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NMBMMR Open File Map SeriesOF–GM–2 and OF–GM–16
PLATE II of III.
Sean D. Connell1
Bernalillo quadrangleNMBMMR OF-DM-16
May 1998
Placitas quadrangleNMBMMR OF-DM-2
June 1995
Sean D. Connell1, Steve M. Cather2 , Bradley Ilg3,Karl E. Karlstrom3, Barbara Menne3, Mark Picha3,
Chris Andronicus3, Adam S. Read2, Paul W . Bauer 2,and Peggy S. Johnson2
NEW
MEXICO
S
TATE M A
P
NM
Bu
re
au
of Mines & MineralR
eso
ur
ce
s
Earth Science for the 21st Century
Ne w Me x i c o Tech
Dr. Peter A. ScholleDirector and State Geologist
Dr. Paul W . BauerGeologic MappingProgram Director
17 February 2000 Revision
1New Mexico Bureau of Mines and Mineral Resources, Socorro, NM 87801,Albuquerque Office, Albuquerque, NM 87106
2New Mexico Bureau of Mines and Mineral Resources, Socorro, NM 878013Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, NM 87131
CROSS SECTION LOCATIONS
CC'
B
B'
A'
D'
E'
D
E
A
Bernalillo Quadrangle –NMBMMR OF-DM-16
(Connell, 1998)
Placitas Quadrangle –NMBMMR OF-DM-2(Connell, et al., 1995)
106°37'30"35°22'30"
106°22'30"35°22'30"
106°37'30"35°15'
106°30' 106°22'30"35°15'
NEW MEXICO BUREAU OF MINES AND MINERAL RESOURCESA DIVISION OF NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY
Geology of the Bernalillo and Placitas quadrangles, Sandoval County,
New Mexico
PLATE II of III.
GEOLOGIC CROSS SECTIONS
1:24,000
Valley Viewfault Ranchos
fault
Caballofault
Placitasfault
WestLas Huertas
fault
EastLas Huertas
fault
A'E
-9,000'
-8,000'
-7,000'
-6,000'
-5,000'
-4,000'
-3,000'
-2,000'
-1,000'
0 SL
1,000'
2,000'
3,000'
4,000'
5,000'
6,000'
7,000'
8,000'
9,000'
10,000'
11,000'
12,000'
13,000'
14,000'
15,000'
16,000feet ASL
Xu
Xu
Xu
Xu
Xu
Xu
Xu
Xu
Xu
Ys
Jm
Kml
Kml
QTspcs
Kmf
Tg?
Kmf
Kml
Py
Jm
Kmf
Tspc
Kmf
Kmf
Kmf
Kmf
Kmf
Kmf
Pa
Jm
Pa
Pa
Py
Py
Pa
Py
Jm
Jm
Jm Jm
Xu
PaPy
Pa
Pa
Py
Py
Pa
PaKmf
Jm
˛m
ˇcp
Xu
Jm
Jm
Kmf
Kmu
Khd
Kd
Jt
Je
Ma
PgPsJm
Kd
KhdKmu
Je
Je
JmJt
Jt
Kd
KhdKmu
Pa
˛s
ˇm
Je
Jt
Kd
Pg
Khd Kmf
Ma
Ma
Ma
Ma
Ma
Pg Ps
Kd
Jt
Je
Khd
Khd
Khd
Khd
Jm
Kd
Kd
Kd
Pg Ps
Pg
Ps
PgPs
Je Jt
JtJe
Je
JeMa
Ma
˛s
Pa
Ma
Khd
Khd
Jt
JeJe
Jt
Kd
Kd
Jt
Kd
Je
Pg
Pg
Ps
Ps
Pg Ps
Ma
ANW
-9,000'
-8,000'
-7,000'
-6,000'
-5,000'
-4,000'
-3,000'
-2,000'
-1,000'
0 SL
1,000'
2,000'
3,000'
4,000'
5,000'
6,000'
7,000'
8,000'
9,000'
10,000feet ASL
-10,000'
BE
RN
AL
ILL
OP
LA
CIT
AS
Ys
Ys
Xu
˛m
˛s
Ma
˛m
˛s
Pay
QTsa
Tsp
Te?
Tg
Kmf
KhdKmu
Kml
KdJm
Je
Jt
ˇcp
ˇz
˛m
?
?
Psg
Pa
PyPsPg
ˇm ˇz
ˇcp
ˇz
Kml Kml
KhdKmu
Kmu
ˇz
ˇm
˛s
˛s
˛m
ˇm
ˇcp
ˇz
Kml
Kml
Kmu
Jt
Kml
Kmu
ˇcp
ˇcp
ˇz ˇm
˛m
˛s
˛s
˛m
˛s
ˇzˇm
ˇcp ˇcp
Py
Pa
Kml
Kml
Kmu
Kmu
Kmu
Kml Kmu
Khd
Kml
ˇcp ˇcp
ˇz
ˇm
Ps
ˇmˇz
˛s
˛s
˛m
˛m
˛m ˛s
˛s
˛m
˛m˛s
ˇzˇm
ˇcp
ˇcp
ˇzˇm
Kml
Kmu
QHaQpm
Ranchitofault
Bernalillofault
Lucefault
QTspcs
Tz
QTo
Tz
QTo
Tg
Pay
ˇcp
ˇz
Psg
ˇm
ˇcpˇm
Kmf
Khd
Kml
Kd
Jm
Je
Jt
Je
Jt
Jm
Kd
Kml
Khd
Kmf
Kmu
Kmu
Tg
Tz
QTo
Tz
QTo
Tg
Kmf
KhdKmu
Kml
Pay
ˇcp
ˇz
Psg
Jm
Kd
Je
Jt
˛m
?
Tspc
Tspc
ˇm ˇz
RioGrande
QrpQae/Qay
Qae/Qam
-10,000'
ˇm
Qre
-4,000'
-3,000'
-2,000'
-1,000'
0 SL
1,000'
2,000'
3,000'
4,000'
5,000'
6,000'
7,000'
8,000'
9,000'
10,000'
Placitasfault
QTo
Kmf
Khd
Kmu
Kml
Pa
ˇcp
ˇz
Ps
Jm
˛m
Qre and Qpm
ˇm
B'S
-4,000'
-3,000'
-2,000'
-1,000'
0 SL
1,000'
2,000'
3,000'
4,000'
5,000'
6,000'
7,000'
8,000'
9,000'
10,000'
16,000feet ASL
12,000'
13,000'
14,000'
15,000'
11,000'
BN
16,000feet ASL
11,000'
12,000'
13,000'
14,000'
15,000'
QpmQrp and QHa
Qss QssQTst
Qss
QTsa
QTsa
QTsa
QToQTspcs
QTspcs
QTst
QTspcs
Tspc
Tg
Te
Te
Tg
Tspc
Kmu
Khd
Kmu
Kd
Jt
Je
Pg Py
Bend inCross Section B-B'
Kmf
Khd
Kmu
Kmf
KmlJm
KdJt
Pa
ˇcp ˇz
Ps
˛m
ˇm
Pg Py
JtJe
ˇcp
Khd
Kmu
Kmf
Kml
Kd
Jm
Jt Je
Jm
KdKml
Khd
Kmu
Kml
Khd
Kmu
Py
ˇmˇz
ˇcp
˛m
ˇz
Py
Pa
˛m
Pg Psˇm
ˇcp
˛s
Ma
˛s
Xms
Xa
Xms
Xas
Xas
Xa
Xa
Xms
˛s
Ma
Ma
˛s
Xas
Xas
Xas
Xa Xss
Xss
Ys
Ys
Ys
Xa
Xa
XaXa
Xa
Xas˛s
Je
Jt
Jm
KdKml
Khd
KmfKmu
Ma
Xss
Lomosfault
Placitas fault zone
? ?
Las Huertasgeomorphic surface
No Vertical Exaggeration
0 SL
1,000'
2,000'
3,000'
4,000'
5,000'
6,000'
7,000feet ASL
4,000'
5,000'
6,000'
7,000'
0 SL
1,000'
2,000'
3,000'
WestValley View
fault
CW
EastValley View
fault
RG49
8025
2
Pa
Ps
˛m
Pg
Py
ˇm
˛s
Ma
˛s
BRE EF
W
C'E
Escalafault
SanFrancisco
fault
Escalasyncline Py
Pa
Ps
Pg
˛m
Qay
Qay
Y/Xu
Y/Xu
Kmf
Tg
Te
QTsa
QTst
QTspcs
Tspc
Tspc?
Tsps?
QTsa
Kmu
KhdKml
TD700 ft
TD610 ft
TD495 ft
No Vertical Exaggeration
RG51
722
(pro
ject
ed)
SHD
-B1
SHD
2
SHD
1
SAP2 R
io G
rand
e
SAP1
SASF
1
RWP-
14 (p
roje
cted
)
Qrp
Qre
Qpm
Projected base of Qrl
Ancestral Rio Grande terraces
Inner valley of the Rio Grande
Qre
Qrd?Qam
Qay
QTo
QTo
QTsa
QHa
Qam
?
?
??
4800'
5000'
5200'
5400'
5600feet ASL
TD265 ft
TD
800
ft
TD101 ft
TD118 ft
TD180 ft
TD43 ft
D'
RG-6
4146
RG-6
2037
(pro
ject
ed)
TD335 ft
TD170 ft
Las Huertasgeomorphic surface
Projectedbase of Qrl
Ancestral Rio Grande terraces
Inner valley of the Rio Grande
Qrp
Qrd?
Qpm
Qrm
Qre
Qay
Qam-Qrd
Qam
??
?
ESE
4800'
5000'
5200'
5400'
5600'
5800feet ASL
DWNW
5,400'
5,600feet ASL
5,200'
5,000'
4,800'
EWNW
5,400'
5,800feet ASL
5,200'
5,000'
4,800'
E'ESE
QTo
?
?
?
?
?
?
?
?
?
?
?
?
Vertical Exaggeration =10x
?
TD
810
ft
TD
1,04
3 ft
Vertical Exaggeration =10x
QTsp
QTsa
5,600'
?
?
Bend inCross Section E-E'
QToQTo
Horizontal Scale
1 0.5 0 1 Mile
1000 0 1000 2000 3000 4000 5000 6000 7000 Feet
Cross sections are constructed based upon the interpretation of the authors madefrom geologic mapping, and available geophysical (regional gravity and aeromagneticsurveys), and subsurface (drillhole) data. Cross sections should be used as an aidto understanding the general geologic framework of the map area, and not be thesole source of information for use in locating or designing wells, buildings, roads,or other man-made structures.