geologic map of the house rock spring quadrangle · 15 4 7 2 5 13 5 7 24 20 2 3 1 1 2 13 27 1 3 c c...
TRANSCRIPT
15
4
7
2
5
13
5
7
24
20
2
3
1
1
2
1327
13
C
C
C
4
9
2
2
24
5
5
83
7
2
15
1
5
7
5
17
7
6
2
8
10
22
15
27
5
5
2
1
2
20
28
8
6
16
PkfQaF
Pkf
Pkh
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Qv
Qv
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Qaf
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Pkf
Pkf
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QaE
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^m
QtQaG
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QgF
Ql
^cp
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QaF
Ql
^cp
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Jmod
Jmos
QaE
^cp
Jmod
Jk
Jmos
Ql
Qd^co
QaFQl
Jk
^cp
^coQl
Jn
Qd
Qd Jn
Jn
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Qd
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Jn
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Jn
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Jn
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Qv
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Qt
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Qaf
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Jk
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Qd
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QaF
Qaf Qd
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Jmos
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Jn
QaF
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QaF
160
160
50
40
240
240
160
45
40
100
10
16045
65
152
2
TR
AIL
CAN
YON
FAU
LT
LOW
ER
EA
ST
KAIB
AB
MO
NO
CLIN
E
UPP
ER
EAST
KAIBAB
MO
NOCLI
NE
Qv
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ST
KA
IBA
BM
ON
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This map was printed on an electronic plotter directly from digital files. Dimensional calibration may vary between electronicplotters 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
Available on World Wide Web at http://geopubs.wr.usgs.gov/map-mf/mf2367/
Any use of trade, firm, or product names in this publication is for descriptive purposes only and does not imply endorsementby the U.S. Government
Upper
Triassic
LowerPermian
Middle(?) and Lower Triassic
Holocene
Pleistocene
QUATERNARY
TRIASSIC
PERMIAN
JURASSIC
Qaf Qs Qd
SURFICIAL DEPOSITS
Qa
Qa
Qg Qa
Qa Qv Qt
3
4
1 1
2
Unconformity
Unconformity
Jn
Jk
Jmos
Jmod
^co
^cp
^cs
^m
Pkf
Pkh
Ptw
Ptb
Pts
Ph
Qaf
Qs
Qd
Qv
Qg1
Qa 1
Qt
Ql
Qa2
Qa3
Qa4
Jn
Jk
Jmos
Jmod
^co
^cs
^cp
^mMoenkopi Formation, undivided (Middle? and Lower Triassic)
Kaibab Formation (Lower Permian)
Harrisburg Member
Toroweap Formation (Lower Permian)
Fossil Mountain Member
Pkh
Pkf
Woods Ranch Member
Brady Canyon Member
Seligman Member
Hermit Formation (Lower Permian)Ph
Ptw
Ptb
Pts
Kayenta Formation (Lower Jurassic)
Shinarump Member
Petrified Forest Member
SEDIMENTARY ROCKSSURFICIAL DEPOSITS
LIST OF MAP UNITS
Artificial fill and quarries (Holocene)
Stream-channel alluvium (Holocene)
Sand-sheet and dune deposits (Holocene)
Young terrace-gravel deposits (Holocene)
Young alluvial fan deposits (Holocene)
Valley-fill deposits (Holocene and Pleistocene)
Talus deposits (Holocene and Pleistocene)
Landslide deposits (Holocene and Pleistocene)
Old terrace-gravel deposits (Holocene and Pleistocene)
Old intermediate alluvial fan deposits (Pleistocene)
Young intermediate alluvial fan deposits(Holocene and Pleistocene)
Old alluvial fan deposits (Pleistocene)
Glen Canyon Group (Lower Jurassic)
Navajo Sandstone (Lower Jurassic)Surficial deposits (Holocene and Pleistocene)
Owl Rock Member
Dinosaur Canyon Member
Springdale Sandstone Member
Moenave Formation (Lower Jurassic)
Chinle Formation (Upper Triassic)
15
C
Qg 2 Ql
Qg 2
Prepared in cooperation with the
U.S. NATIONAL FOREST SERVICE
Universal Transverse Mercator Projection
1927 North American Datum
Clark 1866 Ellipsoid, Zone 12
COCONINO COUNTY, NORTHERN ARIZONA
2001
SCALE 1:24,000
1 KILOMETER
ARIZONA
QUADRANGLE LOCATION
GEOLOGIC MAP OF THE HOUSE ROCK SPRING QUADRANGLE,
Base from U.S. Geological Survey, 1:24,000, House Rock Spring Quadrangle, 1988
Pamphlet accompanies mapMISCELLANEOUS FIELD STUDIES MF-2367DEPARTMENT OF THE INTERIOR
U. S. GEOLOGICAL SURVEY
ByGeorge H. Billingsley and Haydee M. Hampton
11207 30 11205 00 11202 30 11200 00
11207 30 11205 00 11202 30 11200 0036 45 00
36 47 30
36 50 00
36 52 30
36 45 00
36 47 30
36 50 00
36 52 30
CORRELATION OF MAP UNITS
Unconformity
Unconformity
Unconformity
Unconformity
Lower
Jurassic
SEDIMENTARY ROCKS
TR
UE
NO
RT
H
MA
GN
ET
IC N
OR
TH
APPROXIMATE MEANDECLINATION, 1997
13.5O
EXPLANATION
Contact
Fault
Folds
Monocline
Syncline
-(Approximate contact for surficial units and between the Harrisburgand Fossil Mountain Members of the Kaibab Formation)
-Dashed where inferred or approximately located; dotted whereconcealed; bar and ball on downthrown side. Number is estimatedfault separation in feet
-Showing trace of axial surface and direction of plunge; dashed whereapproximately located; dotted where concealed
-Axial trace drawn approximately along steepest part of fold
Anticline
Strike and dip of beds
Inclined
Strike of vertical and subvertical joints
Sinkhole
-As indicated on aerial photos
-Measured in the field
30
CONTOUR INTERVAL 40 FEET
DATUM IS MEAN SEA LEVEL
Geology mapped in 1999 by G.H. BillingsleyDigital database by H.M. Hampton
Edited by Jan L. ZiglerManuscript approved for publication April 23, 2001
Collapse Structure(possible breccia pipe)
1 0.5 0 1 MILE
1 0.5 0
O
Inclined