328000
106°52'30"W
329000
330000
106°50'0"W
331000
332000
333000
334000
106°47'30"W
335000
336000
337000
338000
106°45'0"W
339000
EXPLANATION OF MAP UNITS
3847000
3847000
34°45'0"N
calcicQToQTo
calcicQTo
Qae
5
Qedo
Qedo
Qed
calcicQTo
3846000
34°45'0"N
Qed
QTo
Qe/Qld
Albuquerque based largely on air photo interpretation and geomorphic position, and locally field checked.
Qed
daf
QTo
Qae
3846000
108135
Anthropogenic Deposits
af Artificial fill for highway and railroad grades.
QTo
Qedo
Rock colors are by comparison with Goddard et al. (1948). Mapping of surficial deposits on Llano de
calcicQTo
6
Surficial Deposits
Qed
calcicQTo
3845000
Qed
QTo
calcicQTo
3845000
Qed
Qed
3
calcicQTo
Qae Holocene and late Pleistocene sandy and pebbly alluvium and local eolian sand sheets in generally low
manmade barriers such as levees and irrigation and drainage ditches. Channel consists of pebbly sand in ripple
relief aprons and arroyo channels along valley margins. Sand is light brown (5YR 6/4) to grayish orange (10YR
and small dune bedforms, and larger bars. Laminated sand, silt, and clay form waning-flow deposits. Less than
7/4), unconsolidated, well sorted (eolian) to poorly sorted (alluvium), subangular to subrounded, and composed
5 m thick. Correlative to the Los Padillas formation of latest Pleistocene-Holocene age, together with Qfp
dominantly of quartz. Up to 8 m thick. Interfingers with and overlies Qfp.
af
Qed
calcicQTo
3844000
Qfw Historic floodway of the Rio Grande. Includes active channel and adjacent floodplain contained between
3844000
Qe/lda
calcicQTo
(Connell and Love, 2001).
Qae
Qgf Late Quaternary alluvial, eolian, and playa deposits along graben-floor drainages. Deposits are sand, silty
Qed
Qedo
QTo
Qed
110
irrigation ditches. Consist of sand, silt, and clay. Commonly disturbed by agricultural fields and housing
170
3843000
Qae
3843000
QTo
2
Qe/lda
calcicQTo
154 6
180
3842000
Arroyo Ojito Formation
Qed
Qe/QTo
Qfw
Qgf Qe/lda
34°42'30"N
3842000
QTo
Qe/lda
Qe/lda
Qae
QTo
Qed Late Holocene eolian deposits with recent dune form development. Deposits are light brown (5YR 6/4) to
QTo Late Tertiary and early Quaternary (?) basin fill of Santa Fe Group deposited by ancestral Rio Puerco and
grayish orange (10YR 7/4) to dark yellowish orange (10YR 6/6), unconsolidated, very fine to medium grained,
inter-channel eolian and pedogenic processes. Sediments consists of gravel, pebbly sand, sand, silt, and clay.
moderately well rounded to well rounded sand composed largely of quartz. Contains scattered pebbles. Forms
Qed
calcicQTo
Qed
Sand, fine sand, and silt beds are thin to thick bedded, light brown (5YR 5/6) to grayish orange (10YR 7/4) to
dunes up to 2m in height. In the northern half of the map area, unit contains local areas of sand sheets (unit Qe).
QTo
Qed
4
3841000
Qe/QTo
115
Qae
Qe/QTo
Qed
calcicQTo
Qe/lda
Qedo Holocene eolian deposits with older dune form development. Composition is similar to Qed. Commonly
Interchannel deposits commonly have laterally extensive soils characterized by rubification, clay
buried by or reworked into Qed. Equivalent to unit Qedi of Love (2000).
concentrations, and carbonate nodules. Gravel beds have trough crossbedding, are typically scoured into
underlying finer grained deposits, and generally weather into slopes where not cemented. Gravels are dominated
130
Qed
Qae
3840000
Qe/lda
by red and black chert, tan, brown, and red sandstone, and lesser amounts of Precambrian granite, multicolored
Qe Holocene eolian deposits with subdued or no dune forms. Dominantly sand sheets. Deposit consists of light
Precambrian quartzite, and intermediate intrusive and extrusive volcanic rocks. Pedernal chert and petrified
brown (5YR6/4 to 5YR 5/6), fine to very fine grained, rounded to subrounded sand composed largely of quartz.
127 3
5
148
QTo
Qed
bedded and light brown (5YR 6/4) to grayish orange (10YR 7/4) to moderate yellowish brown (10YR 5/4).
Qed129
calcicQTo
3840000
dark yellowish orange (10YR 6/6), and composed of rounded to subangular grains. Clay beds are thin to thick
124
3841000
QTo
Deposits generally similar to Qe. 1 to 2 m (?) thick.
af
5
Qe/lda
calcicQTo
Qag Late Quaternary sandy eolian (?) aprons downslope from faults on scarps cutting Llano de Albuquerque.
Qed
5
34°42'30"N
developments. Up to 30 m thick. Interfingers with and is overlain by Qae at valley margins. Correlative to the
Los Padillas formation of latest Pleistocene-Holocene age, together with Qfw (Connell and Love, 2001).
af
Qae
clay, and clay. Up to 2 m (?) thick
Qfp Historic floodplain of the Rio Grande between valley margins and artificial barriers such as levees and
Qe/Qld
wood are typically present in sparse amounts. The gravel clast population and paleocurrent indicators indicate
Locally pebbly due to bioturbation (?). Unit typically has one or more episodes of soil development beneath the
Qfp
derivation from generally southeast flowing streams coming off of the Colorado plateau. The presence of Grants
surface. Up to 2 m thick. Qe/ indicates where overlies subjacent unit.
7
obsidian (indicated by the hachured lines) indicates sediment derived in part from the ancestral Rio San Jose
Qae
135
130
3839000
3839000
150QTo
Qae
7
148
Qedo
3838000
Qedo
5
3838000
34°40'0"N
Qe/QTo
Qedo
Qfw
160
Qe/lda sand sheets on the Llano de Albuquerque geomorphic surface (described below).
drainage. At least 1500m thick based on oil test wells to east and west of the Belen quadrangle (as reported in
Qe/Qld sand sheets and subdued dunes on probable Los Duranes formation of middle Pleistocene age
Titus, 1963). Equivalent to units QTui of Love et al (1998) and TQsp of Love (2000). Top of unit is the Llano
(Connell and Love, 2001), which consists of up to 40 m of fining-upward sequences of gravel,
de Albuquerque (lda), a geomorphic surface of maximum basin aggradation that forms the mesa of the same
crossbedded sand, and parallel bedded sand, silt, and clay.
name in the western half of the quadrangle. The Llano de Albuquerque surface underlies units Qe/lda, Qed,
Qe/QTo discontinuous eolian mantle and local exposures of calcic soil at the top of the Arroyo Ojito
Qedo, and Qgf. In the Belen area, the Llano de Albuquerque surface is between 1.2 and 2.7 Ma, but is most
Formation (described below) on fault scarps on the Llano de Albuquerque; isolated exposures along I-25
likely older than 1.6 Ma. (see discussion in Love et al., 2001). Beneath the surface is a white (N9) to bluish
in the middle of the quadrangle are thin (≤ 1m ) eolian mantle on probable Arroyo Ojito Formation.
white (5B9/11), 2-3 m thick, stage III+ - V calcic soil (Machette, 1982; Birkeland, 1999), delineated by
34°40'0"N
northeast-trending hachures on the map where exposed, and on the cross section.
142
3837000
Qed
3837000
4
calcicQTo
Qe/QTo
MAP AND CROSS SECTION SYMBOLS
Qe/lda
Qag
Approximately located contact, queried where uncertain
Qae
3836000
Qedo
Qae
Qgf
Qe/lda
3836000
daf
where buried
120
130
3
Normal fault, ball and bar on downthrown side, dashed where approximately located, dotted
Bedding attitude (dip and dip direction)
Qae
Qgf
Horizontal bedding
5 165
3835000
3835000
Qe/lda
Qed
Paleocurrent direction, with type of indicator noted: t indicates axis of trough cross bed; i
indicates imbricated gravel. Ball is at measurement point
Qedo
Qgf
Qedo
Qag
calcicQTo
3834000
Qedo
3833000
Qedo
Water well with NM State Engineer Office W.A.T.E.R.S. database reference number
Qgf Qedo
Qe/lda
Qag
Qfw
Qe/lda QgfQag
3833000
34°37'30"N
328000
329000
106°52'30"W
330000
331000
332000
333000
106°50'0"W
Rio Puerco
Dalies
334000
335000
336000
106°47'30"W
337000
338000
Geologic Map of the Belen 7.5 - minute Quadrangle
Base from U.S.Geological Survey 1991, from photographs taken 1947 and field checked in 52.
Map edited in 1995
1983 North American datum, UTM projection -- zone 13N
1000- meter Universal Transverse Mercator grid, zone 13, shown in red
by
Geoffrey C. Rawling
Los Lunas
June 2003
Belen NW
Belen
Tome
Magnetic Declination
June, 2003
10º 10' East
At Map Center
1:24,000
0
Belen SW
Veguita
0.25
0.5
1
1.5
2
Turn
0
0.25
0.5
1
1.5
2
Kilometers
CONTOUR INTERVAL 20 FEET
COMMENTS TO MAP USERS
A geologic map displays information on the distribution, nature, orientation, and age relationships
of rock and deposits and the occurrence of structural features. Geologic and fault contacts are
irregular surfaces that form boundaries between different types or ages of units. Data depicted
on this geologic quadrangle map may be based on any of the following: reconnaissance field
geologic mapping, compilation of published and unpublished work, and photogeologic interpretation.
Locations of contacts are not surveyed, but are plotted by interpretation of the position of a given
contact onto a topographic base map; therefore, the accuracy of contact locations depends on the
scale of mapping and the interpretation of the geologist(s). Any enlargement of this map could cause
misunderstanding in the detail of mapping and may result in erroneous interpretations. Site-specific
conditions should be verified by detailed surface mapping or subsurface exploration. Topographic
and cultural changes associated with recent development may not be shown.
Cross sections are constructed based upon the interpretations of the author made from geologic
mapping, and available geophysical, and subsurface (drillhole) data. Cross-sections should be used as
an aid to understanding the general geologic framework of the map area, and not be the sole source
of information for use in locating or designing wells, buildings, roads, or other man-made structures.
The map has not been reviewed according to New Mexico Bureau of Geology and Mineral Resources
standards. The contents of the report and map should not be considered final and complete until
reviewed and published by the New Mexico Bureau of Geology and Mineral Resources. The views and
conclusions contained in this document are those of the authors and should not be interpreted as
necessarily representing the official policies, either expressed or implied, of the State of New Mexico, or
the U.S. Government.
Approximate northward extent of clasts of Grants obsidian, indicating influence of Rio San Jose
on gravel composition in QTo
Qe/lda
Qedo
Qed
Qed
34°37'30"N
QTo
Qed
QTo
Qgf
2
3834000
QgfQag
Qe/QTo
Qe/lda
Qedo
Qe/QTo
Qe/lda
QTo
Axis of elongate concretion. Ball is at measurement point.
219
Miles
DRAFT
NMBGMR OF-GM 00
NATIONAL GEODETIC VERTICAL DATUM OF 1929
This work was performed under the STATEMAP component of the USGS
National Cooperative Geologic Mapping Program. Funding for geological
Textand the New Mexico
mapping was provided by the U.S. Geological Survey
Bureau of Geology and Mineral Resources, a division of New Mexico Tech.
The New Mexico Office of the State Engineer is providing funding for the
compilation effort as well as the hydrologic investigation underway.
New Mexico Bureau of Geology
New Mexico Tech
801 Leroy Place
Socorro, NM 87801-4796
[505] 835-5420
http://geoinfo.nmt.edu
This and other maps are available in PDF format from:
http://geoinfo.nmt.edu/statemap
or contact:
NMBGMR Publications -- [505] 835-5410
NMBGMR Geologic Information Center -- [505] 835-5145
This draft geologic map was produced from scans of hand-drafted
originals from the author(s). It is being distributed in this form because
of the demand for current geologic mapping in this important area.
The final release of this map will be made following peer review and
redrafting in color using NMBGMR cartographic standards. The final
product will be made available on the internet as a PDF file and in a
GIS format.
339000
106°45'0"W
Line of cross section