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23

12

20

13

10

20

25

24 14

10 14

20

10 15

15

20

20

20

20

15

23

13

16

13

12 10

16

10

15

10 10

25

15

28

22 40

38

40

30

40 25

33

25

10

18 10

28

20 13

23

28

22

27

12 18

10

38

50

45

60

3222

30

30

15

12

35

25

24

10

15

27

14

18

24

15

10

64

33 23

13

11

17

25

70

10

12

15

13

10

15

20

25 13

20

45

10

23 35 35

13

45 77

28 10

12

10

18

12

18

13

30

65 18

15

13 10

15

35

20 72

22

40

25 33

18 55 35

40

17

23

15

15

15 23

13

20

20

18

10

15

16

55

10

22

16

25

30

30

12

25

20

27

30

28

18

12

20

17

80

20 10

13

14

25

14

17

10

15

13 15

12

20

27

20

35 20

23

10

32

20

28

50

28

18

17

15

17

16

10

15

24

28

20

14

40

13

27

25

16

10

40

65

18 35

80 24

35 30

38

20 20 18

57

55

20

45

10

40

15

10

30

28

45 40

10

20

10

20

35

20 20

35

12

35

20

10 13

15

10

20

12

15

18 32 10

10

15

10

35

10

12

20

10 10

23

13

17 10

40

55

10

28

30

11

18

15

15

15

55

14

17 14

18

10

10

20

12

28

10

30

10

12

12

10

10

10 12

10

10

10

27

12

10

16

12

13 10

20

10

40

40

10

42

35

22

12

37

45

50

90

35

27

17

18

17

10

13

12

10

48

10

10

70

87

80

85

10

10

10

10

23

13

10

10

17

23

12

16

15

11

10 13

15

15

16

10

10

10

15 12

13

10

10

13

13

10

15

15

11

10

12

10

15

15 15

10 82

10

23

17

10

10

15

20

13

12

14 13

10

18

30

20

25

35

65

90

80 80

12

18

12

10 15

11

85

35

40

45

10

80

10

12

12

13

10

15

13

20

15

35

30

40 40

10 17

28

12

10

10

17

80

10

12

17

30

12

10

18

15

65

90

60

80

90

65

80

75 50

7045

22

75

60

30

11 15

80

6

8

4

3

5

3

5

8

5

9

5

7

4

4 7

4

6

5

5

0

8

3

7

5

2

3

26

28

35

70 25

25

40

68

15

43

43

50

43

68

50

35

26

30

35

40

13

15

18

48

22

22

38

38

35

20

28

28

90 12

45 32

55 50

40

45

36

42

30

10

20

22

18

22

10

12

10

10 16

20

10

20

33

10

28 10

42

16

12

15

45 10

15

20

10

20

22

14

35

15

57

70

90

90

20

80

18

15

90

13

30

15

10

15

14

10

20

Kcol

Kfr

Colorado Group, lower part, undivided (Lower Cretaceous)

Fall River Formation (Lower Cretaceous)

Qa

Qoa

?

Qc Qac

Ql

QTl

?

!@s

?

!@f

@s

?

~!s ~!g

?

mt

Qt

@b

Tbg

?

?

QTp QTp1 QTp2 QTp3

Qp

?

QTg

?

Qog

Qgt

Qgty

Ke

Kfb

Kfr

Kk

Kcol

Kcl

Ktc

Mb

*Mab

Mho

Mh

Mo

Mk

Mmu

Mm

Ml

Mlb

MDt

Du

Cu

Dj

D_m

_pi

_pmw

_pp

_p

_m

_w

_f

Ys

Yn

Yg

Yc

Ynei

Xag

Xbg Xgda Xa Xd

Wd

Xpd

Xgg

Kc

*q

*a

Mts

Mt

Kfl

Kmt

KJm

KJme Js

Jp

Je

#g #qm

#lwt #rp #sn

@#rb

?

#bhqm #di #bhd #d

Qa

Qac

Qog

Qc

mt

Ql

Qoa

Ys

Yg

Yn

Ynei

Yc

Kk

KJme

KJm

Je

Js

Jp

Mts

*q

*a

Mt

Mho

Mh

Mo

Mk

Mb

*Mab

Mmu

Mm

Ml

Mlb

MDt

Du

Dj

D_m

_pp

_u

_pi

_pmw

_p

_m

_w

_f

Xag

Xgg

Xgda

Xa

Xd

Xbg

Xpd

Wd

Qp

Qt

Qgt

Tbg

Qgty

QTg

QTp

QTp1

QTp2

QTp3

~!s

~!g

!@s

@b

@s

@#rb

#lwt

#rp

#sn

#g

#qm

#bhqm

#m

#bhd

#d

Kcl

Ke

Ktc

#di

Kc

Kfb

Kmt

Kfl

QTl

!@f

Disconformities

Unconformities

Unconformity

Unconformity

Unconformity

Unconformity

Unconformity

Unconformity

Unconformity

Unconformity

Local unconformity

Unconformity

Unconformity

Unconformity

Units of Sedimentary and Volcanic Origin Units of Igneous Intrusive and Metamorphosed Igneous Origin

Unconformity

Unconformity

Intrusive contacts

CORRELATION OF MAP UNITS

Big Snowy

Group

Ellis

Group

Madison

Group

Alluvium (Holocene)

Alluvium and colluvium, undivided (Holocene)

Old gravel (Holocene or Pleistocene)

Colluvium (Holocene)

Mine tailings (Holocene)

Landslide deposit (Holocene and Pleistocene)

Old alluvium (Holocene? or Pleistocene)

Belt Supergroup (Mesoproterozoic)

Spokane Formation

Greyson Formation

Newland Formation

Neihart Quartzite

Chamberlain Formation

Kootenai Formation (Lower Cretaceous)

Morrison Formation (Lower Cretaceous and Upper Jurassic)

and Ellis Group (Upper and Middle Jurassic), undivided

Morrison Formation (Lower Cretaceous and Upper Jurassic)

Ellis Group (Upper and Middle Jurassic)

Swift Formation (Upper Jurassic)

Piper Formation (Middle Jurassic)

Sandstone beds in lower and middle parts

Quadrant Formation (Pennsylvanian)

Amsden Formation (Pennsylvanian)

Tyler Formation, undivided (Upper Mississippian)

Heath and Otter Formations, undivided

Heath Formation

Otter Formation

Kibbey Formation

Big Snowy Group, undivided (Upper Mississippian)

Amsden Formation (Pennsylvanian) and Big Snowy Group

(Upper Mississippian), undivided

Madison Group, undivided (Upper and Lower Mississippian)

Mission Canyon Limestone (Upper and Lower Mississippian)

Lodgepole Limestone (Lower Mississippian)

Biohermal limestone in lower part

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 Upper Cambrian rocks

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

Upper and Middle Cambrian rocks, undivided

Pilgrim Formation (Upper Cambrian)

Park Shale (Upper and Middle Cambrian), Meagher Limestone (Middle Cambrian),

and Wolsey Formation (Middle Cambrian), undivided

Park Shale (Upper and Middle Cambrian)

Meagher Limestone (Middle Cambrian)

Wolsey Formation (Middle Cambrian)

Flathead Sandstone (Middle Cambrian)

Augen gneiss (Paleoproterozoic)

Granite gneiss (Paleoproterozoic)

Gneissic granite and granodiorite, undivided (Paleoproterozoic)

Amphibolite (Paleoproterozoic)

Metadiorite (Paleoproterozoic)

Biotite gneiss (Paleoproterozoic)

Pinto Diorite (Paleoproterozoic)

Metadiorite (Neoarchaean)

Pediment gravel (Holocene? and Pleistocene)

Terrace gravel (Holocene and Pleistocene)

Glacial till, undivided (Pleistocene)

Boulder gravel (Pliocene? or Miocene?)

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

(Holocene and Pleistocene)

Older gravel (Pleistocene or Pliocene)

Older pediment gravel, undivided (Pleistocene and Pliocene)

Older pediment gravel, lowest level where two or more adjacent levels 

 overlie bedrock (Pleistocene and Pliocene) 

Older pediment gravel, higher level where two or more adjacent levels

 overlie bedrock (Pleistocene and Pliocene) 

Older pediment gravel, highest level where more than two

 levels overlie bedrock (Pleistocene and Pliocene) 

Sedimentary rocks with minor tuffaceous beds (Pliocene and Miocene)

Gravel and interbedded finer clastic strata (Pliocene and Miocene?)

Sedimentary rocks, undivided (Miocene and Oligocene)

Basalt (Oligocene)

Sedimentary rocks underlying basalt (Oligocene and Eocene?)

Rhyolite with breccia blocks of Paleozoic rocks (Oligocene? and Eocene)

Lithic welded tuff (Eocene)

Rhyolite porphyry (Eocene)

Shonkinite (Eocene)

Granite (Eocene)

Quartz monzonite (Eocene)

Biotite hornblende quartz monzonite (Eocene)

Monzonite (Eocene)

Biotite hornblende dacite (Eocene)

Dacite (Eocene)

Claggett Formation (Upper Cretaceous)

Eagle Sandstone (Upper Cretaceous)

Telegraph Creek Formation (Upper Cretaceous)

Biotite diorite (Eocene)

Cody Shale (Upper Cretaceous)

Frontier Formation, Big Elk Sandstone Member (Upper Cretaceous)

Mowry Shale (Lower Cretaceous) and Thermopolis Shale (Lower 

Cretaceous), undivided

Frontier Formation, lower part (Upper? and Lower Cretaceous)

Older landslide deposit (Pleistocene or Pliocene?)

Fort Logan Formation (Miocene and Oligocene)

LIST OF MAP UNITS

Holocene

Pleistocene

Pliocene

Miocene

Oligocene

Eocene

Upper

Cretaceous

Lower

Cretaceous

Upper

Jurassic

Middle

Jurassic

Upper

Mississippian

Lower

Mississippian

Upper

Devonian

Upper

Cambrian

Middle

Cambrian

Belt

Supergroup

Middle

Devonian

QUATERNARY

TERTIARY

CRETACEOUS

JURASSIC

PENNSYLVANIAN

MISSISSIPPIAN

DEVONIAN

CAMBRIAN

MESOPROTEROZOIC

PALEOPROTEROZOIC

NEOARCHEAN

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 

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

 dotted where concealed 

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; dotted where concealed 

Low-angle fault of gravity origin—Certain. Teeth on upper plate 

MDt Trace of thin formation on steep slope

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

 short dashed where inferred; dotted where concealed 

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

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

Cm Trace of thin formation on steep slope

Jp Trace of thin formation on steep slope

DCm Trace of thin formation on steep slope

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—Showing strike and dip

Inclined joint—Showing strike and dip

40 

65 

10 

20 

30 

APPROXIMATE MEAN

DECLINATION AT

CENTER OF MAP, 1984

MAGNETIC NORTH

16°

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

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

BUBBLING

SPRINGS

BELT PARK

BUTTE

YOGO

PEAK

BANDBOX

MOUNTAIN

WOODHURST

MOUNTAIN

NEIHART

RED HILL

UTICA

STRAWBERRY

BUTTE

MOOSE

MOUNTAIN

SAND POINT

ETTIEN

SPRINGS

INDIAN

HILL

BROWNS

CANYON

TWIN

KINGS HILL

SISTERS

 COXCOMBE

BUTTE

CHARCOAL

GULCH

HOOVER

SPRING

RUSSIAN

FLAT

DAISY PEAK

HAYMAKER

NARROWS

JELLISON

PLACE

VOLCANO

BUTTE

WHITE

SULPHUR

SPRINGS

PINCHOUT

CREEK

FOURMILE

SPRING

CHECKERBOARD

MOUNT

HOWE

MUD CREEK

HAYMAKER

RANCH SW

HAYMAKER

RANCH

111 ̊00' 110 ̊45' 110 ̊30' 110 ̊15' 110 ̊00'

47 ̊00'

46 ̊30'

46 ̊45'

INDEX TO MAJOR SOURCES OF GEOLOGIC MAPPING AND 7.5-MINUTE QUADRANGLES

MAJOR SOURCES OF GEOLOGIC MAPPING

2

1 3

1. Keefer, W.R., 1972, Geologic map of the west half of the Neihart 15-minute quadrangle, central Montana: 

U.S. Geological Survey Miscellaneous Geologic Investigations Map I-726, scale 1:62,500.

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

3. Vogl, J.J., Foster, D.A., Mueller, P.A., Wooden, J.L., and Mogk, D.W., 2004, Lithology and age of preBelt Precambrian basement in the Little Belt Mountains, Montana: implications for the role of the 

Great Falls tectonic zone in the Paleoproterozoic assembly of North America: Northwest Geology, 

v. 33, p. 15-29; figure 2, approximate scale 1:139,000.

PRELIMINARY GEOLOGIC MAP OF THE WHITE SULPHUR SPRINGS 30' x 60' QUADRANGLE, MONTANA

Mitchell W. Reynolds and Theodore R. Brandt

2007

U.S. DEPARTMENT OF THE INTERIOR

U.S. GEOLOGICAL SURVEY

Base from U.S. Geological Survey, 1984

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

Color design of geologic map by Mitchell W. Reynolds

Correlation of map units, list of map units, and index to

geologic mapping drafted by Lisa Ramirez Rukstales

Published by USGS Publications Service Group

Manuscript approved for publication October 13, 2006

Open-File Report 2006-1329

Version 1.1