Geology of the Bernalillo and Placitas s quadrangles ...
Transcript of Geology of the Bernalillo and Placitas s quadrangles ...
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NMBMMR Open File Map SeriesOF–GM–2 and OF–GM–16
Map last modified 17 February 2000PLATE I of III.
(SANDIA CREST)
GNMN
0° 50'
15 MILS
13.5°240 MILS
UTM GRID AND 1954 MAGNETIC NORTHDECLINATION AT CENTER OF SHEET
106°30' 364 367 27'30" 368 370 25'
NEW MEXICO
LOCATION OF QUADRANGLES
374000m E.35°15'
106°22'30"(SANDIA PARK)
3902000m N.
3909
3910
3912
3913
3915
17'30"
(HA
GA
N)
20'
35°22'30"106°22'30"
(SAN F
ELIPE
PUEBLO NE)PLACITAS QUADRANGLE
NEW MEXICO
430 000 FEET
106°30' 364 R. 5 E. 27'30" 368 371 25'
Base from U.S. Geological Survey 1954Polyconic projection, 1927 North American datum, 10,000-foot grid based on New
Mexico coordinate system, cental zone1000-meter Universal Transverse Mercator grid ticks, zone 13, shown in blue
Geologic mapping: S. D. Connell (Quaternary), S. M. Cather (Cenozoic), Bradley Ilg(S.E. section of quadrangle), C. Andronicus, A. S. Read, and K. E. Karlstrom (Proterozoic),
B. Menne and M. Picha (M.S. Theses -- Phanerozoic)
D. J. McCraw, M. M. Mansell, and Glen E. Jones: digital cartographic production
373 460 000 FEET372370(SAN FELIPE PUEBLO)
1 0.5 0 1 MILE
1000 0 1000 2000 3000 4000 5000 6000 7000 FEET
1 0.5 0 1 KILOMETER
NATIONAL GEODETIC VERTICAL DATUM OF 1929
PLACITAS CONTOUR INTERVAL 20 FEET
SCALE 1: 24,000
366000m E.
373
1 590 000FEET
T. 13 N.
3914
DIA
MO
ND
TA
ILR
AN
CH
4.4
MI
3908
3907
3906
3905
3904
T. 12 N.
3903
SAN ANTONITO 14 MIINTERSTATE 40 20 MI
R. 5 E.R. 4 E.366
SANTA FE 39 MILAS VEGAS 105 MI R. 4 E. R. 5 E.367 374
B'
A'
C'
C
(ALAMEDA)
GNMN
0° 54'
16 MILS
12.5°222 MILS
UTM GRID AND 1972 MAGNETIC NORTHDECLINATION AT CENTER OF SHEET
106° 37' 30"
(LOS G
RIEGOS)
ALAMEDA 6.6 MI.ALBUQUERQUE 14 MI.
358 32' 30" 363000m E.
BERNALILLO QUADRANGLENEW MEXICO
470 000 FEET
106° 37' 30" 353000m E. 356 R. 3 E.35' 32' 30"
1 550 000FEET
363420 000 FEET361(SANTA ANA PUEBLO)
3915000m N.
(BERNALILLO NW)
T.13 N.
(LO
MA
MA
CH
ETE
)
BERNALILLO CONTOUR INTERVAL 10 FEET
CU
BA
59 M
I.S
AN
YS
IDR
O 1
6 M
I.
354
Base from U.S. Geological Survey 1954, photorevised 1972Polyconic projection, 1927 North American datum10,000-foot grid based on New Mexico coordinate system, cental zone1000-meterUniversal Transverse Mercator grid ticks, zone 13, shown in blueDashed land lines indicate approximate locationsWest boundaries of San Felipe Grant and Sandia Pueblo Grant adjacient to Rio Grandeomitted due to insufficient data
S. D. Connell: geologic mapping, compilation, Phanerozoic stratigraphy and regionalstructural interpretation refined from borehole data analyses, unit descriptions andcorrelations, and structural cross sections; geology depicted in areas of disturbance (afand daf) interpreted from aerial photography
D. J. McCraw M. M. Mansell, and G. E. Jones: digital cartographic production
35° 15'
3904
17' 30"
20'
35° 22' 30"
3905
3906
3907
3908
3910
3911
3902
3913
355 357 R. 4 E. JEMEZ CANYON DAM 2.7 MI.
35635'354 ALAMEDA 5 MI.ALBUQUERQUE 12 MI.
R. 3 E. R. 4 E. 359 360 361 362
A
D'
D
B
E'
E
A geologic map graphically displays information on the distribution, nature, orientation and age relationships ofrock and surficial units and the occurrence of structural features. These data are derived from geologic field mapping,compilation of published and unpublished work, analyses of borehole geophysics and well-cuttings, and photogeologicinterpretation. Locations of geologic unit contacts are not surveyed; therefore, the accuracy of contact locationsdepends on the scale of mapping and the interpretation of the geologist(s). Portions of the study area were mappedat scales larger than depicted on the geologic map; therefore, the user should be aware of significant variations inmap detail. Any enlargement of this map could cause misunderstanding in the detail of mapping and may result inerroneous interpretations. Site-specific conditions should be verified by detailed surface mapping or subsurfaceexploration.
This map has not been reviewed according to New Mexico Bureau of Mines and Mineral Resources standards.Revision of the map is likely because of the on-going nature of work in the region (Please note the date of lastmodification in the upper right of Plate I). The contents of this map and associated report should not be consideredfinal and complete until reviewed and published by the New Mexico Bureau of Mines and Mineral Resources. Theviews and conclusions contained in this document are those of the authors and should not be interpreted as necessarilyrepresenting the official policies, either or expressed or implied, of the State of New Mexico or the U.S. Government.
Mapping of these quadrangles was funded by matching-funds grants from the 1995 and 1997 STATEMAPcomponent of the National Cooperative Geologic Mapping Program coordinated by theU.S. Geological Survey and the New Mexico Bureau of Mines and Mineral Resources.
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
Sean D. Connell1
Bernalillo quadrangleNMBMMR OF-GM-16
May 1998
David J. McCrawMark M. Mansell
Glen E. JonesRebecca J. TitusDigital Cartography
Placitas quadrangleNMBMMR OF-GM-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
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
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
Plate I of III.17 February 2000 Revision
Tentative correlations of alluvial units in the study area, based upon stratigraphic relations,landscape-topographic position, degree of soil development and physical correlation of units.
This Study
QHa, QHao
Qrp, Qrp1-2, Qrpr
Qay
Qay2
Qrm
Qre
Qpm
Qpo
QTob, QTsp
Connell (1996)
Q9
Qfp9
Q8
Q7
Qoa2
Qoa1
Q6
Q5, Q4, Q3
Q2, QT1
Lambert (1968)
Qya
Qfa
Qya
Qya
Qm
Qe
Qop
Qop
Qu(?)s, Tm
COMMENTS TO MAP USERSPic
ha
(198
2)[1
:12,
000]
INDEX TO GEOLOGIC MAPPING
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°30' 106°22'30"35°22'30"
106°37'30"35°15'
106°30' 106°22'30"35°15'
TURQUOISEHILL
OF-DM–41
MADRID
OF-DM–49
OF-DM–48OF-DM–36
LEMITAR
ABIQUIU 1:100,000
SANJUAN
PUEBLO
LYDEN
SANTODOMINGO
PUEBLO SW
SANTODOMINGOPUEBLO
TETILLAPEAK
CAÑADA
COCHITIDAM
MONTOSOPEAK
HORCADORANCH
FRIJOLES
BLAND
AGUAFRIA
SETONVILLAGE
VALLETOLEDO
GUAJEMOUNTAIN
PUYEESPAÑOLA
WHITEROCK
LOS ALAMOS 1:100,000
GM–73
OF-DM–23
LosAlamos
Santa Fe
OF-DM–42
BERNALILLONW
CERROCONEJO
JEMEZPUEBLO
SANTAANA
PUEBLO
SANFELIPE
PUEBLO
SANFELIPE
PUEBLO NE
SANYSIDRO
LOMACRESTON
GILMAN PONDEROSABEAR
SPRINGSPEAK
REDONDOPEAK
JEMEZSPRINGS
SANMIGUEL
MOUNTAIN
PICTUREROCK
CHILI
RANCHODEL
CHAPARRALSEVEN
SPRINGS
VALLESAN
ANTONIO
GM–45
GM–34
GM–27
OF-DM–15OF-DM–26OF-DM–25
OF-DM–14
OF-DM–19 OF-DM–37OF-DM–45
OF-DM–40
COLLIERDRAW
OJITOSPRING
HOLYGHOSTSPRING
LAVENTANA
SANPABLO
OF-DM–18
GM–33
GM–28
GM–26
(SKY VILLAGE NE)
(SKY VILLAGE NW)
OF-DM–46
SANDIACREST
PLACITAS
BERNALILLO
LOMAMACHETE
ARROYODE LAS
CALABACILLAS
VOLCANORANCH
LA MESITANEGRA SE
LOSGRIEGOS
WINDMESA
ISLETA HUBBELLSPRING
HAGAN
SANDIAPARK
TIJERASSEDILLO
ESCABOSAMOUNT
WASHINGTON
SANFELIPEMESA
CAPTAINDAVIS
MOUNTAIN
SANPEDRO
EDGEWOOD
CHILILI
RIOPUERCO
LOSLUNAS
SETAJIQUE MILBOURN
RANCHDALIESBOSQUE
PEAK
DALIESNW
LA MESITANEGRA
BENAVIDEZRANCH
ESTANCIA
MORIARTYSOUTH
MORIARTYNORTH
KINGDRAW
BELENNW
TOME TOME NE TORREON EWINGBELEN MOUNTAINAIRNE
BELENSW
TURNPUNTA DE
AGUAMOUNTAINAIR
VEGUITAMANZANO
PEAKWILLARD
ALBUQUERQUEWEST
ALBUQUERQUEEAST
TOME SECOMANCHERANCH
(SKY VILLAGE SE)(SKY VILLAGE)
OF-DM–2
OF-DM–9
OF-DM–10 OF-DM–6 OF-DM–1 OF-DM–29
OF-DM–35
OF-DM–20OF-DM–4
OF-DM–3
OF-DM–8OF-DM–5OF-DM–13
OF-DM–21
OF-DM–28
SOCORRO 1:100,000
ALBUQUERQUE 1:100,000
GOLDEN
Alb
uq
uer
qu
eA
rea
ALAMEDA
CAPILLAPEAK
OF-DM–27
LOSLUNAS
OF-DM–16
OF-DM–17
OF-DM–24
LA JOYANW BLACK
BUTTEBECKER
ABEYTAS
SCHOLLE
RAYO HILLSCERROMONTOSO
BECKERSW
LA JOYASAN
ACACIASILVERCREEK
SANLORENZOSPRING
MESADEL
YESO
SIERRADE LACRUZ
SOCORROLOMA
DE LASCANAS
BUSTOSWELL
WATERCANYON
LADRON
OF-DM–34
OF-DM–38
OF-DM–43
OF-DM–47
TAOS SW
CARSONRANCHOSDE TAOS
TRESRITOS
PEÑASCOTRAMPAS
TAOSJUNCTION
VELARDE
JICARITAPEAKEL VALLETRUCHASCHIMAYO
LOSCORDOVAS
TAOS
TRESOREJAS
SHADYBROOK
PUEBLOPEAK
WHEELERPEAK
ARROYOSECO
ARROYOHONDO
CERRODE LOSTAOSES
GM–71
OF-DM–12 OF-DM–33
OF-DM–22
Taos
TAOS 1:100,000
McCLURERESERVOIR ROSILLA
PEAK
ASPENBASIN
COWLESTESUQUE
GLORIETA
SANTA FE
PECOS LOWERCOLONIAS
ELKMOUNTAIN
HONEYBOY
RANCH
SIERRAMOSCA
CUNDIYO TRUCHASPEAK
PECOSFALLS
OF-DM–31
OF-DM–32
OF-DM–7
SANTA FE 1:100,000
ROWEGALISTEOBULL
CANYONNORTH
SAN YSIDRO
OF-DM–11
OF-DM–30
WILDHORSEMESA
OJOHEDIONDA RENCONA
OF-DM–39
LAGUNAORTIZ
OF-DM–50
Connell[1:24,000]
Connell & Cather(Cenozoic)[1:24,000]
Menne (1989)[1:8000]
Karlstrom, Read, Ilg, Bauer,Johnson, Andronicus
(Proterozoic-Phanerozic)[1:12,000]
Connell (1998)
Connell & Cather (1995-8)
Karlstrom, et al. (1995-9)
Menne (1989)
Picha (1982)
Socorro
Grants
Taos
LasCruces
Deming
SANTA FE
Albuquerque
0 10 20 mi
0 10 30 km20
INDEX MAP OF NMBMMR’S
STATEMAP GEOLOGIC QUADRANGLES
02/00NMBMMR STATEMAPQuadrangles
Bernalillo &Placitas
68285
84
285
84
25
40
106°00'
35°00'
34°22'30"
34°30'
107°00'
106°30'
36°00'
36°30'3
285
35°30'
105° 30'35°15'
BELEN 1:100,000
VILLANUEVA 1:100,000
Location Map
37°
35°
33°
109° 107° 105° 103°
50
• •
• •
• •
• •
30
60
80
• •
B B'
• •
5040
30
45
75
56
Andalusite
Sillimanite
7
• • •
AM
40
72
B5
SHD2
ESA1
EFW
I I
I I I
IIII
35° 22' 30"
S A N D I A
M O U N T A I N S
RIO
GRAN
DE
106° 37' 30"
35°15'106° 37' 30"
35° 22' 30"106°22' 30"
35°15'106°22' 30"
CanjilonHill
Placitas
Bernalillo
Las Huertas Creek
Physiography of the Bernalillo - Placitas area based upon 10-m USGS DEM data.
25
25
o
44
85
165
EXPLANATION OF MAP SYMBOLS
Location of geologic cross section
Geologic contact—solid where exposed, dashed where approximately located; dotted where concealed .Geologic contact interpreted location within units af and daf
Approximate location of buried contact separating the ancestral Rio Grande axial-fluvial deposits (QTsa) andpiedmont deposits (QTsp) of the Upper Santa Fe Group on the Bernalillo quadrangle .
Approximate location of contacts separating the transitional (QTst) and piedmont (QTspcs and QTsps) depositsof the Upper Santa Fe Group on the Placitas quadrangle; dotted where concealed
Normal fault —Tic showing dip; solid where exposed, dashed where approximately located, dotted whereconcealed, queried where inferred; ball and bar on downthrown side, upthrown (U) and downthrown (D) sidesindicated where concealed and/or interpreted
Reverse fault—Tic showing dip; solid where exposed, dashed where approximately located, dotted whereconcealed; teeth on upthrown side; ball and bar added where reactivated as a Tertiary normal fault .Anticline—Trace of axial plane showing direction of plunge; dashed where approximately located, dotted whereconcealed, queried where inferred
Syncline—Trace of axial plane showing direction of plunge; dashed where approximately located, dotted whereconcealed, queried where inferred
Monocline with anticlinal bend—Trace of axial plane; short arrow on steeper bend; dashed where approximatelylocated, dotted where concealed, queried where inferred
Monocline with synclinal bend—Trace of axial plane; short arrow on steeper bend; dashed where approximatelylocated, dotted where concealed, queried where inferred
Breccia or gouge zones
Slickensides on fault
Strike and dip of bedding, horizontal bedding
Strike and dip of overturned bedding—ball indicates top of beds known from sedimentary structures .
Strike and dip of joint or fracture
Strike and dip of S1 foliation
Strike and dip of S2 foliation
Strike and dip of magmatic foliation in granite defined by alignment of megacrysts .
Magmatic foliation in granite defined by mafic enclaves
Trend and plunge of lineation—defined by elongate minerals or stretched grains
Metamorphic facies—Showing boundary between diagnostic mineral assemblages .
Metamorphic minerals locality— [1] sillimanite; [2] andalusite; [3] sillimanite and K-feldspar; [4] sillimanite -andalusite +/- K-feldspar and cordierite; [5] sillimanite - andalusite +/- cordierite; [6] chlorite - muscovite +/-biotite; [7] wollastonite; [8] calcite + quartz
Diatomite marker bed at top of Edith Formation (Qre)
Paleoflow direction—measured azimuths of imbricated clasts
Gravels with affinities to western basin-margin deposits
Gravels with affinities to ancestral Rio Grande fluvial facies
Gravels with affinities to eastern basin-margin deposits
Approximate extent of buried fluvial terrace risers of the ancestral Rio Grande (post Santa Fe Group)—Hachuredtowards fluvial terraces; Lomatas Negras Fm. (single hachured line), Edith Fm. (double hachured line), LosDuranes Fm. (triple hachured line), and Arenal Fm. (quadruple hachured line)
Aeromagnetic anomaly (interpreted from U. S. Geological Survey and Sial Geosciences, Inc., 1998) . .Mine or quarry, adit, shaft
Direction of landslide failure and surface movement
Basalt bed
Approximate boundary of tuff ring
Selected locality, Placitas (P), and Bernalillo (B) quadrangles
Water-supply well, included abbreviation
Exploratory or groundwater monitoring well, including abbreviation
Exploratory geotechnical boring, including abbreviation
Las Huertas geomorphic surface
Del Agua geomorphic surface