0 5 3 b w ater-l vle ion c o nt urs a d ground-water-flow
TRANSCRIPT
Waste Water Treatement Plant
Madrid
Lamy
Cerrillos
La Cienega
Cieneguilla
Agua Fria
Santa Fe
Tesuque
Tesuque Pueblo
En Medio
El Dorado
Buckman
Santa Fe River
San Marcos Arroyo
Cienega Creek
Bonanza Creek
Rio Tesuque
Gallina A
rroyo
Arroyo Hondo
Arroyo Calab
asas
Alamo Creek
Galisteo Creek
Cañada Ancha
Rio G
rande
Arroyo de los Chamisos
Santa Fe River
Galisteo C
reek
NicholsReservoir
NambeReservoir
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105°55'W106°W106°5'W106°10'W
35°50
'N35°
45'N
35°40
'N35°
35'N
35°30
'N
0 1 2 3 4 5Miles
0 1 2 3 4 5Kilometers
Water-Level Elevation Contours and Ground-Water-Flow Conditions (2000 to 2005)for the Santa Fe Area,Southern Española Basin, New Mexico
Peggy S. JohnsonOctober 2009
Open File Report: 520
Santa Fe
Las Cruces
Albuquerque
Rio Ch a ma
Peco s R iv erCanad ian R i ver
Rio G
rand
e
Gila R iv er
S an Ju a n R i ver
New Mexico Bureau of Geology & Mineral Resources
New Mexico Tech801 Leroy Place
Socorro, NM 87801-4796(575) 835-5420 / www.geoinfo.nmt.edu
Cartography/GIS Support & Layout: Brigitte Felix
Water-level elevation contours100-foot, dashed where approximate, hashed for closed depression50-foot, hashed for closed depression
Ba se from U.S.Geological Survey 7.5-minute top ographic maps 1983 No rth American datum, Universal Tra nsverse Mercator Pro jection 10,000-meter UTM grid tics, zone 13, sh own in pink
Scale 1:60,000
La Cienega
Santa Fe
Galisteo Lamy
Tesuque
Buckman
Santa Fe
En Medio
El Dorado
Cerrillos
Agua Fria
La Cienega
Cieneguilla
TesuquePueblo
Boundary of ground water unit
Horizontal ground water flow direction
Depth to ground water (feet below land surface)
20 - 100100 - 300300 - 500>500
<20 feet, delineates discharge zone
Reversal of natural ground-water-flow direction
WellsPiezometers
St. Michaels, SF-1Buckman, SF-2ArcheryBuckman, SF-5Santa Fe River/CountySanta Fe FairgroundsJailLas CampanasCuyamungueOWAOWC
Supply well
Ephemeral stream
ABCDEFGHIJKPerennial stream
Vertically upward hydraulic gradient in domestic well pair
Vertically downward hydraulic gradient in domestic well pair
-0.016-0.02-0.04
<0.010.01 - 0.10>0.10
Ground-Water-Flow Conditions
Vertically downward hydraulic gradient in piezometer nest
Vertically upward hydraulic gradient in piezometer nest
LegendSpring with water-level elevation6551Well in Tesuque Fm (Tt) and water-level elevation6551
Hydrogeologic unit, of well completionAncha Formation (QTa)Espinosa Formation (Te)Galisteo Formation (Tg)Mesozoic and Paleozoic, undividedEmbudo Formation (p e)_
TextCOMMENTS TO MAP USERS The purpose of this map is to illustrate important aspects of regional ground water flow. Ground-water-elevation data depicted herein were calculated primarily from depth-to-water measurements taken between 2003 and 2005 by the New Mexico Bureau of Geology and Mineral Resources (NMBGMR) at New Mexico Tech, the New Mexico Office of the State Engineer (NMOSE), and the U.S. Geological Survey (USGS). Some data contained herein were also compiled from existing sources including the New Mexico Environment Department (NMED), the City and County of Santa Fe, private consultants and drilling companies, and records of the Eldorado Water and Sanitation District (EWSD). While utmost care was taken to ensure data quality, the authors can not verify the accuracy of measurements taken by third parties. Land surface elevations used to calculate ground-water elevation values originated from the 10-m digital elevation model (DEM). Ground water levels in the vicinity of pumping wells are erratic and fluctuate significantly over time and natural variations also occur. The user should be aware that conditions change and information contained on this map may not reflect actual or current conditions. Site- and time-specific conditions should be verified by the user. All additional information contained on this map, other than ground-water-elevation data, are interpretations of the author. The ground-water-elevation contours were interpolated from point data using an inverse distance method (IDW) in ARC INFO 9.3, followed by manual adjustment at study area boundaries and well fields. The ground-water elevation contours were used to further interpret or generate ground-water-flow direction, the boundaries of ground-water flow units, and directions of vertical hydraulic-gradient in multilevel piezometers, piezometer nests, and domestic well pairs. This map is subject to revision and has not been reviewed according to NMBGMR editorial standards.