xmg xmv xms - u.s. geological survey publications · pdf filexmv xmv xmv xmv xmv xmv xmv xmv...
TRANSCRIPT
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107°00'00" 106°52'30" 106°45'00" 106°37'30" 106°30'00" 106°22'30" 106°15'00"
107°00'00" 106°52'30" 106°45'00" 106°37'30" 106°30'00" 106°22'30" 106°15'00"
35°00'00"
34°52'30"
34°45'00"
35°00'00"
34°52'30"
34°45'00"
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Long Dalies #1TD 2,539 m
Harlan Ranch #3TD 1,973 m
JoinerSan Clemente #1
TD 1,709 m
Shell IsletaCentral #1TD 4,982 m
Shell Isleta #2TD 6,482 m
TransOcean
Isleta #1TD 3,163 m
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Pueblo of Isleta
tribal lands boundary
MohinasMtn
HiddenMtn
CAT MESA
VOLCANIC FIELD
CAT HILLSVOLCANIC FIELD
WINDMESA
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LOS LUNASVOLCANIC FIELD
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AN
DE
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Pueblo of Isleta triballands boundary
Pueblo of Isletatribal lands boundary
Pueblo of Isletatribal lands boundary
BLACK MESAVOLCANIC FIELD
WEST M
ONTOSA
FAULT
BERNALILLO CO
VALENCIA CO
BERNALILLO CO
VALENCIA CO
BERNALILLO CO
TORRANCE CO
VA
LEN
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CO
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RR
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Base from U.S. Geological SurveyDigital Line Graphs (DLG), 1:100,000, Belen, 1979.Projection, zone 13, Universal Transverse Mercator.1927 North American Datum
Sources of geologic mapping shown on figure 3.GIS database by D. Paco VanSistine.
Manuscript approved for publication December 30, 2004
U.S. DEPARTMENT OF THE INTERIORU.S. GEOLOGICAL SURVEY
SCIENTIFIC INVESTIGATIONS MAP 2913Pamphlet accompanies map
Any use of trade names is for descriptive purposes only and does not imply endorsement by the U.S. Government
For sale by U.S. Geological Survey Information ServicesBox 25286, Federal Center, Denver, CO 802251-888-ASK-USGS
ArcInfo coverages and a PDF for this map are available at http://pubs.usgs.govPrinted on recycled paper
SCALE 1: 50 000
CONTOUR INTERVAL 50 METERSSUPPLEMENTARY CONTOUR INTERVAL 25 METERS
NATIONAL GEODETIC VERTICAL DATUM OF 1929
1 1/ 2 0 1 2 3 4 MILES
1 .5 10 2 3 4 5 KILOMETERS
1U.S. Geological Survey, Denver, Colo.2New Mexico Bureau of Geology and Mineral Resources, Socorro, N. Mex.3Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, N. Mex.
MAP LOCATION
NEW MEXICO
12°
APPROXIMATE MEANDECLINATION, 1979
MA
GN
ET
IC
NO
RT
H
TR
UE
N
OR
TH
GEOLOGIC MAP OF THE
PUEBLO OF ISLETA TRIBAL LANDS AND VICINITY,
BERNALILLO, TORRANCE, AND VALENCIA COUNTIES,
CENTRAL NEW MEXICOBy
Florian Maldonado1, Janet L. Slate1, David W. Love2, Sean D. Connell2, James C. Cole1, and Karl E. Karlstrom3
2007
LIST OF MAP UNITS
EOLIAN, ALLUVIAL, COLLUVIAL, LANDSLIDE, AND PIEDMONT-SLOPE DEPOSITS
Eolian sand (Holocene and upper Pleistocene?)
Younger alluvium and colluvium (Holocene)
Older alluvium and colluvium (Holocene(?) to upper and middle Pleistocene)
Landslide deposits and colluvium (Holocene(?) to upper and middle Pleistocene(?))
Young piedmont-slope deposits (middle Pleistocene)
Volcanic-rich alluvium and colluvium (lower Pleistocene)
FLUVIAL DEPOSITS OF THE RIO GRANDE AND RIO PUERCO
Channel and low terrace deposits of the modern Rio Grande and Rio Puerco (upper Holocene)
Floodplain deposits of the modern Rio Grande and Rio Puerco (upper Holocene to upper Pleistocene(?))
Youngest fluvial terrace deposits of the older Rio Grande and Rio Puerco (upper Pleistocene)
Intermediate fluvial terrace deposits of the older Rio Grande (middle Pleistocene)
Older fluvial terrace deposits of the older Rio Grande (middle Pleistocene)
SANTA FE GROUP
Santa Fe Group, undivided (middle Pleistocene to upper Oligocene)—Shown only on cross section
Eastern piedmont-slope deposits
Intermediate piedmont-slope deposits (middle and lower Pleistocene)
Old piedmont-slope deposits (lower Pleistocene)
Oldest piedmont-slope deposits (Pliocene(?) to upper Miocene(?))
Ancestral Rio Grande
Sand, silt, and clay unit of San Clemente (lower Pleistocene)
Gravel-rich fluvial deposits of the ancestral Rio Grande (lower Pleistocene)
Sand- and silt-rich fluvial deposits of the ancestral Rio Grande (lower Pleistocene)
Sand- and silt-rich (Qs) and gravel-rich (Qg) fluvial deposits of the ancestral Rio Grande, undivided (lower Pleistocene)
Ancestral Rio Puerco, Rio San Jose, and Rio Jemez(?)
Ceja Formation
Sand, silt, and clay unit of Chavez Grant (upper Pliocene(?))
Upper sand and gravel unit (upper Pliocene)
Middle silt, sand, and clay unit (upper Pliocene)
Lower sand and gravel unit (Pliocene)
Sand and gravel unit of Apache graben (Pliocene(?))
Ceja Formation, undivided (Pliocene)
Piedmont-slope and playa-lake deposits
Popotosa Formation (Miocene and upper Oligocene)
PRE-SANTA FE GROUP
Unit of Isleta well number 2 (Oligocene to Eocene)—Shown only on cross section
Galisteo, Baca, and Nacimiento Formations and Ojo Alamo Sandstone, undivided (Eocene to Paleocene)—Shown only on cross section
VOLCANIC AND SUBVOLCANIC ROCKS
Volcanic rocks of Cat Hills volcanic field
Cinder deposits of Cat Hills (upper to middle(?) Pleistocene)
Lava flows of Cat Hills, undivided (upper to middle(?) Pleistocene)
Volcanic rocks of younger Los Lunas volcanic field (El Cerro de Los Lunas)
Lava flows and cinder deposit of younger Los Lunas volcano, undivided (lower Pleistocene)
Volcanic rocks of Black Mesa volcanic field
Lava flow of Black Mesa (upper Pliocene)
Volcanic rocks of Isleta volcanic field
Lava flows of Isleta volcano, undivided (upper Pliocene)
Cinder deposits of Isleta volcano (upper Pliocene)
Hydromagmatic tephra (base-surge) deposits of Isleta volcano (upper Pliocene)
Volcanic rocks of Cat Mesa volcanic field
Lava flow of Cat Mesa (upper Pliocene)
Intrusive rocks of El Cerro Tomé
Andesitic plug of El Cerro Tomé (upper Pliocene)
Volcanic and subvolcanic rocks of older Los Lunas volcanic field (El Cerro de Los Lunas)
Lava flows and intrusive rocks of older Los Lunas volcano, undivided (lower Pliocene)
Volcanic rocks of Wind Mesa volcanic field
Cinder deposits of Wind Mesa (lower Pliocene)
Lava flows of Wind Mesa, undivided (lower Pliocene)
Intrusive rocks of Mohinas Mountain
Basaltic intrusive rocks of Mohinas Mountain (late Miocene)
MESOZOIC AND PALEOZOIC SEDIMENTARY ROCKS
Crevasse Canyon Formation of the Mesaverde Group (Upper Cretaceous)
Triassic and Permian rocks, undivided (Upper and Middle Triassic and Lower Permian)
Madera Group (Upper and Middle Pennsylvanian)
Upper arkosic unit (Upper Pennsylvanian)
Lower cherty fossiliferous limestone unit (Upper and Middle Pennsylvanian)
Sandia Formation (Middle and Lower Pennsylvanian)
PROTEROZOIC INTRUSIVE ROCKS
Mafic intrusive rocks, undivided (Early to Middle Proterozoic)
Manzanita granite of Karlstrom and others (1997) (Early Proterozoic)
Ojito granite of Karlstrom and others (1999b) (Early Proterozoic)
PROTEROZOIC METAMORPHIC ROCKS
Metasedimentary rocks, undivided (Early Proterozoic)
Metavolcaniclastic and mafic metavolcanic rocks, undivided (Early Proterozoic)
MESOZOIC TO PROTEROZOIC ROCKS
Mesozoic to Proterozoic rocks, undivided (Mesozoic to Proterozoic)—Shown only on cross section
Contact—Approximately located; dotted where concealed; queried where uncertain
Normal fault—Bar and ball on downthrown side where relative movement known. Dashed where approximately located; dotted where concealed; queried where uncertain. Arrow indicates direction and amount of dip where known. Where faults cut compound units (for example, Qe/Qpu) the Qe unit is not offset by fault
Lateral fault—Approximately located. Opposed arrows indicate lateral movement
Thrust fault—Sawteeth on upper plate. Dashed where approximately located; dotted where concealed. Opposed arrows (where present) indicate a component of lateral movement
Inferred fault interpreted from aeromagnetic data
Tuff ring that encircles maar at Isleta volcano—Dotted where concealed
Crater at Los Lunas volcano
Anticline
Plunging anticline
Overturned anticline
Plunging syncline—Dotted where concealed
Overturned syncline
Strike and dip of bedding
Inclined
Horizontal
Overturned
Mylonitic layering in Proterozoic rocks
Inclined
Vertical
Sample location number—See table 1
Spring deposits along Hubbell Spring fault—Composed of calcium-carbonate-cemented eolian and alluvial sands
Water-supply and ground-water monitoring well—Showing well-name abbreviation
Oil test well—Showing well-name abbreviation and total depth in meters
Calcic soils (Pleistocene to Pliocene)—Mapped west of the Rio Grande. Soils that formed in the upper part of units Qsc and Tcc are white, have stage II to III carbonate morphology, and are as much as 1 m thick. Soils that formed in the upper part of units Tcu and Tc and underlie the Llano de Albuquerque are white and have stage III to IV carbonate morphology. Generally less than 2 m thick, but locally forms stacks of multiple buried soils as much as 10 m thick in hanging walls of faults
Veneer of younger unit (first symbol; Qe or Qr3) covering older unit (second symbol; varies)
NOTE: Locally, drainages and topographic contours do not register.
Qe
Ti
Tic
Tih
Tfc
Tat
Tlv
Twmc
Twm
Tbim
Tui
Tgb
KcKc
�P
�mu
�ml
�s
XYm
Xmg
Xog
Xms
Xmv
��
Qac
Qaco
Qls
Qva
Qp
Qp2
Qp1
Tpd
Qrc
Qr3
Qr2
Qr1
QTs
Qsc
Qg
Qs
Qsg
Tcc
Tcu
Tcm
Tcl
Tca
Tc
Tp
Qcc
Qch
Qlv
Tbm
Qrf
80
5
45
70
13
RWP 021
Mesa del SolTD 504 m
Qe/Qac
EOLIAN, ALLUVIAL, COLLUVIAL, LANDSLIDE, AND
PIEDMONT-SLOPE DEPOSITS
Easternpiedmont-
slopedeposits
FLUVIAL DEPOSITSOF THE RIO GRANDE
AND RIO PUERCO
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Ancestral Rio Puerco,Rio San Jose, and
Rio Jemez(?)
Ancestral Rio Grande
C O R R E L A T I O N O F M A P U N I T S
S A N T A F E G R O U P PRE-SANTA FEGROUP
VOLCANIC ANDSUBVOLCANIC ROCKS
Volcanic rocks ofCat Hills volcanic field
Volcanic rocks of youngerLos Lunas volcanic field
Volcanic rocks of Cat Mesa volcanic field
Intrusive rocks of Mohinas Mountain
Volcanic rocks of Isleta volcanic field
Volcanic rocks of Black Mesa volcanic field
Intrusive rocks of El Cerro Tomé
Volcanic and subvolcanic rocks ofolder Los Lunas volcanic field
Volcanic rocks of Wind Mesa volcanic field
BEDROCK
Unconformity
Unconformity
Unconformity
Unconformity
Unconformity
Unconformity
Unconformity
Unconformity
Unconformity
Unconformity
Unconformity
Unconformity
Unconformity
Unconformity
Unconformity
UnconformityCalcicsoil
Calcicsoil
Calcicsoil
Calcicsoil
1.2 Ma *
*1.2 Ma
98±20 ka, 110±30 ka,140±38 ka
1.246±0.017 Ma
*
*
1,659±5 Ma1,645±16 Ma * *
3.8±0.04 Ma
3.4±0.4 Ma
3.00±0.01 Ma
2.68±0.04 Ma
8.3±0.02 Ma
2.79±0.04 Ma2.73±0.04 Ma,2.75±0.03 Ma,2.78±0.06 Ma
3.91±0.04 Ma
4.01±0.16 Ma
*
**
*
*
**
*
*
Qe
Qac Qrc
Qrf
Qr3
Qr2
Qr1
QsgQs
QgQsc
Qaco
Qva
Qls
Qp
Qp2
Qp1
Tpd
QTs
Tc
Tcc
Tcu
Tcl
Tca
Tcm
Tbm
Qlv
QchQcc
TicTi Tih
Tfc
Tat
Tlv
TwmTwmc
Tbim
Tp
Kc
Tgb
Tui
�P
�mu
�ml
�s
XYm
XmsXogXmg Xmv
��
Holocene
Pleistocene
Pliocene
Miocene
Oligocene
upperPleistocene
middlePleistocene
lowerPleistocene
QUATERNARY
TERTIARY
CRETACEOUS
11.5 ka
132 ka
785 ka
1.8 Ma
5.3 Ma
EARLY TO MIDDLE PROTEROZOIC
EARLY PROTEROZOIC
PENNSYLVANIAN
TRIASSICAND PERMIAN
Oligoceneand EoceneEocene toPaleocene
Piedmont-slopeand playa-lake
deposits
36.3±1.8 Ma*
View to north of Cat Hills volcanic field
View to south of Floripa cone, largest cone of Cat Hills volcanic field
View to north of Llano de Albuquerque and calcic soil overlying the Ceja Formation (Tc)
Fault and calcic soils overlying the Ceja Formation (Tc), northwestern part of Llano de Albuquerque
Sand dunes overlying the Ceja Formation (Tc), northwestern part of Llano de Albuquerque
BlackbirdHill
Floripa
Llano de Albuquerque
Calcic soil
Calcic soilQe
MOUNTA
INVIEW
FAULT
16,000
14,000
12,000
10,000
8000
6000
4000
2000
0
2000
4000
6000
8000
FEET
16,000
14,000
12,000
10,000
8000
6000
4000
2000
0
2000
4000
6000
8000
FEETA A'
RWP 018(projected)
RWP 036(projected)
Shell Isleta #2(projected)TD 6,482 m
TransOcean Isleta #1(projected)TD 3,163 m
Mesa del Sol(projected)TD 504 m
1000 ft = 304.8 m.Quaternary surficial deposits not shown except for Qrf in Rio Grande area. Santa Fe Group deposits combined into QTs; locally, QTs includes Quaternary surficial and piedmont deposits; QTs exaggerated where thin. Cross section not balanced in some areas due to thickening and thinning across growth faults. Location and dip of Mountainview fault are projected from seismic reflection data (shown in blue) of Russell and Snelson (1994, fig. 7, p. 94), who referred to it as the Rio Grande fault. Other faults interpreted from their seismic reflection data are also shown in blue.
QTs
QTs
QTs QTs QTs
Tui
Tui Tui
Tui
Tgb
Tgb Tgb
Tgb
Tgb
Tgb
Twm
Twm
Twm?Twm?
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��
��
��
��
��
QrfTi
TihQch
Isleta Pueblo grabenWind Mesa horst Mountainview prong
BE
ND
IN
SE
CT
ION
BE
ND
IN
SE
CT
ION
BE
ND
IN
SE
CT
ION
BE
ND
IN
SE
CT
ION
BE
ND
IN
SE
CT
ION
CAT MESAFAULT
WESTERN WINDMESA FAULT
EASTERN WINDMESA FAULT PALACE-PIPELINE
FAULT
McCORMICKRANCH FAULT HUBBELL SPRING FAULT ZONE
WEST MONTOSAFAULT
RIO GRANDE
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Arroyo
de Pab
lo