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with Laramide movement shownMiranda fault zone
Embudo fault
AT
AT AT
A T
A TA
T
A T
AT
TV-205abandoned(projected)
TV-128RG-57268
TV-131RG-78874
TV-133RG-81518
TV-134RG-83373
Ttc
XYuXYuXYu XYu
XYu
Xho
Xho
XYu
Xmg
Tp
Tp Tp TpTp
Tp
Tp
TpTplq
Ttc Ttc Ttc Ttc
TtcQf2
8,000
7,000
6,000
5,000
8,000
7,000
6,000
5,000
Elevationfeet abovesea level
HNW
Elevationfeet abovesea level
H'SE
CROS
S SE
CTIO
N I-
I'
Embu
do fa
ult
Embu
do fa
ult
Embu
do fa
ult
Embu
do fa
ult
Embu
do fa
ult
Embu
do fa
ult
Embu
do fa
ult
Embu
do fa
ult
Embu
do fa
ult
Embu
do fa
ult
Los
Cord
ovas
faul
t
ATAT
AT
AT
ATAT
AT
AT
Picu
ris -
Peco
s fa
ult
Picu
ris -
Peco
s fa
ult
Embu
do fa
ult
Embu
do fa
ult
Embu
do fa
ult
Embu
do fa
ult
Embu
do fa
ult
Embu
do fa
ult
Picu
ris -
Peco
s fa
ult
Lara
mide
mov
emen
t
Lara
mide
mov
emen
t
AT
A TA T
Lara
mide
mov
emen
tA T
Embu
do fa
ult
Embu
do fa
ult
Embu
do fa
ult
Embu
do fa
ult
AT
AT AT
AT AT
ATAT AT
AT
AT
AT AT
AT AT
Mira
nda
faul
t
Proj
ectio
n of
La
Ser
na fa
ult
Embu
do fa
ult
Embu
do fa
ult
Embu
do fa
ult
Embu
do fa
ult
Embu
do fa
ultEm
budo
faul
tEm
budo
faul
t
Embu
do fa
ult
Embu
do fa
ult
Embu
do fa
ult
Embu
do fa
ult
Embu
do fa
ult
Los
Cor
dova
sfa
ult
Lara
mide
mov
emen
t
Lara
mide
mov
emen
t
AT
AT
A T A T
AT AT
ATAT
AT
AT
AT
AT
AT
Proj
ectio
n of
L
a Se
rna
faul
t
Embu
do fa
ult Em
budo
faul
t
Embudo
fault
Los
Cord
ovas
faul
t
Embu
do fa
ult
Embu
do fa
ult
Embu
do fa
ult
Embu
do fa
ult
Embu
do fa
ult
Embu
do fa
ult
Embu
do fa
ult
Embu
do fa
ult
Proj
ectio
n of
Mira
nda
faul
t
Proj
ectio
n of
McG
affe
y fa
ult
fa
ult
Los
Cor
dova
sLa
ram
ide m
ovem
ent
Laram
ide m
ovem
ent
Lara
mide
mov
emen
t
AT
AT
AT
A T
Embu
do fa
ult
AT
AT
AT
AT
ATAT
AT
Proj
ectio
n of
Pi
curis
-Pec
os
faul
t sys
tem
Embu
do fa
ult
Los Cordovas fault
Embu
do fa
ult
Embu
do fa
ult
Embu
do fa
ult
Embu
do fa
ult
Embu
do fa
ult
Embu
do fa
ult
Embu
do fa
ult
Embu
do fa
ult
Embu
do fa
ult
Embu
do fa
ult
Embu
do fa
ult
A T
Lara
mide
mov
emen
t
AT
AT
AT
ATAT
AT
AT
AT
AT
AT
AT
ATAT
A T
? ? ?
GRAVITY MODEL
TV-198RG-80117
TV-149RG-77935
(long projected)
TV-100RG-83352 TV-230
RG-76468
TV-196RG-80207
(projected)
TV-140RG-76925
(projected)
TV-199RG-87207
TV-166RG-79997
TV-263RG-81875
(projected)
TV-139RG-88461
TV-115RG-55576
(projected)
TV-103RG-88886
(projected) TV-191RG-91446
TV-289RG-91454
TV-288RG-91449
TV-107RG-37157x
(projected)
TV-106RG-27921
TV-104RG-52607-CLW
TV-124RG-83204
(projected)
TV-233RG-83497
(projected) TV-167RG-87080
(projected)
TV-127RG-45679
TV-125RG-82804
(artesian)
TV-204
TV-121RG-67154 TV-186
RG-80614TV-192RG-50140
(projected)
TV-171RG-37303
TV-174
TV-208WWTP-10
TV-176WWTP-2
TV-177WWTP-9(projected) TV-232
RG-39071(projected)
TV-260RG-80824
(long projection)TV-119
RG-64885(projected)
TV-162RG-78996
(projected)(projected)
TV-175RG-74193
TV-118RG-18848
TV-183RG-03894
(projected) TV-201RG-62881
TV-234RG-62881
DRY(projected) TV-207
RG-75724
TV-269(projected)
TV-160(projected)
TV-137RG-unknown
TV-168RG-30133 TV-148
RG-91630TV-146RG-85313
TV-111RG-50511
(long projection)
TV-142RG-35148
(long projection)
TV-182RG-03894-S
(long projection) TV-264RG-59636
(projected)
TV-235RG-62881
TV-201RG-62881
(projected)TV-207
RG-75724
?
Tc
TcTc
TcTc
Tto & TcTto & Tc
Tto & Tc
Tto & TcTto & Tc
Tto & TcTto & Tc
Tto & Tc
Tto
Ttc
XhXh
Xh
Xhr1/2
Xho
Xho
XvXv
Xv
Xv
TpTp
TpTp
Tp
Tp
Tp
TpTbo
TpTp Tp
TtcTtc
TtcTtc
Ttc
Ttc
Ttc
TtcTtc
TtoTto
TtoTto
Tto
TtoTto Tto
Tc
TcTc
Tc
Tc Tc
Qt2rp
Xhr3
Qf1Qf1
Ttc
Tsb
Tsb TsbTsb
Tsb
Tsb
XYu
XYu
XYu
XYu XYu
XYu
QTl
QTl
QTl
Tp
TboTp
Tbo
TsbTlcTlc QTl
QTlQTl
Tc
Tlc
TcTcTc
Tto & TcTto & Tc
Tto & Tc
Tto & TcTto & Tc
Tto & Tc
Tto & Tc
Tto
Ttc
XhoXho
Xho
Xv ?
Xv
XvXv
Xmg
Tp TpTp
TpTp
Tp
Tp
Tp
Tp
TpTp
TtcTtc
TtcTtc
Ttc
Ttc
Ttc
Ttc
TtoTto
TtoTto
Tto
TtoTc
Tc
Tc TcQt2rp Qf2
Qf2Qfy
Qf2
Tsb Tsb TsbTsb
Tsb
Tsb
XYu XYu
XYu
XYu
XYu
XYu
XYu
XYu
XYuXYu
XYuXYu XYu
QTl
QTl
QTlQTl
QTl
TsbTsbTsb
TlcTlc
QTl QTl
TsbQTl
TsbQTl
GRAVITY MODELAT
TcTc
TsbTc
Tto & Tc
Tto & Tc
Tto & TcTto & Tc
Tto
Ttc
XYu
XYu
XYu
XYu
XYuXYuXYu
XYu
XYu
XYuXYu
XYuXYuXYu
XYuXYu
XYu
XmgX
Tp
Tp
TpTp
Tp
Tp
Tp
Tp
Tp
Tp
Tp Tp Tp TpTp
Ttc
Ttc
Ttc
Ttc
Ttc
TtcTtc
Ttc TtcTtc
Ttc
Tto
Tto
Tto
TtoTc
TcTc
TcQt2rp
Tsb
Qf1Qf2
TsbTsb
Tsb
QTlQTl
QTl
Qf2
Tsb
Tsb QTlQf1
TcTc
Tc
Tsb
Tsb
Tto & Tc Tto & TcTto & Tc
Tto & Tc
Tto & Tc
Ttc
TpTp
TpTp
TpTp
Tp
Tp
Tp
Tp
Tp Tp
Ttc
TtcTtc
Ttc
Ttc
Ttc
TtcTtc
Ttc
TtoTto
Tto Tto
Tto
TtoTc TcTc
TcTc
Tsb Tsb
QtyQal
?
TplqQf1
Qf1Qf2
?? ?
QTlQTlQTlQTl
QTl
QTl
QTl
QTl
XYu
XYu
XYuXYu
XYuXYu
XYuXYu
XYuXYuXYuXYu
Tsb
TcTc
Tc
Tto & TcTto & Tc
Tto & Tc
Ttc
Tp
TpTp
TpTp
Tp
Tp
Tp
Tp
TpTp
TpTp
Ttc
Ttc
Ttc
Ttc
TtcTtc
TtcTtc
Ttc
Ttc
TtoTto Tto
Tto
Tc
Tc TcTc
Qal Qal
Tsb Tsb
Tsb
QTlQTl
QTl
QTl
QTl
QTl
XYu
XYu
XYuXYuXYu
XYu
XYu
XYuXYu
XYu
XYu
AT
adnariM oyorr
A
.Q.
L ai uqecA
Rio
Pue
blo
de T
aos
Arroyo del Alamo
PICURIS MOUNTAINS
s oaT ed ol beu
P oiR
Arr
oyo
Mir
anda
Spri
ngs
Pon
ce d
e L
eon
hot
spri
ng
s oaT ed ol beu
P oiR
Rio
Gra
nde
del R
anch
o
Rio
Gra
nde
del R
anch
o
Rio
Gra
nde
del R
anch
o
PICURIS MOUNTAINSs oa
T ed ol beuP oi
R
Ace
quia A
cequ
ia
BlueberryHill 68240
68
68
68
Rio
Pue
blod
e T
aos
0 1,000 meters
0 2,000 feet
Elevationfeet abovesea level
ENW
E'SE
CROS
S SE
CTIO
N F
-F'
CROS
S SE
CTIO
N G
-G'
7,000
6,000
5,000
4,000
3,000
2,000
8,000
7,000
6,000
5,000
4,000
3,000
2,000
Elevationfeet abovesea level
DNW
Elevationfeet abovesea level
D'SE
CROS
S SE
CTIO
N F
-F'
CROS
S SE
CTIO
N G
-G'
7,000
6,000
5,000
4,000
3,000
2,000
8,000
7,000
6,000
5,000
4,000
3,000
2,000
Elevationfeet abovesea level
Elevationfeet abovesea level
CNW
C'SE
CROS
S SE
CTIO
N F
-F'
CROS
S SE
CTIO
N G
-G'
CROS
S SE
CTIO
N I-I
'
685707,000
6,000
5,000
4,000
3,000
2,000
7,500
7,000
6,000
5,000
4,000
3,000
2,000
570
Elevationfeet abovesea level
BNW
Elevationfeet abovesea level
B'SE
CROS
S SE
CTIO
N F
-F'
CROS
S SE
CTIO
N G
-G'
CROS
S SE
CTIO
N I-
I'
CROS
S SE
CTIO
N A
-A'
7,000
6,000
5,000
4,000
3,000
2,000
7,500
7,000
6,000
5,000
4,000
3,000
2,000
7,500
7,000
6,000
5,000
4,000
3,000
2,000
1,000
7,500
7,000
6,000
5,000
4,000
3,000
2,000
Elevationfeet abovesea level
ANW
Elevationfeet abovesea level
A'SE
CROS
S SE
CTIO
N F
-F'
CROS
S SE
CTIO
N G
-G'
CROS
S SE
CTIO
N I-
I'
CROS
S SE
CTIO
N B
-B'
TaosCounty
N E W M E X I C O
Scale 1:24,000No vertical exaggeration
GIS Support: Mark Mansell and Brigitte Felix
Location Geologic units (Detailed map unit desriptions are in Appendix 1) Map symbols
Well key
New Mexico Bureau of Geology and Mineral Resources
A division of New Mexico Tech
Socorro, NM 87801(575) 835 5490
geoinfo.nmt.edu
Embu
do fa
ult
Los
Cord
ovas
faul
t
Los
Cor
dova
s fa
ult
Los
Cord
ovas
faul
t
Los
Cor
dova
s fa
ult
Los
Cor
dova
s fa
ult
Los
Cord
ovas
faul
t
Los
Cord
ovas
faul
t
Los
Cord
ovas
faul
t
Los
Cor
dova
s fa
ult
Los
Cor
dova
s fa
ult
Los
Cor
dova
s fa
ult
Embu
do fa
ult
Embu
do fa
ult
Embu
do fa
ult
Proj
ectio
n of
La
Ser
na fa
ult
Proj
ectio
n of
P
icur
is-P
ecos
f
ault
Proj
ectio
n of
M
irand
a fa
ult
Lara
mide
mov
emen
t
Pro
ject
ion
of
Rio
Gra
nde
del R
anch
o fa
ult
Lara
mide
mov
emen
t
Lara
mide
mov
emen
t
Lara
mide
mov
emen
t
A TA T
A T
A T
TV-195RG-87837
TV-199RG-87207
TV-121RG-67154
(projected)
TV-173RG-83207
TV-227RG-83209
TV-238RG-67648
TV-154RG-49046
TV-279RG-85980
TV-163artesian
TV-147artesian
TV-276RG-82913artesian(projected) TV-283
RG-52846
TV-150RG-78943
TV-282RG-82234
TV-145RG-41884
(projected)
TV-155RG-39866
(projected)
TV-143RG-83661
(projected)TV-177
WWTP-9(projected)
TV-165RG-69193
(projected)TV-198RG-80117
TV-280RG-74971
(projected)TV-290(projected)
Spri
ng T
S-56
Spri
ng T
S-58
?
Spri
ng T
S-54
TcTcTsb
Tc
Tto & Tc
Tto & TcTto & Tc Tto & Tc Tto & Tc
Tto & TcTto & Tc Tto & Tc
Tto & Tc
Tto & TcTto & TcTto & Tc
Tto & Tc
Tto
Tp
XYu XYuXYu XYu XYu XYu
XYuXYu
Tp TpTp
Tp TpTp Tp Tp
Tp Tp Tp TpTp
TpTp Tp
TtcTtc Ttc
TtcTtc
TtcTtc
TtcTtcTtc Ttc Ttc
Ttc TtcTtc
TtcTto
TtoTto Tto Tto
Tto TtoTto
Tto TtoTto
Tto
TtoTto
Tto
TcTc Tc Tc Tc Tc Tc Tc
Tc Tc Tc Tc Tc Tc Tc
Qls
Tsb
Tsb
Tsb
TsbTccQls Tcc
Qt2rpQt2rp Qt3rpQalQt2rpTsb Qt2rpQt2rp
TsbTsbTsb TsbTsbTsb
Tsb
TsbTsb
Qf1 QalQt4rp
QTl
QTlQTl
QTlQTl
QTl
QTl QTl QTlQTl
QTl QTl
TlcTsb
Tsb
QTlTlc
Tto & Tc
Tsb
QTl
Tsb
QTl
Tsb
QTl
Tsb
QTl
Tsb
QTl
TsbTsb
QTlTlc
QTl
Arr
oyo
del A
lam
o
WW
TP
ou
tflo
w
Rio
Gra
nde
del R
anch
o
Rio
Fer
nand
o de
Tao
s
Ran
chit
os (
orP
ache
co)
ditc
h
NM-2
40an
d ac
equi
a
967,000
6,000
5,000
4,000
3,000
2,000
7,000
6,000
5,000
4,000
3,000
2,000
1,000
Elevationfeet abovesea level
CROS
S SE
CTIO
N A
-A'
Bend
Bend
CROS
S SE
CTIO
N E
-E'
Bend
CROS
S SE
CTIO
N D
-D'
CROS
S SE
CTIO
N B
-B'
Bend
Elevationfeet abovesea level
CROS
S SE
CTIO
N C
-C'
1,000
FWest
F'East
AT
ATA
T
AT
App
rox.
loca
tion
of
Rio
Pue
blo
grad
ient
cha
nge
AT A
TA T
A T
Lara
mide
mov
emen
t
Los
Cor
dova
sfa
ult
Los
Cor
dova
s fa
ult
Los
Cor
dova
sfa
ult
Los
Cord
ovas
faul
t
Los
Cord
ovas
faul
t
Los
Cord
ovas
faul
t
Embu
do fa
ult
Pro
ject
ion
of
Pic
uris
-Pec
os
faul
t
Proj
ectio
n o
f L
a Se
rna
faul
t
Proj
ectio
n o
f Mira
nda
faul
t
Proj
ectio
n of
R
io G
rand
e d
el R
anch
o fa
ult
TV-272BOR3
TV-273BOR-2A
TV-274, TV-275BOR2B, BOR2C
TV-274intermediate
TV-116RG-90552
(projected)
TV-153RG-75582
(projected)TV-105(projected)
TV-219NGDOM
TV-217BOR1Deep
TV-218BOR1
shallow
TV-103RG-88886
(projected)
TV-229RG-63879
(projected)TV-101(long
projected)
TV-275deep
TV-257RG-82811
Tc
Tto & TcTto & Tc Tto & Tc
Tto
Ttc
XYu
XYuXYu XYu XYu
Tp
Tp TpTp
Tp
TpTp Tp
TtcTtc Ttc TtcTtc Ttc
Ttc
Tto TtoTto Tto
TcTc
Tc Tc Tc
Tc Tc
Qt1QtyQf2Qf11.27 Ma
ash Qt2rprpQalQf1Qf1 QfuQt4 QfuQf1 Qf2 Qf2
Tbo
Qf2 Qf1
QTlQTl QTlQTl
QTlQTl??? ? ? ? ? ? ? ?
Ace
quia
Arr
oyo
del A
lam
o
Hon
do C
anyo
n
Ace
quia
Ace
quia
L
lano
Que
mad
o
CROS
S SE
CTIO
N D
-D'
CROS
S SE
CTIO
N C
-C'
CROS
S SE
CTIO
N E
-E'
Bend
CROS
S SE
CTIO
N B
-B'
CROS
S SE
CTIO
N A
-A'
Rio
Gra
nde
del R
anch
o
Bend
240
Elevation
feet abovesea level
GSW
Elevationfeet abovesea level
G'NE
7,000
6,000
5,000
4,000
3,000
2,000
7,000
6,000
5,000
4,000
3,000
2,000
AT
Lara
mide
mov
emen
t
Lara
mide
mov
emen
t
Lara
mide
mov
emen
t
A T
AT
A
T
AT
A
TA
TA
TA
T
Lara
mide
mov
emen
t
Laram
ide m
ovem
ent
Laram
ide move
ment
Embudo faultEmbudo fault
Embudo fault
Embudo fault
Embu
do fa
ult
Picu
ris-P
ecos
faul
t
Picu
ris-P
ecos
faul
t
Picuris
-Pecos f
ault
TV-209RG-83482
TV-221TV-220
TV-213RG-85775
TV-216RG-85773
TV-211RG-85777
XYu
TtcTtc Ttc
XYu
XYu
XYu
XYu
XhoXmgXmg
Xmg
Xmg
Xvg
Xmg
Tp Tp
TpTp
Tp
Tp Tp
Tplq
Tp
Tp
Tp
Tp
TtcTtc
XYu
Qf1Qf1Qal
QcAce
quia
CROS
S SE
CTIO
N H
-H'
CROS
S SE
CTIO
N J-
J'
CROS
S SE
CTIO
N C
-C'
CROS
S SE
CTIO
N B
-B'
CROS
S SE
CTIO
N A
-A'
Rio
Gra
nde
del R
anch
o
Spri
ng T
V-5
01
7,000
6,000
5,000
4,000
3,000
9,000
8,000
7,000
6,000
5,000
4,000
3,000
9,000
8,000
Elevation
feet abovesea level
INorth
Elevationfeet abovesea level
I'South
A TA T
A T A T
A T AT
AT
Picu
ris-P
ecos
faul
t
La
Sern
a fa
ult
Mira
nda
faul
t
Mira
nda
faul
t
TV-215RG-85771
(projected)TV-214
RG-85772 TV-212RG-85776
Xmg
Xmg
Xmg
Xmg
XmgXmg
Xmg
Xho
Xv
TpTp
Tp
breccia
Qc
Xhr
Xhr6Xhr5
YtpYtpl
XYu
XYu XYu
XYuXYu
Arr
oyo
del A
lam
o
Arr
oyo
Mir
anda
CROS
S SE
CTIO
N I-
I'
Edge
of P
late 1
map
Val
leci
tos
MIRANDA GRABENPICURIS MOUNTAINS
7,000
6,000
5,000
9,000
10,000
8,000
7,000
6,000
5,000
9,000
10,000
8,000
Elevation
feet abovesea level
Elevation
feet abovesea level
JWest
J'East
Lara
mide
mov
emen
t
GRAVITY MODEL
GRAVITY MODEL
GRAVITY MODEL
GRAVITY MODEL
GRAVITY MODEL
Qal Alluvium (latest Pleistocene and Holocene)
Qc Colluvium (middle Pleistocene to Holocene)
Qls Landslides in Rio Grande gorge and tributaries (late Pleistocene to Holocene)
Qfy Qty Young alluvial-fan and stream terrace deposits (latest Pleistocene to Holocene)
Qt4rp Alluvial-fan and stream terrace deposits of the Rio Pueblo de Taos and tributaries (middle? to late Pleistocene)
Qt3rp Alluvial-fan and stream terrace deposits of the Rio Pueblo de Taos and tributaries (middle to late Pleistocene)
Qf2 Alluvial-fan and stream terrace deposits of the Rio Pueblo de Taos Qt2rp and tributaries (middle? Pleistocene)
Qf1 Alluvial-fan and stream terrace deposits of the Rio Pueblo de Taos and tributaries (middle Pleistocene)
Qfu Alluvial fan deposits, undivided (middle to late Pleistocene)
Qfo Alluvial fan and terrace deposits, undivided (middle to late Pleistocene)
Tsb Servilleta Basalt (Pliocene)
QTl Lama formation (Pliocene to early? Pleistocene)
Tlc Clay, Lama formation (Pliocene)
Tc Chamita Formation, undivided, Santa Fe Group (Miocene? and Pliocene)
Tto Ojo Caliente Sandstone of Tesuque Formation, Santa Fe Group (Miocene)
Ttc Chama-El Rito Member of Tesuque Formation, Santa Fe Group (Miocene)
Tp Picuris Formation, undivided (Oligocene to Miocene)
Tplq Llano Quemado Breccia member of Picuris Formation (Oligocene)
Tbo Older basaltic rocks (Oligocene)
Cenozoic deposits and rocks
breccia Mixed fault breccia (late Proterozoic? to Tertiary?) Sedimentary rocks of the Taos Trough, undivided (Pennsylvanian)
Well head (actual elevation, if projected)Volcanic intervals (Tv from well record) Screened interval
OSE well file numberNMBG database name (Table 1 and Figure 5)TV-154
RG-49046
N E W M E X I C O B U R E A U O F G E O L O G Y A N D M I N E R A L R E S O U R C E S
Geologic Cross Sections of the Southern Taos Valley,Taos County, New Mexico
Open-file Report 581June 2016
Plate 2
Paul W. Bauer, Peggy S. Johnson, and Keith I. Kelson
Ytpl Piedra Lumbre Formation, Trampas Group (Mesoproterozoic)
Ytp Pilar Formation, Trampas Group (Mesoproterozoic)
Xh Hondo Group, undivided (Paleoproterozoic)
Xhr Rinconada Formation (Paleoproterozoic)
Xhr6 R6 schist member, Rinconada Formation (Paleoproterozoic)
Xhr5 R5 quartzite member, Rinconada Formation (Paleoproterozoic)
Xhr3 R3 quartzite member, Rinconada Formation (Paleoproterozoic)
Xhr1/2 R1/R2 schist member, Rinconada Formation (Paleoproterozoic)
Xho Ortega Formation, Hondo Group, undivided (Paleoproterozoic)
Xmg Miranda granite (Paleoproterozoic?)
Xvg Glenwoody Formation (Paleoproterozoic)
Xv Vadito Group, undivided
XYu Proterozoic rocks, undivided (Paleoproterozoic and Mesoproterozoic)
Proterozoic rocks Fault – Arrows show sense of vertical movement
Strike-slip fault movement, away
Strike-slip fault movement, towardContactGradational contact
A
T
Paleozoic rocks
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