New
Mexico
Bureauof Mines and Mineral
Resources
Open-file Report 130
WATER-LEVEL DATA COMPILED
FOR
HYDROGEOLOGIC STUDY OF ANIMAS VALLEY,
HIDALGO COUNTY, NEW MEXICO
Keith M. O'Brien
Hydrologi~st
.'' and
William J. Stone
Hydrogeologist
June ~1981
CONTENTS
.................................................
..............................
....................................
.........................................
Introduction
Problem and purpose of study
Purpose of this report
The
Animas
Valley
Sources of data...........................................
. .
Well-numbering
system
Page
1
1
1
3
4
5
.....................................
Water-level configuration and ground-water movement
..........6
Pre-irrigation (1913)
...................................... 8
Modern (1976
Discussion
through
1981)
................................
9
11
...............................................
Water-level
Decline
.........................................
April. 1948 through January. 1955
........................
1913 to 1976
.............................................
References
12
12
14
............................................
Cited
15
......17
Table 1 Well records presented by Schwennesen (1918)
Well records presented by Reeder (1957)
Table 2
Table 3 Well records compiled from the files
of the
Deming
office
of
the
State
Engineer
..
...........32
...............55
Fig
Fig
.1
.2
Plate
Plate
Plate
Plate
............................. 2
.......13
Location of study area
Water-level decline April 1948-January 1955
............in
1 Water-level contour map in 1913
2
Water-level contour map 1976-1981
3 Selected water-level profiles
4 Water-level decline 1913-1977
..........in
..............in
..............in
pocket
pocket
pocket
pocket
1
INTRODUCTION
The
Animas
Valley
is a' closed
basin
located
Hidalgo County, southwest New Mexico (fig.
1).
approximately 8 0 mi
long,1yi~g:between
in
western
The valley is
the Mexican border and
US highway 70. The width of the valley varies 6from
to 12 mi
along its length.
Problem
and
The
purpose
central
of
study
part
of
the
valley
is
an
important
area
for
irrigated agriculture (Lansford and others, 1980) and is the
site
of
the
Lightning
Dock
Known
Geothermal
Resource
Area
(fig.
1). Although an understanding of the hydrogeology of the valley
is important to both
of
the
entire
area's
area
the
agricultural
geothermal
have
not
economy
resources,
been
studied
the
in
and
water
detail
the
development
resources
since
of
1957
the
(Reeder,
1957). The Animas Valley is also an excellent example of a closed
alluvial basin. For these reasons the present study was initiated
as
part
of
the
U.S. Geological
Survey
Water-Resource
Division's
Southwest Alluvial Basin Regional Aquifer System Analysis. The
work is being
funded
under
contract
with U.S.
the Geological
Survey
(WRD), Albuquerque.
Purpose
of
Basic
this
data
report
compiled
for
the
Animas
Valley
study
are
being
released in a series of Bureau Open-file reports
so that the
information
compiled
may
be available
for
use
prior
to
the
completion of the final project report. This report (OF-130)
gives the basic water-level data compiled. Bureau OF-131 will
2
.
.
.
....
.. .
.
. .
. .
.
.
.
..
.....
. .
. .
.
..
....
..
.
.
..
.
.
.
..
.
I
:
,
' ..
r
. .
.
.
. .
..
Figure 1.
Location of study area
,
,
3
OF-132 w i l l g i v e t h e b a s i c
give the basic water-quality data,
dataobtained
from t h e d r i l l i n g and t e s t i n g program, OF-133 w i l l
givethehydrologic
model, and OF-134 w i l l b e t h e f i n a l r e p o r t o n
the project.
The Animas V a l l e y
The Animas V a l l e y l i e s i n t h e Mexican Highlands section of
t h e Basin and Range p h y s i o g r a p h i cp r o v i n c e .
t h e west by t h e P e l o n c i l l o Mountainsand
Mountainsand
t h e PyramidMountains
boundary i s markedby
of US 7 0 .
I t i s boundedon
on t h e east by t h e Animas
( f i g . 1 ) . The n o r t h e r n
an extensive eolian dune field just south
The southernboundary
l i e s across t h e i n t e r n a t i o n a l
boundary i n Mexico.
The climate of t h e Animas V a l l e y i s a r i d t o s e m i a r i d (Cox,
1 9 7 3 ) .P r e c i p i t a t i o ng e n e r a l l ya v e r a g e s
and 2 2 i n c h e si nt h eh i g h e rm o u n t a i n s .
( 1 9 3 1 - 1 9 6 0 ) ,p r e c i p i t a t i o n
andexceeds
1 0 i n c h e si nt h ev a l l e y
Basedon
30 y e a r so fd a t a
a t Lordsburg f a l l s below 5 . 7 1 i n c h e s
13.84 i n c h e s one y e a r i n t e n .R a i n f a l l
is greatest
i n l a t e summer and e a r l y f a l l : . h a l f o f t h e a v e r a g e a n n u a l
p r e c i p i t a t i o no c c u r si nJ u l yt h r o u g hS e p t e m b e r .
Animas Creek,
which rises i n t h e s o u t h e r n P e l o n c i l l o
Mountainsandflows
northerly t o a point just south of the
town of Animas, i s t h e o n l y
p e r e n n i a l stream i n t h e s t u d y
and east v a l l e y m a r g i n s
area.
A l l u v i a lf a n sa l o n gt h e
west
are a source of ephemeral flows.
The P e l o n c i l l o M o u n t a i n s c o n s i s t : i o f v a r i o u s s e d i m e n t a r y
and
strata,
volcanicrocks.Approximately5,000
f.t: o fP a l e o z o i c
approximately 2,500 f t ofCretaceous
s t r a t a , andanundetermined
thicknessofCretaceous
and T e r t i a r y v o l c a n i c r o c k s o c c u r i n t h e
4
area north of the ghost town of Steins and south of Cowboy
Pass (Gillerman, 1958).
The
These
Animas
include
Mountains
consist
approximately
mainly
of
sedimentary
rocks.
3,500
ft of Paleozoic limestone,
dolostone, sandstone, and shale and 10,000-15,000
ft of Cretaceous
.
sandstone and shale (Soule, 1972)
The
Pyramid
Mountains
consist
of a
variety
of
volcanic
and plutonic igneous rocks (Flege, 1959). The northern part
consists of basalt intruded by granodiorite. The central is
part
characterized
by
pyroclastic
volcanics
and
lesser
amounts
of
rhyolite, rhyolitic welded tuff, and basalt. The southern part
is
dominated
by
andesite
with
lesser
amounts
of
rhyolite
and
bas
The valley was the site of two Quaternary lakes: Lake
Cloverdale in the south (Schwennesen, 1918) and Lake Animas in the
north (Fleischhauer and Stone, 1981). The valley is filled with
bolson and lacustrine deposits
of undetermined
Geologic
maps
and
geophysical
surveys
thickness.
confirm
the
basin-and-
range structure of the area. The valley
is a graben and the
bounding ranges are horsts. Complex folding and faulting
is
apparent
within
intervening
the
basin
as
mountain
blocks
and
presumably
occurs
in
th
well.
Sources of data
Water-level
data
used
in this
report
were
compiled
from
published sources and the files of the Deming office of the New
Mexico State Engineer. Published sources include Schwennesen
.
(1918) and Reeder (1957)
4
System of numbering wells in New Mexico.
WELL-NUMBERINGSYSTEM
The system of numbering wells in this report is
that used generally by the Geological Survey
throughout the State. This system is based on the
common subdivisidns in sectionized land. The well
number, in addition to designating the well, locates
its position to the nearest IO-acre tract in the land
net. The number is divided into four segments by
periods. In this areathe first segment denotes the
township south of the New Mexicobase line;the
seconddenotes therange west of the New Mexico
principal meridian; and the~thirddenotes the section.
The fourth segment of the number, which consists of three digits, locates the well in a particular
10-acre tract. For this purpose, the section is divided
into four quarters, numbered 1, 2, 3, and 4, in the
following order: northwest, northeast, southwest, and
southeast. The first digit of the fourth segment gives
the quarter section, which is atract of 160 acres.
Similarly, the quarter section is divided into four
40-acre tracts numbered in the samemanner,and
the second digit denotes the 40-acre tract Finally,
the 40-acre tract is divided into four IO-acre tracts,
and the third digit denotes the IO-acre tract Thus,
well 25.20.24.344 in Hidalgo County is in &e SEXSystem. of
SEl/SWl/, sec. 24, T. 25 S., R. 20 W. If a well cannot be located accurately to a IO-acre tract, a zero
is used as the third digit, and if it cannot be located
accurately to a 40-acre tract, zeros are used for both
the secund andthird digits. If the well cannot be
located more closely thanthe
section, thefourth
segment of the well number is omitted. Whenit
becomespossible to locate more accurately a well
in,whose number zeros have been used, the proper
digit or digits aresubstituted for the zeros. Letters
(a, b, c, etc.) are added to.. the last. segment to
designate the second, third,fourth,and
succeeding
wells in the same 10-acre tract.
numbering wellsin New Mexico (adapted from Reeder,
1957)
6
WATER-LEVEL
CONFIGURATION
AND
GROUND-WATER
MOVEMENT
The records of wells tabulated in Schwennesen's (1918) paper
are incomplete. They do not include the elevation of the land
surface at the wells. Furthermore, well locations are specified
to a quarter-section. Since these important pieces of information
were
the
either
missing
following
Wells
or
deficient,
well
elevations
were
based
on
criteria.
located
to
the
nearest
quarter-section
were
plotted
at
the center of that quarter-section. Wells located to the nearest
section
were
assigned
to
.-. .. ....-. .
center
: ~ . ~ of
~ ~ ~ ~ e ~ . = . s e ':,.::.~ ."~ ~ ~ ~ ; . ' : .
the
'
based on-thewell location map in the Schwennesen paper. The
assignment of an elevation a
towell
withina quarter-section
depended on the amount of relief
in the quarter-section. If there
was less than20 ft of relief ina quarter-section then the assigned
elevation
corresponded
to
the
nearest
contour
line
or
spot
elevatio
If the well location was equidistant beticeen either two contour
lines
ora contour
line
and
a spot
elevation
then
the
mean
value
of these known elevations was used.
In cases where the relief in
a quarter-section exceeded twenty feet, the well location was
refined by reference to Schwennesen's well location map and the
well was assigned an elevation following the criteria stated above.
If the relief in
a quarter-section exceeded 50 ft,
elevation
The
was
well
not
thena well
assigned.
records
in
Reeder's
report
included
both
an
elevation
and an accurate well location. The tabulated elevation at well
locations
was
checked
topographic quadrangles.
by
utilizing
well
location
information
In many cases, the elevationas!
and
7
determined by aneroid barometer was found to be incorrect. These
elevations
were
corrected
by
assigning
an
elevation
which
corresponded to the nearest contour line or spot elevation.
In
cases
where
the
well
combination
of
known
elevations
was
used.
The
in
records
Deming
was
elevations,
of
wells
provided
elevations.
location
at
detailed
equidistant
the
the
well
between
mean
value-of the
New
Mexico
locations
known
State
but
any
Engineer's
inaccurate
Off
well
In accordance with the format adopted for assigning
well elevations, the cantour line or spot~.elevat.ion
closest
to the
. .
well location was utilized. If the well location was equidistant
from
points
of
known
elevation
then
the
mean
value
of
the
known
number
elevations was used.
The
of
above-outlined
water-level
methods
elevation
data
were
utilized
points
from
to
generate
a
which
contours
could
be drawn to define the water-level configuration. WaDer-level
contour
maps
were
constructed
from
Schwenneson's
well
records,
which were collected in 1913, and from the recent well records of
the
State
Engineer's
Office
in
Deminq,
which
included
water-level
information for the years 1976-1981. The utilization of waterlevel
to
data
from
investigate
these
the
two
different
water-level
time
periods
configurations
at
provided
two
a
means
different
time periods. This is an important consideration because the
development
of
large-scale
irrigation
occurred
during
this
time
period. Thus, the inspection of the 1913 water-level configuration
yields
and
information
analysis
of
on
the
ground-water
1976-1981
flow
in
water-level
pre-irrigation
configuration
times
provides
i n f o r m a t i o n on t h e changes of g r o u n d - w a t e r f l o w s i n c e t h e
development of large-scale irrigation.
P r e - I r r i g a t i o n( 1 9 1 3 )
1913 i s shown on
The c o n f i g u r a t i o n o f t h e w a t e r l e v e l i n
P l a t e 1.
circles and t h e
The well l o c a t i o n s a r e p l o t t e d a s
circles.
w a t e r - l e v e le l e v a t i o n sa r en o t e dn e x tt ot h e
representing lines
Contours
of e q u a l w a t e r - l e v e l e l e v a t i o n , h a v e b e e n
drawn by i n t e r p o l a t i n g where necessary between water-level
elevation data points.
The l a c k of d a t ap o i n t sa l o n gt h e
nmU&&i,n.':frfOnt
.~
.
..
'~.:
.
,.
necessitates dashing of the contour lines near the valley
margins.
The d a s h e dc o n t o u rl i n e sf o l l o wp a t h s
to represent the extension
which a r e b e l i e v e d
of known w a t e r - l e v e l e l e v a t i o n c o n t o u r
lines.
S i n c e t h e movement of ground water i s p e r p e n d i c u l a r t o
of ground-water
water-levelelevationcontourlines,thedirection
movement canbedetermined
contour maps.
by i n s p e c t i n g w a t e r - l e v e l e l e v a t i o n
P l a t e 1 i n d i c a t e st h ed i r e c t i o n
of ground-water
movement t o b e n o r t h w a r d b e g i n n i n g a t t h e g r o u n d - w a t e r d i v i d e
i n t h e v i c i n i t y of a well
between t h e Animas and San Luis Valleys
locatedinthe
SW%, Sec. 2 7 , T. 33 S . , R. 2 0 W..(see P l a t e 3,
p r o f i l e A-R'j.
The n o r t h w a r dd i r e c t i o n
c o n t i n u e st ot h en o r t h e r nq u a r t e ro f
of ground-water movement
T.
28 S . ,
i s anabruptdropinthewater-levelelevation
A-A').
R.
(see P l a t e 3, p r o f i l e
The s h a r pd e c r e a s ei nw a t e r - l e v e le l e v a t i o n s
in this region
i s caused by t h e p r e s e n c e
S o u t ho ft h en o r t h e r nq u a r t e ro f
T.
1 9 W. where t h e r e
whichoccurs
of a perchedwaterzone.
28 S . ,
R.
1 9 W. wells are
9
completed
in
a
perched
water-bearing
zone
formed
by
recent
stream alluvium. North of the northern quarter of T. S.,
28 R.
19 W. wells
are'completedin
a
water-bearing
zone
that
defines
the ground-water system of the valley. The transition from the
shallow
perched
water
system
to
the
valley
ground-water
system
explains this abrupt dropin water-level elevations. The
existence
ofthe.valley ground-water
systemin the
Upper
Animas
Valley (south of T. 28S., R. 19 W.) below the perched groundwater
system
The
T. 28.
is
valley
S..,
T. 25 S.
suspected
.but
ground-water
remains
.system
unconfirmed.
moves
northwestward
from
R. 19 W. through the town of Animas to the middle
of
The absence of data points in the vicinity of the
Animas/Playas
Valley
contact
prohibits
the
determination
of
the
direction of ground-water flow
in that region. The directionof
ground-water
movement
changes
from
northwestward
to
northward
in
T. 25 S. and continues in that direction to the Gila River
drainage system. In T. 24 S., the contour lines are deflected
to
an
water
orientation
moving
from
paralleling
the
the
mountains
valley
to
margins
recharge
indicating
the
valley
ground
ground-
water system. At the connection of Lordsburg and Animas Valleys
in T. 22 S., there is a slight deflection of the 4,000-foot
contour
Valley
line
into
suggesting
Animas
ground-water
movement
from
Lordsburg
Valley.
Modern (1976 through 1981)
The
water-level
configurakion
defined
by
water-level
-.
~~.
~
data points from the modern period (1976-1981) is on
shown
Plate 2.
There are no data points south
of T. 29 S.
It is
~.
elevation
10
assumed t h a t t h e p e r c h e d g r o u n d - w a t e r s y s t e m r e m a i n s
r e l a t i v e l y unchangedfrom
T.
33 S.,
R.
Water-level e l e v a t i o n d a t a p o i n t s i n
1 9 W.
i n d i c a t e a northwardground-water
D a t ap o i n t sn o r t ho ft h em i d d l eo f
water-Levelelevationsderived
system.
28 S. correspond t o
from t h e ' v a l l e y ground-water
28 S . t o T. 27 S . i s northward.
between Animas and P l a y a sV a l l e y s
movement from t h em i d d l e
A t theground-waterdivide
i n T. 2 1 S . , R. 1%
W.,
of groundwater
water-levelcontoursreflectaninput
Animas Valley.
29 S. and T. 28 S.
3 , p r o f i l e B-B').
T.
The d i r e c t i o no fg r o u n d - w a t e r
P l a y a st ot h e
T.
R.
movement and show t h e e x i s t e n c e
two ground-watersystems(Plate
o ft h e
of T.
20 W. t o T. 28 S . ,
the
from t h e
However, t h es p a r s e n e s so fd a t a
points in this region necessitates further investigation of the
area before
a d e f i n i t i v e ground-water flow direction can be
determined.
The d i r e c t i o n of ground-waterflowfrom
of T.
25 S. i s northward.
valleymarginsbetween
water flowfrom
24 S . ,
21 S. tothemiddle
The w a t e r - l e v e lc o n t o u r sp a r a l l e lt h e
2 1 S . and T.
25 S . i n d i c a t i n g ground-
the c e n t e r
the mountains on the valley margin to
o ft h ev a l l e y( P l a t e
T.
T.
T.
3 , p r o f i l e s D-D'
and E - E ' ) .
I n T. 2 5 S. and
t h e r e i s anareaofperchedshallowgroundwater
3, p r o f i l e C-C').
watersystem
From t h em i d d l e
of 25 S . ,
t h ev a l l e y
moves northward t o t h e G i l a R i v e r d r a i n a g e .
northern part of the
Animas Valley has
few d a t a p o i n t s
(Plate
groundThe
and needs
b e t t e r d e f i n i t i o n of t h e g r o u n d - w a t e r f l o w d i r e c t i o n .
An unpublished 1955 water-level contour
water-level c o n f i g u r a t i o n of t h en o r t h e r n
map d e f i n e s t h e
Animas Valley.This
11
water-level
contour
map
defines
direction from T. 23 S. to T. 22
ground-water
In T. 22
S.
S.,
flow
in
a
northerly
where Lordsburg
and Animas Valleys join, the ground-water flow direction shifts
northwestward to the Gila River drainage. Preliminary water-level
data gathered in
northwesterly
1981and
shownon
ground-water
flow
Plate
in
the
2
also
indicate
proximity
of
a
the
joining
of Animas and Lordsburg valleys. On the basis of this data,
it
appears
into
that
Animas
there
is ground-water
movement
from
Lordsburg
Valley
Valley.
Discussion
Comparison
of
the
two
water-level
configuration
maps
provides
the following observation. Beginning in
T. 27 S. and extending
to T. 24 S., all water-level contour lines have been shifted to
the
southon the
1976
through
1981
water-level
map
relative
to
their positionson the 1913 water-level map. The 4,125-ft and
4,150-ft
water-level
contours
have
moved
from
their
original
positions in the middleof T. 24 S. to the northern and middle
parts of T. 26 S.
The extent to which these two contours have
been shifted to the south reflects the dewatering'effects of
ground-water
pumpageon the
valley
ground-water
system.
12
WATER-LEVEL
DECLINE
Prior to 1948, there was not a large irrigated area in the
Animas Valley utilizing ground-water. However, beginning with
the period from 1948 to 1955, there was a tenfold increase in the
amount
of
irrigated
acreage
utilizing
ground-water
for
irrigation.
Since 1955, the number of irrigated acres has remained relatively
constant. The result of the artificial discharge of water from
the
Animas
Valley
ground-water
system
through
the
of use
wellsis
a decline inthe water level. The decline occurs because the
amount
of
water
withdrawn
by wells
exceeds
the
amount
of
water
recharged to the ground-water system. The decline of the water
level
can
be
shown
by
water-level
decline
maps.
April, 1948 through January, 1955
In 1948,
Subsequently,
most
the
of
the
Animas
ground-water
Valley
system
of
became
the
a
declared
valley
has
basin.
been
closely monitored. A report by Reeder
.(1957) compiled the decline
of the water level between April, 1948 and January, 1955. (f5g;
The declineof the water level coincides with the area under
2).
irrigation. The center of heaviest pumpage coincides with the
center of greatest water-level decline and is located in sec. 35,
T. 25 S.,
From
the
R. 20 W.
center
The greatest water-level decline
is 29.71ft.
of
the
greatest
water-level
decline
water
levels
decrease outward and in an elongated north-south fashion. The
water-level
declined
more
thanft5over an area
extending from the southern part T.of27
24
S.
1955
S.
of
to the
120
mi'
middle
of
T.
Hence, the use of ground water for irrigation from 1948 to
caused
the
water
level
in the
Animas
Valley
to
decline.
13
y R 21 W
\
Figure 2
Water-level
decline
April
1948-January
(adaptedfrom Reeder (1957))
1955
14
1913 to 1976
Comparison of the depth to water
in-1913 and in 1976 at
similar locations yields, in most cases, a water-level decline.
In order
to
construct
a
water-level
decline
map
for
this
time
interval, the 1976 water-level data points were superimposed
on
the 1913 waterilevel data points. The data points for the two
years did not coincide. A set of criteria was adopted in order to
obtain a water level. comparison for the two years. Water-level data
points
were
compared
if
they
were
w'ithin
two
miles
of
each
other
and if their well elevations did not differ by more than 20:.ft.,
These
criteria
". .
. ,.
provided
.
.enough
da'ta
.points'~for
of a fairly definltive water-level dec1ine~'map.:.
The
water
level
declined
over
4).
of the central Animas Valley (Plate
decline,
which
happens
to
coincide
the
.~
~
-
-the-constructi
~
~.
~L
~
entire
irrigated
acreage
The center of greatest
with
the
center
ground-water pumpage is located in sec. 35, T. 25S.,
of
greatest
R. 20 W.
The maximum amount of water-level decline 84
is ft. The water
level declined at least 20
ft over an area extending from the
southern part of T. 27
S. to the northern part of 24
T. S.
In the
Lordsburg
Valley,
water-level
decline
was
centered
on sec. 34, T. 22S., R. 18 W. .(Plate 4). The maximum amounto f
water-level decline was 98 ft. The water-level decline contours
are elongated along the length of the valley NW-SE
in aorientation.
There
has
been
at
leastft60
of
southwest part of T. 22
S.,
water-level
R. 18 W.
declinein
the
15
REFERENCES
Silberman, M.L.,
Armstrong, A . K . ,
New Mexico:
Mountains,HidalgoCounty,
Cox, D.N.,
U.S.
Hoggatt, W.C.,
1 9 7 8 , Geology of c e n t r a l P e l o n c i l l o
and Carten, R.B.,
of Minesand
Todd, V . R . ,
New Mexico Bureau
MineralResources,Circular158,
1973, S o i l s u r v e y
18 p.
New Mexico:
of HidalgoCounty,
Dept. of A g r i c u l t u r e , S o i l C o n s e r v a t i o nS e r v i c e
Forest Service,
i n c o o p e r a t i o n w i t h New Mexico A g r i c u l t u r a l
E x p e r i m e n tS t a t i o n ,
Drewes, M.,
90 p.
and Thorman, C.M.,
1 9 8 0 , Geologic Map of t h eC o t t o n
P a r t of t h e Vanar Quadrangle,
City Quadrangle and the Adjacent
N e w Mexico:
HidalgoCounty,
and Thorman, C . H . ,
Map 1 - 1 2 2 1 ,
1980,Geologic
Quadrangle and the Adjacent
HidalgoCounty,
GeologicalSurvey
U.S.
M i s c e l l a n e o u sI n v e s t i g a t i o n s
Drewes, H . ,
and
1:24,000.
Map of t h eS t e i n s
~
P a r t of t h e Vanar Quadrangle,
New Mexico:
GeologicalSurvey
U.S.
M i s c e l l a n e o u s I n v e s t i g a t i o n s 'Map . I - 1 2 2 0 , .1:24,OO~q:.-:,,..,...
F l e i s c h h a u e r , H.L.,
Jr. andStone,
W.J.,
of Lake Animas, HidalgoCounty,
of Minesand
Flege, R.F.,
New Mexico:
New Mexico Bureau
Mineral Resources, C i r c u l a r 1 7 4 ( i n p r e s s ) .
1959,Geology
N e w Mexico:
1 9 8 1 , Quaternarygeology
of Lordsburgquadrangle,HidalgoCounty,
New Mexico Bureau of Minesand
MineralResources,
B u l l e t i n 6 2 , 36 p.
Gillerman, E l l i o t , 1958,Geology
Mountains,HidalgoCounty,
Arizona:
of t h e c e n t r a l P e l o n c i l l o
New Mexico, andCochiseCounty,
N e w Mexico Bureau of Minesand
B u l l e t i n 57, 152p.
MineralResources,
-
16
Lansford, R.R.,
Sorefisen, E.F.,
Loslebon, L . ,
Creel, B . J . ,
Gollehon, N.R.,
Fisburn, M.,
1980, Sources of
West, F.G.,
i r r i g a t i o n water and i r r i g a t e d and d r y c r o p l a n d a c r e a g e s
i n New Mexico,bycounty,
Experiment S t a t i o n , ResearchReport
Maker, H . J . ,
Cox, D . N . ,
New Mexico A g r i c u l t u r a l
1974-1979:
andAnderson,
4 2 2 , 39 p.
J.U.,
1 9 7 0 , S o i la s s o c i a t i o n s
and l a n d c l a s s i f i c a t i o n f o r i r r i g a t i o n , H i d a l g o
County: New
Mexico AgriculturalExperimentStation,ResearchReport177,
29 p.
Reeder, H.O.,
1957, Ground water i n Animas Valley,HidalgoCounty,
New Mexico:
New Mexico S t a t eE n g i n e e r ' sO f f i c e ,T e c h n i c a l
Report 11, 1 0 1 p .
Schwennesen, A . T . ,
1918, Ground water i n t h e
H a c h i t a , andSan
L u i sB a s i n s ,
Survey,Water-SupplyPaper
N e w Mexico:
Soule, J . M . ,
and g e o t h e r m a ll e a s i n g
Dock KGRA, Animas V a l l e y , New Mexico:
New Mexico G e o l o g i c a l S o c i e t y ,
conference,p.
U.S. Geological
152 p .
422,
Smith,Christian,1978,Geophysics,geology,
s t a t u s oftheLightning
Animas, P l a y a s ,
Guidebook 29th f i e l d
343-348
1 9 7 2 , S t r u c t u r a lg e o l o g y
Mountains, 'Hidalgo County,
of n o r t h e r n p a r t
hew Mexico: \,New Mexico Bureau
1 5 p.
ofMinesandMineralResources,Circular125,
S t o n e , W.J.,
and M i z e l l , 1 9 7 7 , Geothermalresourcesof
a survey of work t o d a t e :
and D r e w e s , H . ,
and
73,. 117.p.
1978,Geologic
andLordsburgQuadrangles,HidalgoCounty,
Map of t h e Gary
New Mexico: U.S.
Geological Survey Miscellaneous Investig-ations
1:24,000
New Mexico--
New Mexico BureauofMines
MineralResources,Open-fileReport
Thorman, C .H.,
of Animas
Map 1-1151;
Table 1
- Well
records presented by Schwennesen
(1918). Elevation of wells
as determined in
this study are given in supplement at end. Asterisk in table indicates water
analyzed; asterisk in supplement indicates
20-50 ft. of relief %insection and
elevation questionable; blank indicates
>50 ft. of relief in
% section and elevation
could not be determined; slash indicates well not in Animas valley.
-I_
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Elevation
Well Number
Elevation
1
/
/
/
/
/
/
/
23
4190
24
4200*
25
4210*
26
4210*
27
4210*
28
4190
29
4190
30
4200*
9
/
/
31
4200*
10
/
32
4190*
11
4270
33
4190
12
4263
34
4200
13
4253
35
4205
14
4234*
36
4237
15
4280
37
4207
16
4265*
38
4165
17
4289*
39
18
4230
40
19
4250*
41
20
4219
42
4158
21
4200*
43
4185
22 ( w e s t well)
4210
44
4157
( e a s t well)
4210
45
4153
(well No. 3)
4210
46
4150
2
3
4
5
6
7
8
'
4190*
'
4195
\
Well N u m b e r
Elevation
,
Well N u m b e r
Elevation
73
4162
47
4160
48
4160
74
4160
49
4160
75
4165
50
4180*
76
4168
51
4 mo*
77
4180
52
4180*
78
4178
53
4180*
79
4184
54
4210
80
4187
55
4150
81
4210*
56
4159
82
4220*
57
4159
83e
4196
58
4154
83f
4196
59
4157
84
4196
60
4156
85
4203
61
4155
86
4203
62
4155
87
4212
63
4157
88
64
4157
89
65
4161
90
4289
66
4161
91
4250*
67
4162
92
4250
,
'
.
4232
'
4255
68
4167
93
4260
69
4172
94
4280*
70
4166
95
4281*
71
4166
96
4330
72
4166
97
lu
m
Well Number
Elevation
Well Number
Elevation
98
4380
123
4450*
99
4390
124
4565
100
4380
125 '
4565
101
4400
126
4570
102
4407
127
4570
103
4420
128
4570
104
4437
129
4565
105
4470
130
4565
106
4300*
131
107
4340*
132
4580
108
4430
133
4580
109
4430
134
4585
110
4470
135
4600*
111
4480
136
4600*
112
4487
137
4590
113
4494
138
4600
114
45259
139
4612
115
4525*
140
4612
116
4525*
141
4612
117
4525*
1 42
4612
118
4530*
143
4625*
119
4565*
144
4625*
120
4537
1 45
4615
121
4550*
146
4615
122
4537
147
4620
Well Number
Elevation,
Well Number
Elevation
148
4645
174
4960
149
4645
175
4975'
150
4645
1 76
151
4655
177a
152
4662
178
5137
153
4670
179
5150
154
4675
l8Oa
155
4675
181
5153
156
4675
182
5235
157
4687
183
5210
158
4710
184
5180
185
5145
159
160
4712
186a
161
4712
187
5275*
162
4735
188
5250*
163
4745
189a
5150*
164
4750*
190a
5150*
4795
191
165
166
1 92
5190
167
193a
5210
168
194a
169
195a
5173
170
196
5155
1 71
197a
5150
172
198
5237
173
199
5232
w
0
Well Nwnber
Elevation
Well Nwnber
Elevation
200
201
4320
226
4320
202
4330
227
4290
203
4370
228
4360
204
229
/
205
230
206
231
207
232
/
/
/
/
/
/
/
/
/
/
/
/
/
/
/
/
/
/
/
/
/
208
233
209
4310
234
210
4310
235
211
4325
236
212
4315
237
213
4337
238
214
4337
239
215
4 310
240
216
4317
241
217
4310
24 2
218
4310
243
219
4305
244
220
4290
245
221
4285
246
222
4317
247
223
4300
248
224
4285
249
225
4315
250
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v. A.
78
0 0
26.20.14.224
rehlrcc
n d Burr
14.234
.Il.W.mcl
Youngbloo,
14.242
do.
79
14.374
14.332
do.
do.
17
66
14.343
do.
67
I4 .I 11.
do.
18
14.4llh
do.
14.413
do.
75
14.424
do.
80
15.224
inbcrcc
63
-
k Burl
15.224"
do.
63
15 3 I 4
90
15314
01
15.334
96
r
-r
Loclllon
6/54
4280
15.U3
1/51
4280
.96
15.344
2/48
4280
130
1\53
4280
!06
15.424
2/48
4280
130
15.424
3/49
4280
I45
15.424
2/52
4280,
193
15.444
4/48
4284
147
17.133
-
4247
17.133
1/53
4247
26.20.15.334
15.344.
E.
N.
'1
T
23.144
23.234
23.234
210
I2
23.234
400
12
T
T
51
Y
Y -
. i
c
c
50
:
-"
2
-
Wall
CICl
-
r
I
.P
LOC.li00
3
e
0
208
21.19.20.334
iwcem
$ 3
-4
"5
I"
x3
0
+$
m
dB
c
-
-
T
-
-
-
-
-
E , "
::
4421
308
-
4/49 ' 4 4 2 1
210
148.6P
5/24/.(9
-
IO/>)
4421
350
139.88
1/25/55
T
2/49
4421
250
l3lDO
7/19/49
T
250
10.334
20.334
"
.
12/54
Drill. co.
20.334n
loilia
Uc.criprioo
WilliMla
10.334a
nestom
Drill. Co.
m.343
;. E.
McKnric
10.433
do.
6/49
4421
210
131.08
1/29/49
T
2Od43
Ucstcrn
Urill. co.
1/53
4421
300
144.25
1/25/55
T
139M
12393
7/29/49
-
218
179.61'
5/13/55
T
151.16
9/17/55
PI
-
21.lll
30.214
193x1) 4400
8/51
4425
-
4450
-
1912(?) 4437
9/52
4415
225
144 8 4
189.33
5/21/49
1/25/55
PI
ilc11rc
12/54
Drill. 6.
4344
200
106.61
1/12/55
-
12/14
4344
I50
98.07
2/31/54
-
-
71.20
1/12/15
T
A
-
Ilimhrc.
Ysllcy
Drill.
31.123
32.211
34.114
-
co.
!J,'A.
ISSM
Younghload
27.10.2.424
2.444
5.244
L
do.
-
61.25
-
0
8 2
'4
I
I
I
I
I
I
I
54
55
dote
Vdtrr
produclnp
intcrvn1
level " (depth*,
mcn.,fc)E
J.R. Reeves
1/50
4180
22.18.34.132
8. Flower
10179
4200
230
180
4020
10179
190-240
D,S
22.18.34.141
R. Umpltrcs
8/80
4200
249
174
4026
169-247
U
23.18.12.100
w.
Glare
8/80
4200
250
170
4030
8/80
8/80
150-250
D
24.19. 7.442
24.19.20.421
P. Kcrr, Sr,
2/61
7/61
150
272
107
100
4121
4168
2/61
7/61
115-150
149-272
D
C. Kerr
F. Ken
4228
4268
3/59
4175
117
56
4119
3/59
.7- 12
38-115
I
P. Kerr, J I .
F. Kerr. Sr.
-176
4155
150
90
4065
-176
90-140
I
abandoned
24.20.1.4100
7/17
4155
95
57
4098
7/77
50- 95
I
250-450 gpm.
24.20.1.410b
F. Kerr.. St.
3/74
4155
120
50
4105
150
60
42
4110
4128
24.20.
F . Kere
4/61
12/50135
6/51
4170
z4.20.1.422a
F. Kerr, SF.
F. Kerr
69-118
55-150
I
24.20.1.422
3/74
4/61
7
4144
12/50
6/51
27- 67
11/60
4158
50
62
4108
11/60
42- 62
4/53
4164
112
37
4127
4/53
37-103
11/60
4160
63
45
4115
11/60
38- 6 3
D
4/73
100
35
180-200
D
150
70
4123
4120
4/73
8/66
4158
4190
8/66
88-131
-179
4180
224
80
4100
-179
174-224
1
8/64
3/49
4180
300
60
4120
8/64
70-200
I
4175
111
3/61 238
4175
3/64
4175
537
2/49
8/64
4175
4180
139
643
60
4/64
4180
4177159
407
54
24.20.
1.240
24.20.1.410
7
lo
11
12
13
14
15
16
4.211
24.20. 9.424
C.E. Raark
24.20.12.242
F. Kerr
24.20.13.414
17
18
24.20.19.230a
C.E. b a r k
C.E. b a r k
A. Smith
R. MoraleS
M.E. Walker
24.20.19.243
R.C.
19
24.20.19.244a
20
21
24.20.19.24Lb
M.E. Walker
48
J.E. Little
M.E. Walker
R.C. EIaeav
B. Walker
M.E. Walker
M.E. Walker
norria, Macaw,
24.20.14.342
24.20.19.000
24.20.19.230
24.20.19.244
44
22
24.20.19.
23
24.20.19. 44
24.20.19.444a
25
327
22.18.19.321
24.20.19.444
mEa"
5/60
100
4170
4151
67
,
0
dcepened
I
*
*
D
D,S
50-112
3/61
50-238
4120
8/64
30-100
62-217
I
4126
4018
4/64
218-iO7
I
5160
40-190
1
4137
2/62
7/58
34- 62
30- 98
68-100
D,S
4065
4080
66- 90
4075
12/59
100-148
2/60
D.S
I
53
4127
1/69
4145
4/53
79-199
25-125
I
25
4127
I
deepened
I
205
deepened
4177
Bogart
26
24.20.22.112
24.20.22.421
C.E. m a r k
2/62
4165
G. Kerr
7/58100
4165
24.20.23.31
J.R. Walter5
1/74
4165
100
29
24.20.25.31
c.
30
31
24.20.25.4
24.20.25.422
Ken
R.A. Kerr
J.H. Barter
2/60
4170
50
4175100
90
150
1/69199
4180
32
33
24.20.27.121
Kerr C a t t l e CO.
4/53
4/53
4170
4177
27
28
!
i
I
1
i
125
125
24.20.29.323
L. Smith
24.20.29.333
M. Smith
11/47142
4186
24.20.29.341
24.20.29.34la
M. Smith
5/61228
4/62
4180
M. Smith
4180
48
490
37
24.20.29.34lb
M. Smith
3/48
4180
38
24.20.31.221
24.20.31.221n
D. MeGhee
1/74
5/73
4190
98
140
24.20.31.221b
D. MeChee
4190
65
4190
160
160
39a
40
41
24.20.31.221~
24.20.33.333
D. McGhee
24.20.34.444
E. Kerr
42
24.20.34.444a
43
24.20.36.222
44
25.19.
7.133
45
24.19.
7.143
E.L.
E.L.
K.L.
N.L.
46
25.19.
1.210
25.19.
7.234
35
~
12/59
36
49
24.19.7.234d
25.19.
1.2340
50
25.19.
51
25.19. 7 . 2 3 4 ~
D. MeGhee
T.H. MCCWLB
5/73
1/74170
9/54
8/62100
.
4129
5/61
4/62
65-228
80
4110
1/74
100-140
HW
50 gpm. deepened
5/73
60-160
M6M
65
4125
4125
5/73
MLM
80
4110
1/74
50-115
100-170
deepened
deepened
50 gem. deepened
50
4132
8/62
80-100
S
S
46- 96
4182
4182
30
22
4160
4/51
20- 30
145
32
4148
8/53
16-145
5/59
2/57120
4193
283
30
4163
100-280
5/59
T.W. MeConls
-173
4205
R . 1 . McDonald
5/66 109
4205
Rlchlns and
NeDmold
7.234b
0.n. Vonnoy
11/51106
4205
420510/48
93
38
70
4205
4205
estimated comple
tion d at e
I
D
4195
11/53
MLM
118
4180
110 3/51 150
I
1
8/53
L. Shnnnon
D
4132
4/51
Kere
Kerr
Folk
Folk
D
43-123
48- 98
51
4190
4180
28
2i
65
83
35
-173
5/66
50- 90
4135
4100
4110
3/51
11/53
45-150
4167
D
T
50-82
*
95
42- 90
*
s o l i d r x P %loo',
w r y h u t . T ,212"
very
ll0l "iltCr
l191
JO5
30
f.Lb7
1/34
l%-JOIl
1
150
1111
I10
86
l,0117
/a110
3/51
2/79
l5-150
611-110
I'
2/79
1197
4220
3/64
4183
205
58
41?8
3/64
109-205
T
I
T.H. tlcx::wl8
7/63
4218
JOO
84
1,134
7/63
R4-300
I
1..
3/59
4193
125
56.
4137
3/59
95-125
0
D
12
U.1.J.
7.142
l'olk
33
25.19.
7.3U
I..
8 I,
28.19.
7.421s
55
25.20. 1.242
l1.A.
56
25.20.8.111
57
25.20.10.111
Slwmon
K.B. IIIIrgctt
Il8tCb
IlCVlCtt
1/51
3/51
(1hlIL.r)
58
25.20.10.222
\'"lL,y IvI~Sbgtur1im lh11r.C11
7/76
4190
180
73
4117
7/76
100-180
59
25.20.10.ma
r r ~ ~ t w ~ ~ ~ i " t t-151,
1190
100
36
1,154
-1%
36-100
170
ClllllCl,
60
61
25.20.10.233
B I J ~ D I ) Uros.
1/L9
4196
25.20.10.244
1/54
4197
70
62
4/70
U i s l m p Bros.
1ll.9
4197
4197
226
63
25.20.10.214n
25.20.10.2441,
L. stex..,rt
s. l:rlgl,t
64
25.20.10.334
1/60
4200
170
65
66
25.20.10.344
BiSlnop
8 . Bisl,op
4200
195
25.20.10.344a
W.A.
2/59
6/52
4200
155
67
25.20.10.413
lhssey
25.20.10.143
B . Bishop
4200
4200
240
68
10162
7/48
69
70
28.20.11.434
25.20.12.123
S.C. Wright
4166
1200
T.U. U ~ C m f s
2/79
4187
71
25.20.13.124
8 . Veck
12/63
4195
72
25.20.13.213
B . Veck
5/65
4195
73
25.20.13.213a
G. Wright
123
25.20.13.214
B . Veck
9/48
7/61
4195
74
4195
75
25.20.13.221
B . Veer
3/64
76
25.20.13.221a
8. Veck
77
25.20.13.233
78
25.20.13.233a
79
80
25.20.13.2331,
25.20.13.343
81
25.20.13.344
82
25.20.13.344a
83
25.20.13.f.33
84
25.20.13.433a
85
86
25.20.14.132
87
2520.15.244
Communicy
Carh. Church
87n
25.20.15.342
88
25.20.15.411
89
25.20.15.444
B . G . Willis, Sr.
90
25.20.16.333
T.H. MeCant~
91
25.20.16.333n
T.R. McCants
25.20.15.240
30- 70
70-226
D
I
30-160
160
I
I
I
I
I
D
I
59
60
40-59
80
4141
1/60
60-169
4140
2/59
45-185
6/52
55-155
4120
10162
19-165
34-107
108
68
4132
6E108
4/66
140
65
4122
2/79
400
80
4115
12/63
40-230
281
96
4099
5/65
56-246
345
55
4140
7/61
200-280
I
1195
400
80
4115
3/64
4195
260
75
4120
70-260
C. Rudiger
4/66
4109
4136
I
decpened
C.J.
90
63
3/64
4/66
I
I
deepened
3/64
104-164
Uishop
107
3/61
4199
4199
GOO
Rudiger
L.F. Rudiger
L.F. Rudiger
5/52
12/52
4199
4210
145
200
Rudiger
2/68
4210
Rudiger
4210
Rudiger
2/52
2/68
4205
200
Rudiger
12/56
4205
150
Wriahe
5/68
4210
7/58
M. Traeey
9/66
5/80
E. Woods
L.F.
L.F.
L.F.
L.F.
S.O.
60-135
dry
30-123
D
55
4144
47
4163
12/52
60-135
60-200
272
76
4134
2/68
135-277
I
150
45
4165
2/52
50-150
80
4125
2/68
60-195
D
D
100-150
D
275
70
4140
5/68
60-250
I
4210
120
75
7/58
80-120
D
4210
200
76
4135
4134
9/66
D
1/53
4208
4208
210
158
140-200
16@-190
40
4168
1/53
125-155
11/72
4212
150
85
70-150
D
4215
350
60
4127
1155
11/72
3/62
3/62
80-103
240-349
l
3/62
4218
142
71
4114
3/62
1/51
4215
142
10162
4220
1220
150
60
4160
292
208
90
76
92
25.20.16.333b
T.H. MeCants
93
25.20.20.244
Baer Cattle Co.
94.
95
25.20.20.244a
25.20.20.444
B a a Farm
H. Hatch
3/81
3/57
96
25.20.22.313
S. Wright
4/55
97
98
25.20.22.313a
G.S. T i p p e t t e
25.20.23.100
S. Wright
99
25.20.23.323
100
4226
3/54
129-150
4136
3/87
4144
4/55
95-292
75-200
45-100
102-203
1/48
10160
4215
203
75
4140
10/60
H . Haceh
6/59
4220
197
85
4135
6/69
25.20.23.3l2
G. De vilblis s
8/49
4220
129
101
102
25.20.23.342a
H. llareh
4/53
4220
172
25.20.23.443
E.A. Merrell
3/62
4223
217
83
4140
3/62
103
25.20.23.443n
G. De vilblis s
8/53
4223
217
157
4166
117-217
5/83
104
25.20.23.443b
G. De vilblis a
120
58-64
25.20.23.443~
4223
300
107
4116
3/49
6162
1050
25.20.24.111
EA. ncrrcll
D. Carbine
3/49
6/62
4223
105
5/80
4210
220
110
4100
106
25.20.24.132
Ricblne Inc.
7/75
1215
395
112
107
25.20.24.133
D. Ritellins
3/58
300
eo
108
z5.20.2f1.233
109
25.20.24.313
mmordson
Clydcl, Devnun,
4/60
1215
4212
4220
11/53
102
I
I
I
I
I
I
D
l
32-107
98-172
I
60-120
118-241
I
5/80
120-130
160-190
D
4103
7/75
82-398
T
4138
3/58
80-225
I
103-226
226
315
D,S
I
60-142
4220
4220
'
72-91 (306 SP~);
123-140 (loo+ gpd
I
3/61
5/52
162
deepcned
83
4137
4/60
85-205
I
Riclllnn
110
111
25.20.24.313n
25.20.25.11.3
It. Jundt
7/52
4220
200
60
4160
3/62
4225
328
130
4095
7/52
3/62
100-195
I~~I,L
YUI~H
~,~,
57-193
I
112
25.20.25.223
Rlchltls Inc.
3/77
4230
sno
1nu
15122
3/77
125-800
I
developed well
(surged); no l o g
(same as 92)
cl ean out, no l o g
cl ean ed out 10162
113
25.211.25.244
D , Richllltl
111.
25.20.25.221
Rlchlllr nron.
12/49
115
25.20.25.314
Rlehills Inc.
116
117
118
25.20.25.314a
25.20.25.314b
25.20.25.331
25.20.25.334
25.20.25.3340
119
120
121
122
123
128
129
124
125
126
127
130
131
132
133
134
135
136
137
138
139
140
141
25.20.25.334b
25.20.25.424
25.20.25.424n
25.20.25.434
25.20.25.434n
25.20.25.443
25.20.25.443n
25.20.25.444
25.20.25.Uk
25.20.26.111
25.20.26.133
25.20.26.140
25.20.26.144
25.20.26.144a
25.20.26.241
25.20.26.2Lla
25.20.26.243
25.20.26.243a
25.20.26.244
25.20.26.244a
25.20.26.34L
42499u
280
5237
160
4/67
4230 120
514
Rlehins
2/53
12/47
7/51
3/48
2/55
4230
4230
4230
4240
4240
304
Richills
4240
4250
4250
4245
4245
4249
424997
4260
4260 129
4220
4225
4225 120
299
506
232
200
150
500
198
E. Richills
Richins
Richins Fnrm
E. Richins
Richins Bros.
Richins Fnnn
Richins 81’0..
R.H. Waael
D. Richins
Richins Bros.
D . Richins
Richins
BIOS.
H . Hatch
J . Reager
E A . Mrrell
Merrell
G. DeVilbiss
R. Crvm
E. CeUm
G. DeVilbiss
S.A.
T.R. Crvm
A. Nerrell
T.R. crm
B. Veck
5/54
6/51
3/61
2/52
12/49
1/49
11/58
12/52
1/59
11/49
4/57
11/56
9/65
4/76
3/49
3/61
11/61
7/49
10153
4/76
2/52
2/78
4225
4225
4225
4225
4225
4225
4230
4230
4230
4159
5/54
215-223
231-271
57-160
4110
4/67
70
4160
2/53
90
4150
2/55
115-160
265-510
100-300
52-107
85-102
63-115
90-100
:28-312
90
4160
3/61
107
102
115
350
140
70
11/58
12/58
1/59
9/56
4/57
112
4105
4113
90
4135
9/65
4/76
3/49
3/61
71
110
65
104
4154
4120
4165
4126
10153
7/76
2/52
2/78
97
500
204
152
146
180
751
44-55
120
350
505
153
200
750
186
500
4109
4152
4163
4131
4150
,
57
115-285
1-446
80-228
150-200
60-150
190-500
50-195
120-468
72-204
98-152
126-146
142-180
200-751
60-120
1-350
340-505
85-153
113-180
150-750
60-185
I
I
I
I
D
D
*
*
D
I
I
I
I
1200 gpm
Clean-OYt,
no log, see 142
142
143
144
145
147
146
25.20.26.344a
25.20.26.344b
25.20.26.344~
25.20.27.
25.20.27.144
25.20.27.222
8. Veek
148
149
150
25.20.27.233
25.20.27.240
25.20.27.240a
8. Wright
R.E. Evans
R. Bredrickson
151
151a
25.20.27.24Ob
25.20.27.240~
K.E. Smith
152
25.20.27.322
25.20.27.340
25.20.27.34Oa
25.20.27.342
25.20.27.400
25.20.27.400a
25.20.27.412
25.20.27.412a
25.20.27.422
s.
153
154
155
156
156a
157
158
159
B. Veck
115
80
4115
4150
12/61
7/53
80
4210
4118
4140
4120
1/73
8/59
4/66
4/55
8/76
8179
4220
4225 245
L225
205
320
392
75
126
4145
3980
4099
4/55
8/76
8179
8/75
10180
4225 135
4225
240
250
120
4090
4105
8/75
10/80
4/79
5/74
5/64
4/55
11/60 ,
4/80
3/76
9/63
4/51
4220
4230
4230
4230
4230
4230 120
4225
4225
4225
287
792
300
220
4114
4110
4130
4155
4165
4110
4085
4130
4145
4/79
5/74
5/64
4/55
11/60
4/80
3/76
9/63
4/57
446-526
75-220
87-148
194-200
I
I
123-204
60-211
130-250
T
8. Veck
F. s t o k e s
s. Wright
D. Blair
c / o S . Wright
P. Agullar
Wright
8. Wright
8. Wright
s.
Wright
D. Flint
1. Parker
S . Wright
s. wcighr
Animas Farmers
95-485
118-218
54-110
117-157
60-197
152-198
500
218
120
157
197
200
12/61
7/53
1/73
8/59
4/66
4230
4230
4230
4220 102
4220
190
250
713
230
154
90
106
120
100
75
65
140
95
80
78-198
280-320
120-155
230-240
200-240
160-180
210-240
175-275
180-250
500-800
100-300
80-215
150-190
210-246
230-705
82-148
50-151
I
I
I
I
D
D
I
l
D
well
160
161
25.20.27.430
25.20.27.4305
162
25.20.27.430b
163
25.20.27.433
25.20.27.443
25.20.27.444
25.20.27.444
25.20.27.444n
25.20.29.410
25.20.29.423
25.20.29:124
164
165
166
167
168
169
170
171
25.20.29.4240
s. Wright
s. Wright
s. Wright
4/65
2/57
3/55
4230
S i d Wright
3/62
s.
8/58
4230
4230
423095
4230
423087
4240
4230
4230
4230
Wright
8. Wright
s. w i g h t
S . Wright
J.E.
Little
J . E . Little
J.P.. L i t t l e
J.E. L i t t l c
4/66
10165
2/55
5/72
5162
11/62
2/63
4230
4230
526
222
100
80
4130
4150
270
75
4155
4/65
2/57
3/55
218
217
250
210
124
90
4140
4138
4135
4130
4143
3/62
8/58
4166
10165
2/55
92
100
440.
440
165
355
72-122
190-440
250-385
I
I
I
D.
D
I
1
I
72
4158
2/63
205-355
deepened
I
deepened, no log
2s.20.29.4241,
25.20.33.430
I d f l m m & h1o1d/ 4 9
174
175
177
25.20.34.134
25.20.34.140
W.A.
58
55-125
42311
125
6/69
4230
685
W.A. Tyler
6/53
4233
160
Tyler
4/51
1,230
185
04
4146
4/57
25.20.34.140"
8.11. l y l o r
5/65
4230
105
4125
8/65.
105-900
I
I
176
25.20.34.144
W.A.
11/61
Tyler
4232
900
222
100
4132
11/61
104-215
I
178
25.20.34.144n
R.V.
4/62 Tyler
4232
400
100
4132
4/62
297-325
380-400
I
179
2C.20.34.144b
W.A.
4232
104
1" 50
I
25.20.34.224
1/62
4232
184
94
4138
1/62
181
2S 20.34.224a
4/57
4232
154
94
4138
4/57
182
183
25.20.34.240
25.20.34.240n
Tyler
R.A. llnteh
R. llRtell
R. Ilntch
R . Hatch
2/50
180
6/11
5235
120-710
6171
l
4235
123
92
4112
3/59
710
146
4143
117-145
3/59
I
1%
185
186
187
188
189
25.20.34.244
R.
4235
1.148
133-350
2/57
H.H.
25.20.34.244b
V . llorch
CatLon City Stove
10161
3/52
4235
25.20.34.244e
25.20.34.333
R. Anrnldva
R.D. Anraldva
2/78
1/76
4240
25.20.34.333a
4240
350
146
140
128
203
205
87
25.20.34.244n
2/57
10148
25.20.34.398
R. Anrsldva
1/76
4240
325
191
25.20.34.333~
W.A.
4240
25.20.34.340
Tyler
M. DeVilbriss
6/53
192
8/58
4240
176
216
195
25.20.34.343
C.M.
5/63
4240
193
25.20.34.344
Tyler
N.T. IkVilbrisr
8/76
194
25.20.34.344a
W.A.
196
25.20.34.344b
25.20.34.422
172
173
n.h.
LOU
99
4131
I
100-210
6/69
470-685
HBfCI,
Hatch
4235
4235
80-160
58-70
D
104-154
D
I
10148
54-144
110
4125
10161
122-140
80
4155
70-128
103
4137
3/52
76-203
2/78
D
D
100 gpm
181-205
D
30 g a l - b a i l e r
test
190
197
Tyler
W.A. Tyler
Wesrern Cottan
120
82-95
4120
1/76
6/53
170-250
I
84-176
I
100
4140
8/58
117-217
I
300
110
4130
5/63
4240
248
109
4131
100-300
174-224
4130
1/58
4240
180
110
4/48
6/53
4240
110
72-74
4237
200
11/50
4237
125
7/48
4237
121
90-180
50-110 4/48
I
D
I
I
dry, abandoned
90-170
Oil
198
25.20.34.422a
w e s t e r n cocton
Oil
199
25.20.34.422b
WesterCotton
..
55
4182
11/50
60-120
Oil
200
25.20.34.434
W.A.
Tyler
25;20.34.434a
W.A.
Tyler
3/57
12153
4240
201
4240
220
'1 5 3
202
25.20.34.4Yb
W.A. Tyler
8/48
4240
117
203
25.20.34.440
25.20.34.440a
E.T. Lee
4240
300
222
25.20.34.444
E.T. Lee
E.T. Lee
E.T. Lee
W.A. Tyler
3/64
3/62
4/68
6/67
2/63
5/48
W.A. Tyler
8 . Veck
11/52
1157
4242
204
205
206
207
25.20.34.444a
25.20.34.444b
W.A. Tyler
4240
4242
4242
4242
4242
208
25.20.34.44Le
209
25.20.34.444d
210
25.20.35.132
211
25.20.34.223
.8. Veek
4/62
4230
4237
212
25.20.95.2230
8 . Veck
7/53
90
4150
I
3/57
96-153
90
100
4150
3/64
4140
3/62
58-117
D
I
90-280
I
170-524
524
300
287
cleaned. no l o g
I
I
I
cleaned, no l o g
58
4181
5/48
58-118
4140
1/57
90-255
I
504
90
130
4107
4/62
82-504
I
4237
205
85
4152
7/53
100-180
120
163
260
cleaned, no l o g
I
213
25.20.35.223
8. Veek
4237
120
48-108
214
25.20.35.313
8. Veck
2/78
4237
480
180-480
215
216
25.20.35.313a
8.
Veek
B . Veck
2/56
4237
200
200
4037
4150
8 . Veck
218
8 . Veck
12/73
4237
4237
210
130
87
25.20.35.313~
25.20.35.314
6/53
3/48
4237
217
4137
25.20.35.314a
8 . Veck
7/62
4237
305
363
100
219
134
4103
25.20.35.313b
I
80-200
2/56
6/53
deepened
I
deepened
106-210
65-125
12/73
155-280
7/62
99-308
I
I
deepcned
I
deepened
322-348
220
25.20.35.314b
8 . Veck
1/62
L237
200
221
25.20.35.314~
8. Veek
7/51
160
70
4167
7/51
60-160
222
25.20.35.340
8 . Veck
7/66
4237
4240
580
125
4115
7/66
66- 90
100-576
I
223
25.20.35.343
8. Veek
5/65
4240
541
110
4130
5/65
303-541
224
25.20.35.343a
B . Veek
7/62
4240
225
8 . Veek
226
25.20.35.343a
25.20.35.343b
8. Vcek
7/55
7/53
4240
4240
580
200
75
95
4165
4145
7/55
7/53
I
I
I
221
25.20.35.344
8 . Vcek
2/52
4240
160
80
4160
228
25.20.35.3148
B. Vcck
12/47
4240
120
229
25.20.35.400
8 . Vcck
1/61
4240
495
90
4150
1/61
95-494
I
230
231
232
25.20.35.433
8 . Vock
8 . Vcck
3/64
12/47
4214
4244
260
120
75
1,165
3/61.
70-260
60-108
I
25.20.35.434
25.20.35.434n
8 . Vcck
5/52
4214
190
73
4171
5/52
100-190
deepened
cleaned. no l o g
100-190
well d r l l l c d t o
120,deepcned LO
200, plvgged t o
160 fc.
120-160
rcsred @ 2000 8pm
60-120
~
234
25.20.3S.1143
29.20.39.4436
8 . Vock
D. V w k
5/65
1/57
4244
4244
620
31n
90
4154
1/57
340-620
188-318
1
235
2 36
25,20135.443b
U. Vuuk
3/55
4244
280
80
4164
3/55
88-274
1
237
25.20.35.444
8 . Vack
2/57
4244
310
90
4154
2/57
230-300
I
238
239
25.20.35.444n
26.18.16.310
8 . Vcek
202
J.G. Urguhnrr
7179
4244
4720
240
26.19.20.222
MI. Warncl, Jr.
5/51
4440
4 35
350
1173
0500
400
272
4228,
1/73
242
26.19.31.133
Ray Cordon
Richins F u n
3/52
4340
400
88
4252
3/52
243
26.19.31.134
26.19.31.331
26.19.31.333
G.W.
Edwards
4/49
3/62
4340
180
386
110
9/64
4340
4340
241
244
245
246
247
248
26.19.31.333n
26.19.31.333b
J. Gouthicr
J. GnuLhice
J. GnuLhieC
8.. Alba
26.19.31.333~
26.20. 2.344
1. Edvards
249
250
26.20.
8. Warn1
251
26.20.
R.H. W m e l
252
26.20.
C.P.
2.344a
8. W&l
257a
2.344b
3.000
Lot 34
26.20. 3.100
Lot 36
26.20. 3.100
Lot 34
26.20.3.130
26.20.3.200
26.20.3.320
26.20. 3,331
258
26.20.
259
260
26.20.3.343
26.20.3.400
262
26.20. 3.4CJa
261
26.20. 3.400
Lor 8
263
26.20.
3.410
V a l lVeiye w
Presbyterian
264
26.20.
3.410a
265
266
267
253
254
255
257
256
3.340
Wearherby
4340
99-199
D
115
130
100
4210
4240
4340
4260
400
980
250
200
585
11/55
4260
300
75
8/48
4260
156
200
110
4340
5/48
1/62
10159
199-225
260-270
340-350
s
190-400
D.8
dry
4230
42'5
6/65
2/56
I
110-385
3/62
150-350
9/64
6/65
I
360-980
I
11/55
I
1
75-157
lOl59
80-200
D
7/66
4240
E.C. Richardson
5/61
4240
215
128
4112
5/61
4/73
125-215
4/73
7/75
163-200
D
9/80
179-192
202-222
D
c l e a n e d , no l o g
D
N.H. D e V i l b i s s
4/73
4240
200
122
C.F.
4/73
4246.
200
140
4118
4106
D. Richins
K. b a r k
7/75
9/80
4245
4250
250
249
140
I35
4105
4115
C. Riehardaon
3/76
4250
220
100
4150
3/76
180-200
D
8. Hicks
9/74
4250
Tyler
L.C. T y l e r
L. T y l e r
1/76
4250
4250
200
200
D
D
90
4160
9/74
200-220
D
170
124
84
4126
4166
1/76
4/57
150-200
127-177
D,S
D
4250~
200
132
4118
12/75
144-176
D
11/79
4250
253
128
4122
11/79
B. Veck
4/65
4250
603
26.20. 3.420
26.20. 3.4?03
Richins, lnc.
1/65
4/61
4250
200
134
4116
1/65
J.T. Hill
4250
125
26.20.
8 . Upshaw
1/76
4254
225
200
4125
4164
4/61
1/76
3.433
B.H.
4/57
12/75
deepening
I
E. Richardson
Mart~iin
deepencd
I
2156
83-200
280-440
4185
- 5 gpm
I
D
100-114
196-245,
90
114-200
95-213
D
D
25 gal
bailer
test
'
268
26.20.
3.434
D. R i c h i n s
2/79
4254
246
268a
269
26.20.
3.440
D. Ovens
8/80
5/79
9/74
4260
4254
4254
322
285
260
3/59
1/65
4243
4243
95
95
1/65
7/74
4243
4243
203
300
380
613
2/62
1/53
4243
80
4163
4125
4135
270
271
26.20. 3.443
26.20. 3.443
26.20. 4.000
P.3. Hardt
26.20. 4.144
L.W. Roark
1. Rorrk
272
273
26.20.
4.144s
274
26.20.
4.144b
275
276
277
26.20. 4 . 1 4 4 ~
26.20. 4.144d
T. Upshav
C. noark
L. Roark
L.W. mark
Roork
C. Bimer
4/59
1/62
4243
4240
4240
4/52
I. Roark
Ronzk
W. mark
W.W.
278
26.20. 4.244
26.20. 4.244a
279
280
26.20. 4.244b
26.20.4.324
M. D e V i l b i s s
W.U. Raark
L. Roark
281
26.20. 4 . 3 2 4 ~
282
283
26.20.4.324b
26.20. 4 . 3 2 4 ~
W.W.
284
26.20. 4.334
H.W.
285
286
26.20,4.344
26.20.4.344n
26.20.4.344b
W.W.
26.20. 4 . 3 4 4 ~
26.20.4.420
W.W.
26.20.
W.W.
287
288
289
290
291
4.422-
26.20.4.430
W.W.
W.W.
C.E.
J.C.
Ronrk
Ronrk
Roork
Rcnrk
Ronrk
Ronlk
Ronrk
Ronrk
200
200
91
115
130
140
4163
4145
4124
2/79
8/80
5/79
180-200
282-312
D
4114
4148
9/74
3/59
250-280
200-255
D,S
4148
1/65
95-200
90
4153
1/65
6-380
183
78
4060
4165
7/74
2/62
390-603
150
200
115
105
4240
200
69
3/63
6/62
4245
4245
631
248
90
125
3/52
6/50
4245
4245
186
106
4171
4155
4120
1153
100-146
4/59
1162
4/52
3163
6/62
D
D
D,S
I
I
deepened
I
D
I
70-200
285-631
121-248
I
1
9/55
4241
4/65
3/57
4246
4246
294
500
200
110
90
105
4156
4141
90-290
9/55
4/65
90-198
3/57
4/52
2/49
4246
42U
4245
180
109
200
70
4176
4/52
85-175
61-109
120
4125
205
72
4173
4/79
3/52
160-200
72-200
D
4245
4246
245
117
4129
2/77
130-215
1
4/79
3/52
2/77
cleaned
80-195
105-162
65-106
4131
deepened, cleaned
1
6
I
cleaned
.
~
26.20. 4.444
26.20. 4.444U
.I.C. Iloark
J.C. Hawk
8/66
6/61
4250
273
42511
750
205
292
'
1.092
4125
st66
6/61
117-750
190-205
291
26.20. 4.444b
J.C. Roork
3/52
4250
200
90
4160
3/52
85-195
295
26.20.5.100
A . PEtUr.IIOII
1/79
4235
250
102
4133
1/77
170-214
296
26.20.5.143
O.A.
Lce
12/53
4235
204
297
298
26.20.5.1434
0.A.
Loo
6/54
4235
375
26.20.5.333
T.J. Tati
5159
4238
407
100
4138
5/59
299
300
26.20.5.334
O.'\.
5/52
4238
206
26.20. 5.344
6/59
4237
275
3
0
1
302
303
305
304
26.20. 5.420
T.J. Tori
O.A. Lee
O.A. Lee
3/56
4240
304
4240
207
D.A. Lcc
1/56
6/53
4240
270
5/65
205
500
306
26.20.
5.444~3
E. Veck
O.A. Lee
4240
4241
5/51
4240
155
307
26.20.
8.440
C.F. B n t h e r b y
303
26.20. 8.443
C.F. Weatherby
9/53
6/65
4251
308
4250
500
4125
309
310
311
312
313
314
315
316
317
26.20. 8.444
C.F. Wierhcrby
26.20.
J.L.
9.144s
26.20. 9.144b
26.20. 9 . 1 4 4 ~
26.20.9.144d
26.20.9.144e
26.20.9.144f
26.20.9.222
318
26.20.9.224
S. Wood
319
26.20.9.243
s.
320
26.20.
S.W. GBrYin
321
26.20.9.244a
26.20. 5.422
26 .'O. 5.222.
26.20.5.443
26.20.5.444
9.144
26.20.
9.244
IRG
D.A.
Lee
4251
Roach
6/79
7/64
J.L.
Roach
6/51
4250
J.L.
RoaCh
4/51
4250
I
10 6Pm
200-395
100
4137
6/59
95-405
I
50-200
I
1-202
I
160-200
D
I
I
93
4147
9/56
68
4172
5/51
87-270
85-205
145-500
I
72-155
I
300
4115
185
135
88
1 47
60
150-500
7/64
100-300
4162
6/51
147-185
4/51
7/53
61-136
I
deepened
I
I
I
I
cleaned. no l o g
J.L. Roach
7/53
354
97
4190
4153
Roach
3/53
4250
200
60
4190
3/53
85-185
J.L. Roach
3/52
4250
200
75
4175
3/52
90-200
J.L. Roach
4/48
4250
148
64
4186
4/48
n.
4/59
L250
200
120
4130
4/59
70-148
120-128
145-165
10154
4250'
200
7/74
3/66
4255
610
4118
7/74
44-610
l
590
346
340-590
3/57
4255
4255
2/58
4255
300
90
I
I
I
2/51
12/56
4255
4257
148
397
73
80
woads
GaTYin
I
D
137
110
4145
101
4154
3/66
3/57
4165
2/58
4182
4177
2/51
12/56
26.20. 9.244b
26.20. 9.244~
26.20. 9.340
325
26.20.9.342
M. Wood
4/64
4257
488
100
4157
4/64
326
327
26.20.9.342a
26.20. 9.344'
X. Wood
2/51
4257
150
72
4185
2/51
H. Wood
86
26.20.
9.434
P. Wood
6/49
6/53
4257
328
4257
360
120
4137
6/53
110-235
277-308
335-340
329
26.20.9.443
26.20. 9.i43a
P. Wood
P. Wood
6/62
4260
525
4160
100
6/62
2/60
4260
4145
307
115
2/60
230-525
102-143
197-303
I
330
331
26.20. 9.444
0. Jackson
700
120
4140
6/79
26.20.9.444a
G. Jackson
6/79
3/74
4260
332
4260
614
124
4136
3/74
153-614
I
333
26.20. 9.444b
P. Wood
2/57
4260
325
80
4180
2/57
133-152
205-210
272-288
295-308
I
334
26.20. 9 . 4 4 4 ~
26.20.10.112
H. Wood
4/48
335
N.L. crvm
2/62
4260
4252
400
336
26.20.10.112a
10152
4252
202
83
337
338
339
26.20.10.122
26.20.10.142
26.20.10.142a
L. CTYrn
E A . Richardson
E.C. Pdchardson
E. Richardson
E X . Richardson
311
342
343
344
345
26.20.10.212
Church (saints)
26.20.10.211
s.
26.20.10.243
26.20.10.243a
R.T. Bonar
B.G. Boner
26.20.10.320
M. Crum
346
26.20.10.321
347
348
26.20.10.321n
M.L. Crm
U.L. crum
349
26.20.10.342n
s. Wright
s. wrishr
350
351
26.20.10.344
A . RUlnos
26.20.10.3440
s.
352
353
26.20.10.3446
J.W. l' lllllips
2/71
26.20.10.344~
s, wrrghlr
/,/A8
26.20.10.342
Wright
WrlghL
~
140
100-330
136-300
80-145
297-303
324-350
I
135'360
72-148
I
75-140
189-400
4169
10152
83-200
4/63
88-294
4166
12/52
70-145
4/63
4255
293
4165
90
4255
145
89
2/50
4260
171
6/49
4260
124
2/53
4260
151
80
4180
2/53
100-151
6/60
4260
234
6/60
116
165
4185
4203
8/50
4/51
50-230
76-116
I
4265
4265
116-165
I
12/65
4260
500
4175
80
79
62
85
4180
8/50
4/51
85-300
357-500
I
65-171
1-73
12/65
I
I
4260
195
63-195
I
4260
117
58-117
12/54
4260
310
157-287
I
I
6/49
4260
180
75
4185
6/49
9162
1/52
4270
65
4205
9/62
1/52
4270
230
4210
200
430
4270
144
116-165 dccpened
I
I
84-144
294-302 (150 %Pmh
344-348 (150 wm)
I
1/50
60
deeoened
I
D
4/48
80-180
82-230
120-200
deepened
I
12/52
4270
*
I
323
324
26.20.10.122a
cleaned
90-285
322
S.W.
ueepened
100-300
6/65
125
4250
4250
J.L.
60
D
Carvio
S.W. carvin
8. Wood
H. Woods
340
I
1511
125
I
dccpened
~
26.20.10.1,34
12/61
42711
466
26. 20. 10~ 434~ ~
12/52
1,270
224
6/51
4270
26.20.10.C34b
'i
I
i
12/61
420-414
161
80
4190
6/51
152-2'4
71-161
95
3/66
158-430
56-160
I
1
120
65-120
I
160-230
I
4260
230
4178
242
82
7/59
72-102
182-242
C
1/53
4260
4168
220
92
1/53
80-219
6/52
4270
175
70
6/52
60-174
1/52
4270
85-200
26.20.11.232
8/48
4269
200
16 7
26.20.11.342
3/52
2/48
4270
243
76-243
4270
160
156
75-160
86
4244
3/55
272
110
4170
2/70
302
300
4180
200
120
4160
7/58
38-207
11/52
99-274
100-190
70
1/53
93-195
26.20.10.444
3/66
4271s
400
5/49
4274
163
359
26.20.10.4441,
10147
4274
360
26.20.10.444~
12/52
4274
361
26.20.11.111
7/59
362
26.20.11.111n
363
2~.20.11.140
364
26.20.11.144
365
366
367
368
26.20.11.413
26.20.13.222
369
26.20.14.121
2/70
4330
4280
370
26.20.14.121n
2/65
4280
371
372
26.20.14.121b
7/58
4280
26.20.14.122
26.20.14.124
9/51
11/52
4280
4280
3/55
26.20.14.124a
2/48150
4280
375
376
26.20.14.133
4280
200
26.20.14.224
1/53
6/48
4295
225
377
378
26.20.14.234
7/50
26.20.14.23a
100
I
I
cleaned
4290
400
.4290
238
4210
abandoned,
casing pulled
129-157
D
abandoned,
casing pulled
26.20.14.311
3/55
4280
401
26.20.14.311a
1/62
4280
5 3
331
382
383
384
26.20.14.321
2/72
26.20.14.321a
10150
4280
4280
26.20.14.324
8/53
4285
4163
500
223
4166
500
119
26.20.14.330
26.20.14.332
5/74
2/62510
4284
500
220
26.20.14.332a
8/54
330
103
4177
117
3/55
75-200
2/72
I
I
deepened
I
deepened
110-200
I
I
I
deepened
deepened
8/53
.
4064
5/74
200-495
100
4185
110-330
343-649
I
I
4285
26.20.14.334
2/61
4285
4284
90
4194
388
26.20.14.334a
s i56
4284
65?
350
8/54
2/61
100
4184
8/56
70-325
389
26.20.14.334b
6/58
4284
500
13
4154
26.20.14.343
2/62
4290
700
100
4190
6/58
2/62
138-498
390
391
392
26.20.14.343a
26.20.14.411
6/54
4290
300
105-300
I
4285
265
4195
4167
6/54
8/53
95
118
393
26.20.14.413
394
26.20.14.423
2/49190
3/48
4290
4290
80-190
75-196
D
395
26.20.15.124
9/58
4270
420
396
397
26.20.15.224
26.20.15.242
3/61
7/51
4275
4280
400
398
26.20.15.242a
1/48
4280
120
55-120
399
400
26.20.15.314
4/69
6/53
550
352
190-550
26.20.15.314a
4270
4270
100
401
26.20.15.314b
5/53
4270
4180
200
90
402
26.20.15.334
403
26.20.15.33
3/51
1/57
404
26.20.15.343a
405
26.20.15.344
406
26.20.15.YZa
407
408
26.20.25.414
26.20.15.424
409
.
4190
193
90
100
I
I
4180
9/58
131-415
l
4175
3/61
197-400
I
7/51
93193
90
4170
deepened
8/53
196
6/53
5/53
I
I
deepened
I
deepened
100-200
75-200
4280
200
448
2/54
4280
4280
290
76
6/53
4280
206
Crabtree 6 Burt
2/48
4280
130
8. Veck
7/58
i280
COO
8. Veck
2/59
4280
193
26.20.15.426
8. Veck
2/48
4280
130
4 10
26.20.15.424b
8. Veck
3/49 145
4280
411
26.20.14.424~
8. Veck
2/52
4280
412
26.20.15.443
A. Rams, Jr.
413
26.20.15.444
A.
414
415
41511
26.20.15.444a
416
417
2/54
114
3924
4166
6/53
195-285
114-132
156-176
190-204
97
4183
7/58
105-340
55-130
I
I
80
80-130
I
I
I
4200
2/52
100
4180
11/59
133-193
132-502
115
4169
2/61
95-550
11/59
4280
193
501
2/61
4284
550
4/48
4284
147
1/53
4247
26.20.22.220
Roman, Jr.
CInbrrcc & Burt
Wenthcrby
v. k c
8/80
4280
200
4150
280
130
26.20.23.100
D. n"rt0"
405
101
4189
3/60
98-395
J.D. Burton
3/60
5/74
4290
26.20.23.133
4290
260
160
413
5/74
180-240
26.20.17.133
deepened
75-150
380
.
k
77-167
379
386
387
4200
.
dfcmned
374
385
I
41711
26.20.10.444:,
373
.
100
60-147
8/80
164-204
234-264
I
I
cleaned, no l o g
deepcncd
deepened
418
26.20.23.133.1
I419
26.20.23.13Jh
J.U. llllrr~ il
J.D. I I ~ l ' t w l
6/53
4290
2DO
3/49
1/49
4290
101
200
Vuck
6/52
4300
,
4295
420
26.20.23.144
J.D.
421
26.20.23.234
422
26.20.23.234a
U.
U.
Vock
2/55
4300
426
26.20.23.2Mb
8, Vcck
4/51
200
423
26.20.23.244
8. Vcek
2/55
4300
4300
424
425
26.20.23.244n
26.20.23.244b
B. Voek
2/48
8. Vcek
3/49
4300
4300
130
151
427
428
26.20.23.311
T. Dwls
10159
4290
175
26.20.23.311s
T. Dnvis
1/53
4290
429
26.20.23.333
T. Davis
430
26.20.23.439
T. Davis
1/53
4/65
4297
4298
432
26.20.23.433a
T. Davis
5/49
4298
431
433
434
4 35
4%
26.20.23.433b
26.20.24.333
T. Davis
3/51
4298
V.E.
Davis
1/66
4308
26.20.24.333a
V.E.
Davis
3/63
4308
26.20.24.333b
26.20.24.343
V.E.
Davis
1/59
4308
1/55
4310
111
135
320
145
200
288
607
351
350
IIII~LOII
J . Davis
150
6/53
1511-175
65-104
74-198
210
400
D
D
85
4215
6/52
180-209
l
9s
4205
2/55
195-400
I
85-185
400
93
107
135
$207
4183
4163
2/55
10159
4/65
155-400
I
80-130
120.151
I
I
'.?5-170
D
95-111
D
3-135
120-320
D
70-145
65-200
110
4198
1/59
85
4225
1/55
112-351
60-130
deepened
I
I
I
I
I
I
I
deepened
deepened
650 gpm
225-350
\
{
~
'
I
437
26.20.24.133
V. Wasbbum
1/63
4310
438
26.20.24.133s
V. Washburn
3/54
4310
439
26.20.25.211
E.W.
4/53
4320
440
441
26.20.26.243
Y. Washbum
K. Washburn
1/59
4305
4310
442
26.20.26.422a
443
26.20.26.422b
445
26.20.29.100
444
446
447
448
449
205
205
3/54
4260'
200
26.20.29.141
26.20.29.142
V. Washbum
6/75
4/74
4260
V. washbum
500
217
26.20.29.142a
K. Washburn
8/49
26.20.29.311
L. wasbbum
12/63
26.20.29.3lla
1. Washburn
4/53
450
26.20.32.233
K. Washburn
451
26.20.35.111
V. Washburn
2e.20.35.111a
26.20.36.224
26.21.4.444
J.C.
4270
150
11/62
4302
V. Washburn
4/51
R.H. wame1
26.21.12.100
ROaIk
T.A. Baker
26.21.13.430
Phelps Dodge
26.18.
V.A.
457a
457b
27.18.
7.100
27.18.12.120
R. Haoren, Jr.
B. Hogan
457e
4576
27.18.12.220
27.18.12.220a
s.5/80
Mullins
457e
27.18.12.220b
27.18.18.240
5.334
Peterson
103
4202
1/59
.
144-205
48-200
160
loo
4100
4154
6/75
4/74
4/53
84-142
65-150
s
300
108
4194
11/62
D
4302
150
85
4217
4/51
120-300
78-92
136-150
2/71
4330
300
145
4185
2/71
204-300
7/66
4200
4283
230
120
4080
7/66
193-203
4420
150
701
80
301
215
4340
4260
2/72
44 75
4460
193
200
105
120
115
120
113
10151
2/72
5/67
9/80
11/80
4375
4350
.
D. B i L t l e
5/80
4350
E. PeLersm
4475
4375
4350
185
163
163
400
9/80
108-148
4255
11/80
157-197
4235
5/80
115-135
4230
5/80
133-163
5/80
133-163
242
4237
4233
1/73
CalmbYs Electric
27.19.
7.340
c o l m b u s Electric
7/54
4375
155
132
4243
7/54
461
27.19.11.231
V.A.
Peterson
4425
4257
6/63
27.19.11.233
V.A.
Peterson
4425
700
390
168
462
463
27.19.11.333
A. Peterson
6/63
7/53
7/78
4400
227,
464
27.19.11.411
27.19.11.412
V.A.
10/53
4425
4425
605
300
I
.
160
4240
7/78
S
I
4162
9/73
230-500
I
4260
8/58
130-498
328
328
4072
3/55
1-328
I
I
152
4248
8/53
140-300
I
27.19.17.343
G . Wsmel
469
27.19.17.433
470
27.19.17.4338
4708
27.19.18.300
471
27119.18.400
472
473
27.19.18 E 4
27.19.19.100
J.P. Byme
3/74
e.
1/76
4401
4 74
27.19.19.1000
D. Jonzen
12/74
4401
475
27.19.19.110
C. CLlRO"
2/77
4 76
R.L.
3/76
477
27.19.19.110n
27.19.19.120
4393
4393
8.11. s t r n n g e
9/61
4400
300
300
300
300
220
478
27.19.19.200
E. Elbroek
3/78
4400
255
3/55
4400
4400
R.H. wane1
8/53
4400
300
R.H. W O m e l
T. Tovnscnd
6/52
4400
300
3/80
4393
250
170
4223
3/80
220-250
D
4400
311
175
4225
9/78
270-311
D
260
170
190
3/74
1/76
255-260
260-300
D.S
4211
178
4223
12/74
200-300
D
D
D
wane1
9/78
C. Cnthcy
Adam
Koow
,
deepened
I
238
R.H.
4400
135-155
140
R.H. Hamel
27.19.17.332
9/73
8/58
deepened
508
500
27.19.17.330
cleaned. no l o g
250-300
350
467
468
deepened
5/67
4355
27.19.
5/59
deepened
S
4200
5/80
Pererson
Peremon
350-500
I
I
I
T
I
T
I
60
T. Hewlert
V.A.
I
40-132
459
460
7.331
99-299
81-151
1/73
7/72
465
466
I
10152
456
458
'
120
142
D
D
132
4260
457
121-300
100-300
303
4310
4260
1/63
151
4310
4254
4254
4193
200
2/51
4/51
454
455
'
6/48
'
K. Washburn
V. Washbvrn
L. Washbum
453
!
26.20.26.422
Riehcns
117
300
300
175
4218
3/76
280-300
180-300
160
4240
9/61
160-220
160
4240
3/78
L75-255
D
S
15-20 gpm.
deepened
~
4 7')
2/77
480
41 74
481
8/53
4400
4400
4400
5/79
9/76
482
27.19.19.220
R. U.u~lulaao
483
484
27.19.19.220a
27.19.19.220b
485
486
27.19.19.222
27.19.19.240
W. Nlenlnulaa
A111m19 Co. Ctr.
W.J. Purelay
3110
2110-300
4200
4/75
200-JOO
300
200
200
4400
4400
250
1.230
4222
5/79
200-2100
9/76
260-300
9/76
4400
4223
9/76
260-300
4/80
4400
4231
2/61
4kOO
320
260
500
170
178
177
169
146
200-240
146-500
300
130-160
180-200
488
27.19.19.344
W.M.
Mnnsey
10/62
4416
750
160
4256
4/80
3/61
10162
4s9
27.19.19.3C4n
L.L.
Wllcy
2/51
4416
280
130
4286
2/51
150-278
490
27.19.19.433
B.F.
Elnsscy
5/65
4416
800
4416
4413
300
141
4275
140-300
135
'>
178
2/55
500
140-309
4413
213
130
4283
5/59
5/48
192-212
350-370
392-412
425-41S
466-486
F.A.
Cwtltim
4254
27.19.19.4330
W . M . Mnssey
2/55
W.M.
Mossey
493
27.19.19.434
27.19.19.434n
5/59
3/48
494
27.19.20.110
Animna School
DiSt.
1/78
4402
486
190
4212
1/78
495
'27.19.20.123
27.19.20.123a
h i m a s School
1/66
12/63
4400
"400
496
310
160
4240
12/63
395-495
140-300
27.19.20.124
27.19.20.124a
H . G . Adam9
1/64
11/66
162-272
220-300
498
27.19.20.142
7.H.
5/74
240-300
20 8pm
499
500
27.19.20.142a
501
27.19.20.143
27.19.20.141,
100 gpm
180 gpm
502
503
491
492
496
487
H.B. Lupc
Animrs School
1/64
4405
272
152
4253
11/66
5/74
4405
4405
300
320
147
135
4258
4270
F. Gaurhier
10153
210
138
4267
150-210
10153
P. Gaulhier
F. Gnuthier
9/75
9/74
4405
4405
4405
300
265
4140
9/74
260-300
265-300
27.19.20.210
R. Adam?
7/62
4405
4235
7/62
280-300
W.A. B a l l a r d
2/66
4405
300
340
170
27.19.20.211
140
4265
504
27.19.20.230
K. Braoks
10177
4405
303
175
4230
300-340
256-303
505
27.19.20.322
Massey Bras.
3/71
4405
800
170
4235
2/66
10177
3/71
1/53
4405
311
130
4275
1/53
158-311
4/49
2/49
4421
135-210
4421
210
208
497
aaPtiEt CIWCI)
Waiters, Jr.
300
*
deepened
deepened
deepened
Farm
506
27.19.20.3225
507
508
27.19.20.334
27.19.20.334s
P. GnULhier
8. Gauthier
F. Gavlhier
509
27.19.20.334b
F. Gaurhier
3/49
4421
25.0
200-250
510
511
27.19.20.334~
8. Gaufhier
4/49
210
135-210
27.19.20.334d
F. Gnuchier
10153
4421
4421
512
513
27.19.20.3k3
27.19.20.443
W.M.
4421
800
4421
514
27.19.20.44s
F. Gaurhier
W.M. Maasaey
5/71
6/49
5/65
4421
250
800
515
516
27.19.20.443b
B.R. Medlin
12/52
300
27.19.20.444
27.19.20.444~
B.R. Medlin
H.N. Massey
6/57
10162
4421
4422
4422
517
350
m3
138
171
4283
10153
42%
5/71
aocpened
deepened
12/52
132
151
4289
4271
154-303
6/57
160
160
4262
4240
10162
200-30
7/72
5/80
138-265
deepened
Stare Hw Dept.
7/72
4400
518a
E. Barnes
5/80
4400
308
180
4220
519
27.19.21.111
J.D.
7/73
4400
285
170
4230
520
27.19.21.113
J. Gaurhier
7/62
4400
185
155
521
27.19.21.120
W. Upshaw
2/76
4400
300
168
4245
4232
3/75
4450
285
170
4280
3/75
5/61
5/78
4450
445p
190
170
4280
5/61
320
205
4245
5/78
260-320
Gray
4/80
4450
252
205
4245
4/80
208-252
44.75
400
235
4240
2/81
278-31R
4475
400
270
4205
3/80
345-365
308
218
138
4299
12/54
143
4282
8/51
,
522
27.19.22.100
523
27.19.22.100a
524
27.19.22.320
C.W. Rifter
W.P. Anderson
D.C. Looney
525
27.19.22.340
A.J.
205-215
258-298
170-250
7/73
7/62
245-285
5250
27.19.22.410
L. Rains
2/81
27.19.22.430
3. Lasher
3/80
527
27.19.29.334
528
27.19.30.213
27.19.30.214
27.19.30.2148
F.A.
T.D.
T.D.
J.E.
531
532
27.19.31.220
27.19.31.222
S A . Strange
11. Strango
1/76
4450
4271
1/76
4450
300
300
179
lola2
145
4305
10162
150-285
533
27.19.32.200
3. Johnson
12/76
4437
300
1ao
4257
12/76
260-300
534
27.19.34.113
L.R.
10177
4475
275
215
4260
10177
227-247
535
27.19.14.114
27.20,2.420
R , Adam
9/52
4475
225
R.11. Wnmol
5/61
4338
520
529
530
12/54
4437
Neal
8/51
Neal
3/71
5/59
4415
4425
GaULhiCr
Offult:
Adanw
4425
800
413
20 spm
cleaned, no l o g
260-300
2/76
526
'
deepened
225-228(1-2
gpm),
312-316 (7-20 gpd
128-218
400-800
213-413
200-225
130
4208
5/61
1
500 8pm
100 Bpm
165 m m .
decpencd
536
I
112-218
27.19.21.100
27.19.21.110
Croom
deepened
deepened
'750
300
518
I
Maasey
133-208
I
~
:
'
~~
wl.
vamd
27.20. 2.421413
K.11.
It<allal
12/54
12/54
539
27.20. 2.444
11.11.
Ilnmul
540
27.20.2.44485
R.11.
llllmul
541
27.20. 4.130
542
543
P
12/54
434f,
4341,
200
2011
150
12/54
4344 110
T. Vtt)~hhurn
12/59
27.20.10.433
V. Waahhurn
27.20.12.230
A. Payno
544
27.20.12.244
II.
545
27.:0.12.244n
O.C.
546
27,20.12.442
11. Moore
547
27.20.12.424
548
27 ?0.12.444n
549
27.20.12.444b
D.C.
550
27.20.13.124
551
27.20.13.410
R.H.
552
537
27.20.
5 38
2.421,
MOOTC
4341,
S
4214
12/54
150
4234
12/54
1,288
83
150
4205
12/59
110-150
10152
4350
4350
4375
150
550
120
4230
5/74
100-150
180-550
S
5/74
1/57
251,
122
4253
1/57
135-215
D
4255
1/57
100-170
197-283
I
I
80
I
3/48
4375
170
2375120
483
J.0. Curry
3/49
4317
200
H. Noore
4/71
4377
600
130
4247
4/71
11/51
4377
255
217
4160
8/61
J.D. curly
3/49
4375
200
133
4242
3/49
96-200
Warnel
3/61
4375120
198
4255
3/61
130-198
27.20.16.400
E l Paso Nature1
GBs co.
7/65
4350
432
18
4332
7/65
553
27.20.16.443
K. Washburn
5/51
5/51
105-125
F. Hill
5/59
125
405
4260
27.20.21.110
4350
4400203
90
554
556
4197
27.20.21.222
E. Ridlens
11154
4350
240
100
5/59
11/54
110-220
*7.20.22.111
27.20.26.310
A.
Hi11
2350
4425
240
E. Elbrock
1/55
10170
27.20.26.311
L. careia
3/53
4425
225
559
27.19. 5.110
1/76
4450
360
560
27.19. 8.210
B. Da rne ll
c. Yerbrough
9/59
4475
561
28.19.10.330
G. Johnson
563
562
28.19.16.240
B. Veck
28.19.16.244
564
28.19.16.440
565
566
:::
Kill8
King
320
4250
I
I
I
I
I
160
4265
10170
120-320
4260
1/76
120-220
320-360
I
190
201-303
D
4525
4500
B. Veck
3/66
4525'
6/63
4525
28.19.16.444
B. Veck
J. Woodard
4/53
4525
380
28.19.16.444a
H.V.
Green
4525
567
28.19.17.211
W.A.
Tyler
4/75
9/58
568
28.19.17.221
W.A.
Tyler
11/61
4500
800
337
735
569
28.19.20.244
J.L.
Foster
4/61
4550
570
28.19.21.240
8. Veek
11/59
4525
350
700
220
571
572
28.19.27.200
F. Croom
J.L. Dunagan
11/70
4575310
4515
391
600
272
573
28.19.27.314
28.19.Y.430
3.1. b a g a n
4/63
10164
4575
1000
272
4599
370
8. Darnell
4525
300
180
4345
576
28.20. 2.200
28.20.12.210
4/10
6/68
H. Strange
8/56
4550
285
250
4300
6/68
8/56
577
29.1c1.20.220
3. C ~ o o m
416;
4655
60
35
4615
4/64
10- 50
578
29.19.34.300
29.20. 2.i10
Cockrell Corp.
G. Godfrey
10171
4800
120
90
579
5/63
4800
30.20.24.330
D. RIchards
7/74
4875
478
520
4710
4322
580
520
600
10111
5/63
7/74
468-490
537-600
M.F. Johnson
S
S
100-240
222
190
4303
4310
12/59
330-350
349-649
5/63
D.S
S
deepened
deepened
225
4300
4255
3/66
6/63
1-416
I
220-380
225
200
4300
4/75
202-512
4300
4301
9/58
11/61
220-337
199
I
I
I
I
250
4300
4305
4/61
262-350
122-430
S
11/59
4265
11/70
3151375
s
4303
4/63
260-340
I
4303
10164
310-370
180-230
D,S
237-283
S
8
C
S
S
200-412
150 gpm
I
I
270
4355
*
C
5/63
574
575
I
240-600
129-250
12/59
28.19.27.230
I
D
100-200
302
350
700
880
765
4500
64
S
1/57
555
,
~~
date estimated
deepened
I
I
D
deepened
deepened
%
, ..
.
3240
3997, , m e o
P"
P
ab
4107.
T 22s
4 0 94,
4160.
T 23s
T 24s
T 25 S
T 26s
R 17W
T 30 S
+
T 31 S
T 32s
i127
T 33 S
' a
49.0
b
5150
e
51 50
\
Platel Water-level
i
contourmap
in 1913
R 21 W
a
T 34 S
a
a
R 19W
-3997
9
e
'
b
e
e
o
4000
-3801
010
3856
b
0 .
0
b
,4004
4102
a4115
4101
.4302
4351
c
4263
4272,"
m
430,jf
.
~
4234
41 23
.4123
04103
4109
-4102
,4248
,4263
-4265
-4273
$257
-
4276
.4298
e4276
0
Plate2 Water- level contour map 1976-81
,46000 c+ e
.
.
Profile A -A'
530
5 IO
49 0
v)
h
E
a,
47c
a
0
c
YY
c
0
.c
g
-
45c
0)
w
43c
410
1913
I
IO
39c
I
I
20
70
60
30
I
I
40
50
I
I
I
1
80
90
Distance (miles)
LandSurface
\
\""""-,
1
\
"WaterLevel
4101
I
4001
470C
I
I
12
I
16
4
8
I
28
I
I
36
32
20
Distance (miles)
24
I
I
Comparative Profile B-B'
29
1977
T2 3
-
c
ffl
E
4201
4101
4001
I
12
I
I
4
I
8
16
I
24
I
I
20
I
I
I
28
32
36
Distance (miles)
4270
424c
4210
0
n
0
4.15C
WaterLevel
I
6
3
I
8
I
7
I
I
5
I
4
I
I
2
1
1977
I
9
Distance (miles)
4
41OOo
I
I
2
I
3
I
I
I
I
I
I
9
I
8
Distance(miles)
Profile E-E'
t
2
.J:
N
!
E
Fi
4600 -
Land Surface
4500 0
ro
9
I
I
"
-
/ WaterLevel
1977
/
'
/
/
/
/
/ - -
\
0
0
0
\
4200 -
-/
0
I
b
/
\
I
<-/
0
/
4
4100 -
40000
I
I
I
2
I
3
I
4
I
75
Plate 3 Selectedwater-level
I
6
I
I
I
8
9
profiles
I
IO
I
II
Distance (miles)
I
14 12
I
13
I
I
1715
I
16
I
I
18
e 4
44
8
88
e14
25
3b
2 5