

Ks

Kcm

Kal

Ygl

Kcl

Kal

Ks

Ki

Yg

_m

QTp

Kgd

Ks

@s2

Qog

Qc

Qoa

*q

Ki

Kevl

Ki

Qp

Ml

Qa

Qc

Dj

Qc

Kcm

!@s

Ki

#ql

Ks

Qp

Qc

Qc

Dj

Ki

Ynu

Qgt

Ki

Kad

Ys

Qog

Kcu

Kevl

Ys

Qoa

Ki

Qc

!@f

Yg

Qa

*Mab

_m

_f_w

Kmb

MDt

Zd

Qa

_m

Qa

Qa

Zd

_p

Qa

Qa

Dj

QTg

Mb

Qa

Ke

Qa

Kcl

*Mab

_w

P*pq

MDt

_pi

Ki

MDt

!@s

MDt

Qac

Qgty

Qa

_pi

!@s

dt

Kmc

_w

_w

Kma

Jme

Dj

Kcu

_p _f

_p

_w

D_m

Kk

Kk

Qa

Jm

Qa

MDt

Ki

Kc

af

Ml

*Mab

Jm

MDt

Qa

_w

_w

Qa

_m

Kmd

*a

_m

Ktc

Qa

Pp

Kcl

Qgt

_w

Kma

*q

Dj

Kk

_p

Kma

Qpw

Kcl

Qc

Kb

Kbqm

Ys

af

Kk

Dj

Qa

~!s2

Qp

Kcl

Ke

Pp

Ygu

!@s

_p

Mm

Zd

D_m

MDt

Qa

Je

Zd

Jm

QTg

Kmb

QTp

_m

!@s

Qa

Kcm

Qgty

Ki

_p

Jme

_pi

_w

Qac

Ke

QTp

Kk

Qa

Kma

Kcm

Qa

Ki

Ml

Qa

!@s

Dj

*q

Kcl

_w

Kcm

Qc

QTg

_pi

Qa

Qa

Kcl

*Mab

D_m

Qac

Ys

af

Ki

af

Qc

Ktc

Kad

Ml

Kmb

Ml

Qgtc

Jm

Qa

Qa

Kcl

Ye

*q

Qbg

Qa

_pi

Jme

_pi

Qa

Qc

Qag

Ke

Qc

QTp

Qc

Zd

D_m

Kmb

_p

_m

Ki

Ktc

QTp

MDt

Mm

QTp

Qa

_w

Qoa

Ki

Qa

QTp Kcl

Qbg

Qpw

!@f

Kk

QTp1

Qp

Kcm

Ml

Kme

Kcu

_m

*q

Qa

Kk

Qc

Kmd

Qc

Yn

Qc

MDt

QTp

Qgt

Kma

Qt

Kd

_pi

!@s

Qa

Mm

_p

Zd

Ki

Ml

Qa

Kd *q

Jme

Kevu

Kcm

P*pq

Qa

!@s

Kad

Kmd

Ki

Qt

Qa

MDt

!@s

_pi

*Mab

Qa

_pi

!@s

Kcl

Jm

Kcm

Ks

Kma

Ki

Qa

Ynu

Ks

Qc

*Mab

!@s

Kk

Ki

Kk

_w

Kmc

Qa

Qa

Qp

Ks Ks

QTg

Ys

_m

Ktc

Kd

Kmb

Qa

Kcu

Kcl

*q

*q

Qa

Kme

_f

Dj

Qt

Kmb

Qa

Qp

Qt

Qt

_m

_p

Qc

Qa

Qgty

*Mab

Kk

dt

Yg

Yg

_f

_f

Kcl

_f

Kma

_f

QTp

Qa

*a

Qa

_m

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20 20

35

10

25 20

25

25

20 50 30

25

15

15

30

10

15

15

25

10

40 15

15

20

30

40

25

15

20 10

25

15

25

25 30

20

20 25

20

30

30

30

25

10

30

25 30

40

70 30

45

40

10

10

10

10

25

20

15

30

20

15

10

30

30

40

20 20

1025

25

20

20 15

15

10

40

15

30

35

15

10

10

10 20

10 15 20

20

10

15 20

25

40

30

15

25

10

25 10

40

30

10

20

75

65

55

65

35

20

15

40 55

25

35

20

30

20

30

353545

20 65

10

45

45

10

80

80

70

65

75

55 50

30

45

15

15

15

10 15

15

25

35

65

50

75

40

35

20

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35

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55

60

60

40 35

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45

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45 55

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10 55 55 60

60 25 50

30

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15

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70

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35

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45

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40

40

55

55

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70

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10

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35

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45

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35 30 30

55 30

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40

40

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40

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30

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55

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30 55 50

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55

30

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15

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65

65

65

50

60

70

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45

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30

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40 50 70

55

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35

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30

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40

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55 20

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30

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25

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30

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20

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75

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20

40

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35

40

35

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15

25

20

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35

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30

25

25

25

30

50

20 35

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55

30

50

40

60 55

35

40

25

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40

45

30

30 25

35

30

20

25

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45

60

80

20

30 60

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35

20

55 30

35

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40

20

25

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30 15

10 45

45

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90

90

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55

55

23

23

21

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30 33 38

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52

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13

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83 75

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15

35

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20

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52

37

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37

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28

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53

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80

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70

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65

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10

10

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10

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15

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20

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17

Norcen Energy Resources, Ltd., Norcen Balcron UTP Kimpton Ranch 1-11

5

5

5

5

5

3

8

9

5

20

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4052

90

PRELIMINARY GEOLOGIC MAP OF THE TOWNSEND 30’ x 60’ QUADRANGLE, MONTANA

By

Mitchell W. Reynolds and Theodore R. Brandt

2006

U.S. DEPARTMENT OF THE INTERIOR

U.S. GEOLOGICAL SURVEY

Base from U.S. Geological Survey, 1976

Photoinspected 1991

Projection and 10,000-meter grid: Universal Transverse Mercator, Zone 12,

25,000-foot ticks: Montana coordinate symtem, south zone

1927 North American Datum

Digital database by Theodore R. Brandt

Supplementary point digital data by Kenzie J. Turner

Color design of geologic map by Mitchell W. Reynolds

Correlation of map units, and Index to geologic 

mapping drafted by Lisa Ramirez Rukstales

Published by USGS Publishing Network

Manuscript approved for publication May 4, 2006

Holocene

Pleistocene

Pliocene

Miocene

Oligocene

Eocene

Upper

Cretaceous

Lower

Cretaceous

Upper

Mississippian

Lower

Mississippian

Upper

Devonian

Upper

Cambrian

Middle

Cambrian

Belt

Supergroup

Middle

Devonian

QUATERNARY

TERTIARY

CRETACEOUS

JURASSIC

PERMIAN

PENNSYLVANIAN

MISSISSIPPIAN

DEVONIAN

CAMBRIAN

UPPER

PROTEROZOIC

MIDDLE

PROTEROZOIC

CLANCY

CASEY

PEAK

TOWNSEND

NE

GURNETT

CREEK WEST

GURNETT

CREEK EAST

MOUNT

EDITH

ALKALI

WINSTON

LAKE

ELKHORN

CROW CREEK

FALLS

TOWNSEND

HOLKER

LIPPERT

GULCH

SULPHUR

BAR CREEK

BATTLE

GIANT HILL

MOUNTAIN

TACOMA

PARK

DEVILS

FENCE

PARKER

TOSTON

DEER PARK

SIXMILE

MOUNTAIN

FRANCIS

RADERSBURG

DUNN CREEK

WILLOW

SPRINGS

PLUNKET

LAKE

LOMBARD

ROY GULCH

MAUDLOW

BLACKTAIL

MOUNTAIN

RADERSBURG

SW

(6)

(6)

(10)

(2,7)

(4,7) (1,7) (8,7)

(5,7)

(9,7)

(3,7)

112 ̊00' 111 ̊45' 111 ̊30' 111 ̊15' 111 ̊00'

46 ̊30'

46 ̊00'

46 ̊15'

INDEX SHOWING QUADRANGLES AND MAJOR SOURCES OF GEOLOGIC MAPPING

[Reference numbers (in parentheses) are listed in order of principal map contributions for the area shown in discrete color]

Contact—Dashed where approximately located; dotted where concealed

Fault—Dashed where approximately located; short dashed where inferred; dotted where 

concealed; queried where uncertain 

Normal fault—Dashed where approximately located; short dashed where inferred; 

dotted where concealed. Ball and bar on downthrown side

dotted where concealed 

Reverse fault—Dashed where approximately located; short dashed where inferred; 

Thrust fault—Dashed where approximately located; short dashed where inferred; dotted 

where concealed. Sawteeth on upper plate 

Strike-slip fault—Arrows show relative direction of displacement; dashed where 

approximately located; short dashed where inferred; dotted where concealed 

Detachment fault—Dotted where concealed. Teeth on upper plate 

Fault—Inferred from gravity survey

Anticline—Showing trace of axial surface. Dashed where approximately located; 

short dashed where inferred; dotted where concealed; queried where uncertain

Overturned anticline—Showing trace of axial surface and direction of dip of limbs. 

Dashed where approximately located

Inverted anticline—Beds in both limbs are overfolded and dip toward trace of axial 

surface shown. Dashed where approximately located; dotted where concealed

Syncline—Showing trace of axial surface. Dashed where approximately located; 

short dashed where inferred; dotted where concealed; queried where uncertain

Overturned syncline—Showing trace of axial surface and direction of dip of limbs. 

Dashed where approximately located; dotted where concealed

Inverted syncline—Beds in both limbs are overturned and dip away from trace of axial 

surface shown. Dashed where approximately located; dotted where concealed

Dikes and sills

Oil or gas test hole—Showing operator and hole number

Plunging anticline—Showing trace of axial surface. Dashed where approximately located; 

dotted where concealed

Plunging syncline—Showing trace of axial surface. Dashed where approximately located; 

dotted where concealed

Fault—Inferred from aeromagnetic survey

Resources, Ltd.

Norcen Energy 

Kimpton Ranch 1-11

Strike and dip of bedding—Selected attitudes only

Horizontal

Inclined

Overturned

Vertical

Inclined layering in igneous rock—Showing strike and dip

Inclined foliation in layered gneiss or schist

Inclined joint

Vertical joint

—Showing strike and dip

—Showing strike and dip

—Showing strike and dip

40 

65 

10 

20 

30 

Open-File Report 2006-1138

Version 1.0

MAJOR SOURCES OF GEOLOGIC MAPPING

1. Freeman, V.L., Ruppel, E.T., and Klepper, M.R., 1958, Geology of part of the Townsend Valley, 

Broadwater and Jefferson Counties, Montana: U.S. Geological Survey Bulletin 1042-N, p. 

481-556, Plate N, scale 1:48,000. Modified using geologic mapping of source 7.

2. Greenwood, W.R., Ludington, Steve, Miller, W.R., and Hanna, W.F., 1990, Mineral Resources of 

the Elkhorn Wilderness Study area, Broadwater and Jefferson Counties, Montana: U.S. 

Geological Survey Bulletin 1805, 37 p., Plate 1, scale 1:48,000. Modified using geologic 

mapping of source 7.

3. Klepper, M.R., Ruppel, E.T., Freeman, V.L., and Weeks, R.A., 1971, Geology and mineral 

deposits, east flank of the Elkhorn Mountains, Broadwater County, Montana: U.S. 

Geological Survey Professional Paper 665, 66 p., Plate 1, scale 1:48,000. Modified using 

geologic mapping of source 7.

4. Klepper, M.R., Weeks, R.A., and Ruppel, E.T., 1957, Geology of the southern Elkhorn Mountains, 

Jefferson and Broadwater Counties, Montana: U.S. Geological Survey Professional Paper 

292, 82 p., Plates 1-3, scale 1:48,000. Modified using geologic mapping of source 7.

5. Nelson, W.H., 1963, Geology of the Duck Creek Pass quadrangle, Montana: U.S. Geological 

Survey Bulletin 1121-J, p. J1-J56, Plate 1, scale 1:62,500. Modified using geologic 

mapping of source 7.

6. Reynolds, M.W., U.S. Geological Survey, unpublished detailed geologic mapping, scale 1:24,000.

7. Reynolds, M.W., U.S. Geological Survey, unpublished reconnaissance and local detailed geologic 

mapping, scale 1:24,000.

8. Robinson, G.D., 1967, Geologic map of the Toston quadrangle, southwestern Montana: U.S. 

Geological Survey Miscellaneous Geologic Investigations Map I-486, scale 1:24,000. 

Modified using geologic mapping of source 7.

9. Skipp, Betty, and Peterson, A.D., 1965, Geologic map of the Maudlow quadrangle, southwestern 

Montana: U.S. Geological Survey Miscellaneous Geologic Investigations Map I-452, scale 

1:24,000. Modified using geologic mapping of source 7.

10. Weeks, R.A., 1974, Geologic map of the Bull Mountain area, Jefferson County, Montana, U.S. 

Geological Survey Open-File Report 74-354, Scale 1:48,000. 

Any use or trade names in this publication is for

descriptive purposes only and does not imply

endorsement by the U.S. Geological Survey

ArcInfo coverages and a PDF for this map are available at

http://pubs.usgs.gov

APPROXIMATE MEAN

DECLINATION AT

CENTER OF MAP, 1975

MAGNETIC NORTH

18°

TRUE NORTH

QUADRANGLE LOCATION

MONTANA

1 0 1 2 3 5 4 6 7 8 9 10 KILOMETERS

SCALE 1:100 000

CONTOUR INTERVAL 50 METERS

NATIONAL GEODETIC VERTICAL DATUM OF 1929

ELEVATIONS SHOWN TO THE NEAREST METER

1 0 1 2 3 4 5 6 7 8 MILES